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Sample records for west siberia russia

  1. Bazhen Fm matured reservoir evaluation (West Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Parnachev, S.; Skripkin, A.; Baranov, V.; Zakharov, S.

    2015-02-01

    The depletion of the traditional sources of hydrocarbons leads to the situation when the biggest players of the oil and gas production market turn to unconventional reserves. Commercial shale oil and gas production levels in the USA have largely determined world prospects for oil and gas industry development. Russia takes one of the leading place in the world in terms of shale oil resources. The main source rock of the West Siberia, the biggest oil and gas basin in Russia under development, the Bazhen Fm and its stratigraphic and lithologic analogs, is located in the territory of over 1,000,000 square kilometers. Provided it has similar key properties (organic carbon content, porosity, permeability) with the deposits of the Bakken Fm and Green River Fm, USA, it is still extremely poorly described with laboratory methods. We have performed the laboratory analysis of core samples from a well drilled in Bazhen Fm deposits with matured organic matter (Tmax>435 °C). It was demonstrated the applicability of the improved steady-state gas flow method to evaluate the permeability of nanopermeable rocks. The role of natural fracturing in forming voids was determided that allows regarding potential Bazhen Fm reservoirs as systems with dual porosity and dual permeability.

  2. Oil field experiments of microbial improved oil recovery in Vyngapour, West Siberia, Russia

    SciTech Connect

    Murygina, V.P.; Mats, A.A.; Arinbasarov, M.U.; Salamov, Z.Z.; Cherkasov, A.B.

    1995-12-31

    Experiments on microbial improved oil recovery (MIOR) have been performed in the Vyngapour oil field in West Siberia for two years. Now, the product of some producing wells of the Vyngapour oil field is 98-99% water cut. The operation of such wells approaches an economic limit. The nutritious composition containing local industry wastes and sources of nitrogen, phosphorus and potassium was pumped into an injection well on the pilot area. This method is called {open_quotes}nutritional flooding.{close_quotes} The mechanism of nutritional flooding is based on intensification of biosynthesis of oil-displacing metabolites by indigenous bacteria and bacteria from food industry wastes in the stratum. 272.5 m{sup 3} of nutritious composition was introduced into the reservoir during the summer of 1993, and 450 m3 of nutritious composition-in 1994. The positive effect of the injections in 1993 showed up in 2-2.5 months and reached its maximum in 7 months after the injections were stopped. By July 1, 1994, 2,268.6 tons of oil was produced over the base variant, and the simultaneous water extraction reduced by 33,902 m{sup 3} as compared with the base variant. The injections in 1994 were carried out on the same pilot area.

  3. Petroleum habitat of East Siberia, Russia

    SciTech Connect

    Clarke, J.W.

    1994-03-01

    East Siberia comprises three petroleum provinces - Lena-Tunguska, Lena-Vilyuy, and Yenisey-Anabar - that occupy the area of the Siberian craton. Petroleum has been generated and has accumulated in Precambrian rifts beneath the sedimentary basins and, more importantly, within the section of the basin itself. The platformal deposits of the basins extend beneath overthrusts on the east and south and are covered by sedimentary rocks of the West Siberian province on the west. Permafrost and gas hydrate deposits are present throughout most of East Siberia. In the Lena-Tunguska province, rifts that developed during Riphean time are filled by thick sedimentary rocks, in which petroleum deposits have formed. In Early Cambrian time a barrier reef extended across the East Siberian craton from southeast to northwest. A lagoon to the west of this reef was the site of thick rhythmic salt deposits, which are the main seals for petroleum in the province. The sedimentary sections of the platform cover ranges in age from Late Proterozoic to Permian. More than 25 oil and gas fields have been discovered in the province, all in Riphean through Lower Cambrian rocks. 17 refs., 7 figs.

  4. The peculiarities of water acidification in European Russia and Western Siberia

    NASA Astrophysics Data System (ADS)

    Moiseenko, T. I.; Gashkina, N. A.; Dinu, M. I.; Kremleva, T. A.

    2015-06-01

    Studies have proven the anthropogenic acidification of waters developing over the spacious territories of European Russia and West Siberia. The acidification is exhibited by the waters of small lakes characterized by bedrock consisting of granite and quartz formations. The acidified lakes of high water transparency, pH values below 6, and the prevalence of strong acids in the anion composition account for 4.4% of 201 lakes of European Russia and 8.2% of 166 explored lakes in the taiga and tundra regions of western Siberia. The main factor causing the development of acidification over the European Russia is the emission of technogenic sulfur by metallurgical smelteries. As for western Siberia, this is the combustion of associated gas at oil-producing enterprises. These processes combined with natural factors determine the complicated mechanism of anthropogenic acidification of waters.

  5. Radioactive Elements in Soils of Siberia (Russia)

    NASA Astrophysics Data System (ADS)

    Baranovskaya, N. V.; Rikhvanov, L. P.; Matveenko, I. N.; Strakhovenko, V. D.; Malikova, I. N.; Shcherbakov, B. L.; Sukhorukov, F. V.; Aturova, V. P.

    2012-04-01

    The Center of State Sanitary and Epidemiological Surveillance Department in Krasnoyarsk Territory, Krasnoyarsk In the course of long-term research a great deal of information on the content of natural and artificial radionuclides in soils of the Siberian regions has been obtained and summarized (Altai and Krasnoyarsk Territories, Altai Republic, Buryatia, Yakutia, Khakassia, Irkutsk, Novosibirsk, Tomsk Oblasts and a number of other Siberian regions). The content level of U(Ra), Th and K in soil of studied areas is within the range of values obtained for soil of other areas of Russia and the world and defined, first of all, by radioactivity of parent rocks. The authors have studied the total level of specific activity for 137Cs most completely in soils of different Siberian regions. The maximum density of such sites with global fallouts (nuclear air explosions in Novaya Zemlya, Lop Nor, Semipalatinsk etc.) is typical for the areas of Altai Territory and Buryatia Republic. Elevated level of radiocesium (to 1000 and more than Bq/kg) is characteristic for the sites adjacent to the area of NFP (Seversk, Zheleznogorsk). Our data obtained in determination of plutonium in soils of different Siberian regions excess remarkably its background accepted for Siberia. Particularly high accumulation levels of Pu in soil were observed in the zones of NFP operation (Seversk, Tomsk Oblast; Zheleznogorsk, Krasnoyarsk Territory, in the sites of accidents fallouts at underground nuclear explosions in Sakha Republic (Yakutia). Abnormally high ratio of 238Pu/239,240Pu in soils of Sakha republic, Aginsk Buryatia Autonomous District, Krasnoyarsk Territory has engaged our attention.

  6. Permafrost sequences on Kurungnakh Island, Lena Delta (NE Siberia, Russia) as key site of the late Quaternary environmental history of West Beringia

    NASA Astrophysics Data System (ADS)

    Wetterich, S.; Kuzmina, S.; Andreev, A. A.; Kienast, F.; Meyer, H.; Schirrmeister, L.; Kuznetsova, T.; Sierralta, M.

    2009-04-01

    Late Quaternary permafrost sequences are widely distributed in the arctic lowlands of Siberia. Because the existence of permafrost has been sensitive to climate changes during the Quaternary past, such frozen deposits are regarded as an archive of palaeoenvironmental dynamics. Late Quaternary palaeoenvironments of the Siberian Arctic were reconstructed by combining data from several fossil bioindicators (pollen, plant macro-fossils, ostracods, insects, and mammal bones) with sedimentological and cryolithological data from permafrost deposits. The late Pleistocene to Holocene sequence on Kurungnakh Island (Lena Delta, NE Siberia) reflects the environmental history of West Beringia and covers glacial/interglacial and stadial/interstadial climate variations with a focus on the Middle Weichselian interstadial (50-32 kyr BP). The record mirrors the development of periglacial landscapes under changing sedimentation regimes which were meandering fluvial during the Early Weichselian, colluvial or proluvial on gently inclined plaines during the Middle and Late Weichselian, and thermokarst-affected during the Holocene. Palaeoecological records indicate the existence of tundra-steppe vegetation under cold continental climate conditions during the Middle Weichselian interstadial. Due to sedimentation gaps in the sequence between 32 and 17 kyr BP and 17 and 8 kyr BP, the Late Weichselian stadial is incompletely represented in the studied outcrops. Nevertheless, by several palaeoecological indications arctic tundra-steppe vegetation under extremely cold-arid conditions prevailed during the late Pleistocene. The tundra-steppe disappeared completely due to lasting paludification during the Holocene. Initially subarctic shrub tundra formed, which later retreated in course of the late Holocene cooling.

  7. East Siberia and Bering Sea, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    On June 5, 2001 MODIS captured this true-color image of Eastern Siberia and the Bering Strait. To the right of the image is the western tip of Alaska's St. Lawrence Island. Credit: Jacques Descloitres, MODIS Land Rapid Response Team

  8. Teaching Soil Science and Ecology in West Siberia: 17 Years of Field Courses

    ERIC Educational Resources Information Center

    Siewert, Christian; Barsukov, Pavel; Demyan, Scott; Babenko, Andrey; Lashchinsky, Nikolay; Smolentseva, Elena

    2014-01-01

    Since 1995, soil-ecological field courses across climatic zones in West Siberia have been organized by scientists from Russia and Germany to meet growing demands for better land use practices. They are focused on virgin landscapes and soils undisturbed by anthropogenic influences to facilitate the learning processes by excluding concealing changes…

  9. A "Mesosiderite" Rock from Northern Siberia, Russia: Not a Meteorite

    NASA Technical Reports Server (NTRS)

    Treiman, Allan H.; Lindstrom, David J.; Schwandt, Craig S.; Franchi, Ian A.; Morgan, Matthew L.

    2002-01-01

    A possible mesosiderite meteorite was found in the area of the Putorana Plateau, Noril'sk district, Siberia, Russia. Although this rock resembles a mesosiderite in its hand-sample aspect and in having Ni-bearing iron metal, it is not a meteorite. This inference is based on the lack of a fusion crust, the lack of cosmogenic nuclides, oxygen with terrestrial isotope ratios, and several mineral chemical criteria. Most likely, the rock is from the iron-metal-bearing basalts of the Siberian Trap basalt sequence, which are mined for their base and platinum-group metals. Mesosiderite imposters like this may be recognized by: (1) the presence of Cu metal in hand sample or as microscopic blebs in the low-Ni metal (kamacite), (2) the absence of high-Ni metal (taenite), and (3) the presence of iron carbide (cohenite) enclosing the kamacite. Even if these macroscopic tests are inconclusive, isotopic and mineral chemical tests will also distinguish rocks like this from mesosiderites.

  10. Tectonosedimentary history of the sedimentary basins in northern west Siberia

    SciTech Connect

    Kunin, N.Ya.; Segalovich, I.E. )

    1993-09-01

    Sedimentary basins of northern west Siberia belong to the Arctic tectonosedimentary province. This basin evolved dissimilarly compared to those in the Urengoy and more southern areas, which resulted in substantial differences in the geologic characteristics. Seismic surveys indicate that the basement surface in northern west Siberia occurs at great depths, in places exceeding 15 km. The depressions of the basement surfaces are filled with the thick Paleozoic and Mesozoic sequences. The paper discussed the results of seismostratigraphic analysis of more than 13,000 km of regional common-depth-point profiles. These profiles identified systems of east-west-trending and isometric structures in the region. Some of the structures are buried; others are mapped in the upper horizons of the sedimentary cover and decrease in magnitude with depth. Cretaceous marine sediments that were deposited under deep-water conditions and did not compensate for the tectonic subsidence are widely present in the region. Noncompensated sedimentation was the longest from the Late Jurassic to the Hauterivian-Barremian on the Gydan peninsula and in adjacent areas. The Jurassic section is dominate by ingressive marine sediments. Sediments that did not compensate for tectonic subsidence widely occurred in the Early Jurassic and resulted in deposition of petroleum source rocks. Triassic and Jurassic strata occur conformable in most of northern west Siberia. Significant deformation of the Triassic sediments are identified in the periphery of the Triassic marine basin. This indicates that surrounding structures were thrust against northern west Siberia at the Triassic and Jurassic time boundary. Isometric structures of high magnitude were formed during the Paleozoic structure stage and these structures continued to grow through the Triassic and Jurassic. These and other results of seismostratigraphic analysis suggest the high oil potential of the region.

  11. Giant gas field of northern West Siberia

    SciTech Connect

    Grace, J.D.; Hart, G.F.

    1986-06-01

    The 66 fields discovered since the 1960s in the northern West Siberian basin contain at least 22 trillion m/sup 3/ (777 tcf) of proved gas, almost one-third of the world's reserves. Half of these fields are giants (> 85 billion m/sup 3/ or 3000 bcf of reserves). These include the largest and second-largest gas fields in the world-Urengoy (8.099 trillion m/sup 3/ or 286 tcf of gas) and Yamburg (4.81 trillion m/sup 3/ or 170 tcf of gas)-as well as most of the other ten largest gas fields in the world. The West Siberian basin occupies a 3.4-million km/sup 2/ (1.31-million mi/sup 2/) arctic lowland immediately east of the Ural Mountains, extending north under the Kara Sea. It is a composite basin, with Mesozoic-Cenozoic basin fill on top of a Paleozoic basin that overlies a crystalline Archean-Proterozoic framework. The productive zones in the northern basin are principally in the Neocomian section (at an average depth of 2800m or 9200 ft) and the Cenomanian section (at an average depth of 2800 m or 9200 ft) and the Cenomanian section (at an average depth of 1100 m or 3600 ft). The former contains reservoirs with gas, condensate, and oil; the latter contains two-thirds of the region's gas. Gas in Cenomanian reservoirs is almost pure methane. Hydrocarbons in Neocomian reservoirs were generated by thermal maturation of sapropelic organic matter contained principally in the Tithonian Bazhenov shale. Methane in the Cenomanian section appears to be a combination of thermogenic gas from the Bazhenov Suite (or deeper) and biogenic gas generated in the Cenomanian section itself, although workers disagree over how much gas came from each source. Continental glaciation during the Pleistocene may have been important in concentrating the methane in Cenomanian reservoirs.

  12. Studies of The Atmosphere of Eastern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Khodzher, T.; Obolkin, V.; Netsvetaeva, O.; Golobokova, L.; Fukuzaki, N.

    These studies aim to investigate fully the atmosphere in the Southern part of Baikal Region (Eastern Siberia) that is characterized by presence of large industrial centers affecting atmospheric pollution above Lake Baikal. Since 1998, three stations to mon- itor continuously a little gas admixtures, aerosols composition, and ionic and multi- elemental composition of precipitations have been created in the frame of ADORC (Niigata, Japan) program under financial support of Japanese Environmental Agency. Monitoring sites were chosen taking into account different level of anthropogenic in- fluence: Irkutsk (52.3 N, 104.4 E) reflects the processes typical of urban conditions; Listvjanka (51,9 N, 104,7 E) is a site under partial influence of regional pollutants; a high-mountain site (2000 m above sea level) Mondy (51,6 N, 101,0 E) characterizes the background areas. Since 2000, these stations are included into International Acid Deposition Monitoring Network in East Asia (EANET). In Eastern Siberia aerosols origin and composition depend substantially on the season, in spite of the fact that the soil and the earth crust serve as their major sources. Anthropogenic input increases in cold season. Proportion between fifteen elements (Ca, Al, Mg , Na, Cr, Mn, Fe, Cu, Zn, Br, Ti, Rb, Sr, Cl, and Pb) is always the same in spring aerosols having soil dust as a major source. In spring, the concentrations of these elements are 2-5 times higher compared to the other seasons. In winter, the concentrations of such elements as Cu, Zn, Br, Pb, and Sb are a magnitude higher in urban aerosols (Irkutsk) then in the aerosols of rural regions. In soluble aerosol fraction, SO42- ion predominates among anions; NH4+ and 1057;a2+ - among cations, representing 40-60

  13. Magnetic declination measurements over European Russia and Siberia in the 18th century

    NASA Astrophysics Data System (ADS)

    Raspopov, O. M.; Meshcheryakov, V. V.

    2011-12-01

    The paper presents the history of measurements of the geomagnetic field parameters over the territory of Russia in the 18th century derived from archival and literature sources. Topographical mapping of the European territory and neighboring seas of the Russian Empire from the late 17th to the mid 18th century during which magnetic measurements were made was of great importance for determining magnetic declination. The magnetic declination in Siberia and its neighboring seas was measured for the first time during the first expedition of V. Bering in 1728 and then during his second expedition (the Great Northern Expedition) in 1733-1742. Magnetic measurements were carried out along the northern coast of Siberia and in the Bering Sea. The academic group of the expedition performed magnetic declination measurements over southern regions of Siberia (Krasnoyarsk, Irkutsk, Nerchinsk, Yakutsk, etc.) in 1735 and 1736. During the second half of the 18th century, Russian expeditions determined geographical coordinates of the cities of European Russia and carried out magnetic declination measurements for them. During these expeditions Inokhodtsev paid attention to the anomalous magnetic declination in the Kursk region. In his opinion, the anomaly could have been caused by the presence of iron ore.

  14. High-latitude regions of Siberia and Northeast Russia in the Paleogene: Stratigraphy, flora, climate, coal accumulation

    NASA Astrophysics Data System (ADS)

    Akhmetiev, M. A.

    2015-07-01

    The geological structure and development history of superposed depressions on the Arctic coast of East Siberia and Bering Sea region (Chukotka, Koryakiya, northern Kamchatka) in the Early Paleogene are considered with the analysis of their flora and climatic parameters. The paleofloral analysis revealed thermophilic assemblages that reflect phases of maximum warming at the Paleocene-Eocene transition and in the Early Eocene. The appearance of thermophilic plants (Magnoliaceae, Myrtaceae, Lauraceae, Araliaceae, Loranthaceae, and others) in the Siberian segment of the Arctic region is explained by the stable atmospheric heat transfer from the Tethys to higher latitudes and absence of the latitudinal orographic barrier (Alpine-Himalayan belt). The plants migrated to high latitudes also along the meridional seaway that connected the Tethys with the Arctic Ocean via marine basins of the Eastern Paratethys, Turgai Strait, and West Siberia. The migration from the American continent was realized along the southern coast of Beringia under influence of a warm current flowing from low latitudes along the western coast of North America. The palm genus Sabal migrated to northern Kamchatka and Koryakiya precisely in this way via southern Alaska. In the Oligocene, shallow-water marine sediments in high-latitude regions were replaced by terrestrial facies. The Late Oligocene was marked by maximum cooling. Coal accumulation in Northeast Russia through the Paleogene is reviewed.

  15. Influenza A (H15N4) virus isolation in Western Siberia, Russia.

    PubMed

    Sivay, Mariya V; Baranovich, Tatiana; Marchenko, Vasiliy Y; Sharshov, Kirill A; Govorkova, Elena A; Shestopalov, Aleksander M; Webby, Richard J

    2013-03-01

    The rarely identified influenza A viruses of the H15 hemagglutinin subtype have been isolated exclusively in Australia. Here we report the isolation of an H15N4 influenza A virus (A/teal/Chany/7119/2008) in Western Siberia, Russia. Phylogenetic analysis demonstrated that the internal genes of the A/teal/Chany/7119/2008 strain belong to the Eurasian clade and that the H15 and N4 genes were introduced into the gene pool of circulating endemic avian influenza viruses through reassortment events.

  16. Oil and gas potential of the Triassic in west Siberia

    SciTech Connect

    Bochkarev, V.S.; Kulakhmetov, N.KH.; Nesterov, I.I. )

    1993-09-01

    Permian-Triassic rocks are widely spread within the West Siberian basin, and they include volcanics, volcanoclastics, and clastics. Their thickness varies from tens of meters of 3000 m. Recently, three commercial oil pools have been discovered in Triassic effusive-sedimentary rocks. These discoveries, together with other geological and geochemical data, identify the Triassic complex as a major play. Oil-bearing intervals have been found in three different types of sequences; a fourth also may be prospective. The first type is represented by lacustrine-terrigenous sediments, which comprise oil-saturated sandstones interbedded with basalts (the Turin series). Oil influxes were obtained in the Yakhlinskaya and Triyurtin-skaya structures in the Shaim region. The second type is distinguished from the first by the presence of coal-bearing intervals in the upper part. Oil was produced in the Yerofeyev area of the Chelyabinsk garben. The third type differs from the other two by the presence of potassic rhyolites and dacites. Their age is not precisely dated, and supposedly they are of Permian age. The largest oil influxes have been obtained from fractured and eroded rocks of this type in the Rogozhnikovskaya and other places in the Krasnoleninsk region. Rhyodacites often underlie Turin basalts, but locally they occur in the upper part of the series. Triassic and Permian-Trissic rocks of the three types are overlain by Jurassic and Cretaceous rocks with a large break. The fourth type of section is completely terrigenous (Tampei series). It is developed in the northern part of west Siberia. Here Triassic sediments are overlain by the Jurassic complex without a break. According to well-log data, productive horizons occur at Urengoy and Beregovaya (in the Urengoy region).

  17. HLA genes of Aleutian Islanders living between Alaska (USA) and Kamchatka (Russia) suggest a possible southern Siberia origin.

    PubMed

    Moscoso, Juan; Crawford, Michael H; Vicario, Jose L; Zlojutro, Mark; Serrano-Vela, Juan I; Reguera, Raquel; Arnaiz-Villena, Antonio

    2008-02-01

    Aleuts HLA profile has been compared with that of neighboring and worldwide populations. Thirteen thousand one hundred and sixty-four chromosomes have been used for this study. Computer programs have obtained HLA allele frequencies, genetic distances between populations, NJ relatedness dendrograms, correspondence analysis and most frequent HLA extended haplotypes. Aleuts have inhabited Aleutian Islands since about 9000 years BP according to fossil and genetic (mtDNA) records. They are genetically different to Eskimo, Amerindian and Na-Dene speakers according to their HLA profile; this correlates with cultural and anthropological Aleut distinctiveness. No typical Amerindian HLA alleles have been found in a significant frequency. Their HLA relatedness to Saami (or Lapps, northern Scandinavians), Finns and Pomors (North-West Russia) indicates an ancient possible origin from the Baikal Lake Area (southern Siberia) around the present day Buryat peopling area; other origins are not discarded. Aleuts characteristic HLA profile may influence future transplantation programs in the region and be useful to study diseases linked to HLA epidemiology.

  18. Reserve Growth in Oil Fields of West Siberian Basin, Russia

    USGS Publications Warehouse

    Verma, Mahendra K.; Ulmishek, Gregory F.

    2006-01-01

    and field delineation activities between the discovery and the first production years. Because of uncertainty in the length of evaluation time and in reported reserves during this initial period, reserve growth based on the first production year is more reliable for model development. However, reserve growth models based both on discovery year and first production year show rapid growth in the first few years and slower growth in the following years. In contrast, the reserve growth patterns for the conterminous United States and offshore Gulf of Mexico show a steady reserve increase throughout the productive lives of the fields. The different reserve booking requirements and the lack of capital investment for improved reservoir management and production technologies in West Siberian fields relative to U.S. fields are the probable causes for the difference in growth patterns. Reserve growth models based on the first production year predict that the reserve growth potential in the 42 largest oil fields of West Siberia over a five-year period (1998-2003) ranges from 270-330 million barrels or 0.34-0.42 percent per year. For a similar five-year period (1996-2001), models for the conterminous United States predict a growth of 0.54-0.75 percent per year. This abstract presents the contents of a poster prepared for the AAPG Hedberg Research Conference on Understanding World Oil Resources, November 12-17, 2006 - Colorado Springs, Colorado. A paper 'Reserve Growth in Oil Fields of West Siberian Basin, Russia' was published in Natural Resources Research, v. 12, no. 2, June, 2003.

  19. Spatial and Temporal Variability of CO2 and CH4 Concentrations in the Atmospheric Surface Layer over West Siberia

    NASA Astrophysics Data System (ADS)

    Belan, Boris D.; Machida, Toshinobu; Sasakawa, Motoki; Davydov, Denis K.; Fofonov, Alexander V.; Krasnov, Oleg A.; Maksyutov, Shamil; Arshinov, Mikhail Yu.

    2015-04-01

    The investigation of greenhouse gas behavior in the atmosphere plays a key role in predicting the global changes of Earth's climate. In this connection, of particular importance is the study of the distribution of sources/sinks of trace gases in the atmospheric surface layer over the different regions of the globe. In order to fill a gap in the data on greenhouse gas concentrations in Russia, National Institute for Environmental Studies (NIES, Japan) and Institute of Atmospheric Optics (IAO SB RAS, Russia) established a network for GHG monitoring (JR-STATION, Japan-Russia Siberian Tall Tower Inland Observation Network). Gas analyzers and meteorological sensors were mounted at radio relay towers located in different regions of West Siberia. The checking equipment was placed in containers at the tower base. In the containers, the climatic parameters optimal for gas analyzer operation were maintained. The work on the network development started in 2001. Since at each of the sites the measurement duration could be different, in this paper we present the data of the greenhouse gas monitoring for eight sites which give the primary idea on the spatial distribution and temporal dynamics of CO2 and CH4 in the atmospheric surface layer over West Siberia. The analysis of the data showed that the average increase in concentration of carbon dioxide by results of our measurements in this territory increases within 1.95 - 2.53 ppm/year, depending on the area. The analysis of long-term data testifies about existence of growth of concentration of methane within 3.2 - 7.2 ppb / year. The presence of a distributed network of the sites operating in the monitoring regime makes it possible not only to investigate the temporal dynamics of CO2 and CH4 at each site and to determine the spatial differences between the concentrations by comparing the data, but also to plot the distribution charts for different moments of time. This work was supported by the Global Environment Research

  20. Snow algal communities on glaciers in the Suntar-Khayata Mountain Range in eastern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Tanaka, Sota; Takeuchi, Nozomu; Miyairi, Masaya; Fujisawa, Yuta; Kadota, Tsutomu; Shirakawa, Tatsuo; Kusaka, Ryo; Takahashi, Shuhei; Enomoto, Hiroyuki; Ohata, Tetsuo; Yabuki, Hironori; Konya, Keiko; Fedorov, Alexander; Konstantinov, Pavel

    2016-09-01

    Snow and ice algal communities were investigated on four glaciers in the Suntar-Khayata Mountain Range in eastern Siberia in Russia over three melting seasons from 2012 to 2014. Two taxa of green algae and five taxa of cyanobacteria were observed on the glaciers. The algal community was dominated by green algae: Ancylonema nordenskioldii in the lower bare ice area and Chloromonas sp. in the upper snow area. The total algal bio-volume showed altitudinal variation, ranging from 0.03 to 4.0 mL m-2, and was greatest in the middle of the glaciers. The altitudinal variations in the algal community were similar on all studied glaciers, suggesting that they are typical in this region. Observations over the three years revealed that there was no significant change in the community structure, but a significant change in the total biomass. Since the mean summer air temperature was significantly higher in 2012 when algal biomass was greater, the difference in algal biomass among the years is probably due to the duration of surface melting. The community structure on the studied glaciers is similar to those on glaciers in Arctic and sub-Arctic regions.

  1. Geochemical characteristics of organic compounds in a permafrost sediment core sample from northeast Siberia, Russia

    NASA Technical Reports Server (NTRS)

    Matsumoto, G. I.; Friedmann, E. I.; Gilichinsky, D. A.

    1995-01-01

    We studied total organic carbon (TOC), hydrocarbons and fatty acids in a permafrost sediment core sample (well 6-90, length 32.0 m, 1.5-2.5 Ma BP) from northeast Siberia (approximately 70 degrees N, 158 degrees E), Russia, to elucidate their geochemical features in relation to source organisms and paleoenvironmental conditions. Long-chain n-alkanes and n-alkanoic acids (>C19) were most predominant hydrocarbons and fatty acids, respectively, so organic matter in the sediment core was derived mainly from vascular plants and, to a much smaller extent, from bacteria. Low concentrations of unsaturated fatty acids revealed that organic matter in the sediment core was considerably degraded during and/or after sedimentation. The predominance of vascular plant components, the major ionic components of nonmarine sources, and geological data strongly implied that the sediment layers were formed in shallow lacustrine environments, such as swamp with large influences of tundra or forest-tundra vegetation. Also, no drastic changes in paleoenvironmental conditions for biological activity or geological events, such as sea transgressions or ice-sheet influences, occurred at the sampling site approximately 100 km from the coast of the East Siberian Sea during the late Pliocene an early Pleistocene periods.

  2. Geochemical characteristics of organic compounds in a permafrost sediment core sample from northeast Siberia, Russia.

    PubMed

    Matsumoto, G I; Friedmann, E I; Gilichinsky, D A

    1995-10-01

    We studied total organic carbon (TOC), hydrocarbons and fatty acids in a permafrost sediment core sample (well 6-90, length 32.0 m, 1.5-2.5 Ma BP) from northeast Siberia (approximately 70 degrees N, 158 degrees E), Russia, to elucidate their geochemical features in relation to source organisms and paleoenvironmental conditions. Long-chain n-alkanes and n-alkanoic acids (>C19) were most predominant hydrocarbons and fatty acids, respectively, so organic matter in the sediment core was derived mainly from vascular plants and, to a much smaller extent, from bacteria. Low concentrations of unsaturated fatty acids revealed that organic matter in the sediment core was considerably degraded during and/or after sedimentation. The predominance of vascular plant components, the major ionic components of nonmarine sources, and geological data strongly implied that the sediment layers were formed in shallow lacustrine environments, such as swamp with large influences of tundra or forest-tundra vegetation. Also, no drastic changes in paleoenvironmental conditions for biological activity or geological events, such as sea transgressions or ice-sheet influences, occurred at the sampling site approximately 100 km from the coast of the East Siberian Sea during the late Pliocene an early Pleistocene periods.

  3. Distribution of trace gases and aerosols in the troposphere over West Siberia and Kara Sea

    NASA Astrophysics Data System (ADS)

    Belan, Boris D.; Arshinov, Mikhail Yu.; Paris, Jean-Daniel; Nédélec, Philippe; Ancellet, Gérard; Pelon, Jacques; Berchet, Antoine; Arzoumanian, Emmanuel; Belan, Sergey B.; Penner, Johannes E.; Balin, Yurii S.; Kokhanenko, Grigorii; Davydov, Denis K.; Ivlev, Georgii A.; Kozlov, Artem V.; Kozlov, Alexander S.; Chernov, Dmitrii G.; Fofonov, Alexader V.; Simonenkov, Denis V.; Tolmachev, Gennadii

    2015-04-01

    The Arctic is affected by climate change much stronger than other regions of the globe. Permafrost thawing can lead to additional methane release, which enhances the greenhouse effect and warming, as well as changes of Arctic tundra ecosystems. A great part of Siberian Arctic is still unexplored. Ground-based investigations are difficult to be carried out in this area due to it is an out-of-the-way place. So, in spite of the high cost, aircraft-based in-situ measurements can provide a good opportunity to fill up the gap in data on the atmospheric composition over this region. The ninth YAK-AEROSIB campaign was focused on the airborne survey of Arctic regions of West Siberia. It was performed in October 2014. During the campaign, the high-precision in-situ measurements of CO2, CH4, CO, O3, black carbon and aerososls, including aerosol lidar profiles, have been carried out in the Siberian troposphere from Novosibirsk to Kara Sea. Vertical distributions of the above atmospheric constituents will be presented. This work was supported by LIA YAK-AEROSIB, CNRS (France), the French Ministry of Foreign Affairs, CEA (France), the Branch of Geology, Geophysics and Mining Sciences of RAS (Program No. 5); State contracts of the Ministry of Education and Science of Russia No. 14.604.21.0100, (RFMTFIBBB210290) and No. 14.613.21.0013 (RFMEFI61314X0013); Interdisciplinary integration projects of the Siberian Branch of the Russian Academy of Science No. 35, No. 70 and No. 131; and Russian Foundation for Basic Research (grants No. 14-05-00526 and 14-05-00590).

  4. Bryozoans from the Jurginskaya Formation (Famennian, Upper Devonian) of the Tom-Kolyvansk area (Western Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Tolokonnikova, Zoya

    2010-10-01

    Nine bryozoan species are described from the Jurginskaya Formation (Famennian, Late Devonian) from Western Siberia, Russia, namely: Leptotrypella pojarkovi Orlovski, 1961, Rhombopora subtilis Nekhoroshev, 1977, Klaucena lalolamina Yang, Hu, Xia, 1988, Eofistulotrypa famennensis sp. n., Atactotoechus cellatus sp. n., Nikiforopora jurgensis sp. n., Eridotrypella tyzhnovi sp. n., Mediapora elegans sp. n., and Klaucena gracilis sp. n. The studied assemblage shows palaeogeographical affinity with Kazakhstan, Kirgizia, Transcaucasia, China, and the United States of America.

  5. Oil and Gas Resources of the West Siberian Basin, Russia

    EIA Publications

    1997-01-01

    Provides an assessment of the oil and gas potential of the West Siberian Basin of Russia. The report was prepared in cooperation with the U. S. Geological Survey (USGS) and is part of the Energy Information Administration's (EIA) Foreign Energy Supply Assessment Program (FESAP).

  6. 30-year lidar observations of the stratospheric aerosol layer state over Tomsk (Western Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Zuev, Vladimir V.; Burlakov, Vladimir D.; Nevzorov, Aleksei V.; Pravdin, Vladimir L.; Savelieva, Ekaterina S.; Gerasimov, Vladislav V.

    2017-02-01

    There are only four lidar stations in the world which have almost continuously performed observations of the stratospheric aerosol layer (SAL) state over the last 30 years. The longest time series of the SAL lidar measurements have been accumulated at the Mauna Loa Observatory (Hawaii) since 1973, the NASA Langley Research Center (Hampton, Virginia) since 1974, and Garmisch-Partenkirchen (Germany) since 1976. The fourth lidar station we present started to perform routine observations of the SAL parameters in Tomsk (56.48° N, 85.05° E, Western Siberia, Russia) in 1986. In this paper, we mainly focus on and discuss the stratospheric background period from 2000 to 2005 and the causes of the SAL perturbations over Tomsk in the 2006-2015 period. During the last decade, volcanic aerosol plumes from tropical Mt. Manam, Soufrière Hills, Rabaul, Merapi, Nabro, and Kelut and extratropical (northern) Mt. Okmok, Kasatochi, Redoubt, Sarychev Peak, Eyjafjallajökull, and Grímsvötn were detected in the stratosphere over Tomsk. When it was possible, we used the NOAA HYSPLIT trajectory model to assign aerosol layers observed over Tomsk to the corresponding volcanic eruptions. The trajectory analysis highlighted some surprising results. For example, in the cases of the Okmok, Kasatochi, and Eyjafjallajökull eruptions, the HYSPLIT air mass backward trajectories, started from altitudes of aerosol layers detected over Tomsk with a lidar, passed over these volcanoes on their eruption days at altitudes higher than the maximum plume altitudes given by the Smithsonian Institution Global Volcanism Program. An explanation of these facts is suggested. The role of both tropical and northern volcanic eruptions in volcanogenic aerosol loading of the midlatitude stratosphere is also discussed. In addition to volcanoes, we considered other possible causes of the SAL perturbations over Tomsk, i.e., the polar stratospheric cloud (PSC) events and smoke plumes from strong forest fires. At least

  7. A population-based study of the associations of stroke occurrence with weather parameters in Siberia, Russia (1982-92).

    PubMed

    Feigin, V L; Nikitin, Y P; Bots, M L; Vinogradova, T E; Grobbee, D E

    2000-03-01

    Previous studies have established a seasonal variation in stroke occurrence, but none have assessed the influence of inclement weather conditions on stroke incidence in a general population of Russia. We performed a stroke population-based study in the Oktiabrsky District of Novosibirsk, Siberia, Russia. Included in the analysis were 1929 patients with their first occurrence of ischemic stroke (IS), 215 patients with their first occurrence of intracerebral hemorrhage (ICH) and 64 patients with their first occurrence of subarachnoid hemorrhage (SAH): all patients were aged between 25 and 74 years. The cumulative daily occurrence of total strokes and stroke subtypes was evaluated in relation to aggregated daily mean values of ambient temperature, relative humidity and air pressure by means of Poisson regression analysis to estimate the rate ratio (RR) with corresponding confidence interval (CI) and to identify the weather parameters of most importance. In a multivariate analysis, with adjustment for the effects of season, solar and geomagnetic activity, and age of the patients, low ambient temperature (RR 1.32; 95% CI 1.05-1.66) and mean value of air pressure (RR 0.986; 95% CI 0.972-0.999) were important predictors of IS occurrence, while mild ambient temperature (RR 1.52; 95% CI 1. 04-2.22) was an important predictor of ICH occurrence. No relationship between SAH occurrence and any one of the weather parameters studied was revealed. There was no interaction between any meteorological variables that was statistically significant. Inclement weather conditions are associated with the occurrence of IS and ICH in Siberia, Russia. Among the meteorological parameters studied, low ambient temperature and mean air pressure are the most important predictors of IS occurrence, whereas the occurrence of ICH is associated with mild ambient temperature. There is no association between any one of the weather parameters studied and the occurrence of SAH.

  8. Oil and gas resources in the West Siberian Basin, Russia

    SciTech Connect

    1997-12-01

    The primary objective of this study is to assess the oil and gas potential of the West Siberian Basin of Russia. The study does not analyze the costs or technology necessary to achieve the estimates of the ultimate recoverable oil and gas. This study uses reservoir data to estimate recoverable oil and gas quantities which were aggregated to the field level. Field totals were summed to a basin total for discovered fields. An estimate of undiscovered oil and gas, from work of the US Geological Survey (USGS), was added to give a total basin resource volume. Recent production decline points out Russia`s need to continue development of its discovered recoverable oil and gas. Continued exploration is required to discover additional oil and gas that remains undiscovered in the basin.

  9. Origin of REE-rich ferrocarbonatites in southern Siberia (Russia): implications based on melt and fluid inclusions

    NASA Astrophysics Data System (ADS)

    Prokopyev, Ilya R.; Borisenko, Alexander S.; Borovikov, Andrey A.; Pavlova, Galina G.

    2016-12-01

    Fe-rich carbonatites with a mineral assemblage of ankerite-calcite or siderite are widespread in southern Siberia, Russia. The siderite carbonatites are associated with F-Ba-Sr-REE mineralization and have a 40Ar/39Ar age of 117.2 ± 1.3 Ma. Melt and fluid inclusions suggest that the carbonatites formed from volatile-rich alkali- and chloride-bearing carbonate melts. Ankerite-calcite carbonatites formed from carbonatite melt at a temperature of more than 790 °C. The ferrocarbonatites (the second phase of carbonatite intrusion) formed from a sulfate-carbonate-chloride fluid phase (brine-melt) at >650 °C and ≥360 MPa. The brine-melt fluid phase had high concentrations of Fe and LREEs. A subsequent hydrothermal overprint contributed to the formation of economically important barite-Sr-fluorite-REE mineralization in polymict siderite breccia.

  10. Assessment of Mesozoic-Kainozoic climate impact on oil-source rock potential (West Siberia)

    NASA Astrophysics Data System (ADS)

    Iskorkina, A. A.; Isaev, V. I.; Terre, D. A.

    2015-11-01

    Based on paleotemperature modeling, the evaluation of the effect of Neo-Pleistocene permafrost rock thickness on geothermal regime of the Bazhenov deposits has been performed. It has been stated that permafrost about 300 m in thickness must be considered for appropriate reconstruction of geothermal history of source rocks in the south-east areas of West Siberia. This condition is relevant to a consistent consideration of oil-generation phase history and can prevent underestimation (to 25%) of hydrocarbon-in-place resources.

  11. Models of hydrocarbon-bearing sequences of West Siberia

    SciTech Connect

    Mkrtohyan, O.M.; Gogonenkov, G.N.; Pavlov, N.E. )

    1991-03-01

    The West Siberian province located within a young plate (platform) is one of the largest in the world in size, reserves, number of unique fields, and hydrocarbon production. The southern, central, and western areas of the province are dominantly oil-bearing, the northern portion gas-bearing. All commercial reserves are within the Devonian-Cenomanian stratigraphic interval. Small accumulations in fractured-vuggy Devon-Carboniferous rocks are located in the zone of unconformity between this sequence and the Jurassic. The potential of the pre-plate middle Paleozoic, platform upper Paleozoic, and Triassic sequences recognized by seismic data in the northern, deepest, part of the plate is not known yet. Most hydrocarbon pools are located in the Jurassic-Cretaceous hydrocarbon-bearing sequences (HBS) within the plate cover. Structural-depositional oil accumulations with very changeable flow rates, a large stratigraphic-depositional accumulation in high permeability basal (quartz) reservoirs, and an oil-condensate and a multiple-pool structural gas field are discovered in the Middle Jurassic composed of potential continental coal-bearing and marine deposits. In most HBS, there is still a prospect of discovering new hydrocarbon pools including pools in more complex traps.

  12. Problems of phytostratigraphy and the correlation of the Lower Jurassic continental sediments in West Siberia and Kuznetsk and Kansk-Achinsk basins

    SciTech Connect

    Mogutcheva, N.K.

    2009-06-15

    Paleofloral and palynological records of Lower Jurassic sediments in West Siberia, Kuznetsk (Kuzbass), and Kansk-Achinsk basins and their correlation are discussed. In a number of recent papers dedicated to the Jurassic stratigraphy of Siberia this problem is ambiguously treated. The reference palynological scale has been developed for the Jurassic West Siberian sediments and an uninterrupted succession of floral assemblages associated with it and with regional stratigraphic units has been recognized. On this basis the scheme of the correlation between the Lower Jurassic sediments of the Kansk-Achinsk and Kuznetsk basins and West Siberia permitting a better age estimate of coal-bearing deposits, is proposed.

  13. Biogeochemistry of carbon and related major and trace elements in peat bog soils of the middle taiga of Western Siberia (Russia).

    NASA Astrophysics Data System (ADS)

    Stepanova, V. A.; Mironycheva-Tokareva, N. P.; Pokrovsky, O. S.

    2012-04-01

    Global climate changes impact the status of wetland ecosystems shifting the balances of the carbon, macro-, and microelements cycles. This study aims to establish the features of accumulation and distribution of major- and trace elements in the organic layer of peat bog soils, belonging to different ecosystems of the oligotrophic bog complex located in the middle taiga of Western Siberia (Khanty-Mansiysk region, Russia). Key areas which are selected for this study include the following bog conjugate elementary ecosystems: higher ryam, lower ryam, ridge-hollow complex, and oligotrophic poor fen as characterized previously [1]. We have sampled various peat types along the entire length of the soil column (every 10 cm down to 3 m). Peat samples were analyzed for a wide range of macro- and microelements using an ICP-MS technique following full acid digestion in a microwave oven. These measurements allowed quantitative estimates of major- and trace elements in the peat deposits within the whole bog complex and individual elementary landscapes. Based on the data obtained, the lateral and radial geochemical structures of the bog landscapes were determined and clarified for the first time for middle taiga of the West Siberian plain. The similar regime of mineral nutrition during the complete bog landscape formation was detected for the peat deposits based on the measurements of some major- and trace elements (Ca, Fe, Mg, etc.). The vertical distribution of some major and some trace elements along the profile of peat column is rather uniform with relatively strong increase in the bottom organic layers. This strongly suggests the similarity of the processes of element accumulation in the peat and relatively weak post depositional redistribution of elements within the peat soil profile. Overall, obtained corroborate the existing view on chemical composition of peats being determined by botanical peat's components (which forms this peat deposit), atmospheric precipitation

  14. Collection of radiocarbon dates on the mammoths ( Mammuthus primigenius) and other genera of Wrangel Island, northeast Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Vartanyan, Sergey L.; Arslanov, Khikmat A.; Karhu, Juha A.; Possnert, Göran; Sulerzhitsky, Leopold D.

    2008-07-01

    We present and discuss a full list of radiocarbon dates for woolly mammoth and other species of the Mammoth fauna available from Wrangel Island, northeast Siberia, Russia. Most of the radiocarbon dates are published here for the first time. Of the124 radiocarbon dates on mammoth bone, 106 fall between 3700 and 9000 yr ago. We believe these dates bracket the period of mammoth isolation on Wrangel Island and their ultimate extinction, which we attribute to natural causes. The absence of dates between 9-12 ka probably indicates a period when mammoths were absent from Wrangel Island. Long bone dimensions of Holocene mammoths from Wrangel Island indicate that these animals were comparable in size to those on the mainland; although they were not large animals, neither can they be classified as dwarfs. Occurrence of mammoth Holocene refugia on the mainland is suggested. Based on other species of the Mammoth fauna that have also been radiocarbon on Wrangel Island, including horse, bison, musk ox and woolly rhinoceros, it appears that the mammoth was the only species of that fauna that inhabited Wrangel Island in the mid-Holocene.

  15. First Asian record of Panthera (Leo) fossilis (Mammalia, Carnivora, Felidae) in the Early Pleistocene of Western Siberia, Russia.

    PubMed

    Sotnikova, Marina V; Foronova, Irina V

    2014-08-01

    A lion-like pantherine felid is described as Panthera (Leo) fossilis from the late Early Pleistocene sediments of the Kuznetsk Basin (Western Siberia, Russia). The find of P. fossilis first recorded in Asia considerably extends the current notion of the eastward expansion of the most ancient lions. The Siberian lion is geologically the oldest form and is dimensionally among the largest members of the group of fossil lions on the Eurasian continent. Although known by mandibular remains only, it is readily distinguished from Panthera (Leo) spelaea by a heavy built mandibular corpus with rectangular profile in the cheek teeth area, a deep, well-outlined and narrow anterior section of the masseteric fossa, and a large p4 supported by a big unreduced anterior root. The Siberian lion shares these features with the European Middle Pleistocene P. fossilis and the American Late Pleistocene P. (Leo) atrox, which suggests their close relationship. P. atrox originated from P. fossilis and was isolated in North America south of the Late Pleistocene ice sheets. This explains why the American lion has retained more primitive features than the coeval Eurasian cave lion P. (L.) spelaea.

  16. Physical and chemical stability of nanostructured lipid drug carriers (NLC) based on natural lipids from Baikal region (Siberia, Russia).

    PubMed

    Averina, E S; Müller, R H; Popov, D V; Radnaeva, L D

    2011-05-01

    At the turn of the millennium, a new generation of lipid nanoparticles for pharmacology was developed, nanostructured lipid carriers (NLC). The features of NLC structure which allow the inclusion of natural biologically active lipids in the NLC matrix open a wide prospect for the creation of high performance drug carriers. In this study NLC formulations were developed based on natural lipids from the Siberia region (Russia): fish oil from Lake Baikal fish; polyunsaturated fatty acid fractions and monounsaturated and saturated fatty acid fractions from fish oil and Siberian pine seed oil. Formulation parameters of NLC such as as type of surfactant and storage conditions were evaluated. The data obtained indicated high physical stability of NLC formulated on the basis of pure fish oil stabilized by Tween 80 and NLC formulated on the basis of free fatty acids stabilized by Poloxamer 188. The good chemical stability of the lipid matrix and the high concentrations of the biologically active polyunsaturated fatty acids in the NLC developed open wide prospects for their use in pharmaceutics and cosmetics.

  17. Benthic bioindicators from the lakes of Northern Yakutia (Siberia, Russia) in paleoclimatic research

    NASA Astrophysics Data System (ADS)

    Tumanov, O. N.; Nazarova, L. B.; Frolova, L. A.; Pestryakova, L. A.

    2012-04-01

    High latitude regions are particularly affected by global climate change. Aquatic ecosystems are known to respond quickly and sensitively to such changes (Carpenter et al., 1992; Findlay et al. 2001; Smol et al., 2005). This effect is especially dramatic in regions with continental climates such as Northern and Eastern Siberia. In 2008, Russian-German expedition investigated 33 lakes of Kolyma river basin, North-Eastern Yakutia. The region of investigation is located in the mouth of Kolyma river between approximately 68°2' and 69°4' N and between 159°8' and 161°9' E. It's a most north-eastern region of Yakutia, so it's suitable for paleolimnological investigations. The investigated lakes are situated along the 200 km transect crossing 3 vegetation zones: polygonal tundra, forest tundra and northern taiga. The main aims were establishing a calibration dataset for paleoenvironmental reconstructions by using aquatic organisms, investigation of limnological variables and the influence of the environmental conditions on distribution of aquatic organisms in Yakutian lakes. The modern benthic fauna of the lakes is represented by 89 taxa from 14 taxonomic groups. The most abundant group was Mollusca. The most taxonomically diverse group was Chironomidae. A unique for this region species were discovered, such as Cincinna kamchatica, Physa jarochnovitschae, Colymbetes dolabratus, Ilybius wasastjernae, Xestochironomus sp., Agrypnia sp. etc. Cluster analysis of taxonomical composition of the benthic fauna of these lakes showed high dependency to vegetation zones. The highest levels of hydrobiological indexes (Shannon, Evenness, species richness) were registered in forest tundra. CCA analysis showed that the most influential factors in species distribution were climate-dependant factors, such as mean Tair of July, pH and water depth. Data from taxonomical analysis of Chironomidae group were used for establishing a calibration dataset for paleoenvironmental reconstructions.

  18. Genetic characterization of an isolate of HIV type 1 AG recombinant form circulating in Siberia, Russia.

    PubMed

    Baryshev, P B; Bogachev, V V; Gashnikova, N M

    2012-12-01

    Before 2008, HIV-1 subtype A was the predominant genetic variant in the Novosibirsk oblast of Russia as well as in most parts of this country. However, a rapid spread of the recombinant HIV-1 02_AG form has been reported in Novosibirsk since 2009. We have analyzed the genome of the 10.RU.6637 isolate, a HIV-1 02_AG recombinant form, which represents a monophyletic cluster of the HIV-1 variants widespread in this region. Phylogenetic analysis has shown that the Siberian 10.RU.6637 isolate displays the highest sequence identity to the HIV-1 subtype AG forms circulating in Uzbekistan. However, recombination analysis of 10.RU.6637 has demonstrated that this isolate is a recombinant form between HIV-1 subtype A and CRF02_AG, differing in its genetic structure from both the CRF02_AG reference sequences and the Central Asian variants of HIV-1 02_AG.

  19. Content and distribution of trace metals in pristine permafrost environments of Northeastern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Antcibor, I.; Eschenbach, A.; Kutzbach, L.; Bolshiyanov, D.; Pfeiffer, E.-M.

    2012-04-01

    Arctic regions are one of the most sensitive areas with respect to climatic changes and human impacts. Research is required to discover how the function of permafrost soils as a buffering system for metal pollutants could change in response to the predicted changes. The goal of this work is to determine the background levels of trace metals in the pristine arctic ecosystems of the Lena River Delta in Northeastern Siberia and to evaluate the possible effect of human impacts on this arctic region. The Lena River Delta represents areas with different dominating geomorphologic processes that can generally be divided between accumulation and erosion sites. Frequent changes of the river water level create different periods of sedimentation and result in the formation of stratified soils and sediment layers which are dominated either by mineral substrates with allochthonous organic matter or pure autochthonous peat. The deposited sediments that have formed the delta islands are mostly composed of sand fractions; therefore the buffering effects of clay materials can be neglected. Samoylov Island is representative of the south-central and eastern modern delta surfaces of the Lena River Delta and is selected as a pilot study site. We determined total element contents of Fe, Mn, Zn, Cd, Ni, Cu, As, Pb, Co and Hg in soil horizons from different polygonal elevated rims, polygonal depressed centers and the middle floodplain. High gravimetric concentrations (related to dry mass of soil material) of Mn and Fe are found within all soil profiles and vary from 0.14 to 1.39 g kg-1 and from 10.7 to 41.2 g kg-1, respectively. While the trace element concentrations do not exceed typical crustal abundances, the maximum values of most of the metals are observed within the soil profile situated at the middle floodplain. This finding suggests that apart from the parent material the second potential source of trace metals is due to allochthonous substance input during annual flooding of the

  20. Phytoplankton community structure in the Lena Delta (Siberia, Russia) in relation to hydrography

    NASA Astrophysics Data System (ADS)

    Kraberg, A. C.; Druzhkova, E.; Heim, B.; Loeder, M. J. G.; Wiltshire, K. H.

    2013-02-01

    The Lena Delta in Northern Siberia is one of the largest river deltas in the world. During peak discharge, after the ice melt in spring, it delivers between 60-8000 m3s-1 of water and sediment into the Arctic Ocean. The Lena Delta and the Laptev Sea coast also constitute a~continuous permafrost region. Ongoing climate change, which is particularly pronounced in the Arctic, is leading to increased rates of permafrost thaw. This is likely to profoundly change the discharge rates of the Lena River and the chemistry of the river waters which are discharged into the coastal Laptev Sea, e.g. by increasing concentrations of inorganic nutrients, DOC and importantly methane. These physical and chemical changes will also affect the composition of and interactions between phytoplankton and zooplankton communities, forming the basis of the food web. However, before potential consequences of climate change for coastal arctic plankton communities can be judged, the inherent status of the diversity and linked foodweb interactions within the delta need to be established. As part of the AWI Lena Delta Programme in 2010 the phyto- and microzooplankton community in three river channels as well as four coastal transects were investigated to capture the typical river phytoplankton communities and the transitional zone of brackish/marine conditions. Most CTD profiles from 23 coastal stations showed very strong stratification. The only exception to this was a small a shallow and mixed area running from the outflow of Bykovskaya channel in a northerly direction parallel to the shore (transect 3). Of the five stations in this area three had a salinity of close to zero. Two further stations had salinities of around 2 and 5 throughout the water column. In the remaining transects on the other hand salinities varied between 5-30 with depth. Phytoplankton counts from the outflow from the Lena were dominated by diatoms (Aulacoseira species) cyanobacteria (Aphanizomenon, Pseudanabaena) and

  1. Investigations of adaptation mechanisms of different halophytes types in different soil salinity conditions (Southern Central Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Slyusar, Natalia; Pechurkin, Nickolay

    High salt concentration in the soil is one of the limiting factors affecting plant growth and development. However, there are plants that are physiologically adapted to high salts concen-trations -halophytes. Studies of halophytes reveals mechanisms of adaptation to this factor. Investigations were conducted in the steppe zone of Southern Central Siberia (Russia, Khaka-sia), nearest coastal zone of the Lake Kurinka. The work was carried on route and stationary methods. As a results was conducted about 100 geobotanical descriptions, was defined species composition, covering, vertical and horizontal structure of plant communities, the productivity of above ground dry phytomass. As a result of field work was identified various types of plant communities, that are located on soils with a salinity degree are 0,2 -7,16 g / l. Type of saline -sulfate-sodium. Suaeda plant communities was located in the meadow-saline soil (soil salinity degree 5 -7 g / l). The dominant is euhalophyte Suaeda linifolia Pall. and subdominant is glycohalophyte Puccinellia tenuissima. A plant community has two layers. Total covering is 50 -55During the study period (2004 -2009), the change was observed in the soil salinity degree in the range of 2.27 -7.16 g / l. The plan community productivity varied from 99 to 201 g/m2 by years of research. Also was noted that the salt amount in the plants biomass varies depending on the type of halophyte. In the cells of euhalophyte Suaeda linifolia the salt amount was 10-35The investigation noted that relations between the main photosynthetic pigments (chlorophylls and carotenoids) have changes depending on the type of halophyte. Thus, in typical glycohalophyte Puccinellia tenuissima, Elytrigia repens and Phragmites australis chlorophyll content remained relatively high during the summer period and were 0,74, 0,61 and 0,53

  2. Investigating the Human Dimension of Unprecedented Global Climate Change in northeastern Siberia, Russia: Understandings, Perceptions and Responses

    NASA Astrophysics Data System (ADS)

    Crate, S.

    2009-12-01

    An urgent challenge of the 21st century is to investigate understandings, perceptions and responses of populations confronting the local effects of global climate change. This paper describes the most recent results of one such project working with rural native Viliui Sakha communities, Turkic-speaking horse & cattle breeders in northeastern Siberia, Russia. The research questions are: 1) What local effects of global climate change are Viliui Sakha communities observing, how are Viliui Sakha perceiving these changes and how are the changes affecting both their subsistence survival and their cultural orientations? 2) What local knowledge exists about past climate perturbations and how does that knowledge influence contemporary adaptation to global climate change? 3) How can anecdotal (local) knowledge and regional scientific knowledge about the local effects of global climate change be integrated to enhance both local adaptive responses and policy efforts? The four-village, three-year study is a collaborative effort involving the active participation of the targeted communities, field assistants, native specialists, an in-country research team and an international collaborator. The project is founded on the PI’s 20 years of ongoing research and work with rural Viliui Sakha communities and on her fluency in both the Sakha and Russian languages. A central focus of this project is the integration of local and scientific knowledges. We are documenting local knowledge on the community, elder and archival levels. We are collaborating with scientists in Yakutsk for regional scientific data. Our project team has just returned from the second summer of field work and this presentation will cover the project results to date. Hayfields are inundated with water.

  3. Changes in CO_{2} trends observed in the lower troposphere over West Siberia

    NASA Astrophysics Data System (ADS)

    Belan, Boris D.; Machida, Toshinobu; Sasakawa, Motoki; Maksyutov, Shamil; Davydov, Denis; Fofonov, Alexandr; Arshinov, Mikhail

    2016-04-01

    Long-term airborne observations of greenhouse gases carried out in the troposphere over south-western area of West Siberia since 1997 allowed some specific features in CO2 trends to be revealed at different heights. At an altitude of 7 km above ground level (AGL), the average annual rate of CO2 increase was 1.72 ppm yr-1. The main distinctive features in the tendencies of CO2 mixing ratio have been found in the lower troposphere. Thus, for the period from 1997 to 2004, July concentrations of CO2 at an altitude of 500 m AGL increased slightly with a rate of 0.17 ppm yr-1, while since 2005 they began to rise dramatically with a rate of 3.64 ppm yr-1. Analysis of the possible causes of such long-term behavior showed that it was resulted from neither reduction of forest area, nor wildfires, nor forest diseases. Also it is impossible to state that reducing CO2 sink has been caused by the impact of climate changes on ecosystems. Possibly, anthropogenic CO2 accumulation resulted in that Siberian forests cannot assimilate such additional amount of carbon dioxide. A decrease in the sink for atmospheric CO2 is also observed in the Amazon (Brienen et al. 2015). Brienen et al. (2015) assume that it may be caused by a sustained long-term increase in tree mortality. There is also a supposition that it can be a result of a vegetation replacement by other types of plants or young trees, which absorb less amount of CO2 (Kunstler et al., 2015; Crowther T. W., 2015). However, it seems highly unlikely to test these hyposeses in the near future due to a huge area of West Siberia, most regions of which are difficult to access. This work was funded by the Global Environment Research Account for National Institutes of the Ministry of the Environment (Japan) and Russian Foundation for Basic Research (grant No. 14-05-00590). Brienen R.J.W. et al. 2015. Long-term decline of the Amazon carbon sink. Nature. 519 (7543), 344-348. Kunstler G. et al. 2015. Plant functional traits have globally

  4. Observations of wetland methane fluxes in West Siberia with automated chamber system

    NASA Astrophysics Data System (ADS)

    Maksyutov, Shamil; Krasnov, Oleg; Shelevoi, Valentin; Nadeev, Alexander; Glagolev, Mikhail

    2013-04-01

    An automatic sampling and analysis system for measuring methane and CO2 fluxes from soil was developed and applied to the flux measurements at boreal wetland near Plotnikovo, Tomsk region in the southern part of West Siberia in 2012. Measurements were performed on mesotrophic open bog at the bog periphery. Solar powered automated system is used to open and close six static chambers equipped with air actuators. Analysis system uses semiconductor sensor for methane and NDIR for carbon dioxide. Air and soil temperatures, as well as groundwater table are recorded. Seasonal variations of the emissions summarized as weekly mean fluxes correlate well with soil temperature. Season-high fluxes vary from 3.9 to 22 mgCH4/m2/h between chambers. The vegetation map created from high resolution aerial photos and ground survey data was used for analysis of the spatial flux distribution. The methane and CO2 fluxes appear clearly related to the vegetation and soil conditions. Higher emission rates are observed over waterlogged surfaces with presence of sedge and cotton-grass while lowest emission rates correspond to dry hummocks.

  5. Spatial heterogeneity of greening and browning between and within bioclimatic zones in northern West Siberia

    NASA Astrophysics Data System (ADS)

    Miles, Victoria V.; Esau, Igor

    2016-11-01

    Studies of the normalized difference vegetation index (NDVI) have found broad changes in vegetation productivity in high northern latitudes in the past decades, including increases in NDVI (‘greening’) in tundra regions and decreases (‘browning’) in forest regions. The causes of these changes are not well understood but have been attributed to a variety of factors. We use Moderate Resolution Imaging Spectrometer (MODIS) satellite data for 2000-2014 and focus on northern West Siberia—a hot spot of extensive landcover change due to rapid resource development, geomorphic change, climate change and reindeer grazing. The region is relatively little-studied in terms of vegetation productivity patterns and trends. This study examines changes between and within bioclimatic sub-zones and reveals differences between forest and treeless areas and differences in productivity even down to the tree species level. Our results show that only 18% of the total northern West Siberia area had statistically significant changes in productivity, with 8.4% increasing (greening) and 9.6% decreasing (browning). We find spatial heterogeneity in the trends, and contrasting trends both between and within bioclimatic zones. A key finding is the identification of contrasting trends for different species within the same bioclimatic zone. Browning is most prominent in areas of denser tree coverage, and particularly in evergreen coniferous forest with dark (Picea abie, Picea obovata) or light (Pinus sylvestris) evergreen and evergreen-majority mixed forests. In contrast, low density deciduous needle-leaf forest dominated by larch (Larix sibirica), shows a significant increase in productivity, even while neighboring different species show productivity decrease. These results underscore the complexity of the patterns of variability and trends in vegetation productivity, and suggest the need for spatially and thematically detailed studies to better understand the response of different

  6. Petroleum geology and resources of the Baykit High province, East Siberia, Russia

    USGS Publications Warehouse

    Ulmishek, Gregory F.

    2001-01-01

    The Baykit High province consists of two principal structural units?the Baykit regional high in the west, which occupies most of the province, and the Katanga structural saddle in the east. The province is on the western margin of the Siberian craton east of theYenisey Ridge foldbelt. The province is an exploration frontier and only a few prospects have been drilled. The oldest sedimentary rocks of the province, Riphean carbonate and clastic strata of Late Proterozoic age (1,650?650 million years old) that were deposited on the passive margin, cover the Archean?Lower Proterozoic basement. Basal Vendian (uppermost Proterozoic, 650?570 million years old) clastic rocks unconformably overlie various units of the Riphean and locally lie directly on the basement. Younger Vendian and lowermost Cambrian rocks are primarily dolomites. The Vendian/Cambrian boundary is con-formable, and its exact stratigraphic position has not been identified with certainty. The Lower Cambrian section is thick, and it consists of alternating beds of dolomite and evaporites (mostly salt). Middle and Upper Cambrian strata are composed of shale and dolomite. Ordovician-Silurian and upper Paleozoic rocks are thin, and they are present only in the northern areas of the province. Structural pattern of Riphean rocks differs substantially from that of Vendian-Cambrian rocks. A single total petroleum system (TPS) was identified in the Baykit High province. Discovered oil of the system is chiefly concentrated in Riphean carbonate reservoirs of the Yurubchen-Tokhom zone that is currently being explored and that has the Abstract 1 potential to become a giant field (or group of fields). The TPS also contains about 5 trillion cubic feet of discovered recover-able gas in clastic reservoir rocks at the base of the Vendian section. Petroleum source rocks are absent in the stratigraphic succession over most of the TPS area. Riphean organic-rich shales and carbonates that crop out in the Yenisey Ridge foldbelt

  7. Chineysky Layered Intrusion with unique V and PGE-Cu ores (Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Gongalskiy, Bronislav; Krivolutskaya, Nadezda

    2010-05-01

    system in Late Proterozoic. There are two types of commercial mineralization in the Chiney massif: Fe-Ti-V and Cu with precious metals. Nowadays the Chiney massif comprises the largest V recourses in Russia. The iron ores are concentrated in the central part of the intrusion and are represented by two varieties: disseminated and massive (the early-magmatic type); veins and irregular bodies (the late-magmatic type). Sulfide minerals occur as accessory disseminations in all rocks of the massif, but their higher concentrations are distributed locally. The copper commercial mineralization is confined to the contact zone of gabbroids with the host rocks, so endo-and exocontact ores are determined. The disseminated mineralization predominates sharply. Vein bodies are distributed in the limited region and localized at a small distance from the bottom of the intrusion. The main ore mineral is chalcopyrite, that is very unusual for Cu-Ni deposits (Cu/Ni=10-100, Pd/Pt=3 in ores). The major minerals are pyrrhotite and pentlandite. Many rare minerals of noble metals (Ag, Au, PGE) were found too. In general, the minerals consist of compounds of Pd with Bi, Te, Sb, Sn, As, and Ni; compounds of Pt with As, S, and Fe; a compound of Rh with As-S, as well hessite (Ag2Te) and Au-Ag-(Hg) alloys. It was found froodite; sobolevskite; kotulskite; sudburyite; stibiopalladinite; mertieite II; isomertieite; paolovite; michenerite; arsenopalladinite; merenskiite; majakite et ctr. References 1. Gongalskiy B.I., N.A. Krivolutskaya, A.A. Ariskin, G.S. Nikolaev.// Geochemistry International. 2008. Vol. 46. No. 7. P. 637-665. 2. Gongalskiy B. I., Yu. G. Safonov, N. A. Krivolutskaya, V. Yu. Prokof'ev, and A. A. Yushin. A // Doklady Earth Sciences. 2007.Vol. 415, No. 5. P. 671-674.

  8. Interaction of rock, water, and plants in central Siberia (Russia) dominated by continuous permafrost: biotic versus abiotic fluxes

    NASA Astrophysics Data System (ADS)

    Viers, J.; Pokrovsky, O. S.; Prokushkin, A. S.; Beaulieu, E.; Dupre, B.

    2009-12-01

    Boreal forests mainly located between the latitudes 46°N and 66°N play a key role in regulating global carbon cycle and climate of the Earth. These forests store about 42 gigatons of carbon (Gt C) of above ground biomass and 200 Gt C of soil organic matter that represents about 8 and 13% of the global amounts (Jarvis et al., 2001 and references therein). The last technical paper on climate change and water of the IPCC reports abnormal thawing of permafrost, increase of the active period, increase of river runoff and changes in the distribution of plants and their productivity for artic and sub-arctic regions (www.ipcc.ch and references therein). Within the context of global warming, forested permafrost regions appear to be very sensitive and are likely to be deeply modified in a near future. In return, these modifications affecting the functioning of these ecosystems will influence the whole Earth system. Among forested boreal regions, Central Siberia (Russia), that spreads over more than 4,000,000 km2, is very interesting due to the presence of permafrost within the specific geological substratum. Indeed, this area offers large basaltic surface and chemical weathering of basaltic rocks is considered to be the main process removing carbon dioxide from the atmosphere over geological time scale (Dessert et al., 2003). The sampling site is located in the drainage basin of the Nizhniya Tungunska River (eastern tributary of the Yenissey River) on the basaltic plateau of Putorana. Climate is cold with a mean annual air temperature of -9.5°C and annual precipitation of 350mm. 60% of rain is falling during the active period when the surface soil temperature is above zero degrees (end of May to September). At local scale, there are north-facing and south-facing slopes that receive equivalent precipitation but exhibit totally different heat input and consequently above-ground biomass and active layer thickness. Larches and mosses account for more than 85% of the above

  9. Trace element speciation and origin of colloids in surface waters of subarctic zone (NW of Russia and Central Siberia)

    NASA Astrophysics Data System (ADS)

    Pokrovsky, O. S.; Viers, J.; Prokushkin, A. S.; Vasukova, E. V.; Shirokova, L. S.; Dupre, B.

    2008-12-01

    Geochemistry of trace elements (TE) in boreal regions attracts large attention of researchers in view of on- going environmental changes that can affect both the fluxes of these elements to the ocean, their speciation and thus their bioavailability. Most of trace elements in waters of boreal zone are transported via organic and organo-mineral colloids. In order to better understand the processes of colloids formation in surface waters draining watersheds of various lithology and permafrost abundance, comparative study of TE speciation in various geographic zones is necessary. In this work we attempted to generalize the typical features of trace element speciation in boreal arctic and subarctic zones assessed via in-situ dialysis and ultrafiltration. Surface waters of three circumpolar regions in Arkhangelsk region, NW Russia and Central Siberia were studied using unique and rigorous procedure via combination of in-situ dialysis and ultrafiltration (1 kDa, 3.5 kDa, 10 kDa, 100 kDa, 0.22 µm, 0.45 µm, 1 μm, 5 µm). In both filtrates and dialysates, all major and trace elements and dissolved organic carbon were analyzed. In all studied regions, three typical features of colloid speciation have been revealed: i) high proportion of large-size colloids (10 kDa - 0.22 μm and 0.22 μm - 5 µm), mostly composed of Fe oxy(hydr)oxides stabilized by organic matter; ii) presence of organic-rich, small size colloids and conventionally "dissolved" substances (< 1 kDa and 1 - 10 kDa), presumably, fulvic acids, and iii) strong association of all trivalent and tetravalent elements with large-size mineral colloids. Results of the present work allow distinguishing between two possible pathways of colloids formation: 1) Groundwater-borne Fe(II) oxidation and TE coprecipitation in the presence of organic matter originated from plant litter and peat layers of surface horizons at the surface redox front between anoxic groundwaters and surficial OM-rich waters of the riparian zone, and

  10. Global Lessons from Siberia.

    ERIC Educational Resources Information Center

    Tucker, Jan L.

    1993-01-01

    Describes a visit by two U.S. social studies educators to schools in Krasnoyarsk, a city in Siberia, Russia. Discusses economic and social changes brought about by the end of the Cold War. Recommends more international and global education for both Russia and the United States. (CFR)

  11. Food and water security issues in Russia III: food- and waterborne diseases in the Russian Arctic, Siberia and the Far East, 2000–2011

    PubMed Central

    Dudarev, Alexey A.; Dorofeyev, Vitaliy M.; Dushkina, Eugenia V.; Alloyarov, Pavel R.; Chupakhin, Valery S.; Sladkova, Yuliya N.; Kolesnikova, Tatjana A.; Fridman, Kirill B.; Nilsson, Lena Maria; Evengard, Birgitta

    2013-01-01

    Background The food- and waterborne disease situation in Russia requires special attention. Poor quality of centralized water supplies and sewage systems, biological and chemical contamination of drinking water, as well as contamination of food products, promote widespread infectious diseases, significantly exceeding nationwide rates in the population living in the two-thirds of Russian northern territories. Objectives The general aim was to assess the levels of food- and waterborne diseases in selected regions of Russian Arctic, Siberia and the Far East (for the period 2000–2011), and to compare disease levels among regions and with national levels in Russia. Study design and methods This study is the first comparative assessment of the morbidity in these fields of the population of 18 selected regions of Russian Arctic, Siberia and the Far East, using official statistical sources. The incidences of infectious and parasitic food- and waterborne diseases among the general population (including indigenous peoples) have been analyzed in selected regions (per 100,000 of population, averaged for 2000–2011). Results Among compulsory registered infectious and parasitic diseases, there were high rates and widespread incidences in selected regions of shigellosis, yersiniosis, hepatitis A, tularaemia, giardiasis, enterobiasis, ascariasis, diphyllobothriasis, opistorchiasis, echinococcosis and trichinellosis. Conclusion Incidences of infectious and parasitic food- and waterborne diseases in the general population of selected regions of the Russian Arctic, Siberia and the Far East (2000–2011) are alarmingly high. Parallel solutions must be on the agenda, including improvement of sanitary conditions of cities and settlements in the regions, modernization of the water supply and of the sewage system. Provision and monitoring of the quality of the drinking water, a reform of the general healthcare system and the epidemiological surveillance (including gender

  12. Trends in normalized difference vegetation index (NDVI) associated with urban development in northern West Siberia

    NASA Astrophysics Data System (ADS)

    Esau, Igor; Miles, Victoria V.; Davy, Richard; Miles, Martin W.; Kurchatova, Anna

    2016-08-01

    Exploration and exploitation of oil and gas reserves of northern West Siberia has promoted rapid industrialization and urban development in the region. This development leaves significant footprints on the sensitive northern environment, which is already stressed by the global warming. This study reports the region-wide changes in the vegetation cover as well as the corresponding changes in and around 28 selected urbanized areas. The study utilizes the normalized difference vegetation index (NDVI) from high-resolution (250 m) MODIS data acquired for summer months (June through August) over 15 years (2000-2014). The results reveal the increase of NDVI (or "greening") over the northern (tundra and tundra-forest) part of the region. Simultaneously, the southern, forested part shows the widespread decrease of NDVI (or "browning"). These region-wide patterns are, however, highly fragmented. The statistically significant NDVI trends occupy only a small fraction of the region. Urbanization destroys the vegetation cover within the developed areas and at about 5-10 km distance around them. The studied urbanized areas have the NDVI values by 15 to 45 % lower than the corresponding areas at 20-40 km distance. The largest NDVI reduction is typical for the newly developed areas, whereas the older areas show recovery of the vegetation cover. The study reveals a robust indication of the accelerated greening near the older urban areas. Many Siberian cities become greener even against the wider browning trends at their background. Literature discussion suggests that the observed urban greening could be associated not only with special tending of the within-city green areas but also with the urban heat islands and succession of more productive shrub and tree species growing on warmer sandy soils.

  13. Deciduous shrub growth and the greening of the Arctic in West Siberia

    NASA Astrophysics Data System (ADS)

    Forbes, B. C.; Macias Fauria, M.; Zetterberg, P.; Kumpula, T.

    2010-12-01

    Salix lanata and Alnus fruticosa are common and widespread shrub species in the low arctic tundra zone of West Siberia. They often occur in similar local habitats with the live portions of genets up to 100 years old. We have recently established that growth rings of S. lanata provide an excellent proxy for summer temperature. In that study our data were derived from shrubs growing on organic soils near the arctic coast of the Nenets Autonomous Okrug (NAO), west of the Ural Mountains. East of the Urals, in the Yamal-Nenets Autonomous Okrug (YNAO), climate is more continental and sandy soils provide a relatively nutrient-poor substrate for plant growth. By sampling two different species side by side on the Yamal Peninsula, we shed light on the relationship between deciduous shrubs and growing season temperatures in the last half century or so, a period of pronounced regional warming. We discern differences in the climate signal within a single species (S. lanata) as well as between it and a neighboring species with a strongly overlapping ecological amplitude (A. fruticosa). July is the main month for temperature correlation in Alnus, whereas Salix responds to June-July-August temperatures in both regions. The high correlations of shrub growth with summer temperature (r > 0.7 over the period 1956-2004) strongly suggest a link between increased shrub growth and recent decadal warming in both regions (~2°C). Both species showed significant correlation with the regional Normalized Difference Vegetation Index (NDVI), although it was somewhat lower in YNAO compared to NAO, probably due to the relative land cover (10% vs. 20%, respectively) of erect shrubs in both areas, which affects their overall contribution to the NDVI. In both regions Salix lanata biomass peaks in the second half of July. Hand-held leaf area index data from Yamal indicate a significant difference between loamy/clayey and sandy sites. We hypothesized that this same variation would be evident at the

  14. Isolation of two strains of West Nile virus during an outbreak in southern Russia, 1999.

    PubMed Central

    Lvov, D. K.; Butenko, A. M.; Gromashevsky, V. L.; Larichev, V. P.; Gaidamovich, S. Y.; Vyshemirsky, O. I.; Zhukov, A. N.; Lazorenko, V. V.; Salko, V. N.; Kovtunov, A. I.; Galimzyanov, K. M.; Platonov, A. E.; Morozova, T. N.; Khutoretskaya, N. V.; Shishkina, E. O.; Skvortsova, T. M.

    2000-01-01

    From July to September 1999, a widespread outbreak of meningoencephalitis associated with West Nile virus (Flavivirus, Flaviviridae) occurred in southern Russia, with hundreds of cases and dozens of deaths. Two strains of West Nile virus isolated from patient serum and brain-tissue samples reacted in hemagglutination-inhibition and neutralization tests with patients' convalescent-phase sera and immune ascites fluid from other strains of West Nile virus. PMID:10905970

  15. Soil microbiological composition and its evolution along with forest succession in West Siberia

    NASA Astrophysics Data System (ADS)

    Naplekova, Nadezhda N.; Malakhova, Nataliya A.; Maksyutov, Shamil

    2015-04-01

    Natural forest succession process in West Siberia is mostly initiated by fire disturbance and involves changing tree species composition from pioneer species to late succession trees. Along with forest aging, litter and forest biomass accumulate. Changes of the soil nitrogen cycle between succession stages, important for plant functioning, have been reported in a number of studies. To help understanding the mechanism of the changes in the soil nitrogen cycle we analyzed soil microbiological composition for soil profiles (0-160 cm) taken at sites corresponding to three forest succession stages: (1) young pine, age 18-20 years, (2) mid age, dark coniferous, age 50-70 years, (3) mature, fir-spruce, age 170-180 years. Soil samples were taken from each soil horizon and analyzed in the laboratory for quantity and species composition of algae and other microorganisms. Algae community at all stages of succession is dominated by species typical for forest (pp. Chlorhormidium, Chlamydomonas, Chloroccocum, Pleurochloris, Stichococcus). Algae species composition is summarized by formulas: young forest C14X10Ch9H2P4Cf1B2amph4, mid age X16C15Ch10H4P4Cf1B2amph4, mature X24C22Ch17H10P2amph5Cf1, with designations C -- Cyanophyta, X -- Xantophyta, Ch -- Chlorophyta, B -- Bacillariophyta. Diversity is highest in upper two horizons and declines with depth. Microorganism composition on upper 20 cm was analyzed in three types of forests separately for consumers of protein (ammonifiers) and mineral nitrogen, fungi, azotobacter, Clostridium pasteurianum, oligonitrophylic (eg diazotrophs), nitrifiers and denitrifiers. Nitrogen biologic fixation in the mature forest soils is done mostly by oligonitrophyls and microorganisms of the genus Clostridium as well as сyanobacteria of sp. Nostoc, but the production rate appears low. Concentrations (count in gram soil) of nitrogen consumers (eg ammonifiers), oligonitrophyls, Clostridium and denitrifiers increase several fold from young forest to mid

  16. Fracture system influence on the reservoirs rock formation of Ordovician-Devonian carbonates in West Siberia tectonic depression

    NASA Astrophysics Data System (ADS)

    Koveshnikov, A. E.; Nesterova, A. C.; Dolgaya, T. F.

    2016-09-01

    During the Paleozoic period from the beginning of the Cambrian to the end of the Carboniferous in the boundaries of the West Siberia tectonic depression there occurred the sea, where the carbonate platforms were formed by the limestones accumulation. All the area at the end of the Carboniferous period was turned to land. Resulting from Gertsynskaya folding in the times of Permian - Triassic the formed deposits were folded and denudated to a considerable extent. Besides, the reservoir rocks of the crust of weathering including redeposited one, were formed as a result of hypergenesis, during the continental stand of the area in the near-surface zone. A new geological prospecting unit has been suggested which underlies these crusts of weathering and formed during fracture tectonic processes with hydrothermal-metasomatic limestones reworking and the processes of hydrothermal leaching and dolomitization. So, in the carbonate platforms the system of fissure zones related to tectonic disturbance was formed. This has a dendrite profile where the series of tangential, more thinned fractures deviate from the stem and finish in pores and caverns. The carbonate platforms formation in the West Siberia tectonic depression has been analyzed, their dynamics and gradual increasing from the minimal in Ordovician and Silurian to maximal at the end of the Late Devonian has been shown.

  17. Soviet Development Policy in Siberia.

    ERIC Educational Resources Information Center

    Shabad, Theodore

    1978-01-01

    Examines how Soviet economic planners and policymakers cope with the geographic dichotomy of a concentration of population and economic activity in European Russia and the concentration of natural resources in sparsely populated Siberia. (Author/DB)

  18. First record of Mylagaulid rodents (Rodentia, Mammalia) from the Miocene of Eastern Siberia (Olkhon Island, Baikal Lake, Irkutsk Region, Russia).

    PubMed

    Tesakov, A S; Lopatin, A V

    2015-01-01

    A new genus and species of rodent, Lamugaulus olkhonensis, belonging to the subfamily Promylagaulinae of the family Mylagaulidae, is described on the basis of isolated teeth from the Khalagay Formation of the Lower Miocene Tagay locality (Olkhon island, Lake Baikal, Irkutsk Region). This is the first record of mylagaulids in Eastern Siberia, significantly expanding the data on the distribution of this mainly North American group of rodents in Asia and showing its presence outside the Central Asian arid zone.

  19. Technogenic Fallout of Uranium and Thorium in the Vicinity of Novosibirsk (Russia, West Siberia)

    NASA Astrophysics Data System (ADS)

    Artamonova, Svetlana Yu.

    Evaluation of the contribution of definite pollution sources among many others is rather complicated scientific challenge, but its solution may become decisive for the realization of measures aimed at ecological remediation of the territories. Element composition of aerosol particles accumulated during winter in the snow cover of Novosibirsk was determined by means of X-ray fluorescence measurements with synchrotron radiation at the "Siberian Synchrotron and Terahertz Radiation Center" based on VEPP-3 of the Budker Institute of Nuclear Physics SB RAS. Means of ICP-MS and scanning electron microscopy were used additionally. These studies allowed revealing the contribution of separate industrial enterprises into the general technogenic pollution of the megapolis with uranium and thorium.

  20. Gas-emission crater in Central Yamal, West Siberia, Russia, a new permafrost feature

    NASA Astrophysics Data System (ADS)

    Leibman, Marina; Kizyakov, Alexandr; Khomutov, Artem; Dvornikov, Yury; Streletskaya, Irina; Gubarkov, Anatoly

    2016-04-01

    The Yamal crater is a hole funnel-shaped on top and cylinder-shaped down to the bottom, surrounded by a parapet. Field study of the crater included size measurements, photo- video-documentation of the feature and the surrounding environment, and geochemical sampling. The upper part of the geological section within the crater consisted of stratified icy sediments, underlain by almost pure stratified ice of nearly vertical orientation of the layers. The volume of discharged material (volume of the void of the crater) was 6 times larger than the volume of material in the parapet. The difference was due to a significant amount of ice exposed in the walls of the crater, emitted to the surface and melted there. Remote sensing data was processes and validated by field observations to reveal the date of crater formation, previous state of the surface, evolution of the crater and environmental conditions of the surrounding area. Crater formed between 9 October and 1 November 2013. The initial size derived from Digital Elevation Model (DEM) had diameter of the vegetated rim 25-29 m. It turned through a sharp bend into a cylinder with close to vertical sides and diameter 15-16 m. Depth of the hole was impossible to estimate from DEM because of no light reaching walls in the narrow hole. By the time of initial observation in July 2014, water was found at the depth exceeding 50 m below the rim. In November 2014 this depth was 26 m. By September 2015 almost all the crater was flooded, with water surface about 5 m below the rim. The plan dimensions of the crater increased dramatically from initial 25-29 to 47-54 m in 2015. Thus, it took two warm seasons to almost entirely fill in the crater. We suppose that during the next 1-2 years parapet will be entirely destroyed, and as a result the crater will look like an ordinary tundra lake. Excluding impossible and improbable versions of the crater's development, the authors conclude that the origin of this crater can be attributed to the air temperature warming trend along with the extreme of 2012. The increased ground temperature and amount of unfrozen water in the permafrost, expanding of cryopegs, formation of a pingo-like mound and its outburst due to high pressure produced by gas hydrate decomposition within permafrost are the main controls. Similar temperature anomalies may increase in number in the future decades, presenting risks for human activities in the region. This conclusion is supported by recent studies of gas-hydrate behavior in the upper permafrost as well as by subsea processes in gas-bearing provinces where analogue mechanism is known to produce pockmarks - subsea depressions. As the crater is surrounded by the parapet, thus is resulting from expulsion of ice and rocks from beneath to the surface and should not be treated as a "sinkhole", "thermokarst" or "collapse".

  1. Neogene amphibians and reptiles (Caudata, Anura, Gekkota, Lacertilia, and Testudines) from the south of Western Siberia, Russia, and Northeastern Kazakhstan

    PubMed Central

    Zazhigin, Vladimir S.

    2017-01-01

    Background The present-day amphibian and reptile fauna of Western Siberia are the least diverse of the Palaearctic Realm, as a consequence of the unfavourable climatic conditions that predominate in this region. The origin and emergence of these herpetofaunal groups are poorly understood. Aside from the better-explored European Neogene localities yielding amphibian and reptile fossil remains, the Neogene herpetofauna of Western Asia is understudied. The few available data need critical reviews and new interpretations, taking into account the more recent records of the European herpetofauna. The comparison of this previous data with that of European fossil records would provide data on palaeobiogeographic affiliations of the region as well as on the origin and emergence of the present-day fauna of Western Siberia. An overview of the earliest occurrences of certain amphibian lineages is still needed. In addition, studies that address such knowledge gaps can be useful for molecular biologists in their calibration of molecular clocks. Methods and Results In this study, we considered critically reviewed available data from amphibian and reptile fauna from over 40 Western Siberian, Russian and Northeastern Kazakhstan localities, ranging from the Middle Miocene to Early Pleistocene. Herein, we provided new interpretations that arose from our assessment of the previously published and new data. More than 50 amphibians and reptile taxa were identified belonging to families Hynobiidae, Cryptobranchidae, Salamandridae, Palaeobatrachidae, Bombinatoridae, Pelobatidae, Hylidae, Bufonidae, Ranidae, Gekkonidae, Lacertidae, and Emydidae. Palaeobiogeographic analyses were performed for these groups and palaeoprecipitation values were estimated for 12 localities, using the bioclimatic analysis of herpetofaunal assemblages. Conclusion The Neogene assemblage of Western Siberia was found to be dominated by groups of European affinities, such as Palaeobatrachidae, Bombina, Hyla, Bufo

  2. Food and water security issues in Russia II: Water security in general population of Russian Arctic, Siberia and Far East, 2000–2011

    PubMed Central

    Dudarev, Alexey A.; Dushkina, Eugenia V.; Sladkova, Yuliya N.; Alloyarov, Pavel R.; Chupakhin, Valery S.; Dorofeyev, Vitaliy M.; Kolesnikova, Tatjana A.; Fridman, Kirill B.; Evengard, Birgitta; Nilsson, Lena M.

    2013-01-01

    Background Poor state of water supply systems, shortage of water purification facilities and disinfection systems, low quality of drinking water generally in Russia and particularly in the regions of the Russian Arctic, Siberia and Far East have been defined in the literature. However, no standard protocol of water security assessment has been used in the majority of studies. Study design and methods Uniform water security indicators collected from Russian official statistical sources for the period 2000–2011 were used for comparison for 18 selected regions in the Russian Arctic, Siberia and Far East. The following indicators of water security were analyzed: water consumption, chemical and biological contamination of water reservoirs of Categories I and II of water sources (centralized – underground and surface, and non-centralized) and of drinking water. Results Water consumption in selected regions fluctuated from 125 to 340 L/person/day. Centralized water sources (both underground and surface sources) are highly contaminated by chemicals (up to 40–80%) and biological agents (up to 55% in some regions), mainly due to surface water sources. Underground water sources show relatively low levels of biological contamination, while chemical contamination is high due to additional water contamination during water treatment and transportation in pipelines. Non-centralized water sources are highly contaminated (both chemically and biologically) in 32–90% of samples analyzed. Very high levels of chemical contamination of drinking water (up to 51%) were detected in many regions, mainly in the north-western part of the Russian Arctic. Biological contamination of drinking water was generally much lower (2.5–12%) everywhere except Evenki AO (27%), and general and thermotolerant coliform bacteria predominated in drinking water samples from all regions (up to 17.5 and 12.5%, correspondingly). The presence of other agents was much lower: Coliphages – 0.2–2

  3. Lifelong Learning and Adult Education: Russia Meets the West

    NASA Astrophysics Data System (ADS)

    Zajda, Joseph

    2003-03-01

    This article examines the impact of social change and economic transformation on adult education and lifelong learning in post-Soviet Russia. The article begins with a brief economic and historical background to lifelong learning and adult education in terms of its significance as a feature of the Russian cultural heritage. An analysis of Ministerial education policy and curriculum changes reveals that these policies reflect neo-liberal and neo-conservative paradigms in the post-Soviet economy and education. Current issues and trends in adult education are also discussed, with particular attention to the Adult Education Centres, which operate as a vast umbrella framework for a variety of adult education and lifelong learning initiatives. The Centres are designed to promote social justice by means of compensatory education and social rehabilitation for individuals dislocated by economic restructuring. The article comments on their role in helping to develop popular consciousness of democratic rights and active citizenship in a participatory and pluralistic democracy.

  4. Distribution and color variation of gyrfalcons in Russia

    USGS Publications Warehouse

    Ellis, D.H.; Ellis, Catherine H.; Pendleton, G.W.; Panteleyev, A.V.; Rebrova, I.V.; Markin, Y.M.

    1992-01-01

    Gyrfalcon (Falco rusticolus) museum specimens in Moscow (73) and St. Petersburg (132) were divided into four color classes (gray, light gray, white gray, and white) and four longitudinal belts representing major physiographic regions of northern Russia. Gray variants predominated in the west and central regions. White birds were most common in extreme eastern Siberia, but were occasionally found even west of the Ural Mountains. Frequencies were as follows: European Russia 4% white, 50% gray (the remainder were intermediates); western Siberia 0% white, 58% gray; central Siberia 15% white, 42% gray; and eastern Siberia 47% white, 33% gray. Remarkably, in the easternmost subregion, white birds predominated even near the southernmost extension. Because the northernmost portions of the species' range in continental Russia are in central Siberia where white variants were rare, we propose that a better predictor of the white variant is longitude, not latitude. White birds were most frequent at the eastern reaches of both the Palearctic and Nearctic. The best environmental correlates of this distribution pattern may be the southward bending thermal isoclines proceeding eastward toward Greenland or Kamchatka, where both land masses are bathed by cold oceanic currents of Arctic origin. By contrast, the western reaches of both land masses are bathed by warm currents. In these western reaches, Gyrfalcon summer distribution is displaced northward and dark variants predominate. The breeding range of the Gyrfalcon, determined by mapping the locations of the specimens we examined, differs little from the range proposed in 1951.

  5. Using a Whole-stream Approach to Quantify Headwater Yedoma DOC Processing Rates in NE Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Heslop, J.; Walter Anthony, K. M.; Davydova, A.; Davydov, S. P.; Zimov, N.

    2015-12-01

    Climate warming triggers the release of permafrost organic carbon (OC) via permafrost thaw and erosion, exporting large amounts of terrestrial C to aquatic environments and making previously frozen OC from a range of soil depths available for microbial processing. It is estimated 210-476 Pg C is stored in deep, ice-rich loess-dominated soils referred to as yedoma. Yedoma is extensive in NE Siberia and Alaska, where it underlies an area of over 1,000,000 km2 and averages 25 m in thickness. Recent research suggests ancient (Pleistocene-aged) permafrost OC, such as yedoma OC, is rapidly and preferentially utilized by microbial communities in Arctic headwater streams. We utilized a combination of short-term laboratory incubations and a whole-stream approach to examine permafrost-derived dissolved organic carbon (DOC) uptake, processing, and transport rates in a small stream which drains yedoma uplands in Cherskii, NE Siberia. Short-term incubations were conducted on permafrost leachates mixed with stream water to quantify microbial processing rates of permafrost-derived DOC from leachates made with surface (0-15 cm), shallow (70-100 cm), and deep (<2 m) yedoma sediments. In addition, we conducted whole-stream DOC release experiments to quantify permafrost DOC uptake length, rate, and velocity. DOC composition from samples collected during both the incubations and the nutrient-release experiments was characterized using absorbance measurements (SUVA254 and SR) and florescence spectrometry (EEMs) to quantify how DOC composition correlates to and changes with permafrost DOC bioavailability and processing parameters. Preliminary results suggest DOC processing rates may be highest in leachates made from surface sediments, which receive fresh OC input from modern ecosystems, and from deep sediments, which contain ancient, previously immobile OC. Shallow permafrost OC, which experiences degradation from annual freeze-thaw cycles without receiving fresh OC input, may have the

  6. Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010

    USGS Publications Warehouse

    Klett, T.R.

    2011-01-01

    The U.S. Geological Survey, using a geology-based assessment methodology, estimated mean volumes of technically recoverable, conventional, undiscovered petroleum resources at 8 billion barrels of crude oil, 670 trillion cubic feet of natural gas, and 21 billion barrels of natural gas liquids for the West Siberian Basin Province in Russia as part of a program to estimate petroleum resources for priority basins throughout the world.

  7. Natural and environmental vulnerability analysis through remote sensing and GIS techniques: a case study of Indigirka River basin, Eastern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Boori, Mukesh S.; Choudhary, Komal; Kupriyanov, Alexander; Sugimoto, Atsuko; Evers, Mariele

    2016-10-01

    The aim of this research work is to understand natural and environmental vulnerability situation and its cause such as intensity, distribution and socio-economic effect in the Indigirka River basin, Eastern Siberia, Russia. This paper identifies, assess and classify natural and environmental vulnerability using landscape pattern from multidisciplinary approach, based on remote sensing and Geographical Information System (GIS) techniques. A model was developed by following thematic layers: land use/cover, vegetation, wetland, geology, geomorphology and soil in ArcGIS 10.2 software. According to numerical results vulnerability classified into five levels: low, sensible, moderate, high and extreme vulnerability by mean of cluster principal. Results are shows that in natural vulnerability maximum area covered by moderate (29.84%) and sensible (38.61%) vulnerability and environmental vulnerability concentrated by moderate (49.30%) vulnerability. So study area has at medial level vulnerability. The results found that the methodology applied was effective enough in the understanding of the current conservation circumstances of the river basin in relation to their environment with the help of remote sensing and GIS. This study is helpful for decision making for eco-environmental recovering and rebuilding as well as predicting the future development.

  8. Investigations of the Nizhnekanskiy granitoid massif (Middle Siberia, Russia) as a promising territory for deep geological disposal of HLW: Results of pre-exploration stages of the work

    SciTech Connect

    Anderson, E.B.; Shabalev, S.I.; Savonenkov, V.G.; Lyubtseva, E.F.; Rogozin, Y.M.

    1999-07-01

    To decide the final fate of high-level radioactive wastes that are in Krasnoyarsk Land, Russia, and, most importantly the wastes from a weapons complex at the Mining-Chemical Combine (MCC, Krasnoyarsk-26), suitable sites for geological disposal of the wastes are being sought in Middle Siberia. The ultimate goal is to select one site for development of a repository for these wastes. As a result of complex geological-geophysical work completed to date, the two most promising sites are in the northern part of the Nizhnekanskiy granitoid massif (the Yenisei Ridge). These sites are approximately 25 km from the MCC. Based on geotectonic analysis and electrical surveying data, these sites are composed of low-permeability biotite granite that extends to relatively great depth. At present, both sites are undergoing more detailed studies to define the most suitable one for detailed geological exploration. Radiogeochemical studies showed that granitoid rock samples from the massif exhibited high retention for major long-lived radionuclides in the wastes. The general results of the investigations are presented.

  9. Distribution of late Pleistocene ice-rich syngenetic permafrost of the Yedoma Suite in east and central Siberia, Russia

    USGS Publications Warehouse

    Grosse, Guido; Robinson, Joel E.; Bryant, Robin; Taylor, Maxwell D.; Harper, William; DeMasi, Amy; Kyker-Snowman, Emily; Veremeeva, Alexandra; Schirrmeister, Lutz; Harden, Jennifer

    2013-01-01

    This digital database is the product of collaboration between the U.S. Geological Survey, the Geophysical Institute at the University of Alaska, Fairbanks; the Los Altos Hills Foothill College GeoSpatial Technology Certificate Program; the Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany; and the Institute of Physical Chemical and Biological Problems in Soil Science of the Russian Academy of Sciences. The primary goal for creating this digital database is to enhance current estimates of soil organic carbon stored in deep permafrost, in particular the late Pleistocene syngenetic ice-rich permafrost deposits of the Yedoma Suite. Previous studies estimated that Yedoma deposits cover about 1 million square kilometers of a large region in central and eastern Siberia, but these estimates generally are based on maps with scales smaller than 1:10,000,000. Taking into account this large area, it was estimated that Yedoma may store as much as 500 petagrams of soil organic carbon, a large part of which is vulnerable to thaw and mobilization from thermokarst and erosion. To refine assessments of the spatial distribution of Yedoma deposits, we digitized 11 Russian Quaternary geologic maps. Our study focused on extracting geologic units interpreted by us as late Pleistocene ice-rich syngenetic Yedoma deposits based on lithology, ground ice conditions, stratigraphy, and geomorphological and spatial association. These Yedoma units then were merged into a single data layer across map tiles. The spatial database provides a useful update of the spatial distribution of this deposit for an approximately 2.32 million square kilometers land area in Siberia that will (1) serve as a core database for future refinements of Yedoma distribution in additional regions, and (2) provide a starting point to revise the size of deep but thaw-vulnerable permafrost carbon pools in the Arctic based on surface geology and the distribution of cryolithofacies types at high spatial

  10. Tree Line Structure and Dynamics at the Northern Limit of the Larch Forest: Anabar Plateau, Siberia, Russia

    NASA Technical Reports Server (NTRS)

    Kharuk, Viacheslav I.; Ranson, Kenneth J.; Im, Sergey T.; Oskorbin, Pavel A.; Dvinskaya, Maria L.; Ovchinnikov, Dmitriy V.

    2013-01-01

    The goal of the study was to provide an analysis of climate impact before, during, and after the Little Ice Age (LIA) on the larch (Larix gmelinii) tree line at the northern extreme of Siberian forests. Recent decadal climate change impacts on the tree line, regeneration abundance, and age structure were analyzed. The location of the study area was within the forest-tundra ecotone (elevation range 170-450 m) in the Anabar Plateau, northern Siberia. Field studies were conducted along elevational transects. Tree natality/mortality and radial increment were determined based on dendrochronology analyses. Tree morphology, number of living and subfossil trees, regeneration abundance, and age structure were studied. Locations of pre-LIA, LIA, and post-LIA tree lines and refugia boundaries were established. Long-term climate variables and drought index were included in the analysis. It was found that tree mortality from the 16th century through the beginning of the 19th century caused a downward tree line recession. Sparse larch stands experienced deforestation, transforming into tundra with isolated relict trees. The maximum tree mortality and radial growth decrease were observed to have occurred at the beginning of 18th century. Now larch, at its northern boundary in Siberia, is migrating into tundra areas. Upward tree migration was induced by warming in the middle of the 19th century. Refugia played an important role in repopulation of the forest-tundra ecotone by providing a seed source and shelter for recruitment of larch regeneration. Currently this ecotone is being repopulated mainly by tree cohorts that were established after the 1930s. The last two decades of warming did not result in an acceleration of regeneration recruitment because of increased drought conditions. The regeneration line reached (but did not exceed) the pre-LIA tree line location, although contemporary tree heights and stand densities are comparatively lower than in the pre-LIA period. The mean

  11. Petroleum geology and resources of the West Siberian Basin, Russia

    USGS Publications Warehouse

    Ulmishek, Gregory F.

    2003-01-01

    The West Siberian basin is the largest petroleum basin in the world covering an area of about 2.2 million km2. The basin occupies a swampy plain between the Ural Mountains and the Yenisey River. On the north, the basin extends offshore into the southern Kara Sea. On the west, north, and east, the basin is surrounded by the Ural, Yenisey Ridge, and Turukhan-Igarka foldbelts that experienced major deformations during the Hercynian tectonic event and the Novaya Zemlya foldbelt that was deformed in early Cimmerian (Triassic) time. On the south, the folded Caledonian structures of the Central Kazakhstan and Altay-Sayan regions dip northward beneath the basin?s sedimentary cover. The basin is a relatively undeformed Mesozoic sag that overlies the Hercynian accreted terrane and the Early Triassic rift system. The basement is composed of foldbelts that were deformed in Late Carboniferous?Permian time during collision of the Siberian and Kazakhstan continents with the Russian craton. The basement also includes several microcontinental blocks with a relatively undeformed Paleozoic sedimentary sequence. The sedimentary succession of the basin is composed of Middle Triassic through Tertiary clastic rocks. The lower part of this succession is present only in the northern part of the basin; southward, progressively younger strata onlap the basement, so that in the southern areas the basement is overlain by Toarcian and younger rocks. The important stage in tectono-stratigraphic development of the basin was formation of a deep-water sea in Volgian?early Berriasian time. The sea covered more than one million km2 in the central basin area. Highly organic-rich siliceous shales of the Bazhenov Formation were deposited during this time in anoxic conditions on the sea bottom. Rocks of this formation have generated more than 80 percent of West Siberian oil reserves and probably a substantial part of its gas reserves. The deep-water basin was filled by prograding clastic clinoforms

  12. Agricultural landscapes dynamic at the North-West of Russia

    NASA Astrophysics Data System (ADS)

    Guzel, N.

    2012-04-01

    The process of reduction of agrolandscapes has taken place some decades in the North-Western European Russia. During 100 last years the area of agricultural lands have reduced in 1,4 times on the Karelian Isthmus. The most part of it had been abandoned after change of State border after of the Second World War. The processes of overgrowing of the former agricultural lands are studied on the landscapes base. The types of landscapes are distinguished on the based of the morphological relief symptoms, characteristics of the structure rock and the humid regime. Agricultural lands occupy landscapes such as kames, sandy, sandy-loam, clayey plains, sometimes with excess moistening, sandy fluvioglacial plains, loamy morainic plains, mesotrophic and evtrophic peat-bogs. Four stages can be revealed. I - (period to 20 years after termination of agricultural use) - grass-herb meadow with unclosed brush II - (20 - 40) - shrub layer with closed or low-closed canopy and unclosed or low closed small-leaved regrowth III - (40 - 80) - closed small-leaved forest, sometime including the coniferous trees IY - predomination of the coniferous on small-leaved trees Reestablish vegetation successions can be realised by different ways, with different rate, including various trees and ecological groups of species in different landscapes. In the different sites many traits in common are discovered during this processes. The processes taking place in soil of abandoned agricultural lands are expressed more poorly than in vegetation as soil is more "conservative" element of landscape. Now most area occupies former agricultural lands, inhering on III stage and presenting itself small-leaved forest. Over the last decade because of a change in the socio-political situation there has emerged a tendency towards an increase in the area of the cultivated land in the Karelian Isthmus including the secondary development of previously abandoned lands. However, this process is going on spontaneously; there

  13. Climatic extremes in the north of the west Siberia: millennium chronicle inferred from tree rings.

    NASA Astrophysics Data System (ADS)

    Gorlanova, L.; Hantemirov, R.; Shiyatov, S.; Schweingruber, F.

    2003-04-01

    Extreme climatic events, like frosts and temperature drops, have a strong effect on the functioning of subarctic ecosystems. The best tool for long reconstruction of climatic extremes in the northern regions of Siberia is anatomical analysis of annual rings of trees, and specially shrubs. Frost and light rings of living and dead individuals of Siberian juniper (Juniperus sibirica Burgsd.) and Siberian larch (Larix sibirica Ledeb.) growing at the upper (Polar Ural mountains) and polar (Yamal Peninsula) tree lines in the northwest Siberia have been studied to reconstruct summer frosts and many days abrupt fall of temperature during the second half of growing season over the past 1250 years. The oldest living branches of Siberian juniper we are found 840 years old, the oldest living Siberian larches in this region are 500 years old. However dead stems and branches remain for long centuries. Therefore the chronologies of pathological structures, produced using both living and dried-off stems and branches, are more than 1000-year length. In found juniper, the presence of frost rings provides evidence for frosts that occurred in July. Generally in the same summer larches form frost- or light-rings. Long term and pronounced air temperature drop in the middle of very warm period in the second half of July is the factor responsible for fluctuations of wood density (false rings) in annual rings of juniper and larch. Based on these relationships we can interpret incidence of pathological structures in terms of strong temperature abnormalities. Conclusion has been made, that in July the most severe frosts took place in 801, 1109, 1259, 1278, 1328, 1453, 1466, 1481, 1601, 1783, 1857, and 1882 AD. Pronounced temperature drops in the middle of July took place in 1555, 1610, 1621, 1919, 1947 AD. Comparison our data with data from other regions of the world have been shown that there is agreement in the timing of extreme temperature events of 800-801, 1109, 1258-1259, 1453, 1466

  14. [On longevity among the population of Siberia and the Far East].

    PubMed

    Nikitin YuP; Tatarinova, O V

    1996-01-01

    Demographic values of longevity have been calculated on the basis of population census data and mortality tables. Analysis of the present-day level of longevity in Siberia and Far East and its time course in 1979-1993 is presented. Regular reduction of longevity parameters from West to East and lower values of these parameters in comparison with the rest of Russia have been revealed. Negative shifts in the levels of longevity over the period of 1979 to 1993 have been observed for all regions of Siberia and Far East.

  15. The Influence of Seasonal Climatic Parameters on the Permafrost Thermal Regime in West Siberia

    NASA Astrophysics Data System (ADS)

    Popova, V. V.; Shmakin, A. B.

    2009-12-01

    Statistical correlations between seasonal air temperatures and snow depths and active layer depths and permafrost temperatures were analyzed for tundra (Marre-Salle) and northern taiga (Nadym) sites in Western Siberia. Interannual variations in active layer depth in the tundra zone correlated with the average air temperature of the current summer, and in peatland and humid tundra, also with summer temperatures of the preceding 1-2 years. In the northern taiga zone, the active layer depth related to current summer air temperature and to a lesser extent, to spring and/or winter air temperatures. Variations in summer permafrost temperatures at 5-10m depth were correlated with spring air temperatures in the current and preceding 1-2 years. The weather regime during the preceding 1-2 years, therefore, reinforced or weakened ground temperature variations in a given year. Overall, the most important factors influencing the permafrost regime were spring and summer air temperatures, and in one case snow depth. However, statistical links between meteorological and permafrost parameters varied between the tundra and northern taiga zones and among landscape types within each zone, emphasizing the importance of analyses at short temporal scales and for individual terrain units.

  16. Trace metal distribution in pristine permafrost-affected soils of the Lena River Delta and its Hinterland, Northern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Antcibor, I.; Zubrzycki, S.; Eschenbach, A.; Kutzbach, L.; Bol'shiyanov, D.; Pfeiffer, E.-M.

    2013-02-01

    Soils are an important compartment of ecosystems and have the ability to immobilize chemicals preventing their movement to other environment compartments. Predicted climatic changes together with other anthropogenic influences on Arctic terrestrial environments may affect biogeochemical processes enhancing leaching and migration of trace elements in permafrost-affected soils. This is especially important since the Arctic ecosystems are considered to be very sensitive to climatic changes as well as to chemical contamination. This study characterizes background levels of trace metals in permafrost-affected soils of the Lena River Delta and its hinterland in northern Siberia (73.5° N-69.5° N) representing a remote region far from evident anthropogenic trace metal sources. Investigations on total element contents of iron (Fe), arsenic (As), manganese (Mn), zinc (Zn), nickel (Ni), copper (Cu), lead (Pb), cadmium (Cd), cobalt (Co) and mercury (Hg) in different soil types developed in different geological parent materials have been carried out. The highest concentrations of the majority of the measured elements were observed in soils belonging to ice-rich permafrost sediments formed during the Pleistocene (ice-complex) in the Lena River Delta region. Correlation analyses of trace metal concentrations and soil chemical and physical properties at a Holocene estuarine terrace and two modern floodplain levels in the southern-central Lena River Delta (Samoylov Island) showed that the main factors controlling the trace metal distribution in these soils are organic matter content, soil texture and contents of iron and manganese-oxides. Principal Component Analysis (PCA) revealed that soil oxides play a significant role in trace metal distribution in both top and bottom horizons. Occurrence of organic matter contributes to Cd binding in top soils and Cu binding in bottom horizons. Observed ranges of the background concentrations of the majority of trace elements were similar to

  17. Trace metal distribution in pristine permafrost-affected soils of the Lena River delta and its hinterland, northern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Antcibor, I.; Eschenbach, A.; Zubrzycki, S.; Kutzbach, L.; Bolshiyanov, D.; Pfeiffer, E.-M.

    2014-01-01

    Soils are an important compartment of ecosystems and have the ability to buffer and immobilize substances of natural and anthropogenic origin to prevent their movement to other environment compartments. Predicted climatic changes together with other anthropogenic influences on Arctic terrestrial environments may affect biogeochemical processes enhancing leaching and migration of trace elements in permafrost-affected soils. This is especially important since Arctic ecosystems are considered to be highly sensitive to climatic changes as well as to chemical contamination. This study characterises background levels of trace metals in permafrost-affected soils of the Lena River delta and its hinterland in northern Siberia (73.5-69.5° N), representing a remote region far from evident anthropogenic trace metal sources. Investigations on the element content of iron (Fe), arsenic (As), manganese (Mn), zinc (Zn), nickel (Ni), copper (Cu), lead (Pb), cadmium (Cd), cobalt (Co), and mercury (Hg) in different soil types developed in different geological parent materials have been carried out. The highest median concentrations of Fe and Mn were observed in soils belonging to ice-rich permafrost sediments formed during the Pleistocene (ice-complex) while the highest median values of Ni, Pb and Zn were found in soils of both the ice-complex and the Holocene estuarine terrace of the Lena River delta region, as well as in the southernmost study unit of the hinterland area. Detailed observations of trace metal distribution on the micro scale showed that organic matter content, soil texture and iron-oxide contents influenced by cryogenic processes, temperature, and hydrological regimes are the most important factors determining the metal abundance in permafrost-affected soils. The observed range of trace element background concentrations was similar to trace metal levels reported for other pristine northern areas.

  18. Visualizing petroleum systems with a combination of GIS and multimedia technologies: An example from the West Siberia Basin

    SciTech Connect

    Walsh, D.B.; Grace, J.D. )

    1996-01-01

    Petroleum system studies provide an ideal application for the combination of Geographic Information System (GIS) and multimedia technologies. GIS technology is used to build and maintain the spatial and tabular data within the study region. Spatial data may comprise the zones of active source rocks and potential reservoir facies. Similarly, tabular data include the attendant source rock parameters (e.g. pyroloysis results, organic carbon content) and field-level exploration and production histories for the basin. Once the spatial and tabular data base has been constructed, GIS technology is useful in finding favorable exploration trends, such as zones of high organic content, mature source rocks in positions adjacent to sealed, high porosity reservoir facies. Multimedia technology provides powerful visualization tools for petroleum system studies. The components of petroleum system development, most importantly generation, migration and trap development typically span periods of tens to hundreds of millions of years. The ability to animate spatial data over time provides an insightful alternative for studying the development of processes which are only captured in [open quotes]snapshots[close quotes] by static maps. New multimedia-authoring software provides this temporal dimension. The ability to record this data on CD-ROMs and allow user- interactivity further leverages the combination of spatial data bases, tabular data bases and time-based animations. The example used for this study was the Bazhenov-Neocomian petroleum system of West Siberia.

  19. Visualizing petroleum systems with a combination of GIS and multimedia technologies: An example from the West Siberia Basin

    SciTech Connect

    Walsh, D.B.; Grace, J.D.

    1996-12-31

    Petroleum system studies provide an ideal application for the combination of Geographic Information System (GIS) and multimedia technologies. GIS technology is used to build and maintain the spatial and tabular data within the study region. Spatial data may comprise the zones of active source rocks and potential reservoir facies. Similarly, tabular data include the attendant source rock parameters (e.g. pyroloysis results, organic carbon content) and field-level exploration and production histories for the basin. Once the spatial and tabular data base has been constructed, GIS technology is useful in finding favorable exploration trends, such as zones of high organic content, mature source rocks in positions adjacent to sealed, high porosity reservoir facies. Multimedia technology provides powerful visualization tools for petroleum system studies. The components of petroleum system development, most importantly generation, migration and trap development typically span periods of tens to hundreds of millions of years. The ability to animate spatial data over time provides an insightful alternative for studying the development of processes which are only captured in {open_quotes}snapshots{close_quotes} by static maps. New multimedia-authoring software provides this temporal dimension. The ability to record this data on CD-ROMs and allow user- interactivity further leverages the combination of spatial data bases, tabular data bases and time-based animations. The example used for this study was the Bazhenov-Neocomian petroleum system of West Siberia.

  20. Norilsk, Siberia

    NASA Technical Reports Server (NTRS)

    2008-01-01

    Norilsk is a major city in Krasnoyarsk Krai, Russia, and the northernmost city in Siberia. The city was founded in the 1930s as a settlement for the Norilsk mining-metallurgic complex, sitting near the largest nickel-copper-palladium deposits on Earth. Mining and smelting of nickel, copper, cobalt, platinum, palladium are the major industries. The nickel ore is smelted on site at Norilsk. The smelting is directly responsible for severe pollution, generally acid rain and smog. By some estimates, 1 percent of the entire global emissions of sulfur dioxide comes from this one city. Heavy metal pollution near Norilsk is so severe that it is now economically feasible to mine the soil, which has been polluted so severely that it has economic grades of platinum and palladium.

    The image was acquired July 21, 2000, covers an area of 36.9 x 37.6 km, and is located at 69.3 degrees north latitude, 88.2 degrees east longitude.

    The U.S. science team is located at NASA's Jet Propulsion Laboratory, Pasadena, Calif. The Terra mission is part of NASA's Science Mission Directorate.

  1. WETCHIMP-WSL: Intercomparison of wetland methane emissions models over West Siberia

    SciTech Connect

    Bohn, T. J.; Melton, J. R.; Ito, A.; Kleinen, T.; Spahni, R.; Stocker, B. D.; Zhang, B.; Zhu, X.; Schroeder, R.; Glagolev, M. V.; Maksyutov, S.; Brovkin, V.; Chen, G.; Denisov, S. N.; Eliseev, A. V.; Gallego-Sala, A.; McDonald, K. C.; Rawlins, M. A.; Riley, W. J.; Subin, Z. M.; Tian, H.; Zhuang, Q.; Kaplan, J. O.

    2015-06-03

    Wetlands are the world's largest natural source of methane, a powerful greenhouse gas. The strong sensitivity of methane emissions to environmental factors such as soil temperature and moisture has led to concerns about potential positive feedbacks to climate change. This risk is particularly relevant at high latitudes, which have experienced pronounced warming and where thawing permafrost could potentially liberate large amounts of labile carbon over the next 100 years. However, global models disagree as to the magnitude and spatial distribution of emissions, due to uncertainties in wetland area and emissions per unit area and a scarcity of in situ observations. Recent intensive field campaigns across the West Siberian Lowland (WSL) make this an ideal region over which to assess the performance of large-scale process-based wetland models in a high-latitude environment. Here we present the results of a follow-up to the Wetland and Wetland CH4 Intercomparison of Models Project (WETCHIMP), focused on the West Siberian Lowland (WETCHIMP-WSL). We assessed 21 models and 5 inversions over this domain in terms of total CH4 emissions, simulated wetland areas, and CH4 fluxes per unit wetland area and compared these results to an intensive in situ CH4 flux data set, several wetland maps, and two satellite surface water products. We found that (a) despite the large scatter of individual estimates, 12-year mean estimates of annual total emissions over the WSL from forward models (5.34 ± 0.54 Tg CH4 yr⁻¹), inversions (6.06 ± 1.22 Tg CH4 yr⁻¹), and in situ observations (3.91 ± 1.29 Tg CH4 yr⁻¹) largely agreed; (b) forward models using surface water products alone to estimate wetland areas suffered from severe biases in CH4 emissions; (c) the interannual time series of models that lacked either soil thermal physics appropriate to the high latitudes or realistic emissions from

  2. WETCHIMP-WSL: Intercomparison of wetland methane emissions models over West Siberia

    DOE PAGES

    Bohn, T. J.; Melton, J. R.; Ito, A.; ...

    2015-06-03

    Wetlands are the world's largest natural source of methane, a powerful greenhouse gas. The strong sensitivity of methane emissions to environmental factors such as soil temperature and moisture has led to concerns about potential positive feedbacks to climate change. This risk is particularly relevant at high latitudes, which have experienced pronounced warming and where thawing permafrost could potentially liberate large amounts of labile carbon over the next 100 years. However, global models disagree as to the magnitude and spatial distribution of emissions, due to uncertainties in wetland area and emissions per unit area and a scarcity of in situ observations.more » Recent intensive field campaigns across the West Siberian Lowland (WSL) make this an ideal region over which to assess the performance of large-scale process-based wetland models in a high-latitude environment. Here we present the results of a follow-up to the Wetland and Wetland CH4 Intercomparison of Models Project (WETCHIMP), focused on the West Siberian Lowland (WETCHIMP-WSL). We assessed 21 models and 5 inversions over this domain in terms of total CH4 emissions, simulated wetland areas, and CH4 fluxes per unit wetland area and compared these results to an intensive in situ CH4 flux data set, several wetland maps, and two satellite surface water products. We found that (a) despite the large scatter of individual estimates, 12-year mean estimates of annual total emissions over the WSL from forward models (5.34 ± 0.54 Tg CH4 yr⁻¹), inversions (6.06 ± 1.22 Tg CH4 yr⁻¹), and in situ observations (3.91 ± 1.29 Tg CH4 yr⁻¹) largely agreed; (b) forward models using surface water products alone to estimate wetland areas suffered from severe biases in CH4 emissions; (c) the interannual time series of models that lacked either soil thermal physics appropriate to the high latitudes or realistic emissions from unsaturated peatlands tended to be dominated by a single environmental driver

  3. [Demographic factors of longevity in Siberia and Far East].

    PubMed

    Nikitin, Iu P; Tatarinova, O V

    1994-01-01

    Longevity indexes LI2 and LI3 (subjects aged 90 and more and 100 and more, respectively, among subjects of 60 and older) were compared in all administrative units on the basis of results of 1989 Census of the population and data of the Central Statistical Office. These values reduce from West to East: LI2 in Western Siberia is equal to 8.48/1000, LI3 to 0.45/1000, in Eastern Siberia these values are 7.48 and 0.35/1000, in the Far East 5.20 and 0.31/1000, in Russia on the whole 9.16 and 0.47/1000, respectively. The territories with relatively high LI2 values were the Aghinsk Buryat Autonomous Territory (11.42/1000), Yakutia (10.79/1000), Altai (9.41/1000).

  4. The incidence of West Nile disease in Russia in relation to climatic and environmental factors.

    PubMed

    Platonov, Alexander E; Tolpin, Vladimir A; Gridneva, Kristina A; Titkov, Anton V; Platonova, Olga V; Kolyasnikova, Nadezhda M; Busani, Luca; Rezza, Giovanni

    2014-01-23

    Since 1999, human cases of West Nile fever/neuroinvasive disease (WND) have been reported annually in Russia. The highest incidence has been recorded in three provinces of southern European Russia (Volgograd, Astrakhan and Rostov Provinces), yet in 2010-2012 the distribution of human cases expanded northwards considerably. From year to year, the number of WND cases varied widely, with major WND outbreaks in 1999, 2007, 2010, and 2012. The present study was aimed at identifying the most important climatic and environmental factors potentially affecting WND incidence in the three above-mentioned provinces and at building simple prognostic models, using those factors, by the decision trees method. The effects of 96 variables, including mean monthly temperature, relative humidity, precipitation, Normalized Difference Vegetation Index, etc. were taken into account. The findings of this analysis show that an increase of human WND incidence, compared to the previous year, was mostly driven by higher temperatures in May and/or in June, as well as (to a lesser extent) by high August-September temperatures. Declining incidence was associated with cold winters (December and/or January, depending on the region and type of model). WND incidence also tended to decrease during year following major WND outbreaks. Combining this information, the future trend of WND may be, to some extent, predicted, in accordance with the climatic conditions observed before the summer peak of WND incidence.

  5. The Incidence of West Nile Disease in Russia in Relation to Climatic and Environmental Factors

    PubMed Central

    Platonov, Alexander E.; Tolpin, Vladimir A.; Gridneva, Kristina A.; Titkov, Anton V.; Platonova, Olga V.; Kolyasnikova, Nadezhda M.; Busani, Luca; Rezza, Giovanni

    2014-01-01

    Since 1999, human cases of West Nile fever/neuroinvasive disease (WND) have been reported annually in Russia. The highest incidence has been recorded in three provinces of southern European Russia (Volgograd, Astrakhan and Rostov Provinces), yet in 2010–2012 the distribution of human cases expanded northwards considerably. From year to year, the number of WND cases varied widely, with major WND outbreaks in 1999, 2007, 2010, and 2012. The present study was aimed at identifying the most important climatic and environmental factors potentially affecting WND incidence in the three above-mentioned provinces and at building simple prognostic models, using those factors, by the decision trees method. The effects of 96 variables, including mean monthly temperature, relative humidity, precipitation, Normalized Difference Vegetation Index, etc. were taken into account. The findings of this analysis show that an increase of human WND incidence, compared to the previous year, was mostly driven by higher temperatures in May and/or in June, as well as (to a lesser extent) by high August-September temperatures. Declining incidence was associated with cold winters (December and/or January, depending on the region and type of model). WND incidence also tended to decrease during year following major WND outbreaks. Combining this information, the future trend of WND may be, to some extent, predicted, in accordance with the climatic conditions observed before the summer peak of WND incidence. PMID:24464233

  6. Carbon flux estimation for Siberia by inverse modeling constrained by aircraft and tower CO2 measurements

    NASA Astrophysics Data System (ADS)

    Saeki, T.; Maksyutov, S.; Sasakawa, M.; Machida, T.; Arshinov, M.; Tans, P. P.; Conway, T. J.; Saito, M.; Valsala, V.; Oda, T.; Andres, R. J.

    2012-12-01

    Despite Siberian ecosystems being one of the largest carbon reservoirs in the world, the Siberian carbon sink remains poorly understood due to the limited numbers of observations. We present the first results of atmospheric CO2 inversions utilizing measurements from a Siberian tower network (Japan-Russia Siberian Tall Tower Inland Observation Network; JR-STATION) and four aircraft sites, in addition to surface background flask measurements by the National Oceanic and Atmospheric Administration (NOAA). The inverse model estimates monthly fluxes for 68 regions globally. Our inversion with only the NOAA data yielded a boreal Eurasian CO2 flux of -0.56 ± 0.79 GtC yr-1, whereas we obtained a weaker uptake of -0.35 ± 0.61 GtC yr-1 when the Siberian data were also included. This difference is mainly explained by a weakened summer uptake, especially in East Siberia. We also found the inclusion of the Siberian data had significant impacts on inversion results over northeastern Europe as well as boreal Eurasia. The inversion with the Siberian data reduced the regional uncertainty by 22 % on average in boreal Eurasia, and further uncertainty reductions up to 80 % were found in eastern and western Siberia. Larger interannual variability was clearly seen in the inversion including the Siberia data than the inversion without the Siberia data. In the inversion with NOAA plus Siberia data, East Siberia showed larger interannual variability than that in West and Central Siberia. Finally, we conducted forward simulations using estimated fluxes and confirmed that the fit to independent measurements over Central Siberia, which were not included in the inversions, was visibly improved.

  7. Carbon flux estimation for Siberia by inverse modeling constrained by aircraft and tower CO2 measurements

    NASA Astrophysics Data System (ADS)

    Saeki, T.; Maksyutov, S.; Sasakawa, M.; Machida, T.; Arshinov, M.; Tans, P.; Conway, T. J.; Saito, M.; Valsala, V.; Oda, T.; Andres, R. J.; Belikov, D.

    2013-01-01

    Being one of the largest carbon reservoirs in the world, the Siberian carbon sink however remains poorly understood due to the limited numbers of observation. We present the first results of atmospheric CO2 inversions utilizing measurements from a Siberian tower network (Japan-Russia Siberian Tall Tower Inland Observation Network; JR-STATION) and four aircraft sites, in addition to surface background flask measurements by the National Oceanic and Atmospheric Administration (NOAA). Our inversion with only the NOAA data yielded a boreal Eurasian CO2 flux of -0.56 ± 0.79 GtC yr-1, whereas we obtained a weaker uptake of -0.35 ± 0.61 GtC yr-1 when the Siberian data were also included. This difference is mainly explained by a weakened summer uptake, especially in East Siberia. We also found the inclusion of the Siberian data had significant impacts on inversion results over northeastern Europe as well as boreal Eurasia. The inversion with the Siberian data reduced the regional uncertainty by 22% on average in boreal Eurasia, and further uncertainty reductions up to 80% were found in eastern and western Siberia. Larger interannual variability was clearly seen in the inversion which includes the Siberia data than the inversion without the Siberia data. In the inversion with NOAA plus Siberia data, east Siberia showed a larger interannual variability than that in west and central Siberia. Finally, we conducted forward simulations using estimated fluxes and confirmed that the fit to independent measurements over central Siberia, which were not included in inversions, was greatly improved.

  8. Ferrotochilinite, 6FeS · 5Fe(OH)2, a new mineral from the Oktyabr'sky deposit, Noril'sk district, Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Pekov, I. V.; Sereda, E. V.; Polekhovsky, Yu. S.; Britvin, S. N.; Chukanov, N. V.; Yapaskurt, V. O.; Bryzgalov, I. A.

    2013-12-01

    A new mineral, ferrotochilinite, ideally 6FeS · 5Fe(OH)2, was found at the Oktyabr'sky Mine, Oktyabr'skoe Cu-Ni deposit, Noril'sk, Krasnoyarsk krai, Siberia, Russia. It is associated with ferrovalleriite, magnetite and Fe-rich, chlorite-like phyllosilicate in the cavities of pentlandite-mooihoekite-cubanite ore with subordinate magnetite and chalcopyrite. Ferrotochilinite occurs as flattened on [001], prismatic to elongated lamellar crystals up to 0.1 × 0.5 × 3.2 mm, typically split and curved. Aggregates (up to 6.5 mm in size) are fanlike, rosette-like, or chaotic. Ferrotochilinite is dark bronze. The streak is black. The luster is moderately metallic. The Mohs' hardness is ca. 1; VHN is 13 kg/mm2. Cleavage is {001} perfect, micalike. Individuals are flexible, inelastic. D(calc) = 3.467 g/cm3. In reflected light, ferrotochilinite is gray, with the hue changing from pale beige to bluish; bireflectance is distinct. Anisotropy is distinct, with gray bluish to yellowish beige rotation colors. No internal reflections. Reflectance values [ R min- R max, % (λ, nm)] are: 11.6-11.4 (470), 11.2-12.4 (546), 11.1-13.6 (589), 11.0-15.5 (650). The IR spectrum shows the presence of (OH) groups bonded with Fe cations and the absence of H2O molecules. Chemical composition (wt %; electron probe; H content is calculated) is as follows: 0.02 Mg, 61.92 Fe, 0.03 Ni, 0.09 Cu, 19.45 S, 16.3 O, 1.03 H calc; the total is 98.84. The empirical formula calculated on the basis of 6 S atoms is: Mg0.01Fe10.96Ni0.005Cu0.015S6(OH)10.07 = (Fe5.98Cu0.0015Ni0.005)Σ6S6(OH)9.80(Fe{4.89/2+}Mg0.01)Σ4.90(OH)9.80Fe{0.09/3+}(OH)0.27. Ferrotochilinite is monoclinic, space group is C2/ m, Cm or C2, the unit-cell dimensions are: a = 5.463(5), b = 15.865(17), c = 10.825(12) Å, β = 93.7(1)°, V = 936(3) Å3, Z = 2. The strongest reflections in the X-ray powder diffraction pattern ( d, Å- I[ hkl]) are: 10.83-13[001], 5.392-100[002], 3.281-7[023], 2.777-7[150], 2.696-12[004, ], 2.524-12[, ], 2

  9. Assessment of Undiscovered Oil and Gas Resources of the West Siberian Basin Province, Russia, 2008

    USGS Publications Warehouse

    Schenk, Christopher J.; Bird, Kenneth J.; Charpentier, Ronald R.; Gautier, Donald L.; Houseknecht, David W.; Klett, Timothy R.; Moore, Thomas E.; Pawlewicz, Mark J.; Pitman, Janet K.; Tennyson, Marilyn E.

    2008-01-01

    The U.S. Geological Survey (USGS) recently assessed the undiscovered oil and gas potential of the West Siberian Basin Province in Russia as part of the USGS Circum-Arctic Resource Appraisal program. This province is the largest petroleum basin in the world and has an areal extent of about 2.2 million square kilometers. It is a large rift-sag feature bounded to the west by the Ural fold belt, to the north by the Novaya Zemlya fold belt and North Siberian Sill, to the south by the Turgay Depression and Altay-Sayan fold belt, and to the east by the Yenisey Ridge, Turukhan-Igarka uplift, Yenisey-Khatanga Basin, and Taimyr High. The West Siberian Basin Province has a total discovered oil and gas volume of more than 360 billion barrels of oil equivalent (Ulmishek, 2000). Exploration has led to the discovery of tens of giant oil and gas fields, including the Urengoy gas field with more than 3500 trillion cubic feet of gas reserves and Samotlar oil field with reserves of nearly 28 billion barrels of oil (Ulmishek, 2003). This report summarizes the results of a reassessment of the undiscovered oil and gas potential of that part of the province north of the Arctic Circle; a previous assessment that included the entire province was completed in 2000 (Ulmishek, 2000). The total petroleum system (TPS) and assessment units (AU) defined by the USGS for the assessments in 2000 were adopted for this assessment. However, only those parts of the Aus lying wholly or partially north of the Arctic Circle were assessed for this study.

  10. Bracketing the range of lake and wetland methane emissions rates in West Siberia using models, in situ observations, and remote sensing

    NASA Astrophysics Data System (ADS)

    Bohn, T.; Maksyutov, S.; Kim, H.-S.; Glagolev, M.; Schroeder, R.; McDonald, K.; Podest, E.; Chen, X.; Livneh, B.; Lettenmaier, D.

    2012-04-01

    Large uncertainties exist in estimates of global lake and wetland methane emission rates, due in part to their large spatial and temporal heterogeneity and also due to the sparseness of in situ observations. This is especially true of lakes and inundated wetlands, for which ebullition is a major methane pathway. Here we use a large-scale coupled land-atmosphere model and remote sensing observations to bracket the range of possible emissions rates from lakes and wetlands in West Siberia. Our modeling framework consists of a large-scale hydrology model (Variable Infiltration Capacity; VIC), extended to handle carbon cycling and methane emissions, coupled to an atmospheric tracer-transport model (NIES Chemical Tracer Model; CTM) driven by NCAR/NCEP reanalysis fields. In the model, "permanent" lake areas are prescribed by the Global Lake and Wetland Database, bias-corrected to account for small lakes. Seasonal inundation of wetlands is dynamic and has been calibrated to match an inundation dataset derived from remote sensing (AMSR-E and Qscat). We calibrated the model's wetland methane emissions to match in situ observations from a large dataset collected in West Siberia between 2006 and 2010. Lake emission rates are prescribed in several scenarios that span the range of observed rates reported in the literature. We explore the relative sizes of various sources of uncertainty in simulated methane emissions: uncertainty in inundated area, parameter uncertainty in the methane emissions model, and the range of possible lake emissions rates. Using values from different ends of the spectrum of these uncertainty sources leads to markedly different spatial patterns of methane emissions across West Siberia. These emissions are ingested by the atmospheric tracer model to produce maps of atmospheric methane concentrations. We compare the resulting spatial patterns of methane concentrations with remotely-sensed observations from the AIRS and GOSAT satellite sensors and explore

  11. Seasonal cycle and interannual variability of the total CH4 mixing ratios in West Siberia: Results from AIRS/AMSU and chemistry transport models for 2003-2013

    NASA Astrophysics Data System (ADS)

    Lagutin, Anatoly; Mordvin, Egor

    Methane (CH4) is an important greenhouse gas. It has much higher global warming potential comparing to carbon dioxide on per mass emitted basis. Atmospheric methane also plays an important role in atmospheric ozone chemistry and is the main source of water vapor in the stratosphere. The recent increase of CH4 in 2007-2008, after a nearly stable period of about one decade, is attributed to the increased emissions from tropical and Arctic wetlands. However, many uncertainties regarding natural and anthropogenic methane emissions still exist. For example, the total CH4 emissions from wetlands in West Siberia are estimated to be in the range from 1.6 to 20 Tg/year. The main causes leading to such large uncertainties are significant spatial and temporal variation of CH4 emissions and the sparseness of ground observational networks. The purpose of this study is to investigate the seasonal cycle and interannual variability of the total CH4 mixing ratios (CH4-Tot) in West Siberia for 2003-2013 using the AIRS/AMSU-Aqua measurements and the results from chemistry transport models MOZART4 and ACTM-CCSR/NIES/FRCGC. The key feature of the proposed approach is chemistry transport model-based regression equation linking CH4-Tot with mid-upper tropospheric CH4 (in the layer from 50 to 250 hPa below the tropopause), the tropopause height and the surface temperature. The observational information in our approach comes from the AIRS/AMSU measurements. Comparison of the retrieved CH4-Tot with the measurements of CH4 from the Total Carbon Column Observing Network (TCCON) have shown that the model captures observed seasonal cycles and interannual variability at mid-latitude sites. The spatial and temporal distributions of CH4-Tot in West Siberia for 2003-2013 are presented. Analysis of deseasonalized time-series indicates that the total CH4 mixing ratios increases about 4 ppbv/yr from 2007. This work was supported in part by the Russian Foundation for Basic Research (grant No 13

  12. Zonal Features of Bog and Lake Water Chemistry Along a Transect from Boreal to Arid Landscapes in The South of Western Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Kolpakova, Marina N.; Naymushina, Olga S.

    2016-10-01

    Western Siberia is a unique territory where more than 12000 water reservoirs are located. The region is characterized by high bogginess up to 90% in the north. Bog and lake systems are able to accumulate natural and technogenic resources, including trace elements and organic matter. The article presents the results of a surface water chemical composition along a 5-year monitoring. The obtained data allow concluding that dynamics of water chemistry is predetermined by their location in various landscape zones and subordinated to zonal distribution of such major landscape elements as moistening, evaporation, rate of groundwater flow, etc.

  13. [Changes in functional organization of the respiratory system among residents of West Siberia in the winter season].

    PubMed

    Shishkin, G S; Ustiuzhaninova, N V; Gul'tiaeva, V V

    2014-01-01

    The study examines respiratory parameters in healthy young males from Western Siberia. The correlations between the parameters are analyzed and the functional structure of the respiratory system in the summer and in the winter is identified. It was discovered that different regulatory programs operate depending on the temperature of inhaled air. The study shows that the changes in the oxygen request of the body in the summer are achieved through the changes in the volume of pulmonary ventilation ("ventilation" or "summer program"). In the winter, when maintaining the level of energy processes in the body is in conflict with maintaining thermal homeostasis in the respiratory regions of the lungs, pulmonary ventilation becomes limited and the number of functioning lung units is reduced. At the same time, for providing compensation, lung diffusion capacity increases ("diffusion" or "winter program"). This means that the functioning of the apparatus of external respiration is optimized in the winter.

  14. Sub-fossil beetle assemblages associated with the "mammoth fauna" in the Late Pleistocene localities of the Ural Mountains and West Siberia.

    PubMed

    Zinovyev, Evgeniy

    2011-01-01

    The distribution of beetles at the end of the Middle Pleninglacial (=terminal Quaternary) was examined based on sub-fossil material from the Ural Mountains and Western Siberia, Russia. All relevant localities of fossil insects have similar radiocarbon dates, ranging between 33,000 and 22,000 C14 years ago. Being situated across the vast territory from the southern Ural Mountains in the South to the middle Yamal Peninsula in the North, they allow latitudinal changes in beetle assemblages of that time to be traced. These beetles lived simultaneously with mammals of the so-called "mammoth fauna" with mammoth, bison, and wooly rhinoceros, the often co-occurring mega-mammalian bones at some of the sites being evidence of this. The beetle assemblages found between 59° and 57°N appear to be the most interesting. Their bulk is referred to as a "mixed" type, one which includes a characteristic combination of arcto-boreal, boreal, steppe and polyzonal species showing no analogues among recent insect complexes. These peculiar faunas seem to have represented a particular zonal type, which disappeared since the end of the Last Glaciation to arrive here with the extinction of the mammoth biota. In contrast, on the sites lying north of 60°N, the beetle communities were similar to modern sub-arctic and arctic faunas, yet with the participation of some sub-boreal steppe components, such as Poecilus ravus Lutshnik and Carabus sibiricus Fischer-Waldheim. This information, when compared with our knowledge of synchronous insect faunas from other regions of northern Eurasia, suggests that the former distribution of beetles in this region could be accounted for both by palaeo-environmental conditions and the impact of grazing by large ruminant mammals across the so-called "mammoth savannas".

  15. Sub-fossil beetle assemblages associated with the “mammoth fauna” in the Late Pleistocene localities of the Ural Mountains and West Siberia

    PubMed Central

    Zinovyev, Evgeniy

    2011-01-01

    Abstract The distribution of beetles at the end of the Middle Pleninglacial (=terminal Quaternary) was examined based on sub-fossil material from the Ural Mountains and Western Siberia, Russia. All relevant localities of fossil insects have similar radiocarbon dates, ranging between 33,000 and 22,000 C14 years ago. Being situated across the vast territory from the southern Ural Mountains in the South to the middle Yamal Peninsula in the North, they allow latitudinal changes in beetle assemblages of that time to be traced. These beetles lived simultaneously with mammals of the so-called “mammoth fauna” with mammoth, bison, and wooly rhinoceros, the often co-occurring mega-mammalian bones at some of the sites being evidence of this. The beetle assemblages found between 59° and 57°N appear to be the most interesting. Their bulk is referred to as a “mixed” type, one which includes a characteristic combination of arcto-boreal, boreal, steppe and polyzonal species showing no analogues among recent insect complexes. These peculiar faunas seem to have represented a particular zonal type, which disappeared since the end of the Last Glaciation to arrive here with the extinction of the mammoth biota. In contrast, on the sites lying north of 60°N, the beetle communities were similar to modern sub-arctic and arctic faunas, yet with the participation of some sub-boreal steppe components, such as Poecilus ravus Lutshnik and Carabus sibiricus Fischer-Waldheim. This information, when compared with our knowledge of synchronous insect faunas from other regions of northern Eurasia, suggests that the former distribution of beetles in this region could be accounted for both by palaeo-environmental conditions and the impact of grazing by large ruminant mammals across the so-called “mammoth savannas”. PMID:21738409

  16. Granitoid magmatism of Alarmaut granite-metamorphic dome, West Chukotka, NE Russia

    NASA Astrophysics Data System (ADS)

    Luchitskaya, M. V.; Sokolov, S. D.; Bondarenko, G. E.; Katkov, S. M.

    2009-04-01

    financial support of RFBR (projects № 07-05-00255, 08-05-00547), leading scientific school NSh-3172.2008.5, Programs of basic researches ONZ RAS 6. References 1. Parfenov L.M. Continental margins and island arcs of Mesozoides of North-East Asia. Novosibirsk, 1984. 192 p. (in Russian) 2. Zonenshain L.P., Kuz'min M.I., Natapov L.M. Tectonics of lithospheric plates of USSR territory // М.: Nauka, 1990. V. 2. 327 p. (in Russian) 3. Sokolov S.D. Classification and hierarchy of fold constructions. М. GEOS. 2008. P.71-100. (in Russian) 4. Seslavinsky K.B. South-Anyui suture zone (West Chukotka) // Dokl. AN USSR. 1979. V. 249. P. 1181-1185 (in Russian) 5. Natal'in B.A. Early Mesozoic eugeosynclinal systems in the northern part of Circum-Pacifica. М.: Nauka. 1984. 136 p. (in Russian) 6. Sokolov S.D., Bondarenko G.Ye., Morozov O.L.,. Shekhovtsov V.A., Glotov S.P.,. Ganelin A.V., Kravchenko-Berezhnoy I.R. The South Anyui Suture, NE Arctic Russia: facts and problems to solve. Tectonic Evolution of the Bering Shelf-Chukchi Sea-Arctic Margin and Adjacent Landmasses. Geol. Soc. Amer. Spec. Paper, 2002, 360. P. 209-224 7. Sokolov S.D., Bondarenko G.E., Morozov O.L., Luchitskaya M.V. Tectonics of junction zone between Verkhoyan-Chukotka and Koryak-Kamchatka fold // Byul. MOIP. Otd. Geol. 2001. V. 76. Is.6. P.24-37. (in Russian) 8. Bondarenko G.E. Tectonics and geodynamic evolution of Mesozoides of north framework of Pacific Ocean. М.: MGU, 2004. 46 p. (in Russian) 9. Til'man S.M. Comparative tectonics of Mesozoides of northern part of Pacific rim. Novosibirsk: Nauka. 1973. 325 p. (in Russian) 10. Grantz A., Moore T. E., Roeske S.M. Gulf of Alaska to Arctic Ocean: Geological Society of America Continental-Ocean Transect A-3, scale 1:500,000. Menlo Park, California, 1991, 72 р. 11. Sadovsky A.I. Geologic map of USSR, scale 1:200000. Anyui-Chauna series. Paper R-58-XXVII, XXVIII. (Ed: Gel'man M.L.) Explanatory report. Leningrad: VSEGEI, 1970, 84 p. (in Russian) 12. Gel'man M

  17. Detecting Anthropogenic and Climate Change Induced Land Cover and Land Use Change in the Vicinity of an Oil/gas Facility in Northwestern Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Yu, Q.; Shiklomanov, N. I.; Streletskiy, D. A.; Engstrom, R.; Epstein, H. E.

    2015-12-01

    Arctic ecosystems are changing dramatically due to changes in climate, vegetation and human activities. Northwestern Siberia is one of the regions which has been undergoing various land cover and land use changes associated primarily with animal husbandry and oil/gas development. These changes have been exacerbated by warming climatic conditions over the last fifty years. In this study, we investigated land cover and land use changes associated with oil and gas development southeast of the city of Nadym within the context of climate change based on multi-source and multi-temporal remote sensing imagery. The impacts of land use on surface vegetation, radiation, and hydrological properties were evaluated using the Normalized Difference Vegetation Index (NDVI), albedo and the Normalized Difference Water Index (NDWI). The results from a comparison between high spatial resolution imagery acquired in1968 and 2006 indicate that the vegetation cover was reduced in areas disturbed by oil and gas development. Vegetation cover increased in natural landscapes over the same period,. Water logging was found along the linear structures near the oil/gas development, while in natural landscapes the drying of thermokarst lakes is evident due to permafrost degradation. Derived indices suggest that the direct impacts associated with infrastructure development are mostly within 100 m distance from the disturbance source. While these impacts are rather localized they persist for decades despite partial recovery of vegetation after the initial disturbance.

  18. Enriched Nd-Sr-Pb isotopic signatures in the Dovyren layered intrusion ( eastern Siberia, Russia): Evidence for source contamination by ancient upper-crustal material

    USGS Publications Warehouse

    Amelin, Yu. V.; Neymark, L.A.; Ritsk, E. Yu; Nemchin, A.A.

    1996-01-01

    Major- and trace-element concentrations and Nd-, Sr- and Pb-isotopic ratios are reported for the Dovyren layered mafic-ultramafic intrusion in the northern Baikal region, eastern Siberia. Sm-Nd internal isochrons for an olivine gabbro from the layered series and a gabbronorite from a sill at the bottom of the Dovyren intrusion yield ages of 673 ?? 22 and 707 ?? 40 Ma, respectively. Initial isotopic ratios: 87Sr/86Sr (673) from 0.7101 to 0.7135, ??Nd(673 Ma) from - 16.3 to - 14.1, 206Pb/204Pb from 16.80 to 17.14, 207Pb/204Pb from 15.477 to 15.501 and 208Pb/204Pb from 37.17 to 37.59, are similar to those of late Archean-early Proterozoic upper continental crust, but do not appear to be a result of wallrock assimilation in the magma chamber. These isotopic features, as well as high K, Rb and LREE and low Ti concentrations in the calculated composition of the Dovyren parental magma, may be explained by subduction of sediments derived from upper continental crust into depleted mantle and subsequent melting of the metasomatized peridotite.

  19. Hypolactasia in the indigenous populations of northern Russia.

    PubMed

    Kozlov, A I

    1998-01-01

    The distribution of hypolactasia (PH) in the indigenous populations of the polar and related territories of the Russian Federation was investigated by an oral lactose tolerance. The frequency of hypolactasia in Kildin Saami population is 48%, Komi-Izhem-63%, Northern Mansi-71%, Northern Khanty-72%, West Siberia Nenets-78%. Generally hypolactasia frequencies in indigenous groups of Arctic and Sub-Arctic territories of Russia are higher than in the "reference" samples of Slav (Russian, 40-49%) and Permian Finn (Komi-Permiak and Udmurtian, 50-59%) groups.

  20. Detecting crop yield reduction due to irrigation-induced soil salinization in South-West Russia

    NASA Astrophysics Data System (ADS)

    Argaman, E.; Beets, W.; Croes, J.; Keesstra, S.; Verzandvoort, S.; Zeiliguer, A.

    2012-04-01

    The South-European part of the Russian Federation has experienced serious land degradation in the form of soil salinization since the 1960s. This land degradation was caused by intensive, large-scale irrigation on reclaimed land in combination with the salt-rich nature of the substrate. Alkaline soil salinity is believed to be an important factor decreasing crop yield in this area. A large research effort has been directed to the effects of soil salinity on crops, there is a need for simple, easily determinable indicators of crop health and soil salinity in irrigated systems, that can help to detect crop water stress in an early stage. The objectives of this research were to study the effects of soil salinity and vegetation water stress on the performance of alfalfa crop yield and physiological crop properties, and to study the possibility to measure soil salinity and alkalinity and the crop water stress index at plot level using a thermal gun and a regular digital camera. The study area was located in Saratov District, in the South-West part of Russia. Variables on the surface energy balance, crop properties, soil properties and visible reflectance were measured on plots with alfalfa cultures in two fields with and without signs of alkaline soil salinity, and with and without irrigation in July 2009. The research showed no clear adverse effects of soil salinity and soil alkalinity on crop yield and physiological crop properties. Soil salinity, as reflected by the electric conductivity, positively affected the root biomass of alfalfa in the range of 0.15 to 1.52 dS/m . This was a result of EC levels being below the documented threshold to negatively affect Alfalfa, as would be the case in truly saline soils. The soil pH also showed a positive correlation with root biomass within the range of pH 6.2 and 8.5 . From the literature these pH values are generally believed to be too high to exhibit a positive relationship with root biomass. No relationship was found

  1. Was the Devonian geomagnetic field dipolar or multipolar? Palaeointensity studies of Devonian igneous rocks from the Minusa Basin (Siberia) and the Kola Peninsula dykes, Russia

    NASA Astrophysics Data System (ADS)

    Shcherbakova, V. V.; Biggin, A. J.; Veselovskiy, R. V.; Shatsillo, A. V.; Hawkins, L.; Shcherbakov, V. P.; Zhidkov, G. V.

    2017-02-01

    Defining variations in the behaviour of the geomagnetic field through geological time is critical to understanding the dynamics of Earth's core and its response to mantle convection and planetary evolution. Furthermore, the question of whether the axial dipole dominance of the recent palaeomagnetic field persists through the whole of Earth's history is fundamental to determining the reliability of palaeogeographic reconstructions and the efficacy of the magnetosphere in shielding Earth from solar wind radiation. Previous palaeomagnetic directional studies have suggested that the palaeofield had a complex configuration in the Devonian period (419-359 Ma). Here we present new palaeointensity determinations from rocks aged between 408 and 375 Ma from the Minusa Basin (southern Siberia), and the Kola Peninsula to investigate the strength of the field during this enigmatic period. Palaeointensity experiments were performed using the thermal Thellier, microwave Thellier, and Wilson methods on 165 specimens from 25 sites. Six out of eight successful sites from the Minusa Basin and all four successful sites from the Kola Peninsula produced extremely low palaeointensities (< 10 μT). These findings challenge the uniformitarian view of the palaeomagnetic field: field intensities of nearly an order of magnitude lower than Neogene values (except during relatively rare geomagnetic excursions and reversals) together with the widespread appearance of strange directions found in the Devonian suggest that the Earth's field during this time may have had a dominantly multipolar geometry. A persistent, low intensity multipolar magnetic field and associated diminished magnetosphere would increase the impact of solar particles on the Earth's magnetosphere, ionosphere and atmosphere with potential major implications for Earth's climate and biosphere.

  2. Species of coccidia (Apicomplexa: Eimeriidae) in shrews from Alaska, U.S.A., and northeastern Siberia, Russia, with description of two new species.

    PubMed

    Lynch, A J; Duszynski, D W

    2008-08-01

    Fecal samples (n = 636) from 10 species of shrews collected in Alaska (n = 540) and northeastern Siberia (n = 96) were examined for the presence of coccidia (Apicomplexa: Eimeriidae). Five distinct oocyst morphotypes were observed. Three types were consistent with oocysts of previously recognized coccidia species from other shrew hosts. These were Eimeria inyoni, E. vagrantis, and Isospora brevicauda, originally described from the inyo shrew (Sorex tenellus), dusky shrew (S. monticolus), and northern short-tailed shrew (Blarina brevicauda), respectively. We found 5 new host records for E. inyoni, 3 for E. vagrantis, and 3 for I. brevicauda. The 2 additional oocyst morphotypes, both from the tundra shrew (Sorex tundrensis), are putative new species. Sporulated oocysts of Eimeria beringiacea n. sp. are subspheroidal, 17.7 x 15.6 microm (14-24 x 13-20 microm) with a length (L)/width (W) ratio of 1.1 (1.0-1.4); these lack a micropyle (M), an oocyst residuum (OR), and a polar granule (PG). Sporocysts are ellipsoidal, 10.3 x 6.1 microm (7-14 x 4-8 microm), with a L/W ratio of 1.7 (1.3-2.3) and have a Stieda body (SB), Substieda body (SSB), and sporocyst residuum (SR). Oocysts of Eimeria tundraensis n. sp. are spheroidal to subspheroidal, 24.8 x 23.5 microm (23-26 x 22-25 microm), with a L/W ratio of 1.1 (1.0-1.2); these lack a M and OR, but a single PG is present. Sporocysts are elongate ellipsoidal, 15.4 x 8.3 microm (13-17 x 7-9 microm), with a L/W ratio of 1.9 (1.4-2.1) and have a SB, SSB, and SR.

  3. HIV-1 genetic diversity in Russia: CRF63_02A1, a new HIV type 1 genetic variant spreading in Siberia.

    PubMed

    Baryshev, Pavel B; Bogachev, Vladislav V; Gashnikova, Natalya M

    2014-06-01

    One of the factors determining a high degree of heterogeneity in the HIV population is recombination-based variation, which leads to the emergence of the virus variants with a mosaic genome. An example is CRF63_02A1, an HIV-1 variant currently spreading in the Siberian region of Russia. To prove that this HIV-1 variant is a new circulating recombinant form that had emerged as a result of repeated recombination between CRF02_AG and subtype A, we have isolated seven full-length HIV genomes and theoretically analyzed them, that is, reconstructed the phylogenetic relationships, determined recombination breakpoints and regions, and compared them with the regions known for CRF02_AG.

  4. Assessment of undiscovered continuous oil and shale-gas resources in the Bazhenov Formation of the West Siberian Basin Province, Russia, 2016

    USGS Publications Warehouse

    Klett, Timothy R.; Schenk, Christopher J.; Brownfield, Michael E.; Leathers-Miller, Heidi M.; Mercier, Tracey J.; Pitman, Janet K.; Tennyson, Marilyn E.

    2016-11-10

    Using a geology-based assessment methodology, the U.S. Geological Survey estimated mean continuous resources of 12 billion barrels of oil and 75 trillion cubic feet of gas in the Bazhenov Formation of the West Siberian Basin Province, Russia.

  5. The East Atlantic - West Russia Teleconnection in the North Atlantic: Climate Impact and Relation to Rossby Wave Propagation

    NASA Technical Reports Server (NTRS)

    Lim, Young-Kwon

    2014-01-01

    Large-scale winter teleconnection of the East Atlantic - West Russia (EA-WR) over the Atlantic and surrounding regions is examined in order to quantify its impacts on temperature and precipitation and identify the physical mechanisms responsible for its existence. A rotated empirical orthogonal function (REOF) analysis of the upper-tropospheric monthly height field captures successfully the EA-WR pattern and its interannual variation, with the North Atlantic Oscillation as the first mode. EA-WRs climate impact extends from eastern North America to Eurasia. The positive (negative) EA-WR produces positive (negative) temperature anomalies over the eastern US, western Europe and Russia east of Caspian Sea, with negative (positive) anomalies over eastern Canada, eastern Europe including Ural Mountains and the Middle East. These anomalies are largely explained by lower-tropospheric temperature advections. Positive (negative) precipitation anomalies are found over the mid-latitude Atlantic and central Russia around 60E, where lower-level cyclonic (anticyclonic) circulation anomaly is dominant. The eastern Canada and the western Europe are characterized by negative (positive) precipitation anomalies.The EA-WR is found to be closely associated with Rossby wave propagation. Wave activity fluxes show that it is strongly tied to large-scale stationary waves. Furthermore, a stationary wave model (SWM) forced with vorticity transients in the mid-latitude Atlantic (approximately 40N) or diabatic heat source over the subtropical Atlantic near the Caribbean Sea produces well-organized EA-WR-like wave patterns, respectively. Sensitivity tests with the SWM indicate improvement in the simulation of the EA-WR when the mean state is modified to have a positive NAO component that enhances upper-level westerlies between 40-60N.

  6. Vertical distribution of trace gas species in the troposphere over the south of West Siberia: comparison of airborne in situ measurements and satellite data

    NASA Astrophysics Data System (ADS)

    Belan, Boris D.; Arshinov, Mikhail Yu.; Belov, Vladimir V.; Gridnev, Yurii V.; Davydov, Denis K.; Machida, Toshinobu; Paris, Jean-Daniel; Nédélec, Philippe; Fofonov, Alexander V.

    2014-05-01

    A comparison of the vertical distributions of O3, CO, CO2 and CH4 derived from the airborne in situ measurements and satellite observations over the southern part of West Siberia is presented. In this study we used data of monthly research flights of 'Optik' TU-134 aircraft laboratory carried out from 2012 to 2013 and data retrieved from measurements of the Infrared Atmospheric Sounding Interferometer (IASI) instrument on-board the MetOp satellite. It was found that differences in ozone mixing ratios between the airborne and satellite data can vary from +3 to +18 ppb at 0.5 km AGL and form -8 to -37 ppb at 7 km AGL, and relative ones ranged from +8 to +30 % and from -12 to -88 %, respectively. Differences in CO concentrations varied from +32 to +103 ppb at 0.5 km height and from -18 to +23 ppb at 3 km. Relative differences were in the range from -4 to +48 % at 0.5 km and from -8 to +20 % at 7 km. The maximal difference in all CH4 profiles reached 150 ppb in the atmospheric boundary layer, and the minimal one was -10 ppb. The average relative difference varied between +2.8 and -0.5 %. The average difference in CO2 concentration lies within ±1.5 ppm, while individual profiles are incommensurable. Maximal and minimal differences during the all flights were observed in the atmospheric boundary layer (+10 and -12 ppm or +2.3 and -3.3%, respectively). In the free troposphere, relative difference decreased down to ±1.0%. This work was funded by Research funds for Global Environmental Monitoring in NIES (Japan), CNRS (France), the French Ministry of Foreign Affairs, CEA (France), Presidium of RAS (Program No. 4), Brunch of Geology, Geophysics and Mining Sciences of RAS (Program No. 5), Interdisciplinary integration projects of Siberian Branch of RAS (No. 35, No. 70, No. 131), Russian Foundation for Basic Research (grants No 14-05-00526, 14-05-00590).

  7. Multilingual Education in South Siberia: National Schools in the Republics of Altai and Tyva

    ERIC Educational Resources Information Center

    Chevalier, Joan F.

    2012-01-01

    Subtractive bilingualism is widespread throughout Siberia, with indigenous youth often more proficient in Russian than in their non-Russian local languages. Siberia's national schools, which are secondary schools offering instruction in local languages of Russia, provide critical institutional support for minority languages. The goal of this…

  8. Sugmut field: A forced regression deposit within the Neocomian prograding clinoform complex, West Siberian Basin, Russia

    SciTech Connect

    Armentrout, J.M. ); Oleg, M.; Igirgi, M.

    1996-01-01

    The Volgian-Neocomian interval of the Middle Ob Region of the intracratonic West Siberian Basin consists of between 35 and 45 regional transgressive/regressive cycles infilling a basin which had an average water depth of approximately 200 meters. Within local clinoforms, wells have encountered elongate shelf-edge sandstone bodies ranging from 15 to 100 kilometers in strike-oriented length. In most areas the seismic interval correlative to the reservoir sandstone pinches-out against the foreset of the preceding clinoform. This geometric relationship, and the sharp-based log pattern of sandstones along the more landward margin of the sandstone body, suggests that the sandstone may have been deposited as a consequence of marked downward shift in baselevel as part of a lowstand prograding complex, or possibly as a late highstand forced regression deposit. The Sugmut field, located in the northeast part of the study area, is 12 km wide east-west and 75 km long north-south, and grades laterally into shale to the west, south and east. Relative to the regressive phase isopach, the transgressive phase isopach thick shifts slightly northward and eastward indicating the direction of littoral drift and marginward transgression. In the northern part of the field the shelf-edge sandstone interval may correlate with a thin depositional-dip oriented shelf sandstone mapped within the transgressive interval. This mapped pattern may be interpreted as lowstand incision of a fluvial system supplying sand to a shelf-edge delta followed by infilling of the fluvial valley during transgression. Subsequent down-to-the-north regional tilt resulted in structural closure forming the Sugmut field trap.

  9. Sugmut field: A forced regression deposit within the Neocomian prograding clinoform complex, West Siberian Basin, Russia

    SciTech Connect

    Armentrout, J.M.; Oleg, M.; Igirgi, M.

    1996-12-31

    The Volgian-Neocomian interval of the Middle Ob Region of the intracratonic West Siberian Basin consists of between 35 and 45 regional transgressive/regressive cycles infilling a basin which had an average water depth of approximately 200 meters. Within local clinoforms, wells have encountered elongate shelf-edge sandstone bodies ranging from 15 to 100 kilometers in strike-oriented length. In most areas the seismic interval correlative to the reservoir sandstone pinches-out against the foreset of the preceding clinoform. This geometric relationship, and the sharp-based log pattern of sandstones along the more landward margin of the sandstone body, suggests that the sandstone may have been deposited as a consequence of marked downward shift in baselevel as part of a lowstand prograding complex, or possibly as a late highstand forced regression deposit. The Sugmut field, located in the northeast part of the study area, is 12 km wide east-west and 75 km long north-south, and grades laterally into shale to the west, south and east. Relative to the regressive phase isopach, the transgressive phase isopach thick shifts slightly northward and eastward indicating the direction of littoral drift and marginward transgression. In the northern part of the field the shelf-edge sandstone interval may correlate with a thin depositional-dip oriented shelf sandstone mapped within the transgressive interval. This mapped pattern may be interpreted as lowstand incision of a fluvial system supplying sand to a shelf-edge delta followed by infilling of the fluvial valley during transgression. Subsequent down-to-the-north regional tilt resulted in structural closure forming the Sugmut field trap.

  10. Epidemiology of West Nile infection in Volgograd, Russia, in relation to climate change and mosquito (Diptera: Culicidae) bionomics.

    PubMed

    Platonov, Alexander E; Fedorova, Marina V; Karan, Ludmila S; Shopenskaya, Tatyana A; Platonova, Olga V; Zhuravlev, Vitaly I

    2008-12-01

    In 1999, there was the large outbreak of West Nile fever (WNF) in Southern Russia (>500 cases in the Volgograd Province). In 2000-2004, the WNF incidence rate decreased steadily to zero, but a new outbreak occurred in 2007 (64 cases). The analysis of historical climate data for Volgograd from 1900 to present showed that the years 1999 and 2007 were the hottest ones due to a very mild "winter" (Dec.-Mar.) and a hot "summer" (June-Sep.). There are up to 15 potential WNF vectors in Volgograd, but only Culex pipiens and Culex modestus are abundant in late summer, both in urban and rural settings. Only these species are naturally attracted to and feed on both humans and birds. The RNA of pathogenic WN virus genovariant was found by reverse transcriptase polymerase chain reaction only in Culex mosquitoes at the infection rate of about 0.04%. So these species may be considered as potential WNF "bridge vectors" between birds and humans as well as main vectors in sylvatic avain cycle. Their abundance in an epidemic season was higher in the years with a mild winter and a hot summer, so this phenomenon may serve as a connecting link between a climate and WNF epidemiology. These findings give some hints on the predisposing factors for WNF epidemic as well as the possibility to predict WNF outbreaks in the temperate climate zones.

  11. Life cycle of the taiga tick Ixodes persulcatus (Acari: Ixodidae) in the North-West of Russia.

    PubMed

    Grigoryeva, L A; Stanyukovich, M K

    2016-07-01

    The life cycle of Ixodes persulcatus lasts 3 years in the conditions of the Leningrad province (North-West Russia), the development of each phase taking a year. The normal age of the taiga tick is 3 years. The calendar age of larvae and nymphs reaches 11-12 months under favorable abiotic and biotic factors, while the calendar age of adults does not exceed 11 months. At the preimaginal phases of development the ticks that breed in August can feed before or after winter. However, their metamorphosis begins and reaches completion within the same timeframes (from late June to early August) and lasts for about 30-50 (60) days. The survival rate of hungry and engorged larvae and nymphs after wintering is quite high (88.6-100 %). We explain the low activity of larvae and nymphs in late summer and autumn by incomplete development. Morphogenetic diapause of engorged larvae and nymphs interrupts digestion but not metamorphosis which starts only in late June and July after the complete absorption of blood from the gut cavity.

  12. Soil-geographical and ecological tour in West-Russia: 20 years anniversary

    NASA Astrophysics Data System (ADS)

    Kuzyakov, Yakov

    2013-04-01

    Soil-geographical and agro-ecological tour in Russia celebrated in this summer its 20 years anniversary! More than 800 students, PhD students and researcher from Germany, Switzerland, Austria, Sweden and France participated at the tour since 1993. The majority of the participants were students studying soil science, geoecology, geography, agriculture and ecology. The tour is based on a classical Russian zonal approach: a cross-section of climatic zones starting from south taiga, through deciduous forest, forest steppe, steppe, dry steppe, to semi dessert and transition to the desert zone. In each zone the specifics of climate, vegetation, nutrient cycling, and of course soil genesis as well as soil use by forestry and agriculture are described. Half of the soil group units of WRB classification (2006) are presented on about 35 soil profile pits and are described with focus on pedogenic processes and soil forming factors. The following soil groups are described in details by horizons according to WRB soil classification (2006): Arenosols, Podzols, Albeluvisols Histosols, Gleysols, Luvisols, Phaeozems, Chernozems, Kastanozems, Calcisols, Vertisols, Leptosols, Fluvisols, Solonetzes, Solonchaks. In addition to natural conditions, large-scale experiments designing agricultural landscapes (stone steppe), biosphere reserves and conservation areas (Tula-Schneisen, Divnogor'je, Baskunchak), as well as collective agricultural farms (previously kolkhoz) are visited to evaluate the anthropogenic effects on ecosystems and especially on soils. The 2.5 weeks bus journey through many villages and small towns, visits of museums and historical monuments, introduction in the settlement development of different regions provide a broad presentation of Russian history, traditions, life style, and contemporary state. So, combination of very diverse educational part focused on soil and environmental conditions with anthropogenic impacts and local history as well as recent socioeconomic

  13. Preparation for the Recovery of Spent Nuclear Fuel (SNF) at Andreeva Bay, North West Russia - 13309

    SciTech Connect

    Field, D.; McAtamney, N.

    2013-07-01

    Andreeva Bay is located near Murmansk in the Russian Federation close to the Norwegian border. The ex-naval site was used to de-fuel nuclear-powered submarines and icebreakers during the Cold War. Approximately 22,000 fuel assemblies remain in three Dry Storage Units (DSUs) which means that Andreeva Bay has one of the largest stockpiles of highly enriched spent nuclear fuel (SNF) in the world. The high contamination and deteriorating condition of the SNF canisters has made improvements to the management of the SNF a high priority for the international community for safety, security and environmental reasons. International Donors have, since 2002, provided support to projects at Andreeva concerned with improving the management of the SNF. This long-term programme of work has been coordinated between the International Donors and responsible bodies within the Russian Federation. Options for the safe and secure management of SNF at Andreeva Bay were considered in 2004 and developed by a number of Russian Institutes with international participation. This consisted of site investigations, surveys and studies to understand the technical challenges. A principal agreement was reached that the SNF would be removed from the site altogether and transported to Russia's reprocessing facility at Mayak in the Urals. The analytical studies provided the information necessary to develop the construction plan for the site. Following design and regulatory processes, stakeholders endorsed the technical solution in April 2007. This detailed the processes, facilities and equipment required to safely remove the SNF and identified other site services and support facilities required on the site. Implementation of this strategy is now well underway with the facilities in various states of construction. Physical works have been performed to address the most urgent tasks including weather protection over one of the DSUs, installation of shielding over the cells, provision of radiation

  14. Myrmecophilous pygmephoroid mites (Acari: Pygmephoroidea) associated with Lasius flavus (Hymenoptera: Formicidae) in Russia.

    PubMed

    Khaustov, Alexander A

    2015-11-19

    Twenty four species of pygmephoroid mites (Acari: Pygmephoroidea: Neopygmephoridae, Scutacaridae, Microdispidae) are recorded from the ant Lasius flavus (Fabricius) or from its nests from Western Siberia and Crimea. Four of them of the genus Scutacarus Gros, 1845 (Acari: Scutacaridae), S. insolitus sp. nov., S. heterotrichus sp. nov., S. moseri sp. nov. and S. sibiriensis sp. nov. are described as new for science. Four species of scutacarid mites are recorded for the first time in Russia. The comparison of pygmephoroid mite communities associated with Lasius flavus from Crimean and West Siberian populations and notes on phoresy of pygmephoroid mites on ants are provided.

  15. [The role of mutation of gene cyp1A1 and benzapilene in cytogenetic changes of urinary tract epitheliocytes in oil industry workers employed in the oil fields of the North of West Siberia].

    PubMed

    Il'inskikh, N N; Il'inskikh, E N; Il'inskikh, I N; Iamkovaia, E V

    2011-01-01

    The examination of 477 oil industry workers and office personnel (control) employed in the oil fields of the North of Tomsk and Tyumen regions has detected increased number of epithelyocytes with micronuclei and an elevated urine level ofbenzapilene in workers employed in oil production. Especially pronounced changes of the above parameters were observed in men with mutant alleles Val of CYP1A1 gene. An enhanced mutation process in oil production workers may be due to a resultant action of different factors on human genome. Involved may be both mutagens and factors of comutagenic nature. The results obtained in this study suggest a conclusion about urgent need of introduction of new scientifically validated criteria of selection of personnel for oil production in the North of the West Siberia. Health examination of the applicants must include genotyping.

  16. High resilience in the Yamal-Nenets social-ecological system, West Siberian Arctic, Russia.

    PubMed

    Forbes, Bruce C; Stammler, Florian; Kumpula, Timo; Meschtyb, Nina; Pajunen, Anu; Kaarlejärvi, Elina

    2009-12-29

    Tundra ecosystems are vulnerable to hydrocarbon development, in part because small-scale, low-intensity disturbances can affect vegetation, permafrost soils, and wildlife out of proportion to their spatial extent. Scaling up to include human residents, tightly integrated arctic social-ecological systems (SESs) are believed similarly susceptible to industrial impacts and climate change. In contrast to northern Alaska and Canada, most terrestrial and aquatic components of West Siberian oil and gas fields are seasonally exploited by migratory herders, hunters, fishers, and domesticated reindeer (Rangifer tarandus L.). Despite anthropogenic fragmentation and transformation of a large proportion of the environment, recent socioeconomic upheaval, and pronounced climate warming, we find the Yamal-Nenets SES highly resilient according to a few key measures. We detail the remarkable extent to which the system has successfully reorganized in response to recent shocks and evaluate the limits of the system's capacity to respond. Our analytical approach combines quantitative methods with participant observation to understand the overall effects of rapid land use and climate change at the level of the entire Yamal system, detect thresholds crossed using surrogates, and identify potential traps. Institutional constraints and drivers were as important as the documented ecological changes. Particularly crucial to success is the unfettered movement of people and animals in space and time, which allows them to alternately avoid or exploit a wide range of natural and anthropogenic habitats. However, expansion of infrastructure, concomitant terrestrial and freshwater ecosystem degradation, climate change, and a massive influx of workers underway present a looming threat to future resilience.

  17. Evolution of Mesozoic fluvial systems along the SE flank of the West Siberian Basin, Russia

    NASA Astrophysics Data System (ADS)

    Le Heron, Daniel Paul; Buslov, Micha M.; Davies, Clare; Richards, Keith; Safonova, Inna

    2008-07-01

    The Mesozoic stratigraphy in the subsurface of the West Siberian Basin contains prolific hydrocarbon accumulations, and thus the depositional environments of marine and marginal marine Jurassic and Cretaceous age sediments are well-established. However, no information is currently available on strata of equivalent age that crop out along the SE basin margin in the Mariinsk-Krasnoyarsk region, despite the potential of these exposures to supply important information on the sediment supply routes into the main basin. Detailed sedimentological analysis of Jurassic-Cretaceous clastic sediments, in conjunction with palaeo-botanical data, reveals five facies associations that reflect deposition in a range of continental environments. These include sediments that were deposited in braided river systems, which were best developed in the Early Jurassic. These early river systems infilled the relics of a topography that was possibly inherited from earlier Triassic rifting. More mature fluvial land systems evolved in the Mid to Late Jurassic. By the Mid Jurassic, well-defined overbank areas had become established, channel abandonment was commonplace, and mudrocks were deposited on floodplains. Coal deposition occurred in mires, which were subject to periodic incursions by crevasse splay processes. Cretaceous sedimentation saw a renewed influx of sand-grade sediment into the region. It is proposed that landscape evolution throughout the Jurassic was driven simply by peneplanation rather than tectonic processes. By contrast, the influx of sandstones in the Cretaceous is tentatively linked to hinterland rejuvenation/ tectonic uplift, possibly coeval with the growth of large deltaic clinoform complexes of the Neocomian in the basin subsurface.

  18. Return to Siberia: The 2008 Kotuykan River Expedition

    NASA Technical Reports Server (NTRS)

    Ranson, Jon; Kharuk, Slava; Howl, Joanne

    2009-01-01

    In the September-October 2007 issue of'The Earth Observer [volume 19, Number 4, pp. 13-21] we presented an article entitled "Expedition to Siberia: A Firsthand Account." In that article we shared excerpts from a blog that chronicled the adventures of a team of scientists from NASA and Russia's Academy of Science as they embarked on a three-week adventure in the wilds of Siberia in hopes of collecting measurements to validate data from satellites flying 700 km overhead. The same team, plus a couple new participants, headed back to Siberia this past sumner and we are now pleased to present the continuation of their story. For more background details on the expedition to Siberia or if you missed the first part of the story, please refer to the previous article.

  19. Expedition to Siberia: A Firsthand Account

    NASA Technical Reports Server (NTRS)

    Ranson, Jon; Kharuk, Slava; Howl, Joanne

    2007-01-01

    Nowhere on Earth is warming faster than the Arctic. In northern Siberia, average temperatures have risen 3-5 deg F over the past 30 years, whereas the worldwide average increase in that time is 1 deg F. Betweeen July 28 and August 12, 2007, a small international team of remote sensing and forest ecosystem scientists from NASA and Russia's Academy of Science set off on a three-week scientific expedition through the heart of the remote, wild forests of Siberia. They traveled southward down the Kochechum River observing the gradual transition from tundra to taiga, taking inventory of plant species along the way, and making ground-truth measurements to validate data being collected by several NASA satellites flying 700 kilometers overhead.

  20. Biological characteristics of influenza A(H1N1)pdm09 virus circulating in West Siberia during pandemic and post-pandemic periods.

    PubMed

    Prokop'eva, E A; Kurskaya, O G; Saifutdinova, S G; Glushchenko, A V; Shestopalova, L V; Shestopalov, A M; Shkurupii, V A

    2014-03-01

    We studied biological characteristics of influenza A(H1N1)pdm09 virus circulating in Siberia during the 2009 pandemic and the post-pandemic period of 2011. BALB/c mice were chosen as the experimental model. Virus titers in the lungs were evaluated on days 1, 3, 6 and blood serum titers on day 15 after infection with different strains. Blood sera of convalescents after influenza of 2010-2011 epidemic season were analyzed. Influenza A(H1N1)pdm09 virus strains isolated during the post-pandemic period of 2011 were characterized by low epidemic activity and virulence in comparison with the strains isolated during 2009 pandemic period, which indicates completion of the pandemic cycle.

  1. [Molecular variability in the commom shrew Sorex araneus L. from European Russia and Siberia inferred from the length polymorphism of DNA regions flanked by short interspersed elements (Inter-SINE PCR) and the relationships between the Moscow and Seliger chromosome races].

    PubMed

    Bannikova, A A; Bulatova, N Sh; Kramerov, D A

    2006-06-01

    Genetic exchange among chromosomal races of the common shrew Sorex araneus and the problem of reproductive barriers have been extensively studied by means of such molecular markers as mtDNA, microsatellites, and allozymes. In the present study, the interpopulation and interracial polymorphism in the common shrew was derived, using fingerprints generated by amplified DNA regions flanked by short interspersed repeats (SINEs)-interSINE PCR (IS-PCR). We used primers, complementary to consensus sequences of two short retroposons: mammalian element MIR and the SOR element from the genome of Sorex araneus. Genetic differentiation among eleven populations of the common shrew from eight chromosome races was estimated. The NP and MJ analyses, as well as multidimensional scaling showed that all samples examined grouped into two main clusters, corresponding to European Russia and Siberia. The bootstrap support of the European Russia cluster in the NJ and MP analyses was respectively 76 and 61%. The bootstrap index for the Siberian cluster was 100% in both analyses; the Tomsk race, included into this cluster, was separated with the bootstrap support of NJ/MP 92/95%.

  2. Land-use Changes on Peatlands in Russia and Green House Gas Emissions

    NASA Astrophysics Data System (ADS)

    Sirin, A.; Minaeva, T.; Chistotin, M.; Glagolev, M.; Suvorov, G.

    2009-04-01

    Russia possesses vast areas of peatlands and associated paludified shallow peat lands, over 8 and 20% respectively. The country is the largest World peatland nation, and thus could be responsible for the large part of GHG exchange between peatlands and the atmosphere. Russian peatlands present a high variety of natural conditions from permafrost mires to bogs, fens and swamps within boreal, temperate, steppe and semi-arid zones, which have quite different rates of GHG flux, emitting or absorbing carbon dioxide and methane. Many regions of Russia still contain vast areas of virgin mires but in the central European part of Russia, West Siberia and Far East the appreciable part of peatlands was already modified. Peatlands were used in a broad spectrum of human activities connected with direct water level draw-down: peat extraction for different purposes (up to 1.5 million ha), drainage for agriculture, and drainage for forestry (each over 3 million ha). Many peatlands all the over the country were affected by infrastructure development (by road, pipe line construction etc.) with related changes of their hydrology and GHG fluxes. These land uses are under consideration of LULUFC issues of UNFCCC, and peat excavation is directly included in IPCC 2006 Guidelines as a main wetland/peatland land use activity related to climate change mitigation. General estimates and geographical distribution of peatlands drained for agriculture and forestry as well as peatlands under excavation, extracted or abandoned are given based on existing statistical and sectoral information. GHG fluxes from disturbed peatlands are analyzed using available Russian data and the results of specially organized observations in 2004-2008 in the pilot regions in Central European Russia and West Siberia which included a variety of modified and virgin control sites.

  3. Development of A Network of Seismological Observations In The Territory of Siberia

    NASA Astrophysics Data System (ADS)

    Seleznev, V. S.; Emanov, A. F.; Soloviev, V. M.; Dergachev, A. A.; Filina, A. G.; Emanov, A. A.; Kabannik, A. V.

    The present stage of development of geophysical researches in Russia is characterized by scaling re-equipment of apparatus-methodical basis; first of all of systems of digital recording and processing of significant volumes of geophysical information and data transfer by modern telecommunication media. The Geophysical Survey SB RAS in Siberia territory has carried out re-equipment of a significant part of a network of ana- log seismological stations by modern digital recording equipment. More than 60 dig- ital seismic stations realize continuous observations in seismoactive regions of Baikal rift zone, Altai - Sayan fold area and Yakutia. For study of man-caused seismicity, con- nected to development of the largest oil-and-gas deposits, 9 stations in the territory of the West-Siberian oil-and-gas bearing province have been set up. With use of modern telecommunication media a gathering of continuous seismic information from seismi- cally dangerous regions of Siberia in Regional centers of gathering and data processing in Novosibirsk, Irkutsk and Yakutsk has been organized, that has allowed to increase substantially efficiency in work of services of the periodic and operational reports about happening seismic events of natural and man-caused character in the Siberian region and give a significant increase of a scientific information for solving of problem on an evaluation of seismic danger of the territory of Siberia, medium- and short-term prognosis of earthquakes. With use of a highly sensitive digital seismic equipment work on study of a seismic condition in large industrial and civil centers of the ter- ritory of Siberia are begun recently with the purpose of an evaluation of influence weak, but long seismic actions on various buildings and on the man. The outcomes of seismological and active vibroseismic monitoring with use of high-power vibrators of seismically dangerous sites of the Siberia territory and engineering-seismological researches using of new

  4. Ongoing climatic extreme dynamics in Siberia

    NASA Astrophysics Data System (ADS)

    Gordov, E. P.; Shulgina, T. M.; Okladnikov, I. G.; Titov, A. G.

    2013-12-01

    are spatially inhomogeneous. The largest increase in frequency and intensity of heavy precipitation is observed in the north of East Siberia. Negative trends related to precipitation amount decrease are found in the central West Siberia and in the south of East Siberia. The authors acknowledge partial financial support for this research from the Russian Foundation for Basic Research projects (11-05-01190 and 13-05-12034), SB RAS Integration project 131 and project VIII.80.2.1., the Ministry of Education and Science of the Russian Federation contract 8345 and grant of the President of Russian Federation (decree 181).

  5. International Permafrost Field Courses in Siberia: the Synthesis of Research and Education

    NASA Astrophysics Data System (ADS)

    Ablyazina, D.; Boitsov, A.; Grebenets, V.; Kaverin, D.; Klene, A.; Kurchatova, A.; Pfeiffer, E. M.; Zschocke, A.; Shiklomanov, N.; Streletskiy, D.

    2009-04-01

    During summers of 2007 and 2008 a series of International University Courses on Permafrost (IUCP) were conducted in West Siberia, Russia. Courses were organized as part of the International Permafrost Association (IPA) International Polar Year activities. The North of West Siberia region was selected to represent diverse permafrost, climatic and landscape conditions. The courses were jointly organized by the Moscow State University (MSU) and the Tumen' Oil and Gas University (TOGU) with the help from German and U.S. institutions. The program attracted undergraduate and graduate students with diverse interests and backgrounds from Germany, Russia and the U.S. and involved instructors specializing in different aspects of permafrost research. Courses were designed to address three major topics of permafrost-related research: a) permafrost environments characteristic of the discontinuous and continuous zones; b) field instrumentation and techniques; c) permafrost engineering and problems of development in permafrost regions. Methodologically, courses consisted of systematic permafrost investigations at long-term monitoring sites and survey-type expeditions. Systematic, process-based investigations were conducted at a network of sites which constitute the TEPO established by TOGU in collaboration with the gas company NadymGasProm. The observation complex includes an array of 30-m deep boreholes equipped with automatic data collection systems and representing characteristic permafrost landscapes of West Siberia. Boreholes are complemented by sites for snow cover, vegetation, soil, ground ice, and geomorphologic investigations. As part of student research activities, four new Circumpolar Active Layer Monitoring (CALM) sites were established in proximity to boreholes for monitoring spatial distribution and long-term dynamic of the active layer. New sites represent diverse landscapes characteristic of the West Siberian previously underrepresented in the CALM network

  6. [The influence of weather conditions on the epidemiology of vector-borne diseases by the example of West Nile fever in Russia].

    PubMed

    Platonov, A E

    2006-01-01

    Climate changes must influence the incidence of vector-borne infections, but their effects cannot be revealed due to lack of long-term observations. The impact of short-term weather changes may be used as a model. In Russia the biggest numbers of clinical cases of mosquito-borne West Nile infection were registered in 1999 in Volgograd and Astrakhan regions. The analysis of climatic dataset since 1900 shows that 1999 was the hottest year in Volgograd in the 20th century due to a very mild winter (December-March) and a rather hot summer (June-September). The author of the article puts forward a hypothesis that high winter temperatures favored the survival of over-wintering mosquito vectors, and high summer temperature facilitated the growth of the virus in the mosquitoes, as well as propagation of the mosquitoes themselves. The author assumes that conventional threshold temperatures for "beneficial for WNF conditions" in Russia are > or = 3 degrees C in winter, and > or = 22 degrees C in summer. These conditions coincided only in 1948 and 1999. In Astrakhan the "beneficial for WNF conditions" were registered in 30 out of 147 years of observation, and in 12 years between 1964 and 2003. This is not surprising that Astrakhan region is endemic for WNF in accordance with clinical and epidemiological data collected since the sixties. These findings give some hints on the WNF predisposing factors, as well as possibility of weather surveillance and prediction of WNF outbreaks in temperate climatic zones such as Southern Russia.

  7. Novel Lyssaviruses Isolated from Bats in Russia

    PubMed Central

    Botvinkin, Alexandr D.; Poleschuk, Elena M.; Borisova, Tatyana I.; Gazaryan, Suren V.; Yager, Pamela; Rupprecht, Charles E.

    2003-01-01

    Two new rabies-related viruses were discovered in Russia during 2002. Viruses were isolated from bats in Eastern Siberia near Baikal Lake and in the western Caucasus Mountains. After preliminary antigenic and genetic characterization, we found that both viruses should be considered as new putative lyssavirus genotypes. PMID:14720408

  8. On-Going Temperature Extremes in Siberia

    NASA Astrophysics Data System (ADS)

    Shulgina, T. M.; Gordov, E. P.

    2014-12-01

    Ongoing global climate changes accompanied by the restructuring of global processes in the atmosphere and biosphere are strongly pronounced in the Northern Eurasia regions, especially in Siberia. Temperature trends (grows up to 0.5 °C per decade), more frequent occurrence of temperature extremes provoked serious natural disasters (2010 heat waves in Russia, 2013 flood in Russia's Far East) led to socio-economical impact (crop damages, infrastructure failures, respectively). To get reliable knowledge on location, frequency and magnitude of observed extremes we have studied daily max/min temperature trends based on ECMWF ERA Interim Reanalysis data (0,25°×0,25°). This dataset is most accurately reproduces observed temperature behavior in the region. Statistical analysis of daily temperature time series (1979-2012) indicates the asymmetric changes in distribution tails of such extreme indices as warm/cold days/nights. Namely, the warming during winter cold nights is stronger than during warm nights, especially over the north of Siberia. Increases in minimum temperatures are more significant than in maximum temperatures. Warming determined at the high latitudes of the region is achieved mostly due to winter temperature changes. South area of Siberia has slightly cooling during winter and summer. Results obtained provide regional decision-makers with detailed high spatial and temporal resolution climatic information required for adaptation and mitigation measures development. Calculations presented have been realized using information-computational web-GIS system "Climate" (http://climate.scert.ru/) which automatically generates the archive of calculated fields ready for multidisciplinary studies of regional climate change impacts. The authors acknowledge partial financial support for this research from the RFBR (13-05-12034, 14-05-00502), SB RAS 131 and VIII.80.2.1.) and grant of the President of RF (№ 181).

  9. Glacier Evolution in the Altai Mountains, South-West Siberia, for the Last Half Century (with use of Geo-Informational Catalogue)

    NASA Astrophysics Data System (ADS)

    Surazakov, A. B.; Narojniy, Y. K.; Nikitin, S. A.; Aizen, V. B.

    2003-12-01

    To systemize and analyze the information for the period from 1835 to present on altitudinal distributions of glaciers, exposition, their numbers and surface areas in basins, volumes, genetic classification, location of lower and upper level of glaciers, average firn line position and main morphometric characteristics, DataBase on glacier dynamics in the Altai Mountains (AGDB) has been developed in ArcGIS Format [Tomsk State University, Russia]. Data from Glacier Catalogue [1962], topographic maps with the scale of 1:25000 and 1:50000 and air photos, which fixed glaciers' state on 1952, were digitized. Instrumental observational data on glacier tongue retreat from twenty glaciers since 1835, and radio-echo sounding measurements of 120 glacier volumes were also digitized in the AGDB. Modern state of Altai glaciers and their changes since 1952 were assessed from Resurs space images and partially from instrumental observations. Based on estimation from Resurs for the period from 1952 to 1998, the value of Altai glacier retreating was about 56.9 km2, i.e. 7.1 % of total area, varied from 4 % for valley glaciers to 16 % for glaciers of flat mountain tops. Retreat of 2-8 m per year was accompanied by their 10% mass loss. The slightest degradation occurred in inner (central) part of the glacier system, in the heads of river basins with large-scale glaciation, e.g., in the Katunski, Nothern-Chuiski and Southern-Chuiski ranges, amounting to 6.3%. These are the highest regions, reaching up to 4506 m., and 80% of Altai's glaciers are located there. In the river basins with relatively small-glacierized areas, at the peripheral regions, e.g., Kurai, Chihacheva ranges, the degradation reached its maximum values up to 22%.

  10. Current state of forest mapping with Landsat data in Siberia

    NASA Astrophysics Data System (ADS)

    Maksyutov, Shamil; Sedykh, Vladimir; Kuzmenko, Ekaterina; Farber, Sergey; Kalinicheva, Svetlana; Fedorov, Alexander; Schepaschenko, Dmitry

    2016-04-01

    We review a current state of a forest type mapping with Landsat data in Siberia. Target algorithm should be based on dynamic vegetation approach to be applicable to the analysis of the forest type distribution for Siberia, aiming at capability of mapping Siberian forest landscapes for applications such as predicting response of forest composition to climate change. We present data for several areas in West Siberian middle taiga, Central Siberia and East Siberia near Yakutsk. Analysis of the field survey, forest inventory data was made to produce forest type classification accounting for several stages for forest succession and variations in habitats and landforms. Supervised classification was applied to the areas were the ground truth and inventory data are available, including several limited area maps and vegetation survey transects. In Laryegan basin in West Siberia the upland forest areas are dominated by mix of Scots pine on sandy soils and Siberian pine with presence of fir and spruce on the others. Abundance of Scots pine decreases to the west due to change in soils. Those types are separable using Landsat spectral data. In the permafrost area around Yakutsk the most widespread succession type is birch to larch. Three stages of the birch to larch succession are detectable from Landsat image. When Landsat data is used in both West and East Siberia, distinction between deciduous broad-leaved species (birch, aspen, and willow) is generally difficult. Similar problem exist for distinguishing between dark coniferous species (Siberian pine, fir and spruce). Image classification can be improved by applying landform type analysis, such as separation into floodplain, terrace, sloping hills. Additional layers of information can be a promising way to complement Landsat data.

  11. A review of myrmecophilous mites of the family Microdispidae (Acari, Heterostigmatina) of Western Siberia

    PubMed Central

    Khaustov, Alexander A.

    2014-01-01

    Abstract Five species of myrmecophilous microdispid mites (Acari: Microdispidae) are recorded from Western Siberia, Russia. Unguidispus lasii Kurosa, 1979, Unguidispus japonicus Kurosa, 1979, Caesarodispus minutus (Sevastianov, 1981), and Caesarodispus samsinaki (Mahunka, 1967), comb. n. are reported from Russia for the first time. Unguidispus polyctenus (Sevastianov, 1969) and Caesarodispus samsinaki are redescribed. The keys to species of the genera Unguidispus Mahunka, 1970 and Caesarodispus Mahunka, 1977 are provided. PMID:25493064

  12. Dragon Lake, Siberia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Nicknamed 'Dragon Lake,' this body of water is formed by the Bratskove Reservoir, built along the Angara river in southern Siberia, near the city of Bratsk. This image was acquired in winter, when the lake is frozen. This image was acquired by Landsat 7's Enhanced Thematic Mapper plus (ETM+) sensor on December 19, 1999. This is a natural color composite image made using blue, green, and red wavelengths. Image provided by the USGS EROS Data Center Satellite Systems Branch

  13. [Results of studies of human dirofilariasis in Russia].

    PubMed

    Sergiev, V P; Supriaga, V G; Bronshteĭn, A M; Ganushkina, L A; Rakova, V M; Morozov, E N; Fedianina, L V; Frolova, A A; Morozova, L F; Ivanova, I B; Darchenkova, N N; Zhukova, L A

    2014-01-01

    Human dirofilariasis is a pressing health problem in Russia. By 2014, there have been as many as 850 Dirofilaria repens-infested people living in 42 subjects of the Russian Federation. One of the favorable factors for circulation and spread of invasion is a temperature of above +20-24 degrees C; when the latter is maintained during at least 20 days there may be 1.-1.5 circulations of invasion in the carrier and a 2.8-fold increase in transmission intensity. The border ofa dirofilariasis area with a temperate climate is southward to 58 degrees N in European Russia and West Siberia and southward to 50 degrees N in the Far East. The conditions in the human body have been found to be more favorable for the development of Dirofilaria than considered before and allow the helminth to achieve sexual maturity and to propagate. If man has microfilaremia, he may be a source of invasion. It is necessary to examine venous blood by the enrichment method and, if possible, polymerase chain reaction and enzyme immunoassay, which make it possible to establish a diagnosis in occult invasion and to identify a pathogen species.

  14. Increased Pathogenicity of West Nile Virus (WNV) by Glycosylation of Envelope Protein and Seroprevalence of WNV in Wild Birds in Far Eastern Russia

    PubMed Central

    Kariwa, Hiroaki; Murata, Ryo; Totani, Masashi; Yoshii, Kentaro; Takashima, Ikuo

    2013-01-01

    In this review, we discuss the possibility that the glycosylation of West Nile (WN) virus E-protein may be associated with enhanced pathogenicity and higher replication of WN virus. The results indicate that E-protein glycosylation allows the virus to multiply in a heat-stable manner and therefore, has a critical role in enhanced viremic levels and virulence of WN virus in young-chick infection model. The effect of the glycosylation of the E protein on the pathogenicity of WN virus in young chicks was further investigated. The results indicate that glycosylation of the WN virus E protein is important for viral multiplication in peripheral organs and that it is associated with the strong pathogenicity of WN virus in birds. The micro-focus reduction neutralization test (FRNT) in which a large number of serum samples can be handled at once with a small volume (15 μL) of serum was useful for differential diagnosis between Japanese encephalitis and WN virus infections in infected chicks. Serological investigation was performed among wild birds in the Far Eastern region of Russia using the FRNT. Antibodies specific to WN virus were detected in 21 samples of resident and migratory birds out of 145 wild bird samples in the region. PMID:24351738

  15. Aluminium phosphate and phosphate-sulphate minerals in kyanite schists of the Ichetuyskoye area, West Transbaikalia, Russia: crystal chemistry and evolution

    NASA Astrophysics Data System (ADS)

    Izbrodin, Ivan A.; Ripp, German S.; Doroshkevich, Anna G.

    2011-01-01

    Aluminium phosphate and aluminium phosphate-sulphate (APS) minerals occur as disseminated crystals and fine-grained aggregates in kyanite schists near Ichetuyskoye, in the Dzhida basin (West Transbaikal region, Russia). Petrographical, mineralogical and geochemical data suggest a metamorphic evolution through prograde and retrograde stages. Lazulite-scorzalite and trolleite in association with kyanite, quartz, muscovite, paragonite, topaz, rutile, magnetite and hematite formed during the prograde stage. More than 25 minerals identified in schists are genetically related to the retrograde stage. Some phosphates and all of the APS minerals belong to the alunite, beudantite and plumbogummite groups. Electron-microprobe data reveal the presence of wide compositional variations and complex solid-solution series among the members. The main crystal-chemical variations of the APS solid-solution series in the alunite supergroup concern the relative proportions of svanbergite, woodhouseite, goyazite, crandallite, florencite-(Ce) and natroalunite. Chemical analyses of APS minerals indicate extremely high amounts of LREE, Sr, Ba, Ca and Na. In some cases, APS minerals have compositions of Ba and Ca,Ba phosphates- sulphates.

  16. Organochlorine pesticide, polychlorinated biphenyl and heavy metal concentrations in wolves (Canis lupus L. 1758) from north-west Russia.

    PubMed

    Shore, R F; Casulli, A; Bologov, V; Wienburg, C L; Afsar, A; Toyne, P; Dell'Omo, G

    2001-12-03

    The wolf Canis lupus is a major terrestrial predator in eastern Europe and, as a top carnivore, may be exposed to high concentrations of contaminants that are readily transferred through the food chain. Despite this, there are few published data on pollutant and pesticide levels in wolves. This study utilised tissues from animals legally killed by hunters for other reasons (animals were not killed for the purposes of this study) to carry out the only detailed investigation of contaminants in wolves in Europe and the first in animals from Eastern Europe. The livers of 58 wolves from the Tver and Smoliensk regions of northwest Russia (54 degrees N 31 degrees E to 57 degrees N 35 degrees E) were analysed for seven organochlorine pesticides, 24 PCB congeners, Aroclor 1254-matched summed PCBs (sigmaPCBs), total mercury, cadmium and lead. Cadmium, most of the organochlorine pesticides and many PCB congeners were not detectable in any of the wolves. Hexachlorobenzene, alpha-HCH, pp'DDE, PCB congeners 118, 138, 149 and 156 and lead were detected in up to 6% of livers. Dieldrin, PCB congeners 153, 170 and 180, sigmaPCBs and mercury were detected more frequently. Contaminant levels were generally low; maximum wet weight concentrations of any of the organochlorine pesticides, sigmaPCBs and mercury were less than 0.1, 1 and 0.25 microg g(-1), respectively. PCB congeners 153, 170 and 180 accounted for 41% of the sigmaPCBs. Dieldrin, sigmaPCBs and mercury concentrations did not vary significantly between males and females nor between adult and juvenile (< 12 months old) wolves apart from the sigmaPCB concentration, which was on average five times higher in adults than juveniles. Liver residues were generally below the level normally associated with adverse effects except for lead levels which exceeded the critical 5 microg g(-1) dry wt. concentration in three of the 58 animals examined.

  17. Flooding in Central Siberia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    A mixture of snowmelt and ice jams in late May and June of this year caused the Taz River (left) and the Yenisey River (right) in central Siberia to overflow their banks. The flooding can be seen in this image taken on June 11, 2002, by the MODIS (Moderate Resolution Imaging Spectroradiometer) instrument aboard the Terra satellite. Normally, the rivers would resemble thin black lines in MODIS imagery. In the false-color images sage green and rusty orange is land, and water is black. Clouds are white and pink. Credit: Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC

  18. Sequence stratigraphic setting of the Priob Field within the Neocomian prograding complex of the West Siberian Basin, Russia

    SciTech Connect

    Mkrtchyan, O.M.; Armentrout, J.M.

    1995-08-01

    The Neocomian strata of the West Siberian Basin are a prograding complex unique in its aerial extent, structure and hydrocarbon reserves, such as Priob Field in the Ob River area. Interpretation of the basin history is based on well data and seismic reflection profile. As many as 45 transgressive-regressive depositional sequences, called cyclites, prograde into the deep-water basin formed during Late Jurassic and Early Cretaceous. Each transgressive-regressive sequence is defined by a coarsening-upward cycle of shale, siltstone and sandstone, and is considered a chronostratigraphic subdivision of the prograding complex. Each sequence boundary is regionally correlatable on seismic reflection profiles, and is identified on well logs by sharp contacts between regressive sandstones below and thin transgressive shales above. Subordinate progradational wedges are locally developed within these sequences and contain major hydrocarbon reserves. These depositional wedges map as lens-shaped packages downlapping the outermost shelf (Priob zone) or as narrow progradational wedges downlapping the foreset reflections of the slope clinoforms immediately beyond the shelf break (Sugmut zone). Regressive facies of the shelf consist of thin but wide spread sandstones that also contain major hydrocarbon reserves. Pervasive sediment starvation during the Late Neocomian resulted in deposition of thin regionally extensive shales that provide top-seal to the Neocomian hydrocarbon system. At the Priob field, a deep erosional incision has been mapped at the AS11 shelf-edge. Sands transported through this incised valley were deposited as a prograding wedge along the shoreline, forming the reservoir facies for the Priob hydrocarbon accumulation. Stratigraphic aspects of the Priob trap include top and lateral shale seals and subtle regional structural tilt. Types of stratigraphic traps are discussed and the possibility of predicting additional such traps are analyzed.

  19. Comparison of the Impact of the Arctic Oscillation and East Atlantic - West Russia Teleconnection on Interannual Variation in East Asian Winter Temperatures and Monsoon

    NASA Technical Reports Server (NTRS)

    Lim, Young-Kwon; Kim, Hae-Dong

    2014-01-01

    The large-scale impacts of the Arctic Oscillation (AO) and the East Atlantic/West Russia (EA/WR) teleconnection on the East Asian winter climate anomalies are compared for the past 34 winters focusing on 1) interannual monthly to seasonal temperature variability, 2) East Asian winter monsoon (EAWM), and 3) the Siberian high (SH) and cold surge. Regression analysis reveals warming by AO and EA/WR over mid-latitude East Asia during their positive phase and vice versa. The EA/WR impact is found to be comparable to the AO impact in affecting the East Asian temperature and monsoon. For example, warm (cold) months over mid-latitude East Asia during the positive (negative) AO are clearly seen when the AO and EA/WR are in the same phase. Near zero correlation is found between temperature and the AO phase when both teleconnections are in an opposite phase. The well-known negative relationship between SH and the AO phase is observed significantly more often when the AO is in the same phase with the EA/WR. Also, the indices of EAWM, cold surge, and SH are found to be more highly negative-correlated with the EA/WR rather than with the AO. The advective temperature change and associated circulation demonstrate that the anomalous large-scale field including the SH over the mid-latitude Asian inland is better represented by the EA/WR, influencing the East Asian winter climates. These results suggest that the impact of EA/WR should be considered more important than previously thought for a better understanding of East Asian winter temperature and monsoon variability.

  20. Moscow, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Moscow, the political and economic heart of Russia, sits on the far eastern end of Europe, roughly 1300 kilometers (815 miles) west of the Ural Mountains and the Asian continent. The city boasts a population of nine million and encompasses an area of 1035 square kilometers (405 square miles). The Moscow River runs through the center of the city, and the Kremlin, the seat of the Russian government, lies in the direct center. Moscow is thought to have been founded in the 12th Century by Yury Dolgoruky, Prince of Suzdal, who hosted a big feast on the site. The city was shortly after established as a trading route along the Moscow River. Ivan III, who is largely credited with uniting all of Russia, built the Kremlin's cathedrals and declared Moscow the capital of his new kingdom in the 15th century. In the 17th century, Ivan the Great moved the capital to St. Petersburg, where it remained until the Bolsheviks brought the seat of government back to Moscow in 1918. Over the years the city has been sacked and burnt to the ground by the Tartars, the Poles, and the French. Thanks to the resilient spirit of the Russian people, the city remains as vital as ever. Now it is as capitalist in nature as London or New York, and everything from Big Macs to BMWs can be found on its streets. The blue-gray pixels in this false-color image are urban areas. The light green areas surrounding the city are farms and the brown regions are more sparsely vegetated areas. This image of Moscow was acquired by the Enhanced Thematic Mapper plus (ETM+), flying aboard the Landsat 7 satellite. July 23, 2002, marks the 30th anniversary of the Landsat program. (Click to read the press release-Celebrating 30 Years of Imaging the Earth.) The Landsat program has been particularly instrumental in tracking land use and land cover changes-such as increased urban growth-over the last three decades. Image courtesy Ron Beck, USGS EROS Data Center Satellite Systems Branch

  1. THE DEVELOPMENT AND THE STRATEGY OF THE OIL AND GAS PIPELINES OF RUSSIA

    NASA Astrophysics Data System (ADS)

    Motomura, Masumi

    The Russian oil and gas industry earns more than half of the Russian tax revenue and foreign currency, and has been playing the role of the backbone of the state economy through the eras of the Soviet Union and the Russian Federation. With the elongation of distance to the European market from the oil producing regions, starting from Baku in the era of Imperial Russia to the Second Baku (Volga-Ural) and the third Baku (West Siberia) in turn, the role of the oil pipeline system as the transportation infrastructure became more and more important and the deployment of pipelines has become one of the indispensable pillars of oil strategy. Now, the oil pipeline network is to reach the Pacific Ocean, which will enable Northeast Asia to be added as a destination for Russian oil, with a result of expanding influence for Russia in these regions. On the other hand, gas exports from the Soviet Union to Eastern Europe started in 1967 by constructing a trunk pipeline from Ukraine, which was extended to West Germany in 1973, overcoming the confrontation between the East and the West and becoming a regional stabilizer. The United States considered this pipeline as an energy weapon and criticized this deal by saying that when Soviet gas flows to Western Europe, its political influence must flow like the gas itself. However, the Soviet Union collapsed in 1991, while gas transportation continued without any disruption. This is evidence that the gas pipeline from the Soviet Union was purely for a business purpose and was not politicized. Recently, Russia is aiming to export gas to northeastern Asia, which is expected to be a new stabilizer in this region, although different types of diffi culties (especially about the method of determination of the gas price) still need to be resolved.

  2. Peculiarities of strength and deformability properties of clay soils in districts of Western Siberia

    NASA Astrophysics Data System (ADS)

    Efimenko, Sergey; Efimenko, Vladimir; Sukhorukov, Alexey

    2016-01-01

    The article demonstrates the methodology of the substantiation of the calculated values of moisture, strength, and deformability characteristics of clay subgrade soils for the design of pavements by strength conditions in II, III, and IV road-climatic zones in West Siberia. The main purpose of the work is to ensure the quality of the design of roads in newly developed regions of Russia. To achieve this goal the following problems have been solved: the dislocation of boundary lines of road-climatic zones has been specified, zoning of the investigated territory for the design of roads has been detailed; regularities of changes in strength and deformability characteristics of clay subgrade soils of their moisture have been established; the territorial normalization of the calculated values of moisture, strength, and deformability of clay subgrade soils in relation to the allocated road districts has been carried out. Specification of boundary lines of road-climatic zones has been implemented on the basis of the taxonomic system "zone-subzone-road district". The calculated values of moisture, strength, and deformability characteristics of clay soils, established and differentiated according to road-climatic zones, will ensure the required level of the reliability of transport infrastructure facilities during the life cycle of roads.

  3. Vegetation and climate in the Western Sayan Mts according to pollen data from Lugovoe Mire as a background for prehistoric cultural change in southern Middle Siberia

    NASA Astrophysics Data System (ADS)

    Blyakharchuk, Tatiana A.; Chernova, Natalia A.

    2013-09-01

    On the basis of pollen and spore analyses and radiocarbon dating of peat deposits of Lugovoe Mire in southern Middle Siberia, changes of vegetation and climate of the Western Sayan Mts and the Khakasia Republic (Russia) since 6000 yr 14C BP (5000 cal yr BC) are found to correspond with the development of archaeological cultures and with the pollen-based palaeoclimatic reconstruction of Levina and Orlova (1993) constructed for the forest-steppe zone of the south of West Siberia. Three phases in the development of the regional vegetation (Abies, Betula, and Pinus) are distinguished in the pollen diagram of Lugovoe Mire, which form the environmental background for the archaeological cultures developed in this region. The first penetration of ancient hunting-fishing tribes into this area occurred during the ‘Abies stage' of the vegetation. Bronze Age cultures practiced agriculture and animal husbandry mostly during the ‘Betula stage'. Beginning in the Iron Age, archaeological cultures bloomed in the study area on the background of expanding Pinus sylvestris forests. The origin of all these cultures was connected with migrations of people from the southwest or southeast. An important reason for these migrations was dry climatic phases at millennial intervals, which influenced especially strongly the more southerly homelands of the migrating ancient tribes.

  4. Artemia cyst production in Russia

    NASA Astrophysics Data System (ADS)

    Litvinenko, Liudmila I.; Litvinenko, Aleksandr I.; Boiko, Elena G.; Kutsanov, Kirill

    2015-11-01

    In Western Siberia (Russia) there are about 100 Artemia lakes with total area over 1 600 km2. Geographically these lakes are located between 51°-56°N and 61°-82°E. In general these lakes are shallow (depth less than 1.5 m), small or medium size (0.1 to 10 km2); they are chloride; their total salinity is from 40 to 250 g/L. The harvesting of cysts per year is only in 20-40 lakes. In Russia 550 tons of dry Artemia cysts (14%-18% of the world production) were harvested annually. This includes about 350 tons in the Altai region and 200 tons in other regions. During our regular 20-year study period the cyst harvest was: 95 tons in Kurgan; 65 tons in Omsk, 20 tons in Novosibirsk, 20 tons in Tyumen. Ways of increasing cyst harvest in Russia are considered in this article. During the last 30 years the harvest of cysts in Russia has increased from 7-20 to 500-600 tons. A significant influence of dryness of the year was found on productivity in selected lakes, but taken for all the lakes together, the relationship was not significant. The optimal salinity for productivity of cysts in the lakes was determined. Analysis of productivity of the lakes and the harvesting results showed that the stocks of cysts are underutilized by approximately 1.7 times.

  5. Russia Between West and East

    DTIC Science & Technology

    2003-10-01

    well-being is alien to the Russian people, whose deep-rooted spiritual requirement, according to Fyodor Dostoyevsky , “is the requirement of suffering, an...Moscow, 1961), p. 105. 14. F. Dostoyevsky , A Writer’s Diary, 1873, p. 256. 19 As long as we are moved, just like Russian philosopher Konstantin Leontiev

  6. Genome sequence of Desulfosporosinus sp. OT, an acidophilic sulfate-reducing bacterium from copper mining waste in Norilsk, Northern Siberia.

    PubMed

    Abicht, Helge K; Mancini, Stefano; Karnachuk, Olga V; Solioz, Marc

    2011-11-01

    We have sequenced the genome of Desulfosporosinus sp. OT, a Gram-positive, acidophilic sulfate-reducing Firmicute isolated from copper tailing sediment in the Norilsk mining-smelting area in Northern Siberia, Russia. This represents the first sequenced genome of a Desulfosporosinus species. The genome has a size of 5.7 Mb and encodes 6,222 putative proteins.

  7. Eastern Siberia terrain intelligence

    USGS Publications Warehouse

    ,

    1942-01-01

    The following folio of terrain intelligence maps, charts and explanatory tables represent an attempt to bring together available data on natural physical conditions such as will affect military operations in Eastern Siberia. The area covered is the easternmost section of the U.S.S.R.; that is the area east of the Yenisei River. Each map and accompanying table is devoted· to a specialized set of problems; together they cover such subjects as geology, construction materials, mineral fuels, terrain, water supply, rivers and climate. The data is somewhat generalized due to the scale of treatment as well as to the scarcity of basic data. Each of the maps are rated as to reliability according to the reliability scale on the following page. Considerable of the data shown is of an interpretative nature, although precise data from literature was used wherever possible. The maps and tables were compiled  by a special group from the United States Geological Survey in cooperation with the Intelligence Branch of the Office, Chief of Engineers, War Department.

  8. Circulation patterns governing October snowfalls in southern Siberia

    NASA Astrophysics Data System (ADS)

    Bednorz, Ewa; Wibig, Joanna

    2015-12-01

    This study is focused on early fall season in southern Siberia (50-60 N) and is purposed as a contribution to the discussion on the climatic relevance of October Eurasian snow cover. Analysis is based on the daily snow depth data from 43 stations from years 1980-2012, available in the database of All-Russian Research Institute of Hydrometeorological Information—World Data Centre. The snow cover season in southern Siberia starts in early autumn and the number of days with snowfall varies from less than 5 days in the southernmost zone along the parallel 50 N to more than 25 days in the northeastern part of the analyzed area. October snowfall in southern Siberia is associated with occurrence of negative anomalies of sea level pressure (SLP), usually spreading right over the place of recorded intense snowfall or extending eastward from it. Negative anomalies of air temperature at the 850 hPa geopotential level (T850) occurring with increased cyclonic activity are also observed. Negative T850 anomalies are located west or northwest of the SLP depressions. Counterclockwise circulation around low-pressure systems transports cold Arctic air from the north or even colder Siberian polar air from the east, to the west, and northwest parts of cyclones, and induces negative anomalies of temperature. The pattern of T850 anomalies during heavy snowfalls in the eastern part of the southern Siberia is shifted counterclockwise in regard to SLP anomalies: the strongest negative T850 anomalies are located west or northwest of the SLP depressions.

  9. Biogeochemical phosphorus mass balance for Lake Baikal, southeastern Siberia, Russia

    USGS Publications Warehouse

    Callender, E.; Granina, L.

    1997-01-01

    Extensive data for Lake Baikal have been synthesized into a geochemical mass balance for phosphorus (P). Some of the P budget and internal cycling terms for Baikal have been compared to similar terms for oligotrophic Lake Superior, mesotrophic Lake Michigan and the Baltic Sea, and the Ocean. Lake Baikal has a large external source of fluvial P compared to the Laurentian upper Great Lakes and the Ocean. The major tributary to Lake Baikal has experienced substantial increases in organic P loading during the past 25 years. This, coupled with potential P inputs from possible phosphorite mining, may threaten Baikal's oligotrophic status in the future. Water-column remineralization of particulate organic P is substantially greater in Lake Baikal than in the Laurentian Great Lakes. This is probably due to the great water depths of Lake Baikal. There is a gradient in P burial efficiency, with very high values (80%) for Lake Baikal and Lake Superior, lower values (50%) for Lake Michigan and the Baltic Sea, and a low value (13%) for the Ocean. The accumulation rate of P in Lake Baikal sediments is somewhat greater than that in the Laurentian upper Great Lakes and the Baltic Sea, and much greater than in the Ocean. Benthic regeneration rates are surprisingly similar for large lacustrine and marine environments and supply less than 10% of the P utilized for primary production in these aquatic environments.

  10. Genetic diversity of Echinococcus spp. in Russia.

    PubMed

    Konyaev, Sergey V; Yanagida, Tetsuya; Nakao, Minoru; Ingovatova, Galina M; Shoykhet, Yakov N; Bondarev, Alexandr Y; Odnokurtsev, Valeriy A; Loskutova, Kyunnyay S; Lukmanova, Gulnur I; Dokuchaev, Nikolai E; Spiridonov, Sergey; Alshinecky, Mikhail V; Sivkova, Tatyana N; Andreyanov, Oleg N; Abramov, Sergey A; Krivopalov, Anton V; Karpenko, Sergey V; Lopatina, Natalia V; Dupal, Tamara A; Sako, Yasuhito; Ito, Akira

    2013-11-01

    In Russia, both alveolar and cystic echinococcoses are endemic. This study aimed to identify the aetiological agents of the diseases and to investigate the distribution of each Echinococcus species in Russia. A total of 75 Echinococcus specimens were collected from 14 host species from 2010 to 2012. Based on the mitochondrial DNA sequences, they were identified as Echinococcus granulosus sensu stricto (s.s.), E. canadensis and E. multilocularis. E. granulosus s.s. was confirmed in the European Russia and the Altai region. Three genotypes, G6, G8 and G10 of E. canadensis were detected in Yakutia. G6 was also found in the Altai region. Four genotypes of E. multilocularis were confirmed; the Asian genotype in the western Siberia and the European Russia, the Mongolian genotype in an island of Baikal Lake and the Altai Republic, the European genotype from a captive monkey in Moscow Zoo and the North American genotype in Yakutia. The present distributional record will become a basis of public health to control echinococcoses in Russia. The rich genetic diversity demonstrates the importance of Russia in investigating the evolutionary history of the genus Echinococcus.

  11. The American Expeditionary Force Siberia: A Case Study of Operational Art with Ambiguous Strategic Objectives

    DTIC Science & Technology

    2014-05-22

    Also in June 1919, a new phase in operations for the Allies in Siberia began. With the signing the Treaty of Versailles , any pretext of the Allied...accomplished what it set out to do” 80 Ultimately, the Czech legion left Russia, but by then the Treaty of Versailles was nearly a year old. The...was whether the armistice agreement of 11 November 1918 or the Treaty of Versailles signed on 28 June 1919 defined that specific termination criterion

  12. Kondyor Massif, Russia

    NASA Technical Reports Server (NTRS)

    2008-01-01

    This is neither an impact crater nor a volcano. It is a perfect circular intrusion, about 10 km in diameter with a topographic ridge up to 600 m high. The Kondyor Massif is located in Eastern Siberia, Russia, north of the city of Khabarovsk. It is a rare form of igneous intrusion called alkaline-ultrabasic massif and it is full of rare minerals. The river flowing out of it forms placer mineral deposits. Last year 4 tons of platinum were mined there. A remarkable and very unusual mineralogical feature of the deposit is the presence of coarse crystals of Pt-Fe alloy, coated with gold. This 3-D perspective view was created by draping a simulated natural color ASTER composite over an ASTER-derived digital elevation model.

    The image was acquired on June 10, 2006, and is located at 57.6 degrees north latitude, 134.6 degrees east longitude.

    The U.S. science team is located at NASA's Jet Propulsion Laboratory, Pasadena, Calif. The Terra mission is part of NASA's Science Mission Directorate.

  13. Mapping forest succesion types in Siberia with Landsat data

    NASA Astrophysics Data System (ADS)

    Maksyutov, S. S.; Sedykh, V.; Kleptsova, I.; Frolov, A.; Silaev, A.; Kuzmenko, E.; Farber, S.; Kuzmik, N.; Sokolov, V. A.; Fedorov, A.; Nikolaeva, S.

    2013-12-01

    We develop a forest typology system based on dynamic vegetation approach and apply it to the analysis of the forest type distribution for several test areas in Siberia, aiming at capability of mapping whole Siberian forests based on Landsat data. Test region locations are: two in West Siberian middle taiga (Laryegan and Nyagan), one in Central Siberia and one in East Siberia near Yakutsk. The ground truth data are based on analysis of the field survey, forest inventory data from the point of view of the successional forest type classification. Supervised classification was applied to the areas covered with analysis of the ground truth and inventory data, using several limited area maps and vegetation survey transects published in literature. In Laryegan basin the upland forest areas are dominated (as climax forest species) by Scots pine on sandy soils and Siberian pine with presence of fir and spruce on the others. Those types are separable using Landsat spectral data alone. In the permafrost area around Yakutsk the most widespread succession type is birch to larch succession. Three stages of the birch to larch succession are detectable from Landsat image. When Landsat data is used in both West and East Siberia, distinction between deciduous broad-leaved species (birch, aspen, and willow) is difficult due to similarity in spectral signatures. Same problem exist for distinguishing between dark coniferous species (Siberian pine, fir and spruce). Image classification can be improved by applying landscape type analysis, such as separation into floodplain, terrace, sloping hills. Additional layers of information seem to be a promising way to complement Landsat data, including SAR-based biomass maps and terrain data

  14. Russia report

    NASA Astrophysics Data System (ADS)

    Along with cementing the joint Shuttle-Mir Program in late June with a $400 million contract, the U.S. and Russia signed a deal to team up on global environmental issues. Under the agreement, U.S. and Russian scientists will establish modern facilities for petroleum research, including advanced geographic systems technology, petroleum geochemistry, and seismic processing to help Russia transition to a “market” economy, Interior Secreary Bruce Babbitt reports. The program, to be funded by the U.S. Agency for International Development, will produce maps, technical reports, and other data for investment decisions.

  15. Mapping wetland and forest landscapes in Siberia with Landsat data

    NASA Astrophysics Data System (ADS)

    Maksyutov, Shamil; Kleptsova, Irina; Glagolev, Mikhail; Sedykh, Vladimir; Kuzmenko, Ekaterina; Silaev, Anton; Frolov, Alexander; Nikolaeva, Svetlana; Fedorov, Alexander

    2014-05-01

    Landsat data availability provides opportunity for improving the knowledge of the Siberian ecosystems necessary for quantifying the response of the regional carbon cycle to the climate change. We developed a new wetland map based on Landsat data for whole West Siberia aiming at scaling up the methane emission observations. Mid-summer Landsat scenes were used in supervised classification method, based on ground truth data obtained during multiple field surveys. The method allows distinguishing following wetland types: pine-dwarf shrubs-sphagnum bogs or ryams, ridge-hollows complexes, shallow-water complexes, sedge-sphagnum poor fens, herbaceous-sphagnum poor fens, sedge-(moss) poor fens and fens, wooded swamps or sogra, palsa complexes. In our estimates wetlands cover 36% of the taiga area. Total methane emission from WS taiga mires is estimated as 3.6 TgC/yr,which is 77% larger as compared to the earlier estimate based on partial Landsat mapping combined with low resolution map due to higher fraction of fen area. We make an attempt to develop a forest typology system useful for a dynamic vegetation modeling and apply it to the analysis of the forest type distribution for several test areas in West and East Siberia, aiming at capability of mapping whole Siberian forests based on Landsat data. Test region locations are: two in West Siberian middle taiga (Laryegan and Nyagan), and one in East Siberia near Yakutsk. The ground truth data are based on analysis of the field survey, forest inventory data from the point of view of the successional forest type classification. Supervised classification was applied to the areas where ample ground truth and inventory data are available, using several limited area maps and vegetation survey. In Laryegan basin the upland forest areas are dominated (as climax forest species) by Scots pine on sandy soils and Siberian pine with presence of fir and spruce on the others. Those types are separable using Landsat spectral data alone. In

  16. [Distribution of viruses from the Californian encephalitis serogroup (Bunyaviridae, Bunyavirus) in the northern expanses of Russia].

    PubMed

    L'vov, S D; Gromashevskiĭ, V L; Morozova, T N; Aristova, V A; Skvortsova, T M; Galkina, I V; L'vov, D K; Butenko, A M; Mitchell, K D; Savage, H M; Selivanov, Ia M; Egorov, N Ia; Androsov, I A; Tugutov, L D; Cherniavskiĭ, V F; Mikhaĭlova, N B; Mayer, V A; Galimov, V R; Sokolova, N G; Andronova, O N; Semenov, V B; Baĭluk, F N; Pogorelyĭ, Iu D; Fadeev, E S; Grekov, E I

    1997-01-01

    The study was carried out in 1983-1991 and covered a territory of about 10 x 10(6) km2 in various physico-geographic areas (East Fennoscandia, Northern Russian Plain, West Siberia, Central Siberia, North-Eastern Siberia, and Northern Pacific Region) in the Arctic, Subarctic, Northern-Central-Southern taiga, forest-steppe, and steppe in Northern Russia. A total of 251 strains were isolated from 1391,900 mosquitoes, identified as the California group snowshoe hare (83), Inkoo (44), and Tahyna (2) viruses; 122 strains were not completely identified. Some of the strains with uncommon antigenic composition can be natural reassortants. Fifty-two percent of strains were isolated from Aedes communis and the associate species of mosquitoes, other hosts were A. excrucians (8%), A. cantans (6.25%), A. flavescens (6.25%), A. ciprius (6.25%), A. punctor (4.5%), A. vexans (4.5%), A. cataphylla (3.6%), A. nigripes (3.6%), and A. hexodontus (2.6%). The infection rate of mosquitoes was 0.009% in the tundra, 0.012% in forest-tundra, 0.01% in Northern taiga, 0.02% in Central taiga, 0.017% in Southern taiga, 0.026% in forest-steppe, and 0.097% in steppe. The epidemic season is one month in the tundra (from the beginning of July till the beginning of August), two months in Northern taiga (July-August), and three months in Central taiga (from the second half of June till the beginning of September). The highest infection rate of mosquitoes was observed at the end of the epidemic season in all regions. SSH strains prevailed to the East from the Enisei river, whereas to the West and in the Subarctic regions INK virus predominated, SSH being rare; in the taiga the distribution was quite the opposite. TAH virus was virtually absent. Human morbidity was observed in all territories studied. The immune stratum of adult population is about 30% in the tundra and forest-tundra and about 50% in Northern and Central taiga.

  17. Flooding on Russia's Lena River

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Nearly every year in the late spring, ice blocks the flow of water at the mouth of the Lena River in northeastern Russia and gives rise to floods across the Siberian plains. This year's floods can be seen in this image taken on June 2, 2002, by the MODIS (Moderate Resolution Imaging Spectroradiometer) instrument aboard the Terra satellite. The river runs down the left side of the image, and its delta is shrouded in ice (red) at the top of the image. Normally, the river would resemble a thin black line in MODIS imagery. The river, which is Russia's longest, flows 2,641 miles (4,250 kilometers) south to north through Siberia and into the Laptev Sea. In the winter, the river becomes nearly frozen. In the spring, however, water upstream thaws earlier than water at the mouth of the river. As the southern end of the river begins to melt, blocks of ice travel downstream to the still frozen delta, pile up, and often obstruct the flow of water. Flooding doesn't always occur on the same parts of the river. The floods hit further south last year. If the flooding grows severe enough, explosive charges are typically used to break up the ice jams. In these false-color images land areas are a dull, light green or tan, and water is black. Clouds appear pink, and ice comes across as bright red. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC

  18. Enterprise systems in Russia: 1992-2012

    NASA Astrophysics Data System (ADS)

    Kataev, Michael Yu; Bulysheva, Larisa A.; Emelyanenko, Alexander A.; Emelyanenko, Vladimir A.

    2013-05-01

    This paper introduces the enterprise systems (ES) development and implementation in Russia in the past three decades. Historic analysis shows that, in terms of time frame, the development of ACS (Automated Control Systems) in the former Soviet Union and the ERP (Enterprise Resource Planning) in the West was almost parallel. In this paper, the current status and the major trend of ES in Russia is discussed.

  19. [Plant viruses of the Asian territory of Russia: taxonomy and nomenclature].

    PubMed

    Gnutova, R V

    2011-01-01

    This review presents the results of long-term study of the species diversity of plant viruses on the Asian territory of Russia. The known and new viruses were revealed in agro- and biocenoses and identified not only for the Far East and Siberia but also for Russia. Based on the criteria of traditional and molecular-genetic taxonomy, 50 viruses were referred to 8 families and 18 genera of the currently known 17 families and 78 genera of plant viruses. The taxonomic status of new phytopathogenic viruses revealed on the Asian territory of Russia was defined.

  20. Petroleum geology of east Siberia

    SciTech Connect

    Clarke, J.W. )

    1991-03-01

    Two oil-gas provinces are present in East Siberia: the Lena-Tunguska in the central, southern, and western parts, and the Khatanga-Viluy along the northern and eastern margins. The provinces developed as rift-sag features in late Proterozoic and Paleozoic time. The identified oil and gas deposits of the Lena-Tunguska province appear to be associated with a Proterozoic rift that extends east-northeast across the southern part of the basin. These deposits are in upper Proterozoic and Cambrian sandstones and carbonate rocks, sealed by Cambrian salt and argillites. The oil and gas deposits of the Khatanga-Vilyuy province are within foreland downwarps that developed in connection with docking of crustal plates during the Mesozoic: during the Triassic on the north and during the Cretaceous on the east. The source of the petroleum in the immature rocks of the southeastern Lena-Tunguska province is uncertain, perhaps being derived from rocks in a downwarp to the south or from source beds that are now beneath a conjectured thrust sheet. This province has both oil and gas pools, but is gas prone in general. The source beds for the Khatanga-Vilyuy province are Permian and Mesozoic in age; the province is gas prone. More than 40 oil and gas fields have now been discovered in East Siberia.

  1. Fire Impact on Carbon Emissions on Logged and Unlogged Scots pine Forest Sites in Siberia

    NASA Astrophysics Data System (ADS)

    Ivanova, G.; Kukavskaya, E.; Buryak, L.; Kalenskaya, O.; Bogorodskaya, A.; Conard, S. G.

    2012-12-01

    Fires cover millions ha of boreal forests of Russia annually, mostly in Siberia. Wildfire and forest harvesting are the major disturbances in Siberia's boreal zone. Logged areas appear to be highly susceptible to fire due to a combination of high fuel loads and accessibility for human-caused ignition. Fire spreading from logging sites to surrounding forest is a common situation in this region. Changing patterns of timber harvesting increase landscape complexity and can be expected to increase the emissions and ecosystem damage from wildfires, inhibit recovery of natural ecosystems, and exacerbate impacts of wildfire on changing climate and on air quality. Fire effects on pine stands and biomass of surface vegetation were estimated on logged and unlogged sites in the Central Siberia region as a part of the project "The Influence of Changing Forestry Practices on the Effects of Wildfire and on Interactions Between Fire and Changing Climate in Central Siberia" supported by NASA (NEESPI). Fires occurring on logged areas were typically of higher severity than those in unlogged forests, but the specific effects of fire and logging varied widely among forest types and as a result of weather patterns during and prior to the fire. Consumption of surface and ground fuels in spring fires was 25% to 50% of that in summer fires. Estimated carbon emissions due to fire were 2-5 times higher on logged areas compared to undisturbed sites. Post-fire soil respiration decreases found for both site types partially offset carbon losses. Carbon emissions from fire and post-fire ecosystem damage on logged sites are expected to increase under changing climate conditions in Siberia.

  2. Review of the genus Oncopsis Burmeister, 1838 (Homoptera: Auchenorrhyncha: Cicadellidae: Macropsinae) of Russia and adjacent countries with description of a new species from Central Asia.

    PubMed

    Tishechkin, Dmitri Yu

    2017-01-11

    Illustrated descriptions and data on host plants and distribution for 21 species of Oncopsis of Russia and adjacent countries are given, and O. abdykulovi sp. n. from Central Asia is described. Conspecificity of O. planiscuta from East Siberia and Sakhalin,of O. tristis from Moscow Area, Alati Mts., and Sakhalin, and of O. burjatica from East Siberia and Sakhalin is corroborated by male calling signal analysis.

  3. Petroleum geology of East Siberia

    SciTech Connect

    Clarke, J.W.

    1986-05-01

    The unmetamorphosed geologic section of the East Siberian region consists of upper Proterozoic clastic and carbonate sediments; Cambrian evaporites, carbonates, and black shales; Ordovician to permian clastic and carbonate sediments; Triassic basaltic flows and intrusives; and Jurassic and Cretaceous clastic sediments. During the Cambrian, a barrier reef extended across the region. Salt and anhydrite were deposited in the vast lagoon to the southwest behind this reef. The structure is typical of platforms; broad, gentle warps are complicated by smaller highs. The total area of East Siberia that is potentially favorable for oil and gas is 3.23 million km/sup 2/ (1.24 million mi/sup 2/). Deposits in the Lena-Tunguska province are in stratigraphic traps in Proterozoic to Cambrian clastic and carbonate sediments sealed by Cambrian salt and in anticlinal structures in areas of salt tectonics. Source beds seem to be Proterozoic. Pools in the Khatanga-Vilyuy province are in anticlines in Triassic, Jurassic, and Cretaceous clastic sedimentary rocks. Source beds are Permian carbonaceous shale. Most discoveries have been of gas; however, several fields have oil rings. The traps appear to have been filled by oil at one time. Undiscovered recoverable petroleum resources of East Siberia are assessed, at 90% probability, within the range of 2.2-14.6 billion bbl of oil and 72-278 tcf of gas. Mean estimates are 7.3 billion bbl of oil and 158 tcf of gas, respectively. Gas-hydrate deposits in the Lena-Vilyuy province, where permafrost is more than 400 m thick, are estimated to contain 27 tcf of possibly recoverable gas.

  4. Sea ice, rain-on-snow and tundra reindeer nomadism in Arctic Russia.

    PubMed

    Forbes, Bruce C; Kumpula, Timo; Meschtyb, Nina; Laptander, Roza; Macias-Fauria, Marc; Zetterberg, Pentti; Verdonen, Mariana; Skarin, Anna; Kim, Kwang-Yul; Boisvert, Linette N; Stroeve, Julienne C; Bartsch, Annett

    2016-11-01

    Sea ice loss is accelerating in the Barents and Kara Seas (BKS). Assessing potential linkages between sea ice retreat/thinning and the region's ancient and unique social-ecological systems is a pressing task. Tundra nomadism remains a vitally important livelihood for indigenous Nenets and their large reindeer herds. Warming summer air temperatures have been linked to more frequent and sustained summer high-pressure systems over West Siberia, Russia, but not to sea ice retreat. At the same time, autumn/winter rain-on-snow (ROS) events have become more frequent and intense. Here, we review evidence for autumn atmospheric warming and precipitation increases over Arctic coastal lands in proximity to BKS ice loss. Two major ROS events during November 2006 and 2013 led to massive winter reindeer mortality episodes on the Yamal Peninsula. Fieldwork with migratory herders has revealed that the ecological and socio-economic impacts from the catastrophic 2013 event will unfold for years to come. The suggested link between sea ice loss, more frequent and intense ROS events and high reindeer mortality has serious implications for the future of tundra Nenets nomadism.

  5. Sea ice, rain-on-snow and tundra reindeer nomadism in Arctic Russia

    PubMed Central

    Kumpula, Timo; Meschtyb, Nina; Laptander, Roza; Macias-Fauria, Marc; Zetterberg, Pentti; Verdonen, Mariana; Kim, Kwang-Yul; Boisvert, Linette N.; Stroeve, Julienne C.; Bartsch, Annett

    2016-01-01

    Sea ice loss is accelerating in the Barents and Kara Seas (BKS). Assessing potential linkages between sea ice retreat/thinning and the region's ancient and unique social–ecological systems is a pressing task. Tundra nomadism remains a vitally important livelihood for indigenous Nenets and their large reindeer herds. Warming summer air temperatures have been linked to more frequent and sustained summer high-pressure systems over West Siberia, Russia, but not to sea ice retreat. At the same time, autumn/winter rain-on-snow (ROS) events have become more frequent and intense. Here, we review evidence for autumn atmospheric warming and precipitation increases over Arctic coastal lands in proximity to BKS ice loss. Two major ROS events during November 2006 and 2013 led to massive winter reindeer mortality episodes on the Yamal Peninsula. Fieldwork with migratory herders has revealed that the ecological and socio-economic impacts from the catastrophic 2013 event will unfold for years to come. The suggested link between sea ice loss, more frequent and intense ROS events and high reindeer mortality has serious implications for the future of tundra Nenets nomadism. PMID:27852939

  6. Assessment of a Forest-fire Danger Index for Russia Using Remote Sensing Information

    NASA Astrophysics Data System (ADS)

    Sukhinin, Anatoly; McRae, Douglas; Ji-Zhong, Jin; Dubrovskaya, Olga; Ponomarev, Eugene

    2010-05-01

    Intensive exploitation of Siberian forest resources requires to increase the level of their protection. In Russia, forests annually disturbed by fire make up about 6% of the total forest area, whereas they account for hundredth or even thousandth of percent in the West European countries and Canada. Devastating forest fires associated with long draughts have become very common over recent decades in some parts of Siberia and the Russian Far East. Fires burning under these conditions disturb hundreds of thousands hectares of forest lands. Forest fires impact essentially on different biogeocenosis and on ecological situation in region as well. Thus their detrimental effects, including economic damage, are hard to overestimate. Remote sensing data using is more perspective method for forests monitoring in Russia. Moreover satellite data is only available information for non-protected Russian boreal forests and tundra also. To be efficient, modern forest fire managers require a reliable method for estimating fire danger. For large remote forested areas, such as found in Russia where a dense network of local weather station needed to calculate fire danger does not exist, this can be a major problem. However, remote sensing using satellite data can provide reasonable estimates of fire danger across Russia to allow for an understanding of the current fire situation. An algorithm has been developed that can assess current fire danger by inputting ambient weather conditions derived from remote sensing data obtained from NOAA, TERRA-series satellites. Necessary inputs for calculating fire danger, such as surface temperature, dew-point temperature, and precipitation, are obtained from AVHRR, MODIS and ATOVS satellite data. By generating the final products as maps a concise picture can be presented of fire danger across Russia. In order to understand future fire suppression needs, fire danger predictions for an advanced 7-day period can be made using meteorological forecasts

  7. Sea Ice, Hydrocarbon Extraction, Rain-on-Snow and Tundra Reindeer Nomadism in Arctic Russia

    NASA Astrophysics Data System (ADS)

    Forbes, B. C.; Kumpula, T.; Meschtyb, N.; Laptander, R.; Macias-Fauria, M.; Zetterberg, P.; Verdonen, M.

    2015-12-01

    It is assumed that retreating sea ice in the Eurasian Arctic will accelerate hydrocarbon development and associated tanker traffic along Russia's Northern Sea Route. However, oil and gas extraction along the Kara and Barents Sea coasts will likely keep developing rapidly regardless of whether the Northwest Eurasian climate continues to warm. Less certain are the real and potential linkages to regional biota and social-ecological systems. Reindeer nomadism continues to be a vitally important livelihood for indigenous tundra Nenets and their large herds of semi-domestic reindeer. Warming summer air temperatures over the NW Russian Arctic have been linked to increases in tundra productivity, longer growing seasons, and accelerated growth of tall deciduous shrubs. These temperature increases have, in turn, been linked to more frequent and sustained summer high-pressure systems over West Siberia, but not to sea ice retreat. At the same time, winters have been warming and rain-on-snow (ROS) events have become more frequent and intense, leading to record-breaking winter and spring mortality of reindeer. What is driving this increase in ROS frequency and intensity is not clear. Recent modelling and simulation have found statistically significant near-surface atmospheric warming and precipitation increases during autumn and winter over Arctic coastal lands in proximity to regions of sea-ice loss. During the winter of 2013-14 an extensive and lasting ROS event led to the starvation of 61,000 reindeer out of a population of ca. 300,000 animals on Yamal Peninsula, West Siberia. Historically, this is the region's largest recorded mortality episode. More than a year later, participatory fieldwork with nomadic herders during spring-summer 2015 revealed that the ecological and socio-economic impacts from this extreme event will unfold for years to come. There is an urgent need to understand whether and how ongoing Barents and Kara Sea ice retreat may affect the region's ancient

  8. Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic

    NASA Astrophysics Data System (ADS)

    Cocks, L. Robin M.; Torsvik, Trond H.

    2007-05-01

    The old terrane of Siberia occupied a very substantial area in the centre of today's political Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China. Siberia's location within the Early Neoproterozoic Rodinia Superterrane is contentious (since few if any reliable palaeomagnetic data exist between about 1.0 Ga and 540 Ma), but Siberia probably became independent during the breakup of Rodinia soon after 800 Ma and continued to be so until very near the end of the Palaeozoic, when it became an integral part of the Pangea Supercontinent. The boundaries of the cratonic core of the Siberian Terrane (including the Patom area) are briefly described, together with summaries of some of the geologically complex surrounding areas, and it is concluded that all of the Palaeozoic underlying the West Siberian Basin (including the Ob-Saisan Surgut area), Tomsk Terrane, Altai-Sayan Terranes (including Salair, Kuznetsk Alatau, Batenov, Kobdin and West Sayan), Ertix Terrane, Barguzin Terrane, Tuva-Mongol Terrane, Central Mongolia Terrane Assemblage, Gobi Altai and Mandalovoo Terranes, Okhotsk Terrane and much of the Verkhoyansk-Kolyma region all formed parts of peri-Siberia, and thus rotated with the main Siberian Craton as those areas were progressively accreted to the main Siberian Terrane at various times during the latest Neoproterozoic and Palaeozoic. The Ertix Terrane is a new term combining what has been termed the "Altay Terrane" or "NE Xinjiang" area of China, and the Baytag, Baaran and Bidz terranes of Mongolia. The Silurian Tuvaella brachiopod fauna is restricted only to today's southern parts of peri-Siberia. Thus, allowing for subsequent rotation, the fauna occurs only in the N of the Siberian Terrane, and, as well as being a helpful indicator of what marginal terranes made up peri-Siberia, is distinctive as being the only Silurian fauna known from northern higher latitudes globally. In contrast, the other terranes adjacent to peri-Siberia

  9. Wildfires, smoke, and burn scars, near Yakutsk, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    The Lena River in central Siberia is hidden beneath a veil of smoke from multiple wildfires burning around the city of Yakutsk, Russia. Fires have been burning in the region off and on since late May 2002, and may be agricultural in cause. This image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Terra satellite on July 23, 2002. In the false=-color image, vegetation is bright green, smoke is blueish-white, and burned areas are reddish-brown. In both images, fire detections are marked with red outlines. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  10. Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Temperate and green in the summer, the Kamchatka Peninsula in northeastern Russia freezes over completely in the winter. This true-color image of the Kamchatka Peninsula was acquired on December 12, 2001, by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra spacecraft. The peninsula is surrounded by the Sea of Okhotsk to the west and by the Bering Sea to the east. The ice and snow highlight the stunning valleys and tall peaks of the Sredinnyy Khrebet, which is the volcanic mountain range running down the center of the peninsula. The mountains along the range reach heights of over 3500 meters (11,484 feet). Many of the volcanoes are still active, and ash and volcanic rock has turned the snow a dark gray on the eastern side of the range. The light blue latticework of ridges, valleys, and alluvial fans extending from the center of the range were likely carved out by past and present glaciers and by run-off from spring snowmelt. The small island that extends off of the tip of the peninsula is Ostrov Paramushir (Paramushir Island). Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC

  11. Long-term dynamics of atmospheric circulation over Siberia and its relationship with air temperature

    NASA Astrophysics Data System (ADS)

    Podnebesnykh, N. V.; Ippolitov, I. I.

    2012-12-01

    The main objective of this study is the investigation of cyclone characteristics variability in the region bounded by the coordinates 50°-70° N, 60°-110° W which includes Western Siberia and the part of Eastern Siberia for the time interval 1976-2006, as well as the establishment of statistical relationships between the temperature conditions and the atmospheric circulation. For the dynamics of the climatic characteristics of cyclones and anticyclones over Siberia surface synoptic maps were used, and to study the trends of air temperature daily data from 169 ground-based meteorological stations and posts located in the study area were analyzed. During the period of the modern warming the territory of Siberia was characterized by rapidly temperature increase: average annual value was 0.36°C/10 years, and average monthly value was 0.83°C/10 years. The positive trend of temperature increasing is shown for all months except November. The total number of cyclones over the territory of under study for the period of 1976-2006 has decreased at a rate of 1.4 cyclone/10 years. For further analysis all cyclones were divided into three groups, according to their directions: north, west and south. It was found the number of south and west cyclones decreased, whole the number of cyclone from north directions increased. Such multidirectional dynamics of cyclones from different directions can be associated with the processes of strengthening and weakening of the Polar and Arctic fronts in the Atlantic sector of the Northern Hemisphere. Among characteristics of vortex activity the pressure in the centers of cyclones and anticyclones has the greatest influence on the air temperature and the total number of cyclones has the smallest. Multiple regression models have shown that in different months of a year the circulation can describe from 54% to 82% of temperature variability.

  12. [Occupational digestive diseases in chemical industry workers of West Siberia].

    PubMed

    Pomytkina, T E; Pershin, A N

    2010-01-01

    The high incidence of chronic digestive diseases is recorded in chemical industry workers exposed to the isolated action of noxious substances. The aim of the investigation was to make a hygienic assessment of the risk for occupational digestive diseases in chemical industry workers exposed to a combination of noxious drugs. The working conditions and the prevalence of digestive diseases were studied in 4120 workers engaged in chemical and auxiliary processes. Under the isolated action of noxious substances, the workers had an average of 35% increase in the incidence of digestive diseases than unexposed ones (p < 0.05). Under the combined action of hazardous substances, the incidence of digestive diseases was 1.7-fold greater (p < 0.05) than in the unexposed subjects and 1.2-fold greater in those under isolated action. The odd ratio and relative risk for digestive diseases in the workers exposed to a combination of noxious substances were 4.0-11.1 and 3.5-10.7 times higher, respectively (p < 0.05) than in the unexposed subjects.

  13. [Tuberculosis epidemiology-epizoology relationship in West Siberia].

    PubMed

    Krasnov, V A; Murashkina, G S

    1998-01-01

    Comparison of tuberculosis epizootic tension with some parameters characterizing the epidemiological situation in areas with different incidence rates of cattle tuberculosis under present conditions showed their inverse correlation. It is suggested that with a drastic improvement of the epizootic situation, the cattle becomes an agent of natural immunization of inhabitants in poor districts, as evidenced not only by the lack of new cases of tuberculosis in human beings, but by an increase in cases with residual posttuberculous changes in the lung (14.1% of the stock breeders examined in the long poor tuberculosis area versus 3.7% in this infection-free area), as well as by high infection rates (74.2 versus 43.5%).

  14. [Endemic goiter in the extreme North of West Siberia].

    PubMed

    Luzina, I G; Suplotova, L A; Osadchenko, G A

    1998-01-01

    Random examinations covering 8-60-year-old 4345 citizens of 12 settlements of the Yamal-Nenets Autonomic Territory discovered goiter endemia throughout the territory but most evident the endemy manifested in the Far North. The prevalence of endemic goiter among schoolchildren made up 52.8% (enlargement of the goiter of the 1st and 2nd degree), among adults-49.2%. By ultrasound investigation, the above percentages were 29 and 26.4%, respectively. This corresponds to moderate endemia. The median of urinary iodine excretion averaged in the territory 5.1 micrograms%, while overall iodine insufficiency (number of children with urinary iodine < 10 micrograms%) was 81.9%. In the Far North iodine excretion was less but goiter incidence was higher than normal. Thus, in the Far North goiter endemia is rather serious.

  15. Specific features in the formation of the population of Siberia.

    PubMed

    Trufakin, V A

    2007-01-01

    Population migration played the main role in the development of the North-East regions of Russia, and the processes of natural moving and reproduction of new generations were their after-effects. It is possible to mark out the main periods of population formation. The period of establishing from the beginning of development (the second half of the XVI century) to the 20th of the last century. The period of accomulation and intensive use of human resources (till the beginning of the 80th of the last century) when the population increased more than twice and reached 28 mln people, 3 mln of them living in the circumpolar regions. To the end of the 20th century the period of inert growth and stabilization of population numbers with the following stage of its decreasing. The main fundamental specific feature of Siberian population is its genetic diversity. This, on the one hand, points out the biological stability of the new generations of Siberian population and, on the other hand, predetermines the formation of peculiar features of pathology and the prevalence of the diseases among various categories and ethnic groups of the population. The intensive use of natural resources in Siberia (including people), inadequate social and economic development of Siberian territories are reflected in high levels of health loss in the population as the result of mortality, disability and morbidity caused by accidents and traumas, diseases of blood circulation system, respiratory and gastrointestinal diseases, malignant neoplasms, alcoholism, sexually transmitted diseases (which in some ethnic regions 1,5-5,5 times are above the average index for Russia) . Most of these diseases belong to the category of socially important pathology and reveal the problems of providing living conditions and medical care in these regions. We may suggest that despite of negative trends in health loss in Siberian population it is possible to preserve biological (genetic) stability of the new

  16. Unique Locality of Wooly Rhinoceros in Arctic Siberia

    NASA Astrophysics Data System (ADS)

    Davydov, S.; Sher, A.; Boeskorov, G.; Lazarev, P.; Binladen, J.; Willerslev, E.; Tikhonov, A.

    2009-12-01

    A permafrost goldfield area in northeastern Yakutia, Russia turns out to be the richest locality of extinct woolly rhinoceros in the world. It has yielded fossil horns of about 50 rhino individuals, and recently the most complete mummified body of this extinct giant. The age of fossils is about 40-50 thousand years before present, but permafrost helped to preserve them in perfect condition. The fossils, and especially mummies, present a perfect material for genetic studies. Woolly rhinoceros, Coelodonta antiquitatis (Blum.), is one of the symbols of the Ice Age and one of few large mammal species that disappeared from Eurasia about 14 000 years ago. Recently, a substantially complete mummy of woolly rhinoceros was found in permafrost at the Rodinka site near Cherskiy, northeastern Yakutia, Russia (68.76°N, 161.63°E). It is the body of an adult female, weighing almost 900 kg, with the preserved skull, two horns, lower jaw, one ear, and tail. The length of the carcass is about 2 m, the live length of the animal is estimated as more than 3 m. The right legs are partly preserved and the chest and belly cavities are partly empty; almost all hair has been lost. Despite these defects, it is the most complete mummy of woolly rhino ever found in permafrost. A fragment of rib from the body has been AMS dated to 39140±390 BP (OxA-18755). In recent years the Rodinka site has yielded an unprecedented number of woolly rhino fossils and is so far the richest locality for this extinct species. The woolly rhino had a very wide distribution in the Late Pleistocene - from France to the Bering Strait and from China to the high-arctic islands. It was perfectly adapted to the variety of severe periglacial (tundra-steppe) environments. Intriguingly, it was the only large Siberian mammal that never crossed the Bering Land Bridge to Alaska. In the vast lowlands of Arctic Siberia Coelodonta fossils are common, but much less abundant (below 1%) compared to those of other large Ice Age

  17. Extensive Burn Scars in Russia's Amur Region

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Vast areas of southeastern Russia have been scorched by fires over the last few weeks. All across Siberia fires have been raging, and this Moderate Resolution Imaging Spectroradiometer (MODIS) image from May 15, 2002, shows extensive, dark burn scars along with actively burning fires (red dots) on the north side of the Amur River, which separates Russia (north) and China (south). The southern Amur region is largely devoted to farming and other agriculture, and these fires may have been set intentionally to prepare the land for the growing season. Fire is often used to clear land of unwanted vegetation, and to return the nutrients stored in vegetation back to the soil. However, fires that are too frequent or severe can devastate the soil, eventually making it unsuitable for farming or grazing. Fires can also escape control and spread into protected areas. In this image, fires are mostly concentrated in a lowland area within the drainage basin of the Zeya River, which drains from the frozen lake at the top of the image. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC

  18. Conifer Decline and Mortality in Siberia

    NASA Astrophysics Data System (ADS)

    Kharuk, V.; Im, S.; Ranson, K.

    2015-12-01

    "Dark needle conifer" (DNC: Abies sibirica, Pinus sibirica and Picea obovata) decline and mortality increase were documented in Russia during recent decades. Here we analyzed causes and scale of Siberian pine and fir mortality in Altai-Sayan and Baikal Lake Regions and West Siberian Plane based on in situdata and remote sensing (QuickBird, Landsat, GRACE). Geographically, mortality began on the margins of the DNC range (i.e., within the forest-steppe and conifer-broadleaf ecotones) and on terrain features with maximal water stress risk (narrow-shaped hilltops, convex steep south facing slopes, shallow well-drained soils). Within ridges, mortality occurred mainly along mountain passes, where stands faced drying winds. Regularly mortality was observed to decrease with elevation increase with the exception of Baikal Lake Mountains, where it was minimal near the lake shore and increased with elevation (up to about 1000 m a.s.l.). Siberian pine and fir mortality followed a drying trend with consecutive droughts since the 1980s. Dendrochronology analysis showed that mortality was correlated with vapor pressure deficit increase, drought index, soil moisture decrease and occurrence of late frosts. In Baikal region Siberian pine mortality correlated with Baikal watershed meteorological variables. An impact of previous year climate conditions on the current growth was found (r2 = 0.6). Thus, water-stressed trees became sensitive to bark beetles and fungi impact (including Polygraphus proximus and Heterobasidion annosum). At present, an increase in mortality is observed within the majority of DNC range. Results obtained also showed a primary role of water stress in that phenomenon with a secondary role of bark beetles and fungi attacks. In future climate with increased drought severity and frequency Siberian pine and fir will partly disappear from its current range, and will be substituted by drought-tolerant species (e.g., Pinus silvestris, Larix sibirica).

  19. Family business in Russia: the path to middle class?

    PubMed

    Barkhatova, N; McMylor, P; Mellor, R

    2001-06-01

    The paper seeks to explore via a series of interview-based case studies aspects of the emergence of an entrepreneurial middle-class in Russia. The paper notes the origins of those studied in the professional or highly skilled workers in the former Soviet Union. The paper reveals the complexity and fragility of the circumstances of these entrepreneurs and suggests that commentary in both Russia and the West that pins its hopes for social stability on the emergence of a new property owning middle class in Russia are, at best, premature.

  20. Siberia Integrated Regional Study megaproject: challenges, approaches and first results

    NASA Astrophysics Data System (ADS)

    Gordov, Evgeny; Vaganov, Evgeny

    2010-05-01

    -going changes of regional climatic characteristics including those, which control vegetation dynamics. In particular,it is shown that fields of long-term temperature trends have inhomogeneous structure. One can separate regions with maximum warming rates, which are located mostly in East Siberia. Spatial distribution of seasonally mean temperature changes is specific for seasons. Winter and spring seasons made the main contribution to climate warming. However, autumn became more cool at the vast territories in the north of West and East Siberia. In general, changes are within range -0.5°С to +0.5°С every 10 years. Currently, efforts of the community involved are concentrated on issues related to regional and global risks rising with regional environment changes. There are three main scientific problems, whose solution is very important for understanding potential change of the whole Earth System dynamics and has strong regional socio-economical impact: Permafrost fate, especially its border shift, which seriously threats to infrastructure and might form significant carbon source; Desert - steppe- forest-tundra ecosystems borders shifts to North, which might change region input into global carbon cycle as well as provoke serious socio-economical consequences for local population; and Temperature/precipitation/hydrology regime change, which might increase risks of forest and peat fires thus increasing significantly carbon release from the region under study.

  1. Crisis and Response: The Emergence of Modern Jewish Politics in Russia.

    ERIC Educational Resources Information Center

    Ritterband, Paul

    This collection of documents examines the response of the Jewish people--primarily in Russia but also in the West--to the sociological and political crises of Tsarist Russia between the years 1800 and 1914. It emphasizes in particular the emergence and interaction of the two ideologies which formulated the most radical solutions to the Jewish…

  2. Investigation of ancient DNA from Western Siberia and the Sargat culture.

    PubMed

    Bennett, Casey C; Kaestle, Frederika A

    2010-04-01

    Mitochondrial DNA from 14 archaeological samples at the Ural State University in Yekaterinburg, Russia, was extracted to test the feasibility of ancient DNA work on their collection. These samples come from a number of sites that fall into two groupings. Seven samples are from three sites, dating to the 8th-12th century AD, that belong to a northern group of what are thought to be Ugrians, who lived along the Ural Mountains in northwestern Siberia. The remaining seven samples are from two sites that belong to a southern group representing the Sargat culture, dating between roughly the 5th century BC and the 5th century AD, from southwestern Siberia near the Ural Mountains and the present-day Kazakhstan border. The samples are derived from several burial types, including kurgan burials. They also represent a number of different skeletal elements and a range of observed preservation. The northern sites repeatedly failed to amplify after multiple extraction and amplification attempts, but the samples from the southern sites were successfully extracted and amplified. The sequences obtained from the southern sites support the hypothesis that the Sargat culture was a potential zone of intermixture between native Ugrian and/or Siberian populations and steppe peoples from the south, possibly early Iranian or Indo-Iranian, which has been previously suggested by archaeological analysis.

  3. Multi-Sensor Remote Sensing of Forest Dynamics in Central Siberia

    NASA Technical Reports Server (NTRS)

    Ransom, K. J.; Sun, G.; Kharuk, V. I.; Howl, J.

    2011-01-01

    The forested regions of Siberia, Russia are vast and contain about a quarter of the world's forests that have not experienced harvesting. However, many Siberian forests are facing twin pressures of rapidly changing climate and increasing timber harvest activity. Monitoring the dynamics and mapping the structural parameters of the forest is important for understanding the causes and consequences of changes observed in these areas. Because of the inaccessibility and large extent of this forest, remote sensing data can play an important role for observing forest state and change. In Central Siberia, multi-sensor remote sensing data have been used to monitor forest disturbances and to map above-ground biomass from the Sayan Mountains in the south to the taiga-tundra boundaries in the north. Radar images from the Shuttle Imaging Radar-C (SIR-C)/XSAR mission were used for forest biomass estimation in the Sayan Mountains. Radar images from the Japanese Earth Resources Satellite-1 (JERS-1), European Remote Sensing Satellite-1 (ERS-1) and Canada's RADARSAT-1, and data from ETM+ on-board Landsat-7 were used to characterize forest disturbances from logging, fire, and insect damage in Boguchany and Priangare areas.

  4. The perils and pitfalls of business in Russia

    SciTech Connect

    Spears, R.B.

    1995-09-01

    It is not for the lack of trying that few Western oil companies have profitable operations in Russia. Quite the contrary. Every oil company with a thirst for opportunity has searched that once-forbidden region for deals. This gold rush was triggered by an apparent crying need or Western know-how and capital, but appearances in Russia often widely differ from reality. Hype of early oil ventures set a false tone of promise, but company and company came home poorer and wiser. The gold rush went bust. Now in the fourth year of the West`s involvement in Russia`s oilfields, operators are soberly evaluating their prospects. Even while signals are encouraging the West, like a reduction in export tariffs and some progress on contract law, a remarkable event is occuring that throws out many Western arguments for continuing involvement and investment: On their own, the Russians are arresting their production decline and have increased output. This will have immediate and long term effects on Westerners. First, it lends credibility to Russian voices demanding that Mother Russia not sign away its precious resources to foreigners. Second, it encourages trade barriers to protect domestic industry. Third, it weakens the bargaining position of Westerners. Fourth, it reduces the options available to Western operators. What remains will be E&P opportunities where Western technology and capital really can play a role-complex reservoirs, hostile environments-but poor contract terms.

  5. Planned LLR station in Russia and its impact on the lunar ephemeris accuracy

    NASA Astrophysics Data System (ADS)

    Vasilyev, M.; Yagudina, E.; Torre, J.-M.; Feraudy, D.

    2015-08-01

    Precise modern Lunar Ephemerides (DE/LE, USA; INPOP series, France and EPM-ERA IAA, Russia) are based only on LLR (Lunar Laser Ranging) observations obtained at sixth LLR ground stations during 1969-2013 years. At present there are only four stations active: Grasse (Cerga), McDonald, Apache Point (Apollo) and Matera (Italy). To improve the accuracy of lunar ephemerides the new stations are necessary. Now exist two projects of new LLR stations: Altay (Russia) and Hartebeesthoek in South Africa (1m telescope). La Silla (Chilli) station is very promising but now only under theoretical consideration. In the paper, the impact of a installation of new LLR device on the 3.12 m telescope at Altay station Siberia, Russia is considered. To check the actuality of the project it should be shown, in particular, that the accuracy of the lunar ephemeris will visibly increase. The only way to prove that fact now is the numerical simulation.

  6. High-Resolution Regional Biomass Map of Siberia from Glas, Palsar L-Band Radar and Landsat Vcf Data

    NASA Astrophysics Data System (ADS)

    Sun, G.; Ranson, K.; Montesano, P.; Zhang, Z.; Kharuk, V.

    2015-12-01

    The Arctic-Boreal zone is known be warming at an accelerated rate relative to other biomes. The taiga or boreal forest covers over 16 x106 km2 of Arctic North America, Scandinavia, and Eurasia. A large part of the northern Boreal forests are in Russia's Siberia, as area with recent accelerated climate warming. During the last two decades we have been working on characterization of boreal forests in north-central Siberia using field and satellite measurements. We have published results of circumpolar biomass using field plots, airborne (PALS, ACTM) and spaceborne (GLAS) lidar data with ASTER DEM, LANDSAT and MODIS land cover classification, MODIS burned area and WWF's ecoregion map. Researchers from ESA and Russia have also been working on biomass (or growing stock) mapping in Siberia. For example, they developed a pan-boreal growing stock volume map at 1-kilometer scale using hyper-temporal ENVISAT ASAR ScanSAR backscatter data. Using the annual PALSAR mosaics from 2007 to 2010 growing stock volume maps were retrieved based on a supervised random forest regression approach. This method is being used in the ESA/Russia ZAPAS project for Central Siberia Biomass mapping. Spatially specific biomass maps of this region at higher resolution are desired for carbon cycle and climate change studies. In this study, our work focused on improving resolution ( 50 m) of a biomass map based on PALSAR L-band data and Landsat Vegetation Canopy Fraction products. GLAS data were carefully processed and screened using land cover classification, local slope, and acquisition dates. The biomass at remaining footprints was estimated using a model developed from field measurements at GLAS footprints. The GLAS biomass samples were then aggregated into 1 Mg/ha bins of biomass and mean VCF and PALSAR backscatter and textures were calculated for each of these biomass bins. The resulted biomass/signature data was used to train a random forest model for biomass mapping of entire region from 50o

  7. [Early encounters of German-language explorers with the Tibetan medicine in Siberia in the modern era].

    PubMed

    Surkova, Natalia; Chekhirova, Galina V; Aseeva, Tamara; Nikolaev, Sergey; Agalzew, Grigori; Melzer, Jörg; Vennos, Cécile; Schwabl, Herbert; Saller, Reinhard

    2012-01-01

    The spreading of Tibetan Buddhism and with it the Tibetan medicine in the region east of Lake Baikal, goes back to the 17th century. At the beginning of the 18th century, German speaking scholars were among the first to undertake scientific expeditions through Siberia. As such they were amongst the first scientists of the modern era who encountered the traditions, concepts, and therapeutic methods of Tibetan medicine. The aim of this article is to describe and analyze these first encounters with Tibetan medicine by the example of selected men of science of the 18th and 19th century. This work is based on extensive studies of sources in archives and libraries in Russia and Switzerland. We found documents related to the following scientists: Daniel Gottlieb Messerschmidt (1685-1735), Johann Georg Gmelin (1709-1755), Erik Laxmann (1737-1796), Friedrich Adelung (1768-1843), and Joseph Rehmann (1779-1831). They mentioned the distribution of Tibetan medicine within Russia, the use of medicinal plants and formulas as well as therapeutic techniques. For the scientific community of the time these first encounters of Europeans with practitioners of Tibetan medicine could not lift Tibetan medicine out of other exotic context in the field of ethnography. For today's researchers, these encounters are an important evidence for more than 300 years of development of Tibetan medicine on the vast territory of Siberia. The practice and the scientific examination of Tibetan medicine in Siberia is an active endeavor until today. The present work shows that it is possible and rewarding to follow up the historic and cultural connections from Europe to Asia via the Siberian link.

  8. Information Needs Research in Russia and Lithuania, 1965-2003

    ERIC Educational Resources Information Center

    Maceviciute, Elena

    2006-01-01

    Introduction: The invisibility of research on information needs from the East and Central Europe in the West suggested an exploration of the published research output from Lithuania and Russia from 1965 to 2003. Method: The data were collected from the abstracting journal Informatika-59. The publications were retrieved from Lithuanian and Russian…

  9. Systematics and biology of some species of Micrurapteryx Spuler (Lepidoptera, Gracillariidae) from the Holarctic Region, with re-description of M. caraganella (Hering) from Siberia.

    PubMed

    Kirichenko, Natalia; Triberti, Paolo; Mutanen, Marko; Magnoux, Emmanuelle; Landry, Jean-François; Lopez-Vaamonde, Carlos

    2016-01-01

    During a DNA barcoding campaign of leaf-mining insects from Siberia, a genetically divergent lineage of a gracillariid belonging to the genus Micrurapteryx was discovered, whose larvae developed on Caragana Fabr. and Medicago L. (Fabaceae). Specimens from Siberia showed similar external morphology to the Palearctic Micrurapteryx gradatella and the Nearctic Parectopa occulta but differed in male genitalia, DNA barcodes, and nuclear genes histone H3 and 28S. Members of this lineage are re-described here as Micrurapteryx caraganella (Hering, 1957), comb. n., an available name published with only a brief description of its larva and leaf mine. Micrurapteryx caraganella is widely distributed throughout Siberia, from Tyumen oblast in the West to Transbaikalia in the East. Occasionally it may severely affect its main host, Caragana arborescens Lam. This species has been confused in the past with Micrurapteryx gradatella in Siberia, but field observations confirm that Micrurapteryx gradatella exists in Siberia and is sympatric with Micrurapteryx caraganella, at least in the Krasnoyarsk region, where it feeds on different host plants (Vicia amoena Fisch. and Vicia sp.). In addition, based on both morphological and molecular evidence as well as examination of type specimens, the North American Parectopa occulta Braun, 1922 and Parectopa albicostella Braun, 1925 are transferred to Micrurapteryx as Micrurapteryx occulta (Braun, 1922), comb. n. with albicostella as its junior synonym (syn. n.). Characters used to distinguish Micrurapteryx from Parectopa are presented and illustrated. These findings provide another example of the potential of DNA barcoding to reveal overlooked species and illuminate nomenclatural problems.

  10. Fire Emissions Estimates in Siberia: Evaluation of Uncertainties in Area Burned, Land Cover, and Fuel Consumption

    NASA Astrophysics Data System (ADS)

    Kukavskaya, E.; Soja, A. J.; Ivanova, G. A.; Petkov, A.; Ponomarev, E. I.; Conard, S. G.

    2012-12-01

    Wildfire is one of the main disturbance factors in the boreal zone of Russia. Fires in the Russian boreal forest range from low-severity surface fires to high-severity crown fires. Estimates of carbon emissions from fires in Russia vary substantially due to differences in ecosystem classification and mapping, burned area calculations, and estimates of fuel consumption. We examined uncertainties in different parameters used to estimate biomass burning emissions. Several fire datasets (Institute of Forest burned area product, MCD45, MCD64, MOD14/MYD14, official data) were compared to estimate uncertainties in area burned in Siberia. Area burned was found to differ significantly by data source, with satellite data being by an order of magnitude greater than ground-based data. Differences between mapped ecosystems were also compared and contrasted on the basis of five land cover maps (GLC-2000, Globcover-2009, MODIS Collection 4 and 5 Global Land Cover, and the Digitized Ecosystem map of the Former Soviet Union) to evaluate the potential for error resulting from disparate vegetation structure and fuel consumption estimates. The examination of land cover maps showed that estimates of relative proportion of fire by ecosystem type varied substantially for the same year from map to map. Fuel consumption remains one of the main uncertainties in estimates of biomass burning emissions in Siberia. Accurate fuel consumption estimates are obtained in the course of fire experiments with pre- and post-fire biomass measuring. Our large-scale experiments carried out in the course of the FIRE BEAR (Fire Effects in the Boreal Eurasia Region) Project provided quantitative and qualitative data on ecosystem state and carbon emissions due to fires of known behavior in major forest types of Siberia that could be used to verify large-scale carbon emissions estimates. Global climate change is expected to result in increase of fire hazard and area burned, leading to impacts on global air

  11. Wetland classification based on Landsat and its application for methane emission inventory of West Siberian taiga zone

    NASA Astrophysics Data System (ADS)

    Kleptsova, Irina; Maksyutov, Shamil; Glagolev, Mikhail

    2013-04-01

    emission. Lakes are widespread over taiga mire systems occupying 16% of the territory and contributing 15% of CH4 flux to the atmosphere. The rest of the territory is mainly occupied by fens, poor fens and swamps (13%) contributing 33% of the total CH4 flux. Applying the new map resulted in total methane emissions from taiga zone of 3.53 TgC/yr which is 87% higher than the former estimates by Glagolev et al. (2011). This considerable revision is caused by the changes in fractional coverages of methane emitting landscapes. Glagolev M, Kleptsova I, Filippov I, Maksyutov S, Machida T. 2011. Regional methane emission from West Siberia mire landscapes. ERL 6 045214. doi: 10.1088/1748-9326/6/4/045214 Romanova EA, Bybina RT , Golitsyna EF , Ivanova GM , Usova LI, Trushnikova LG. 1977. Wetland typology map of West Siberian lowland scale 1:2500 000 GUGK: Leningrad, Russia

  12. Long-Term Measurements of Carbon Monoxide and Aerosols at the ZOTTO tall tower, Siberia

    NASA Astrophysics Data System (ADS)

    Andreae, M. O.; Birmili, W.; Chi, X.; Heimann, M.; Heintzenberg, J.; Mikhailov, E.; Panov, A.

    2012-04-01

    The Zotino Tall Tower Observatory (ZOTTO), operated by the Max Planck Institutes for Biogeochemistry and Chemistry and the Institute of Forest (Krasnoyarsk), is located at 89.35°E, 60.80°N, 114 m asl. at a very remote continental site in Siberia, Russia. It centers on a 300-m tower designed for scientific measurements of chemical (trace gases, aerosol) and physical (meteorological) properties. The instrumentation at the observatory includes a CO Monitor, a Particle Soot Absorption Photometer (PSAP) for determining the aerosol absorption coefficient, a nephelometer for the determination of the aerosol scattering coefficient, and a Differential Mobility Particle Sizer (DMPS) to measure the aerosol number size distribution. We present measurements made from October 2006 until March 2011, with some interruptions due to technical reasons. An annual cycle of the background CO mixing rations was observed with summer minima around 90 ppb and winter maxima of about 175 ppb. Amplitude and phase of the annual cycle were generally similar to that reported by NOAA-ESRL for latitude 61°N, but showed an earlier onset of the elevated winter values. Episodes of elevated CO and aerosol concentrations, typically lasting for several days, are superimposed on the background seasonal cycle. During winter, these pollution episodes are usually associated with air masses that have passed over the central Siberian region around Omsk and Novosibirsk - a heavily industrialized area. During spring and summer, elevated levels of CO and aerosols are often caused by agricultural fires in southern Siberia and Kazakhstan or by forest fires in boreal Siberia. The optical properties of the aerosol showed more pronounced seasonal variability than the aerosol mass and number concentrations. Wintertime aerosols were highly absorbing, with single scattering albedos (SSA) around 0.85, consistent with a dominant fossil fuel combustion source. In contrast, summertime aerosols had very low absorption

  13. First genetic characterization of rotavirus C in Russia.

    PubMed

    Zhirakovskaia, Elena; Tikunov, Artem; Klemesheva, Vera; Loginovskikh, Natalia; Netesov, Sergey; Tikunova, Nina

    2016-04-01

    Rotaviruses C (RVC) cause sporadic cases and outbreaks of diarrhea in humans and animals worldwide. The aim of this study was to monitor RVC during a surveillance study of sporadic cases of viral gastroenteritis in the Novosibirsk and Omsk regions of Russia from 2006 to 2011. A total of 2144 stool samples from children and adults hospitalized with acute gastroenteritis were tested for RVC by RT-PCR. Sixteen RVC-positive stool samples were detected at a rate of 0.6% (13/2037) in children and 2.8% (3/107) in adults. The low detection rate suggested that RVC infection was an uncommon cause of hospitalization in Russia. The complete VP7, VP4, VP6, and NSP4 gene sequences were determined. It was found that RVCs with at least two different genome backgrounds circulated in Siberia. VP4, VP6, and NSP4 gene sequences of most Russian RVC strains clustered with South Asian strains, while the VP7 gene showed a closer relationship to European strains. Meanwhile, only VP4 and NSP4 sequences of the strain Omsk08-386 clustered with South Asian strains, while its VP6 and VP7 sequences clustered with European strains. This is the first genetic characterization of Russian RVC strains and the first report on the prevalence of RVC in the Asian part of Russia.

  14. Promoting sustainable energy strategies in Russia

    SciTech Connect

    Watson, R.K.

    1995-12-31

    Enormous structural changes are taking place in the economy of Russia. It is important that vital sectors of the economy undergo a smooth transition from a centrally-planned paradigm to a more market-oriented structure. Introducing market-oriented-institutional structures and energy planning approaches to Russian utilities can facilitate the transition to the market and allow them to become vehicles for change rather than mere witnesses. As real electricity prices increase relative to other prices, a significant industrial restructuring can be expected, with an accompanying reduction of energy consumption. By developing programs to help industry become more energy-efficiency, the electricity sector can play a central role in Russia`s economic recovery. A robust energy sector will be in a much better position to lead other sectors of the economy toward market-oriented solutions to the present economic crisis. Because of the magnitude of the task of recreating an economy for one of the world`s superpowers, institutional restructuring should take place incrementally. The transition of US utilities from a {open_quotes}build-and-grow{close_quotes} paradigm to one of Integrated Resource Planning (IRP) and subsequently to a hybrid of competition and IRP began and is continuing on the state and regional level. Local success stories on the West Coast and New England persuaded other states to adopt these methods. This strategy could also prove to be very effective in regions of Russia that are served by integrated electricity grids, such as the South Russia Power pool (Yuzhenergo) that serves the North Caucasus region. As the Russian energy system currently undergoes change, simultaneously privatizing and restructuring, these issues will be largely decided within the next two years. One of the greatest challenges involves implementing an environmentally sustainable strategy which ensures that energy efficiency and renewable energy are incorporated into the new structure.

  15. The Coast of Siberia: A Vladivostok Spring.

    ERIC Educational Resources Information Center

    Ronayne, Betty Lee

    This paper describes experiences of a reference librarian at California State University (Sacramento) who spent three weeks in Vladivostok (Russia) to assess the library and research needs of faculty and students at the Far Eastern State Technical University. After briefly describing the city of Vladivostok and its military role in the Soviet…

  16. White Sea - Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    At bottom center of this true-color Moderate Resolution Imaging Spectroradiometer (MODIS) image from April 13, 2001, the White Sea in western Russia is becoming free of ice in its southern extent. Meanwhile, the blue-green waters along the coast of the peninsula jutting out into the Barents Sea to the northeast could be due to a phytoplankton bloom.

  17. Home Education in Russia

    ERIC Educational Resources Information Center

    Staroverova, T. I.

    2011-01-01

    From the eighteenth through the early twentieth centuries, home education (home schooling) by tutors and governesses in Russia was a customary form of schooling for an overwhelming majority of members of the nobility. Social and political transformations of the twentieth century led to substantial changes as the state got actively involved with…

  18. Dating Violence in Russia

    ERIC Educational Resources Information Center

    Lysova, A. V.

    2007-01-01

    The phenomenon of violence in interpersonal relationships has been little studied in Russia, and the phenomenon of violence between dating partners has not been the object of scientific interest at all. The study on which the present article is based was designed to obtain information about the violence in dating among students enrolled in…

  19. Rehabilitation in Russia

    ERIC Educational Resources Information Center

    Martz, Erin

    2005-01-01

    For several decades, the disability community in Russia has battled for its rights. In 1995, a disability rights law was passed that covered multiple areas, such as environmental access, education, and work. This article focuses on Russian rehabilitation philosophy and practice. It is written from a mixture of perspectives?personal experience,…

  20. Russia: St. Petersburg

    Atmospheric Science Data Center

    2013-04-17

    ... 1703. This marshy, low-lying area possesses many rivers and islands, and about 300 bridges, of which more than twenty are drawbridges. The ... of the 20th century, Russia's westernmost border served as a barrier to international interaction, and the forests in this region were ...

  1. Ozone profile observations in Siberia in 2014

    NASA Astrophysics Data System (ADS)

    Dorokhov, Valery; Balugin, Nikolay; Yushkov, Vladimir; Makshtas, Alexander; Ivlev, Georgii; Shepelev, Dmitry; Nakajima, Hideaki

    2014-05-01

    The ozonesonde observations of atmospheric ozone profiles at Salekhard aerological station (66.5N, 66.7E) in Western Siberia, Russian Federation are carried out since January 1997. In 1997-2013 we used electrochemical 2Z-ECC ozonesondes for ozone profile observations in the winter-spring period to study the ozone loss in the Arctic regions. The results of ozonesonde observation at Salekhard station are in the NDACC database. In January 2014 we upgraded this ozonesounding station with the new iMet-1 radiosonde and electrochemical 2Z-V7 ozonesonde of Droplet Measurement Technologies (DMT), USA. The first results of ozonesonde profile measurements recorded in January-March 2014 at Salekhard aerological station will be presented and discussed.

  2. Dust pollution of snow cover in the industrial areas of Tomsk city (Western Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Talovskaya, A. V.; Filimonenko, E. A.; Osipova, N. A.; Yazikov, E. G.; Nadeina, L. V.

    2016-03-01

    This article describes the results of long-term monitoring (2007-2014) of snow cover pollution in the territory of Tomsk city. Snow samples were collected in the territory of Tomsk. Determination of dust load level was carried out by comparing with the background and reference values. It has been determined that the north-east and central parts of Tomsk are the most contaminated areas, where brickworks, coal and gas-fired thermal power plant are located. The analysis of long-term dynamics showed a dust load decrease in the vicinity of coal and gas-fired thermal power plant due to upgrading of the existing dust collecting systems. During the monitoring period the high dust load in the vicinity of brickworks did not change. The lowest value of the dust load on snow cover was detected in the vicinity of the petrochemical plant and concrete product plants. The near and far zones of dust load on snow cover were determined with the reference to the location of the studied plants.

  3. Waste management in the Irkutsk Region, Siberia, Russia: environmental assessment of current practice focusing on landfilling.

    PubMed

    Starostina, Vlada; Damgaard, Anders; Rechberger, Helmut; Christensen, Thomas H

    2014-05-01

    The municipal waste management system of the region of Irkutsk is described and a life cycle assessment (LCA) performed to assess the environmental performance of the system. Annually about 500 000 tons of waste are managed. The waste originates from three sources: household waste (27%), commercial waste (23%) and office & institutional waste (44%). Other waste of unknown composition constitutes 6%. Only 3% of the waste is recycled; 97% of the municipal waste is disposed of at the old Alexandrovsky landfill. The environmental impact from the current system is dominated by the landfill, which has no gas or leachate collection system. The global warming contribution is due to the emission of methane of the order of 420 000 tons CO2-equivalents per year. Collection and transport of the waste are insignificant compared with impacts from the landfill. As the old landfill runs out of capacity in a few years, the LCA modelling showed that introduction of a new and modern landfill with gas and leachate collection could improve the performance of the waste management system significantly. Collection of landfill gas and utilization for 30 years for electricity production (gas turbine) would reduce the global warming completely and result in a net saving of 100 000 CO2-equivalents per year due to storage of biogenic carbon in the landfill beyond 100 years. Considering other first-order degradation rates for the landfilled organic matter did not overtly affect the results, while assumptions about the top cover oxidation of methane significantly affected the results. This shows the importance of controlling the gas escape from the landfill.

  4. Temperature sensitivity of frozen peatland soils organic matter decomposition (North-Western Siberia, Nadym site, Russia)

    NASA Astrophysics Data System (ADS)

    Tarkhov, Matvey; Matyshak, George; Yakushev, Andrey; Bobrik, Ann

    2016-04-01

    Peatland soils play a considerable role in carbon cycle because of storing approximately 50% of total Earth's soils carbon. The steady temperature increase in arctic soils may cause a rapid organic matter decomposition in thawed layers - that will result in additional significant greenhouse gases emission (CO2, CH4). For further predictions improvement of soils response to global climate changes it is necessary to estimate the temperature sensitivity of soils organic matter decomposition. The purpose of the study was to estimate the response of frozen peatland soils organic matter to increase in the temperature of their functioning. The study object was frozen peatland soils of forest-tundra (the Tyumen region), developing under permafrost conditions. Weakly and medium decomposed moss peat samples were taken from different depths for laboratory studies and stored at 4 °C before the experiment started. At laboratory the response of CO2 efflux, basal respiration (BR) and soils enzymatic (esters) activity (SEA) to temperature increase was estimated. For 1.5 months one part of peat samples was subjected to sequential temperature increase from 4 to 25 °C and CO2 efflux was measured. Another part of the peat samples was simultaneously incubated at 4, 15 and 25 °C for 1-4 days for BR and SEA estimation. To identify the specifics of frozen peatland soils response the identical experiments were done with peat samples from southern taiga (the Moscow region). First results showed the contrast response of peatland soils from different ecosystems to temperature increase. For all studied soils the positive feedback to temperature increase was noticed, however the organic matter mineralization rate, estimated by CO2 efflux, differed a lot. The CO2 efflux values of forest-tundra samples were 3 times lower in comparison with southern taiga on average: the maximal difference was at 16-22 °C range. The microbial biomass activity, estimated by BR and SEA, also tended to increase with temperature for both peatland soils. The BR values of forest-tundra samples in comparison with southern taiga were 1.5 times lower on average, whereas SEA values caused the more significant difference: starting from 4 °C the forest-tundra samples SEA was presented by a factor of 100 lower values if compared with southern taiga samples. The temperature coefficient Q10, calculated on the basis of CO2 efflux values, revealed the maximal forest-tundra samples temperature sensitivity in «low» temperature range 4-13 °C (Q10=4,1). For the southern taiga samples only small Q10 variations (from 2.5 to 2.2) with increasing temperature were fixed. Thus, we have found that the contrasting temperature sensitivity results are related to peatland soils from different ecosystems. This fact must be considered when predicting the peatland soils response to changes in functioning conditions.

  5. Palaeoenvironmental dynamics inferred from late Quaternary permafrost deposits on Kurungnakh Island, Lena Delta, Northeast Siberia, Russia

    NASA Astrophysics Data System (ADS)

    Wetterich, Sebastian; Kuzmina, Svetlana; Andreev, Andrei A.; Kienast, Frank; Meyer, Hanno; Schirrmeister, Lutz; Kuznetsova, Tatyana; Sierralta, Melanie

    2008-08-01

    Late Quaternary palaeoenvironments of the Siberian Arctic were reconstructed by combining data from several fossil bioindicators (pollen, plant macro-fossils, ostracods, insects, and mammal bones) with sedimentological and cryolithological data from permafrost deposits. The record mirrors the environmental history of Beringia and covers glacial/interglacial and stadial/interstadial climate variations with a focus on the Middle Weichselian interstadial (50-32 kyr BP). The late Pleistocene to Holocene sequence on Kurungnakh Island reflects the development of periglacial landscapes under changing sedimentation regimes which were meandering fluvial during the Early Weichselian, colluvial or proluvial on gently inclined plaines during the Middle and Late Weichselian, and thermokarst-affected during the Holocene. Palaeoecological records indicate the existence of tundra-steppe vegetation under cold continental climate conditions during the Middle Weichselian interstadial. Due to sedimentation gaps in the sequence between 32 and 17 kyr BP and 17 and 8 kyr BP, the Late Weichselian stadial is incompletely represented in the studied outcrops. Nevertheless, by several palaeoecological indications arctic tundra-steppe vegetation under extremely cold-arid conditions prevailed during the late Pleistocene. The tundra-steppe disappeared completely due to lasting paludification during the Holocene. Initially subarctic shrub tundra formed, which later retreated in course of the late Holocene cooling.

  6. Flora from the Induan stage (Lower Triassic) of Middle Siberia

    NASA Astrophysics Data System (ADS)

    Mogucheva, N. K.

    2016-05-01

    The first data on the taxonomic composition of the Induan flora of Siberia are presented. The investigation of Triassic reference sections in northern Siberia (eastern Taimyr, Lena-Anabar Trough, Verkhoyansk region) and correlation with volcano-sedimentary complexes of the Tungus and Kuznetsk basins made it possible to establish for the first time the taxonomic composition of the flora from the Induan Stage of Siberia. Its composition is heterogeneous, forming two large plant formations, which occupied different ecological niches. On the eastern coastal-marine margins of Siberia (eastern Taimyr, Olenek coast, Verkhoyansk region), the Induan flora was largely characterized by lepidophytic ( Tomiostrobus) plants, while in the intracontinental areas (Tungus and Kuznetsk basins, partly Verkhoyansk region), it was characterized by Equisetales-Filicales communities.

  7. Russia`s atomic tsar: Viktor N. Mikhailov

    SciTech Connect

    Reams, C.A.

    1996-12-01

    Minatom (Ministry of Atomic Energy) was created to manage Russia`s nuclear weapons program in the age of disarmament. The ministry is responsible for the development, production, and maintenance of nuclear weapons, warhead dismantlement, the production of nuclear materials for weapons, the disposition of nuclear materials disassembled from warheads, the administration of Russia`s vast nuclear weapons complex, the development of policy for the future role of Russia`s nuclear complex and payment of employees entrusted with such tasks. Thus, Minatom is instrumental in the implementation of arms control, disarmament and nonproliferation agreements. The director of Minatom, Viktor N. Mikhailov, wields a great deal of power and influence over Russia`s nuclear infrastructure. He is an important player amidst efforts to reduce the threats posed by Russia`s decaying nuclear complex. There are certainly other personalities in the Russian government who influence Minatom; however, few affect the ministry as profoundly as Mikhailov. His ability to influence Russia`s nuclear complex has been clearly demonstrated by his policies in relation to the US purchase of Russian highly enriched uranium, the planned fissile material storage facility at Mayak, materials protection, control and accountability programs, and his unwavering determination to sell Iran commercial nuclear technology. Mikhailov has also been a key negotiator when dealing with the US on issues of transparency of weapons dismantlement and fissile material disposition, as well as the use of US threat reduction funds. His policies and concerns in these areas will affect the prospects for the successful negotiation and implementation of future nuclear threat reduction programs and agreements with Russia.

  8. Atmospheric CO2 and CH4 Measurement Network on Towers in Siberia

    NASA Astrophysics Data System (ADS)

    Shimoyama, K.; Machida, T.; Shinohara, A.; Maksyutov, S.; Arshinov, M.; Davydov, D.; Fofonov, A.; Krasnov, O.; Fedoseev, N.; Belan, B.; Belan, H.; Inoue, G.

    2006-12-01

    In order to estimate CO2 and CH4 fluxes at regional to sub-continental scale by an inverse model, a network of tall towers for atmospheric CO2 and CH4 measurements has been established over a region of thousand square kilometers in west Siberia. In-situ continuous measurements have been conducted at 6 stations: Berezorechka (56.17N, 84.33E) since 2002, Parabel (58.25N, 82.40E) and Igrim (63.20N, 64.48E) since 2004, Demyanskoe (59.78N, 70.87E) and Noyabrsk (63.43N, 76.76E) since 2005, and Yakutsk (62.83N, 129.35E) in east Siberia since 2005. Over next two years, installations of 4 more stations are planned. This study provides some results of observation from this network. Seasonal cycles of CO2 showed quite similar trends in growing season (May to September) among the west Siberian sites. The remarkable decrease of CO2 concentration occurred in early May and the seasonal minimum was observed between July and August. On the other hand, the short-term (from several days to week) variations in CO2 concentrations were quite different among the sites, particularly during the growing season. Rather large variation of more than 25 ppm within a week was observed during winter. The changes in CO2 concentrations at the nearby sites were almost identical. Monthly mean values of CO2 during the growing season were relatively higher at the northern sites than at southern sites. These observational results evidentially reflected the regional characteristics of CO2 flux variation, transportation, and mixing process. Daily cycles of CH4 in summer showed nocturnal increase and diurnal decrease which was due to emission of CH4 from wetland accumulated over night, and diurnal convective mixing. Relatively high concentrations of CH4 were observed in winter and summer. Because there is one of the world's vastest wetland in western Siberia, the peak of CH4 in summer implies the significant role of CH4 emissions from the west Siberian wetland to the atmosphere. On the other hand, an

  9. Confronting Russia, Again

    DTIC Science & Technology

    2009-04-01

    countercartel” composed of the EU, the United States, China, Japan, India, and South Korea under the supervison of the International Energy Agency (IEA...Russias rhetoric and campaign to expand its strategic influence are indicative of a perception by Moscow that its resurgence is a zero sum game vis-à-vis...the United States. Russian influence and power are the result of its asymmetric energy relationship with Europe and its position in international

  10. The Age of Dinosaurs in Russia and Mongolia

    NASA Astrophysics Data System (ADS)

    Benton, Michael J.; Shishkin, Mikhail A.; Unwin, David M.; Kurochkin, Evgenii N.

    2003-12-01

    The former Soviet Union covers a vast area of land, and over the last 200 years, many dozens of extraordinary dinosaurs and other fossil amphibians, reptiles, birds and mammals have been found in Mesozoic rocks in its territories. The Permo-Triassic of the Ural Mountains of Russia have produced hundreds of superb specimens, and many of the dinosaurs from Mongolia are unique. This is the first compilation in any Western language of this large body of Russian research and the first time so much of this research, previously unexplored by the West, has been introduced in English. The Age of Dinosaurs in Russia and Mongolia is written by a unique mix of Russian and Western palaeontologists, and provides an entrée to a range of fossil faunas, in particular reptiles, that have been little known outside Russia. It will undoubtedly become a major reference work for all vertebrate palaeontologists.

  11. An annotated catalogue of the gamasid mites associated with small mammals in Asiatic Russia. The family Laelapidae s. str. (Acari: Mesostigmata: Gamasina).

    PubMed

    Vinarski, Maxim V; Korallo-Vinarskaya, Natalia P

    2016-05-16

    Twenty-nine species of mites of the family Laelapidae s. str. have been recorded as associated with small mammals (rodents, insectivores) in Asiatic Russia (Siberia and the Russian Far East). These species belong to two subfamilies (Laelapinae, Myonyssinae) and six genera: Androlaelaps Berlese, 1903, Dipolaelaps Zemskaya & Piontkovskaya, 1960, Laelaps C.L. Koch, 1836, Hyperlaelaps Zakhvatkin, 1948, Myonyssus Tiraboschi, 1904, Oryctolaelaps Lange, 1955. A list of the species, with data on synonymy, geographic ranges, and relationships with mammal hosts is provided. Some considerations concerning patterns of distribution of the parasitic Laelaptidae of Asiatic Russia are presented as well as their classifications from the point of view of known host association records.

  12. Fuel Consumption and Fire Emissions Estimates in Siberia: Impact of Vegetation Types, Meteorological Conditions, Forestry Practices and Fire Regimes

    NASA Astrophysics Data System (ADS)

    Kukavskaya, Elena; Conard, Susan; Ivanova, Galina; Buryak, Ludmila; Soja, Amber; Zhila, Sergey

    2015-04-01

    Boreal forests play a crucial role in carbon budgets with Siberian carbon fluxes and pools making a major contribution to the regional and global carbon cycle. Wildfire is the main ecological disturbance in Siberia that leads to changes in forest species composition and structure and in carbon storage, as well as direct emissions of greenhouse gases and aerosols to the atmosphere. At present, the global scientific community is highly interested in quantitative and accurate estimates of fire emissions. Little research on wildland fuel consumption and carbon emission estimates has been carried out in Russia until recently. From 2000 to 2007 we conducted a series of experimental fires of varying fireline intensity in light-coniferous forest of central Siberia to obtain quantitative and qualitative data on fire behavior and carbon emissions due to fires of known behavior. From 2009 to 2013 we examined a number of burned logged areas to assess the potential impact of forest practices on fire emissions. In 2013-2014 burned areas in dark-coniferous and deciduous forests were examined to determine fuel consumption and carbon emissions. We have combined and analyzed the scarce data available in the literature with data obtained in the course of our long-term research to determine the impact of various factors on fuel consumption and to develop models of carbon emissions for different ecosystems of Siberia. Carbon emissions varied drastically (from 0.5 to 40.9 tC/ha) as a function of vegetation type, weather conditions, anthropogenic effects and fire behavior characteristics and periodicity. Our study provides a basis for better understanding of the feedbacks between wildland fire emissions and changing anthropogenic disturbance patterns and climate. The data obtained could be used by air quality agencies to calculate local emissions and by managers to develop strategies to mitigate negative smoke impacts on the environmentand human health.

  13. Systenostrema alba Larsson 1988 (Microsporidia, Thelohaniidae) in the Dragonfly Aeshna viridis (Odonata, Aeshnidae) from South Siberia: morphology and molecular characterization.

    PubMed

    Sokolova, Yuliya Y; Kryukova, Nataliya A; Glupov, Viktor V; Fuxa, James R

    2006-01-01

    An octospore microsporidium was found in the nymphs of Aeshna viridis, collected in intermittent streams near Novosibirsk, Siberia, Russia in 2003. Spores were uninucleate and measured 6.1+/-0.07 x 3.0+/-0.04 microm on fresh smears. The polar filament was anisofilar having 10-11 anterior coils (thicker filament diam.) and 10-11 posterior (thinner filament diam.) coils. Sporophorous vesicles were persistent and measured 12.3+/-0.23 x 11.9+/-0.20 microm. The infection was restricted to the adipose tissue and caused the formation of whitish "cysts" containing mature octospores. Based on ultrastructural similarity we consider this Siberian isolate to be Systenostrema alba, a species described from Aeshna grandis collected in Sweden (Larsson 1988). Maximum likelihood, neighbor joining, and maximum parsimony analyses of the small subunit rDNA all placed Systenostrema alba (Accession no. AY953292) as the sister taxon to a clade consisting of Thelohania solenopsae, Tubulinosema ratisbonensis, and Tubulinosema acridophagus.

  14. Birch Stands Growth Increase in Western Siberia

    NASA Technical Reports Server (NTRS)

    Kharuk, Viacheslav I.; Kuzmichev, Valeriy V.; Im, Sergey T.; Ranson, Kenneth J.

    2014-01-01

    Birch (Betula pendula Roth) growth within the Western Siberia forest-steppe was analyzed based on long-term (1897-2006) inventory data (height, diameter at breast height [dbh], and stand volume). Analysis of biometry parameters showed increased growth at the beginning of twenty-first century compared to similar stands (stands age = 40-60 years) at the end of nineteenth century. Mean height, dbh, and stem volume increased from 14 to 20 m, from 16 to 22 cm, and from approx. 63 to approx. 220 cu m/ha, respectively. Significant correlations were found between the stands mean height, dbh, and volume on the one hand, and vegetation period length (r(sub s) = 0.71 to 0.74), atmospheric CO2 concentration (r(sub s) = 0.71 to 0.76), and drought index (Standardized Precipitation-Evapotranspiration Index, r(sub s) = -0.33 to -0.51) on the other hand. The results obtained have revealed apparent climate-induced impacts (e.g. increase of vegetation period length and birch habitat drying due to drought increase) on the stands growth. Along with this, a high correlation of birch biometric parameters and [CO2] in ambient air indicated an effect of CO2 fertilization. Meanwhile, further drought increase may switch birch stand growth into decline and greater mortality as has already been observed within the Trans-Baikal forest-steppe ecotone.

  15. Thermal Properties of West Siberian Sediments in Application to Basin and Petroleum Systems Modeling

    NASA Astrophysics Data System (ADS)

    Romushkevich, Raisa; Popov, Evgeny; Popov, Yury; Chekhonin, Evgeny; Myasnikov, Artem; Kazak, Andrey; Belenkaya, Irina; Zagranovskaya, Dzhuliya

    2016-04-01

    Quality of heat flow and rock thermal property data is the crucial question in basin and petroleum system modeling. A number of significant deviations in thermal conductivity values were observed during our integral geothermal study of West Siberian platform reporting that the corrections should be carried out in basin models. The experimental data including thermal anisotropy and heterogeneity measurements were obtained along of more than 15 000 core samples and about 4 500 core plugs. The measurements were performed in 1993-2015 with the optical scanning technique within the Continental Super-Deep Drilling Program (Russia) for scientific super-deep well Tyumenskaya SG-6, parametric super-deep well Yen-Yakhinskaya, and deep well Yarudeyskaya-38 as well as for 13 oil and gas fields in the West Siberia. Variations of the thermal conductivity tensor components in parallel and perpendicular direction to the layer stratification (assessed for 2D anisotropy model of the rock studied), volumetric heat capacity and thermal anisotropy coefficient values and average values of the thermal properties were the subject of statistical analysis for the uppermost deposits aged by: T3-J2 (200-165 Ma); J2-J3 (165-150 Ma); J3 (150-145 Ma); K1 (145-136 Ma); K1 (136-125 Ma); K1-K2 (125-94 Ma); K2-Pg+Ng+Q (94-0 Ma). Uncertainties caused by deviations of thermal conductivity data from its average values were found to be as high as 45 % leading to unexpected errors in the basin heat flow determinations. Also, the essential spatial-temporal variations in the thermal rock properties in the study area is proposed to be taken into account in thermo-hydrodynamic modeling of hydrocarbon recovery with thermal methods. The research work was done with financial support of the Russian Ministry of Education and Science (unique identification number RFMEFI58114X0008).

  16. Biosensor development in Russia.

    PubMed

    Reshetilov, Anatoly N

    2007-07-01

    The review summarizes the current Russian research in the field of biological sensors for detection of carbohydrates, alcohols, medicines, enzyme inhibitors, toxicants, heavy metal ions, as well as viruses and microbial cells. Some of the presented works describe the analytical parameters of biosensors; other publications provide a basis for their development. The review covers mainly publications that have appeared over the past 10 years. As a whole, the collected material gives an idea of the main tendencies of biosensor development in Russia. The review is not meant to be comprehensive but highlights the major trends in this field in the last decade.

  17. Academic medicine in Russia.

    PubMed

    Burger, Edward J; Ziganshina, Lilia; Ziganshin, Airat U

    2004-12-01

    Academic medicine, along with professionalism of the medical community in Russia underwent a remarkable evolution from the Revolution through the decline of the Soviet Union. The Soviet period brought about an enormous expansion of numbers of admissions to medical schools and a corresponding increase in the number of new physicians. Academic medical institutions were separated from institutions of higher learning in general and medical science was separated from the mainstream of science. Many of these features have been reversed in the past 14 years and re-professionalization of medicine has resumed.

  18. Shiveluch Volcano, Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2001-01-01

    On the night of June 4, 2001, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) captured this thermal image of the erupting Shiveluch volcano. Located on Russia's Kamchatka Peninsula, Shiveluch rises to an altitude of 2,447 meters (8,028 feet). The active lava dome complex is seen as a bright (hot) area on the summit of the volcano. To the southwest, a second hot area is either a debris avalanche or hot ash deposit. Trailing to the west is a 25-kilometer (15-mile) ash plume, seen as a cold 'cloud' streaming from the summit. At least 60 large eruptions have occurred here during the last 10,000 years; the largest historical eruptions were in 1854 and 1964.

    Because Kamchatka is located along the major aircraft routes between North America/Europe and Asia, this area is constantly monitored for potential ash hazards to aircraft. The area is part of the 'Ring of Fire,' a string of volcanoes that encircles the Pacific Ocean.

    The lower image is the same as the upper, except it has been color-coded: red is hot, light greens to dark green are progressively colder, and gray/black are the coldest areas.

    The image is located at 56.7 degrees north latitude, 161.3 degrees east longitude.

    ASTER is one of five Earth-observing instruments launched Dec. 18, 1999, on NASA's Terra satellite. The instrument was built by Japan's Ministry of International Trade and Industry. A joint U.S./Japan science team is responsible for validation and calibration of the instrument and the data products. The primary goal of the ASTER mission is to obtain high-resolution image data in 14 channels over the entire land surface, as well as black and white stereo images. With revisit time of between 4 and 16 days, ASTER will provide the capability for repeat coverage of changing areas on Earth's surface.

  19. Russia’s Naval Future.

    DTIC Science & Technology

    1994-03-24

    31 vii Viii ULS OF URn PAGE Figure I .......................................... 42 ix RUSSIA’S NAVAL FUTURE CHATER I...convinced Peter that Russia must become a naval power. To accomplish this goal, he set out in 1697 to visit European cities -especially English and

  20. Flooding in Southern Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Over the past two weeks, heavy rains have inundated southern Russia, giving rise to floods that killed up to 83 people and drove thousands from their homes. This false-color image acquired on June 23, 2002, by the Moderate-resolution Imaging Spectroradiometer (MODIS) aboard the Terra satellite shows some of the worst flooding. The Black Sea is the dark patch in the lower left-hand corner. The city of Krasnodor, Russia, which was one of the cities hardest hit, sits on the western edge of the larger lake on the left side of the image, and Stavropol, which lost more lives than any other city, sits just east of the small cluster of lakes on the right-hand side of the image. Normally, the rivers and smaller lakes in this image cannot even be seen clearly on MODIS imagery. In this false-color image, the ground is green and blue and water is black or dark brown. Clouds come across as pink and white. Credit: Image courtesy Jesse Allen, NASA GSFC, based on data provided by the MODIS Rapid Response System.

  1. Syphilis soars in Russia.

    PubMed

    Ingram, M

    1995-07-08

    The number of adults with syphilis in Russia has increased 15-fold since the collapse of the Soviet Union. The rate in children is 20 times higher than it was 4 years ago. 126,500 cases were registered with the health ministry over the past year, while 7900 were in 1990. The number of cases in children increased from 38 in 1991 to 761 this year; most of these cases were acquired via sexual transmission. Lilia Tikhonova, the health ministry's chief specialist on sexually transmitted diseases (STDs), blamed the increases on "the complete perversion of our society's morals," the rapid growth of child prostitution, the influx of homeless people and refugees into the cities, and miracle cures that are used in place of seeing a specialist. In communist Russia, patients were required to register passport details and previous sexual contacts, and future sexual contact was forbidden for a period; anyone breaking these rules faced 5 years in jail. Current law only punishes those who knowingly infect their sexual partners. Health officials in the Ukraine, where a similar increase in the number of STDs has been noted, blame black market condoms. Over the past 5 years, cheap foreign condoms have flooded the market.

  2. Artificial radionuclides in Russia due to the Fukushima NPP accident

    NASA Astrophysics Data System (ADS)

    Polianskaia, Olga; Vakulovsky, Sergey; Kim, Vera; Yahryushin, Valery; Volokitin, Andrey

    2013-04-01

    Radioactive emission into the atmosphere from the damaged reactors of the Fukushima Daiichi nuclear power plant (NPP) started on March 12th, 2011. The network of Federal Hydrometeorology and Environmental Monitoring Service (Rosgydromet) carries out supervision over a radiation situation on the territory of Russia. In Russia, the first radionuclides from Fukushima were detected on March 20th in the Far East by network. From March 20th to April 30th I-131 (particulate form), Cs-137 and Cs-134 were detected in samples of atmospheric aerosols at the 30 stations of networks and the same ones were detected in fallout at the 25 stations of networks. The first detection of I-131 in the European territory of Russia (ETR) occurred on March 23rd; and in the South and the North of Siberia - on March 26th. The volumetric activities of I-131 in the ETR sharply increased from March 28th to 30th. Along with the increasing content of I-131 cesium isotopes appeared in the air. The maximum values of radionuclides volume activity were observed between April 3rd and 4th: for I-131 - 4,0 mBq/m3, for Cs-137 - 1,15 mBq/m3, for Cs-134 - 1,04 mBq/m3. Observed in the Far East, the maximum values for I-131 were 2-4 times lower than in the ETR. The maximum values for I-131 in the Asian territory of Russia (ATR) were 2 - 8 times lower, than in the ETR. The Cs-137/Cs-134 ratio in samples of atmospheric aerosols was about 1. The ratio I-131/Cs-137 in air changed in a wide range. From March 23rd to April 5th the ratio fluctuated within 11 to 34, from April 5th to 20th of the ratio decreased and varied within 1,5 to 7,7, further it became less than 1. The value of cesium isotopes in second quarter of 2011 in fallout was lower than 2 Bq/m2. The addition to the density of soil contamination by Cs-137 by 2 to 3 orders of magnitude less than the decrease of the density of contamination with this isotope of the global origin due to radioactive decay. Based on the obtained experimental data we can

  3. Systematics and biology of some species of Micrurapteryx Spuler (Lepidoptera, Gracillariidae) from the Holarctic Region, with re-description of M. caraganella (Hering) from Siberia

    PubMed Central

    Kirichenko, Natalia; Triberti, Paolo; Mutanen, Marko; Magnoux, Emmanuelle; Landry, Jean-François; Lopez-Vaamonde, Carlos

    2016-01-01

    Abstract During a DNA barcoding campaign of leaf-mining insects from Siberia, a genetically divergent lineage of a gracillariid belonging to the genus Micrurapteryx was discovered, whose larvae developed on Caragana Fabr. and Medicago L. (Fabaceae). Specimens from Siberia showed similar external morphology to the Palearctic Micrurapteryx gradatella and the Nearctic Parectopa occulta but differed in male genitalia, DNA barcodes, and nuclear genes histone H3 and 28S. Members of this lineage are re-described here as Micrurapteryx caraganella (Hering, 1957), comb. n., an available name published with only a brief description of its larva and leaf mine. Micrurapteryx caraganella is widely distributed throughout Siberia, from Tyumen oblast in the West to Transbaikalia in the East. Occasionally it may severely affect its main host, Caragana arborescens Lam. This species has been confused in the past with Micrurapteryx gradatella in Siberia, but field observations confirm that Micrurapteryx gradatella exists in Siberia and is sympatric with Micrurapteryx caraganella, at least in the Krasnoyarsk region, where it feeds on different host plants (Vicia amoena Fisch. and Vicia sp.). In addition, based on both morphological and molecular evidence as well as examination of type specimens, the North American Parectopa occulta Braun, 1922 and Parectopa albicostella Braun, 1925 are transferred to Micrurapteryx as Micrurapteryx occulta (Braun, 1922), comb. n. with albicostella as its junior synonym (syn. n.). Characters used to distinguish Micrurapteryx from Parectopa are presented and illustrated. These findings provide another example of the potential of DNA barcoding to reveal overlooked species and illuminate nomenclatural problems. PMID:27110203

  4. BRDF characteristics of tundra vegetation communities in Yamal, Western Siberia

    NASA Astrophysics Data System (ADS)

    Buchhorn, Marcel; Heim, Birgit; Walker, Donald A. Skip; Epstein, Howard; Leibman, Marina

    2013-04-01

    Satellite data from platforms with pointing capabilities (CHRIS/Proba, RapidEye) or from sensors with wide swath (AVHRR, MODIS, MERIS) is influenced by the bidirectional reflectance distribution function (BRDF). This effect can cause significant changes in the measured spectral surface reflectance depending on the solar illumination geometry and sensor viewing conditions. The Environmental Mapping and Analysis Program (EnMAP), a German hyperspectral mission with expected launch in 2016, will provide high spectral resolution observations with a ground sampling distance of 30 meters. Since the EnMAP sensor has pointing capabilities, both spectral and directional reflection characteristics need to be taken into account for the algorithms development for vegetation parameters. The 'hyperspectral method development for Arctic VEGetation biomes' (hy-Arc-VEG) project is part of the national preparation program for the EnMAP mission. Within the EnMAP projcect hy-Arc-VEG we developed a portable field spectro-goniometer, named ManTIS (Manual Transportable Instrument for Spherical BRDF observations), for the in-situ measurements of anisotropic effects of tundra surfaces (national and international patent pending - DE 102011117713.6). The goniometer was designed for field use in difficult as well as challenging terrain and climate. It is therefore of low weight, without electrical devices and weatherproof. It can be disassembled and packed into small boxes for transport. The current off-nadir viewing capacity is matched to the EnMAP sensor configuration (up to 30°). We carried out spectral field and goniometer measurements on the joint YAMAL 2011 expedition (RU-US-DE) organized by the Earth-Cryosphere Institute (ECI) in August 2011 on the Yamal Peninsula, northwestern Siberia, Russia. The field goniometer measurements (conducted under varying sun zenith angles) as well as field spectro-radiometrical measurements were carried out at the NASA Yamal Land Cover/Land Use Change

  5. An 84-kyr paleomagnetic record from the sediments of Lake Baikal, Siberia

    USGS Publications Warehouse

    Peck, J.A.; King, J.W.; Colman, Steven M.; Kravchinsky, V.A.

    1996-01-01

    We have conducted a paleomagnetic study of sediment cores obtained from the Selenga prodelta region of Lake Baikal, Russia. This record, which spans approximately the last 84 kyr, contributes to a better understanding of the nature of geomagnetic field behavior in Siberia and is a useful correlation and dating tool. We demonstrate that the Lake Baikal sediments are recording variations in the geomagnetic field. The directional record displays secular variation behavior with a geomagnetic excursion at 20 ka and additional excursions appearing as large-amplitude secular variation at 41, 61, and 67 ka. Smoothing of the geomagnetic excursion behavior occurs in Lake Baikal sediments owing to the intermediate sedimentation rate (13 cm kyr-1). The Lake Baikal relative paleointensity record correlates to absolute paleointensity data for the last 10 kyr and to relative paleointensity records from the Mediterranean Sea and Indian Ocean for the last 84 kyr. This correlation suggests a strong global (i.e., dipole) component to these records and further supports the reliability of sediments as recorders of relative geomagnetic paleointensity. We show that a relative geomagnetic intensity stratigraphy has a potential resolution of 7 kyr by correlating continental and marine records. The geomagnetic intensity stratigraphy helps constrain the age of the difficult to date Lake Baikal sediments.

  6. Airborne trace metals and organochlorine compounds in arctic Alaska and Siberia: How important?

    SciTech Connect

    Landers, D.H.; Allen-Gil, S.; Gubala, C.P.; Ford, J.

    1995-12-31

    Metal contaminants of anthropogenic origin identified in the arctic atmosphere and the presence of organochlorines in arctic marine mammal tissues has raised the question of the importance of long-range transport of contaminants to the Arctic. Research focused on arctic regions in Alaska and the Taimyr peninsula of north central Russia. Inland watersheds were examined for evidence of increases in trace metal flux during the past 150 years and the presence of organochlorine compounds. Fish and ground squirrels were examined for body burdens of organic contaminants and plasma biomarkers were examined to evaluate biological effects. Sediment data from several lakes suggest that over broad regions, trace metal fluxes have increased only slightly (< 10%), if at all, since the pre-industrial era. The highest metal concentrations in lake sediments are associated with known elevated geologic sources of metals within the respective watersheds. Organochlorines are present in remote inland arctic ecosystems and are most concentrated in the tissues (e.g. liver) of organisms representing higher trophic levels. Arctic Siberia and Alaska (Taimyr peninsula) are similar with regard to contaminant concentrations. However, lichen and moss data suggest that Pb from Eurasian sources does not reach arctic Alaska. The results indicate that long range, transpolar transport and deposition of trace metals is not a large scale current phenomena in the two study regions. The transport and deposition of organochlorine compounds, however, is occurring but at relatively low levels.

  7. Trace metals in the coals of the East Siberia: Distribution, utilization and environmental aspects

    SciTech Connect

    Pashkov, G.L.; Kuznetsov, P.N.; Kuzmin, V.I.; Boiko, Y.V.; Kontsevoi, A.A.

    1998-12-31

    Three coal basins in East Siberia, the Russia Lena, Kansk-Achinsk and South-Yakutsk basins, are huge coal basins which contain various sorts of both brown and high quality subbituminous and bituminous coals with low ash and sulfur content. The coals have great industrial significance for the production of energy, coke and chemicals. However, these coals are less characterized in terms of the content and distribution of trace metals, some of which are of industrial significance, other metals are toxic and radioactive. The data on the distribution of trace metals in these three coal basins, their geochemical occurrence and the behavior in chemical treatment and burning are presented in the paper. Separate coals were found to contain a large amount of valuable metals such as Ge (up to 1,400 g/ton of ash), V (up to 1,400 g/t), Sc (up to 220 g/t), Nb (up to 280 g/t), Cr (up to 1,300 g/t), Co (up to 320 g/t), Ni (580 g/t) and thus could be an industrial source of metal production. The methods for the extraction of Ge, Sc, Y, Nb and other metals prior or after combustion are described. The aspects of coal characterization in terms of toxic and radioactive impact on the environment are discussed.

  8. Nuclear plant emergency preparedness in Russia.

    PubMed

    Sullivan, Randolph L

    2009-11-01

    An international team of experts conducted a detailed operational review at the Volgodonsk nuclear power plant. The review was the first mission by an International Atomic Energy Agency Operational Safety Review Team to Russia in over a decade. The author reviewed the emergency preparedness program in detail. Emergency preparedness professionals in the West are largely unfamiliar with Russian nuclear plant emergency preparedness programs, and the legacy of Chernobyl may leave some doubt as to their efficacy. This article describes the program in some detail and compares some elements to programs in the United States. The author was favorably impressed with the state of nuclear plant emergency preparedness in the Russian Federation and identified program elements that should be considered for implementation elsewhere.

  9. Japan-Russia Pediatric Society.

    PubMed

    Nihei, K; Thunemathu, Y; Kobayashi, N

    1993-12-01

    In March 1990, medical interchange between Japan and the Soviet Union began with a letter from the local health bureau of Khabarovsk. We visited Khabarovsk three times and Kamchatka once, and saw many hospitals and patients. Russian doctors of pediatrics visited Japan. Medical information was exchanged and discussed. The Japan-Russia Pediatric Society was established to perform interchange of medical information, technology and staff such as doctors, nurses and technicians between Japan and Russia, especially the Far East district of Russia. The Society meeting has been held three times: Tokyo (1991), Khabarovsk (1992) and Niigata (1993). It is necessary to continue the interchange between the two countries.

  10. A new model of crustal structure of Siberia

    NASA Astrophysics Data System (ADS)

    Cherepanova, Y.; Artemieva, I. M.; Thybo, H.

    2010-12-01

    We report a new model of the structure of the crust in Siberia that encompasses two large tectonic regions, the Paleozoic West Siberian Basin and the Precambrian Siberian craton. The area of study covers a significant part of the north Eurasia and extends from the Ural mountains in the west to the Verkoyansk Ridge/Lena river in the east, and from the Arctic shelf in the north to the Tien Shan and Altay-Sayans mountains in the south. The new crustal model is based on our new ("from scratch") compilation of all available reliable seismic data and includes the results of seismic reflection, refraction and receiver functions studies, based on old and newly acquired seismic data (from the late 1960-ies until present). Seismic structure along seismic profiles is digitized with a 50 km lateral spacing which is comparable with the resolution of seismic models. Structural parameters based on gravity modeling, or tectonic similarities, or seismic data reported not along seismic reflection/refraction profiles but as interpolated contour maps are excluded from the new crustal database. Due to uneven quality of seismic data related both to data acquisition problems and interpretation limitations, a special attention is paid to the data quality problem, and quality parameters are incorporated into the new database of regional crustal structure. The present database comprises detailed and reliable information on the seismic structure of the crust for most of the tectonic structures of the region and provides valuable constraints for geophysical modeling of the mantle structure. We observe important spatial correlations between the crustal structure (thickness of the sediments, the basement, and different crustal layers, and average basement velocities) and tectonic and geological settings. Statistical analysis of age-dependence (we use tectono-thermal ages) of crustal parameters allows for distinguishing the effects of various tectonic processes on the crustal structure. The

  11. Industrial Development of Siberia and the Soviet Far East.

    DTIC Science & Technology

    1984-09-01

    21 (This argument is perhaps unintentionally fed by the central leadership’s emphasis on investing in renovation and technical reequipment of...Malov, "Po programme ’ energia ’," Pravda, May 12, 1982, p. 2. " M. Matafonov, "Open up Siberia’s Treasure Houses," Sotsialisticheskaia industriia

  12. Classifications of bog peat sensitivity to anthropogenic impact (Western Siberia)

    NASA Astrophysics Data System (ADS)

    Kramarenko, V. V.; Matveenko, I. A.; Nikitenkov, A. N.; Molokov, V. Y.; Khoroshko, A. P.

    2016-09-01

    The article deals with strength parameters of peats in Western Siberia, evaluates their transformations under the anthropogenic mechanical impact, presents peat classification in terms of sensitivity allowing the forecast of strength loss when destructing their structure in the process of building roads, pipelines. Sensitivity classification also permits predicting roadability for construction design.

  13. Petroleum Resource Management and Assessment project for the Western Siberian Administration Russia. TDA feasibility study. Export trade information

    SciTech Connect

    Not Available

    1993-01-01

    The objective of the study is: (1) To determine the nature and availability of the information necessary for Resource Assessment in oil fields to be open to foreign investment; (2) To determine what resources are required to implement the 'Alberta Model' of Resource Management in Siberia; (3) To establish a pilot Data Collection and Information System, including software, hardware and technology; (4) To indicate whether the studied database model and related software can meet Russia's long term requirements for information management in the petroleum sector; (5) The transfer of information techniques to the Russian implementation teams; and (6) To define the requirements for a resource/economic study.

  14. Summer Harvest in Saratov, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Russia's Saratov Oblast (province) is located in the southeastern portion of the East-European plain, in the Lower Volga River Valley. Southern Russia produces roughly 40 percent of the country's total agricultural output, and Saratov Oblast is the largest producer of grain in the Volga region. Vegetation changes in the province's agricultural lands between spring and summer are apparent in these images acquired on May 31 and July 18, 2002 (upper and lower image panels, respectively) by the Multi-angle Imaging SpectroRadiometer (MISR).

    The left-hand panels are natural color views acquired by MISR's vertical-viewing (nadir) camera. Less vegetation and more earth tones (indicative of bare soils) are apparent in the summer image (lower left). Farmers in the region utilize staggered sowing to help stabilize yields, and a number of different stages of crop maturity can be observed. The main crop is spring wheat, cultivated under non-irrigated conditions. A short growing season and relatively low and variable rainfall are the major limitations to production. Saratov city is apparent as the light gray pixels on the left (west) bank of the Volga River. Riparian vegetation along the Volga exhibits dark green hues, with some new growth appearing in summer.

    The right-hand panels are multi-angle composites created with red band data from MISR's 60-degree backward, nadir and 60-degree forward-viewing cameras displayed as red, green and blue respectively. In these images, color variations serve as a proxy for changes in angular reflectance, and the spring and summer views were processed identically to preserve relative variations in brightness between the two dates. Urban areas and vegetation along the Volga banks look similar in the two seasonal multi-angle composites. The agricultural areas, on the other hand, look strikingly different. This can be attributed to differences in brightness and texture between bare soil and vegetated land. The chestnut-colored soils in

  15. Nursing and health in Russia.

    PubMed

    1998-01-01

    There are over one million nurses in Russia, and they work in a crippled healthcare system facing a dramatic increase in infectious diseases. But nurses are valiantly coping with the country's health crisis and becoming a recognized profession.

  16. Modern Nanoparticle Research in Russia

    NASA Astrophysics Data System (ADS)

    Andrievski, R. A.

    2003-12-01

    Nanoparticle and nanomaterial research has become one of the most active frontier areas. In Russia and countries of the former Soviet Union work devoted to the thorough study of ultrafine media (low-dimensional subjects) started early. In the present paper a short historical review is given and the problems of nanoparticle research in Russia and some related fields (such as nanomaterials, nanochemistry, and nanophysics) are discussed.

  17. Crustal structure of Siberia: a new appraisal of old seismic data

    NASA Astrophysics Data System (ADS)

    Cherepanova, Yu; Artemieva, I. M.; Milshtein, E.; Erinchek, Yu. M.; Thybo, H.

    2010-05-01

    We review the structure of the crust and the sedimentary cover in an area that encompasses two largest tectonic regions, the Paleozoic West Siberia basin and the Precambrian Siberian craton, and extends from the Ural mountains in the west to the Verkoyansk Ridge/Lena river in the east, and from the Arctic shelf in the north to the Tien Shan and Altay-Sayans mountains in the south. We compiled "from scratch" all available seismic data for the region, from the late 1960-ies until present. Our compilation includes results of seismic reflection, refraction and receiver functions studies, based on old and newly acquired seismic data; data along seismic profiles are digitized with a 50 km lateral spacing which is comparable with resolution of seismic models. Seismic data on the structure of the sedimentary cover was complemented by borehole data, where available. Due to uneven quality of seismic data related both to data acquisition and interpretation, a special attention was paid to this problem and quality parameters are incorporated into the new database of regional crustal structure. We have intentionally excluded unreliable constraints, such as based on gravity modelling or tectonic similarities, or seismic data reported not along seismic reflection/ refraction profiles but as interpolated contour maps. The present database comprises detailed and reliable information on the seismic structure of the crust for most of the tectonic structures of the region and allows examining spatial correlations with tectonic and geological structures, providing the basis for studies of crustal evolution and mantle modeling.

  18. The main features of the interaction of mantle magmas with granulite complexes of the lower crust and their relationship with granitic melts (exemplified by the Early Caledonides of the West Baikal Region, Russia)

    NASA Astrophysics Data System (ADS)

    Vladimirov, Alexandr; Khromykh, Sergei; Mekhonoshin, Alexei; Volkova, Nina; Travin, Alexei; Mikheev, Evgeny; Vladimirova, Anna

    2016-04-01

    Granulite complexes occurring in the Early Caledonian southern folded framing of the Siberian Craton are deeply eroded fragments of the Vendian-Early Paleozoic accretionary prism, which is an indicator of the early stages of the Paleo-Asian Ocean (Gladkochub et al., 2010). The main feature of the granulite complexes is a wide development of gabbro-pyroxenites composing tectonic plates, synmetamorphic intrusive bodies, and numerous disintegrated fragments (boudins and enclaves), immersed in a metamorphic matrix. The volume of basites reaches 5-10 %, which allows us to consider mantle magmatism as a heat source for the granulite metamorphism. The most studied polygon is Chernorud granulite zone, which is a part of the Olkhon metamorphic terrane, West Baikal Region. Just this polygon was used for considering the problems of interaction of mantle magmas with lower crust granulite complexes and their relationship with granitic melts. The Chernorud Zone is a typical example of the accretionary prism with a predominance of metabasalts (70-80 %), subordinate amounts of marbles, quartzites and metapelites that have been subjected to granulite facies metamorphism and viscoelastic flow of rock masses. Study of two-pyroxene granulites (metabasalts) and garnet-sillimanite gneisses (metapelites) allows us to estimate P-T metamorphic conditions (P = 7.7-8.6 kbar, T = 770-820°C) and their U-Pb metamorphic age (530-500 Ma). Metabasalts correspond in their geochemistry to the island-arc tholeiitic series (Volkova et al., 2010; Gladkochub et al., 2010). Sin-metamorphic gabbro-pyroxenites formed in two stages: 1) Chernorud complex - tectonic slices and body's exhumed from deep earth crust levels (10-12 kb) and composed of arc tholeiitic series rocks (age T ≥ 500 Ma); 2) Ulan-Khargana complex - supply magmatic canals and fragmented tabular intrusions. This rocks composition corresponds to subalkaline petrochemical series (OIB) and U/Pb age is equal to 485±10 Ma (Travin et al., 2009

  19. Post-fire succession of ground vegetation of central Siberia in Scots pine forests

    NASA Astrophysics Data System (ADS)

    Kovaleva, N.; Ivanova, G. A.; Conard, S. G.

    2012-04-01

    Extensive wildfires have affected the Russian region in the last decade. Scots pine forests (Pinus sylvestris L.) are widespread in central Siberia and fire occurrence is high in these forests, whose dominant fire regime is one of frequent surface fires. We studied post- fire succession of ground vegetation has been studied on nine experimental fires of varying severity (from 620 to 5220 kW/m) in middle taiga Scots pine forests of central Siberia (Russia). It proved from our study that all species of the succession process are present from initial stages. We did not find any trend of ground vegetation diversity with the time during 8 years after the fire. Our investigation showed that post- fire recovery of the ground vegetation is determined by initial forest type, fire severity and litter burning depth. Fire severity had a clear effect in initial succession in study area and it clearly had an impact on percentage cover, biomass and structure of ground vegetation. In a lesser degree the small shrubs are damaged during ground fires. The dominating species (Vaccinium vitis-idaea and V. myrtillus) regained the cover values above or close to 6—8 years. The post- fire biomass of ground vegetation 93—100% consists of species (Vaccinium vitis-idaea and V. myrtillus) that survived after the fire and increased in the cover with the time. In pine forests mosses and lichens suffer to a greater degree after ground fires. Lichen layer was completely lost after the fires of any severity. Decrease of mosses species diversity takes place after ground fires. The post- fire cover and species diversity of the green mosses were progressively lower with increasing the fire severity during the observation period. Maximum changes are discovered in the post- fire structure of plant microgroups after the high- severity fire which resulted in intensive invasion by the post- fire mosses (Polytrichum strictum and P. commune). There is a positive trend of green moss microgroups recovery

  20. Mitochondrial DNA diversity in indigenous populations of the southern extent of Siberia, and the origins of Native American haplogroups.

    PubMed

    Starikovskaya, Elena B; Sukernik, Rem I; Derbeneva, Olga A; Volodko, Natalia V; Ruiz-Pesini, Eduardo; Torroni, Antonio; Brown, Michael D; Lott, Marie T; Hosseini, Seyed H; Huoponen, Kirsi; Wallace, Douglas C

    2005-01-01

    In search of the ancestors of Native American mitochondrial DNA (mtDNA) haplogroups, we analyzed the mtDNA of 531 individuals from nine indigenous populations in Siberia. All mtDNAs were subjected to high-resolution RFLP analysis, sequencing of the control-region hypervariable segment I (HVS-I), and surveyed for additional polymorphic markers in the coding region. Furthermore, the mtDNAs selected according to haplogroup/subhaplogroup status were completely sequenced. Phylogenetic analyses of the resulting data, combined with those from previously published Siberian arctic and sub-arctic populations, revealed that remnants of the ancient Siberian gene pool are still evident in Siberian populations, suggesting that the founding haplotypes of the Native American A-D branches originated in different parts of Siberia. Thus, lineage A complete sequences revealed in the Mansi of the Lower Ob and the Ket of the Lower Yenisei belong to A1, suggesting that A1 mtDNAs occasionally found in the remnants of hunting-gathering populations of northwestern and northern Siberia belonged to a common gene pool of the Siberian progenitors of Paleoindians. Moreover, lineage B1, which is the most closely related to the American B2, occurred in the Tubalar and Tuvan inhabiting the territory between the upper reaches of the Ob River in the west, to the Upper Yenisei region in the east. Finally, the sequence variants of haplogroups C and D, which are most similar to Native American C1 and D1, were detected in the Ulchi of the Lower Amur. Overall, our data suggest that the immediate ancestors of the Siberian/Beringian migrants who gave rise to ancient (pre-Clovis) Paleoindians have a common origin with aboriginal people of the area now designated the Altai-Sayan Upland, as well as the Lower Amur/Sea of Okhotsk region.

  1. Russia`s Great Game in a nuclear South Asia

    SciTech Connect

    Pilat, J.F.; Taylor, T.T.

    1998-12-31

    Lost in the noise of Pakistan`s nuclear weapon tests in the western Baluchistan desert on 28 and 30 May was a surprising diplomatic move by Russia. On 23 May, Russia became the first state to express its willingness to recognize India as a nuclear-weapon state, provided that India commits itself to the international nonproliferation regime. Russia`s Ambassador to India, Albert Chernyshev, stated in the days after the Indian but before the Pakistani nuclear tests that ``India proclaimed itself a nuclear weapons power. One now hopes that India will behave as a nuclear weapons power by acting responsibly. Every nuclear weapons state has some rights. But for getting recognition it must have some obligations. Once it is ready to show these obligations by joining the nonproliferation regime, its recognition as a nuclear weapons power will follow.`` Russia`s Great Game in South Asia in pursuit of short-term economic and other interests appears to be a serious obstacle on the path to dealing effectively with the South Asian nuclear crisis. Grave damage to security, stability and nonproliferation has already resulted from India`s and Pakistan`s actions, but the situation does not have to spiral out of control. It is imperative that the international community respond appropriately to this challenge. The international community is at a crossroads and Russia`s actions will be critical. Will it be willing to go beyond the narrow economic and political calculations reflected in its diplomatic posturing, and take actions that will serve its long-term interests by bridging differences with other great powers in order to demonstrate to India that it has not chosen the right path. If Russia decides it can gain from India`s current, perilous path and blocks or otherwise frustrates appropriate responses, the nuclear danger on the subcontinent will escalate and the global regimes to promote nonproliferation and to ban testing will be seriously, perhaps fatally, weakened with

  2. Health lifestyles and political ideology in Belarus, Russia, and Ukraine.

    PubMed

    Cockerham, William C; Hinote, Brian P; Cockerham, Geoffrey B; Abbott, Pamela

    2006-04-01

    This paper examines the association of political ideology with health lifestyle practices and self-rated health in Belarus, Russia, and Ukraine. The political trajectory of post-Soviet societies has taken two divergent paths, either toward democracy or autocracy. The health trajectory has followed the same pattern with the more autocratic states continuing to experience a mortality crisis, while those former socialist countries that have embraced democracy and moved closer to the West have escaped this crisis. This paper investigates whether political ideology in three post-Soviet countries that are firmly (Belarus), increasingly (Russia), or recently (Ukraine) autocratic is related to health lifestyles and health self-ratings. Data were collected by face-to-face interviews (N = 8406) with a representative national sample of the adult population. The results show that respondents who are against restoring communism have healthier lifestyles and rate their health better than respondents who wish to see communism return.

  3. Coast of the East Siberian Sea, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Sea ice is pulling away from the coastline of northeastern Siberia in the east Siberia Sea. This true-color Moderate Resolution Imaging Spectroradiometer (MODIS) image from May 26, 2002, also the thinning of ice in bays and coves, and the blue reflection of the water from beneath causes the ice to appear bright blue. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  4. A review of the genus Drymeia Meigen, 1826 (Diptera: Muscidae) in Russia.

    PubMed

    Sorokina, Vera S; Pont, Adrian C

    2015-08-14

    A key is provided to the 26 species of the genus Drymeia Meigen, 1826 known from Russia and four additional species that may be found in Russia (D. brumalis (Rondani, 1866), D. cantabrigensis (Huckett, 1965), D. gymnophthalma (Hennig, 1963), D. similis (Malloch, 1918)). The key includes the 10 new species here described from the mountains of South Siberia (D. acrostichalis sp. nov., D. aristata sp. nov., D. cilitarsis sp. nov., D. glabra sp. nov., D. grandis sp. nov., D. grisea sp. nov., D. longiseta sp. nov., D. phaonina sp. nov., D. puchokana sp. nov., D. triseta sp. nov.,) and other two new species from the Russian Arctic (D. cristata sp. nov., D. taymirensis sp. nov.). Five species (D. fasciculata (Stein, 1916), D. firthiana (Huckett, 1965), D. groenlandica (Lundbeck, 1901), D. quadrisetosa (Malloch, 1919), D. neoborealis (Snyder, 1949)) are newly recorded from Russia. Three new synonymies are proposed: D. pribilofensis (Malloch, 1921) (syn: D. inaequalis (Malloch, 1922)), D. setibasis (Huckett, 1965) (syn: D. gymnophthalma sibirica (Lavčiev, 1971, unavailable junior secondary homonym) and D. quadrisetosa (Malloch, 1919) (syn: D. amurensis (Lavčiev, 1971)). The male terminalia and the female ovipositors of the new species are illustrated. New faunistic data are given for some previously described species of Russian Drymeia.

  5. Status of forest resources and the environment in Siberia

    SciTech Connect

    Danilin, I.; Sokoly, V.

    1997-12-31

    The Siberian forests are considered to be one of the most important biomes on earth. The forested area of Siberia constitutes about 20 percent of the total world forested area and nearly 50 percent of the total world coniferous forested area. About 605 million hectares are covered with stands, these areas make up about 48 percent of the total area. Nearly 450 million hectares are covered with coniferous species. The total growing stock of stemwood is 61.4 billion m{sup 3} as compared to North America - 50.3 billion m{sup 3} of which 51 billion m{sup 3} is made up of coniferous species. About 38.5 billion m{sup 3} (nearly 63 percent) of the growing stock are classified as mature and overmature forests. Nearly 65 percent of the Siberian forests are growing in areas with permafrost and more than 60 percent of the forested areas are classified as mountain forests. The carbon stock, accumulated in forest ecosystems of Siberia, exceeds 94 billion tons in total, with annual carbon sequestration at more than 170 million tons. This sink could be significantly increased by implementation of rational forestry in Siberia. Average stock per 1 ha of mature and overmature stands is 148 m{sup 3}. Average annual growth per 1 ha of forest-forming species is 1.31 m{sup 3}, among them conifers - 1.17 m{sup 3}. Siberia has roughly 40% of its original forests intact (the United States has less than 5% of its ancient forests).

  6. [Lactase deficiency among representatives of various nationalities of Siberia].

    PubMed

    Zhvavyĭ, N F; Kozlov, A I; Kondik, V M

    1991-01-01

    Some features of lactase tolerance were investigated in representatives of varying groups of indigenous population in Siberia-Mansi, Khanty, Nenets, Buryats. The indirect method was used to evaluate lactase activity. A total of 92 subjects were investigated. It was found that 32% of the representatives of the Urals population group and 53% of Buryats were capable of lactase assimilating. The data obtained correspond to the cultural-genetic hypothesis on the nature of lactase tolerance in the representatives of different ethnic groups.

  7. Fire effects on hydrochemistry of streams draining watersheds with continuous permafrost distribution in Central Siberia

    NASA Astrophysics Data System (ADS)

    Prokushkin, Anatoly; Pokrovsky, Oleg; Kawahigashi, Masayuki; Viers, Jerome

    2010-05-01

    Wildfires, assumed to be the main disturbance factor in the boreal biome, are tended to increase in frequency and severity under "dry warming" (Conard et al. 2002). Short fire-return interval in larch dominated permafrost terrains of Siberia (Kharuk et al., 2008) exert significant control on ecosystem biogeochemical cycling throughout the complex influences of deforestation, ground vegetation and organic layer combustion as well as deepen soil active layer. Despite extensive research of fire impact on carbon exchange between soil, forest biomass and atmosphere in permafrost affected regions of Siberia, much less is known on the role of fire in control of element transport in rivers and watersheds affected by fire events. To analyze the effect of fires on chemical composition of surface fluids in permafrost zone, fourteen small forested watersheds (3-25 km2) have been selected in mid-stream of Nizhnyaya Tunguska River (Yenissey basin, Central Siberia, Russia). Analysis of larch trees in forest stands of the area demonstrated that presumably all basins were affected by wildfires in the past. Selected watersheds have been influenced by ground fires (>90% of watershed area) ca 110, 60 and 15 years ago (respectively in 1899, 1947 and 1993). Water sampling campaign has been conducted from snowmelt (mid-May) to the start of freezing (mid-October) on weekly and/or monthly interval in 2006-2009. In this study, we analyzed the dissolved loads for major and trace element concentrations. In terms of concentration changes in the course of the year, concentrations of dissolved organic carbon (DOC as well as associated elements like Fe, Al, Y and REE) and inorganic ions (e.g. DIC, Cl, Ca, Na, Mg etc.) demonstrated opposite tendencies during a frost-free season in all streams. However, basins with recent fire effect exhibited generally lower DOC concentrations in streams along with much more pronounced seasonal increase in concentrations of inorganic compounds. The increased

  8. Hydrothermal conditions of South Eastern Siberia under the ongoing warming

    NASA Astrophysics Data System (ADS)

    Voropay, N. N.; Maksyutova, E. V.; Riazanova, A. A.

    2016-11-01

    A great increase in air temperature has been observed since 1976. Siberia is a region with most severe ongoing climate change. To monitor the extreme weather events is important. To evaluate moisture conditions we used the D.A. Ped index (Si). Monthly air temperature and precipitation data from 19 weather stations of South Eastern Siberia (50-60° N 90-120° E) were used for the index calculation during the vegetation period. During 1976-2010 the number of droughts in the study region was more than the number of excessive moisture periods. The maximal statistically significant trend (0.4-0.6 per 10 years) in Eastern Siberia was observed in May. The characteristics of the winter-spring period preceding the vegetation season were analyzed. Significant positive trends exist in the study area for the May temperature (0.5-0.9 °C per 10 years) and the May sum of positive temperatures (14-28 °C per 10 years). There are tendencies to increase the number of days with temperatures above zero in March (1-3 days per 10 years) and the sum of positive temperatures in April (5-16 °C per 10 years). The stable transition of air temperature over 0 °C shifts into early dates by 1-7 days every 10 years.

  9. 77 FR 12880 - Uranium From Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-03-02

    ... investigation on uranium from Russia would be likely to lead to continuation or recurrence of material injury to... Publication 4307 (February 2012), entitled Uranium from Russia: Investigation No. 731-TA-539-C (Third...

  10. Database of in-situ field measurements for estimates of fuel consumption and fire emissions in Siberia

    NASA Astrophysics Data System (ADS)

    Kukavskaya, Elena; Conard, Susan; Buryak, Ludmila; Ivanova, Galina; Soja, Amber; Kalenskaya, Olga; Zhila, Sergey; Zarubin, Denis; Groisman, Pavel

    2016-04-01

    Wildfires show great variability in the amount of fuel consumed and carbon emitted to the atmosphere. Various types of models are used to calculate global or large scale regional fire emissions. However, in the databases used to estimate fuel consumptions, data for Russia are typically under-represented. Meanwhile, the differences in vegetation and fire regimes in the boreal forests in North America and Eurasia argue strongly for the need of regional ecosystem-specific data. For about 15 years we have been collecting field data on fuel loads and consumption in different ecosystem types of Siberia. We conducted a series of experimental burnings of varying fireline intensity in Scots pine and larch forests of central Siberia to obtain quantitative and qualitative data on fire behavior and carbon emissions. In addition, we examined wildfire behavior and effects in different vegetation types including Scots pine, Siberian pine, fir, birch, poplar, and larch-dominated forests; evergreen coniferous shrubs; grasslands, and peats. We investigated various ecosystem zones of Siberia (central and southern taiga, forest-steppe, steppe, mountains) in the different subjects of the Russian Federation (Krasnoyarsk Kray, Republic of Khakassia, Republic of Buryatia, Tuva Republic, Zabaikalsky Kray). To evaluate the impact of forest practices on fire emissions, burned and unburned logged sites and forest plantations were examined. We found large variations of fuel consumption and fire emission rates among different vegetation types depending on growing conditions, fire behavior characteristics and anthropogenic factors. Changes in the climate system result in an increase in fire frequency, area burned, the number of extreme fires, fire season length, fire season severity, and the number of ignitions from lightning. This leads to an increase of fire-related emissions of carbon to the atmosphere. The field measurement database we compiled is required for improving accuracy of existing

  11. The White Sea, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Editor's Note: The caption below, published on May 10, 2001, is incorrect. According to Masha Vorontsova, director of the International Fund for Animal Welfare in Moscow, the situation with the seal pups in the White Sea is normal. There is no disaster and there never was. For more details, refer to the article entitled 'No Danger' on the New Scientist home page. The Earth Observatory regrets the earlier errant report. Original Caption According to the Russian Polar Research Institute for Fisheries and Oceanography, between 250,000 and 300,000 Greenland seal pups face death by starvation over the next two months due to a cruel trick by mother nature. The seals, most of them less than two months old, are trapped on ice sheets that remain locked in the White Sea, located near Archangel in Northern Russia. Typically, during the spring thaw the ice sheets break up and flow with the currents northward into the Barents Sea, the seals' spring feeding grounds. The seal pups hitch a ride on the ice floes, living on their own individual stores of fat until they arrive in the Barents Sea. Their mothers departed for the Barents Sea weeks ago. In a normal year, the seal pups' trip from the White Sea out to the Barents takes about six weeks and the seals have adapted to rely upon this mechanism of mother nature. During their yearly migration, the mother seals usually stay with their pups and feed them until their pelts turn from white to grey--a sign that the pups are mature enough to swim and feed themselves. Unfortunately, this year unusually strong northerly winds created a bottleneck of ice near the mouth of the white sea, thus blocking the flow of ice and trapping the pups. These true-color images of the White Sea were acquired by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra spacecraft. This image, taken May 2, 2000 that there is usually much less ice in the White Sea this time of year as most of it is typically en route to the

  12. Hydrological processes at the Suntar-Hayata ridge (Eastern Siberia) in past, current and future climate

    NASA Astrophysics Data System (ADS)

    Nesterova, Nataliia; Semenova, Olga; Lebedeva, Liudmila

    2016-04-01

    The detailed studies of permafrost, hydrological and glaciological processes at the Suntar-Hayata Ridge started within the Program of International Geophysical Year (1957-1958). The Suntar-Hayta Ridge (with highest mountain reaching 2959 m) is situated in Eastern Siberia and divides the Lena, Indigirka and the Okhotsk sea rivers basins. It is characterized by original combination of climate, geological and glaciological conditions. In 2015 our research group got the access to the reports of High-Mountain Glaciological and Geocriological Suntar-Hayata station which were stored in the archives of Melnikov Permafrost Institute in Yakutsk (Russia). We used revealed data for assessment of runoff formation processes and the factors affecting them in remote high-elevation permafrost area, and estimated the parameters of hydrological model based on those findings. Two watersheds of different scale were selected as the objects of our studies - the Suntar river (7680 km2) and the Sakharyniya River (84.4 km2). The Hydrograph model (Vinogradov et al., 2011; Semenova et al., 2013) was used in the study as it explicitly describes hydrological processes in different permafrost environments including the dynamics of ground thaw/freeze (ex., Lebedeva et al., 2014). In the Hydrograph model the processes have a physical basis and certain strategic conceptual simplifications. The level of model complexity is suitable for a remote, sparsely gauged region such as Eastern Siberia as it allows for a priori assessment of the model parameters. Based on the observations (meteorological data, ground temperature at different depth, soil profile physical properties, characteristics of vegetation, snow measurements, etc.) the model parameters were estimated for four main landscapes of the studied watersheds (bare ground, mountain tundra, sparse larch forest and riparian forest at swamped soils). At the first stage we conducted the simulation of individual processes and compared the results with

  13. The diversity and prevalence of hard ticks attacking human hosts in Eastern Siberia (Russian Federation) with first description of invasion of non-endemic tick species.

    PubMed

    Khasnatinov, Maxim Anatolyevich; Liapunov, Alexander Valeryevich; Manzarova, Ellina Lopsonovna; Kulakova, Nina Viktorovna; Petrova, Irina Viktorovna; Danchinova, Galina Anatolyevna

    2016-02-01

    Hard ticks are the vectors of many pathogens including tick-borne encephalitis virus and the Lyme disease agent Borrelia burgdorferi sensu lato. In Eastern Siberia, Ixodes persulcatus, Dermacentor nuttalli, Dermacentor silvarum and Haemaphysalis concinna are regarded as aggressive to humans. Recently, significant changes in world tick fauna have been reported and this affects the spread of tick-borne pathogens. We studied the current species diversity, population structure and prevalence of tick-borne pathogens of hard ticks (Acari: Ixodidae) that attacked humans in Eastern Siberia (Irkutsk region, Russia). In total, 31,892 individual ticks were identified and analysed during the years 2007-2014. The majority (85.4%) of victims was bitten by I. persulcatus, 14.55% of attacks on humans were caused by D. nuttalli and D. silvarum, whereas H. concinna was documented only in 15 cases (0.05%). The seasonal activity and the age/gender structure of the tick population were studied as well. Among all the studied ticks, three unconventional species, i.e. Rhipicephalus sanguineus, Dermacentor reticulatus and Amblyomma americanum, were identified. Analysis of tick bite histories indicates at least three events of invasion of non-endemic ticks into the ecosystems of northern Eurasia with harsh continental climates. Invading ticks are able to reach the adult life stage and are aggressive to the local human population. Phylogenetic analysis of mt 16S rRNA gene fragments suggests multiple independent routes of tick migration to Eastern Siberia. Possible implications to human health and epidemiology of tick-borne infections are discussed.

  14. Spatio-temporal dynamics of climatic extreme indices over Siberia

    NASA Astrophysics Data System (ADS)

    Shulgina, Tamara; Gordov, Evgeny; Genina, Elena

    2013-04-01

    Nowadays numerous investigations are aimed at analysis of regional climatic extremes becoming more pronounced under climate change. In particular, obtained results indicate decrease of number of frost days and increase of growing season length over the most part of Siberian territory, and precipitation intensity increases in the northern part of Siberia [1]. To obtain the complete pattern of ongoing changes in climatic extremes the following indices dynamics should be analyzed: percentage of days when minimum/maximum temperature less than 10th percentile, percentage of days minimum/maximum temperature greater than 90th percentile, maximum length of dry/wet spell. Climatic extreme assessments are obtained based on ECMWF ERA Interim Reanalysis and APHRODITE JMA data for the time period from 1979 to 2007. These datasets reproduce the statistics of observed climate features in Siberia more accurately [1]. Modern techniques of mathematical statistics are used for analysis of the temporal and spatial behavior of above mentioned climatic characteristics. Data analysis has been done using computational-geoinformational web-system for analysis of regional climatic change [2]. Surface temperature and precipitation extreme assessments obtained for Siberian territory can help to get a better understanding of current changes in the biosphere and socio-economic aspects. Partial financial support for this research from the Russian Foundation for Basic Research (project 11-05-01190a), SB RAS projects VIII.80.2.1 and 131, and the Russian Federation Ministry of Education and Science grant # 8345 is acknowledged. 1. Shulgina T.M., Genina E.Yu., Gordov E.P. Dynamics of climatic characteristics influencing vegetation in Siberia // Environmental Research Letters, 2011. - DOI: 10.1088/1748-9326/6/4/045210. - 7 p. 2. Evgeny Gordov et al. Development of Information-Computational Infrastructure for Environmental research in Siberia as a baseline component of the Northern Eurasia Earth

  15. 76 FR 11273 - Ammonium Nitrate From Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-03-01

    ... COMMISSION Ammonium Nitrate From Russia AGENCY: United States International Trade Commission. ACTION: Institution of a five-year review concerning the suspended investigation on ammonium nitrate from Russia... investigation on ammonium nitrate from Russia would be likely to lead to continuation or recurrence of...

  16. On Eulimnogammarus messerschmidtii, sp. n. (Amphipoda: Gammaridea) from Lake Baikal, Siberia, with redescription of E. cyanoides (Sowinsky) and remarks on taxonomy of the genus Eulimnogammarus.

    PubMed

    Bedulina, Daria S; Takhteev, Vadim V; Pogrebnyak, Svyatoslav G; Govorukhina, Ekaterina B; Madyarova, Ekaterina V; Lubyaga, Yulia A; Vereshchagina, Kseniya P; Timofeyev, Maxim A; Luckenbach, Till

    2014-07-22

    A new amphipod species of the endemic fauna of Lake Baikal (East Siberia, Russia), Eulimnogammarus messerschmidtii sp. n., from the littoral zone of the northern part of the lake is described. The species is characterized by the presence of a group of spines with dense setae on the last 4 body segments. The basal peduncular segment of antenna 1 bears bunches of dense setae without spines, uropods 3 are covered by dense simple setae without plumose setae and the outer ramus has a second small article. The body length of sampled specimens ranges from 7.5 to 18 mm. Population analysis at one of the sampling points revealed a spring-summer reproduction period for this species. This species was previously erroneously identified as E. cyanoides. E. cyanoides is here redescribed in details based on the lectotype. The differences between E. messerschmidtii sp. n., E. cyanoides and other closely related Eulimnogammarus species are described. The taxonomy of the genus Eulimnogammarus is discussed.

  17. Stability and biodegradability of humic substances from Arctic soils of Western Siberia: insights from 13C-NMR spectroscopy and elemental analysis

    NASA Astrophysics Data System (ADS)

    Ejarque, E.; Abakumov, E.

    2015-11-01

    Arctic soils contain large amounts of organic matter which, globally, exceed the amount of carbon stored in vegetation biomass and in the atmosphere. Recent studies emphasize the potential sensitivity for this soil organic matter (SOM) to be mineralised when faced with increasing ambient temperatures. In order to better refine the predictions about the response of SOM to climate warming, there is a need to increase the spatial coverage of empirical data on SOM quantity and quality in the Arctic area. This study provides, for the first time, a characterisation of SOM from the Gydan Peninsula in the Yamal Region, Western Siberia, Russia. On the one hand, soil humic acids and their humification state were characterised by measuring the elemental composition and diversity of functional groups using solid-state 13C-NMR spectroscopy. Also, the total mineralisable carbon was measured. Our results show that there is a uniformity of SOM characteristics throughout the studied region, as well as within soil profiles. Such in-depth homogeneity, together with a predominance of aliphatic carbon structures, suggests the accumulation in soil of raw and slightly decomposed organic matter. Moreover, results on total mineralisable carbon suggest a high lability of these compounds. The mineralisation rate was found to be independent of SOM quality, and to be mainly explained solely by the total carbon content. Overall, our results provide further evidence on the fundamental role that the soils of Western Siberia may have on regulating the global carbon balance when faced with increasing ambient temperatures.

  18. Demonstrating the Potential of ALOS PALSAR Backscatter and InSAR Coherence for Forest Growing Stock Volume Estimation in Central Siberia

    NASA Astrophysics Data System (ADS)

    Thiel, Christian; Schmullius, Christiane

    2016-08-01

    The full potential of ALOS PA LSAR L-band interferometric (InSAR) coherence data for the estimation of forest growing stock volume (GSV) in the boreal forest has rarely been investigated. Moreover, ALOS PALSAR backscatter and InSAR coherence have yet to be used together to delineate GSV. Due to the observation strategy and the high acquisition success rate over Eurasia, a large amount of high quality ALOS PALSAR L-band data is available over Siberia. Consequently, this paper investigates the capability of ALOS PALSAR backscatter and InSAR coherence for the estimation of GSV in Central Siberia, Russia. The potential of backscatter and coherence are directly compared using the same inventory data. Altogether, 87 PALSAR images are used and eleven forest inventory sites are investigated. Based on this large dataset it was observed that InSAR coherence acquired in frozen conditions offers the highest potential for GSV estimation. The saturation level for single coherence images was on average 230 m3/ha, with an average R2 between coherence and GSV of 0.58. PALSAR backscatter acquired in unfrozen conditions could also estimate GSV; however, the saturation levels (75-100 m3/ha) and the average R2 (0.42-0.48) were lower. HV backscatter offered only a slightly greater potential than HH backscatter.

  19. Stability and biodegradability of organic matter from Arctic soils of Western Siberia: Insights from 13C-NMR spectroscopy and elemental analysis

    NASA Astrophysics Data System (ADS)

    Ejarque, Elisabet; Abakumov, Evgeny

    2016-04-01

    Arctic soils contain large amounts of organic matter which, globally, exceed the amount of carbon stored in vegetation biomass and in the atmosphere. Recent studies emphasize the potential sensitivity for this soil organic matter (SOM) to be mineralised when faced with increasing ambient temperatures. In order to better refine the predictions about the response of SOM to climate warming, there is a need to increase the spatial coverage of empirical data on SOM quantity and quality in the Arctic area. This study provides, for the first time, a characterisation of SOM from the Gydan Peninsula in the Yamal Region, Western Siberia, Russia. On the one hand, soil humic acids and their humification state were characterised by measuring the elemental composition and diversity of functional groups using solid-state 13C-NMR spectroscopy. Also, the total mineralisable carbon was measured. Our results show that there is a predominance of aliphatic carbon structures, with a distribution of functional groups that has a minimal variation both regionally and within soil depth. Such vertical homogeneity and low level of aromaticity reflects the accumulation in soil of lowly decomposed organic matter due to cold temperatures. Mineralisation rates were found to be independent of SOM quality, and to be mainly explained solely by the total carbon content. Overall, our results provide further evidence on the sensitivity that the soils of Western Siberia may have to increasing ambient temperatures and highlight the important role that this region can play in the global carbon balance under the effects of climate warming.

  20. Russia’s Proliferation Pathways

    DTIC Science & Technology

    2009-01-01

    Kh-55 nuclear-capable cruise missiles to Iran and China in 2000-01.[107] And of course the murder of Anatoly Litvinenko in November 2006 by polonium ...Phasing Out Civilian HEU in Russia,” Nonproliferation Review XV, no. 2 (July 2008): 209-236. 115. Ibid., 209. 116. Ibid., 210 . 117. Sonia Ben

  1. Shannon Lucid Trains in Russia

    NASA Technical Reports Server (NTRS)

    1995-01-01

    Astronaut Shannon Lucid is seen egressing from a training version of a soyez spacecraft, during a water survival training session in Russia. In March of 1996, Lucid accompanied the STS-76 crew to the Russian space station, Mir, where she stayed for a little over four months before returning to Earth with the STS-79 crew.

  2. Gender Asymmetries in Today's Russia

    ERIC Educational Resources Information Center

    Rimashevskaia, N. M.

    2011-01-01

    There can be no doubt that gender attitudes and the gender stereotypes formed on their basis have a deep-rooted social character. This stems unequivocally from the parallels of development of social processes and gender models. The ideology of gender began to flourish in Russia along with perestroika, an ideology that in the past quarter-century…

  3. Scholars at Risk in Russia

    NASA Astrophysics Data System (ADS)

    Orlov, Yuri

    2006-04-01

    I will share my general thoughts on safe haven for scholars at risk, based on my own experience, and will discuss scholars at risk in Russia. At the present time, these are mostly scientists falsely accused of espionage. I will highlight the special issues this fact raises for providing support or safe haven for such scientists.

  4. Patterns of smoking in Russia

    PubMed Central

    McKee, M.; Bobak, M.; Rose, R.; Shkolnikov, V.; Chenet, L.; Leon, D.

    1998-01-01

    BACKGROUND—Tobacco is a leading cause of avoidable death in Russia but there is, as yet, relatively little information in the public domain on who is smoking and how this is changing. This information is important for those seeking to develop effective policies to tackle this issue.
OBJECTIVE—To determine the prevalence of smoking in Russia and its association with sociodemographic factors.
DESIGN—Cross-sectional survey on patterns of tobacco consumption.
SETTING—Data were collected using the New Russia Barometer, a multi-stage stratified-sample survey of the population of the Russian Federation undertaken in the summer of 1996.
PARTICIPANTS—Data were available on 1587 individuals (response rate 65.7%). Respondents differed little from the overall Russian population in terms of age, sex, education, and voting intention.
MAIN OUTCOME MEASURES—Prevalence of current and past smoking.
RESULTS—Smoking is common among males of all ages and in all areas. Of those aged 18-24 years, 65% smoke, rising to 73% in those aged 25-34 and then falling steadily to reach 41% in those aged 65 and older. Among women, smoking is much more common among the young (27% in those aged 18-34) than among the middle-aged and elderly (5% in those aged 55 and older), and more common among those living in urban areas than in rural areas. Smoking is also more common among men and women suffering material deprivation but there is no independent association with education. Among men, but not women, church attendance is inversely associated with smoking. In both sexes, but especially women, heavy drinking and smoking are associated.
CONCLUSIONS—Tobacco poses a major threat to the health of future generations in Russia, especially among women. A robust policy response is required.


Keywords: prevalence; Russia; smoking PMID:9706750

  5. Ice Complex formation in arctic East Siberia during the MIS3 Interstadial

    NASA Astrophysics Data System (ADS)

    Wetterich, Sebastian; Tumskoy, Vladimir; Rudaya, Natalia; Andreev, Andrei A.; Opel, Thomas; Meyer, Hanno; Schirrmeister, Lutz; Hüls, Matthias

    2014-01-01

    A continuous 15 m long sequence of Ice Complex permafrost (Yedoma) exposed in a thermo-cirque at the southern coast of Bol'shoy Lyakhovsky Island (New Siberian Archipelago, Dmitry Laptev Strait) was studied to reconstruct past landscape and environmental dynamics. The sequence accumulated during the Marine Isotope Stage 3 (MIS3) Interstadial between >49 and 29 ka BP in an ice-wedge polygon. The frozen deposits were cryolithologically described and sampled on a vertical bluff between two ice wedges. According to sedimentological and geochronological data, the section is subdivided into three units which correlate with environmental conditions of the early, middle, and late MIS3 period. Palynological data support this stratification. The stable isotope signature of texture ice in the polygon structure reflects fractionation due to local freeze-thaw processes, while the signature of an approximately 5 m wide and more than 17 m high ice wedge fits very well into the regional stable-water isotope record. Regional climate dynamics during the MIS3 Interstadial and local landscape conditions of the polygonal patterned ground controlled the Ice Complex formation. The sequence presented here completes previously published MIS3 permafrost records in Northeast Siberia. Late Quaternary stadial-interstadial climate variability in arctic West Beringia is preserved at millennial resolution in the Ice Complex. A MIS3 climate optimum was revealed between 48 and 38 ka BP from the Ice Complex on Bol'shoy Lyakhovsky Island.

  6. [Basic features of the nemoral curculionid-beetle fauna (Coleoptera, Curculionoidea) from eastern Europe and Western Siberia].

    PubMed

    Legalov, A A

    2011-01-01

    There are 132 curculionids associated with deciduous trees in eastern Europe and western Siberia. The weevils and bark beetles make up the basis of the fauna, forming almost 80%. The fauna of oak is the richest (64 species). The species composition on the ash-tree (50% are monophages) is highly original. Impoverishment of the species composition from the west to the east is revealed. The fauna declines by 18% from 45 to 550 E. The species composition reduces two times beyond the Urals. The faunal boundaries are revealed from west to east and from east to west. The most significant boundary (47% of the fauna do not pass it) for distribution of species to the east is situated between 40 and 45 degrees E. Two significant faunal boundaries are revealed from south to north. The fauna of curculionids of deciduous trees is formed by four groups of species. The southern European species (54%) and western palaearctic species (40%) dominate. The species composition of the studied territory is similar to the fauna of Middle Europe. Formation of the modern fauna of curculionids of deciduous trees in eastern Europe probably occurred in the Holocene. The western Palaearctic and Transpalaearctic species could have occupied the considered territory since the Late Pleistocene. Southern European species appeared in the considered territory after the Valdai glaciation during the warming in the Atlantic period of the Holocene. Penetration of East Palaearctic species began rather recently (last few decades), probably due to climate warming and economic activities.

  7. Prevalence of type 2 diabetes in northern populations of Siberia.

    PubMed

    Dogadin, S A; Mashtakov, B P; Taranushenko, T E

    2001-04-01

    In the first part of the study the prevalence and incidence of diagnosed Type 2 diabetes among adult rural populations of southern, central and northern areas of the Krasnoyarsk region of Siberia is compared. The six-year mean incidence of diabetes in the southern area was 0.86 per 1000 (95% CI: 0.66-1.06), in the central area this incidence was 0.79 (0.57-1.01). In contrast, in the northern area the mean Type 2 incidence among indigenous population was 0.16 per 1000 (0-0.43) and among aliens it was 0.38 (0.22-0.54). The age-standardised Type 2 diabetes prevalence in the population of southern and central areas were 10.23 (9.55-10.-92) and 10.77 (9.99-11.55), respectively. In the northern area among aliens it was 8.98 (8.18-9.78) and among indigenous peoples only 2.54 per 1000 (1.46-3.62). The second part of this study consists of a population based survey to determine the prevalence rate of Type 2 diabetes among 596 Evenks and 306 alien inhabitants in Evenkia (82% eligible participants of Baikit district). No cases of glucose intolerance were found among Evenks in this study and one case of Type 2 diabetes was confirmed among aliens (prevalence rate 3.27 per 1000). These data indicate that Type 2 diabetes is still rare among northern indigenous populations of Siberia and that diabetes in northern alien populations is less prevalent than among peoples of central and southern areas of Siberia.

  8. [Testate amoebae inhabiting middle taiga bogs in Western Siberia].

    PubMed

    Kur'ina, I V; Preĭs, Iu I; Bobrov, A A

    2010-01-01

    The population of testate amoebae from the most typical middle taiga bogs of Western Siberia have been studied. More than one hundred (103) species and intraspecific taxons of testate amoebae have been revealed in recent surface samples. The relation between ecological characteristics of habitats and the composition of a Protozoa population has been demonstrated. The ecological preferences of species concerning the index of wetness, ash level, and acidity have been revealed. Using the correspondence analysis, the ecological optimums and the tolerance of species and intraspecific taxons of testate amoebae have been established.

  9. Influence of Surface Condition over Siberia on the East Asian Climate

    NASA Astrophysics Data System (ADS)

    Arai, M.; Kimoto, M.

    2006-12-01

    Using observational data and atmospheric general circulation model, relationship between surface condition over Siberia and circulation over East Asia is examined. We notice particularly the influence of springtime surface temperature over Siberia, which becomes high when the snowmelt is encouraged in situ. It is found that when the surface temperature over Siberia is high in April, blocking events over northeastern Siberia and the Okhotsk Sea in May and June occur more frequently than climatology. In the year when the surface temperature over Siberia is high, a jet stream over the north of Siberia is formed in the upper troposphere corresponding to the enhanced meridional temperature gradient, and the polar frontal jet is observed earlier than climatology. Blocking anticyclones over northeastern Siberia and the Okhotsk Sea is considered to be formed by Rossby wave propagation along the polar frontal jet in early summer. Therefore, the early establishment of the polar frontal jet is consistent with the increase of the blocking frequency. Associated with the enhancement of blocking activity is the intensification of the surface Okhotsk high, and cold anomaly to its south over the northern part of Japan during the early summer season. The amplified Okhotsk high also causes the enhancement of the Baiu front, which is a part of East Asian monsoon. The finding of this study suggests monitoring the springtime surface condition over northern Siberia as one of the promising predictors for the early summer climate over East Asia. We also examined the future climate change on the Eurasian Continent and East Asia due to the global warming, using a general circulation model. The surface temperature over Siberia increases and springtime snowmelt is enhanced under doubled CO2 condition. Summertime blocking anticyclones are also increased and the Baiu front is enhanced, compared with the simulation of the present climate. These results are manifestation of relationship between

  10. The evolutionary history of sharp- and blunt-snouted lenok (Brachymystax lenok (Pallas, 1773)) and its implications for the paleo-hydrological history of Siberia

    PubMed Central

    2008-01-01

    Background Broad-scale phylogeographic studies of freshwater organisms provide not only an invaluable framework for understanding the evolutionary history of species, but also a genetic imprint of the paleo-hydrological dynamics stemming from climatic change. Few such studies have been carried out in Siberia, a vast region over which the extent of Pleistocene glaciation is still disputed. Brachymystax lenok is a salmonid fish distributed throughout Siberia, exhibiting two forms hypothesized to have undergone extensive range expansion, genetic exchange, and multiple speciation. A comprehensive phylogeographic investigation should clarify these hypotheses as well as provide insights on Siberia's paleo-hydrological stability. Results Molecular-sequence (mtDNA) based phylogenetic and morphological analysis of Brachymystax throughout Siberia support that sharp- and blunt-snouted lenok are independent evolutionary lineages, with the majority of their variation distributed among major river basins. Their evolutionary independence was further supported through the analysis of 11 microsatellite loci in three areas of sympatry, which revealed little to no evidence of introgression. Phylogeographic structure reflects climatic limitations, especially for blunt-snouted lenok above 56° N during one or more glacial maxima. Presumed glacial refugia as well as interbasin exchange were not congruent for the two lineages, perhaps reflecting differing dispersal abilities and response to climatic change. Inferred demographic expansions were dated earlier than the Last Glacial Maximum (LGM). Evidence for repeated trans-basin exchange was especially clear between the Amur and Lena catchments. Divergence of sharp-snouted lenok in the Selenga-Baikal catchment may correspond to the isolation of Lake Baikal in the mid-Pleistocene, while older isolation events are apparent for blunt-snouted lenok in the extreme east and sharp-snouted lenok in the extreme west of their respective

  11. Vertical plate motions in the West Siberian Basin

    NASA Astrophysics Data System (ADS)

    Vibe, Yulia

    2014-05-01

    The West Siberian Basin is a sedimentary basin situated between the Ural Mountains and the Siberian Craton. The Basin has experienced several periods of subsidence and uplift since the arrival of the Siberian Traps c. 250 Ma. Although the Basin is extensively explored and hosts large reserves of Oil and Gas, the forces driving the vertical motions are poorly understood. In this work we attempt to analyse the amount, timing and location of subsidence and uplift in the Basin to shed light on the possible causes of these motions. A detailed description of sedimentary layers is published in a number of Soviet-era books and articles and serves as a basis for our research. This data is first converted into sediment grids through time. Subsequently, the sediments, the sediment load and the compaction are taken into account ('backstripping') to produce the depth of the Basin at respective time steps. With this technique we calculate the tectonic component of subsidence. Uncertainties related to uplift events are estimated by the unconformities in the stratigraphic charts. One of the possible driving forces of vertical motions is a change of force balance arising at plate boundaries. Since active plate tectonics have been absent from West Siberia since the formation of the Urengoy and Khodosey Rifts, c. 250Ma, we study the far-field tectonic effects as a potential driving mechanism. Indeed, some of the significant vertical events in the West Siberian Basin coincide with the major tectonic events around Siberia. An example is the spreading in the Arctic (Eurasian Basin) in the Eocene (56 Ma) which was synchronous with initiation of uplift events in the northern part of West Siberia. In the middle Oligocene (33 Ma), the northern and eastern parts of the basin were subjected to uplift as subsidence migrated southwards and the Basin rose above the sea level. This was coincident with the changes of plate motions in the northern North Atlantic and Indo-European collision.

  12. Fe-U-PGE-Au-Ag-Cu Deposits of the Udokan-Chiney Region (East Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Gongalskiy, B.; Krivolutskaya, N.; Murashov, K.; Nistratov, S.; Gryazev, S.

    2012-04-01

    Introduction. Cupriferous sandstones-shales and magmatic copper-nickel deposits mark out the western and southern boundaries of the Siberian Craton accordingly. Of special interest are the Paleoproterozoic deposits of the Udokan-Chiney mining district (Gongalskiy, Krivolutskaya, 2008). Copper reserves and resources of this region are estimated at more than 50 Mt. Half of them is concentrated at the unique Udokan Deposit and the second half is distributed among sedimentary (Unkur, Pravoingamakitskoye, Sakinskoye, Krasnoye, Burpala) and magmatic deposits of the Chiney (Rudnoye, Verkhnechineyskoye, Kontaktovoye), Luktur and Maylav massifs. Results. It was established that the ores are characterized by similarity in chemical composition (main, major and rare elements that are Ag, Au, PGE) and mineral assemblages with varying proportions. It is important to emphasize that Fe role in mineralization was previously ignored. Meanwhile the Udokan deposit contains 10 Mt of magnetite metacrystals so as chalcocite ores may contain up to 50% magnetite too. It has been recently found that the Chiney titanomagnetite ores comprise commercially significant uranium and rare-earth metal concentrations (Makaryev et al., 2011). Thus the Udokan-Chiney region comprises Cu, Fe, Ti, V, U, REE, Ag, Au, PGE. These deposits differ from similar objects, the Olympic Dam in particular, by a much smaller content of fluid-bearing minerals. Copper mineralization at the Udokan is represented by chalcocite-bornite ores. They occur as ore beds conformable with sedimentary structures or as cross-cutting veins. The central zones of the former are often brecciated. They are rimmed by fine magnetite, bornite, and chalcocite dissemination. Bornite-chalcopyrite and chalcopyrite-pyrite veins are known at the lower levels of the Udokan ore bed. Such ore compositions are predominant in other ore deposits in sedimentary rocks (Pravoingamakitskoye, Unkur) and have a hydrothermal origin. Silver grades are up to 370 g/t in grab samples (Gongalskiy et al., 2008a). The long-lived Udokan-Chiney ore-magmatic has small areal extent of explosive rocks and breccias (n*10 m) with massive sulfide veins (chalcopyrite, pyrrhotite) which are similar to Sudbury offset dikes. While the same vertical zones at the Rudnoye deposit have been confirmed over 0.5 km downward from the lower contact of the Chiney massif. Conclusions. Multielement and similar mineralogical composition ores of different deposits in the Udokan-Chiney area reflect long evolution of ore processes in very movable block of the crust. Observed combination of magmatic, sedimentary and partially hydrothermal deposits is a result of the telescoping of a wide range of metals into a limited area.

  13. A long-living species of the hydrophiloid beetles: Helophorus sibiricus from the early Miocene deposits of Kartashevo (Siberia, Russia)

    PubMed Central

    Fikáček, Martin; Prokin, Alexander; Angus, Robert B.

    2011-01-01

    Abstract The recent hydrophiloid species Helophorus (Gephelophorus) sibiricus (Motschulsky, 1860) is recorded from the early Miocene deposits of Kartashevo assigned to the Ombinsk Formation. A detailed comparison with recent specimens allowed a confident identification of the fossil specimen, which is therefore the oldest record of a recent species for the Hydrophiloidea. The paleodistribution as well as recent distribution of the species is summarized, and the relevance of the fossil is discussed. In addition, the complex geological settings of the Kartashevo area are briefly summarized. PMID:22259280

  14. Direct observations of reactive atmospheric gases at ZOTTO station in the middle of Siberia as a base for large-scale modeling of atmospheric chemistry over Northern Eurasia

    NASA Astrophysics Data System (ADS)

    Skorokhod, Andrey; Belikov, Igor; Shtabkin, Yury; Moiseenko, Konstantin; Pankratova, Natalia; Vasileva, Anastasia; Rakitin, Vadim; Heimann, Martin

    2015-04-01

    polluted cases which are quite regular CO may increase till 400 ppb and more. Most uncertainties are due to the wild fires, which are often in different regions of Siberia. Numerical assessment of climatically important natural and anthropogenic emission sources influencing observed CO and O3 concentrations and their seasonal variability was made using GEOS-Chem model. According to the results, during the cold period CO concentrations in the surface layer is largely driven atmospheric transport from anthropogenic sources in Western Europe (up to 20 ppb), south of European Russia (up to 35 ppb) and south-western Siberia (up to 28 ppb). During the warm season they are usually affected by air transport from eastern Siberia, where the main contribution to the CO emissions are biogenic VOC oxidation (up to 15 ppb) and wildfires (up to 12 ppb). Transport of pollutants from south-western Siberia can add about 2,5 ppb to the ozone summer level in Central Siberia. In wintertime this factor leads to a reduced surface ozone level by 2 ppb. The contribution of large remote emission sources (Europe) is estimated within 1 ppb. Generally the simulation results indicate a significant role of long-range air transport in addition to regional natural and anthropogenic sources of air pollution which determine the total balance of surface CO. These processes need to be considered in quantitative analyses of the factors that determine the long-term photochemical system evolution in the lower troposphere over the continental regions of Northern Eurasia. This work was supported by the Russian Scientific Fund under grant 14-47-00049.

  15. [NEW FINDINGS OF BAT ECTOPARASITES (CHIROPTERA: VESPERTILIONIDAE) IN SOUTHERN SIBERIA].

    PubMed

    Orlova, M V; Zhigalin, A V; Khritankov, A M

    2015-01-01

    The data on new findings of ectoparasites (mites and insects) of bats (Chiroptera: Vespertilionidae) in the Western Sayan and Tuva are represented. The bat fly Basilia mongolensis mongolensis Theodor, 1966 was discovered in the territory of Russia for the first time. Gamasid mite Spinturnix bregetovae Stanyukovich, 1995 is new for the region. New hosts were described for some ectoparasites.

  16. Airborne studies of submicron aerosol in the troposphere over West Siberia

    SciTech Connect

    Panchenko, M.V.; Zuev, V.E.; Belan, B.D.; Terpugova, S.A.

    1996-04-01

    Submicron fraction particles that have the longest lifespan and are included in almost all atmospheric processes are of special importance among the great variety of sizes of particles present in the atmosphere. Submicron particles mainly determine the opticle state of the atmosphere in the visible spectral range, essentially cause the absorption of infrared radiation and, since they are the products and participants in all aerosol-to-gas transformations, accumulate of a lot of various chemical compounds and transfer them to large distances. Investigation of the processes of the spatial-temporal variability of aerosol particles for different climatic zones of the earth is the experimental base for studying their effect on climatically and ecologically significant factors and estimating their unfavorable tendencies. The increasing anthropogenic loading of the earth`s atmosphere is creating an urgency for aerosol research. Regardless of how perfect the analytical and numerical methods of solving radiation problems may be, success in forecasting climatic change is mainly determined by the reliability of the experimental data on optical parameters of the atmosphere and of the description of their variability under the effect of external factors.

  17. [Transformation of soil organic matter in microarthropod community from the Northern Taiga of West Siberia].

    PubMed

    Mordkovich, V G; Berezina, O G; Liubechanskiĭ, I I; Andrievskiĭ, V S; Marchenko, I I

    2006-01-01

    Recolonization of defaunated soil by springtails as well as by gamasid and oribatid mites and the changes in organic matter content of soil were studied in the northern taiga. After a one-year exposure in gauze bags (1.7 mm mesh), the abundance of microarthropods was higher but the number of species was lower compared to the surrounding soil. Large surface and litter forms did not colonize the samples, while the number of small and/or soil forms was higher. Soil samples inaccessible for microarthropods (0.15 mm mesh) were depleted of organic carbon compared to both surrounding soil and recolonized samples. The content of humic and fulvic acids was higher in the samples inaccessible to microarthropods. Humification processes prevailed in soils in the absence of microarthropods.

  18. Measurements of Ultra-fine and Fine Aerosol Particles over Siberia: Large-scale Airborne Campaigns

    NASA Astrophysics Data System (ADS)

    Arshinov, Mikhail; Paris, Jean-Daniel; Stohl, Andreas; Belan, Boris; Ciais, Philippe; Nédélec, Philippe

    2010-05-01

    In this paper we discuss the results of in-situ measurements of ultra-fine and fine aerosol particles carried out in the troposphere from 500 to 7000 m in the framework of several International and Russian State Projects. Number concentrations of ultra-fine and fine aerosol particles measured during intensive airborne campaigns are presented. Measurements carried over a great part of Siberia were focused on particles with diameters from 3 to 21 nm to study new particle formation in the free/upper troposphere over middle and high latitudes of Asia, which is the most unexplored region of the Northern Hemisphere. Joint International airborne surveys were performed along the following routes: Novosibirsk-Salekhard-Khatanga-Chokurdakh-Pevek-Yakutsk-Mirny-Novosibirsk (YAK-AEROSIB/PLARCAT2008 Project) and Novosibirsk-Mirny-Yakutsk-Lensk-Bratsk-Novosibirsk (YAK-AEROSIB Project). The flights over Lake Baikal was conducted under Russian State contract. Concentrations of ultra-fine and fine particles were measured with automated diffusion battery (ADB, designed by ICKC SB RAS, Novosibirsk, Russia) modified for airborne applications. The airborne ADB coupled with CPC has an additional aspiration unit to compensate ambient pressure and changing flow rate. It enabled to classify nanoparticles in three size ranges: 3-6 nm, 6-21 nm, and 21-200 nm. To identify new particle formation events we used similar specific criteria as Young et al. (2007): (1) N3-6nm >10 cm-3, (2) R1=N3-6/N621 >1 and R2=N321/N21200 >0.5. So when one of the ratios R1 or R2 tends to decrease to the above limits the new particle formation is weakened. It is very important to notice that space scale where new particle formation was observed is rather large. All the events revealed in the FT occurred under clean air conditions (low CO mixing ratios). Measurements carried out in the atmospheric boundary layer over Baikal Lake did not reveal any event of new particle formation. Concentrations of ultra

  19. Estimation of Fire Radiative Energy in Siberia Using MODIS Data

    NASA Astrophysics Data System (ADS)

    Shvetsov, Eugene; Ponomarev, Evgenii

    2014-05-01

    The intensity of heat release during biomass combustion is an important characteristic of wildfires. Space-borne systems, such as MODIS radiometer, provide observations of fire locations, as well as an estimate of the amount of radiant energy emitted by the fire. Such measures of fire radiative power (FRP) provide information on the fireline heat release intensity and on the rate of biomass combustion in large scale and are important for the analysis of fire impact on vegetation. In this study we analyzed the spatial distribution and temporal dynamics of detected wildfires in Siberia considering their radiative power. For the analysis we used database of fire detections made by MODIS instrument located on TERRA and AQUA satellites for 2002- 2013. For the detected fire pixels the frequency of their occurrence was calculated depending on the radiative power. More than 80% of all detected pixels had radiative power less than 100 MW. The distribution of fires according to their radiative power values was obtained for different regions of Siberia characterized by various vegetation and climatic conditions. Geospatial analysis performed using vegetation maps for the territory of Siberia and GIS layers of active fire detections showed that fires in deciduous and pine forests generally had lower intensities than fires in larch and spruce/fir forests. The rate of biomass combustion and the amount of heat emitted are strongly related to fuel moisture and therefore to weather conditions. In this study weather conditions were characterized using Russian and Canadian weather fire danger indices. Using images obtained during day and night satellite passes daily and long-term dynamics of fire radiative power was calculated. The long-term dynamics of fire radiative power measured by MODIS sensor was compared to weather fire danger indices calculated using on-ground weather stations data located in several Siberian regions mostly liable to fires. For most of the weather stations

  20. Aerospace Medical Support in Russia

    NASA Technical Reports Server (NTRS)

    Castleberry, Tara; Chamberlin, Blake; Cole, Richard; Dowell, Gene; Savage, Scott

    2011-01-01

    This slide presentation reviews the role of the flight surgeon in support of aerospace medical support operations at the Gagarin Cosmonaut Training Center (GCTC), also known as Star City, in Russia. The flight surgeon in this role is the medical advocate for non-russian astronauts, and also provides medical care for illness and injury for astronauts, family members, and guests as well as civil servants and contractors. The flight surgeon also provides support for hazardous training. There are various photos of the area, and the office, and some of the equipment that is used.

  1. Emission of greenhouse gases from geographically isolated wetlands of Western Siberia

    NASA Astrophysics Data System (ADS)

    Golovatskaya, E.; Dyukarev, E.; Veretennikova, E.

    2014-12-01

    Wetlands are integral components of landscapes with specific nutrient dynamics and carbon sequestration potentials, which frequently differ, based on hydroperiod and seasonal hydropattern, as well as the constituent concentration of inputs, site-specific storages and vegetation structures. Human modifications have the potential to significantly alter controls on carbon dynamics. This study focused on determining carbon emissions (CO2 and CH4) from geographically isolated peatlands within the Ob-Tom River Interfluve area of Western Siberia affected by water diversion for municipal use by the city of Tomsk, Russia. Two oligotrophic wetlands within the study area were selected for site-specific CO2 studies, the Timiryazevskoe (16 ha) and Kirsanovskoe wetlands (29 ha), both affected by the Tomsk water intake (177 water wells 250 000 m3 water daily). Measurements of СО2 and CH4 emissions from peat surfaces were carried out bi-monthly in growing periods from 2008-2013 in two dominate vegetation zones, pine- shrub-sphagnum phytocenosis (ryam) and sedge-sphagnum fens. СО2 emissions were measured using OPTOGAS-500.4 infrared gas analyzer and dark chamber. Methane emissions were measured using static chamber method. Air samples were collected by syringes and analyzed at gas chromatograph Shimadzu-GC14B. Observations were accompanied by measurement of air temperature and humidity, surface temperature, peat temperature at various depths and the water table level. CО2 emission over the vegetative growing period had clearly pronounced seasonal dynamics with maximum values in the middle of the growing season (mid-July) and minimum values in spring and autumn. The average total flux over the studied period is 123±55 gС/m2 at sedge-sphagnum fen of Kirsanovskoe wetland and 323±66 gС/m2 at fen of Timiryazevskoe wetland. Total СО2 flux for the snow-free period at ryam sites of Timiryazevskoe and Kirsanovskoe wetlands is 238±84 and 260±47 gС/m2 accordingly. Methane

  2. Soil Organic Matter in Forest Ecosystems of the Forest-tundra zone of Central Siberia

    NASA Astrophysics Data System (ADS)

    Mukhortova, Liudmila

    2010-05-01

    Our study was conducted on 17 forest sample plots in the forest-tundra zone of Central Siberia, Krasnoyarsk region, Russia. They were covered by larch/feather moss/shrub and larch/grass forest types growing on cryozems and podburs (Cryosols). The investigation was aimed at estimating soil organic matter storage and structure in forest ecosystems growing along the northern tree line. Such ecosystems have low rates of exchange processes and biological productivity. Estimating soil carbon in these forest types is important for a deeper understanding of their role in biogeochemical cycles and forecasting consequences of climate changes. Soil organic matter was divided into pools by biodegradation resistance level and, hence, different roles of these pools in biological cycles. The soil organic matter was divided into an easily mineralizable (LMOM) fraction, which includes labile (insoluble) (LOM) and mobile (soluble) (MOM) organic compounds, and a stable organic matter fraction that is humus substances bound with soil matrix. The forest-tundra soil carbon was found to total 30.9 to 125.9 tons/ha. Plant residues were the main part of the soil easily mineralizable organic matter and contained from 13.3 to 62.4% of this carbon. Plant residue carbon was mainly allocated on the soil surface, in the forest litter. Plant residues in the soil (dead roots + other "mortmass") were calculated to contribute 10-30% of the plant residues carbon, or 2.5-15.1% of the total soil carbon. Soil surface and in-soil dead plant material included 60-95% of heavily decomposed residues that made up a forest litter fermentation subhorizon and an "other mortmass" fraction of the root detritus. Mobile organic matter (substances dissolved in water and 0.1N NaOH) of plant residues was found to allocate 15-25% of carbon. In soil humus, MOM contribution ranged 14 to 64%. Easily mineralizable organic matter carbon appeared to generally dominate forest-tundra soil carbon pool. It was measured to

  3. Long-Term Measurements of Carbon Monoxide and Aerosols at the ZOTTO tall tower, Siberia

    NASA Astrophysics Data System (ADS)

    Mayer, J. C.; Birmili, W.; Heimann, M.; Heintzenberg, J.; Juergens, N.; Kisilyakhov, Y.; Panov, A.; Andreae, M. O.

    2009-12-01

    The Zotino Tall Tower Observatory (ZOTTO), operated by the Max Planck Institutes for Biogeochemistry and Chemistry and the Institute of Forest (Krasnoyarsk), is located at 89.35°E, 60.80°N, 114 m asl. in Siberia, Russia. It centers on a 300-m tower designed for scientific measurements of chemical (trace gases, aerosol) and physical (meteorological) properties at a very remote, continental site. The instrumentation at the observatory comprises a CO Monitor, a Particle Soot Absorption Photometer (PSAP) for determining the aerosol absorption coefficient, a nephelometer for the determination of the aerosol scattering coefficient, and a Differential Mobility Particle Sizer (DMPS) to measure the aerosol number size distribution. We present measurements made from October 2006 until May 2008, with some interruptions due to technical reasons. An annual cycle of CO was observed with summer minima around 80 ppb and winter maxima of about 180 ppb. Amplitude and phase of the annual cycle were comparable to that reported by NOAA-ESRL for latitude 61°N. Periods of elevated CO concentrations, typically lasting for one to three days, interrupted the mean annual cycle. Backward trajectories computed with the NOAA HYSPLIT model indicated changes of air mass origin associated with the CO peaks. It was found, that for several peaks air masses have passed over the region of Novosibirsk - a heavily industrialized area. During summer, very sharp peaks of CO concentration with no change of air mass origin were observed. In this case, local wild fires are most likely the cause of the increase of CO concentrations. This general picture was confirmed by the output of the MATCH (Model of Atmospheric Transport and Chemistry) model that predicted CO concentrations in good agreement with the measured CO concentration at the ZOTTO site, resembling the typical annual cycle of CO concentrations. Furthermore, some of the peaks related to changes of the air mass origin were also predicted by the

  4. Large-scale treeline changes recorded in Siberia

    NASA Astrophysics Data System (ADS)

    Esper, Jan; Schweingruber, Fritz H.

    2004-03-01

    Analysis of a multi-species network of western Siberian ecotone sites revealed pulses of tree invasion into genuine treeless tundra environments in the 1940s and 1950s and after the early 1970s. In addition, increases in radial stem growth synchronous to the late 20th century treeline change are observed. Both treeline changes and growth increases correspond with decadal-scale periods of temperature that are warmer than in any other period since observations started, suggesting - even if indirect - the sensitivity of large-scale treeline changes to this climatic forcing. The mid 20th century recruitment period reported here for the western Siberian network is compared with local findings from Europe and North America suggesting a circumpolar trend perhaps related to climate warming patterns. For western Siberia, the presence of relict stumps, nevertheless, indicates that this present colonization is reoccupying sites that had tree cover earlier in the last millennium.

  5. Linkage between seasonal hydrology and carbon flux dynamics in tundra ponds: Samoylov Island, Lena River Delta, Siberia

    NASA Astrophysics Data System (ADS)

    Abnizova, Anna; Bornemann, Niko; Boike, Julia

    2010-05-01

    Arctic ponds have been recently recognized as being highly sensitive to changing climate. To date, ponds and lakes are disappearing in Alaska, Siberia and Canadian High Arctic because of climate warming (Fitzgerald et al. 2003; Smith et al. 2005; and Smol et al. 2007). While numerous limnological studies have been done on arctic ponds located in the Canadian High Arctic (Douglas and Smol, 1994; Hamilton et al. 2001; Lim et al., 2001), there is a limited number of studies on tundra ponds located in other circumpolar environments (e.g. Northern Siberia). Duff et al. (1999) describes tundra lakes in northern Russia as clear, dilute, oligotrophic lakes with low nutrients and dissolved organic carbon concentration. While numerous ponds and lakes exists in the Lena River Delta averaging to 2120 lakes of all sizes for every 1000 km2, no studies have been done to understand carbon flux dynamics of these freshwater ecosystems. In this study hydrological monitoring based on water balance framework was applied to a series of ponds and lakes located on Samoylov Island, 120 km south of the Arctic Ocean in the southern central Lena River Delta (72° 22' N, 126 ° 30' E) from July to September 2008. To better understand spatial differences in pond hydrology and carbon flux dynamics, the physical and biochemical data was collected from 42 tundra ponds. The selection of the ponds was based on their size (small, medium, large) and depth values ranging from 10 to 120 cm. The estimation of the seasonal water budget in 2008 showed that losses through evapotranspiration were offset by similar precipitation inputs and resulted in the equilibrium storage values in the study ponds prior to the freeze-back. Preliminary analysis showed that more than 50% of the ponds had DOC > 6.5 mg/l which exceeds average value of other Arctic ponds reported in literature (Duff et al. 1999 and Hamilton et al. 2001). Elevated DOC concentrations (> 8 mg/l) were found in the small and medium ponds with depth

  6. What is the P value of Siberian soils? Soil phosphorus status in south-western Siberia and comparison with a global data set

    NASA Astrophysics Data System (ADS)

    Brédoire, Félix; Bakker, Mark R.; Augusto, Laurent; Barsukov, Pavel A.; Derrien, Delphine; Nikitich, Polina; Rusalimova, Olga; Zeller, Bernd; Achat, David L.

    2016-04-01

    Climate change is particularly strong in northern Eurasia and substantial ecological changes are expected in this extensive region. The reshaping and migration northwards of bioclimatic zones may offer opportunities for agricultural development in western and central Siberia. However, the bioclimatic vegetation models currently employed for projections still do not consider soil fertility, in spite of this being highly critical for plant growth. In the present study, we surveyed the phosphorus (P) status in the south-west of Siberia where soils have developed on loess parent material. We selected six sites differing in pedoclimatic conditions and the soil was sampled at different depths down to 1 m in aspen (Populus tremula L.) forest as well as in grassland areas. The P status was assessed by conventional methods and by isotope dilution kinetics. We found that P concentrations and stocks, as well as their distribution through the soil profile, were fairly homogeneous on the regional scale studied, although there were some differences between sites (particularly in organic P). The young age of the soils, together with slow kinetics of soil formation processes have probably not yet resulted in a sufficiently wide range of soil physico-chemical conditions to observe a more diverging P status. The comparison of our data set with similar vegetation contexts on the global scale revealed that the soils of south-western Siberia, and more generally of northern Eurasia, often have (very) high levels of total, organic and inorganic P. The amount of plant-available P in topsoils, estimated by the isotopically exchangeable phosphate ions, was not particularly high but was intermediate on the global scale. However, large stocks of plant-available P are stored in subsurface layers which currently have low fine-root exploration intensities. These results suggest that the P resource is unlikely to constrain vegetation growth and agricultural development under the present

  7. Diamondiferous eclogites from Siberia: Remnants of Archean oceanic crust

    NASA Astrophysics Data System (ADS)

    Jacob, D.; Jagoutz, E.; Lowry, D.; Mattey, D.; Kudrjavtseva, G.

    1994-12-01

    We have investigated eight diamond-bearing bimineralic eclogite xenoliths from the Udachnaya Mine, Yakutia, Siberia, in terms of major elements, 87Sr /86Sr- , 143Nd /144Nd and oxygen isotopic ratios. The β18O-values, measured with the new laser-fluorination technique, are different from mantle values and range between 5.19 and 7.38%. with an average error of 0.08%.. Strontium and neodymium initial isotopic ratios for cpx are between 0.70226 and 0.70699 and 0.51170 and 0.51257, respectively. Chemically and petrographically, the Siberian eclogites are very similar to the South African eclogite suite from Roberts Victor or Bellsbank, the most important similarities being the late Archean age (2.76 Ga) and the δ18O values that deviate from mantle values. However, differences exist in detail, as no samples with δ18O values lower than mantle values have yet been reported from Siberia and the cesium concentrations of the Siberian eclogites are generally lower than those of the Roberts Victor eclogite suite. The data obtained from the studied sample suite are best explained by a model proposing an origin from Archean oceanic crust that was intensely altered prior to subduction to mantle depths. Using oxygen isotopic values, the effects of seawater alteration can be shown and the composition of the unaltered protolith qualitatively estimated. We propose that mantle eclogites from kimberlites were generated by a globally operating subduction process during the late Archean and that differences between samples from different cratons are small compared to their similarities.

  8. Influence of Logging on the Effects of Wildfire in Siberia

    NASA Astrophysics Data System (ADS)

    Kukavskaya, Elena; Ivanova, Galina; Buryak, Ludmilla; Kalenskaya, Olga; Bogorodskaya, Anna; Zhila, Sergey; McRae, Douglas; Conard, Susan

    2013-04-01

    The Russian boreal zone supports a huge terrestrial carbon pool. Changes in this pool and related changes in land cover have global significance in terms of climate change. Moreover, it is a tremendous and largely untapped reservoir of wood products. The main natural disturbance in these forests is wildfire, which modifies the carbon budget and has potentially important climate feedbacks. In addition both legal and illegal logging are increasing in many forest areas of Siberia. From 2009 to 2012, we investigated a number of logged and unlogged sites to evaluate the impact of logging on wildfire characteristics and subsequent effects of wildfires on the ecosystem. The research was conducted in 3 different ecoregions of Siberia: taiga forest (Angara region), forest-steppe (Shushenskoe region), and mountain forest (Chita region). We analyzed fire effects in different forest types as a function of both the presence of logging and harvest methods. Logged areas often had higher fuel loads due to logging debris, and typically experienced higher severity fires than unlogged forests. We found large variations among sites depending on forest types, type of logging activity, and weather conditions prior to and during burning. Illegal logging resulted in much higher fire hazard than legal logging. Fuel consumption was highest on repeatedly burned areas, where ground cover was often burned to the mineral layer. Estimated carbon emissions were up to 5 times higher on logged areas than on unlogged sites. Soil respiration was less on both burned and logged areas than in undisturbed forest. Changing patterns in the harvest of wood products can be expected to increase the emissions and ecosystem damage from wildfires, inhibit recovery of natural ecosystems, and exacerbate impacts of wildland fire on changing climate and air quality. The research was supported by NASA LCLUC Program, RFBR grant # 12-04-31258, and Russian Academy of Sciences.

  9. Paleobiology of the Mesoproterozoic Billyakh Group, Anabar Uplift, northern Siberia

    NASA Technical Reports Server (NTRS)

    Sergeev, V. N.; Knoll, A. H.; Grotzinger, J. P.

    1995-01-01

    Silicified peritidal carbonates of the Mesoproterozoic Kotuikan and Yusmastakh Formations, Anabar Uplift, northeastern Siberia, contain exceptionally well-preserved microfossils. The assemblage is dominated by ellipsoidal akinetes of nostocalean cyanobacteria (Archaeoellipsoides) and problematic spheroidal unicells (Myxococcoides); both are allochthonous and presumably planktonic. The assemblage also includes distinctive mat-forming scytonematacean and entophysalidacean cyanobacteria, diverse short trichomes interpreted as cyanobacterial hormogonia or germinated akinetes, rare longer trichomes, and several types of colonial unicells. Although many taxa in the Kotuikan-Yusmastakh assemblage are long-ranging prokaryotes, the overall character of the assemblage is distinctly Mesoproterozoic, with its major features shared by broadly coeval floras from Canada, China, India, and elsewhere in Siberia. Microfossils also occur in middle to inner shelf shales of the Ust'-Il'ya and lower Kotuikan Formations. Leiosphaerid acritarchs (up to several hundred microns in diameter) characterize this facies. As in other Mesoproterozoic acritarch assemblages, acanthomorphic and other complex forms that typify Neoproterozoic assemblages are absent. The combination in Billyakh assemblages of exceptional preservation and low eukaryotic diversity supports the hypothesis that nucleated organisms diversified markedly near the Mesoproterozoic-Neoproterozoic boundary. The assemblages also demonstrate the antiquity of cyanobacteria capable of cell differentiation and suggest the importance of both changing peritidal substrates and evolving eukaryotes in determining stratigraphic patterns of Proterozoic prokaryotes. The permineralized assemblage contains 33 species belonging to 17 genera. Ten new species or new combinations are proposed: Archaeoellipsoides costatus n. sp., A. elongatus n. comb., A. dolichos n. comb., A. minor n. nom., A. crassus n. comb., A. major n. comb., A. bactroformis n

  10. Biomass burning emissions estimates in the boreal forests of Siberia

    NASA Astrophysics Data System (ADS)

    Kukavskaya, E. A.; Ivanova, G. A.; Soja, A. J.; Conard, S. G.

    2012-04-01

    Wildfire is the main boreal forest disturbance and can burn 10-30 million hectares annually, thus modifying the global carbon budget through direct fire emissions, postfire biogenic emissions, and by maintaining or altering ecosystems through establishing the beginning and end of successional processes. Fires in the Russian boreal forest range from low-severity surface fires to high-severity crown fires. Estimates of carbon emissions from fires in Russian boreal forests vary substantially due to differences in ecosystems types, burned area calculations, and the amount of fuel consumed. There is an urgent need to obtain more accurate and impartial fire carbon loss estimates in the boreal forests of Siberia due to their considerable contribution to the regional and global carbon balance. We examined uncertainties in estimates of carbon emissions. Area burned in the Siberian region was analyzed and compared using distinct methodologies. Differences between mapped ecosystems were also compared and contrasted to evaluate the potential for error resulting from disparate vegetation structure and fuel consumption estimates. Accurate fuel consumption estimates are obtained in the course of fire experiments with pre- and post-fire biomass measuring. Our large-scale experiments carried out in the course of the FIRE BEAR (Fire Effects in the Boreal Eurasia Region) Project provided quantitative and qualitative data on ecosystem state and carbon emissions due to fires of known behavior in major forest types of Siberia that could be used to verify large-scale carbon emissions estimates. Carbon emissions from fires vary annually and interannually and can increase several times in extreme fire years in comparison to normal fire years. Climate change and increasing drought length have increased the probability of high-severity fire occurrences. This would result in greater carbon losses and efflux to the atmosphere. This research was supported by NASA LCLUC Program, Fulbright

  11. The first record of "spelaeoid" bears in Arctic Siberia

    NASA Astrophysics Data System (ADS)

    Sher, Andrei V.; Weinstock, Jacobo; Baryshnikov, Gennady F.; Davydov, Sergey P.; Boeskorov, Gennady G.; Zazhigin, Vladimir S.; Nikolskiy, Pavel A.

    2011-08-01

    For a long time, "spelaeoid" (cave-bear-like) bears, Ursus ( Spelearctos) spp., were believed to be almost purely European animals. Their geographic range has recently been extended to the east, in southern Siberia, Transbaikalia, Kirghizia, Mongolia and Korea. Two unexpected new findings, presented here in detail, significantly change existing views on the distribution of cave bears; both were found in North-Eastern Siberia, far beyond the Arctic Circle, more than 1500 km to the north-east of the previously accepted range. One of the fossils is a mandible, found near the town of Cherskiy at 68.73°N, 161.38°E. The analysis of local geology and accompanying mammal fossils suggests that it comes from the Olyorian Fauna (Early to early Middle Pleistocene). Morphologically, the Cherskiy mandible is closest to Ursus savini, a small middle Pleistocene cave bear from the British Cromer Forest-bed Formation, but differs in having a slightly more advanced dentition, and thus it is described as a new subspecies Ursus savini nordostensis. Another newly recognized fossil of the "spelaeoid" bear is an astragalus found at the Oskhordokh site at 67.54°N, 135.67°E, on a large gravel bar on the right bank of the Adycha River. This specimen is attributed to Ursus cf . deningeri. The paper also presents an interesting example of the interaction between classical and "molecular" palaeontology. The new finds significantly change existing ideas on the ecology and evolution of cave bears, some of the most remarkable members of the extinct Pleistocene megafauna.

  12. Russia's Policy and Standing in Nanotechnology

    ERIC Educational Resources Information Center

    Terekhov, Alexander I.

    2013-01-01

    In this article, I consider the historical stages of development of nanotechnology in Russia as well as the political framework for this. It is shown that early federal nanotechnology programs in Russia date back to the 1990s and that since the mid-2000s, nanotechnology has attracted the increasing attention of government. I characterize the…

  13. 76 FR 47238 - Ammonium Nitrate From Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-08-04

    ... COMMISSION Ammonium Nitrate From Russia Determination On the basis of the record \\1\\ developed in the subject... order on ammonium nitrate from Russia would be likely to lead to continuation or recurrence of material... Commission are contained in USITC Publication 4249 (August 2011), entitled Ammonium Nitrate from...

  14. Russia [Teachers Guide and Student Readings].

    ERIC Educational Resources Information Center

    Allegheny County Schools, Pittsburgh, PA. Intercultural Understanding Project.

    This teaching unit, one of a series of curriculum guides on different world areas for use at the secondary level, treats the culture and history of Russia, oftentimes comparing it with that of the United States. Major teaching objectives are to have students compare and contrast basic geographic, cultural, and historical information on Russia and…

  15. A Holocene molluscan succession from floodplain sediments of the upper Lena River (Lake Baikal region), Siberia

    NASA Astrophysics Data System (ADS)

    White, Dustin; Preece, Richard C.; Shchetnikov, Alexander A.; Parfitt, Simon A.; Dlussky, Konstantin G.

    2008-05-01

    Floodplain sediments of the upper Lena River near Basovo in south-central Siberia have yielded the most detailed Holocene molluscan succession yet reported from the entire eastern Palaearctic. Over 72,500 shells from at least 28 species of terrestrial and 23 species of freshwater mollusc have been recovered, an abundance and diversity far higher than previously reported from the region. The molluscan assemblages are dominated by land snails, especially members of the genus Vallonia, represented by five species including Vallonia tenuilabris and two poorly known species Vallonia kamtschatica and Vallonia cf. chinensis. Other noteworthy species recovered include Gastrocopta theeli, Carychium pessimum, Vertigo extima (southernmost record), Vertigo microsphaera and the first Asian records of three other taxa ( Vertigo geyeri, Vertigo genesii and Vertigo parcedentata). Illustrations are provided for the critical species, since opinions differ about the status of various taxa and the correct names that should be used. The molluscan assemblages show clear successional trends during the early to mid-Holocene, reflecting episodes of dryness/wetness on the floodplain. Drier conditions at ca 6350 14C yr BP coincide with major changes in the archaeological record seen at other sites in the region but it remains unclear whether the two are linked. A prominent charcoal-rich horizon dated to ca 2800 14C yr BP marks a burning event in the catchment, which resulted in a two-fold increase in sediment accumulation rate. Remains of small mammals occurred throughout the sequence including a tooth of Microtus cf. maximowiczii, possibly the first occurrence of Ungar vole west of Lake Baikal. The faunal analyses have been integrated with a detailed pedological study of the sedimentary profile and a chronology was obtained by means of 12 AMS radiocarbon dates. This study provides the first detailed palaeoecological information relating to Holocene molluscan assemblages from the Cis

  16. The carbon balance of Russia

    NASA Astrophysics Data System (ADS)

    Dolman, Han; Shvidenko, Anatoly; Recapp Russia Synthesis Team

    2013-04-01

    We determine the net land to atmosphere flux of carbon in Russia, including Ukraine, Belarus and Kazakhstan using inventory based, eddy covariance, and inversion methods. Our high boundary estimate is -342 Tg C yr-1 from the eddy covariance method, and this is close to the upper bounds of the inventory based Land Ecosystem Assessment and inverse models estimate. A lower boundary estimate is provided at -1350 Tg C yr-1 from from the inversion models. The average of the three methods is -613.5 Tg C yr-1. The methane emission is estimated separately at 41.4 TgC yr-1. These three methods agree well within their respective error bounds. There is thus good consistency between bottom up and top down methods. The forests of Russia primarily cause the net atmosphere to land flux ( -692 Tg C yr-1 from the LEA) with remarkable little interannual variability. It remains however remarkable that the three methods provide such close estimates (-615, -662, -554 TgCyr-1) for NBP, given the inherent uncertainties in all of the approaches. The lack of recent forest inventories, the few eddy covariance sites and associated uncertainty with upscaling and under sampling of concentrations for the inversions are among the prime causes of the uncertainty. The DGVMs suggest a much lower uptake at -91Tg C yr-1 and we argue that this is caused by a high estimate of heterotrophic respiration compared to other methods.

  17. Analysis of the landscape structure in the tundra zone for western Siberia based on satellite data

    NASA Astrophysics Data System (ADS)

    Golubyatnikov, L. L.; Zarov, E. A.; Kazantsev, V. S.; Filippov, I. V.; Gavrilov, G. O.

    2015-12-01

    The landscape structure are investigated for typical and southern tundra subzones of western Siberia based on satellite images from Landsat and WorldView. The microlandscape types for the considered regions are selected and areas of microlandscapes are defined on the basis of satellite information and accounting data of field studies. The areas of the main wetland landscapes in the different types of bogs in northwestern Siberia are defined.

  18. Russia

    Atmospheric Science Data Center

    2013-04-16

    ... viewing. Each image covers an area about 345 kilometers x 278 kilometers. The Amur River, in the upper right, and Lake Bolon, at ... view due to sunglint (mirror-like reflection of the Sun's rays by the water). The Amur River valley is a primary breeding ground for ...

  19. The Migration Behavior of College Students in Siberia

    ERIC Educational Resources Information Center

    Gorbacheva, E. A.

    2008-01-01

    Given the conditions of the aging of the population of Russia there has been a steady decline in the size of the population, and starting in 2006 that includes a decline in the size of the working-age population. This is a very serious problem in regard to the social and economic development of the country, and the ways to solve the problem will…

  20. Precursor genes of future pandemic influenza viruses are perpetuated in ducks nesting in Siberia.

    PubMed

    Okazaki, K; Takada, A; Ito, T; Imai, M; Takakuwa, H; Hatta, M; Ozaki, H; Tanizaki, T; Nagano, T; Ninomiya, A; Demenev, V A; Tyaptirganov, M M; Karatayeva, T D; Yamnikova, S S; Lvov, D K; Kida, H

    2000-01-01

    Influenza A viruses of different subtypes were isolated from fecal samples of ducks in their nesting areas in Siberia in summer from 1996 to 1998. Phylogenetic analysis of the NP genes of the isolates in Siberia and those in Hokkaido, Japan on their flyway of migration from Siberia to the south in autumn revealed that they belong to the Eurasian lineage of avian influenza viruses. It is noted that the genes of the isolates in Siberia are closely related to those of H5N1 influenza virus strains isolated from chickens and humans in Hong Kong in 1997 as well as to those of isolates from domestic birds in southern China. The results indicate that influenza viruses perpetuated in ducks nesting in Siberia should have contributed genes in the emergence of the H5N1 virus in Hong Kong. Vaccine prepared from avirulent A/duck/Hokkaido/4/96 (H5N3) influenza virus was potent enough to protect mice from challenge with lethal dose of the pathogenic H5N1 virus [19]. Intensive surveillance study of aquatic birds especially in Siberia is, therefore, stressed to provide information on the future pandemic influenza virus strains and for vaccine preparation.

  1. The taiga tick Ixodes persulcatus (Acari: Ixodidae) in the Sakha Republic (Yakutia) of Russia: distributional and reproductive ranges.

    PubMed

    Uspensky, Igor; Garruto, Ralph M; Goldfarb, Lev

    2003-01-01

    The finding of an unfed adult female of the taiga tick Ixodes persulcatus Schulze is reported from the northern part of Eastern Siberia (the central part of the Sakha Republic [former Yakutia]) of Russia. This finding supplements other reported single findings of the taiga tick in different sites of the central part of the Sakha Republic, thus increasing its distributional range. The reproductive range of the taiga tick is limited to two separate areas in the southern parts of the Republic. The most probable mode of tick introduction northwards from the border of the reproductive range is by spring bird migrations from their wintering areas to breeding sites. The possibility of the establishment of stable tick populations in the areas of introduction is also considered.

  2. The history of the development of Ayurvedic medicine in Russia.

    PubMed

    Ragozin, Boris Vladimirovich

    2016-01-01

    Ayurveda is one of the world's oldest medical sciences, with a history that goes back more than 5,000 years. The knowledge of Ayurveda has at various times had an impact on a number of branches of medicine: From ancient Greek medicine in the West to the Chinese and Tibetan in the East. Ayurveda continues to retain its prominent position in our modern world, being officially recognised by the World Health Organisation (WHO) and enjoying great popularity in the US, Germany, Italy and the Netherlands. In India, Ayurveda is recognised by conventional medicine on a par with modern medical science. In the Soviet Union a strong interest in Ayurveda arose for the first time after the Chernobyl disaster, and since then Ayurveda has been actively developing in Russia. In this article we present the chronology of the development of Ayurvedic medicine in Russia since 1989, explore academic literature on the subject available in Russian and review the existing Ayurvedic products and services offered on the Russian market.

  3. The history of the development of Ayurvedic medicine in Russia

    PubMed Central

    Ragozin, Boris Vladimirovich

    2016-01-01

    Ayurveda is one of the world's oldest medical sciences, with a history that goes back more than 5,000 years. The knowledge of Ayurveda has at various times had an impact on a number of branches of medicine: From ancient Greek medicine in the West to the Chinese and Tibetan in the East. Ayurveda continues to retain its prominent position in our modern world, being officially recognised by the World Health Organisation (WHO) and enjoying great popularity in the US, Germany, Italy and the Netherlands. In India, Ayurveda is recognised by conventional medicine on a par with modern medical science. In the Soviet Union a strong interest in Ayurveda arose for the first time after the Chernobyl disaster, and since then Ayurveda has been actively developing in Russia. In this article we present the chronology of the development of Ayurvedic medicine in Russia since 1989, explore academic literature on the subject available in Russian and review the existing Ayurvedic products and services offered on the Russian market. PMID:27143798

  4. A 33,000-Year-Old Incipient Dog from the Altai Mountains of Siberia: Evidence of the Earliest Domestication Disrupted by the Last Glacial Maximum

    PubMed Central

    Ovodov, Nikolai D.; Crockford, Susan J.; Kuzmin, Yaroslav V.; Higham, Thomas F. G.; Hodgins, Gregory W. L.; van der Plicht, Johannes

    2011-01-01

    Background Virtually all well-documented remains of early domestic dog (Canis familiaris) come from the late Glacial and early Holocene periods (ca. 14,000–9000 calendar years ago, cal BP), with few putative dogs found prior to the Last Glacial Maximum (LGM, ca. 26,500–19,000 cal BP). The dearth of pre-LGM dog-like canids and incomplete state of their preservation has until now prevented an understanding of the morphological features of transitional forms between wild wolves and domesticated dogs in temporal perspective. Methodology/Principal Finding We describe the well-preserved remains of a dog-like canid from the Razboinichya Cave (Altai Mountains of southern Siberia). Because of the extraordinary preservation of the material, including skull, mandibles (both sides) and teeth, it was possible to conduct a complete morphological description and comparison with representative examples of pre-LGM wild wolves, modern wolves, prehistoric domesticated dogs, and early dog-like canids, using morphological criteria to distinguish between wolves and dogs. It was found that the Razboinichya Cave individual is most similar to fully domesticated dogs from Greenland (about 1000 years old), and unlike ancient and modern wolves, and putative dogs from Eliseevichi I site in central Russia. Direct AMS radiocarbon dating of the skull and mandible of the Razboinichya canid conducted in three independent laboratories resulted in highly compatible ages, with average value of ca. 33,000 cal BP. Conclusions/Significance The Razboinichya Cave specimen appears to be an incipient dog that did not give rise to late Glacial – early Holocene lineages and probably represents wolf domestication disrupted by the climatic and cultural changes associated with the LGM. The two earliest incipient dogs from Western Europe (Goyet, Belguim) and Siberia (Razboinichya), separated by thousands of kilometers, show that dog domestication was multiregional, and thus had no single place of origin (as

  5. Nuclear weapons and NATO-Russia relations

    SciTech Connect

    Cornwell, G.C.

    1998-12-01

    Despite the development of positive institutional arrangements such as Russian participation in the NATO-led peacekeeping force in Bosnia and the NATO- Russia Permanent Joint Council, the strategic culture of Russia has not changed in any fundamental sense. Russian strategic culture has not evolved in ways that would make Russian policies compatible with those of NATO countries in the necessary economic, social, technological, and military spheres. On the domestic side, Russia has yet to establish a stable democracy and the necessary legal, judicial, and regulatory institutions for a free-market economy. Russia evidently lacks the necessary cultural traditions, including concepts of accountability and transparency, to make these adaptations in the short-term. Owing in part to its institutional shortcomings, severe socioeconomic setbacks have afflicted Russia. Russian conventional military strength has been weakened, and a concomitant reliance by the Russians on nuclear weapons as their ultimate line of defense has increased. The breakdown in the infrastructure that supports Russian early warning and surveillance systems and nuclear weapons stewardship defense, coupled with a tendency towards has exacerbated Russian anxiety and distrust toward NATO. Russia`s reliance on nuclear weapons as the ultimate line of defense, coupled with a tendency toward suspicion and distrust toward NATO, could lead to dangerous strategic miscalculation and nuclear catastrophe.

  6. Fires in Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Numerous thermal anomalies were detected on the Kamchatka Peninsula in northeastern Russia in late June and early July by the Moderate Resolution Imaging Spectroradiometer (MODIS). Some of the anomalies (red dots) were fires, but at least one was the result of ongoing volcanic activity at one of the Peninsula's numerous active volcanoes. The erupting volcano, called Sheveluch, can be seen most clearly in the image from July 8, 2002. It is located in the upper right quadrant of the image, and appears as a grayish circular patch amid the surrounding green vegetation. In its center is a red dot indicating that MODIS detected a thermal signature coming from the restless volcano. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  7. Quo Vadis?: Russia's health challenges.

    PubMed

    Marquez, Patricio V

    2011-01-01

    The roots of the health crisis in the Russian Federation are not entirely, or even primarily, in the state of the health care system. High levels of mortality and morbidity, particularly among working-age males, reflect many other factors that transcend the health system as they are related to the aging of the population, growing urbanization, lifestyles and risky behaviours. Spending more money on healthcare, while necessary, will not be sufficient to improve Russia's health outcomes on a sustainable basis. A multisectoral strategy is required, coupled with increased health expenditures and structural reforms to improve the efficiency and effectiveness of healthcare organization, financing and service delivery. However, it should be clear that improving health outcomes is a complex, medium- to long-term undertaking that should be addressed forcefully by the government at the federal and regional levels as a priority social objective.

  8. Russia's energy policy: A framing comment

    SciTech Connect

    Aslund, A.

    2006-05-15

    A prominent specialist on the Russian economy provides a framing comment on two preceding papers entitled 'Russia's Energy Policy' (by Vladimir Milov, Leonard Coburn, and Igor Danchenko) and 'Russia's Energy Policy: A Divergent View' (by Matthew J. Sagers). The author argues that Russia's current energy policy should be viewed as an outcome of competition between three overlapping programs. In this context, he identifies three policy models - the old Soviet, the liberal or oligarchic, and the most recent state capitalist. The latter is currently supported by President Putin, who prioritizes diversification of the country's economy at the expense of diminished investments in the oil and gas sector.

  9. Influence of logging on the effects of wildfire in Siberia

    NASA Astrophysics Data System (ADS)

    Kukavskaya, E. A.; Buryak, L. V.; Ivanova, G. A.; Conard, S. G.; Kalenskaya, O. P.; Zhila, S. V.; McRae, D. J.

    2013-12-01

    The Russian boreal zone supports a huge terrestrial carbon pool. Moreover, it is a tremendous reservoir of wood products concentrated mainly in Siberia. The main natural disturbance in these forests is wildfire, which modifies the carbon budget and has potentially important climate feedbacks. In addition, both legal and illegal logging increase landscape complexity and affect burning conditions and fuel consumption. We investigated 100 individual sites with different histories of logging and fire on a total of 23 study areas in three different regions of Siberia to evaluate the impacts of fire and logging on fuel loads, carbon emissions, and tree regeneration in pine and larch forests. We found large variations of fire and logging effects among regions depending on growing conditions and type of logging activity. Logged areas in the Angara region had the highest surface and ground fuel loads (up to 135 t ha-1), mainly due to logging debris. This resulted in high carbon emissions where fires occurred on logged sites (up to 41 tC ha-1). The Shushenskoe/Minusinsk and Zabaikal regions are characterized by better slash removal and a smaller amount of carbon emitted to the atmosphere during fires. Illegal logging, which is widespread in the Zabaikal region, resulted in an increase in fire hazard and higher carbon emissions than legal logging. The highest fuel loads (on average 108 t ha-1) and carbon emissions (18-28 tC ha-1) in the Zabaikal region are on repeatedly burned unlogged sites where trees fell on the ground following the first fire event. Partial logging in the Shushenskoe/Minusinsk region has insufficient impact on stand density, tree mortality, and other forest conditions to substantially increase fire hazard or affect carbon stocks. Repeated fires on logged sites resulted in insufficient tree regeneration and transformation of forest to grasslands. We conclude that negative impacts of fire and logging on air quality, the carbon cycle, and ecosystem

  10. Season - dependent and source-influenced aerosol in Northern Siberia

    NASA Astrophysics Data System (ADS)

    Popovicheva, Olga; Makshtas, Alexander; Bogorodsky, Peter; Eleftheriadis, Kostantinos; Diapouli, Evangelia; Shonia, Natalia; Uttal, Taneil

    2016-04-01

    Aerosol may serve as a tracer of arctic pollution, allowing a link to climate response if its major characteristics relating to natural and anthropogeneous sources are defined. It has been shown that BC and sulfates are the most important aerosol constituents measured in the Arctic boundary layer; these species demonstrate similar seasonal variations with a peak during winter to early spring and a minimum in summer. Long - time gap in consistent aerosol observations in the Russian Arctic strongly limits the assessment of air pollution and climate impacts. On-line monitoring, sampling, and analyses of atmospheric aerosols were carried out at the Tiksi Hydrometeorological Observatory, Northern Siberia, during one year from September 2014 to 2015. Physico-chemical characterization combining aethalometry, thermo-optical analysis, and analytical chemistry was used in order to identify the seasonal variability of aerosols and to link their composition to possible sources, as well as to characterize the differences in aerosol chemical composition between natural background conditions and BC-pollution episodes. The present study reports the first results from the Tiksi Observatory on season-dependent and source-influenced characteristics of aerosol species, such as carbon fractions (OC, EC), inorganic and organic functionalities of chemical compounds, sulfates, nitrates and other ion components, and elements. In addition, data obtained by individual particles analysis provide insight into micromarkers of combustion sources. Aerosol at the Tiksi Observatory is found to be originated from natural marine, biogenic, and continental sources as well as influenced by local residential activity and regional pollution. Characterization of aerosols during OC and BC-pollution episodes, combined with analysis of the wind direction, atmosphere stability, and air mass trajectories, allows for the identification of the sources which are responsible for the emission of hazardous compounds

  11. Horizons West.

    ERIC Educational Resources Information Center

    Kitses, Jim

    The western is the most popular and enduring of Hollywood forms. It is one embodiment of a traditional theme in American culture: the West as both Garden of natural dignity and innocence and also as treacherous Desert resisting the gradual sweep of agrarian progress and community values. Westerns have in common: a) history, America's past; b)…

  12. Siberia Integrated Regional Study information-computational and instrumental infrastructure development

    NASA Astrophysics Data System (ADS)

    Gordov, E. P.; Kabanov, M. V.; Krutikov, V. A.; Kuzin, V. I.; Lykosov, V. N.; Okladnikov, I.; Titov, A. G.; Vaganov, E. A.

    2011-12-01

    Reported are several important steps in development of information-computational and instrumental infrastructure of the NEESPI mega-project Siberia Integrated Regional Study, which is devoted to investigation of global change impact on Siberia environment and related feedback. Firstly, development of scientific and technological basis and creation of a reference network for monitoring of climatic changes in Siberia is planned for 2012-2017. The network will include 12 reference monitoring stations equipped with modern instrumentation for monitoring spread across Siberia as well as data center aimed at storage of instrumental and modeling data and providing an access to those. The stations will be created at the following sites: Barnaul (Aktru), Chita (Arakhley), Irkutsk (Mondy), Khaty-Mansiisk (Shapsha), Krasnoyarsk (Zotino), Kyzyl (Dolinnaya), Nadym (Polyarnaya), Novosibirsk (Chany), Tomsk (Vasyuganie), Tomsk (Akademgorodok), Ulan-Ude (Istomino) and Yakutsk (Spasskaya Pad') and supported in operation by relevant SB RAS research Institutes and Siberian Universities. Also a suite of models is under development now, which will comprise global and regional climatic and meteorological models run at the Siberian Supercomputer Center. The CLEARS (CLimate and Environment Analysis and Research System) information-computational web-GIS is planned to be deployed at the data center and used for analysis of recent and future climatic and environmental changes in Siberia. Altogether these components will form a SB RAS megascience facility aimed at detailed monitoring of on-going natural and climatic processes on this territory and prognoses of their dynamics in future. It should create an information basis for decision-making on future socio-economic development of Siberia. It will also improve significantly efficiency of international scientific cooperation in Siberia.

  13. Quantitative estimates of Mid- to late Holocene Climate Variability in northeastern Siberia inferred from chironomids in lake sediments

    NASA Astrophysics Data System (ADS)

    Nazarova, Larisa; Diekmann, Bernhard; Pestrjakova, Ludmila; Herzschuh, Ulrike; Subetto, Dmitry

    2010-05-01

    Yakutia (Russia, northeastern part of Eurasia) represents one of Earths most extreme climatic settings in the world with deep-reaching frozen ground and a semiarid continental climate with highest seasonal temperature contrasts in the northern hemisphere. The amplitude of temperature variations around the year sometimes exceeds 100oC. There are few examples of quantitative palaeoecological studies in Siberia and these data have to be tested by quantitative studies from other sites in this region, inferred from different proxies and using regional calibration datasets and temperature models that are still lacking. Chironomid midges (Insecta, Diptera, Chironomidae) have been widely used to reconstruct past climate variability in many areas of Western Europe and North America. A chironomid-mean July air temperature inference model has been developed, based on a modern calibration set of 200 lakes sampled along a transect from 110° to 159° E and 61° to73° N in northern Russia. The inference model was applied to sediment cores from 2 lakes in the Central Yakutia in order to reconstruct past July air temperatures. The lacustrine records span mid- to late Holocene. The downcore variability in the chironomid assemblages and the composition of organic matter give evidence of climate-driven and interrelated changes in biological productivity, lacustrine trophic states, and lake-level fluctuations. Three phases of the climate development in Central Yakutia can be derived from the geochemical composition of the lake cores and according to the inferred from chironomid assemblages mean July air ToC. Content of organic matters reached maximal values in the period between 7000-4500 yBP. Sedimentation rate is especially high, numerous molluscs shells are found in sediments. All this along with the reconstructed air temperature confirmed that Mid Holocene optimum in Central Yakutia took place in this period with the maximal temperatures up to 4oC above present day ToC. Strong

  14. The Influences of Land Surface Properties on Soil Thermal Regimes in the Low Arctic of Northwestern Siberia

    NASA Astrophysics Data System (ADS)

    Epstein, H. E.; Frost, G. V., Jr.; Matyshak, G. V.; Walker, D. A.; Meakem, V. M.

    2014-12-01

    Understanding the feedbacks among climate, permafrost, and vegetation is crucial for assessments of arctic ecosystem vulnerability and response to climate change, and for development of sustainable engineering and management methods associated with infrastructure. Vegetation, snow cover, and near-surface soil organic layers are key determinants in regulating the energy exchange between the atmosphere and the deeper soils. Here we present high-temporal resolution soil thermal regime data over annual time extents for multiple sites at two locations in the Low Arctic of northwestern Siberia. At a location near Nadym, Russia, we measured soil temperatures at various depths in the soil profile (down to 60 cm) at three sites: 1) a boreal forest stand with lichen understory and a shallow organic layer (8 cm), 2) a young, cryoturbated Sphagnum peatland with soil organic layers to 40 cm depth, and 3) an old Sphagnum peatland with deep organic soil horizons (58+ cm). At a location near Kharp, Russia, we measured soil temperatures at 5 and 20 cm depth for sites along a chronosequence of tall alder shrub expansion, from short-statured tundra to mature and old alder stands, with deeper organic layers. The deeper snow accumulation at the Nadym forest site kept winter soil temperatures dramatically warmer than the peatland soils, up to 8 °C difference, but the shading of the forest tended to cool the surface during the summer. The overall effect of the forest was cooler summer soils in the near-surface layers, yet warmer summer soils at the deeper layers (20-60 cm). The forest location had substantially greater thawing degree days at depth (20-60 cm), compared to the Sphagnum peatlands. At the Kharp site, mature alder shrub stands cooled summer soil temperatures relative to shorter tundra by up to 8 °C (at 20 cm depth), yet warmed winter soils by greater than 10 °C. Mature and old shrubland locations had reduced thawing degree days at 20 cm depth relative to short

  15. Ancient DNA Reveals Prehistoric Gene-Flow from Siberia in the Complex Human Population History of North East Europe

    PubMed Central

    Der Sarkissian, Clio; Balanovsky, Oleg; Brandt, Guido; Khartanovich, Valery; Buzhilova, Alexandra; Koshel, Sergey; Zaporozhchenko, Valery; Gronenborn, Detlef; Moiseyev, Vyacheslav; Kolpakov, Eugen; Shumkin, Vladimir; Alt, Kurt W.; Balanovska, Elena; Cooper, Alan; Haak, Wolfgang

    2013-01-01

    North East Europe harbors a high diversity of cultures and languages, suggesting a complex genetic history. Archaeological, anthropological, and genetic research has revealed a series of influences from Western and Eastern Eurasia in the past. While genetic data from modern-day populations is commonly used to make inferences about their origins and past migrations, ancient DNA provides a powerful test of such hypotheses by giving a snapshot of the past genetic diversity. In order to better understand the dynamics that have shaped the gene pool of North East Europeans, we generated and analyzed 34 mitochondrial genotypes from the skeletal remains of three archaeological sites in northwest Russia. These sites were dated to the Mesolithic and the Early Metal Age (7,500 and 3,500 uncalibrated years Before Present). We applied a suite of population genetic analyses (principal component analysis, genetic distance mapping, haplotype sharing analyses) and compared past demographic models through coalescent simulations using Bayesian Serial SimCoal and Approximate Bayesian Computation. Comparisons of genetic data from ancient and modern-day populations revealed significant changes in the mitochondrial makeup of North East Europeans through time. Mesolithic foragers showed high frequencies and diversity of haplogroups U (U2e, U4, U5a), a pattern observed previously in European hunter-gatherers from Iberia to Scandinavia. In contrast, the presence of mitochondrial DNA haplogroups C, D, and Z in Early Metal Age individuals suggested discontinuity with Mesolithic hunter-gatherers and genetic influx from central/eastern Siberia. We identified remarkable genetic dissimilarities between prehistoric and modern-day North East Europeans/Saami, which suggests an important role of post-Mesolithic migrations from Western Europe and subsequent population replacement/extinctions. This work demonstrates how ancient DNA can improve our understanding of human population movements across

  16. Ancient DNA reveals prehistoric gene-flow from siberia in the complex human population history of North East Europe.

    PubMed

    Der Sarkissian, Clio; Balanovsky, Oleg; Brandt, Guido; Khartanovich, Valery; Buzhilova, Alexandra; Koshel, Sergey; Zaporozhchenko, Valery; Gronenborn, Detlef; Moiseyev, Vyacheslav; Kolpakov, Eugen; Shumkin, Vladimir; Alt, Kurt W; Balanovska, Elena; Cooper, Alan; Haak, Wolfgang

    2013-01-01

    North East Europe harbors a high diversity of cultures and languages, suggesting a complex genetic history. Archaeological, anthropological, and genetic research has revealed a series of influences from Western and Eastern Eurasia in the past. While genetic data from modern-day populations is commonly used to make inferences about their origins and past migrations, ancient DNA provides a powerful test of such hypotheses by giving a snapshot of the past genetic diversity. In order to better understand the dynamics that have shaped the gene pool of North East Europeans, we generated and analyzed 34 mitochondrial genotypes from the skeletal remains of three archaeological sites in northwest Russia. These sites were dated to the Mesolithic and the Early Metal Age (7,500 and 3,500 uncalibrated years Before Present). We applied a suite of population genetic analyses (principal component analysis, genetic distance mapping, haplotype sharing analyses) and compared past demographic models through coalescent simulations using Bayesian Serial SimCoal and Approximate Bayesian Computation. Comparisons of genetic data from ancient and modern-day populations revealed significant changes in the mitochondrial makeup of North East Europeans through time. Mesolithic foragers showed high frequencies and diversity of haplogroups U (U2e, U4, U5a), a pattern observed previously in European hunter-gatherers from Iberia to Scandinavia. In contrast, the presence of mitochondrial DNA haplogroups C, D, and Z in Early Metal Age individuals suggested discontinuity with Mesolithic hunter-gatherers and genetic influx from central/eastern Siberia. We identified remarkable genetic dissimilarities between prehistoric and modern-day North East Europeans/Saami, which suggests an important role of post-Mesolithic migrations from Western Europe and subsequent population replacement/extinctions. This work demonstrates how ancient DNA can improve our understanding of human population movements across

  17. Surveillance of tick-borne encephalitis virus in wild birds and ticks in Tomsk city and its suburbs (Western Siberia).

    PubMed

    Mikryukova, Tamara P; Moskvitina, Nina S; Kononova, Yulia V; Korobitsyn, Igor G; Kartashov, Mikhail Y; Tyuten Kov, Oleg Y; Protopopova, Elena V; Romanenko, Vladimir N; Chausov, Evgeny V; Gashkov, Sergey I; Konovalova, Svetlana N; Moskvitin, Sergey S; Tupota, Natalya L; Sementsova, Alexandra O; Ternovoi, Vladimir A; Loktev, Valery B

    2014-03-01

    To study the role of wild birds in the transmission of tick borne encephalitis virus (TBEV), we investigated randomly captured wild birds bearing ixodid ticks in a very highly endemic TBE region located in Tomsk city and its suburbs in the south of Western Siberia, Russia. The 779 wild birds representing 60 species were captured carrying a total of 841 ticks, Ixodes pavlovskyi Pom., 1946 (n=531), Ixodes persulcatus P. Sch., 1930 (n=244), and Ixodes plumbeus Leach. 1815 (n=66). The highest average number of ticks per bird in a particular species was found for the fieldfare (Turdus pilaris Linnaeus, 1758) (5.60 ticks/bird) and the tree pipit (Anthus trivialis Linnaeus, 1758) (13.25 ticks/bird). Samples from wild birds and ticks collected in highly endemic periods from 2006 to 2011 were tested for the TBEV markers using monoclonal modified enzyme immunoassay (EIA) and RT-PCR. TBEV RNA and antigen were found in 9.7% and 22.8% samples collected from wild birds, respectively. TBEV markers were also detected in 14.1% I. persulcatus ticks, 5.2% I. pavlovskyi, and 4.2% I. plumbeus ticks collected from wild birds. Two TBEV strains were also isolated on PKE (pig kidney embryo) cells from fieldfare and Blyth's reed warbler (Acrocephalus dumetorum Blyth, 1849). Sequencing of 5'-NCR of TBEV revealed that all TBEV isolates belong to Far Eastern (dominate) and Siberian genotypes. Several phylogenetic subgroups included TBEV sequences novel for the Tomsk region. Our data suggest that wild birds are potential disseminators of TBEV, TBEV-infected ixodid ticks, and possibly other tick-borne infections.

  18. Climatically induced interannual variability in aboveground production in forest-tundra and northern taiga of central Siberia.

    PubMed

    Knorre, Anastasia A; Kirdyanov, Alexander V; Vaganov, Eugene A

    2006-02-01

    To investigate the variability of primary production of boreal forest ecosystems under the current climatic changes, we compared the dynamics of annual increments and productivity of the main components of plant community (trees, shrubs, mosses) at three sites in the north of Siberia (Russia). Annual radial growth of trees and shrubs was mostly defined by summer temperature regime (positive correlation), but climatic response of woody plants was species specific and depends on local conditions. Dynamics of annual increments of mosses were opposite to tree growth. The difference in climatic response of the different vegetation components of the forest ecosystems indicates that these components seem to be adapted to use climatic conditions during the short and severe northern summer, and decreasing in annual production of one component is usually combined with the increase of other component productivity. Average productivity in the northern forest ecosystems varies from 0.05 to 0.14 t ha(-1) year(-1) for trees, from 0.05 to 0.18 t ha(-1) year(-1) for shrubs and from 0.54 to 0.66 t ha(-1) year(-1) for mosses. Higher values of tree productivity combined with lower annual moss productivity were found in sites in northern taiga in comparison with forest-tundra. Different tendencies in the productivity of the dominant species from each vegetation level (trees, shrubs, mosses) were indicated for the last 10 years studied (1990-1999): while productivity of mosses is increasing, productivity of trees is decreasing, but there is no obvious trend in the productivity of shrubs. Our results show that in the long term, the main contribution to changes in annual biomass productivity in forest-tundra and northern taiga ecosystems under the predicted climatic changes will be determined by living ground cover.

  19. Russia ends pact to curb uranium use

    NASA Astrophysics Data System (ADS)

    Allen, Michael

    2016-11-01

    The Russian government has terminated an agreement between the country's nuclear body, Rosatom, and the US Department of Energy (DOE) into the feasibility of converting research reactors in Russia to low-enriched uranium (LEU).

  20. The Social Position of Schoolteachers in Russia

    ERIC Educational Resources Information Center

    Il'in, V. A.; Shabunova, A. A.; Leonidova, G. V.

    2013-01-01

    Research on the teaching profession in Russia shows that teachers are characterized by low pay and low prestige. There is an urgent need to change this situation if the modernization and innovative development of Russian society are to be achieved.

  1. Glacial Refugium of Pinus pumila (Pall.) Regel in Northeastern Siberia

    SciTech Connect

    Shilo, N A; Lozhkin, A V; Anderson, P M; Brown, T A; Pakhomov, A Y; Solomatkina, T B

    2007-02-10

    One of the most glowing representatives of the Kolyma flora [1], ''Pinus pumila'' (Pall.) Regel (Japanese stone pine), is a typical shrub in larch forests of the northern Okhotsk region, basins of the Kolyma and Indigirka rivers, and high-shrub tundra of the Chukchi Peninsula. It also forms a pine belt in mountains above the forest boundary, which gives way to the grass-underbrush mountain tundra and bald mountains. In the southern Chukchi Peninsula, ''Pinus pumila'' along with ''Duschekia fruticosa'' (Rupr.) Pouzar and ''Betula middendorffii'' Trautv. et C. A. Mey form trailing forests transitional between tundra and taiga [2]. Pinus pumila pollen, usually predominating in subfossil spore-and-pollen spectra of northeastern Siberia, is found as single grains or a subordinate component (up 2-3%, rarely 10%) in spectra of lacustrine deposits formed during the last glacial stage (isotope stage 2) in the Preboreal and Boreal times of the Holocene. Sometimes, its content increases to 15-22% in spectra of lacustrine deposits synchronous to the last glacial stage near the northern coast of the Sea of Okhotsk [3], evidently indicating the proximity of Japanese stone pine thickets.

  2. Time scaling of tree rings cell production in Siberia

    NASA Astrophysics Data System (ADS)

    Popkova, Margarita; Babushkina, Elena; Tychkov, Ivan; Shishov, Vladimir; Vaganov, Eugene

    2016-04-01

    It is assumed that an annual tree-ring growth is adequately determined by a linear function of local or regional precipitation and temperature with a set of coefficients that are temporally invariant. But often that relations are non-linear. The process-based tree-ring VS-model can be used to resolve the critical processes linking climate variables to tree-ring formation. This work describes a new block of VS-model which allows to estimate a cell production in tree rings and transfer it into time scale based on the simulated integral growth rates of the model. In the algorithm of time identification for cell production we used a integral growth rates simulated by the VS-model for each growing season. The obtained detailed approach with a calculation of the time of each cell formation improves significantly the date accuracy of new cell formation in growing season. As a result for each cell in the tree-ring we estimate the temporal moment of the cell production corresponded to the seasonal growth rate in the same time scale. The approach was applied and tested for the cell measurements obtained for Scots pine (Pinus sylvestris) for the period 1964-2013 in Malaya Minusa river (Khakassia, South Siberia). The work was supported by the Russian Science Foundation (RSF # 14-14-00219)

  3. Georgia’s Brightest Future Includes Russia

    DTIC Science & Technology

    2012-03-01

    deforestation , cement production pollution and construction waste as a result of these efforts. These claims are supported by a Time magazine article in...Russian Military Intelligence…” 9 Yepifantsev, Andrei, “Russia in Transcaucasia: What’s Gone Wrong?” 24 Sept 2011, Russia in Global Affairs. Article...Russian Federation until 2020. There are many references in differing language, intended to evoke the return of Russia’s global importance. Only

  4. US DOE International energy policy on Russia

    SciTech Connect

    Gale, B.G.

    1996-04-01

    This report describes the importance of the United States Department of Energy`s (US DOE) International Energy Policy to Russia. Key objectives identified include the support of the transition to democracy and a market based economy. The U.S.interests at stake, importance of energy to Russia, key institutional mechanism, energy-policy committee, joint energy activities, and the key to the success of other U.S. policy are discussed.

  5. Eruption of Shiveluch Volcano, Kamchatka, Russia

    NASA Technical Reports Server (NTRS)

    2001-01-01

    On the night of June 4, 2001 ASTER captured this thermal image of the erupting Shiveluch volcano. Located on Russia's Kamchatka Peninsula, Shiveluch rises to an altitude of 8028'. The active lava dome complex is seen as a bright (hot) area on the summit of the volcano. To the southwest, a second hot area is either a debris avalanche or hot ash deposit. Trailing to the west is a 25 km ash plume, seen as a cold 'cloud' streaming from the summit. At least 60 large eruptions have occurred during the last 10,000 years; the largest historical eruptions were in 1854 and 1964. Because Kamchatka is located along the major aircraft routes between North America/Europe and the Far East, this area is constantly monitored for potential ash hazards to aircraft. The lower image is the same as the upper, except it has been color coded: red is hot, light greens to dark green are progressively colder, and gray/black are the coldest areas.

    The image is located at 56.7 degrees north latitude, 161.3 degrees east longitude.

    Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) is one of five Earth-observing instruments launched December 18, 1999, on NASA's Terra satellite. The instrument was built by Japan's Ministry of International Trade and Industry. A joint U.S./Japan science team is responsible for validation and calibration of the instrument and the data products. Dr. Anne Kahle at NASA's Jet Propulsion Laboratory, Pasadena, Calif., is the U.S. Science team leader; Moshe Pniel of JPL is the project manager. ASTER is the only high resolution imaging sensor on Terra. The primary goal of the ASTER mission is to obtain high-resolution image data in 14 channels over the entire land surface, as well as black and white stereo images. With revisit time of between 4 and 16 days, ASTER will provide the capability for repeat coverage of changing areas on Earth's surface.

    The broad spectral coverage and high spectral resolution of ASTER will provide scientists in

  6. Composition of asphaltenes and resins of west Siberian petroleums

    SciTech Connect

    Goncharov, I.V.; Babicheva, T.A.; Bodak, A.N.; Nemirovskaya, G.B.; Mashigorov, A.A.

    1985-01-01

    ESR and X-ray diffraction analysis was used to examine asphaltene and resin samples of West Siberia. Experiments were carried out to simulate the effect of catagenesis on resin and asphaltene composition. Processes of thermocatalytic transformations of crude oil in the deposit were found to have no marked effect on asphaltene and resin composition. Transformation of the organic input at sedimentation was assumed to be the main factor determining the qualitative and quantitative composition of crude oil resins and asphaltenes of West Siberia. Petroleums formed from organic matter, accumulating under reducing conditions, contain more asphaltenes and resins, they include much tetravalent vanadium and the asphaltenes have abundant paramagnetic centres. Petroleums formed from oxidized organic matter contain very little asphaltene low concentrations of paramagnetic centers, and little tetravalent vanadium. Resins of these petroleums are rich in oxygen. High levels of asphalt-resin matter in petroleums is related to the presence in the initial organic progenitors of polyunsaturated fatty acids and various nitrogen- and sulfur-containing compounds.

  7. [Characteristics of zonal distribution of the gamasid mites connected with small mammals and their nests in Western Siberia].

    PubMed

    Mal'kova, M G

    2010-01-01

    Analysis of long-term data on the fauna, landscape distribution, and structure of communities of the gamasid mites (Acari:Parasitiformes:Mesostigmata) connected with small mammals and their nests in the plain part of Western Siberia is carried out. By now, presence of 249 gamasid mite species is established in the territory under study, including 193 free-living and 56 parasitic species. Gamasid mites are represented by the maximal number of species on small mammals and in thers nests in northern forest-steppe (102 and 105 species respectively). Nine parasitic species from two ecological groups (epizoic and nidicolous) were found in all landscape zones of the West Siberian Plain, namely: 1) epizoic species Laelaps clethrionomydis Lange, 1955, Laelaps hilaris C. L. Koch, 1836, and Hyperlaelaps arvalis Zachvatkin, 1948 (obligatory non-exclusive hematophagous); 2) nidicolous species Androlaelaps casalis Berlese, 1887 (obligatory non-exclusive hematophagous), Eulaelaps stabularis C. L. Koch, 1836, Haemogamasus nidiformnes Bregetova, 1955 (facultative hematophagous), Haemnogamnasus ambulans Thorell, 1872 (obligatory non-exclusive hematophagous), Hirstionyssus isabellinus Oudemans, 1913, and Hirstionyssus eusoricis Bregetova, 1956 (obligatory exclusive hematophagous). Last three species demonstrate the mixed type of parasitism. The population of gamasid mites on small mammals is most specific in tundra, southern forest-steppe and steppe; the fauna of gamasid mites in nests is most specific in southern forest-steppe and steppe.

  8. Degradation processes of hydrological resources by human and climate - example of small lakes in Northern Kazakhstan and Southern Siberia.

    NASA Astrophysics Data System (ADS)

    Meyer, Burghard; Schreiner, Vera

    2014-05-01

    The presentation discusses (on the basis of an actual application in the development of a curriculum for Integrated Water Cycle Management in Kazakhstan; TEMPUS I-WEB project) the diverse scientific approaches to explain the degradation of hydrological resources in West-Siberia and Nord-Kazakhstan by focussing on natural and anthropogenic causes by the example of the dry out of small lakes. Since Pleistocene in the region a diverse mosaic of large and small lakes of at total shrinking surface area was formed. On natural causes it includes (1) climatic cycling, (2) lake developments since the Pleistocene originate by the Northern glaciations by ice dammed lakes (without tectonics). The man made causes are (1) the sediment accumulation in lakes, (2) the (problematic) water management and water usage and (3) the land use changes in the watersheds. Climate change includes finally both natural and climatic causes of the change. The latter is explained using actual reports of (1) IPCC on extreme events and (2) gives a note about radiative forcing components as proxy to integrate.

  9. Vegetation Structure Changes in the South Part of Western Siberia at the End of XX Century

    NASA Astrophysics Data System (ADS)

    Dyukarev, E.; Pologova, N. N.; Golovatskaya, E. A.; Dyukarev, A. G.; Gordov, E. P.; Okladnikov, I. G.; Titov, A. G.

    2010-12-01

    Understanding human impact on changes in vegetation composition and structure can be performed using analysis of space images obtained from high resolution satellite sensors. Natural ecosystems at the South and Sob-Taiga zone of Western Siberia are characterized by development of an early succession stages, given the projected increase in disturbance, or will be converted into human-dominated terrestrial production systems. Disturbances appear to be increasing in some regions, leading to fragmentation of natural ecosystems and to a generally "weedier," structurally simpler biosphere with fewer systems in a more ecologically complex old-growth state. The analysis of structure of vegetation cover at two test sites located at the south-west part of the West-Siberian Plain in the South and Sub-Taiga zone was made using LANDSAT space images and ground data obtained in various seasons and years. The studied area of the first test site (“Bakchar”) is occupied by bogs, paludificated forests and cultivated lands. Test site “Tomsk” covered by cultivated lands and dark coniferous forest complexes. Vegetation classification was made using NELDA project legend (www.fsl.orst.edu/nelda). The main part of Site “Bakchar” is occupied by tree dominated classes (66%). Wetlands occupy about 43% of the area. Part of herbaceous vegetation is rather low (9%). Site “Tomsk” has completely different structure of classes. More than one-half of the area (52%) is covered by cultivated lands. Forests occupy 42% of the area. Wetlands (9%) exist in the Ob’-Tom’ interfluve and left bank of the Ob’ river. During the XX century the vegetation cover was exposed to natural and anthropogenic changes. Comparison of space images from different years (1990, 1999 and 2007) allowed to reveal dynamics in vegetation cover. Decrease of forest area in 1990-1999 at site “Bakchar” are primary occurs due to intense forest cutting for timber industry and local use. A strong wind have

  10. New Holocene refugia of giant deer (Megaloceros giganteus Blum.) in Siberia: updated extinction patterns

    NASA Astrophysics Data System (ADS)

    van der Plicht, J.; Molodin, V. I.; Kuzmin, Y. V.; Vasiliev, S. K.; Postnov, A. V.; Slavinsky, V. S.

    2015-04-01

    We obtained new data on the existence of giant deer (Megaloceros giganteus Blum.) in Siberia during the Holocene. Bones and antler of giant deer from new localities in western (Baraba forest steppe) and eastern (Angara River basin) Siberia are dated by radiocarbon, ranging 7900-10,300 BP (ca 8800-12,200 cal BP). Based on these data, we can extend the 'Siberian' Early Holocene habitat of giant deer at least 2400 km to the east compared to previous works. The final extinction of giant deer turned out to be more complex than it was previously thought, with perhaps relatively large refugium in Western Siberia at 7900-7000 BP (ca 8800-7900 cal BP) which was reduced to the Trans-Urals region at 7000-6800 BP (ca 7900-7600 cal BP).

  11. Continuous measurements of aerosol particles in Arctic Russia and Finland

    NASA Astrophysics Data System (ADS)

    Asmi, Eija; Kondratyev, Vladimir; Brus, David; Lihavainen, Heikki; Laurila, Tuomas; Aurela, Mika; Hatakka, Juha; Viisanen, Yrjö; Reshetnikov, Alexander; Ivakhov, Victor; Uttal, Taneil; Makshtas, Alexander

    2013-04-01

    The Arctic and northern boreal regions of Eurasia are experiencing rapid environmental changes due to pressures by human activities. The largest anthropogenic climate forcings are due to aerosol particles and greenhouse gases (GHGs). The Arctic environment is highly sensitive to changes in aerosol concentrations or composition, largely due to the high surface reflectance for the most part of the year. Concentrations of aerosols in winter and spring Arctic are affected by 'Arctic Haze', a phenomenon suggested to arise from the transport of pollutants from lower latitudes and further strengthened by the strong stratification of the Arctic wintertime atmosphere. Sources and transport patterns of aerosols into the Arctic are, however, not fully understood. In order to monitor the changes within the Arctic region, as well as to understand the sources and feedback mechanisms, direct measurements of aerosols within the Arctic are needed. So far, direct year-round observations have been inadequate especially within the Russian side of the Arctic. This is the reason why a new climate observatory was founded in Tiksi, Russia. Tiksi meteorological observatory in northern Siberia (71o 36' N; 128o 53' E) on the shore of the Laptev Sea has been operating since 1930s. Recently, it was upgraded and joint in the network of the IASOA, in the framework of the International Polar Year Activity project. The project is run in collaboration between National Oceanic and Atmospheric Administration (NOAA) with the support of the National Science Foundation (NSF), Roshydromet (AARI and MGO units), government of the Republic of Sakha (Yakutia) and the Finnish Meteorological Institute (FMI). The research activities of FMI in Tiksi include e.g. continuous long-term measurements of aerosol physical properties, which have been successfully continued since summer 2010. These, together with the FMI measurements in Pallas station in northern Finland since 1999, provide important information on the

  12. Why Russia is not a state

    SciTech Connect

    Stern, J.E.

    1993-08-16

    This article makes two principal points. First the author argues that the Russian federation has never been a state and is not sustainable as a state. Four centrifugal indicators are presented to support this claim: ethnic divisiveness; uncertainty about the legitimacy of Russia`s current borders; competing claims for legitimacy on the part of federal and regional leaders; and army units` unpredictable allegiances. Second, she argues that Soviet policies intended to facilitate central control of the periphery had the perverse effect of creating ethnic identity and demands for national autonomy where, in many cases, they did not exist prior to the Communist regime. Following the introduction, part one briefly reviews the concepts of state, nation, and nationalism and the roles they play in Russia. Criteria for state-hood are discussed. Part two lists the main ethnic groups in Russia and considers the roots of ethnic nationalism in the Russian Federation. Part three discusses confusion over the legitimacy of the physical, economic, and political boundaries of the Russian Federation. Part four discusses political disarray in the center and the regions and the lack of unity among order-enforcing entities. The Volga-Ural region -- where there is a large concentration of nuclear weapons and facilities, and which is especially volatile politically -- is discussed in somewhat more detail. Part five argues that these factors taken together call into question Russia`s identity as a state. The author concludes that Russia remains a multi-ethnic empire in which the rule of law is still not supreme.

  13. Agrolandscape Research of Geosystems in the South of Central Siberia

    NASA Astrophysics Data System (ADS)

    Lysanova, G.; Soja, A. J.

    2012-12-01

    Minusinskaya basin, the area under research, is situated in the south of Central Siberia and is an agrarian region, which differs from another territories of Siberia. The territory provides for foodstuff not only its population but another regions as well. Nature-climate conditions favour the development of agriculture and cattle-breeding. Complex geographical study of rural lands, which is implemented by two approaches: a natural and industrial system block is necessary for rational use of agrolandscapes. Agrolandscapes are objects for rationalization of land management in agricultural regions. From our point of view application of a landscape map as a base for working out of agrolandscape map (Fig. 1a) and a map of agronatural potential of geosystems (Fig. 2), gives an opportunity to take stock of reserves of agricultural lands not only in quantitative but qualitative respects and also to determine the ways of optimal transformation of arable lands depending on nature conditions of regions and their development. Landscape maps that reflect differentiation of not only natural formations, changed by anthropogenious influence and also natural analogues, concern to a number of important tools of planning for optimal land use. The main principles of working out of typological landscape map of a medium scale aroused from targets and tasks of agrolandscape estimation of the territory [1]. The landscape map was worked out according to V.A. Nikolaev's methodology [2]: types of landscapes correlated with types of lands use, composition of cereals in rotation of crops, agro-techniques, crop capacity, climate indices, etc. Existing natural-agricultural systems are shown in the map. Their characteristics includes information about natural and agricultural blocks. Agronatural potential had been calculated by summarize estimations of its component parts. As a result of these calculations 30 arable agrolandscapes, marked out into the landscape map, were joined according to summ

  14. Enzyme activities along a latitudinal transect in Western Siberia

    NASA Astrophysics Data System (ADS)

    Schnecker, Jörg; Wild, Birgit; Eloy Alves, Ricardo J.; Gentsch, Norman; Gittel, Antje; Knoltsch, Anna; Lashchinskiy, Nikolay; Mikutta, Robert; Takriti, Mounir; Richter, Andreas

    2014-05-01

    Decomposition of soil organic matter (SOM) and thus carbon and nutrient cycling in soils is mediated by the activity of extracellular enzymes. The specific activities of these enzymes and their ratios to each other represent the link between the composition of soil organic matter and the nutrient demand of the microbial community. Depending on the difference between microbial nutrient demand and substrate availability, extracellular enzymes can enhance or slow down different nutrient cycles in the soil. We investigated activities of six extracellular enzymes (cellobiohydrolase, leucine-amino-peptidase, N-acetylglucosaminidase, chitotriosidase, phosphatase and phenoloxidase) in the topsoil organic horizon, topsoil mineral horizon and subsoil horizon in seven ecosystems along a 1,500 km-long North-South transect in Western Siberia. The transect included sites in the southern tundra, northern taiga, middle taiga, southern taiga, forest-steppe (in forested patches as well as in adjacent meadows) and Steppe. We found that enzyme patterns varied stronger with soil depth than between ecosystems. Differences between horizons were mainly based on the increasing ratio of oxidative enzymes to hydrolytic enzymes. Differences between sites were more pronounced in topsoil than in subsoil mineral horizons, but did not reflect the north-south transect and the related gradients in temperature and precipitation. The observed differences between sites in topsoil horizons might therefore result from differences in vegetation rather than climatic factors. The decreasing variability in the enzyme pattern with depth might also indicate that the composition of soil organic matter becomes more similar with soil depth, most likely by an increasing proportion of microbial remains compared to plant derived constituents of SOM. This also indicates, that SOM becomes less divers the more it is processed by soil microorganisms. Our findings highlight the importance of soil depth on enzyme

  15. Nitrogen dynamics in Turbic Cryosols from Siberia and Greenland.

    PubMed

    Wild, Birgit; Schnecker, Jörg; Bárta, Jiří; Capek, Petr; Guggenberger, Georg; Hofhansl, Florian; Kaiser, Christina; Lashchinsky, Nikolaj; Mikutta, Robert; Mooshammer, Maria; Santrůčková, Hana; Shibistova, Olga; Urich, Tim; Zimov, Sergey A; Richter, Andreas

    2013-12-01

    Turbic Cryosols (permafrost soils characterized by cryoturbation, i.e., by mixing of soil layers due to freezing and thawing) are widespread across the Arctic, and contain large amounts of poorly decomposed organic material buried in the subsoil. This cryoturbated organic matter exhibits retarded decomposition compared to organic material in the topsoil. Since soil organic matter (SOM) decomposition is known to be tightly linked to N availability, we investigated N transformation rates in different soil horizons of three tundra sites in north-eastern Siberia and Greenland. We measured gross rates of protein depolymerization, N mineralization (ammonification) and nitrification, as well as microbial uptake of amino acids and NH4(+) using an array of (15)N pool dilution approaches. We found that all sites and horizons were characterized by low N availability, as indicated by low N mineralization compared to protein depolymerization rates (with gross N mineralization accounting on average for 14% of gross protein depolymerization). The proportion of organic N mineralized was significantly higher at the Greenland than at the Siberian sites, suggesting differences in N limitation. The proportion of organic N mineralized, however, did not differ significantly between soil horizons, pointing to a similar N demand of the microbial community of each horizon. In contrast, absolute N transformation rates were significantly lower in cryoturbated than in organic horizons, with cryoturbated horizons reaching not more than 32% of the transformation rates in organic horizons. Our results thus indicate a deceleration of the entire N cycle in cryoturbated soil horizons, especially strongly reduced rates of protein depolymerization (16% of organic horizons) which is considered the rate-limiting step in soil N cycling.

  16. Parameterization of tree-ring growth in Siberia

    NASA Astrophysics Data System (ADS)

    Tychkov, Ivan; Popkova, Margarita; Shishov, Vladimir; Vaganov, Eugene

    2016-04-01

    No doubt, climate-tree growth relationship is an one of the useful and interesting subject of studying in dendrochronology. It provides an information of tree growth dependency on climatic environment, but also, gives information about growth conditions and whole tree-ring growth process for long-term periods. New parameterization approach of the Vaganov-Shashkin process-based model (VS-model) is developed to described critical process linking climate variables with tree-ring formation. The approach (co-called VS-Oscilloscope) is presented as a computer software with graphical interface. As most process-based tree-ring models, VS-model's initial purpose is to describe variability of tree-ring radial growth due to variability of climatic factors, but also to determinate principal factors limiting tree-ring growth. The principal factors affecting on the growth rate of cambial cells in the VS-model are temperature, day light and soil moisture. Detailed testing of VS-Oscilloscope was done for semi-arid area of southern Siberia (Khakassian region). Significant correlations between initial tree-ring chronologies and simulated tree-ring growth curves were obtained. Direct natural observations confirm obtained simulation results including unique growth characteristic for semi-arid habitats. New results concerning formation of wide and narrow rings under different climate conditions are considered. By itself the new parameterization approach (VS-oscilloscope) is an useful instrument for better understanding of various processes in tree-ring formation. The work was supported by the Russian Science Foundation (RSF # 14-14-00219).

  17. Ground and aircraft-based methane measurements in Siberia: source attribution using tracers and models

    NASA Astrophysics Data System (ADS)

    Arzoumanian, E.; Paris, J. D.; Pruvost, A.; Peng, S.; Turquety, S.; Berchet, A.; Pison, I.; Helle, J.; Arshinov, M.; Belan, B. D.

    2015-12-01

    Methane (CH4) is the second most important anthropogenic greenhouse gas. It is also naturally emitted by a number of processes, including microbial activity in wetlands, permafrost degradation and wildfires. Our current understanding of the extent and amplitude of its natural sources, as well as the large scale driving factors, remain highly uncertain (Kirschke et al., Nature Geosci., 2013). Furthermore, high latitude regions are large natural sources of CH4 in the atmosphere. Observing boreal/Arctic CH4 variability and understanding its main driving processes using atmospheric measurements and transport model is the task of this work. YAK-AEROSIB atmospheric airborne campaigns (flights in the tropospheric layer up to 9 km connecting the two cities of Novosibirsk and Yakutsk) and continuous measurements at Fonovaya Observatory (60 km west of Tomsk - 56° 25'07"N, 84° 04'27"E) have been performed in order to provide observational data on the composition of Siberian air. The study is focused on 2012, during which a strong heat wave impacted Siberia, leading to the highest mean daily temperature values on record since the beginning of the 20th century. This abnormal drought has led to numerous large forest fires. A chemistry-transport model (CHIMERE), combined with datasets for anthropogenic (EDGAR) emissions and models for wetlands (ORCHIDEE) and wildfires (APIFLAME), is used to determine contributions of CH4 sources in the region. Recent results concerning CH4 fluxes and its atmospheric variability in the Siberian territory derived from a modeled-based analysis will be shown and discussed. This work was funded by CNRS (France), the French Ministry of Foreign Affairs, CEA (France), Presidium of RAS (Program No. 4), Brunch of Geology, Geophysics and Mining Sciences of RAS (Program No. 5), Interdisciplinary integration projects of Siberian Branch of RAS (No. 35, No. 70, No. 131), Russian Foundation for Basic Research (grants No 14-05-00526, 14-05-00590). Kirschke, S

  18. Trends in the normalized difference vegetation index (NDVI) associated with urban development in arctic and subarctic Western Siberia

    NASA Astrophysics Data System (ADS)

    Outten, S.; Miles, V.; Ezau, I.

    2015-12-01

    Changes in normalized difference vegetation index (NDVI) in the high Arctic have been reliably documented, with widespread "greening" (increase in NDVI), specifically along the northern rim of Eurasia and Alaska. Whereas in West Siberia south of 65N, widespread "browning" (decrease in NDVI) has been noted, although the causes remain largely unclear. In this study we report results of statistical analysis of the spatial and temporal changes in NDVI around 28 major urban areas in the arctic and subarctic Western Siberia. Exploration and exploitation of oil and gas reserves has led to rapid industrialization and urban development in the region. This development has significant impact on the environment and particularly in the vegetation cover in and around the urbanized areas. The analysis is based on 15 years (2000-2014) of high-resolution (250 m) Moderate Resolution Imaging Spectroradiometer (MODIS) data acquired for summer months (June through August) over the entire arctic and subarctic Western Siberian region. The analysis shows that the NDVI background trends are generally in agreement with the trends reported in previous coarse-resolution NDVI studies. Our study reveals greening over the arctic (tundra and tundra-forest) part of the region. Simultaneously, the southern (boreal taiga forest) part is browning, with the more densely vegetation areas or areas with highest NDVI, particularly along Ob River showing strong negative trend. The unexpected and interesting finding of the study is statistically robust indication of the accelerated increase of NDVI ("greening") in the older urban areas. Many Siberian cities become greener even against the decrease in the NDVI background. Moreover, interannual variations of urban NDVI are not coherent with the NDVI background variability. We also find that in tundra zones, NDVI values are higher in a 5-10 km buffer zone around the city edge than in rural areas (40 km distance from the city edge), and in taiga in a 5-10 km

  19. [Polyploid races of earthworms (Lumbricidae, Oligochaeta) in the East European plain and Siberia].

    PubMed

    Vsevolodova-Perel', T S; Bulatova, N Sh

    2008-01-01

    The distribution of polyploid races of earthworms in the East European plain and Siberia was analyzed. Amphimictic autopolyploid races of two species of the Asian genus Eisenia, E. nordenskioldi and A. atlavinyteae, are widespread in Siberia, from its southern boundary to the arctic region, while polyploid Lumbricidae in the East-European plain, except for the Volga region, are represented mainly by parthenogenetic forms of other genera. This is presumably related to differences in the Pleistocene environmental history between the two adjacent geographic regions of Eurasia.

  20. West Africa

    NASA Technical Reports Server (NTRS)

    2002-01-01

    With its vast expanses of sand, framed by mountain ranges and exposed rock, northwestern Africa makes a pretty picture when viewed from above. This image was acquired by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra spacecraft. The Canary Islands can be seen on the left side of the image just off Africa's Atlantic shore. The light brown expanse running through the northern two thirds of the image is the Sahara Desert. The desert runs up against the dark brown Haut Atlas mountain range of Morocco in the northwest, the Atlantic Ocean to the west and the semi-arid (light brown pixels) Sahelian region in the South. The Sahara, however, isn't staying put. Since the 1960s, the desert has been expanding into the Sahelian region at a rate of up to 6 kilometers per year. In the 1980s this desert expansion, combined with over cultivation of the Sahel, caused a major famine across west Africa. Over the summer months, strong winds pick up sands from the Sahara and blow them across the Atlantic as far west as North America, causing air pollution in Miami and damaging coral reefs in the Bahamas and the Florida Keys. The white outlines on the map represent country borders. Starting at the top-most portion of the map and working clockwise, the countries shown are Morocco, Western Sahara, Mauritania, Senegal, Mali, Burkina Fasso, Nigeria, Mali (again), and Algeria. Image by Reto Stockli, Robert Simmon, and Brian Montgomery, NASA Earth Observatory, based on data from MODIS

  1. Struggling to survive in Russia.

    PubMed

    Gadasina, A

    1997-01-01

    Abortion has long been the traditional method of family planning (FP) in Russia. Today, abortions are free, but contraception is not. The birth rate has decreased between 1989 and 1995, and the death rate has increased. The present economic situation has had a marked adverse effect on women who are expected to juggle jobs, household duties, and child care responsibilities. In order to survive, women sometimes must engage in work that compromises their health. Many women have resorted in prostitution, and this has caused an unprecedented explosion in the incidence of sexually transmitted diseases, especially syphilis. The number of people newly registered as HIV-positive in the first half of 1997 exceeded the total for 1996. While sex education is still restricted, erotica and pornography is widely available. Cases of syphilis are increasing among the young, and, in 1996, about 2500 girls under age 15 gave birth and an equal number had abortions. Only 12% of all pregnant women and 25% of newborn infants can be considered healthy. In 1994, the government launched a FP program that is being carried out by a few public and private organizations. One of these, the Russian FP Association, has created more than 50 branches in different regions, opened youth centers, and provided sex education and reproductive health counseling. The overall effort has led to a 27% reduction in abortions, and a 25% reduction in abortion mortality. These efforts, however, have been opposed by "pro-life" forces and by the Communist wing of the government that reduced the budget. The FP Association is fighting back by lobbying and explaining the need for its work.

  2. Space Biology in Russia Today

    NASA Astrophysics Data System (ADS)

    Grigoriev, Anatoly; Sychev, Vladimir; Ilyin, Eugene

    At present space biology research in Russia is making significant progress in several areas of high priority. Gravitational biology. In April-May 2013, a successful 30-day flight of the biological satellite (biosatellite) Bion-M1 was conducted, which carried rodents (mice and gerbils), geckos, fish, mollusks, crustaceans, microorganisms, insects, lower and higher plants, seeds, etc. The investigations were performed by Russian scientists as well as by researchers from NASA, CNES, DLR and South Korea. Foton-M4 carrying various biological specimens is scheduled to launch in 2014. Work has begun to develop science research programs to be implemented onboard Bion-M2 and Bion-M3 as well as on high apogee recoverable spacecraft. Study of the effects of microgravity on the growth and development of higher plants cultivated over several generations on the International Space Station (ISS) has been recently completed. Space radiobiology. Regular experiments aimed at investigating the effects of high-energy galactic cosmic rays on the animal central nervous system and behavior are being carried out using the Particle Accelerator in the town of Dubna. Biological (environmental) life support systems. In recent years, experiments have been performed on the ISS to upgrade technologies of plant cultivation in microgravity. Advanced greenhouse mockups have been built and are currentlyundergoing bioengineering tests. Technologies of waste utilization in space are being developed. Astrobiology experiments in orbital missions. In 2010, the Biorisk experiment on bacterial and fungal spores, seeds and dormant forms of organisms was completed. The payload containing the specimens was installed on the exterior wall of the ISS and was exposed to outer space for 31 months. In addition, Bion-M1 also carried seeds, bacterial spores and microbes that were exposed to outer space effects. The survival rate of bacterial spores incorporated into man-made meteorites, that were attached to the

  3. [Palivizumab: four seasons in Russia].

    PubMed

    Baranov, A A; Ivanov, D O; Aliamovskaia, G A; Amirova, V R; Antoniuk, I V; Asmolova, G A; Beliaeva, I A; Bokeria, E L; Briukhanova, O A; Vinogradova, I V; Vlasova, E V; Galustian, A N; Gafarova, G V; Gorev, V V; Davydova, I V; Degtiarev, D N; Degtiareva, E A; Dolgikh, V V; Donits, I M; Zakharova, N I; Zernova, L Iu; Zimina, E P; Zuev, V V; Keshishian, E S; Kovalev, I A; Koltunov, I E; Korsunskiĭ, A A; Krivoshchekov, E V; Krsheminskaia, I V; Kuznetsova, S N; Liubimenko, V A; Namazova-Baranova, L S; Nesterenko, É V; Nikolaev, S V; Ovsiannikov, D Iu; Pavlova, T I; Potapova, M V; Rychkova, L V; Safarov, A A; Safina, A I; Skachkova, M A; Soldatova, I G; Turti, T V; Filatova, N A; Shakirova, R M; Ianulevich, O S

    2014-01-01

    In 2010, the Russian Federation (RF) registered palivizumab--innovative drug, based on monoclonal antibodies for passive immunization of seasonal respiratory syncytial virus (RSV) infection in children of disease severe progress risk group, which include primarily premature infants, children with bronchopulmonary dysplasia and hemodynamically significant congenital heart disease. Currently, palivizumab is included in the list of recommended medicines and medical care standards of different countries, including Russia. In the review the results of Russian research on the progress of RSV infection, its epidemiology and immunization experience gained over the 2010-2014 period are summarized in relation to the foreign data. During the four epidemic seasons palivizumab immunization covered more than 3,200 children of severe RSV infection risk group with a progressive annual increase in the number of patients who received the drug. Geography of palivizumab immunization is also greatly expanded in our country during this time. If during the first two seasons measures of immunization were taken mainly in Moscow and St. Petersburg, at the present time, thirty one territorial entities of the Russian Federation have the experience in the drug application. Analysis of the results of RSV infection immunization (made in several regions) confirms the high clinical efficacy and palivizumab safety already demonstrated in international studies. In addition, the analysis presents the potential to improve the efficiency of the integrated RSV infection immunization programs, realizing in the establishment of high-risk child group register, adequate counseling for parents, as well as the development of the routing of patients and coordination of interaction between different health institutions during the immunization.

  4. Moult migration of emperor geese Chen canagica between Alaska and Russia

    USGS Publications Warehouse

    Hupp, J.W.; Schmutz, J.A.; Ely, C.R.; Syroechkovskiy, E.E.; Kondratyev, Alexander V.; Eldridge, W.D.; Lappo, E.

    2007-01-01

    We studied reproductive success and post-breeding movements of 32 adult female emperor geese Chen canagica that were marked with satellite radio transmitters on their nesting area on the Yukon-Kuskokwim Delta (YKD), Alaska 2000–2004. All 16 females that failed to successfully reproduce departed the YKD and moulted remiges either on the north coast of the Chukotka Peninsula, Russia (n=15), or on St. Lawrence Island, Alaska (n=1). Of 16 females that successfully nested, one migrated to Russia following hatch whereas the remainder stayed on the YKD. While moulting on the Chukotka Peninsula, emperor geese with satellite transmitters primarily used coastal lagoons west of Kolyuchin Bay. We observed 21,150 adult-plumaged emperor geese during aerial surveys in Chukotka in 2002. Most (95%) were in the same region used by geese that had been marked with satellite transmitters in Alaska. The number of emperor geese observed in Russia was comparable to our estimate of ≥20,000 adults that either do not nest or nest unsuccessfully each year on the YKD, suggesting that most nonproductive adults, or ≥28% of the adult population departs the YKD to moult elsewhere. The number of moult migrants may be substantially higher in years of poor reproductive success or if adult-plumaged birds that are not of breeding age also leave the YKD. Moult migration of emperor geese between Alaska and Russia is likely substantially greater than previously believed. Russian moulting habitats are important to the North American population of emperor geese and events that affect survival of geese in Russia could impact population trends on the YKD. Protection of coastal lagoons on the north coast of Chukotka is warranted.

  5. DNA analysis of a 30,000-year-old Urocitellus glacialis from northeastern Siberia reveals phylogenetic relationships between ancient and present-day arctic ground squirrels

    PubMed Central

    Faerman, Marina; Bar-Gal, Gila Kahila; Boaretto, Elisabetta; Boeskorov, Gennady G.; Dokuchaev, Nikolai E.; Ermakov, Oleg A.; Golenishchev, Fedor N.; Gubin, Stanislav V.; Mintz, Eugenia; Simonov, Evgeniy; Surin, Vadim L.; Titov, Sergei V.; Zanina, Oksana G.; Formozov, Nikolai A.

    2017-01-01

    In contrast to the abundant fossil record of arctic ground squirrels, Urocitellus parryii, from eastern Beringia, only a limited number of fossils is known from its western part. In 1946, unnamed GULAG prisoners discovered a nest with three mummified carcasses of arctic ground squirrels in the permafrost sediments of the El’ga river, Yakutia, Russia, that were later attributed to a new species, Citellus (Urocitellus) glacialis Vinogr. To verify this assignment and to explore phylogenetic relationships between ancient and present-day arctic ground squirrels, we performed 14C dating and ancient DNA analyses of one of the El’ga mummies and four contemporaneous fossils from Duvanny Yar, northeastern Yakutia. Phylogenetic reconstructions, based on complete cytochrome b gene sequences of five Late Pleistocene arctic ground squirrels and those of modern U. parryii from 21 locations across western Beringia, provided no support for earlier proposals that ancient arctic ground squirrels from Siberia constitute a distinct species. In fact, we observed genetic continuity of the glacialis mitochondrial DNA lineage in modern U. parryii of the Kamchatka peninsula. When viewed in a broader geographic perspective, our findings provide new insights into the genetic history of U. parryii in Late Pleistocene Beringia. PMID:28205612

  6. Russian populations of Puccinia triticina in distant regions are not differentiated for virulence and molecular genotype

    Technology Transfer Automated Retrieval System (TEKTRAN)

    The objective of this study was to determine whether genetically distinct groups of Puccinia triticina are present in four regions of Russia. Collections of P. triticina were obtained from the Central, North Caucasus, Volga, and West Siberia regions of Russia from 2006 to 2010. Ninety-nine single ur...

  7. Flooding of the Ob River, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    A mixture of heavy rainfall, snowmelt, and ice jams in late May and early June of this year caused the Ob River and surrounding tributaries in Western Siberia to overflow their banks. The flooding can be seen in thess image taken on June 16, 2002, by the MODIS (Moderate Resolution Imaging Spectroradiometer) instrument aboard the Terra satellite. Last year, the river flooded farther north. Normally, the river resembles a thin black line, but floods have swollen the river considerably. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  8. Forest Fires in Russia and Northern China

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Smoke plumes from forest fires scattered along the border between the Russian Far East and northern China are clearly visible in this true-color image from the Sea-viewing Wide-Field-of-view Sensor (SeaWiFS) on June 16, 2000. Fires in Siberia occur every summer, and severe outbreaks occur every ten years or so, with the most recent in 1998. The fires are ignited by lightning, and are so remote that it is impossible to fight them effectively. Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

  9. Integrated Paleomagnetism and U-Pb Geochronology of Mafic Dikes of the Eastern Anabar Shield Region, Siberia: Implications for Mesoproterozoic Paleolatitude of Siberia and Comparison with Laurentia.

    PubMed

    Ernst; Buchan; Hamilton; Okrugin; Tomshin

    2000-07-01

    This article reports the first joint paleomagnetic and U-Pb geochronologic study of Precambrian diabase dikes in the Anabar Shield and adjacent Riphean cover of Siberia. It was undertaken to allow comparison with similar published studies in Laurentia and to test Proterozoic reconstructions of Siberia and Laurentia. An east-trending Kuonamka dike yielded a provisional U-Pb baddeleyite emplacement age of 1503+/-5 Ma and a virtual geomagnetic pole at 16 degrees S, 221 degrees E (dm=17&j0;, dp=10&j0;). A paleomagnetic pole at 6 degrees N, 234 degrees E (dm=28&j0;, dp=14&j0;) was obtained from five Kuonamka dikes. An east-southeast-trending Chieress dike yielded a U-Pb baddeleyite emplacement age of 1384+/-2 Ma and a virtual geomagnetic pole at 4 degrees N, 258 degrees E (dm=9&j0;, dp=5&j0;). Kuonamka and Chieress poles are interpreted to be primary but do not average out secular variation. Assuming that the Siberian Plate has remained intact since the Mesoproterozoic, except for mid-Paleozoic opening of the Viljuy Rift, then the above results indicate that the Siberian Plate was in low latitudes at ca. 1503 and 1384 Ma, broadly similar to low latitudes determined for Laurentia from well-dated paleopoles at 1460-1420, 1320-1290, and 1267 Ma. This would allow Laurentia and Siberia to have been attached in the Mesoproterozoic, as suggested in several recent studies based on geological criteria. However, because paleomagnetic results from the Anabar Shield region do not average out secular variation and the ages of poles from Siberia and Laurentia are not well matched, it is not yet possible to distinguish between these reconstructions or to rule out other configurations that also maintain the two cratons at low paleolatitudes.

  10. Radioactive contamination of pine (Pinus sylvestris) in Krasnoyarsk (Russia) following fallout from the Fukushima accident.

    PubMed

    Bolsunovsky, A; Dementyev, D

    2014-12-01

    Following the Fukushima accident in March 2011, samples of pine trees (Pinus sylvestris) were collected from three sites near the city of Krasnoyarsk (Siberia, Russia) during 2011-2012 and analyzed for artificial radionuclides. Concentrations of Fukushima-derived radionuclides in the samples of pine needles in April 2011 reached 5.51 ± 0.52 Bq kg(-1)(131)I, 0.92 ± 0.04 Bq kg(-1)(134)Cs, and 1.51 ± 0.07 Bq kg(-1)(137)Cs. An important finding was the detection of (134)Cs from the Fukushima accident not only in the pine needles and branches but also in the new shoots in 2012, which suggested a transfer of Fukushima cesium isotopes from branches to shoots. In 2011 and 2012, the (137)Cs/(134)Cs ratio for pine needles and branches collected in sampling areas Krasnoyarsk-1 and Krasnoyarsk-2 was greater than 1 (varying within a range of 1.2-2.6), suggesting the presence of "older", pre-Fukushima accident (137)Cs. Calculations showed that for pine samples growing in areas of the Krasnoyarskii Krai unaffected by contamination from the nuclear facility, the activity of the Fukushima-derived cesium isotopes was two-three times higher than the activity of the pre-accident (137)Cs.

  11. Petrography of impact glasses and melt breccias from the El'gygytgyn impact structure, Russia

    NASA Astrophysics Data System (ADS)

    Pittarello, Lidia; Koeberl, Christian

    2013-07-01

    The El'gygytgyn impact structure, 18 km in diameter and 3.6 Ma old, in Arctic Siberia, Russia, is the only impact structure on Earth mostly excavated in acidic volcanic rocks. The Late Cretaceous volcanic target includes lavas, tuffs, and ignimbrites of rhyolitic, dacitic, and andesitic composition, and local occurrence of basalt. Although the ejecta blanket around the crater is nearly completely eroded, bomb-shaped impact glasses, redeposited after the impact event, occur in lacustrine terraces within the crater. Here we present detailed petrographic descriptions of newly collected impact glass-bearing samples. The observed features contribute to constrain the formation of the melt and its cooling history within the framework of the impact process. The collected samples can be grouped into two types, characterized by specific features: (1) "pure" glasses, containing very few clasts or new crystals and which were likely formed during the early stages of cratering and (2) a second type, which represents composite samples with impact melt breccia lenses embedded in silicate glass. These mixed samples probably resulted from inclusion of unmelted impact debris during ejection and deposition. After deposition the glassy portions continued to deform, whereas the impact melt breccia inclusions that probably had already cooled down behaved as rigid bodies in the flow.

  12. Helminth infections in domestic dogs from Russia

    PubMed Central

    Moskvina, T. V.; Ermolenko, A. V.

    2016-01-01

    Dogs are the hosts for a wide helminth spectrum including tapeworms, flatworms, and nematodes. These parasites affect the dog health and cause morbidity and mortality, especially in young and old animals. Some species, as Toxocara canis, Ancylostoma caninum, Dipylidium caninum, and Echinococcus spp. are well-known zoonotic parasites worldwide, resulting in high public health risks. Poor data about canine helminth species and prevalence are available in Russia, mainly due to the absence of official guidelines for the control of dog parasites. Moreover, the consequent low quality of veterinary monitoring and use of preventive measures, the high rate of environmental contamination by dog feces and the increase of stray dog populations, make the control of the environmental contamination by dog helminths very difficult in this country. This paper reviews the knowledge on canine helminth fauna and prevalence in Russia. Practical aspects related to diagnosis, treatment, and control of parasitic diseases of dogs in Russia are discussed. PMID:27956777

  13. EDITORIAL: Siberia Integrated Regional Study: multidisciplinary investigations of the dynamic relationship between the Siberian environment and global climate change

    NASA Astrophysics Data System (ADS)

    Gordov, E. P.; Vaganov, E. A.

    2010-03-01

    Environmental Sciences) biannual Young Scientists' School (YSS) and international conferences [15]. These include lecture courses for young scientists, training sessions, invited lectures and thematic workshops (www.scert.ru/en/conferences/). The first event was organized in 2000, and thereafter each year 50-70 young scientists from Russia and the Commonwealth of Independent States participate in CITES and ENVIROMIS conferences. These events are organized to support multidisciplinary education, contain no parallel sessions, are composed of about 50% students, and all presentations are posted to assist future professional activity. In the first years, these activities were supported internationally (INTAS, the EC International Cooperation Program within FP5 and FP6); however, recent activities have been supported by the Russian Foundation for Basic Research, the RF Ministry of Education and Science and the SB RAS. Some results gained in the course of SIRS projects being carried out, and current challenges While some findings on regional climate dynamics were reported in the EGU 2009 NEESPI session and in manuscripts listed on the NEESPI website (www.neespi.org/science/NEESPI_publications.pdf), a majority of them have been published in Russian journals and are still unknown in the international climatic community. However, additional reports can be found in the Enviro-RISKS final scientific report [16], mainly in the third volume devoted to climate change, terrestrial ecosystems and hydrology (www.dmi.dk/dmi/sr08-05-3.pdf). We have already established that temperatures have increased, particularly in the winter in Eastern Siberia (0.5°/decade), and the number of frost days (~1 day yr-1) and growing season length has also increased (~1 day yr-1) [17, 18]. Even more troubling is the potential for these transient phenomena to manifest themselves as nonlinear reactions to ongoing climatic change [19]. There are three main scientific research challenges to the SIRS community, which

  14. Sredinnyy Khrebet, Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    The Kamchatka Peninsula in eastern Russia is shown in this scene created from a preliminary elevation model derived from the first data collected during the Shuttle Radar Topography Mission (SRTM) on February 12, 2000. Sredinnyy Khrebet, the mountain range that makes up the spine of the peninsula, is a chain of active volcanic peaks. Pleistocene and recent glaciers have carved the broad valleys and jagged ridges that are common here. The relative youth of the volcanism is revealed by the topography as infilling and smoothing of the otherwise rugged terrain by lava, ash, and pyroclastic flows, particularly surrounding the high peaks in the south central part of the image. Elevations here range from near sea level up to 2,618 meters (8,590 feet). Two visualization methods were combined to produce this image: shading and color coding of topographic height. The shade image was derived by computing topographic slope in the north-south direction. Northern slopes appear bright and southern slopes appear dark. Color coding is directly related to topographic height, with green at the lower elevations, rising through yellow, red, and magenta, to white at the highest elevations. Elevation data used in this image were acquired by the Shuttle Radar Topography Mission (SRTM) aboard Space Shuttle Endeavour, launched on February 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on Space Shuttle Endeavour in 1994. SRTM was designed to collect three-dimensional measurements of Earth's surface. To collect the 3-D data, engineers added a 60-meter-long (200-foot) mast, installed additional C-band and X-band antennas, and improved tracking and navigation devices. The mission is a cooperative project between the National Aeronautics and Space Administration (NASA), the National Imagery and Mapping Agency (NIMA) of the U.S. Department of Defense, and the German and Italian space

  15. Shaded Relief, Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2000-01-01

    This topographic image shows the western side of the volcanically active Kamchatka Peninsula, Russia. The data are from the first C-band mapping swath of the Shuttle Radar Topography Mission (SRTM). On the left side are four rivers, which flow northwest to the Sea of Okhotsk. These rivers are, from the south to north, Tigil, Amanina, Voyampolka, and Zhilovaya. The broad, flat floodplains of the rivers are shown in blue. These rivers are important spawning grounds for salmon. In the right side of the image is the Sredinnyy Khrebet, the volcanic mountain range that makes up the 3spine2 of the peninsula. The cluster of hills to the lower right is a field of small dormant volcanoes. High resolution SRTM topographic data will be used by geologists to study how volcanoes form and understand the hazards posed by future eruptions.

    This shaded relief image was generated using topographic data from the Shuttle Radar Topography Mission. A computer-generated artificial light source illuminates the elevation data to produce a pattern of light and shadows. Slopes facing the light appear bright, while those facing away are shaded. On flatter surfaces, the pattern of light and shadows can reveal subtle features in the terrain. Colors show the elevation as measured by SRTM. Colors range from blue at the lowest elevations to white at the highest elevations. This image contains about 2300 meters (7500 feet) of total relief. Shaded relief maps are commonly used in applications such as geologic mapping and land use planning.

    The Shuttle Radar Topography Mission (SRTM), launched on February 11,2000, uses the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. The mission is designed to collect three-dimensional measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter-long (200-foot) mast, an additional C-band imaging antenna and

  16. Perspective View, Kamchatka Peninsula, Russia

    NASA Technical Reports Server (NTRS)

    2000-01-01

    This perspective view shows the western side of the volcanically active Kamchatka Peninsula, Russia. The data are from the first C-band mapping swath of the Shuttle Radar Topography Mission (SRTM). In the foreground is the broad, flat floodplain of the Amanina River, shown in blue. In background of the image is the Sredinnyy Khrebet, the volcanic mountain range that makes up the 3spine2 of the peninsula. The cluster of hills in the upper right is a field of small dormant volcanoes. High resolution SRTM topographic data will be used by geologists to study how volcanoes form and understand the hazards posed by future eruptions.

    This shaded relief perspective view was generated using topographic data from the Shuttle Radar Topography Mission. A computer-generated artificial light source illuminates the elevation data to produce a pattern of light and shadows. Slopes facing the light appear bright, while those facing away are shaded. On flatter surfaces, the pattern of light and shadows can reveal subtle features in the terrain. Colors show the elevation as measured by SRTM. Colors range from blue at the lowest elevations to white at the highest elevations. This image contains about 2300 meters (7500 feet) of total relief. To emphasize subtle differences in topography, the relief is exaggerated by a factor of 5.

    The Shuttle Radar Topography Mission (SRTM), launched on February 11,2000, uses the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. The mission is designed to collect three-dimensional measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter-long (200-foot) mast, an additional C-band imaging antenna and improved tracking and navigation devices. The mission is a cooperative project between the National Aeronautics and Space Administration (NASA), the National Imagery and Mapping Agency (NIMA) and the

  17. United States/Russia Space Cooperation Documentary

    NASA Technical Reports Server (NTRS)

    1993-01-01

    This video documents the initiative to develop a multinational, permanent space research laboratory. Historical background on the U.S. and Soviet manned space flight program as well as joint efforts such as the Apollo-Soyuz link up is shown. The current initiative will begin with collaborative missions involving NASA's space shuttle and Russia's Mir space station, and culminate in a permanently manned space station involving the U.S., Russia, Japan, Canada, and ESA. Shown are computer simulations of the proposed space station. Commentary is provided by the NASA administrator, former astronauts, cosmonauts, and Russian and American space experts.

  18. Cowpox in a human, Russia, 2015.

    PubMed

    Popova, A Y; Maksyutov, R A; Taranov, O S; Tregubchak, T V; Zaikovskaya, A V; Sergeev, A A; Vlashchenko, I V; Bodnev, S A; Ternovoi, V A; Alexandrova, N S; Tarasov, A L; Konovalova, N V; Koroleva, A A; Bulychev, L E; Pyankov, O V; Demina, Y V; Agafonov, A P; Shchelkunov, S N; Miheev, V N

    2017-03-01

    We investigated the first laboratory-confirmed human case of cowpox virus infection in Russia since 1991. Phylogenetic studies of haemagglutinin, TNF-α receptor-like protein and thymidine kinase regions showed significant differences with known orthopoxviruses, including unique amino-acid substitutions and deletions. The described cowpox virus strain, taking into account differences, is genetically closely related to strains isolated years ago in the same geographical region (European part of Russia and Finland), which suggests circulation of viral strains with common origin in wild rodents without spread over long distances and appearance in other parts of the world.

  19. The 'Ice Hill': An example of 'retarded deglaciation' in siberia

    NASA Astrophysics Data System (ADS)

    Astakhov, Valery I.; Isayeva, Lia L.

    The geological structure of one of the southernmost sites of thick ice beds in the Yenisei valley near the Arctic Circle is discussed. The erosion contacts of the foliated and contorted ice, abundance of glacial debris and the position between the basal till and ablation cover indicate a glacial origin for the ice layer. The ice occurs in the cores of arcuate accretion ridges built of ablation materials. The overlying sequence consists of a series of diamicton flows alternating with lacustrine and outwash sediments. Laterally the ice-rock complex changes into thick lacustrine rhythmites underlain by basal tills. The ice-containing hummocky terrain is often lower than the adjacent lacustrine plain. Therefore inversion of ice-controlled topography is suggested. Several stages of glaciokarst development are supposed to have occurred after an eastward moving ice lobe stagnated more than 50 ka BP. The main depositional events are associated with the Middle Weichselian draining of ice-dammed Lake Igarka, and with Early Holocene topographic inversion. The Holocene warming apparently caused diapiric deformation of the buried ice probably because of the density and thickness differences between the ice and the overburden. The long history of burial and preservation of the remnants of basal glacier ice was controlled by Pleistocene permafrost. Landscape evolution in Northern Siberia is governed by such 'retarded deglaciation', in contrast with Atlantic environments. The thick ablation sequence may be described in terms of a Spitsbergen model, but the Siberian basal tills, because of their position within the permafrost, must be regarded as exfoliated layers of debris-rich ice according to Shantzer-Lavrushin's model. The occurrence of buried glacier ice and the mode of distribution of the permafrost shows the relict nature of the latter. In areas of modern and former retarded deglaciation intermittent diamicton flows are supposed to mark episodes of climatic amelioration like

  20. [Health of workers engaged into mining industry in Siberia and Far North].

    PubMed

    Rukavishnikov, V S; Shaiakhmetov, S F; Pankov, V A; Kolycheva, I V

    2004-01-01

    Based on longstanding analysis of transitory disablement morbidity among workers engaged into mining industry of Siberia and Far North, the authors defined factors and conditions contributing to health deterioration among these workers. These factors and conditions are severe climate conditions, long exposure to hazards, bad health care, ineffective methods of treatment and prophylaxis.

  1. Fire Impact on Surface Fuels and Carbon Emissions in Scots pine Logged Sites of Siberia

    NASA Astrophysics Data System (ADS)

    Ivanova, G. A.; Kukavskaya, E. A.; Bogorodskaya, A. V.; Ivanov, V. A.; Zhila, S. V.; Conard, S. G.

    2012-04-01

    Forest fire and large-scale forest harvesting are the two major disturbances in the Russian boreal forests. Non-recovered logged sites total about a million hectares. Logged sites are characterized by higher fire hazard than forest sites due great amounts of logging slash, which dries out much more rapidly compared to understory fuels. Moreover, most logging sites can be easily accessed by local population. Both legal and illegal logging are also increasing rapidly in many forest areas of Siberia. Fire effects on forest overstory, subcanopy woody layer, and ground vegetation biomass were estimated on logged vs. unlogged sites in the Central Siberia region in 2009-2012 as a part of the project "The Influence of Changing Forestry Practices on the Effects of Wildfire and on Interactions Between Fire and Changing Climate in Central Siberia" supported by NASA (NEESPI). Dead down woody fuels are significantly less at unburned/logged area of dry southern regions compared to more humid northern regions. Fuel consumption was typically less in spring fires than during summer fires. Fire-caused carbon emissions on logged sites appeared to be twice that on unlogged sites. Soil respiration is less at logged areas compared to undisturbed forest. After fire soil respiration decreases both at logged and unlogged areas. arbon emissions from fire and post-fire ecosystem damage on logged sites are expected to increase under changing climate conditions and as a result of anticipated increases in future forest harvesting in Siberia.

  2. 75 FR 9252 - Magnesium From China and Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-03-01

    ... COMMISSION Magnesium From China and Russia AGENCY: United States International Trade Commission. ] ACTION: Institution of five-year reviews concerning the antidumping duty orders on magnesium from China and Russia... antidumping duty orders on magnesium from China and Russia would be likely to lead to continuation...

  3. Chinese Students in the Higher Educational Institutions of Russia

    ERIC Educational Resources Information Center

    Aref'ev, A. L.

    2012-01-01

    There has been an increase in the number of students from China studying in Russia, but still less than 2 percent of Chinese who study abroad do so in Russia. A third of these students would not encourage others to do so, on the grounds that educational conditions are not good and that they feel unwelcome in Russia. Most of these students…

  4. 76 FR 77015 - Solid Urea From Russia and Ukraine

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-12-09

    ... COMMISSION Solid Urea From Russia and Ukraine Determination On the basis of the record \\1\\ developed in the... antidumping duty orders on solid urea from Russia and Ukraine would be likely to lead to continuation or... 2011), entitled Solid Urea from Russia and Ukraine: Investigation Nos. 731-TA- 340-E and 340-H...

  5. 76 FR 15339 - Solid Urea From Russia and Ukraine

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-03-21

    ... COMMISSION Solid Urea From Russia and Ukraine AGENCY: United States International Trade Commission. ACTION... orders on solid urea from Russia and Ukraine. SUMMARY: The Commission hereby gives notice that it will...)) to determine whether revocation of the antidumping duty orders on solid urea from Russia and...

  6. Analyses of changes in vegetation cover in the South and Sub-Taiga of Western Siberia using Landsat data

    NASA Astrophysics Data System (ADS)

    Dyukarev, Egor; Pologova, Nina; Golovatskaya, Eugenia

    2010-05-01

    Understanding human impact on vegetation composition and structure, at scales from the patch to the globe, and capacity to monitor change over time is fundamental research problem to address Global Change and ensure sustainable development. Natural ecosystems at the South and Sob-Taiga zone of Western Siberia are characterized by development of an early successional states, given the projected increase in disturbance, or will be converted into human-dominated terrestrial production systems. Disturbances (e.g., fire, dieback due to insect attacks) appear to be increasing in some regions, leading to fragmentation of natural ecosystems and to a generally "weedier," structurally simpler biosphere with fewer systems in a more ecologically complex old-growth state. The analysis of structure of vegetation cover at two test sites located at the south-west part of the West-Siberian Plain in the South and Sub-Taiga zone was made using LANDSAT space images and ground data. The studied area of the first test site ("Bakchar") is occupied by bogs, paludificated forests and cultivated lands. Test site "Tomsk" covered by cultivated lands in the south, dark coniferous forest complexes an early and old-growth state in the north part. Mire types at the test sites are presented by open fens, ridge-hollow / ridge-lake complexes and pine-shrub-sphagnum communities with different tree height and layer density. During the XX century the vegetation cover was exposed to natural and anthropogenic changes. Comparison of space images from different years (1990, 1999 and 2007) allowed revealing dynamics in vegetation cover. Forest change was calculated using the Disturbance Index (Healey, 2006). Decrease of forest area in 1990-1999 are primary occurs due to intense forest cutting for timber industry and local use. A strong wind have damaged forests between 1990 and 1999 in stripes oriented from south-west to north -east in the prevailing wind direction. Strong winds were registered in 2003

  7. Space Radar Image of Moscow, Russia

    NASA Technical Reports Server (NTRS)

    1994-01-01

    This is a vertically polarized L-band image of the southern half of Moscow, an area which has been inhabited for 2,000 years. The image covers a diameter of approximately 50 kilometers (31 miles) and was taken on September 30, 1994 by the Spaceborne Imaging Radar-C/X-band Synthetic Aperture Radar aboard the space shuttle Endeavour. The city of Moscow was founded about 750 years ago and today is home to about 8 million residents. The southern half of the circular highway (a road that looks like a ring) can easily be identified as well as the roads and railways radiating out from the center of the city. The city was named after the Moskwa River and replaced Russia's former capital, St. Petersburg, after the Russian Revolution in 1917. The river winding through Moscow shows up in various gray shades. The circular structure of many city roads can easily be identified, although subway connections covering several hundred kilometers are not visible in this image. The white areas within the ring road and outside of it are buildings of the city itself and it suburban towns. Two of many airports are located in the west and southeast of Moscow, near the corners of the image. The Kremlin is located north just outside of the imaged city center. It was actually built in the 16th century, when Ivan III was czar, and is famous for its various churches. In the surrounding area, light gray indicates forests, while the dark patches are agricultural areas. The various shades from middle gray to dark gray indicate different stages of harvesting, ploughing and grassland. Spaceborne Imaging Radar-C and X-band Synthetic Aperture Radar (SIR-C/X-SAR) is part of NASA's Mission to Planet Earth. The radars illuminate Earth with microwaves, allowing detailed observations at any time, regardless of weather or sunlight conditions. SIR-C/X-SAR uses three microwave wavelengths: L-band (24 cm), C-band (6 cm) and X-band (3 cm). The multi-frequency data will be used by the international scientific

  8. Integrated chronostratigraphy of Proterozoic-Cambrian boundary beds in the western Anabar region, northern Siberia

    NASA Technical Reports Server (NTRS)

    Kaufman, A. J.; Knoll, A. H.; Semikhatov, M. A.; Grotzinger, J. P.; Jacobsen, S. B.; Adams, W.

    1996-01-01

    Carbonate-rich sedimentary rocks of the western Anabar region, northern Siberia, preserve an exceptional record of evolutionary and biogeochemical events near the Proterozoic/Cambrian boundary. Sedimentologically, the boundary succession can be divided into three sequences representing successive episodes of late transgressive to early highstand deposition; four parasequences are recognized in the sequence corresponding lithostratigraphically to the Manykal Formation. Small shelly fossils are abundant and include many taxa that also occur in standard sections of southeastern Siberia. Despite this coincidence of faunal elements, biostratigraphic correlations between the two regions have been controversial because numerous species that first appear at or immediately above the basal Tommotian boundary in southeastern sections have first appearances scattered through more than thirty metres of section in the western Anabar. Carbon- and Sr-isotopic data on petrographically and geochemically screened samples collected at one- to two-metre intervals in a section along the Kotuikan River, favour correlation of the Staraya Reckha Formation and most of the overlying Manykai Formation with sub-Tommotian carbonates in southeastern Siberia. In contrast, isotopic data suggest that the uppermost Manykai Formation and the basal 26 m of the unconformably overlying Medvezhya Formation may have no equivalent in the southeast; they appear to provide a sedimentary and palaeontological record of an evolutionarily significant time interval represented in southeastern Siberia only by the sub-Tommotian unconformity. Correlations with radiometrically dated horizons in the Olenek and Kharaulakh regions of northern Siberia suggest that this interval lasted approximately three to six million years, during which essentially all 'basal Tommotian' small shelly fossils evolved.

  9. Modern nature and climate changes in Siberia: new methods and results of analysis of instrumented observations

    NASA Astrophysics Data System (ADS)

    Kabanov, Mikhail V.

    2002-02-01

    Peculiarity of nature and climate changes in middle latitudes of the Northern Hemisphere and in Siberia is that the temporal variability of meteorological quantities here has a wide range and their spatial variability has a complicated zone structure. Therefore, regional monitoring of modern nature and climate changes in Siberia is of scientific interest from the viewpoint of the global changes observed. Another Siberian peculiarity is associated with the fact that there are many unique objects that have global importance both as natural complexes (boreal forests, water- bog systems, Baikal lake, etc.) And as technogenic objects (oil and gas production, coal mining, metallurgy, transport, etc.). Therefore monitoring and modeling of regional nature and climate changes in Siberia have great practical importance, which is underestimated now, for industrial development of Siberia. Taking into account the above peculiarities and tendencies on investigation of global and regional environmental and climate changes, the multidisciplinary project on Climate and Ecological Monitoring of Siberia (CEMS) was accepted to the research and development program Sibir' since 1993. To realize this project, the Climate and Ecological Observatory was established in Tomsk at the Institute for Optical Monitoring (IOM) SB RAS. At the present time the stations (the basic and background ones) of this observatory are in a progress and theory and instruments for monitoring are being developed as well. In this paper we discuss some results obtained in the framework of CEMS project that were partially published in the monographs, in scientific journals, and will be published in the Proceedings of the 8th Joint International Symposium on Atmospheric and Ocean Optics and Atmosphere Physics. This review has a purpose not only to discuss the obtained regularities but also to formulate scientific and technical tasks for further investigations into the regional changes of technogenic, natural, and

  10. Smoke and Clouds over Russia

    NASA Technical Reports Server (NTRS)

    2001-01-01

    Several mountain ranges and a portion of the Amur River are visible in this set of MISR images of Russia's far east Khabarovsk region. The images were acquired on May 13, 2001 during Terra orbit 7452. The view from MISR's 70-degree forward-looking camera is at the top left; the 26-degree forward-looking view is at the top right. The larger image at the bottom is a stereo 'anaglyph' created using the cameras at two intermediate angles. To view the stereo image in 3-D you need red/blue glasses with the red filter placed over your left eye. All of the images are oriented with north to the left to facilitate stereo viewing. Each image covers an area about 345 kilometers x 278 kilometers.

    The Amur River, in the upper right, and Lake Bolon, at the top center, are most prominent in the 26-degree view due to sunglint (mirror-like reflection of the Sun's rays by the water). The Amur River valley is a primary breeding ground for storks and cranes and a stopover for large numbers of migratory birds. About 20% of the Amur wetlands are protected by official conservation measures, but human development has converted large portions to agricultural uses. Other notable features in these images are several mountain chains, including the Badzhal'skiy to the left of center and the Bureiskiy in the lower left.

    Smoke plumes from several forest fires can be seen. They are especially apparent in the 70-degree view where the smoke's visibility is accentuated, in part, by the long slant path through the atmosphere. The largest plumes are in the lower left and upper right, with some smaller plumes above and to the right of the image centers. In the upper images the hazy region in the vicinity of these smaller plumes has the appearance of low-altitude smoke, but depth perception provided by the stereo anaglyph shows that it is actually a distinct layer of high-altitude cirrus clouds. Whether the cirrus is related to the fires is uncertain. It is possible, however, for the fires have

  11. The "Ride for Russia" Tree Lichen Survey

    ERIC Educational Resources Information Center

    Young, Simon

    2013-01-01

    The prevalence of nine indicator lichens found on trees in Northern Europe and Western Russia was used for monitoring air quality. The 4200 mile route of the survey went through eight countries. Surveys were carried out in cities, towns, countryside and forests, and along motorways. The author has conducted tree lichen surveys with pupils from…

  12. Life-Threatening Sochi Virus Infections, Russia.

    PubMed

    Kruger, Detlev H; Tkachenko, Evgeniy A; Morozov, Vyacheslav G; Yunicheva, Yulia V; Pilikova, Olga M; Malkin, Gennadiy; Ishmukhametov, Aydar A; Heinemann, Patrick; Witkowski, Peter T; Klempa, Boris; Dzagurova, Tamara K

    2015-12-01

    Sochi virus was recently identified as a new hantavirus genotype carried by the Black Sea field mouse, Apodemus ponticus. We evaluated 62 patients in Russia with Sochi virus infection. Most clinical cases were severe, and the case-fatality rate was as high as 14.5%.

  13. Novel variant of tickborne encephalitis virus, Russia.

    PubMed

    Ternovoi, Vladimir A; Protopopova, Elena V; Chausov, Eugene V; Novikov, Dmitry V; Leonova, Galina N; Netesov, Sergey V; Loktev, Valery B

    2007-10-01

    We isolated a novel strain of tickborne encephalitis virus (TBEV), Glubinnoe/2004, from a patient with a fatal case in Russia. We sequenced the strain, whose landmark features included 57 amino acid substitutions and 5 modified cleavage sites. Phylogenetically, Glubinnoe/2004 is a novel variant that belongs to the Eastern type of TBEV.

  14. Child Care in Russia: In Transition.

    ERIC Educational Resources Information Center

    Ispa, Jean

    With the advent of "perestroika" and "glasnost," Russian childcare and education underwent a transitional period in practice and theory. Contrasting impressions from an earlier visit under the Communist regime, this book describes the experiences of Jean Ispa in her travels to Russia, observing children in six child care…

  15. Education in the Fate of Today's Russia

    ERIC Educational Resources Information Center

    Borisenkov, V.P.; Kraevskii, V.V.; Valeev, G.Kh.; Avtonomova, N.S.; Evdokimov, A.K.; Shchedrina, T.G.; Belomestnova, N.V.; Beliaeva, M.A.; Shimina, A.N.; Karmanchikov, A.J.; Korol, A.D.; Varnavskaia, N.Ia.; Berezhnova, E.V.; Daniliuk, A.Ia.; Anua, R.G.; Sidorina, T.Iu.; Tarba, I.D.; Arlamov, A.A.

    2008-01-01

    Education in the fate of today's Russia was the topic of a scientific seminar titled "Philosophy, Education, and Society," held in the summer of 2007 in the city of Gagra by the editors of the journals "Voprosy filosofii" and "Pedagogika," the Moscow N.E. Bauman State Technical University, and the Russian Academy of…

  16. SAYANI'91 - A joint United States/Commonwealth of Independent States field campaign to investigate forest decline damage in the Krasnoyarsk region of southcentral Siberia

    NASA Technical Reports Server (NTRS)

    Williams, D. L.; Kharuk, V. I.; Zhirin, V. M.; Rock, B. N.; Ranson, K. J.; Wessman, C. A.; Curtiss, B.

    1992-01-01

    The field experiment described took place in the Sayani Mountains of Siberia. The purpose of the joint field campaign was to observe and exchange methodologies with Russian scientists with regard to the development of remote sensing techniques for the early detection and assessment of forest decline damage believed to be associated with atmospheric deposition and/or insect and disease infestations. Several types of passive and active remote sensing measurements were made in conjunction with biophysical measurements on vegetative samples collected from four study sites representing a strong elevational gradient. Relatively cloud-free SPOT data were also acquired over the study area. Moderate canopy damage was recorded at the mid-elevation site (3400 ft/1037 m). The lowest levels of damage were recorded at the lowest elevation site (2300 ft/701 m.) At all sites, east versus west flagging of the canopy was noted (i.e., full canopy on the west-facing side of the canopy, significantly less foliage on the east-facing side).

  17. The changing nature of murder in Russia.

    PubMed

    Chervyakov, Valeriy V; Shkolnikov, Vladimir M; Pridemore, William Alex; McKee, Martin

    2002-11-01

    The death rate from homicide in Russia increased rapidly during the 1990 s. It is now about 20 times higher than in western Europe and is among the highest recorded anywhere in the world. However, this issue has received little attention so far from public health researchers or policymakers. This paper describes the changing nature of homicide during the 1990 s in Russia as a whole and, in more detail, in the Udmurt Republic. The study uses data from three sources: routine mortality data for Russia from 1970 to 1999; statistics on criminal investigations and convictions in Russia between 1990 and 1997; and an in-depth study of homicide trial records in the Udmurt Republic in 1989-1991 and 1998.Deaths from homicide increased between 1970 and 1985, falling slightly during the 1985 anti-alcohol campaign and then resuming their increase until 1994. Another fall in the late 1990 s was arrested in 1998, with an increase in 1999. By 1999 the age standardised homicide death rate in Russia was 81% higher than in 1990, an increase almost twice that of all causes of death combined. Throughout the 1990 s about 10% of those convicted of homicide were female. Of those homicides leading to convictions in the Udmurt Republic, 71% of those killed by males were male, as were 76% of those killed by females. Killings of women by men often involved sexual assaults. In Russia as a whole, about 80% of those convicted of homicide were reported to be under the influence of alcohol at the time. In the Udmurt Republic, where data on both offender and victim were available, victims were also commonly intoxicated. The nature of homicide in Russia has changed considerably in less than a decade, with many more now involving aggravating circumstances, such as murder to conceal another crime, in association with robbery or rape, or by a group of people. Although still a small proportion of the total convicted, the number of murders by hired killers is also on the rise. The characteristics of those

  18. Inclusions of chlorides in natural diamonds from Siberia

    NASA Astrophysics Data System (ADS)

    Titkov, Sergey; Ryabchikov, Igor; Pomazansky, Bogdan; Magazina, Larisa

    2010-05-01

    In recent years, microinclusions of Cl-bearing high density fluids that contained silicic, carbonatitic and saline components in variable proportions have been revealed in octahedral diamonds with cloudy central or intermediate growth zones, in diamonds with fibrous coat and in fibrous cubic diamonds from many kimberlite deposits (Tomlinson et al., 2006; Klein-BenDavid et al., 2007 and references therein). Experimental works have shown that chloride-bearing system is a favorable medium for diamond growth (Palyanov et al., 2007). In course of study of microinclusions in diamonds from Siberia unusual chloride microinclusions with specific morphologies have been found by us in a rounded dark-grey dodecahedron from the placer deposits with unknown source in northern Yakutia and in a dark-grey coarse-grained polycrystalline aggregate of diamond from the kimberlites of western Yakutia. The rounded dodecahedron represented V variety according to the diamond classification by Y.L.Orlov consisted of a quite perfect core and fibrous coat with abundant black microinclusions. Its rounded shape was formed during post growth dissolution. The polycrystalline diamond aggregate contained numerous black microinclusions of magnetite and some other Fe-phase as was reported previously (Titkov et al., 2003). The microinclusions were studied using a JEOL JSM-5300 scanning electron microscope equipped with an Oxford LINK ISIS energy-dispersive spectrometer with an analytical range from Be to U. In preparation for analysis, each sample was crushed after being wrapped in a special paper to avoid contamination. Analysis was performed on rough surfaces of fragments that were fairly flat and oriented nearly perpendicular to the electron beam. These samples were carbon coated. Study of rounded dodecahedron fragments revealed irregular cavity, about 30 m across. Its main volume was occupied by a large inclusion of variable composition with an average of 20.6 wt% Na, 15.5 wt% K, 0.6 wt% S, 0

  19. Lithostratigraphic, conodont, and other faunal links between lower Paleozoic strata in northern and central Alaska and northeastern Russia

    USGS Publications Warehouse

    Dumoulin, Julie A.; Harris, Anita G.; Gagiev, Mussa; Bradley, Dwight C.; Repetski, John E.

    2002-01-01

    Lower Paleozoic platform carbonate strata in northern Alaska (parts of the Arctic Alaska, York, and Seward terranes; herein called the North Alaska carbonate platform) and central Alaska (Farewell terrane) share distinctive lithologic and faunal features, and may have formed on a single continental fragment situated between Siberia and Laurentia. Sedimentary successions in northern and central Alaska overlie Late Proterozoic metamorphosed basement; contain Late Proterozoic ooid-rich dolostones, Middle Cambrian outer shelf deposits, and Ordovician, Silurian, and Devonian shallow-water platform facies, and include fossils of both Siberian and Laurentian biotic provinces. The presence in the Alaskan terranes of Siberian forms not seen in wellstudied cratonal margin sequences of western Laurentia implies that the Alaskan rocks were not attached to Laurentia during the early Paleozoic.The Siberian cratonal succession includes Archean basement, Ordovician shallow-water siliciclastic rocks, and Upper Silurian–Devonian evaporites, none of which have counterparts in the Alaskan successions, and contains only a few of the Laurentian conodonts that occur in Alaska. Thus we conclude that the lower Paleozoic platform successions of northern and central Alaska were not part of the Siberian craton during their deposition, but may have formed on a crustal fragment rifted away from Siberia during the Late Proterozoic. The Alaskan strata have more similarities to coeval rocks in some peri-Siberian terranes of northeastern Russia (Kotelny, Chukotka, and Omulevka). Lithologic ties between northern Alaska, the Farewell terrane, and the peri-Siberian terranes diminish after the Middle Devonian, but Siberian afµnities in northern and central Alaskan biotas persist into the late Paleozoic.

  20. Greening of the Arctic: Partitioning Warming Versus Reindeer Herbivory for Willow Populations on Yamal Peninsula, Northwest Siberia

    NASA Astrophysics Data System (ADS)

    Forbes, B. C.; Macias-Fauria, M.; Zetterberg, P.; Kumpula, T.

    2012-12-01

    Arctic warming has been linked to observed increases in tundra shrub cover and growth in recent decades on the basis of significant relationships between deciduous shrub growth/biomass and temperature. These vegetation trends have been linked to Arctic sea-ice decline and thus to the sea-ice/albedo feedback known as Arctic amplification. However, the interactions between climate, sea ice, tundra vegetation and herbivores remain poorly understood. Recently we revealed a 50-year growth response over a >100,000 km2 area to a rise in summer temperature for willow (Salix lanata), one the most abundant shrub genera at and north of the continental treeline and an important source of reindeer forage in spring, summer and autumn. We demonstrated that whereas plant productivity is related to sea ice in late spring, the growing season peak responds to persistent synoptic-scale air masses over West Siberia associated with Fennoscandian weather systems through the Rossby wave train. Substrate was important for biomass accumulation, yet a strong correlation between growth and temperature encompasses all observed soil types. Vegetation was especially responsive to temperature in early summer. However, the role of herbivory was not addressed. The present data set explores the relationship between long-term herbivory and growth trends of shrubs experiencing warming in recent decades. Semi-domestic reindeer managed by indigenous Nenets nomads occur at high densities in summer on exposed ridge tops and graze heavily on prostrate and low erect willows. A few meters away in moderately sloped landslides tall willows remain virtually ungrazed as their canopies have grown above the browse line of ca. 180 cm. Here we detail the responses of neighboring shrub populations with and without intensive herbivory yet subject to the same decadal warming trend.

  1. The Security of Russia's Nuclear Arsenal: The Human Factor

    SciTech Connect

    Ball, D.Y.

    1999-10-12

    Assertions by the Russian military that all of their nuclear weapons are secure against theft and that nuclear units within the military are somehow insulated from the problems plaguing the Russian military should not be accepted uncritically. Accordingly, we should not give unwarranted credence to the pronouncements of military figures like Cal.-Gen. Igor Valynkin, Chief of the Defense Ministry's 12th Main Directorate, which oversees the country's nuclear arsenal. He contends that ''Russian nuclear weapons are under reliable supervision'' and that ''talk about the unreliability of our control over nuclear weapons has only one pragmatic goal--to convince international society that the country is incapable of maintaining nuclear safety and to introduce international oversight over those weapons, as it is done, for example, in Iraq.'' While the comparison to Iraq is preposterous, many analysts might agree with Valynkin's sanguine appraisal of the security of Russia's nuclear weapons. In contrast, I argue that the numerous difficulties confronting the military as a whole should cause concern in the West over the security of the Russian nuclear arsenal.

  2. Mesozoic tectonics of the Arctic: New constraints from provenance studies,Taimyr, Russia

    NASA Astrophysics Data System (ADS)

    Zhang, X.; Pease, V.

    2013-12-01

    Understanding the tectonic development of the Arctic Ocean is important for understanding global tectonics and the framework of petroleum and mineral resources in the Arctic area. The Eurasia and Amerasia basins are the principal physiographic domains of the Arctic Ocean. The Eurasia Basin is known to be the result of slow seafloor spreading; the origin of the Amerasia Basin however remains controversial. Lack of information on the timing, structure, and geochemistry of geological units around the Amerasia Basin limits our ability to understand its development. The Taimyr Peninsula where Mesozoic deformation is well-developed provides a natural laboratory to investigate the tectonic development of the Amerasia Basin. Provenance studies of Taimyr constrain the source areas of Mesozoic sediments in the region and thus identify affinities between them. Detrital zircons from six samples of Triassic and Jurassic sandstone from Southern Taimyr were dated using LA-ICP-MS to test existing models for the opening of the Amerasia Basin. Two Triassic samples present great similarity in detrital zircon population with Triassic sandstone from the paleo-Taimyr river system, including Chukotka, the Wrangel Island and the New Siberian Islands. These samples all contain Permo-Triassic (236 - 250 Ma), Permo-Carboniferous (260 - 330 Ma), Devonian (340 - 390 Ma) late Precambrian-Silurian (420 - 580 Ma) and Neoproterozoic (620 - 1000 Ma) zircons. These detrital zircon ages suggest Triassic sediments in these locations may have been derived from Siberia Trap, Taimyr and the Ural Mountains of Arctic Russia. It is therefore likely that Taimyr, Chukotka, the Wrangel Island and the New Siberian Islands which are separated at present were close to each other or belonged to the same large drainage system before the opening of the Amerasia Basin. Two Middle Jurassic samples and two Upper Jurassic samples from Taimyr have dominant Permo-Triassic peaks (246 - 260 Ma) suggesting a proximal source

  3. Thermal processes of thermokarst lakes in the continuous permafrost zone of northern Siberia - observations and modeling (Lena River Delta, Siberia)

    NASA Astrophysics Data System (ADS)

    Boike, J.; Georgi, C.; Kirilin, G.; Muster, S.; Abramova, K.; Fedorova, I.; Chetverova, A.; Grigoriev, M.; Bornemann, N.; Langer, M.

    2015-10-01

    Thermokarst lakes are typical features of the northern permafrost ecosystems, and play an important role in the thermal exchange between atmosphere and subsurface. The objective of this study is to describe the main thermal processes of the lakes and to quantify the heat exchange with the underlying sediments. The thermal regimes of five lakes located within the continuous permafrost zone of northern Siberia (Lena River Delta) were investigated using hourly water temperature and water level records covering a 3-year period (2009-2012), together with bathymetric survey data. The lakes included thermokarst lakes located on Holocene river terraces that may be connected to Lena River water during spring flooding, and a thermokarst lake located on deposits of the Pleistocene Ice Complex. Lakes were covered by ice up to 2 m thick that persisted for more than 7 months of the year, from October until about mid-June. Lake-bottom temperatures increased at the start of the ice-covered period due to upward-directed heat flux from the underlying thawed sediment. Prior to ice break-up, solar radiation effectively warmed the water beneath the ice cover and induced convective mixing. Ice break-up started at the beginning of June and lasted until the middle or end of June. Mixing occurred within the entire water column from the start of ice break-up and continued during the ice-free periods, as confirmed by the Wedderburn numbers, a quantitative measure of the balance between wind mixing and stratification that is important for describing the biogeochemical cycles of lakes. The lake thermal regime was modeled numerically using the FLake model. The model demonstrated good agreement with observations with regard to the mean lake temperature, with a good reproduction of the summer stratification during the ice-free period, but poor agreement during the ice-covered period. Modeled sensitivity to lake depth demonstrated that lakes in this climatic zone with mean depths > 5 m develop

  4. Clinical trials in Russia: achieving excellence

    NASA Astrophysics Data System (ADS)

    Reznik, Robert S.; Ichim, Thomas E.; Petrov, Vladimir; Reznik, Boris N.

    2005-06-01

    The Russian population offers a unique opportunity for conducting clinical trials in general, and specifically in the area of Medical Devices. Although the regulatory framework for approval of clinical trials and eventual marketing registration is based on an American-style format, details of operating in the Russian framework are very different. Understanding and leveraging the unique characteristics of the Russian system on the patient side, the investigator side, and the regulatory side is important in extracting optimum value out of clinical trials in Russia. Having performed Medical Device research and clinical trials in Russia, the authors overview the present system and describe various strategies for working in this growing but still under-utilized clinical trials arena.

  5. Stable isotope ratios of atmospheric CO_{2} and CH_{4} over Siberia measured at ZOTTO

    NASA Astrophysics Data System (ADS)

    Timokhina, Anastasiya; Prokushkin, Anatily; Lavric, Jost; Heimann, Martin

    2016-04-01

    The boreal and arctic zones of Siberia housing the large amounts of carbon stored in the living biomass of forests and wetlands, as well as in soils and specifically permafrost, play a crucial role in earth's global carbon cycle. The long-term studies of greenhouse gases (GHG) concentrations are important instruments to analyze the response of these systems to climate warming. In parallel to GHG observations, the measurements of their stable isotopic composition can provide useful information for distinguishing contribution of individual GHG source to their atmospheric variations, since each source has its own isotopic signature. In this study we report first results of laboratory analyses of the CO2 and CH4 concentrations, the stable isotope ratio of δ13C-CO2, δ18O-CO2, δ13C-CH4, δD-CH4 measured in one-liter glass flasks which were obtained from 301 height of ZOTTO (Zotino Tall Tower Observatory, near 60° N, 90° E, about 20 km west of the Yenisei River) during 2008 - 2013 and 2010 - 2013 for stable isotope composition of CO2 and CH4. The magnitudes of δ13C-CO2 and δ18O-CO2 in a seasonal cycle are -1.4±0.1‰ (-7.6 - -9.0‰) and -2.2±0.2‰ (-0.1 - -2.3‰), respectively. The δ13C-CO2 seasonal pattern opposes the CO2 concentrations, with a gradual enrichment in heavy isotope occurring during May - July, reflecting its discrimination in photosynthesis, and further depletion in August - September as photosynthetic activity decreases comparatively to ecosystem respiration. Relationship between the CO2 concentrations and respective δ13C-CO2 (Keeling plot) reveals isotopic source signature for growing season (May - September) -27.3±1.4‰ and -30.4±2.5‰ for winter (January - March). The behavior of δ18O-CO2 associated with both high photosynthetic rate in the June (enrichment of atmospheric CO2 by 18O as consequence of CO2 equilibrium with "heavy" leaf water) and respiratory activity of forest floor in June - October (depletion of respired CO2 by 18O

  6. NATO Needs a Comprehensive Strategy for Russia

    DTIC Science & Technology

    2015-01-01

    plausible future Russian coer- cion and threats, reassure NATO member states, and help support the security of non-NATO states, especially Ukraine. However...and prospective adversaries. Rhetoric against Russia has been forceful, while the response to Russian behavior is centered on a debate about...Ukraine Stability in Afghanistan 70 60 50 40 30 20 10 80 0 United States Europe 59 73 49 43 53 43 55 41 53 57 3 • What degree of Russian influence should

  7. Land Change in Russia since 2000

    NASA Astrophysics Data System (ADS)

    de Beurs, K.; Ioffe, G.; Nefedova, T.

    2010-12-01

    Agricultural reform has been an important anthropogenic change process shaping landscapes in European Russia since the formal collapse of the Soviet Union at the end of 1991. Widespread land abandonment is perhaps the most evident side effect of the reform, even visible in synoptic imagery. While land abandonment as a result of the collapse of the Soviet Union is relatively well documented, few studies have investigated the unfolding process of abandonment that results from rural population declines. Russia’s population is projected to shrink by a staggering 29% by 2050 and population dynamics are predicted to play a significant role structuring rural landscapes across European Russia. While often treated as a unified whole with respect to agricultural reform, significant regional diversity exists in Russia. Official statistics at the rayon (county) level are typically skewed toward large-scale farming and farm data from important household productions are summarized into regional averages. In addition, data at sub-district level can often only be obtained by visiting rural administrators in person. Large scale official data thus need to be interpreted with caution. Here we present data collected during the summer of 2010 from representative settlements and enterprises in selected counties within the oblasts (states) of Kostroma and Samara. These field data will provide an initial overview of the economic and social state in modern rural western Russia. We will combine the field data with established socio-demographic observations as well as satellite observations at multiple scales to understand the effect of global change and to project future developments.

  8. [Wood transformation in dead-standing trees in the forest-tundra of Central Siberia].

    PubMed

    Mukhortova, L V; Kirdianov, A V; Myglan, V S; Guggenberger, G

    2009-01-01

    Changes in the composition of wood organic matter in dead-standing spruce and larch trees depending on the period after their death have been studied in the north of Central Siberia. The period after tree death has been estimated by means of cross-dating. The results show that changes in the composition of wood organic matter in 63% of cases are contingent on tree species. Wood decomposition in dead-standing trees is accompanied by an increase in the contents of alkali-soluble organic compounds. Lignin oxidation in larch begins approximately 80 years after tree death, whereas its transformation in spruce begins not earlier than after 100 years. In the forest-tundra of Central Siberia, the rate of wood organic matter transformation in dead-standing trees is one to two orders of magnitude lower than in fallen wood, which accounts for their role as a long-term store of carbon and mineral elements in these ecosystems.

  9. The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum.

    PubMed

    Alexandrov, G A; Brovkin, V A; Kleinen, T

    2016-04-20

    Boreal and subarctic peatlands are an important dynamical component of the earth system. They are sensitive to climate change, and could either continue to serve as a carbon sink or become a carbon source. Climatic thresholds for switching peatlands from sink to source are not well defined, and therefore, incorporating peatlands into Earth system models is a challenging task. Here we introduce a climatic index, warm precipitation excess, to delineate the potential geographic distribution of boreal peatlands for a given climate and landscape morphology. This allows us to explain the present-day distribution of peatlands in Western Siberia, their absence during the Last Glacial Maximum, their expansion during the mid-Holocene, and to form a working hypothesis about the trend to peatland degradation in the southern taiga belt of Western Siberia under an RCP 8.5 scenario for the projected climate in year 2100.

  10. Growth dynamics and biodiversity of larch forest after wildfire at the north of central Siberia

    SciTech Connect

    Danilin, I.

    1996-12-31

    Investigations of qualitative and quantitative changes occurring in disturbed forest communities in Siberia are now recognized as important issues, since anthropogenic stress is increasingly affecting forests from year to year and often results in irreversible decomposition of forest ecosystems over large areas. In forests of central Siberia, fire accounts for the greatest disturbance. The level of fire-caused forest destruction is noticeably high. Space imagery analysis has revealed that, from 1980 throughout 1995, the average annual forest area covered by fires was more than 500,000 ha. In as much as this is a country with permafrost soils, fires promote swamping and treeless areas. However, forests regenerate naturally on some burned areas. Forest regeneration can occur either with stand replacement (through secondary birch) or without replacement when new forests are formed by the pre-fire edificators. The second way of succession is ecologically more preferable, because the larch population is more resistant to external influences and keeps its native biodiversity.

  11. An Estimation of Change in Forest Area in Central Siberia Using Multi Temporal SAR Data

    NASA Astrophysics Data System (ADS)

    Tanase, Mihai; Le Toan, Thuy; de la Riva, Juan; Santoro, Maurizio

    2008-11-01

    The objective of this study is forest cover change quantification in Central Siberia, using ALOS-PALSAR data and forest/biomass map product of SIBERIA project. Two sites (Irkutsk and Krasnoyarsk), covering around 50,000 km2 each are studied. The classification algorithm is developed in the Irkutsk site and applied without further modification to the Krasnoyarsk site. Classification accuracy is assessed for the Krasnoyarsk site using as reference data from the Russian forest inventory. Over the studied period, a net forest cover loss of 9 to 11.5 % is estimated, depending on the site. Deforestation affects 12.2% to 16% of the area while forest regrowth is registered for only 3.2 to 4.5% of the studied area. Among the different causes that could explain forest area loss (e.g. natural disasters, clear cuts etc.) the geometric shape of the detected forest cover changes suggests an active deforestation process.

  12. The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum

    NASA Astrophysics Data System (ADS)

    Alexandrov, G. A.; Brovkin, V. A.; Kleinen, T.

    2016-04-01

    Boreal and subarctic peatlands are an important dynamical component of the earth system. They are sensitive to climate change, and could either continue to serve as a carbon sink or become a carbon source. Climatic thresholds for switching peatlands from sink to source are not well defined, and therefore, incorporating peatlands into Earth system models is a challenging task. Here we introduce a climatic index, warm precipitation excess, to delineate the potential geographic distribution of boreal peatlands for a given climate and landscape morphology. This allows us to explain the present-day distribution of peatlands in Western Siberia, their absence during the Last Glacial Maximum, their expansion during the mid-Holocene, and to form a working hypothesis about the trend to peatland degradation in the southern taiga belt of Western Siberia under an RCP 8.5 scenario for the projected climate in year 2100.

  13. The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum

    PubMed Central

    Alexandrov, G. A.; Brovkin, V. A.; Kleinen, T.

    2016-01-01

    Boreal and subarctic peatlands are an important dynamical component of the earth system. They are sensitive to climate change, and could either continue to serve as a carbon sink or become a carbon source. Climatic thresholds for switching peatlands from sink to source are not well defined, and therefore, incorporating peatlands into Earth system models is a challenging task. Here we introduce a climatic index, warm precipitation excess, to delineate the potential geographic distribution of boreal peatlands for a given climate and landscape morphology. This allows us to explain the present-day distribution of peatlands in Western Siberia, their absence during the Last Glacial Maximum, their expansion during the mid-Holocene, and to form a working hypothesis about the trend to peatland degradation in the southern taiga belt of Western Siberia under an RCP 8.5 scenario for the projected climate in year 2100. PMID:27095029

  14. Flooding of the Taz, Pur, and Yenisey Rivers, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    Each spring and summer, rivers across Siberia experience flooding as the waters in the south begin to melt and run before the ice has retreated from the northern limits. The ice causes jams which are sometimes loosened up using explosives. This pair of MODIS images from June 18, 2002, shows flooding on the Pur (left), Taz (center), and Yenisey (right) Rivers in central Siberia. In the false-color image, ice and snow are red, clouds are white, water is black, and vegetation is green. Bare soil is brown. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  15. Food legislation and its harmonization in Russia.

    PubMed

    Shamtsyan, Mark

    2014-08-01

    Bringing Russian legislation into compliance with international norms and standards is necessary after its accession to the World Trade Organization. Harmonization of food legislation and of sanitary and phytosanitary measures are among the problems that had to be solved first. Many Russian food and trade regulations had been changed or are still in the process of being reformed, largely owing to a policy of integration pursued by the Customs Union of Russia, Belarus and Kazakhstan. However, as a member of the Eurasian Economic Community, Russia is also engaged not only in harmonization throughout the Customs Union but also Kirgizstan and Tajikistan, and Armenia, Moldova and Ukraine as observer countries. Russia also continues to coordinate policy reforms closely with the European Union, its primary trade partner, ultimately bringing Russian food and sanitary norms closer to international standards (e.g. Codex). Today, all participants in the Russian food production chain, processing and sale of foods have to deal with growing numbers of security standards. Many organizations are certified under several schemes, which leads to unnecessary costs. Harmonization of standards has helped promote solutions in the domestic market as well as import-export of foods and raw materials for production. Priorities have included food safety for human health, consumer protection, removal of hazardous and/or adulterated products and increased competition within the domestic food market as well as mutual recognition of certification in bilateral and multilateral (inter)national agreements.

  16. When did "scientific psychology" begin in Russia?

    PubMed

    Sirotkina, Irina

    2006-01-01

    The pattern of the institutionalisation of psychology in Russia was as complex as in other countries. The institutionalisation was more than a single event or even a series of events: it was a manifold process that involved various actors, groups, and political parties, and took at least several decades. Psychology was taught within the subject of philosophy, but as a separate course, at high schools, from the early nineteenth century. When, in mid-century, philosophy was banned from universities for political reasons, logic and psychology still remained in the curriculum. Psychology became a contested area in the 1860s, with the rise of the radical movement that accompanied the abolition of serfdom and other reforms. The young radicals, or nihilists, favoured positive science and gave clear preference to physiology; at medical schools, psychology gradually became part of physiology and psychiatry teaching. Psychiatric clinics provided a venue for the first psychological experiments; the first courses in experimental psychology were also taught to psychiatry students. At the turn of the century, humanities departments joined in by opening laboratories and adding courses in experimental psychology to the philosophical psychology traditionally taught. Yet by 1917, the year when the monarchy ended in Russia, only two universities, in Moscow and Odessa, had succeeded in founding laboratories. The institutionalisation of psychology on a mass scale followed the Bolshevik revolution in Russia. The new communist regime facilitated the country's modernisation, and psychology became one of its instruments.

  17. Potential change in forest types and stand heights in central Siberia in a warming climate

    NASA Astrophysics Data System (ADS)

    Tchebakova, N. M.; Parfenova, E. I.; Korets, M. A.; Conard, S. G.

    2016-03-01

    Previous regional studies in Siberia have demonstrated climate warming and associated changes in distribution of vegetation and forest types, starting at the end of the 20th century. In this study we used two regional bioclimatic envelope models to simulate potential changes in forest types distribution and developed new regression models to simulate changes in stand height in tablelands and southern mountains of central Siberia under warming 21st century climate. Stand height models were based on forest inventory data (2850 plots). The forest type and stand height maps were superimposed to identify how heights would change in different forest types in future climates. Climate projections from the general circulation model Hadley HadCM3 for emission scenarios B1 and A2 for 2080s were paired with the regional bioclimatic models. Under the harsh A2 scenario, simulated changes included: a 80%-90% decrease in forest-tundra and tundra, a 30% decrease in forest area, a ˜400% increase in forest-steppe, and a 2200% increase in steppe, forest-steppe and steppe would cover 55% of central Siberia. Under sufficiently moist conditions, the southern and middle taiga were simulated to benefit from 21st century climate warming. Habitats suitable for highly-productive forests (≥30-40 m stand height) were simulated to increase at the expense of less productive forests (10-20 m). In response to the more extreme A2 climate the area of these highly-productive forests would increase 10%-25%. Stand height increases of 10 m were simulated over 35%-50% of the current forest area in central Siberia. In the extremely warm A2 climate scenario, the tall trees (25-30 m) would occur over 8%-12% of area in all forest types except forest-tundra by the end of the century. In forest-steppe, trees of 30-40 m may cover some 15% of the area under sufficient moisture.

  18. Study of micronutrients cycling in boreal forest of Central Siberia on continuous permafrost using Copper (Cu) and zinc (Zn) isotope fractionation

    NASA Astrophysics Data System (ADS)

    Viers, Jérôme; Prokushkin, Anatoly; Pokrovsky, Oleg; Kirdyanov, Anatoly; Chabaux, François; Oliva, Priscia

    2010-05-01

    larch (Larix gmelinii (Rupr.) Rupr.) which possess about 35% of the total forest carbon stock of Russia (Kobak et al. 1996). Larch forests, composed of L. dahurica (including the sister species L. gmelinii and L. cajanderii), have the ability to grow in continuous permafrost where winter temperature customarily drops below -40 °C. Larch is the main dominant species in permafrost zone of Siberia capable to grow on soils with the active layer depth as little as 10-30 cm (Abaimov et al., 2002). Within this study we measured the concentrations of Zn, Cu and their isotopic composition in plants, soils and surficial fluids. Nutrient availability is the main factor limiting plant productivity in taiga and tundra ecosystems (Shaver and Chapin 1995) and, consequently, the understanding of these elements cycling is of high interest for the biogeochemistry of such environments. These measurements have been performed on larch needles collected as a function of time during the growing season, on the other plant species (dwarf shrubs and mosses), on soils, and on interstitial and riverwaters during both springflood and low water level period (summer and autumn). The 66Zn of soils varies between 0.02 and 0.13‰. The isotopic composition of larch needles changes as a function of location (north-facing slope, south-facing slope and riparian zone). The 66Zn of needles collected in riparian zone (66Zn = -0.15 to -0.21‰) exhibit lighter isotopic composition than those collected in both north- and south-facing slope (66Zn = 0.05-0.37‰). Dwarf shrubs exhibit higher values of 66Zn than mosses (0.23 to 0.80 and 0.03 to 0.1, respectively). We are currently acquiring new data on soil porewaters and river solutions. It is anticipated that these data will help us to trace Zn cycling in this specific ecosystem of boreal zone.

  19. From East to West: patterns of genetic diversity of populations living in four Eurasian regions.

    PubMed

    Kutuev, I; Khusainova, R; Karunas, A; Yunusbayev, B; Fedorova, S; Lebedev, Y; Hunsmann, G; Khusnutdinova, E

    2006-01-01

    We have analyzed the distribution and patterns of the genetic diversity of eight Alu loci (ACE, ApoA1, PV92, TPA25, NBC27, NBC102, NBC148, and NBC182) in 1,049 individuals representing 16 populations of the Volga-Ural region (Bashkirs, Tatars, Komis, Maris, Mordvins, and Udmurts), Central Asia (Kazakhs, Uzbeks, and Uighurs), the North Caucasus (Karachays, Kumyks, Kuban Nogays, and Karanogays), and Central South Siberia (Yakuts, Kalmyks and Evenks). Geographic divide between Europe and Asia, e.g. the Ural Mountains and the Caspian Sea, can also be considered as a genetic boundary. The data indicates that the populations of the two boundary regions between Europe and Asia, the Volga-Ural region of Russia, and populations of the North Caucasus are more similar to European than to Asian populations. Finally, Siberian and Central Asian populations are genetically closely related to each other.

  20. Variations in the intensity of the geomagnetic field in Siberia during the last 13000 years

    NASA Astrophysics Data System (ADS)

    Nachasova, I. E.; Burakov, K. S.; Pilipenko, O. V.

    2015-01-01

    The thermal magnetization of the samples from the archaeological sites in Siberia is studied. The magnetization of the collected samples was studied using the authors' modification of the Thellier method amended by the magnetic anisotropy and chemical alterations. Resulting from the study of the burned material from the Kazachka site, the time series of the geomagnetic field intensity in Siberia spanning the time interval from 10000 to 1000 B.C. is obtained. These data are unique in terms of the duration and representativeness. For the first time, the main variation in the intensity of the geomagnetic field is traced by studying the magnetization of the samples from a single archeological site. The pattern of the variations in the intensity of the geomagnetic field in Siberia from 11000 B.C. to 2000 A.D., which is reconstructed from the data of the Kazachka, Ust-Karenga, and some other sites of Cis-Baikalia, indicates that the characteristics time of the long-period oscillation in the intensity of the geomagnetic field is about 8000 years. It also suggests the existence of rapid variations superimposed on the main oscillation.

  1. Long-lived connection between southern Siberia and northern Laurentia in the Proterozoic

    NASA Astrophysics Data System (ADS)

    Ernst, R. E.; Hamilton, M. A.; Söderlund, U.; Hanes, J. A.; Gladkochub, D. P.; Okrugin, A. V.; Kolotilina, T.; Mekhonoshin, A. S.; Bleeker, W.; Lecheminant, A. N.; Buchan, K. L.; Chamberlain, K. R.; Didenko, A. N.

    2016-06-01

    Precambrian supercontinents Nuna-Columbia (1.7 to 1.3 billion years ago) and Rodinia (1.1 to 0.7 billion years ago) have been proposed. However, the arrangements of crustal blocks within these supercontinents are poorly known. Huge, dominantly basaltic magmatic outpourings and intrusions, covering up to millions of square kilometres, termed Large Igneous Provinces, typically accompany (super) continent breakup, or attempted breakup and offer an important tool for reconstructing supercontinents. Here we focus on the Large Igneous Province record for Siberia and Laurentia, whose relative position in Nuna-Columbia and Rodinia reconstructions is highly controversial. We present precise geochronology--nine U-Pb and six Ar-Ar ages--on dolerite dykes and sills, along with existing dates from the literature, that constrain the timing of emplacement of Large Igneous Province magmatism in southern Siberia and northern Laurentia between 1,900 and 720 million years ago. We identify four robust age matches between the continents 1,870, 1,750, 1,350 and 720 million years ago, as well as several additional approximate age correlations that indicate southern Siberia and northern Laurentia were probably near neighbours for this 1.2-billion-year interval. Our reconstructions provide a framework for evaluating the shared geological, tectonic and metallogenic histories of these continental blocks.

  2. Modeling of nutrient concentrations in the river Loktinka, Western Siberia

    NASA Astrophysics Data System (ADS)

    Sheludkov, Artyom; Kiesel, Jens; Veshkurtseva, Tatyana

    2014-05-01

    Nutrient pollution is the process where too many nutrients, mainly nitrogen and phosphorus, are added to bodies of water and act as fertilizer, causing excessive growth of algae and threatening the natural species assemblages. The investigated catchment area is the river Loktinka which is located in the southern part of the West Siberian Plain, in the forest-steppe vegetation region. One of the most serious contaminant of the surface waters in the region are nutrients. The main input of nutrients comes from untreated runoff from agricultural fields and pastures. To mitigate agricultural non-point source pollution, simulation tools can aid in the development of temporal and spatial management plans. This study presents a software application of a Geohydrological Analysis Model, developed by Prof. Kalinin, Tyumen State University, Russian Federation (1998) for the region. The model is based on "Runoff Forming Surfaces", which are a distinguished part of the catchment characterized by a set of natural components such as land use, soil and elevation. These areas are relatively homogeneous and lead to the same parameters for representing the hydrological cycle. The model is used to simulate the water quality situation which was sampled during spring runoff in 2013. Results of the Siberian Geohydrological Analysis Model are compared to simulations carried out with the Soil and Water Assessment Tool (SWAT).

  3. Quaternary glaciations in the Verkhoyansk Mountains, Northeast Siberia

    NASA Astrophysics Data System (ADS)

    Stauch, Georg; Lehmkuhl, Frank

    2010-07-01

    Geomorphological mapping revealed five terminal moraines in the central Verkhoyansk Mountains. The youngest terminal moraine (I) was formed at least 50 ka ago according to new IRSL (infrared optically stimulated luminescence) dates. Older terminal moraines in the western foreland of the mountains are much more extensive in size. Although the smallest of these older moraines, moraine II, has not been dated, moraine III is 80 to 90 ka, moraine IV is 100 to 120 ka, and the outermost moraine V was deposited around 135 ka. This glaciation history is comparable to that of the Barents and Kara ice sheet and partly to that of the Polar Ural Mountains regarding the timing of the glaciations. However, no glaciation occurred during the global last glacial maximum (MIS 2). Based on cirque orientation and different glacier extent on the eastern and western flanks of the Verkhoyansk Mountains, local glaciations are mainly controlled by moisture transport from the west across the Eurasian continent. Thus glaciations in the Verkhoyansk Mountains not only express local climate changes but also are strongly influenced by the extent of the Eurasian ice sheets.

  4. 7. DETAIL VIEW OF WEST SIDE OF WEST BRIDGE ABUTMENT ...

    Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey

    7. DETAIL VIEW OF WEST SIDE OF WEST BRIDGE ABUTMENT AND UNKNOWN STRUCTURE FROM BELOW, FACING NORTHWEST - West Branch Bridge, South Carolina Road S-569 spanning West Branch of Pacolet River, Pacolet, Spartanburg County, SC

  5. Historical earthquakes studies in Eastern Siberia: State-of-the-art and plans for future

    NASA Astrophysics Data System (ADS)

    Radziminovich, Ya. B.; Shchetnikov, A. A.

    2013-01-01

    Many problems in investigating historical seismicity of East Siberia remain unsolved. A list of these problems may refer particularly to the quality and reliability of data sources, completeness of parametric earthquake catalogues, and precision and transparency of estimates for the main parameters of historical earthquakes. The main purpose of this paper is to highlight the current status of the studies of historical seismicity in Eastern Siberia, as well as analysis of existing macroseismic and parametric earthquake catalogues. We also made an attempt to identify the main shortcomings of existing catalogues and to clarify the reasons for their appearance in the light of the history of seismic observations in Eastern Siberia. Contentious issues in the catalogues of earthquakes are considered by the example of three strong historical earthquakes, important for assessing seismic hazard in the region. In particular, it was found that due to technical error the parameters of large M = 7.7 earthquakes of 1742 were transferred from the regional catalogue to the worldwide database with incorrect epicenter coordinates. The way some stereotypes concerning active tectonics influences on the localization of the epicenter is shown by the example of a strong М = 6.4 earthquake of 1814. Effect of insufficient use of the primary data source on completeness of earthquake catalogues is illustrated by the example of a strong M = 7.0 event of 1859. Analysis of the state-of-the-art of historical earthquakes studies in Eastern Siberia allows us to propose the following activities in the near future: (1) database compilation including initial descriptions of macroseismic effects with reference to their place and time of occurrence; (2) parameterization of the maximum possible (magnitude-unlimited) number of historical earthquakes on the basis of all the data available; (3) compilation of an improved version of the parametric historical earthquake catalogue for East Siberia with

  6. Climatological conditions of enhanced Arctic storm activity in relation to permafrost degradation in eastern Siberia

    NASA Astrophysics Data System (ADS)

    Iijima, Y.; Nakamura, T.; PARK, H.; Fedorov, A. N.

    2015-12-01

    The last decade (2000-2010) was the warmest on record at high northern latitudes. Surface air temperature anomalies and associated sea level pressure fields in Arctic exhibited different spatial patterns at the beginning of the 21st century than they did throughout the majority of the 20th century. In eastern Siberia, the abrupt soil warming within upper permafrost layer and deepening active layer thickness has observed in response to increasing in soil moisture under wet hydro-climatic conditions during the warming period of 2000s. According to climatological analyses, the large positive anomalies of both rainfall and snow accumulation in eastern Siberia are caused by strengthened cyclonic pattern in these years which induce more water vapor advection. These anomalies are more enhanced than those before 1990s and continuously appear after 2004. Long-term simulation of permafrost temperature and active layer thickness using a sophisticated land surface model (CHANGE) was carried out. The correlations between precipitation in late summer and soil temperature showed that the most regions exhibited either negative or not significant correlations between precipitation and soil temperature during the past period (1961-1980), whereas positive correlations were observed during the recent period (1991-2009). A region of significantly positive correlation was observed along the Siberian coast and in eastern Siberia and could have corresponded with areas of increased storm activity. The soil warming is thus due to not only increasing in snow accumulation which is well-known relationship by previous studies but also increasing in rainfall in late summer which furthermore accelerates the warming due to changes in hydro-thermal properties within the active layer. The precipitation increase in the last decade led to deepening active layer accompanying with remarkable increase in soil moisture. The perennially waterlogged conditions had exacerbated the boreal forest habitat; that

  7. Radiative and cloud microphysical effects of forest fire smoke over North America and Siberia

    NASA Astrophysics Data System (ADS)

    vant-Hull, Brian

    Aerosol affects climate both through direct radiative effects and by indirect effects on cloud development. Absorbing aerosols have additional influence on the vertical temperature profile of the atmospheric column. Forest fire smoke contributes roughly half of the global absorbing aerosol, with most of the unsupervised burning occurring in the forests of Canada and Siberia. Radiative effects of smoke are studied for the case of a Canadian smoke plume that blanketed the U.S. mid-Atlantic seaboard. Optical properties derived from aircraft in situ measurements demonstrate that the smoke formed a layer with a base 2 km above the surface, and absorptive heating in this layer could have strengthened and maintained the subsidence inversion responsible for the layer structure. An optical model of the smoke formed from a blend of aircraft and AERONET measurements allows retrieval of the smoke aerosol by satellite, so that comparisons are possible to measurements made by any instrument in the region. For this case an optical model based purely on AERONET measurements provides the best satellite retrieval of optical depth, but a model based mainly on aircraft measurements agreed best with spectrum wide-forcing measurements, demonstrating the dangers of a simple optical model for all retrievals. A study done in the Amazonian burning season demonstrates that sun/observation geometry is useful to control bias from shadowed and illuminated portions of clouds. Sub-pixel mixing of cloud and aerosol also produces bias that is minimized for optically thick clouds. Since such biases can never be fully eliminated, the only valid study is a comparison of two data sets with equivalent geometry and so, presumably, equal bias. Canada and Siberia were chosen so that forested areas are compared at the same latitudes. Summertime Canadian aerosol is primarily smoke, while Europe contributes a great deal of sulfate to Siberia aerosol. The average cloud droplet size was significantly smaller in

  8. Russian-US Partnership to Study the 23-km-diameter El'gygtgyn Impact Crater, Northeast Russia

    NASA Technical Reports Server (NTRS)

    Sharpton, Virgil L.; Minyuk, Pavel S.; Brigham-Grette, Julie; Glushkova, Olga; Layer, Paul; Raikevich, Mikhail; Stone, David; Smirnov, Valdimir

    2002-01-01

    El'gygytgyn crater, located within Eastern Siberia, is a Pliocene-aged (3.6 Ma), well-preserved impact crater with a rim diameter of roughly 23 km. The target rocks are a coherent assemblage of crystalline rocks ranging from andesite to basalt. At the time of impact the region was forested and the Arctic Ocean was nearly ice-free. A 15-km lake fills the center of the feature and water depths are approximately 175 m. Evidence of shock metamorphism, -- including coesite, fused mineral glasses, and planar deformation features in quartz -- has been reported. This feature is one of the youngest and best preserved complex craters on Earth. Because of its remote Arctic setting, however, El gygytgyn crater remains poorly investigated. The objectives of this three-year project are to establish and maintain a research partnership between scientists from Russia and the United States interested in the El gygytgyn crater. The principal institutions in the U.S. will be the Geophysical Institute, University of Alaska Fairbanks and the University of Massachusetts Amherst. The principal institution in Russia will be the North East Interdisciplinary Scientific Research Institute (NEISRI), which is the Far-East Branch of the Russian Academy of Science. Three science tasks are identified for the exchange program: (1) Evaluate impactite samples collected during previous field excursions for evidence of and level of shock deformation. (2) Build a high-resolution digital elevation model for the crater and its surroundings using interferometric synthetic aperture radar techniques on JERS-1, ERS-1, ERS-2, and/or RadarSat range-doppler data. (3) Gather all existing surface data available from Russian and U.S. institutions (DEM, remote sensing image data, field-based lithological and sample maps, and existing geophysical data) and assemble into a Geographic Information Systems database.

  9. America's Historic West.

    ERIC Educational Resources Information Center

    Beardsley, Donna A.

    Settlers who pushed west over the Great Divide to the shores of the Pacific Ocean found the American West to be an expanse of extreme differences in time, topography, and ways of life. This paper elaborates on several historic sites in the American West. The purpose of the paper is to introduce a series of places to the students and teachers of…

  10. Russia in the World Water Management

    NASA Astrophysics Data System (ADS)

    Bibikova, Tatiana; Koronkevich, Nikolay; Barabanova, Elena; Zaytseva, Irina

    2014-05-01

    The comparison of Russia and the countries of the former USSR with other countries of the world on various natural and anthropogenic characteristics, including those for water sector, has become more popular in recent years. At the same time, after the break-up of the Soviet Union there were significant changes in political, social and economic spheres on the territory of new formed countries, that influenced their water resources state. Such changes as well as other environmental changes may become even more significant in the future that predetermines the necessity of the profound study of the question, as all the conditions and changes still have not been fully explored. First of all, it concerns the economic crisis including water sector in the early 90's which has not been fully overcome until present time despite economic recovery in the last years of the twentieth century. Together with the changes in climatic conditions it caused perceptible changes in the river runoff on the territory of Russia, Ukraine and Belarus, countries which have much in common. As the result, peculiar conditions for the formation and usage of water resources on the territory of the former Soviet Union have been formed. The laboratory of hydrology of the Institute of Geography of Russian Academy of Sciences analysed the situation with water resources in the countries of the former Soviet Union, and the position of Russia in the global water industry. The comparison of changes in various water consumption characteristics of the states was made; the evaluation of influence of changing economic activity on the river flow and quality of waters was analysed; comparison by the availability of water resources, anthropogenic influence, efficiency of water use, with world characteristics was made. There were 19 countries selected, including the Post-Soviet states, which occupy 54% of land and form 56% of the world population. Among the compared parameters there were: availability of water

  11. "Russia and Europe"--The Fundamental Problem of Courses in the History of Russia

    ERIC Educational Resources Information Center

    Vul'fson, B. L.

    2009-01-01

    Russia is witnessing an unprecedented explosion of interest in its history. This is entirely understandable. In the Russians' desire to understand the profound changes going on in different areas of their lives they are attempting to look at the past with new eyes, because the past has merged with the present and to a large extent determines its…

  12. News of Education in Russia: [2010--The Year of the Schoolteacher in Russia

    ERIC Educational Resources Information Center

    Russian Education and Society, 2011

    2011-01-01

    This article presents statements by President Dmitry A. Medvedev at the meeting of the Council on the Implementation of Priority National Projects and Demographic Policy on the development of education, health care, and demography, and at the ceremony on the occasion of the launching of the Year of the Schoolteacher in Russia, held at the Russian…

  13. Natural factors of technological disasters in Russia

    NASA Astrophysics Data System (ADS)

    Petrova, Elena

    2010-05-01

    More than 90 percent of disasters occurring in the Russian Federation are technological accidents and catastrophes, which account for nearly 80 percent of all the fatalities and affected people. A total of 1966 technological disasters and 152 natural ones occurred in Russia in 2008. In addition to technical, social, and economic causes of technological disasters, natural factors also play an essential role in triggering or magnifying them. A data base of technological disasters happened in Russia since 1992 has been created. More than 11,000 events are listed in the data base. New information is constantly being added to it. Occurrence time and location, a type of disaster, a number of people killed and affected, economic and ecological losses as well as a probable cause of every disaster are registered; its short description is also included. Using collected data a contribution of various natural hazards and phenomena to occurrence of technological disasters in Russia was assessed. Almost 5 percent of all technological disasters listed in the data base were triggered by natural processes. Natural factors caused the most part of accidents at power supply systems (72 percent), 11 percent of accidents at heat- and 9 percent at water supply systems; more than 10 percent of sudden collapses of buildings and mines as well as water accidents; 4.5 percent of pipeline ruptures, and 2 to 3 percent of air crashes, automobile and railway accidents. The majority of these technological disasters and accidents caused by natural factors were produced by windstorms and hurricanes (37 percent), snowfalls and snowstorms (27 percent), rainfalls (16 percent), hard frost and icy conditions of roads (12 percent), and thunderstorms (nearly 4 percent). Climate changes expected until the end of the century will have important consequences for frequency increasing and change in spatial distribution of technological disasters triggered by hydrometeorological phenomena. Increasing of

  14. Russia’s Approach to Cyber Warfare

    DTIC Science & Technology

    2016-09-01

    tools of IW can— in fact, should—be brought to bear before the onset of military operations in order to achieve the state’s objectives without having to...Shaheen Gori, “Brandishing the Cybered Bear .” 39 Russia is believed to have conducted low-level information warfare against Ukraine since at least 2009...Unwala and Shaheen Gori, “Brandishing the Cybered Bear : Information War and the Russian-Ukraine Conflict,” Military Cyber Affairs: Volume 1, Issue 1

  15. Immobilization of excess weapons plutonium in Russia

    SciTech Connect

    Borisov, G B; Jardine, L J; Mansourov, O A

    1999-01-25

    In this paper, we examine the logic and framework for the development of a capability to immobilize excess Russian weapons plutonium by the year 2004. The initial activities underway in Russia, summarized here, include engineering feasibility studies of the immobilization of plutonium-containing materials at the Krasnoyarsk and Mayak industrial sites. In addition, research and development (R&D) studies are underway at Russian institutes to develop glass and ceramic forms suitable for the immobilization of plutonium-containing materials, residues, and wastes and for their geologic disposal.

  16. Space Radar Image of Baikal Lake, Russia

    NASA Technical Reports Server (NTRS)

    1994-01-01

    This is an X-band black-and-white image of the forests east of the Baikal Forest in the Jablonowy Mountains of Russia. The image is centered at 52.5 degrees north latitude and 116 degrees east longitude near the mining town of Bukatschatscha. This image was acquired by the Spaceborne Imaging Radar-C/X-band Synthetic Aperture Radar aboard the space shuttle Endeavour on October 4, 1994, during the second flight of the spaceborne radar. This area is part of an international research project known as the Taiga Aerospace Investigation using Geographic Information System Applications.

  17. A Short Assessment of Select Remediation Issues at the Russian Research Center-Kurchatov Institute, Moscow, Russia

    SciTech Connect

    Gephart, Roy E.

    2007-06-01

    At the invitation of the National Academies, Roy Gephart traveled to Russia with an eight-member U.S. team during June, 2008 to participate in a workshop hosted by the National Academies and the Russian Academy of Sciences on radiation contamination and remediation issues in the former Soviet Union. Cleanup problems were assessed by the American participants for six Russian sites: Kurchatov Institute, Lakes 10 and 11 at Mayak, Andreev Bay, Krasnokamensk Mining Enterprise (Siberia), Almaz Mining Enterprise (North Caucasus), and one site for testing peaceful nuclear explosions. Roy lead the Russian Research Center-Kurchatov Institute review session and wrote an assessment of key cleanup issues. Kurchatov is the leading institute in the Former Soviet Union devoted to military and civilian nuclear programs. Founded in 1943 in the outskirts of Moscow, this 100 hectare site of nearly undeveloped, prime real estate is now surrounded by densely populated urban and business districts. Today there are growing concerns over the public safety and environmental security of the site resulting from increasingly obsolete nuclear facilities and a legacy of inadequate waste management practices that resulted in contaminant releases and challenging remediation problems. In addition, there is growing concern over the presence of nuclear facilities within urban areas creating potential targets for terrorist attacks.

  18. 75 FR 35086 - Magnesium From China and Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-21

    ... COMMISSION Magnesium From China and Russia AGENCY: United States International Trade Commission. ACTION... orders on magnesium from China and Russia. SUMMARY: The Commission hereby gives notice that it will...)) to determine whether revocation of the antidumping duty orders on magnesium from China and...

  19. 76 FR 11813 - Magnesium From China and Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-03-03

    ... COMMISSION Magnesium From China and Russia Determinations On the basis of the record \\1\\ developed in the... antidumping duty order on magnesium from China would be likely to lead to continuation or recurrence of... China and Russia: Investigation Nos.731-TA- 1071-1072 (Review). By order of the Commission....

  20. Engineering and Technical Education in Russia, in Numbers

    ERIC Educational Resources Information Center

    Aref'ev, A. L.; Aref'ev, M. A.

    2013-01-01

    An analysis of the main tendencies in the development of engineering and technical education in Russia during the last 100 years shows that earlier strengths have been lost, and that currently technical education in Russia is far behind modern world standards.

  1. Adolescent Drunkenness: Perception of the Problem in Russia and Germany

    ERIC Educational Resources Information Center

    Rybakova, L. N.

    2013-01-01

    Alcohol abuse in Russia among children is increasing, but programs to address this problem have not been adequately developed. The experience of other countries in equipping children to handle alcohol in a mature and safe way can be used as a basis for creating new programs in Russia.

  2. Higher Education Reform in Russia: Democratization or Bureaucratization?

    ERIC Educational Resources Information Center

    Panfilova, T. V.

    2011-01-01

    Recent reforms have increased the level of administrative oversight, and also of interference of the structure and content of university education in Russia. This is leading to a weakening of Russian higher education. In this article, the author talks about the reform of the system of higher education in Russia and the bureaucratization of higher…

  3. 77 FR 51825 - Ferrovanadium and Nitrided Vanadium From Russia

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-08-27

    ... COMMISSION Ferrovanadium and Nitrided Vanadium From Russia Determination On the basis of the record \\1... antidumping duty order on ferrovanadium and nitrided vanadium from Russia would not be likely to lead to... contained in USITC Publication 4345 (August 2012), entitled Ferrovanadium and Nitrided Vanadium from...

  4. The Universities of Russia: Areas and Prospects of Development

    ERIC Educational Resources Information Center

    Berdashkevich, A. P.

    2011-01-01

    The last two decades have seen a significant increase in university students in Russia, the growth of private and state-financed higher education, and the beginnings of a move to a national network of research institutions. The recent economic recession, however, poses a challenge to the continuance of current fee-based higher education in Russia.…

  5. 78 FR 55096 - Ferrosilicon from Russia and Venezuela

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-09

    ... COMMISSION Ferrosilicon from Russia and Venezuela Determination On the basis of the record \\1\\ developed in... Russia and Venezuela of ferrosilicon, provided for in subheadings 7202.21.10, 7202.21.50, 7202.21.75... Venezuela. Accordingly, effective July 19, 2013, the Commission instituted antidumping duty...

  6. REE, Uranium (U) and Thorium (Th) contents in Betula pendula leaf growing around Komsomolsk gold concentration plant tailing (Kemerovo region, Western Siberia, Russia)

    NASA Astrophysics Data System (ADS)

    Yusupov, D. V.; Karpenko, Yu A.

    2016-09-01

    The article deals with the research findings of peculiarities of REE, Uranium and Thorium distribution in the territory surrounding the tailing of former Komsomolsk gold concentration plant according to the data from Betula pendula leaf testing. In the leaf element composition the slight deficiency of MREE and substantial excess of HREE are presented. In the nearest impacted area around the tailing, La, Yb, U and Th content, and Th/U ratio are lower than in the distant buffer area. It is shown, that value of Th/U ratio and REE can be an indicator for geochemical transformations of technogenic landscapes in mining districts. The results of the research can be used for biomonitoring of the territory around the tailing.

  7. Model of erosion-landslide interaction in the context of the reservoir water level variations (East Siberia, Russia): Factors, environment and mechanisms

    NASA Astrophysics Data System (ADS)

    Mazaeva, Oksana; Khak, Viktoria; Kozyreva, Elena

    2013-12-01

    A comprehensive investigation of landslide-erosion interactions has been carried out in the local shore geosystem of the Bykovo site located on the left shore of the Bratsk reservoir. The landslide process develops in the Mid-Quaternary grounds (aQ of the erosion-accumulative terrace's fragment that comprises sand, sand with pebbles, sandy loams and loams. This study aims to assess the environmental factors of interacting landslide and gully erosion processes, to estimate their temporal dynamics by comparative analysis of cartographic models based on the data of repeated theodolite surveys, and to find out what level regime of the reservoir stimulates the activation of the landslide process. The authors propose two-stage descriptive model of erosion-landslide interaction and development mechanisms in the context of the reservoir water level variations in the Bratsk reservoir. The activation of landslide processes in the reservoir shores follows the periods of high water level stands. Shore slope stability is disturbed by abrasion of slope foot and inundation of the slide zone. The soils subject to landslide, erosion-landslide and erosion processes differ in their microstructure and properties. Largest erosion susceptibility is typical of soils with skeleton-aggregated microstructure, fine- and coarse-silt sandy loams and loams of high porosity, whose interstructural bonds are attributed to water-soluble salts (Sws = 0.4-0.5%) and high carbonate contents (Scr = 34-66%). High dispersion and aggregation of clay fractions is typical of the loams of the slide zone. The structure of soils subject to deformation slide is represented primarily by fine-sand particles and aggregates with smaller cohesion and strength properties.

  8. Low seismic velocity layers in the Earth's crust beneath Eastern Siberia (Russia) and Central Mongolia: receiver function data and their possible geological implication

    NASA Astrophysics Data System (ADS)

    Zorin, Yu. A.; Mordvinova, V. V.; Turutanov, E. Kh; Belichenko, B. G.; Artemyev, A. A.; Kosarev, G. L.; Gao, S. S.

    2002-12-01

    Analysis of teleseismic receiver functions at digital stations along the Bratsk-Irkutsk-Ulanbaatar-Undurshil profile suggests that low-velocity layers in the Earth's crust exist not only beneath the Baikal rift zone, where such a layer was found earlier by Deep Seismic Sounding (DSS), but also beneath Early Paleozoic Sayan-Baikal, Paleozoic Mongolian, Early Mesozoic Mongolia-Okhotsk fold areas, and beneath the Siberian platform. The reliability of detection of the low-velocity layers by receiver function analysis has been checked by numerical modeling. The results of this modeling demonstrate that receiver functions can reveal the low-velocity layers in the crust if the initial model (starting approximation) is close to real velocity distribution, and if the model medium is divided into thin layers. Averaged DSS velocity model without low-velocity layers was used as starting approximation for the inversion of observed receiver functions. The low-velocity layers are interpreted to reflect inhomogeneities of the Earth's crust formed during its evolution. Most of these layers are presumed to correspond to thick mylonite zones related to large pre-Cenozoic thrusts. The mylonites possess a great seismic anisotropy caused by the mineral orientation formed by the ductile flow in large thrust zones. They can result in low-velocity layers only for seismic waves whose rays are oriented perpendicular to the mylonite foliation, i.e., in the direction of the minimum velocity; the velocities along the foliation direction can be rather high. Therefore, the low-angle mylonite zones can be distinguished by the receiver function method, which uses the waves from the teleseismic events with nearly vertically oriented rays. The suggestion that the low-velocity layers mark low-angle thrusts is in agreement with gravity and geological data. The amount of overthrusting is estimated to be as large as several hundred kilometers. Multichannel seismic profiling can be used to verify the existence and the deep geometry of the presumed thrusts.

  9. Investigation of the tritium content in surface water, bottom sediments (zoobenthos), macrophytes, and fish in the mid-stream region of the Yenisei River (Siberia, Russia).

    PubMed

    Bondareva, Lydia; Schultz, Michael K

    2015-11-01

    The potential sources of tritium input to the Yenisei River ecosystem are derived from local operations of nuclear facilities of the Mining and Chemical Combine operated by the state-owned Rosatom corporation and from sources derived from global weapons testing fallout and nuclear power. The background tritium concentrations in zoobenthos, bottom sediments, relevant commercial fish species, and widespread endogenous aquatic plants have been obtained for the first time in this region. Our results demonstrate that the major input term of tritium to this region of the Yenisei is derived from nearby mining operations of Rosatom, with tritium concentrations in aquatic plants marginally exceeding the observed background values obtained from upstream control sample collection sites.

  10. The Ioko-Dovyren layered massif (Southern Siberia, Russia): 2. Melt vs sulphide percolation process and modeling sulphide saturation in the parental magmas and original cumulates

    NASA Astrophysics Data System (ADS)

    Ariskin, Alexey; Danyushevsky, Leonid

    2013-04-01

    An important feature of the Dovyren intrusive complex [1] is its fertility due to the presence of massive sulphide ores near the bottom of the Ioko-Dovyren massif (YDM, SW and NE margins), as well as PGE-reefs in anorthosites from the Ol-gabbronorite zone in the centre [2]. These observations argue for the importance of downward percolation of sulphides through the porous space of cumulates and probable link of this process with upward migration of intercumulus melts at a post-cumulus stage. Indirectly, this is supported by the basic conclusion on the open-system behavior of the magma chamber [1]. A key aspect of these speculations is the onset of sulphide immiscibility in YDM parental magmas and the original cumulates. To reconstruct the sulphide saturation history, we applied a newly developed sulphide version of COMAGMAT (ver. 5.2 [3]) to the rocks from the chilled zone of YDM and underlying ultramafic sills, by simulating the course of their crystallization coupled with the SCSS calculations. Modeled crystallization trajectories evidence for under-saturated nature of the most primitive parental magmas (1310oC, Fo88) from which the chilled rocks were crystallized, whereas more evolved rocks from the sills demonstrate sulphide saturation starting from their initial temperature (1190oC, Fo85), see [1]. This correlates with the absence of sulphide ores in the central parts of the pluton and their occurrence in underlying ultramafics and YDM border series containing olivine Fo~85. Another set of calculations was carried out to demonstrate the effect of bulk Ni contents in Ol cumulate piles on the evolution of SCSS during their post-cumulus crystallization [3]. To achieve the goal, two calculations by the COMAGMAT-5.2 model were carried out. The first one involved modelling equilibrium crystallization for an initial mixture of Ol (Fo88) and intercumulus melt (~1320oC), with the starting composition corresponding to that of a bottom Pl-dunite (2315 ppm NiO, 0.030 wt% S). The second modelling was performed for the initial trapped melt only (517 ppm NiO, 0.067 wt% S), estimated for the primitive Ol orthocumulate. The major difference between these calculations is the onset of modelled sulphide saturation. In the case of "Ol cumulus pile", the sulphide liquid appears at 1209oC, slightly earlier than plagioclase and pyroxenes start to crystallize. For the "Ol-free magma", sulphides appear at much lower temperature (~1173oC) where the Ol-Pl-Opx-Cpx assemblage is stable. This indicates that the presence of a large amount of Ni-enriched Ol crystals should be considered as a "Ni-buffer" which does not allow for Ni content in the trapped melt to decrease significantly, giving rise to earlier precipitation of sulphides as it follows from the pronounced effect of Ni on sulphide solubility discussed in [3]. This research was supported by AngloAmerican, BHP Billiton and Votorantim Metais through AMIRA project P962, by the Australian Research Council funding to the CODES, and the Russian Foundation for Basic Research (projects 08-05-00194a, 11-05-00268a). [1] Ariskin et al. (2013) This volume [2] Kislov E.V. (1998) The Yoko-Dovyren Layered Massif, Ulan-Ude, 264 p. (in Russian) [3] Ariskin et al. (2012). Abs. 12th Intern. Ni-Cu-(PGE) symp. (China)

  11. The Ioko-Dovyren layered massif (Southern Siberia, Russia): 1. Internal structure, magma compositions, and fingerprints of open magma chamber behavior

    NASA Astrophysics Data System (ADS)

    Ariskin, Alexey; Danyushevsky, Leonid; Nikolaev, Georgy

    2013-04-01

    The Yoko-Dovyren massif (YDM) is located ~60 km to NE of the Baikal Lake, being morphologically a ridge of 26 km long and up to 2114 m high. Geologically, the pluton is a lens-shaped body (up to 3.5 thick) which together with associated peridotite sills, diabase dikes, and overlying volcanics represents a volcanic-plutonic association (728+/-2.4 Ma [1]), formed in the Late Riphean within a huge rifting system (the Olokit trough) at the southern margin of the Siberian craton. A unique feature of the regional geology is the concordance of the igneous rocks with the enclosing carbonate-terrigenous sediments along its strike and dip, which is nearly vertical due to post-intrusive folding. This allows one to sample the intrusive complex across the strike, from the lower to upper contacts. The modal layering of YDM includes a bottom unit of plagioclase lherzolites (100-150 m) followed by a succession of cumulates including: Pl-bearing and adcumulate dunites (Ol+Chr, 800-900 m), troctolite (Ol+Pl+Chr, ~700 m), Ol gabbro (Pl+Ol+Cpx, Pig-gabbro and quartz gabbronorites (Pl+Cpx±Opx±Pig). Despite its Precambrian age, YDM was not metamorphosed significantly, so that most of intrusive rocks are very fresh, preserving both their igneous textures and original mineralogy. Parental magma compositions have been evaluated based on studies of the chilled zones and underlying ultramafic sills. The most primitive rocks of YDM have been discovered at the lower contact composed of chilled diabases and picritic rocks containing variable amounts of Ol, and ophitic textures of their groundmass. The FeO-MgO trend displayed by these high porosity cumulates suggests them to contain originally olivine ~Fo88. The COMAGMAT model calculations indicate the initial temperature of the heterogeneous magma is to be of 1310oC, with the magmatic melt containing ~12% MgO [2]. Using this composition as starting one, we simulated the parent crystallization sequence which corresponds to that observed in the YDM cumulates. Estimates for Ol-gabbronorites and Pl-dunites from ultramafic sills result in more evolved magma containing Ol~Fo85 at T~1190oC. Both geochemical and cumulate structure of YDM is indicative of a significant amount of mafic melts to be extracted from the original cumulate piles, followed by their expulsion from the magma staging chamber. Fingerprints of such an open-system behavior are recorded in (1) strong depletion in incompatible elements of the bulk YDM composition with respect to parental magmas, (2) a complimentary "over-enrichment" with Ol cumulates and sulfides, (3) insignificant variations of Ol composition throughout the Layered Series, and (4) the absence of the Upper Border Series as a marginal compositional reversal. This research was supported by AngloAmerican, BHP Billiton and Votorantim Metais through AMIRA project P962, by the Australian Research Council funding to the CODES, and the Russian Foundation for Basic Research (projects 08-05-00194a, 11-05-00268a). [1] Ariskin et al. (2013) Geochem. Intern. [2] Ariskin et al. (2012)Abs. 12th Intern. Ni-Cu-(PGE) symp. (China)

  12. Role of polymorphic variants of MTR gene A2756G and SHMT1 gene C1420T in the development of prostatic cancer in residents of the Western Siberian Region of Russia.

    PubMed

    Weiner, A S; Oskina, N A; Lacarev, A F; Petrova, V D; Ganov, D I; Boyarskih, U A; Tonacheva, O G; Voronina, E N; Filipenko, M L

    2012-02-01

    Allelic variants of folate cycle enzyme genes can contribute to predisposition to cancer. The impact of polymorphic loci A2756G of MTR gene and of C1420T of SHMT1 gene for the risk of prostatic cancer was studied in residents of West Siberia. The frequency of alleles of these loci in patients (N=371) and controls (N=285) was determined and the data were statistically processed. No statistically significant association with prostatic cancer was detected for any of the studied loci.

  13. Space Surveillance: United States, Russia, and China

    NASA Astrophysics Data System (ADS)

    Seidelmann, P. K.

    2012-06-01

    With the launch of Sputnik, the United States and Russia began the process of tracking artificial satellites. This led to developments for observations, orbit determination, and catalog maintenance. The two countries followed somewhat different approaches to the same problem based on the available hardware and theoretical developments. As more sophisticated hardware and theories have been developed, progress has been made. However, new problems have developed because of debris, collision possibilities, and reentering objects. In addition, the range of spacecraft has increased to include geosynchronous orbits. In more recent times the European Space Agency (ESA) and China have become involved in various aspects of Space Surveillance. In 1994, the first meeting between United States and Russian experts in the field of space surveillance was held. Since then, seven more US Russia Space Surveillance Workshops have been held, with the addition of participants from ESA. Terry Alfriend has been the US Technical Chairman for many of these workshops. In 2009 a US China Space Surveillance Technical Interchange was held in Shanghai, China, and Terry was the US Technical Chairman.

  14. New archeomagnetic intensity data from Western Russia

    NASA Astrophysics Data System (ADS)

    Salnaya, Natasha; Gallet, Yves; Akimova, Stanislava; Antipov, Ilya; Glazunova, Olga

    2015-04-01

    We recently started a new archeomagnetism research program for Western Russia. The main objective of this project is to recover the geomagnetic field intensity variations in Western Russia over the past two millennia, in order to compare these variations with those already known from Western and Eastern Europe. We sampled several ensembles of baked brick fragments precisely dated by historical constraints between the XIIth and XIVth centuries AD from the archeological site of Novgorod, south of St Petersburg, and between the XVIIth and XVIIIth centuries AD from the Monastery of New Jerusalem located close to Moscow. Most fragments, with a magnetic mineralogy dominated by magnetite, are suitable for archeointensity experiments. For some fragments from Novgorod, the magnetization is carried by a mixture of magnetite and another mineral of high coercivity and low unblocking temperature. The unblocking temperatures are close to 200°C. This mineral, most probably a form of hematite with Al substitutions, is therefore similar to that previously reported from archeological fired-clay artifacts originating from Europe and South America. Archeointensity experiments were conducted using the experimental protocol developed for the Triaxe magnetometer. We will present our first archeointensity results and a preliminary comparison with available European results, mostly from France and Bulgaria.

  15. Changes in Russia's Military and Nuclear Doctrine

    SciTech Connect

    Wolkov, Benjamin M.; Balatsky, Galya I.

    2012-07-26

    In 1993, the Russian Federation set out a new military doctrine that would determine the direction of its armed forces until President Putin set out the next doctrine in 2000. The Russian Federation creating the doctrine was new; the USSR had recently collapsed, Gorbachev - the creator of the predecessor to this doctrine in 1987 - was out of office, and the new Russian military had only been formed in May, 1992.1 The analysis of the 1993 doctrine is as follows: a definition of how doctrine is defined; a short history of Russian military doctrine leading up to the 1993 doctrine (officially the Basic Provisions of the Military Doctrine of the Russian Federation); and finally, what the doctrine established. An overview of the 1993 doctrine is: (1) Russia's 1993 doctrine was a return to older, more aggressive doctrine as a result of stability concerns surrounding the recent collapse of the USSR; (2) Russia turned from Gorbachev's 'defensive defense' in the 1987 doctrine to aggressive defense with the option of preempting or striking back against an aggressor; (3) Russia was deeply concerned about how nationalism would affect the former Soviet Republics, particularly in respect to the ethnic Russians still living abroad; and (4) Nuclear doctrine pledged to not be the first to use nuclear weapons but provided for the potential for escalation from a conventional to a nuclear war. The 2000 doctrine (officially the Russian Federation Military Doctrine) was created in a more stable world than the 1993 doctrine was. The Russian Federation had survived independence and the 'threat of direct military aggression against the Russian Federation and its allies' had diminished. It had secured all of the nuclear weapons from its neighbors Ukraine, Belarus, and Kazakhstan, and had elected a new president, Vladimir Putin, to replace Boris Yeltsin. Yet, even as the doctrine took more defensive tones than the 1993 doctrine, it expanded its nuclear options. Below are a new definition of

  16. Family and family therapy in Russia.

    PubMed

    Bebtschuk, Marina; Smirnova, Daria; Khayretdinov, Oleg

    2012-04-01

    This article represents the information about family and family therapy in the context of culture, traditions and contemporary changes of social situations in Russia. The legislation of family rights are mentioned within items about marriage and family in the Constitution, Civil Code and Family Code of the Russian Federation which has changed during recent years. The definition of family and description of family structure are given through the prism of the current demographic situation, dynamics of statistics of marriage and divorce rates, mental disorders, disabilities and such phenomena as social abandonment. The actual curriculum, teaching of family therapy and its disadvantages, system of continuous education, supervision and initiatives of the Institute of Integrative Family Therapy in improvement of preparing of specialists who can provide qualified psychosocial assistance for the family according to the actual needs of society are noted. The directions of state and private practice of family counselling and therapy both for psychiatric patients and medical patients, for adults and children in a family systemic approach are highlighted with an indication of the spectrum of techniques and methods used by Russian professionals. The main obstacles and perspectives of development of family therapy in Russia are summarized.

  17. Recent ecohydrological change in relation to permafrost degradation in eastern Siberia

    NASA Astrophysics Data System (ADS)

    Iijima, Y.; Fedorov, A. N.; Maximov, T. C.

    2010-12-01

    Recently, our continuous observations during the last decade revealed considerable evidence of abrupt land surface moistening and synchronized rapid soil warming within active layer and upper part of permafrost in the central Lena River basin in eastern Siberia. The present study focuses firstly on the linkage between atmospheric and land surface variations in eastern Siberia in terms of the hydrothermal variations within the surface layer of the permafrost and influence of storm track activity in Arctic during pre-winter and snow start season and moreover on the linkage between the permafrost degradation and ecohydrological change in this region. We utilized soil temperature, moisture and active layer thickness data from the observational network in the left and right banks of the Lena River in the Yakutsk area. Daily data of precipitation and snow depth and reanalysis dataset were used to analyze the large-scale atmospheric fields and determine storm-track activity. The peculiar feature of the warming is that the soil moisture correspondingly increases within the active layer observed at many sites in the Yakutsk area. This hydro-thermal change is primarily due to wetting climate conditions rather than atmospheric warming with abnormally large amounts of winter snow accumulation and summer precipitation in the central and southern part of the Lena River basin. The wetting conditions in eastern Siberia are likely due to enhancement of cyclonic anomaly over the Arctic Ocean and eastward propagation of storm activities in summer and early winter. Water vapor flux from Pacific side (Okhotsk sea) was enhanced in conjunction with the manifested precipitation over the eastern Siberia. As results, consecutive positive anomalies of winter snow accumulation and next summer precipitation which had seldom occurred in the second half of the last century in eastern Siberia effectively humidified land surface on the permafrost region after 2005 resulting abrupt soil warming in

  18. Factors promoting larch dominance in Eastern Siberia: fire versus growth performance and implications for carbon dynamics

    NASA Astrophysics Data System (ADS)

    Schulze, E.-D.; Wirth, C.; Mollicone, D.; von Lüpke, N.; Ziegler, W.; Achard, F.; Mund, M.; Prokushkin, A.; Scherbina, S.

    2012-01-01

    The relative roles of fire and climate in determining canopy species composition and aboveground carbon stocks were investigated. Measurements were made along a transect extending from the dark taiga zone of Central Siberia, where Picea and Abies dominate the canopy, into the Larix zone of Eastern Siberia. We test the hypotheses that the change in canopy species composition is based (1) on climate-driven performance only, (2) on fire only, or (3) on fire-performance interactions. We show that the evergreen conifers Picea obovata and Abies sibirica are the natural late-successional species both in Central and Eastern Siberia, provided there has been no fire for an extended period of time. There are no changes in the climate-driven performance of the observed species. Fire appears to be the main factor explaining the dominance of Larix. Of lesser influence were longitude, hydrology and active-layer thickness. Stand-replacing fires decreased from 300 to 50 yr between the Yenisei Ridge and the upper Tunguska. Repeated non-stand-replacing surface fires eliminated the regeneration of Abies and Picea. With every 100 yr since the last fire, the percentage of Larix decreased by 20 %. Biomass of stems of single trees did not show signs of age-related decline. Relative diameter increment was 0.41 ± 0.20 % at breast height and stem volume increased linearly over time with a rate of about 0.36 t C ha-1 yr-1 independent of age class and species. Stand volumes reached about 130 t C ha-1 (equivalent to about 520 m3 ha-1). Individual trees of Larix were older than 600 yr. The maximum age and biomass seemed to be limited by fungal rot of heart wood. 60 % of old Larix and Picea and 30 % of Pinus sibirica trees were affected by stem rot. Implications for the future role of fire and of plant diseases are discussed.

  19. New Palaeomagnetic Data from the Kitoy River, South Siberia and applications to the Neoproterozoic palaeogeography

    NASA Astrophysics Data System (ADS)

    Pisarevsky, Sergei; Gladkochub, Dmitry; Konstantinov, Konstantine; Mazukabzov, Anatoly; Stanevich, Arkady; Tait, Jennifer; Donskaya, Tatiana

    2010-05-01

    Revealing of past continental configurations has advanced by extending our knowledge backwards through time. Although the evolution of Pangaea and Gondwanaland is relatively well established, the exact configuration of the earlier supercontinent Rodinia and its predecessors are still widely debated due to our poor knowledge of the palaeogeography in the Neoproterozoic. The Neoproterozoic - Early Cambrian interval is marked by at least two major tectonic reconfigurations of the Earth: the final breakup of the remnants of the Rodinia supercontinent and the assembly of Gondwanaland. This was also one of the greatest orogenic epochs (Baikalian - Pan-African - Cadomian - Timanian orogenies). Many high-quality palaeomagnetic poles were used to construct Phanerozoic APWPs for the majority of continents, and there is general agreement about Phanerozoic tectonic history. In contrast, Neoproterozoic palaeomagnetic data are scarce and controversial, and it is impossible at this stage to apply the traditional APWP method. For example, no highly reliable and well dated Siberian palaeomagnetic poles with ages between ~600 and ~900 Ma have been published so far. Here we present new palaeomagnetic data from the ~750 Ma mafic dyke swarm of the Kitoy River, southern Siberia. Dykes are unaltered, 0.3 to 3 m thick, shallow dipping with N to NNW trends. We collected 172 oriented cores of 14 dykes and host Archaean granites and gneisses for the baked contact tests. Thermal and AF demagnetisations revealed a stable bipolar remanence. The corresponding preliminary palaeomagnetic pole generally supports previously published palaeogeographic reconstructions with southern Siberia facing northern Laurentia with a significant gap in between. This gap is believed to be filled by some other continent or microcontinents. This Siberia-Laurentia configuration apparently did not change since ~1500 Ma until after 750 Ma.

  20. Fire Regime and Land Abandonment in European Russia: Case Study of Smolensk Oblast

    NASA Astrophysics Data System (ADS)

    Krylov, A.; McCarty, J. L.; Potapov, P.; Turubanova, S.; Prishchepov, A. V.; Manisha, A.; Romanenkov, V.; Rukhovitch, D.; Koroleva, P.; Hansen, M.

    2014-12-01

    Fires in anthropogenically-dominated landscapes are generally attributed to ecosystem management, agriculture, and policy drivers. In European Russia, fire mainly occurring on agricultural lands, wetlands, and abandoned lands. In the agricultural practice in Russia prescribed fires are believed to increase pasture and hay productivity, suppress trees and shrub expansion, and reduce fire hazards, with fire frequency fire dependent on land use and agricultural practices. The large-scale socio-economic transition since the fall of the Soviet Union has led to changes in land use and land management, including land abandonment and changing agricultural practices. In June 2014, an extensive field campaign was completed in the Smolensk Oblast, located approximately two hundred kilometers west of Moscow on the border with Belarus. Our field sampling was based on circa 1985 Landsat-based forest cover map (Potapov et al., 2014). Points were randomly selected from the non-forested class of the 1985 classification, prior to the collapse of the Soviet Union. Of total field collects, 55% points were sampled on land in either early or late stage of abandonment, 15% from actively cropped fields, and 30% from hay or pasture. Fire frequency was calculated for the 108 field points using 1 km Moderate Resolution Imaging Spectroradiometer (MODIS) active fire data for years 2000-2014. Also we calculated percent of points burned in spring 2014 using 30 m Landsat 8 Operational Land Imager (OLI) data to derive burn scars. Actively cropped fields had lowest burn frequency while abandoned lands - early and late stage abandonment - had highest frequency. Fire frequency was significantly higher on wet soils than dry soils, with no relationship between fire frequency and tree canopy cover. We hypothesize, higher fire frequency on abandoned lands was likely due to greater fuel loads and because of traditional belief in rural Russia that fire is efficient way to suppress tree and shrub expansion.

  1. An arctic fox rabies virus strain as the cause of human rabies in Russian Siberia.

    PubMed

    Kuzmin, I V

    1999-01-01

    A case of human rabies in the arctic zone of Siberia is described. The victim was bitten by a wolf, but characterization of the isolate by monoclonal antibodies showed that it was an arctic fox virus strain. This discovery reaffirmed the value of strain typing rabies virus isolates in regions where this has not been done already: such characterization pertains to the identification of the reservoir host, to the natural history of the virus in the reservoir, and to future surveillance, post-exposure treatment, and public education in the region.

  2. Ethnomyocological data from Siberia and North-East Asia on the effect of Amanita muscaria.

    PubMed

    Saar, M

    1991-02-01

    The paper includes literary data on the use of Amanita muscaria in Siberia and North-East Asia as well as information collected from ethnographers investigating these areas during the past decades. A survey is given on the cases and rules of Amanita muscaria consumption and the ways of its administration. The peoples having the tradition of Amanita muscaria consumption were aware of its different psychotrophic qualities and were able to use for several purposes. The fungus has been used by them as a psychostimulant having a simultaneous effect on several psychic functions.

  3. [Prospects for the development of health resort and recreational resources in southern Siberia].

    PubMed

    Dzhabarova, N K; Iakovenko, E S; Levitskiĭ, E F; Lukovskaia, I A

    2010-01-01

    Long-term monitoring natural health remedial factors of southern Siberia provided materials for the comparative evaluation of bioclimatic characteristics of sanatorium-and-spa facilities in major health and recreational areas of this region. The most promising localities for climatic balneotherapy, tourist and recreational activities have been identified at the territory of the Altai-Sayan mountain system. The database of sanatorium-and-spa facilities, health and recreational sites located in this region is presented. The rational exploitation of mountainous landscapes including strict constraints on nature use activities is recommended as a basis for the further development of recreational industry.

  4. Paleomagnetism of Angara-Vitim batholith: relative position of Siberia and Europe in Permian

    NASA Astrophysics Data System (ADS)

    Fedyukin, I.; Shatsillo, A.

    2012-12-01

    In the Late Paleozoic paleomagnetic data of the Siberian platform is a white spot on the general background of the received data. These paleomagnetic data are needed to develop APWP of the Siberian platform, paleogeography and assessment of its place in the global paleoreconstructions for the Late Paleozoic. In particular, to determine the relative motions of Siberia and the Europe during the amalgamation of the supercontinent Pangea. The purpose of this paper is to obtain reliable data for the Late Paleozoic of the Siberian platform. The main object of the present study is the Late Paleozoic Angara-Vitim batholith (AVB). Age AVB is well defined (U-Pb 294 +/- 6 Ma). The study area is located in the northern part of the Baikal-Patom folded region, namely Patom passive margin. Where is superimposed tectonic processes absent. During the detailed thermo-cleaning revealed the presence of high-temperature characteristic components of magnetization. This component is present in the samples as the most stable. The main mineral - a carrier of magnetization is magnetite, hematite content with a subordinate, and maghemite (magnetic iron oxide modification of γ-Fe2O3, the transition from magnetite to hematite). The presence of hematite and maghemite in granites associated with increased activity of the volatile oxygen in the formation of these rocks. The direction of the remanent magnetization vector shows high stability in the entire range of demagnetization (from 120 C to 640 C) and is characterized by northern declinations and steep negative inclinations. In favor of a primary thermoremanent nature magnetization AVB granitoids may indicate two things: 1) the difference between the calculated directions from known areas of Mesozoic-Cenozoic directions Siberia, 2) positive "test firing" (regional remagnetization of older rocks Patom passive margin). The parameters of the pole: Plat=36.9, Plong=124.4, A95=6.4. The obtained data say that in the early Permian time, the Siberian

  5. Modelling Climate/Global Change and Assessing Environmental Risks for Siberia

    NASA Astrophysics Data System (ADS)

    Lykosov, V. N.; Kabanov, M. V.; Heimann, M.; Gordov, E. P.

    2009-04-01

    The state-of-the-art climate models are based on a combined atmosphere-ocean general circulation model. A central direction of their development is associated with an increasingly accurate description of all physical processes participating in climate formation. In modeling global climate, it is necessary to reconstruct seasonal and monthly mean values, seasonal variability (monsoon cycle, parameters of storm-tracks, etc.), climatic variability (its dominating modes, such as El Niño or Arctic Oscillation), etc. At the same time, it is quite urgent now to use modern mathematical models in studying regional climate and ecological peculiarities, in particular, that of Northern Eurasia. It is related with the fact that, according to modern ideas, natural environment in mid- and high latitudes of the Northern hemisphere is most sensitive to the observed global climate changes. One should consider such tasks of modeling regional climate as detailed reconstruction of its characteristics, investigation of the peculiarities of hydrological cycle, estimation of the possibility of extreme phenomena to occur, and investigation of the consequences of the regional climate changes for the environment and socio-economic relations as its basic tasks. Changes in nature and climate in Siberia are of special interest in view of the global change in the Earth system. The vast continental territory of Siberia is undoubtedly a ponderable natural territorial region of Eurasian continent, which is characterized by the various combinations of climate-forming factors. Forests, water, and wetland areas are situated on a significant part of Siberia. They play planetary important regulating role due to the processes of emission and accumulation of the main greenhouse gases (carbon dioxide, methane, etc.). Evidence of the enhanced rates of the warming observed in the region and the consequences of such warming for natural environment are undoubtedly important reason for integrated regional

  6. Biomedical journals and databases in Russia and Russian language in the former Soviet Union and beyond

    PubMed Central

    Vlassov, Vasiliy V; Danishevskiy, Kirill D

    2008-01-01

    In the 20th century, Russian biomedical science experienced a decline from the blossom of the early years to a drastic state. Through the first decades of the USSR, it was transformed to suit the ideological requirements of a totalitarian state and biased directives of communist leaders. Later, depressing economic conditions and isolation from the international research community further impeded its development. Contemporary Russia has inherited a system of medical education quite different from the west as well as counterproductive regulations for the allocation of research funding. The methodology of medical and epidemiological research in Russia is largely outdated. Epidemiology continues to focus on infectious disease and results of the best studies tend to be published in international periodicals. MEDLINE continues to be the best database to search for Russian biomedical publications, despite only a small proportion being indexed. The database of the Moscow Central Medical Library is the largest national database of medical periodicals, but does not provide abstracts and full subject heading codes, and it does not cover even the entire collection of the Library. New databases and catalogs (e.g. Panteleimon) that have appeared recently are incomplete and do not enable effective searching. PMID:18826569

  7. On the discovery of a cave lion from the Malyi Anyui River (Chukotka, Russia)

    NASA Astrophysics Data System (ADS)

    Kirillova, I. V.; Tiunov, A. V.; Levchenko, V. A.; Chernova, O. F.; Yudin, V. G.; Bertuch, F.; Shidlovskiy, F. K.

    2015-06-01

    An incomplete postcranial skeleton (67 elements) of a cave lion, a lower jaw and a bundle of fine yellowish hair were found by a local resident in 2008 and 2009 washed out from the perennially frozen Pleistocene sediments in the lower reaches of the Malyi Anyui River (western Chukotka). This is the first skeleton of a cave lion (Panthera spelaea Goldfuss) to be found in Russia. The bone sizes are similar to finds of cave lion bones known from N-E Russia, but larger than East Beringian and smaller than West European ones. The remains have been studied using a variety of methods, including morphology, morphometry, SEM-examination, AMS-dating, and isotopic study, which included examination of over 100 samples of various members of the mammoth faunal assemblage (mammoth, wooly rhinoceros, bison, horse, bear, etc.). The results showed that the northeastern Asian cave lion hunted mainly bison and horses, but not reindeer, unlike its Western Europe counterpart. Bone and claw sheath dating showed an unexpectedly old geochronological age of over 61,000 years (OZQ290, OZQ291), while the hair was dated 28,690 ± 130 (OZQ292), which makes its affinity with the same individual as the skeleton questionable. Further studies to investigate possible unremoved contamination and obtain more reliable date are planned.

  8. Excess Weapons Plutonium Immobilization in Russia

    SciTech Connect

    Jardine, L.; Borisov, G.B.

    2000-04-15

    The joint goal of the Russian work is to establish a full-scale plutonium immobilization facility at a Russian industrial site by 2005. To achieve this requires that the necessary engineering and technical basis be developed in these Russian projects and the needed Russian approvals be obtained to conduct industrial-scale immobilization of plutonium-containing materials at a Russian industrial site by the 2005 date. This meeting and future work will provide the basis for joint decisions. Supporting R&D projects are being carried out at Russian Institutes that directly support the technical needs of Russian industrial sites to immobilize plutonium-containing materials. Special R&D on plutonium materials is also being carried out to support excess weapons disposition in Russia and the US, including nonproliferation studies of plutonium recovery from immobilization forms and accelerated radiation damage studies of the US-specified plutonium ceramic for immobilizing plutonium. This intriguing and extraordinary cooperation on certain aspects of the weapons plutonium problem is now progressing well and much work with plutonium has been completed in the past two years. Because much excellent and unique scientific and engineering technical work has now been completed in Russia in many aspects of plutonium immobilization, this meeting in St. Petersburg was both timely and necessary to summarize, review, and discuss these efforts among those who performed the actual work. The results of this meeting will help the US and Russia jointly define the future direction of the Russian plutonium immobilization program, and make it an even stronger and more integrated Russian program. The two objectives for the meeting were to: (1) Bring together the Russian organizations, experts, and managers performing the work into one place for four days to review and discuss their work with each other; and (2) Publish a meeting summary and a proceedings to compile reports of all the excellent

  9. Mouth of the Ob River, Russia

    NASA Technical Reports Server (NTRS)

    2002-01-01

    These images from the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Terra satellite shows the cause and effect of the large-scale seasonal flooding experienced on rivers throughout Siberia each year. Because many Siberian rivers flow from south to north, they flood regularly in the spring as meltwater from southern latitudes backs up against the still-frozen northern reaches of the rivers.These images show the Ob' River on the western edge of the Central Siberian Plateau. The images from June 20, 2002, show the mouth of the Ob' River (large river at left) where it empties into Kara Sea. In the false-color image, Vegetation appears in bright green, water appears dark blue or black, and ice appears bright blue. The ice is still choking the river's outlet to the sea.The effect of this ice block on the more southern stretches of the river can be seen in the images captured on June 17. In the false-color image, water is black, vegetation is in shades of gold and green, and clouds are pale orange. In the northernmost portion of the Ob' visible in this image (the Ob' runs southeast to northwest in the image), what is normally a fine mesh of braided streams and branches of the river channel has become almost a lake in places. The flood waters have engorged the river to 52 kilometers (32 miles) wide in places. Rivers can back up for hundreds of miles, and cause devastating flooding for towns and villages along the banks. Often, explosives are dropped into ice jams in an effort to free the river and give the flood waters a chance to escape. The spring and summer floods of 2002 have proven to be quite severe and perhaps as many as 100,000 people have been affected across the country. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

  10. Fatal attraction: Explaining Russia's sensitive nuclear transfers to Iran

    NASA Astrophysics Data System (ADS)

    Kuchinsky, Leah R.

    This paper explores Russia's sensitive nuclear assistance to Iran in an effort to determine why a supplier state might proliferate against its own apparent security interests. The goal is to help readers understand the supply-side dynamics of nuclear proliferation. Through careful reconstruction of the historical narrative, using open source data, this study tests the plausibility of a "fatalistic calculus" explanation, identified by Stephen Sestanovich as a possible driver for Russia's behavior. According to the hypothesis, Russia has cooperated with Iran as a way both to stay in the good graces of a neighbor that is suspected of developing nuclear weapons and to win short-term influence and profits. The paper also examines the role of other factors advanced in the existing supply-side literature, such as economic motives identified by physicist and nonproliferation scholar David Albright. The findings show that bureaucratic, economic and fatalistic factors have each played a role in motivating Russia's cooperation with Iran, with their relative importance shifting over time. Fatalism begets a strategy of Russian "minimaxing," in the lexicon of Russia scholar Robert Freedman, wherein Russia attempts to minimize damage to its relationship with the U.S. while maximizing influence in Iran via nuclear cooperation. Fatalism, as actualized by minimaxing, best explains Russia's behavior after former Russian president Vladmir Putin came to power, when the bureaucratic and economic arguments become less cogent.

  11. Petroleum and geothermal production technology in Russia: Summary of information obtained during informational meetings with several Russian Institutes

    SciTech Connect

    Schafer, D.M.; Glowka, D.A.; Teufel, L.W.

    1995-04-01

    Russian scientists and engineers have drilled the deepest holes in the world. It is recognized that this experience has given them an expertise in drilling superdeep holes, as well as other aspects of drilling, completions, and geophysics. More and more US oil and gas companies are vigorously expanding their exploration and development into Russia. It is important for them to identify and use Russian technology in drilling, completion, logging, and reservoir characterization to the extent possible, in order to both reduce drilling costs and help support the Russian economy. While these US companies are interested in becoming involved in and/or sponsoring research in Russia, they have been unsure as to which scientists and institutes are working on problems of interest. It was also important to determine in which areas Russian technology is farther advanced than in the West. Such technology could then be commercialized as part of the Industrial Partnering Program. In order to develop a clear understanding of these issues, two Sandia engineers with drilling and completions expertise and a geophysicist with expertise in reservoir analysis traveled to Russia to meet with Russian scientists and engineers to discuss their technologies and areas of interest. This report contains a summary of the information obtained during the visit.

  12. Superconductivity in Russia: Update and prospects

    NASA Technical Reports Server (NTRS)

    Ozhogin, V.

    1995-01-01

    The research projects and new technological developments that have occured in Russia are highlighted in this document. Some of the research discussed includes: x-ray structure analysis of YBCO superconducting single crystals and accompanying phase transformations; the role of electron-electron interaction in High Temperature Superconductors (HTSC); the formation of Cooper pairs in crystals; the synthesis and research on a new family of superconductors based on complex copper and mercury oxides (HgBa2CuO4 + alpha and HgBa2CaCu2O6 + alpha); methods for the extraction of higher (up to C200) fullerenes and metalfullerenides has been developed; and process of production of Josephson junctions and development of SQUID's.

  13. Bios-3 project in Krasnoyarsk, Russia

    PubMed

    Wheeler, R M

    1994-01-01

    The article in this issue by Gitelson and Okladnikov provides a valuable summary of some of the work conducted at the Bios-3 project in Krasnoyarsk, Russia. As the title suggests, the focus is on humans and their role in a CELSS biosphere. I am aware of several translated reports and some recent articles by Dr. Gitelson and colleagues in which the Bios project is described, but this paper provides some information that I have not seen previously in an english article. Although the discussion is focused on bioregeneration, the authors state that complementary physicochemical technologies and some stowage may be needed in a CELSS. For example, animal protein foods were taken into the Bios-3 chamber, since, as the authors state, "products of animal origin would make the system considerably more complicated and energy inefficient."

  14. Stationary plasma thruster evaluation in Russia

    NASA Technical Reports Server (NTRS)

    Brophy, John R.

    1992-01-01

    A team of electric propulsion specialists from U.S. government laboratories experimentally evaluated the performance of a 1.35-kW Stationary Plasma Thruster (SPT) at the Scientific Research Institute of Thermal Processes in Moscow and at 'Fakel' Enterprise in Kaliningrad, Russia. The evaluation was performed using a combination of U.S. and Russian instrumentation and indicated that the actual performance of the thruster appears to be close to the claimed performance. The claimed performance was a specific impulse of 16,000 m/s, an overall efficiency of 50 percent, and an input power of 1.35 kW, and is superior to the performance of western electric thrusters at this specific impulse. The unique performance capabilities of the stationary plasma thruster, along with claims that more than fifty of the 660-W thrusters have been flown in space on Russian spacecraft, attracted the interest of western spacecraft propulsion specialists. A two-phase program was initiated to evaluate the stationary plasma thruster performance and technology. The first phase of this program, to experimentally evaluate the performance of the thruster with U.S. instrumentation in Russia, is described in this report. The second phase objective is to determine the suitability of the stationary plasma thruster technology for use on western spacecraft. This will be accomplished by bringing stationary plasma thrusters to the U.S. for quantification of thruster erosion rates, measurements of the performance variation as a function of long-duration operation, quantification of the exhaust beam divergence angle, and determination of the non-propellant efflux from the thruster. These issues require quantification in order to maximize the probability for user application of the SPT technology and significantly increase the propulsion capabilities of U.S. spacecraft.

  15. New System of Food Control in Russia

    NASA Astrophysics Data System (ADS)

    Ermakova, Irina V.

    Food safety is quite important for human health in all countries. Humanity has the uniform space and must take care about all parts of it. Pollution of one region leads to the same state of others regions through water, land, air, living organisms. The poor-quality or poisoned food products can pollute the territory and influence negatively on the environment. The food security is important, especially, in connection with the possibility of terrorist attacks. The Federal Service of control in sphere of protection of the rights of consumers was formed in Russia in 2004. This Service carries out the activity directly and through the territorial organizations in interaction with administrative structures in food control and inspection, namely in sanitary-epidemiological service, veterinary service, grain service, inspection of trade connections and standardization and certification. The control is carried out on the basis of laws. The law № 29-FZ concerns the quality and safety of foodstuff and how to control it. The law 134-FZ attracted the protection of the rights of legal persons and individual businessmen. The modification of the law №234-FZ about protection of the rights of consumers is connected with new food - GMOs. Great attention is paid to the safety of new food. Private companies also perform analysis of heavy metals, mycotoxins, radiation and the presence of bacteria, virus or genetically modified organisms. We would like to thank the group Pilot Study "Food chain security" for very important work concerning food safety in different countries. They help us to understand internal problems in Russia and to create the cooperation with other countries. All these steps are very important for the protection population from toxic food.

  16. Modeling and Assessing Insect Disturbance on Boreal Forests in the Krasnoyarsk region of Russia by Employing the FAREAST Gap Model and Local Forest Inventory and Disturbance Data.

    NASA Astrophysics Data System (ADS)

    Erler, A. E.; Shuman, J. K.; Soukhavolosky, V.; Kovalev, A.; Stevens, T.; Shugart, H. H.

    2008-12-01

    FAREAST: an individual-based forest dynamics model was initially developed to simulate the forested region around Changbai Mountain in northern China. In recent years the model has been expanded across Siberia. The model output for biomass (tCha-1) has been verified against forest inventory data for a number of sites across Russia. With this success, an additional module for the model was written by Anton Kovalev to predict the impact of insect disturbance on the Boreal forests. This model predicts the probability of an insect outbreak occurring, and then, by assessing each individual tree in a modeled stand, predicts whether a tree will be killed as a result of insect predation. From this, a disturbance index is calculated that includes lost biomass as a result of insect disturbance and subsequent species composition. This disturbance "fingerprint" is being compared to forest inventory and insect disturbance data from the Usolsky forests in the Krasnoyarsk region of central Siberia. Silkworm disturbance is expressed in this geo- database as a percentage of trees damaged or killed in a stand. The forest inventory data allows us to calculate a biomass estimate that will be compared to the biomass outputs generated by the model post insect disturbance. The validation of simulated biomass with independent inventory data confirms that FAREAST is a robust model of Russian forest dynamics. Effective validation of the insect disturbance model will allow us to generate a more complete picture of the changing ecology of the Siberian Boreal landscape. The economic cost of lumber lost as a result of Silkworm damage has been enormous, if verified, FAREAST will afford us the opportunity to estimate the extent of that loss and predict the changing ecological dynamics of the Boreal forest system under the worlds evolving climate.

  17. [Prevalence of atrophic gastritis in different populations in Siberia on medical evidence of the serological survey].

    PubMed

    Reshetnikov, O V; Kurilovich, S A; Krotov, S A; Krotova, V A; Bessonov, P P; Vasil'ev, R R; Tatarinova, O V; Muchina, E G

    2008-01-01

    Prevalence of atrophic gastritis in various population of Siberia with serological tests was studied. Representative samples of Novosibirsk adult population and also urban and rural population of Yakutia were examined. 348 persons at the age more than 45 years (180 males and 168 females) were studied. Concentration of pepsinogen I, gastrin 17 and antibodies to Helicobacter pilori in blood serum was estimated with immune-enzyme analysis ("Biohit GastroPanel", "Biohit", Finland). In addition, domestic test-systems were used for detection cytotoxic (expressing CagA-protein) strains H. pylori. Level of markers (pepsinogen, gastrin, antibodies to Helicobacter pilori and antibodies to CagA H. pilori) in observing populations had no difference between males and females, and also did not depend on age. Occurrence of atrophy in body of stomach in Novosibirsk population, urban and rural population of Yakutia was 10.1, 16.7 and 25.6% respectively, and in antral part--10.7, 25.6 and 8.9% respectively. Total atrophy was registered in 1% in all groups. Helicobacter infection was detected in 78-88% of population. Domestic immune-enzyme test-systems were comparable with data of histological examination and demonstrated greater sensitivity at H. pylori detection vs. foreign. High prevalence of atrophic gastritis in various groups of Siberia population was noticed, which must be was bounded with great level of H. pylori infection in population.

  18. ICESat-Derived Elevation Changes on the Lena Delta and Laptev Sea, Siberia

    NASA Astrophysics Data System (ADS)

    Muskett, Reginald

    2014-05-01

    We employ elevation data from the Ice, Cloud, and land Elevation Satellite (ICESat) Geoscience Laser Altimeter System (GLAS) to investigate surface changes across the Lena Delta and sea ice of the coastal Laptev Sea, Siberia during winters of 2003 through 2008. We compare ICESat GLAS-derived elevation changes on sea ice and the Bykovskaya and Sardakhskaya Channels with datum-corrected tide gauge height measurements from Danai, Sannikova and Tiksi stations. We find the coastal sea ice and large inland ice covered channels elevation changes are in phase with the tide-height changes on a same-month-year and datum controlled basis. Furthermore, we find elevation change on tundra drained lake basins to be +0.03 +/- 0.02 m, on average. These findings indicate ICESat GLAS is capable of detection of tide fluxes of ice covered coastal rivers and with a small error range is suitable for investigations of active-layer and permafrost dynamics associated with seasonal freezing (heave) and thawing (subsidence) using repeat-location profiles. Ref.: Muskett, R.R., "ICESat-Derived Elevation Changes on the Lena Delta and Laptev Sea, Siberia," Open Journal of Modern Hydrology, 4 (1), pp. 1-9, 2014. http://www.scirp.org/journal/PaperDownload.aspx?paperID=41709.

  19. Climate-Induced Mortality of Siberian Pine and Fir in the Lake Baikal Watershed, Siberia

    NASA Technical Reports Server (NTRS)

    Kharuk, Viacheslav I.; Im, Sergei T.; Petrov, Ilya A.; Golyukov, Alexei S.; Ranson, Kenneth J.; Yagunov, Mikhail N.

    2016-01-01

    Siberian pine (Pinus sibirica) and fir (Abies sibirica) (so called ''dark needle conifers", DNC) showed decreased radial growth increment within the Lake Baikal watershed since the 1980s with increasing mortality recorded since the year 2000. Tree ring width was strongly correlated with vapor pressure deficit, aridity and root zone moisture. Water stress from droughts made trees more susceptible to insect attacks causing mortality in about 10% of DNC stands within the Lake Baikal watershed. Within Siberia DNC mortality increased in the southern part of the DNC range. Biogeographically, tree mortality was located within the DNC - forest-steppes transition. Tree mortality was significantly correlated with drought and soil moisture anomalies. Within the interior of the DNC range mortality occurred within relief features with high water stress risk (i.e., steep convex south facing slopes with shallow well-drained soils). In general, DNC mortality in Siberia was induced by increased aridity and severe drought (inciting factors) in synergy with biotic attacks (contributing factor). In future climate scenarios with predicted increase in aridity DNC could be eliminated from the southern part of its current range and will be replaced by drought-resistant conifers and broadleaf species (e.g., Larix sibirica, Pinus silvestris, and Betula pubescence).

  20. Endurance of larch forest ecosystems in eastern Siberia under warming trends

    NASA Astrophysics Data System (ADS)

    Sato, H.; Iwahana, G.; Ohta, T.

    2015-12-01

    The larch (Larix spp.) forest in eastern Siberia is the world's largest coniferous forest. However, its existence depends on near-surface permafrost, which increases water availability for trees, and the boundary of the forest closely follows the permafrost zone. Therefore, the degradation of near-surface permafrost due to forecasted warming trends during the 21st century is expected to affect the larch forest in Siberia. However, predictions of how warming trends will affect this forest vary greatly, and many uncertainties remain about land-atmospheric interactions within the ecosystem. We developed an integrated land surface model to analyze how the Siberian larch forest will react to current warming trends. This model analyzed interactions between vegetation dynamics and thermo-hydrology and showed that, under climatic conditions predicted by the Intergovernmental Panel on Climate Change (IPCC) Representative Concentration Pathway (RCP) scenarios 2.6 and 8.5, annual larch net primary production (NPP) increased about 2 and 3 times, respectively, by the end of 21st century compared with that in the 20th century. Soil water content during larch growing season showed no obvious trend, even after decay of surface permafrost and accompanying sub-surface runoff. A sensitivity test showed that the forecasted warming and pluvial trends extended leafing days of larches and reduced water shortages during the growing season, thereby increasing productivity.

  1. Bird orientation at high latitudes: flight routes between Siberia and North America across the Arctic Ocean

    PubMed

    Alerstam; Gudmundsson

    1999-12-22

    Bird migration and orientation at high latitudes are of special interest because of the difficulties associated with different compass systems in polar areas and because of the considerable differences between flight routes conforming to loxodromes (rhumblines) or orthodromes (great circle routes). Regular and widespread east-north-east migration of birds from the northern tundra of Siberia towards North America across the Arctic Ocean (without landmark influences) were recorded by ship-based tracking radar studies in July and August. Field observations indicated that waders, including species such as Phalaropusfulicarius and Calidris melanotos, dominated, but also terns and skuas may have been involved. Analysis of flight directions in relation to the wind showed that these movements are not caused by wind drift. Assuming possible orientation principles based on celestial or geomagnetic cues, different flight trajectories across the Arctic Ocean were calculated: geographical loxodromes, sun compass routes, magnetic loxodromes and magnetoclinic routes. The probabilities of these four alternatives are evaluated on the basis of both the availability of required orientation cues and the predicted flight paths. This evaluation supports orientation along sun compass routes. Because of the longitudinal time displacement sun compass routes show gradually changing compass courses in close agreement with orthodromes. It is suggested that an important migration link between Siberia and North American stopover sites 1000-2500km apart across the Arctic Ocean has evolved based on sun compass orientation along orthodrome-like routes.

  2. Methane mapping and its seasonal cycle in the atmosphere of Western Siberia as observed by IASI

    NASA Astrophysics Data System (ADS)

    Khamatnurova, Marina; Gribanov, Konstantin; Zadvornykh, Ilya; Rokotyan, Nikita; Zakharov, Vyacheslav

    2014-05-01

    Western Siberia is wide area covered with pristine peatlands which play important role in global carbon balance. Large areas of arctic and subarctic wetlands are vulnerable to climate change and industrial activity on oil, natural gas mining together with their transportation. These areas can have important feedback mechanisms in global warming, due to their large carbon stocks and the presence of permafrost. This study presents iterative regularization methods, software tool and some results on CH4 content retrieval from Infrared Atmospheric Sounding Interferometer (IASI/MetOp series) spectra measured over Western Siberia. Dense coverage of IASI measurements can be used to map sink and source regions on the territory of target region. Because of pure statistics of direct vertical profile measurements and low signal to noise ratio for northern part of target region, only most stable methods of methane content retrieval are required. We used iteratively regularized Gauss-Newton and Levenberg-Marquardt methods without using a priory covariance matrices for methane vertical profiles. Some examples of interatively calculated averaging kernels for both methods are represented. Spatial distribution methane columnar value maps, seasonal variations for whole target region are represented. Comparison of ground-based FTIR measurements of methane in atmosphere with obtained IASI-CH4 over Kourovka site is presented. Comparison of GOSAT standard products for methane and our retrieval results are presented and discussed.

  3. Phosphorus status of soils from contrasting forested ecosystems in southwestern Siberia

    NASA Astrophysics Data System (ADS)

    Achat, D. L.; Bakker, M. R.; Zeller, B.; Derrien, D.; Barsukov, P.; Nikitich, P.

    2011-12-01

    Phosphorus is one of the most limiting nutrients in many ecosystems and mineral reserves available for fertilizer production are forecasted to last for no more than 100 yrs. Crop requirements for P are often lower in forests than in agriculture and P fertilization to forest ecosystems is not very common on a global scale. In southern Siberia, expected climate change would lead to higher overall precipitation, higher temperatures and subsequently to changes in land use (i.e. agricultural land could increase on detriment of forests). In the present work we evaluated P status in four forested ecosystems in southwestern Siberia including 1 site with lowland Populus tremula, and 3 upland sites in the Salair mountains with Populus tremula, Abies siberica or with small forest openings. The upland sites feature twice higher productivity than the lowland sites and it was suggested that thick snow cover on those sites would enable winter activity of microbial communities leading to faster soil degradation processes and higher nutrient availability. We thus wanted to test whether biological processes in the upland sites were of larger impact on P status than in the lowland sites. We combined 32P isotopic dilution techniques (for diffusive P), chemical extractions (for total P, organic P) and fumigation/incubation/respiration methods (for microbial P) to test this hypothesis. Additional soil analyses (C, N and othes) were performed. Results will be interpreted in the light of the exising knowledge on botany, climate, pedology and expected implications for future land use, would this occur to change.

  4. A longer climate memory carried by soil freeze-thaw processes in Siberia

    NASA Astrophysics Data System (ADS)

    Matsumura, Shinji; Yamazaki, Koji

    2012-12-01

    The climate memory of a land surface generally persists for only a few months, but analysis of surface meteorological data revealed a longer-term climate memory carried by soil freeze-thaw processes in Siberia. Surface temperature variability during the snowmelt season corresponds reasonably well with that in the summer of the following year, when most stations show a secondary autocorrelation peak. The surface temperature memory is thought to be stored as variations in the amount of snowmelt water held in the soil, and through soil freezing, which emerges as latent heat variations in the near-surface atmosphere during soil thawing approximately one year later. The ground conditions are dry in the longer-term climate memory regions, such as eastern Siberia, where less snow cover (higher surface air temperature) in spring results in less snowmelt water or lower soil moisture in the summer. Consequently, through soil freezing, it will require less latent heat to thaw in the summer of the following year, resulting in higher surface air temperature. In addition to soil moisture and snow cover, soil freeze-thaw processes can also act as agents of climate memory in the near-surface atmosphere.

  5. 300. VACANT LOTS BETWEEN WEST MADISON ALLEY AND WEST CHESTNUT ...

    Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey

    300. VACANT LOTS BETWEEN WEST MADISON ALLEY AND WEST CHESTNUT STREET, TOWARD WEST - Russell Neighborhood, Bounded by Congress & Esquire Alley, Fifteenth & Twenty-first Streets, Louisville, Jefferson County, KY

  6. 13. VIEW OF BRIDGE, LOOKING WEST FROM THE WEST TOWER ...

    Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey

    13. VIEW OF BRIDGE, LOOKING WEST FROM THE WEST TOWER TO THE MAIN SUSPENSION CABLE WEST ANCHORAGE. February 1987 - Verde River Sheep Bridge, Spanning Verde River (Tonto National Forest), Cave Creek, Maricopa County, AZ

  7. 110. WEST CHESTNUT STREET PAPTIST CHURCH AT 1725 WEST CHESTNUT ...

    Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey

    110. WEST CHESTNUT STREET PAPTIST CHURCH AT 1725 WEST CHESTNUT STREET, WEST SIDE - Russell Neighborhood, Bounded by Congress & Esquire Alley, Fifteenth & Twenty-first Streets, Louisville, Jefferson County, KY

  8. West Nile fever--a reemerging mosquito-borne viral disease in Europe.

    PubMed Central

    Hubálek, Z.; Halouzka, J.

    1999-01-01

    West Nile virus causes sporadic cases and outbreaks of human and equine disease in Europe (western Mediterranean and southern Russia in 1962-64, Belarus and Ukraine in the 1970s and 1980s, Romania in 1996-97, Czechland in 1997, and Italy in 1998). Environmental factors, including human activities, that enhance population densities of vector mosquitoes (heavy rains followed by floods, irrigation, higher than usual temperature, or formation of ecologic niches that enable mass breeding of mosquitoes) could increase the incidence of West Nile fever. PMID:10511520

  9. Petrology of the Plutonic Rocks of west-central Alaska

    USGS Publications Warehouse

    Miller, Thomas P.

    1970-01-01

    A series of plutons in west-central Alaska defines the Hogatza plutonic belt which extends for about 200 miles in an east-west direction from the northeastern Seward Peninsula to the Koyukuk River. The plutonic rocks have an aggregate area of about 1,200 square miles and their composition, distribution, and possible petrogenesis are discussed for the first time in this report. Field, petrographic and chemical data supported by K/Ar age dating indicate the plutonic rocks are divisible into two suites differing in age, location, and composition. The western plutons are mid-Cretaceous (~100 m.y.) in age and consist of a heterogeneous assemblage of monzonite, syenite, quartz monzonite. Associated with these granitic rocks is a group of alkaline sub-silicic rocks that forma belt of intrusive complexes extending for a distance of at least 180 miles from west-central Alaska to the Bering Sea. The complex at Granite Mountain shows a rare example of zoning from an alkaline rim to a quartz-bearing core. The occurrence of a similar complex at Cape Dezhnev on the easternmost tip of Siberia suggests the alkaline province may extend into Siberia. The easternmost plutons are Late Cretaceous (180 m.y.) in age and composed primarily of granodiorite and quartz monzonite similar to calc-alkaline plutons found throughout the North America Cordillera. The plutons are epizonal and intrude deformed but unmetamorphosed Lower Cretaceous andesitic volcanics and volcanic graywacke which constitute the highly mobile Yukon-Koyukuk volcanogenic province of west-central Alaska. No older rocks have been found within the confines of this vast tract; the occurrence of a bounding ophiolite sequence has lead to the suggestion that the province was formed by large-scale rifting and is underlain by oceanic crust. The possibility of no juvenile sialic crust over much of the area suggests that the potassium-rich magma now represented by the alkaline rocks originated in the mantle. The distribution of the

  10. Engineering a Business School in a Former Soviet-Era Closed City: The Case of Omsk, Siberia

    ERIC Educational Resources Information Center

    Chukhlomin, Valeri; Chukhlomina, Irina

    2013-01-01

    This article describes a modernization project undertaken by a nationally accredited Russian university located in Omsk, Siberia, and aimed at developing a new international business school. A unique feature of the project is that it was successfully implemented in a former Soviet-era closed city. Until 1991, the university hadn't had any…

  11. Palaeodistribution modelling of European vegetation types at the Last Glacial Maximum using modern analogues from Siberia: Prospects and limitations

    NASA Astrophysics Data System (ADS)

    Janská, Veronika; Jiménez-Alfaro, Borja; Chytrý, Milan; Divíšek, Jan; Anenkhonov, Oleg; Korolyuk, Andrey; Lashchinskyi, Nikolai; Culek, Martin

    2017-03-01

    We modelled the European distribution of vegetation types at the Last Glacial Maximum (LGM) using present-day data from Siberia, a region hypothesized to be a modern analogue of European glacial climate. Distribution models were calibrated with current climate using 6274 vegetation-plot records surveyed in Siberia. Out of 22 initially used vegetation types, good or moderately good models in terms of statistical validation and expert-based evaluation were computed for 18 types, which were then projected to European climate at the LGM. The resulting distributions were generally consistent with reconstructions based on pollen records and dynamic vegetation models. Spatial predictions were most reliable for steppe, forest-steppe, taiga, tundra, fens and bogs in eastern and central Europe, which had LGM climate more similar to present-day Siberia. The models for western and southern Europe, regions with a lower degree of climatic analogy, were only reliable for mires and steppe vegetation, respectively. Modelling LGM vegetation types for the wetter and warmer regions of Europe would therefore require gathering calibration data from outside Siberia. Our approach adds value to the reconstruction of vegetation at the LGM, which is limited by scarcity of pollen and macrofossil data, suggesting where specific habitats could have occurred. Despite the uncertainties of climatic extrapolations and the difficulty of validating the projections for vegetation types, the integration of palaeodistribution modelling with other approaches has a great potential for improving our understanding of biodiversity patterns during the LGM.

  12. Virologic and genetic studies relate Amerind origins to the indigenous people of the Mongolia/Manchuria/southeastern Siberia region.

    PubMed Central

    Neel, J V; Biggar, R J; Sukernik, R I

    1994-01-01

    A commonly held theory is that the first wave of migrants into the New World was derivative from the ethnic groups then inhibiting eastern Siberia. However, these ethnic groups lack a mtDNA haplogroup (B) that is well represented in Amerindian tribes. Also, the time depth of the other three mtDNA haplogroups found in Amerindians (A, C, and D) appears to be greater in the Amerindians than in the eastern Siberian ethnic groups. In this communication we demonstrate that the human T-cell lymphotrophic virus type II, present in 11 of the 38 Amerindian tribes thus far examined, is not present in any of the 10 ethnic groups of eastern Siberia that we have studied. However, the virus has just been reported in the indigenous population of Mongolia, and mtDNA haplogroup B is also represented in this region. On the basis of these facts, we propose that the ancestors of the first migrants to the New World were not derived from north and central Siberia but from populations to the south, inhabiting the regions of Mongolia, Manchuria, and/or the extreme southeastern tip of Siberia. Images PMID:7938021

  13. Experience and Perspectives of Art History Development in Educational Space of Siberia at the Turn of XX-XXI ?enturies

    ERIC Educational Resources Information Center

    Nekhvyadovich, Larisa Ivanovna; Chernyaeva, Irina Valerievna

    2016-01-01

    The article has a program-analytical nature, contains an analysis and assessment of the scientific school of T. M. Stepanskaya, Doctor of Arts, professor, member of Russian Union of Artists. The goal of T. M. Stepanskaya's professional activity is incorporation of Art History in higher educational institutions in Siberia. The authors consider the…

  14. Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite

    SciTech Connect

    Anderson, K.B.

    1994-08-01

    Analysis of three amber (resinite) samples collected from Middle and Upper Cretaceous sediments in the Taimyr Peninsula, Siberia, indicates that these materials are based on copolymers of biformene (I) and communol (II). No resinites of similar structural character have previously been described and hence, these samples represent a previously unknown structural sub-class of resinite.

  15. 5. EASTSIDE RESERVOIR, LOOKING WEST. WEST DAM UNDER CONSTRUCTION, QUARRIES ...

    Library of Congress Historic Buildings Survey, Historic Engineering Record, Historic Landscapes Survey

    5. EASTSIDE RESERVOIR, LOOKING WEST. WEST DAM UNDER CONSTRUCTION, QUARRIES TO LEFT MIDDLE GROUND OF PICTURE. - Eastside Reservoir, Diamond & Domenigoni Valleys, southwest of Hemet, Hemet, Riverside County, CA

  16. Pan-Observation Results on Snow Sublimation and its Parameterization in Both forested and Open Environment in Taiga of Eastern Siberia

    NASA Astrophysics Data System (ADS)

    Zhang, Y.; Suzuki, K.; Kubota, J.; Kadota, T.; Ohata, T.

    2002-12-01

    In the sub-arctic region of Siberia, like the Lena and Bikal basins, the snow cover is a dominant hydrological component to affect the river discharge and regional water resource. Sublimation from snow surface, which can sustained about seven months (later October to earlier May), has been identified as important hydrological process in high altitude and latitude region, which, as result of particularly complex mass and energy exchanges, remain incompletely, understood, though there has been recent progress in process studies. A survey of snow sublimation values from North American and Russian mass balance studies (Mcnay et al., 1988; Barry, 1991;) suggests that in boreal, montane and subalpine forests 25-45 % of the annual snowfall can sublimate from snow (Pomeroy and Gray, 1995). This range has been confirmed for other snowy environments such as maritime Japan (Nakai et al., 1993). From March to May of 2002, intensive observations on snow sublimation using pan method and meteorological condition of near ground surface atmosphere were made in Mogot experimental watershed, which is located in the southern mountain region of eastern Siberia (55.5°N, 124.7°E) approximately 60 km north of Tynda, in the Amur region, Russia. The land surface is predominantly covered by larch forest, but birch forest partly covers the ridge area and higher elevations are covered by pine forest. The observations, including the snow and meteorological elements, were conducted at three sites with different vegetation cover and surface condition: A sparse larch forest covers Site LF; Site OP is grassland and Site ES contains a sparse larch forest of east slope. The transparent plastic pan used for sublimation measurement was in diameter of 22 cm and depth of 20 cm. A natural snow bulk of the same size and shape as the pan was set at the 1 cm higher level than surrounding snow surface. The snow bulk in the pan was renewed according its temperature difference with surrounding snow. But it

  17. The Regional Institution of Higher Learning in Today's Russia

    ERIC Educational Resources Information Center

    Karamurzov, B. S.

    2014-01-01

    The regional universities in Russia are an important resource for the development of Russian society, but more needs to be done to increase their effectiveness, including tackling corruption and leveraging local competitive advantages.

  18. Evaluating the performance of Russia in the research in nanotechnology

    NASA Astrophysics Data System (ADS)

    Terekhov, A. I.

    2012-11-01

    The article analyzes the development of nano research in Russia during the years 1990-2010. To identify the contribution of Russia in nanoscience and to compare it with the contribution of other countries, we used the international multidisciplinary database Science Citation Index Expanded. Scientific performance is measured based on the growth rate of nano publications by countries and in the world, authorship patterns, indexes of international collaboration, etc. The indicators used are the national publication output, the total citations and the average citation per nano publication, the number and subject profile of highly cited nano publications; contribution and impact of Russian institutions. The article describes the current state and trends of nano research in Russia, their key players and the existing "centers of excellence." It also discusses some inconsistencies of Russia's science policy in the field of nanotechnology in light of the performed bibliometric study.

  19. Formation and growth rates of atmospheric nanoparticles: four years of observations at two West Siberian stations

    NASA Astrophysics Data System (ADS)

    Arshinov, Mikhail Yu.; Belan, Boris D.; Davydov, Denis K.; Kozlov, Artem V.; Arshinova, Victoria

    2015-04-01

    In spite of fact that the first report on the new particle formation (NPF) itself was done by John Aitken more than one century ago (Aitken, 1898), a phenomenon of NPF bursts taken place in the atmosphere was discovered not very long ago. Nevertheless, to date it is known that they may occur quite often in a variety of environments (Kulmala et al., 2004; Hirsikko et al., 2011). Siberia occupies a vast area covered by forests, but the comprehensive data on burst frequency, as well as on formation and growth rates of freshly nucleated particles in this key region are still lacking. Continuous measurements of aerosol size distribution carried out in recent years at two West Siberian stations (TOR-station - 56o28'41"N, 85o03'15"E; Fonovaya Observatory - 56o25'07"N, 84o04'27"E) allowed this gap in data to be filled up. Analysis of the size spectra classified in accordance with criteria proposed by Dal Maso et al. (2005) and Hammed et al. (2007) enabled a conclusion to be drawn that NPF events in Wets Siberia are more often observed during spring (from March to May) and early autumn (secondary frequency peak in September). On average, particle formation bursts took place on 23-28 % of all days. Such a seasonal pattern of the NPF occurrence is very similar to one observed at SMEAR II Station (Hyytiälä, Finland; Dal Maso et al. 2005, 2007). Formation rates (FR) of particles with diameters below 25 nm varied in a wide range from 0.1 to 10 cm-3 s-1. Mean values of FR for the entire period of observations were 1.7 cm-3s-1 (median = 1.13 cm-3 s-1) at TOR-station and 0.88 cm-3 s-1 (median = 0.69 cm-3 s-1) at Fonovaya Observatory. Enhanced values of FR are usually observed from spring to autumn. Mean growth rates of observed at TOR-station and Fonovaya Observatory were 6.5 nm h-1 (median = 5.0 nm h-1) and 8.3 nm h-1 (median = 6.4 nm h-1), respectively. This work was supported by the Branch of Geology, Geophysics and Mining Sciences of RAS (Program No. 5); State contracts of

  20. Historical Development of Nematology in Russia

    PubMed Central

    Mjuge, S. G.

    1977-01-01

    The development of Russian hematology is considered from the late nineteenth century to 1970. The dominant influences of I. N. Filipjev and A. A. Paramonov are discussed in the context of the persons whom they influenced and their conceptual approach to the problems posed hy nematodes. The advantages and disadvantages of the framework of Russian scientific administration are compared to those in the West. PMID:19305563

  1. U.S.-Russia Relations: Refocus, Rebuild, Reenergize

    DTIC Science & Technology

    2015-02-01

    Geopolitics: Rivalry or Partnership for China, Russia and Central Asia ? Routledge Contemporary Asia Series; 38. New York: Routledge, 2012. (HF...Summer 2013): 38-46. Kireeva, Anna. "Russia’s East Asia Policy: New Opportunities and Challenges." Perceptions 17, no. 4(Winter 2012): 49-78...Routledge Contemporary Asia Series; 38. New York: Routledge, 2012. (HF 3630.2 .Z7 C628 2012) Feifer, Gregory. Russians: The People behind the Power. New

  2. Efficacy of Aggression Replacement Training among Children from North-West Russia

    ERIC Educational Resources Information Center

    Koposov, Roman; Gundersen, Knut K.; Svartdal, Frode

    2014-01-01

    The aim of the study was to assess whether the Aggression Replacement Training (ART) programme is effective in increasing social skills and decreasing problem behaviour. The sample consisted of 232 children (mean age 10.9 yrs, SD = 2.32), their parents and teachers. The study had a quasi-experimental design with intervention and control groups.…

  3. Clinical pharmacology in Russia-historical development and current state.

    PubMed

    Zagorodnikova Goryachkina, Ksenia; Burbello, Aleksandra; Sychev, Dmitry; Frolov, Maxim; Kukes, Vladimir; Petrov, Vladimir

    2015-02-01

    Clinical pharmacology in Russia has long history and is currently active, but rather unrecognized internationally. It is governmentally approved as a teaching/scientific specialty since 1983 and as a medical specialty since 1997. Courses of clinical pharmacology are included in the undergraduate curricula in the 5th and/or 6th year of education at all medical schools in the Russian Federation. Postgraduate education includes initial specialization in internal medicine with further residency in clinical pharmacology. Governmental legislation recommends that every healthcare institution has either a department or a single position of clinical pharmacologist. Major routine duties include information about and monitoring of medication use, consultations in difficult clinical situations, pharmacogenetic counseling, therapeutic drug monitoring, pharmacovigilance, and participation in drug and therapeutics (formulary) committees. There are official experts in clinical pharmacology in Russia responsible for coordinating relevant legislative issues. The chief expert clinical pharmacologist represents the discipline directly at the Ministry of Health. Research in clinical pharmacology in Russia is extensive and variable, but only some of it is published i