Biogeochemistry of the Russian Arctic. Kara Sea: Research results under the SIRRO project, 1995-003

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• 作者：E. M. Galimov (1)
  L. A. Kodina (1)
  O. V. Stepanets (1)
  G. S. Korobeinik (1)
  
• 刊名：Geochemistry International
• 出版年：2006
• 出版时间：November 2006
• 年：2006
• 卷：44
• 期：11
• 页码：1053-1104
• 全文大小：1694KB
• 参考文献：1. E. M. Galimov, N. R. Laverov, O. V. Stepanets, and L. A. Kodina, “Preliminary Results of Ecological and Geochemical Investigations of the Russian Arctic Seas (Data obtained from Cruise 22 of the R/V Academik Boris Petrov),-Geokhimiya, No. 7, 579-97 (1996) [Geochem. Int. g class="a-plus-plus">34g>, 521-38 (1996)].
  2. / Siberian River Run-off in the Kara Sea. Characterization, Quantification, Variability and Environmental Significance. Proceedings in Marine Science,-Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6.
  3. Rep. Polar Mar. Res. g class="a-plus-plus">266g>, 266 (1988); g class="a-plus-plus">300g>, 239 (1999); g class="a-plus-plus">360g> 141 (2000); g class="a-plus-plus">393g>, 287 (2001); g class="a-plus-plus">419g>, 278 (2002); g class="a-plus-plus">450g>, 109 (2003).
  4. L. A. Kodina, M. P. Bogacheva, L. N. Vlasova, and E. M. Galimov, “Particulate Organic Matter from the Yenisei Estuary: Isotopic Composition, Distribution, and Genesis,-Geokhimiya, No. 11, 1206-217 (1999) [Geochem. Int. g class="a-plus-plus">37g>, 1087-096 (1999)].
  5. L. A. Kodina, S. V. Lyutsarev, and M. P. Bogacheva, “Sources of the Sedimentary Material in Drift Ice of the Arctic Basin According to Isotope Data on Organic Carbon from an Ice-Related Suspension,-Dokl. Earth Sci. g class="a-plus-plus">371g>, 526-30 (2000) [Dokl. Akad. Nauk g class="a-plus-plus">371g> (4), 511-15 (2000)].
  6. M. P. Bogacheva, S. V. Lyutsarev, and L. A. Kodina, “Particulate Organic Carbon in River and Sea Waters: Concentration and Stable Isotope Ratio,-Rep. Polar Mar. Res. g class="a-plus-plus">393g>, 161-64 (2001).
  7. L. A. Kodina, S. V. Lyutsarev, and M. P. Bogacheva, “Isotopic Composition of Organic Carbon of Ice Suspension as an Indicator of the Source of the Sedimentary Material of Drifting Arctic Ice: Evidence from Particulate Matter in the Drifting Ice of the Barents Sea,-in / Experience of System Oceanological Studies in Arctic, Ed. by A.P. Lisitsyn, M. E. Vonogradov, and E. A. Romankevich (Nauchnyi Mir, Moscow, 2001), 244-55 [in Russian].
  8. G. S. Korobeinik, V. G. Tokarev, T. I. Vaisman, and L. A. Kodina, “Distribution of Hydrocarbon Gases in the Water Sequence along the Yenisei River-Kara Sea Profile,-in / Experience of System Oceanological Studies in Arctic, Ed. by A. P. Lisitsyn, M. E. Vinogradov, and E. A. Romankevich (Nauchnyi Mir, Moscow, 2001), [in Russian].
  9. L. A. Kodina, “Carbon Isotope Composition of Phytoplankton on the Yenisei River-Estuary-Open Sea System and the Application of Isotopic Approach for Evaluation of Phytoplankton Contribution to the Yenisei POC Load,-Rep. Polar Mar. Res. g class="a-plus-plus">419g>, 143-49 (2002).
  10. L. A. Kodina, V. G. Tokarev, L. N. Vlasova, et al., “New Findings of Ikaite in the Kara Sea During RV “Akademik Boris Petrov-Cruise 36, September 2001,-Rep. Polar Mar. Res. g class="a-plus-plus">419g>, 164-72 (2002).
  11. L. A. Kodina and E. M. Galimov, “Authigenic Carbonate Mineral Ikaite Originated from Biogenic Methane in the Kara Sea Sediments,-in / Proceedings of 12th Annual V.M. Goldschmidt Conference, Davos Switzerland, 2002 Geochim. Cosmochim. Acta, Spec. Suppl. A409 (2002).
  12. L. A. Kodina and M. P. Bogacheva, “POC Isotope Composition in the Ob Estuary as Compared with the Yenisei System,-Rep. Polar Mar. Res. g class="a-plus-plus">419g>, 151-57 (2002).
  13. G. S. Korobeinik, V. G. Tokarev, and T. I. Vaisman, “Geochemistry of Hydrocarbon Gases in the Kara Sea Sediments,-Rep. Polar Mar. Res. g class="a-plus-plus">419g>, 158-64 (2002).
  14. L. A. Kodina, V. G. Tokarev, L. N. Vlasova, and G. S. Korobeinik, “Contribution of Biogenic Methane to Ikaite Formation in the Kara Sea: Evidence from the Stable Carbon Isotope Geochemistry,-in / Siberian River Run-Off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, 349-75.
  15. S. V. Lyutsarev and S. S. Shanin, “Characteristic Features of Particulate Organic Carbon Distribution in the Water Column of the Black Sea,-Okeanologiya g class="a-plus-plus">36g>(4) (1996) [Oceanology g class="a-plus-plus">36g>, 504-08 (1996)].
  16. S. Opsahl and R. Benne, “Distribution and Cycling of Terrigenous Dissolved Organic Matter in the Ocean,-Nature g class="a-plus-plus">386g>, 480-82 (1977). external" href="http://dx.doi.org/10.1038/386480a0">CrossRef
  17. V. V. Gordeev, J. M. Martin, S. I. Sidorov, and M. V. Sidorova, “A Reassessment of the Eurasian River Input of Water, Sediment, Major Elements, and Nutrients to the Arctic Ocean,-Am. J. Sci. g class="a-plus-plus">296g>, 664-91 (1996). external" href="http://dx.doi.org/10.2475/ajs.296.6.664">CrossRef
  18. H. Kohler, B. Meon, V. V. Gordeev et al., “Dissolved Organic Matter (DOM) in the Estuaries of Ob and Yenisei and Adjacent Kara Sea, Russia-in / Siberian River Run-off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, 281-08.
  19. M. J. K?rcher, M. Kulakov, S. Pivovarov et al., “Atlantic Water Flow to the Kara Sea: Comparing Model Results with Observations,-in / Siberian River Run-Off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 47-3.
  20. B. Meon and R. M. W. Amon, “Heterotrophic Bacterial Activity and Fluxes of Dissolved Free Amino Acids and Glucose in the Arctic Rivers Ob, Yenisei and the Adjacent Kara Sea,-Aquatic Microb. Ecol. g class="a-plus-plus">37g>, 121-35 (2004).
  21. I. H. Harms and M. J. Karcher, “Kara Sea Freshwater Dispersion and Export in the Late 1990s,-J. Geophys. Res. g class="a-plus-plus">110g>, C08007 (2005).
  22. V. K. Pavlov and S. I. Pfirman, “Hydrographic Structure and Variability of the Kara Sea: Implications for Pollutant Distribution,-Deep-Sea Res. II g class="a-plus-plus">42g>,(6) 1369-390 (1995). external" href="http://dx.doi.org/10.1016/0967-0645(95)00046-1">CrossRef
  23. / Ecology and Bioresources of the Kara Sea, Ed. by G. G. Matishov (AN SSSR, Apatity, 1989) [in Russian].
  24. J. Gaillardet, B. Dupre, P. Louvat, and S. J. Allegre, “Global Silicate Weathering and CO₂ Consumption Rates Deduced from the Chemistry of Large Rivers,-Chem. Geol. g class="a-plus-plus">159g>, 3-0 (1999). external" href="http://dx.doi.org/10.1016/S0009-2541(99)00031-5">CrossRef
  25. R. K. Dixon, S. Brown, R. A. Houghton, et al., “Carbon Pools and Flux of Global Forest Ecosystems,-Science g class="a-plus-plus">263g>, 185-90 (1994). external" href="http://dx.doi.org/10.1126/science.263.5144.185">CrossRef
  26. D. Unger and B. Gaye-Haake, K Neuman et al., “Biogeochemistry of Suspended and Sedimentary Material in the Ob and Yenisei Rivers and Kara Sea: Amino Acids and Amino Sugars,-Cont. Shelf Res. g class="a-plus-plus">25g>, 437-70 (2005). external" href="http://dx.doi.org/10.1016/j.csr.2004.09.014">CrossRef
  27. A. P. Lisitsyn, V. P. Shevchenko, M. E. Vinogradov, et al., “Flux of Sedimentary Material in the Kara Sea and in the Ob and Yenisei Estuaries,-Okeanologiya g class="a-plus-plus">34g>,(5) 748-58 (1994).
  28. E. A. Romankevich and A. A. Vetrov, / Carbon Cycle in Arctic Seas (Nauka, Moscow, 2001) [in Russian].
  29. V. I. Vedernikov, A. B. Demidov, and A. I. Sud’bin, “Primary Production and Chlorophyll in the Kara Sea in September, 1993,-Okeanologiya g class="a-plus-plus">34g>,(5) 693-03 (1994).
  30. R. A. H?rner, “Ecology of Sea Ice Microalga,-in / Sea Ice Biota Ed. by R. A. H?rner (CRC Press, Boca Raton, Florida, 1985), pp. 84-03.
  31. M. G?sselin, M. Lewasseur, P. A. Wheeler, et al., “New Measurements of Phytoplankton and Algal Production in the Arctic Ocean,-in / Deep Sea Res. Part II: Topical Studies in Oceanography, g class="a-plus-plus">44g>,(8) 1633-625 (1997).
  32. P. A. Wheeler, M. G?sselin, E. Sherr, et al., “Active Cycling of Organic Carbon in the Central Arctic Ocean,-Nature g class="a-plus-plus">380g>, 697-99 (1996). external" href="http://dx.doi.org/10.1038/380697a0">CrossRef
  33. D. Hebbeln and H. Berner, “Surface Sediment Distribution in the Fram Strait,-Deep-Sea Res. I g class="a-plus-plus">40g>(9), 1731-745 (1993). external" href="http://dx.doi.org/10.1016/0967-0637(93)90029-3">CrossRef
  34. R. Goerike and B. Ery, “Variations of Marine Plankton δ¹³C with Latitude, Temperature, and Dissolved CO₂ in the World Ocean,-Glob. Biogeochem. Cycles g class="a-plus-plus">8g>(1), 85-0 (1994). external" href="http://dx.doi.org/10.1029/93GB03272">CrossRef
  35. W. O. Smith, I. D. Walsh, D. C. Booth, and J. W. Deming, “Particulate Matter and Phytoplankton and Bacterial Biomass Distributions in the Northeast Water Polynya During Summer 1992,-J. Geophys. Res. g class="a-plus-plus">100g>(C3), 4341-356 (1995). external" href="http://dx.doi.org/10.1029/94JC02765">CrossRef
  36. C. J. Schubert and R. Stein, “Lipid Distribution in Surface Sediments from the Eastern Central Arctic Ocean,-Mar. Geol. g class="a-plus-plus">138g>(1-), 11-5 (1997). external" href="http://dx.doi.org/10.1016/S0025-3227(97)00017-0">CrossRef
  37. H. Notholt, “Die Auswirkungen der ‘NorthEastWater’—Polynya auf die Sedimentation vor NO Gronland und Untersuchungen zur Paleo-Ozeanographie seit dem Mittelwechsel,-Ber. Polarforsch. g class="a-plus-plus">275g>, 120 (1998).
  38. V. V. Larionov and P. R. Makarevich, “The Taxonomic and Ecological Descriptions of the Phytoplankton Assemblages from the Yenisei Bay and Adjacent Waters of the Kara Sea in September 2000,-Rep. Polar Mar. Res. g class="a-plus-plus">393g>, 48-2 (2001).
  39. V. V. Larionov and L. A. Kodina, “Phytoplankton of the Ob-Yenisei Transects,-Rep. Polar Mar. Res. g class="a-plus-plus">393g>, 48-2 (2000).
  40. V. V. Larionov, “Phytoplankton of the Ob-Yenisei Shallows in the Autumn,-Rep. Polar Mar. Res. g class="a-plus-plus">450g>, 20-1 (2003).
  41. V. V. Larionov, “Phytoplankton Distribution in the Ob and Yenisei Estuaries and Adjacent Kara Sea,-Rep. Polar Mar. Res g class="a-plus-plus">419g>, 41-3 (2002).
  42. E.-M. N?thig, Y. Okolodkov, V. V. larionov, and P. R. Makarevich, “Phytoplankton distribution in the Inner Kara Sea: A Comparizon of Three Summer Investigations,-in / Siberian River Run-off in the Kara sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 173-83.
  43. P. R. Makarevich, N. V. Druzhkov, V, V, Larionov, and E. I. Druzhnikova, “The Freshwater Phytoplankton Biomass and Its Role in the Formation of a Highly Productive Zone of the Ob-Yenisei Shallows (Southern Kara Sea),-in / Siberian River Run-Off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 181-85.
  44. P. D. Tortell, J. R. Reinfelder, and F. M. M. Morel, “Active Uptake of Bicarbonate by Diatoms,-Nature g class="a-plus-plus">390g>, 243-44 (1997). external" href="http://dx.doi.org/10.1038/36765">CrossRef
  45. B. Fry and S. C. Wainright, “Diatom Sources of ¹³C-Rich Carbon in Marine Food Webs,-Mar. Ecol. Progress Ser. g class="a-plus-plus">76g>, 149-57 (1991).
  46. E. M. Galimov, / Biological Isotope Fractionation (Academic Press, New York-Toronto-Orlando, 1984).
  47. M. A. Goňi, M. B. Yunker, R. W. MacDonald, and T. I. Eglinton, “The Supply and Preservation of Ancient and Modern Components of Organic Carbon in the Canadian Beaufort Shelf of the Arctic Ocean,-Mar. Chem., No. 93, 53-3 (2005).
  48. S. Pivovarov, R. Schlitzer, and A. Novikhin, “Modern Discharge: Data and Modeling,-in / Siberian River Run-off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 9-7.
  49. R. M. Holmes, B. J. Peterson, A. V. Zhulidov, et al., “Nutrient Chemistry of the Ob and Yenisei Rivers, Siberia: Results from June 2000 Expedition and Evaluation of Long-Term Data Set,-Mar. Chem. g class="a-plus-plus">75g>, 219-27 (2001). external" href="http://dx.doi.org/10.1016/S0304-4203(01)00038-X">CrossRef
  50. K. Fahl, R. Stein, B. Gaye-Haake et al., “Biomarkers in Surface Sediments from the Ob and Yenisei Estuaries and the Southern Kara Sea: Evidence for Particulate Organic Carbon Sources, Pathways, and degradation,-in / Siberian River Run-off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 329-49.
  51. H. K?hler, B. Meon, V. V. Gordeev et al., “Dissolved Organic Matter (DOM) in the Estuaries of Ob and Yenisei and Adjacent Kara Sea, Russia,-in / Siberian River Run-off in the Kara Sea. Characterization, Quantification, Variability, and Environmental Significance. Proceedings in Marine Science, Ed. by R. Stein, K. Fahl, D. Fuetterer, E. M. Galimov, and O. V. Stepanets (Elsevier, Amsterdam, 2003), Vol. 6, pp. 281-08.
  52. R. Benner, B. Biddanda, B. Black, and M. McCarthy, “Abundance, Size Distribution, and Stable Carbon and Nitrogen Isotopic Composition of Marine Organic Mater Isolated by Tangential Ultrafiltration,-Mar. Chem. g class="a-plus-plus">57g>, 343-63 (1997). external" href="http://dx.doi.org/10.1016/S0304-4203(97)00013-3">CrossRef
  53. V. Stanovoy and N. Schmelkov, “Water Temperature Fluctuations in the Marginal Zones in the Svjataja Anna and Voronin Troughs,-Rep. Polar Mar. Res. g class="a-plus-plus">419g>, 22-8 (2002).
  54. L. A. Kodina and V. I. Peresypkin, “Stable Carbon Isotope (δ¹³C_org) Ratio and Lignin-Derived Phenol Distribution in Surface Sediments of the Inner Kara Sea,-in / Scientific Cruise Report of the Kara-Sea Expedition 2001 of R/V Akademik Boris Petrov, Ed. by R. Stein, and O. V. Stepanets, Ber. Polarforsch. Meeresforsch. g class="a-plus-plus">419g>, 134-41 (2002).
  55. E. M. Galimov, “Carbon Isotope Composition of Antarctic Plants,-Geochim. Cosmochim. Acta, No. 64, 1737-739 (2000).
  56. E. M. Galimov, “Fractionation of Carbon Isotope in the Way from Living to Fossil Organic Matter,-in / Stable Isotope in Biosphere, Ed. by E. Wada et al. (Kyoto Univ., Kyoto, 1995), 133-70.
  57. A. M. Bol’shakov and A. V. Egorov, “Results of Gasometry in the Kara Sea,-Okeanologiya g class="a-plus-plus">35g>(3), 399-04 (1995).
  58. A. N. Belyaeva and G. Eglinton, “Lipid Biomarker Accumulation in the Kara Sea Sediments,-Okeanologiya g class="a-plus-plus">37g>(5), 705-14 (1997) [Oceanology g class="a-plus-plus">37g>, 634-42 (1997)].
  59. E. M. Galimov, “Sources and Mechanisms of Formation of Gaseous Hydrocarbons in Sedimentary Rocks,-Chem. Geol. g class="a-plus-plus">71g>, 77-5 (1988). external" href="http://dx.doi.org/10.1016/0009-2541(88)90107-6">CrossRef
  60. B. B. Namsaraev, I. I. Rusanov, A. S. Savichev, et al., “Bacterial Oxidation of Methane in the Estuary of the Yenisei River and Kara Sea,-Okeanologiya g class="a-plus-plus">35g>(1), 88-3 (1995).
  61. E. M. Galimov, “The Pattern δ¹³C_org Versus HI/OI Relation in Recent Sediments as an Indicator of Geochemical Regime in Marine Basing: Comparison of the Black Sea, Kara Sea and Cariaco Trench,-Chem. Geol. g class="a-plus-plus">204g>, 287-01 (2004). external" href="http://dx.doi.org/10.1016/j.chemgeo.2003.11.014">CrossRef
  62. E. M. Galimov, L. A. Kodina, L. I. Zhiltsova, et al., “Organic Carbon Geochemistry in the North Western Black Sea Danube River System,-Estuar. Coast. Shelf Sci., No. 54, 631-41 (2002).
  63. R. V. Krishnamurthy, M. Machavaram, M. Baskaran, et al., “Organic Carbon Flow in the Ob, Yenisey and Kara Sea of the Arctic Region,-Mar. Poll. Bull. g class="a-plus-plus">42g>(9), 726-32 (2001). external" href="http://dx.doi.org/10.1016/S0025-326X(00)00202-2">CrossRef
  
• 作者单位：E. M. Galimov (1)
  L. A. Kodina (1)
  O. V. Stepanets (1)
  G. S. Korobeinik (1)
  
  1. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, ul. Kosygina 19, Moscow, 119311, Russia
  
• ISSN：1556-1968

文摘

The Kara Sea is an area uniquely suitable for studying processes in the river-sea system. This is a shallow sea into which two great Siberian rivers, Yenisei and Ob, flow. From 1995 to 2003, the sea was studied by six international expeditions aboard the R/V Akademik Boris Petrov. This publication summarizes the results obtained, within the framework of this project, at the Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences. Various hydrogeochemical parameters, concentrations and isotopic composition of organic and carbonate carbon of the sediments, plankton, particulate organic matter, hydrocarbons, and dissolved CO2 were examined throughout the whole sea area at more than 200 sites. The δ13C varies from ?2 and ?4-where Atlantic waters enter the Kara Sea and in the North-eastern part of the water area to ?7-in the Yenisei and Ob estuaries. The value of δ13C of the plankton is only weakly correlated with the δ13C of the organic matter from the sediments and is lower by as much as 3-- The paper presents the results obtained from a number of meridional river-sea profiles. It was determined from the relations between the isotopic compositions of plankton and particulate matter that the riverwaters carry material consisting of 70% detrital-humus matter and 30% planktonogenic material in the river part, and the material contained in the off-shore waters consists of 30% terrigenous components, with the contribution of bioproducers amounting to 70%. The carbon isotopic composition of the plankton ranges from ?9 to ?5-in the riverine part, from ?8 to ?7-in the estuaries, and from ?7.0 to ?5% in the marine part. The relative lightness of the carbon isotopic composition of plankton in Arctic waters is explained by the temperature effect, elevated CO2 concentrations, and long-distance CO2 supply to the sea with riverwaters. The data obtained on the isotopic composition of CO2 in the surface waters of the Kara Sea were used to map the distribution of δ13CCO 2. The complex of hydrocarbon gases extracted from the waters included methane, C2–C5, and unsaturated C2=–C4= hydrocarbons, for which variations in the concentrations in the waters were studied along river-estuary-sea profiles. The geochemistry of hydrocarbon gases in surface fresh waters is characterized by comparable concentrations of methane (0.3- μl/l) and heavier hydrocarbons, including unsaturated ones. Microbiological methane with δ13C from ?05 to ?0-first occurs in the sediments at depths of 40-00 cm. The sediments practically everywhere display traces of methane oxidation in the form of a shift of the δ13C of methane toward higher values and the occurrence of autogenic carbonate material, including ikaite, enriched in the light isotope. Ikaite (δ13C from ?5 to ?0- was found and examined in several profiles. The redox conditions in the sediments varied from normal in the southern part of the sea to highly oxidized along the Novaya Zemlya Trough. Vertical sections through the sediments of the latter exemplify the complete suppression of the biochemical activity of microorganisms. Our data provide insight into the biogeochemistry of the Kara Sea and make it possible to specify the background values needed for ecological control during the future exploration operations and extraction of hydrocarbons in the Kara Sea.