METHANE IN GROUND ICE AND FROZEN SEDIMENTS IN THE COASTAL ZONE AND ON THE SHELF OF KARA SEA

I. D. Streletskaya; A. A. Vasiliev; G. E. Oblogov; P. B. Semenov; B. G. Vanshtein; E. M. Rivkina

doi:10.15356/2076-6734-2018-1-65-77

METHANE IN GROUND ICE AND FROZEN SEDIMENTS IN THE COASTAL ZONE AND ON THE SHELF OF KARA SEA

I. D. Streletskaya, A. A. Vasiliev, G. E. Oblogov, P. B. Semenov, B. G. Vanshtein, E. M. Rivkina

https://doi.org/10.15356/2076-6734-2018-1-65-77

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Abstract

Summary Degradation of permafrost on the continental shelf and shores of the Arctic seas may be a main cause of the methane emission to the atmosphere from marine sediments. To quantify this effect it is necessary to have reliable data on the methane content in the underground ice and frozen Quaternary deposits. Samples of frozen (permafrost) sediments and ground ice, taken in three reference coastal sections made in the Mid- and Late Pleistocene coastal exposures and on the Kara sea shelf, were collected and studied. The samples were analyzed to determine composition, salinity, organic carbon content, and other characteristics of the underground ices. About 270 samples allowed determination of the gas composition and the methane concentration. The gas is present in the pores of the rocks and air bubbles in the ice. Gas was present in pores of sediments and in bubbles within the ice. It has been established that the composition of non-hydrocarbon gases in the underground ice does not correspond to the composition of the atmosphere in the time of formation of them. The methane content in the underground ice and frozen sediments is characterized by very high variability. The highest concentrations of methane are inherent in layers of the massive ground ice and reach up to 23000 ppm; the maximum concentration of methane in the massive vein ices does not exceed 900 ppm. High concentrations of methane in layers of the massive ice confirm their non-glacier formation. The highest, up to 6400 ppm, methane concentrations in permafrost sediments are characteristic for the Late Pleistocene marine clays, while in the Mid Pleistocene marine clays it does not exceed 1700 ppm. The isotopic composition of methane in frozen sediments and ground ice in both, the Cara Sea coast and shelf, is indicative of similar bacterial genesis of the gas. The total organic carbon content plays the limiting role in the methane production and its accumulation in the frozen sediments and ground ice.

Keywords

ground ice, isotopic composition, methane content, Neopleistocene, permafrost,

About the Authors

I. D. Streletskaya

Lomonosov Moscow State University
Russian Federation

A. A. Vasiliev

Earth Cryosphere Institute, Siberian Branch, Russian Academy of Sciences; Tyumen State University
Russian Federation

G. E. Oblogov

Earth Cryosphere Institute, Siberian Branch, Russian Academy of Sciences; Tyumen State University
Russian Federation

P. B. Semenov

All-Russian Research Institute of Geology and Mineral Resources of the World Ocean (FSUE «VNIIOkeangeologia named after academician I.S. Gramberg»)
Russian Federation

Saint-Petersburg

B. G. Vanshtein

All-Russian Research Institute of Geology and Mineral Resources of the World Ocean (FSUE «VNIIOkeangeologia named after academician I.S. Gramberg»)
Russian Federation

Saint-Petersburg

E. M. Rivkina

Institute of Physicochemical and Biological Problems in Soil Sciences, Russian Academy of Sciences
Russian Federation

Moscow Region, Pushchino

References

1. Schuur E.A.G., Mcguire A.D., Schadel C., Grosse G., Harden J.W., Hayes D.J., Hugelius G., Koven C.D., Kuhry P., Lawrence D.M., Natali S.M., Olefeldt D., Romanovsky V.E., Schaefer K., Turetsky M.R., Treat C.C., Vonk J.E. Climate change and the permafrost carbon feedback. Nature. 2015, 520: 171–179.

2. Shakhova N., Semiletov I., Salyuk A., Yusupov V., Kosmach D., Gustafsson Ö. Extensive methane venting to the atmosphere from sediments of the East Siberian Arctic shelf. Science. 2010, 327: 1246–1250.

3. Streletskiy D.A., Anisimov O.A., Vasiliev A.A. Permafrost degradation. Snow and Ice-Related Hazards, Risks and Disasters. Elsevier. 2014, Chapter 10: 303–344.

4. Rokos S.I., Kostin A.D., Dlugach A.G. Free gas and permafrost in the sediments of the upper part of the section of the shallow areas of the shelf of the Pechora and Kara Seas. Sedimentologicheskiye protsessy i evolyutsiya morskikh ekosistem v usloviyakh morskogo periglyatsiala. Sedimentological processes and evolution of marine ecosystems in marine periglacial conditions. Apatity, 2001: 40–51. [In Russian].

5. Coffin R.B., Smith J.P., Plummer R.E., Yoza B., Larsen R.K., Millholland L.C., Montgomery M.T. Spatial variation in shallow sediment methane sources and cycling on the Alaskan Beaufort Sea Shelf Slope. Marine and Petroleum Geology. 2013, 45: 186–197.

6. Portnov A., Mienert J., Serov P. Modeling the evolution of climate-sensitive Arctic subsea permafrost in regions of extensive gas expulsion at the West Yamal shelf. Journ. of Geophys. Research. Biogeoscience. 2014, 119 (11): 2082–2094. doi: 10.1002/2014JG002685.

7. Olefeldt D., Turetsky M.R., Crilland P.M., McGuire A.D. Environmental and physical controls on northern terrestrial methane emissions across permafrost zones. Global Change Biology. 2012, 19 (2): 589–603. doi: 10.1111/gcb.12071.

8. St-Jean M., Lauriol B., Clark I.D., Lacelle D., Zdanowicz C. Investigation of ice-wedge infilling processes using stable oxygen and hydrogen isotopes, crystallography and occluded gases (O2, N2, Ar). Permafrost Periglac. Processes. 2011, 22: 49–64. doi: 10.1002/ppp.680,2011.

9. Rivkina E.M., Gilichinskiy D.A., Fedorov-Davydov D.G., Rivkin F.M., Shcherbakova V.M. Regularities in the distribution of greenhouse gases in permafrost rocks. Materialy Pervoy konferentsii geokriologov Rossii. Materials of the First Conf. of Geocryologists of Russia. M.: Moscow State University. 1996, 4: 157–162. [In Russian].

10. Rivkina Ye.M., Krayev G.N., Krivushin K.V., Laurinavichyus K.S., Fedorov-Davydov D.G., Kholodov A.L., Shcherbakova V.A., Gilichinskiy D.A. Methane in the permafrost deposits of the northeastern sector of the Arctic. Kriosfera Zemli. Cryosphere of the Earth. 2006, 10 (3): 23–41. [In Russian].

11. Cherbunina M.Yu., Brushkov A.V. Methane in the Late Pleistocene ice complex of Central Yakutia (Mamontova Gora). Materialy pyatoy konferentsii geokriologov Rossii. Materials of the Fifth Conf. of Russian Geocryologists. V. 3. Moscow: Universitetskaya kniga, 2016: 168–173. [In Russian].

12. Mel'nikov V.P., Spesivtsev V.I., Kulikov V.N.. Degassing of hydrocarbons as a source of ice formation on the shelf of the Pechora Sea. Itogi fundamental'nykh issledovaniy kriosfery Zemli v Arktike i Subarktike. Results of fundamental research of the Earth's cryosphere in the Arctic and Subarctic. Novosibirsk: Nauka. 1997: 259–269. [In Russian].

13. Rivkin F.M. The distribution of methane in frozen rocks in the Bovanenkovo gas condensate field on the Yamal peninsula. Itogi fundamental'nykh issledovaniy kriosfery Zemli v Arktike i Subarktike. Results of fundamental research of the Earth's cryosphere in the Arctic and Subarctic. Novosibirsk: Nauka, 1997: 168–173. [In Russian].

14. Rivkina Ye.M., Gilichinskiy D.A. Methane as a paleoindicator of genesis and dynamics of frozen sequences. Litologiya i poleznyye iskopayemyye. Lithology and Minerals. 1996, 4: 183–193. [In Russian].

15. Moorman B.J., Michel F.A., Wilson A.T. Development of tabular massive ground ice at Peninsula Point. N.T.W. Canada. Proc. of the 7th Intern. Conf. on Permafrost. Yellowknife. Canada. 1998: 757–761.

16. Lacelle D., Bjornson J., Lauriol B., Clark I.D., Troutet Y. Segregated intrusive ice of subglacial meltwater origin in retrogressive thaw flow headwalls. Richardson Mountains, NWT, Canada. Quaternary Science Reviews. 2004, 23: 681–696.

17. Cardyn R., Clark I.D., Lacelle D., Lauriol B., Zdanowicz C., Calmels F. Molar gas ratios of air entrapped in ice: A new tool to determine the origin of relict massive ground ice bodies in permafrost // Quaternary Research. 2007, 68: 239–248.

18. Lein A.YU., Leybman M.O., Savvichev A.S, Miller Yu.M, Pimenov N.V. Isotope-biogeochemical features of underground formation ice of the Yugorsk and Yamal peninsulas. Geokhimiya. Geochemistry. 2003, 10: 1084–1104. [In Russian].

19. Vasil'yev A.A., Streletskaya I.D., Mel'nikov V.P., Oblogov G.Ye. Methane in ground ice and frozen Quaternary deposits of Western Yamal. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2015, 465 (5): 604– 607. [In Russian].

20. Rivkina Ye.M., Samarkin V.A., Gilichinskiy D.A. Methane in the permafrost sediments of the Kolyma–Indigirskaya lowland. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 1992, 323 (3): 559–563. [In Russian].

21. Gilichinsky D., Rivkina E., Samarkin V. The ancient viablemicroorganisms and radioactive gases in West Beringia Permafrost: Research opportunities for Paleoecological implications and Forecast. Terrestrial paleoenvironmental studies in Beringia. Fairbanks Alaska. 1997: 134–145.

22. Wright J.F., Chuvilin E.M., Dallimore S.R. Methane hydrate formation and dissociation in fine sands at temperatures near 0 °C. Proc. of the 7th Intern. Conf. on Permafrost. Yellowknife. Canada. 1998: 1147–1153.

23. Lein A.Yu., Savvichev A.S., Leibman M.O., Miller Yu.M., and Pimenov N.V. Isotopic-biogeochemical peculiarities of tabular ground ice of Yugorsky and Yamal peninsula // Proc. of the 8th Int. Conf. on Permafrost (Zurich, Switzerland). Lisse, Netherlands: A.A.Balkema Publishers. 2003, 2: 661–666.

24. Leibman M.O., Hubberten H.-W., Lein A.Yu., Streletskaya I.D., Vanshtein B.G. Tabular ground ice origin in the Arctic coastal zone: cryolithological and isotopegeochemical reconstruction of conditions for its formation. Proc. of the 8th Intern. Conf. on Permafrost (Zürich, Switzerland). Lisse, Netherlands: A.A. Balkema Publishers, 2003, 1: 645–650.

25. Bondarev V.L., Mirotvorskiy M.Yu., Zvereva V.B., Oblekov G.I., Shaydullin R.M., Gudzenko V.T. Gaseogeochemical characteristics of the supernormal deposits of the Yamal Peninsula (on the example of the Bovanenkovo oil-condensate field). Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy. Geology, geophysics and development of oil and gas fields. 2008, 5: 22–34. [In Russian].

26. Forman S.L., Ingolfsson O., Gataullin V., Manley W.F., Lokrantz H. Late Quaternary stratigraphy, glacial limits and paleoenvironments of Maresale area, western Yamal Peninsula, Russia. Quaternary Research. 2002, 21: 1–12.

27. Kanevskiy M.Z., Streletskaya I.D., Vasil'yev A.A. Regularities in the formation of the cryogenic structure of the Quaternary deposits of the Western Yamal (on the example of the Marre-Sale district). Kriosfera Zemli. Cryosphere of the Earth. 2005, IX (3): 16–27. [In Russian].

28. Streletskaya I.D., Kanevskiy M.Z., Vasil'yev A.A. Massive ground ice in dislocated Quaternary sediments of western Yamal. Kriosfera Zemli. Cryosphere of the Earth. 2006, X (2): 68–78. [In Russian].

29. Streletskaya I.D., Shpolyanskaya N.A., Kritsuk L.N., Surkov A.V. Cenozoic deposits of the Western Yamal and the problem of their genesis. Vestnik MGU. Ser. 5. Geografiya. Herald of the Moscow State University. Ser. 5. Geography. 2009, 3: 50–57. [In Russian].

30. Bassinot F.C., Labeyrie L.L., Vincent E., Quidelleur X., Shackleton N.J., Lancelot Y. The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal. Earth and Planetary Science Letters. 1994, 126: 91–108.

31. Streletskaya I.D., Vasil'yev A.A., Oblogov G.Ye., Matyukhin A.G. Isotopic composition of the underground ice of the Western Yamal (Marre-Sale). Led i Sneg. Ice and Snow. 2013, 2 (122): 83–92. [In Russian].

32. Streletskaya I.D., Gusev Ye.A., Vasil'yev A.A., Oblogov G.Ye., Anikina N.YU., Arslanov KH.A., Derevyanko L.G., Pushina Z.V. Geocryological structure of Quaternary sediments of the shores of western Taimyr. Kriosfera Zemli. Cryosphere of the Earth. 2013, XVII (3): 17–26. [In Russian].

33. Streletskaya I.D., Vasiliev A.A., Vanstein B.G. Erosion of sediment and organic carbon from the Kara Sea coast. Arctic, Antarctic, and Alpine Research. 2009, 41 (1): 79–87.

34. Lazukov G.I. Antropogen severnoy poloviny Zapadnoy Sibiri (paleogeografiya). Anthropogen of the northern part of Western Siberia (paleogeography). Moscow: Moscow State University Publishing House, 1972: 250 p. [In Russian].

35. Baulin V.V., Shmelev L.M., Solomatin V.I. On the traces of ancient permafrost processes in the Middle Quaternary sediments of the lower reaches of the river Ob. Periglyatsial'nyye yavleniya na territorii SSSR. Periglacial phenomena on the territory of the USSR. Moscow: Moscow State University Publishing House, 1960: 206–219. [In Russian].

36. Alperin M.J., Reeburgh W.S. Inhibition experiments on anaerobic methane oxidation. Applied Environmetal Microbiology. 1985, 50: 940–945.

37. Raynaud D. The integrity of the ice record of greenhouse gases with a special focus on atmospheric. Led I Sneg. Ice and Snow. 2012, 2 (118): 5–14.

38. Boereboom T., Samyn D., Meyer H., Tison J.-L. Stable isotope and gas properties of two climatically contrasting (Pleistocene and Holocene) ice wedges from Cape Mamontov Klyk, Laptev Sea, northern Siberia. The Cryosphere. 2013, 7: 31–46. doi: 10.5194/tc-731-2013.

39. Streletskaya I.D., Vasiliev A.A., Melnikov V.P., Oblogov G.E. Estimation of Atmospheric Paleo Circulation Based on Isotope Composition of Ice Wedges. Doklady Earth Sciences. 2014, 457 (2): 1025–1027.

40. Portnov A., Smith A.J., Mienert J., Cherkashov G., Rekant P., Semenov P., Serov P., Vanshtein B. Offshore permafrost decay and massive seabed methane escape in water depths > 20 m at the South Kara Sea shelf. Geophys. Research Letters. 2013, 40: 3787–3792. doi: 10.1002/grl.50735.

41. Bock J., Martinerie P., Witrant E., Chappellaz J. Atmospheric impacts and ice core imprints of a methane pulse from clathrates. Earth and Planetary Science Letters. 2012, 349–350: 98–108. http://dx.doi.org/10.1016/j.epsl.2012.06.052.

42. Whiticar M.J. Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane. Chemical Geology. 1999, 161: 291–314.

43. Yakushev V.S. Prirodnyy gaz i gazovyye gidraty v kriolitozone. Natural gas and gas hydrates in the cryolithozone. Moscow: VNIIGAZ (All-Union Scientific Research Institute of Gas), 2009: 192 p. [In Russian].

Supplementary files

For citation: Streletskaya I.D., Vasiliev A.A., Oblogov G.E., Semenov P.B., Vanshtein B.G., Rivkina E.M. METHANE IN GROUND ICE AND FROZEN SEDIMENTS IN THE COASTAL ZONE AND ON THE SHELF OF KARA SEA. Ice and Snow. 2018;58(1):65-77. https://doi.org/10.15356/2076-6734-2018-1-65-77

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