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Development of Surficial Deposits on Belyi Island (Kara Sea) during the Last 40,000 Years

Published online by Cambridge University Press:  19 November 2018

A Yurtaev ,
A Alexandrovskiy ,
V Skripkin ,
E Zazovskaya  and
A Dolgikh
A Yurtaev*
Affiliation:
Tyumen State University, Institute of Environmental and Agricultural Biology (X-BIO), Tyumen, Russia
A Alexandrovskiy
Affiliation:
Institute of Geography, Russian Academy of Sciences, Department of Soil Geography & Evolution, Moscow, Russia
V Skripkin
Affiliation:
Institute of Environmental Geochemistry of NAS and MES of Ukraine, Kiev, Ukraine
E Zazovskaya
Affiliation:
Institute of Geography, Russian Academy of Sciences, Department of Soil Geography & Evolution, Moscow, Russia
A Dolgikh
Affiliation:
Institute of Geography, Russian Academy of Sciences, Department of Soil Geography & Evolution, Moscow, Russia The People’s Friendship University of Russia (RUDN), Department of Science and Innovation Policy, Moscow, Russia
*
*Corresponding author. Email: [email protected].
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Abstract

A series of radiocarbon (14C) dates of peat and other materials, containing organic matter, were obtained from Belyi Island. We have identified a large group of dates associates with MIS 1, as well as a significant group of dates associated with the Kargin (MIS 3) period (40–31 ka cal BP). A large number of dates from the Late Glacial period and from the Early Holocene (MIS 1—ca. 14–9 ka cal BP) point to this time interval being associated with warm climate conditions (the Holocene thermal maximum). The climate cooled off significantly during the Middle and Late Holocene, and the intensity of peat accumulation declined. The dates from the MIS 2 period are missing, due to the conditions of this period being extremely unfavorable for the accumulation of peat, as well as of other materials suitable for 14C dating.

Keywords

Arcticburied peatenvironmentHoloceneLate Pleistocenemarine transgressionpaleoclimateradiocarbon dating
Type
Soil
Information
Radiocarbon , Volume 60 , Special Issue 5: 2nd Radiocarbon in the Environment Conference, Debrecen, Hungary, July 3–7, 2017 Part 2 of 2 and Radiocarbon & Diet 2 International Conference Aarhus, Denmark, June 20–23, 2017 , October 2018 , pp. 1439 - 1455
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

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Footnotes

Selected Papers from the 2nd Radiocarbon in the Environment Conference, Debrecen, Hungary, 3–7 July 2017

References

REFERENCES

Abakumov, EV, Shamilishviliy, GA, Yurtaev, AA. 2017. Soil polychemical contamination on Beliy Island as key background and reference plot for Yamal region. Polish Polar Research 38(3):313–332.Google Scholar
Alexandrovskiy, A, Yurtaev, A, Skripkin, V, Dolgikh, A, Yakimov, A. 2017. Radiocarbon age of the buried and modern peat soils on the Belyi Island (Kara Sea). Cryosols in Perspective: A View from the Permafrost Heartland. August 21–28, Yakutsk, Sakha (Yakutiya) Republic, Russia. p 9–10.Google Scholar
Artemyeva, ZS, Yurtaev, AA, Alexandrovskiy, AL, Zazovskaya, EP. 2016. The organic matter of the buried peat soils on Bely Island (Kara Sea). Byulleten’ pochvennogo instituta im. V.V. Dokuchayeva 85:36–55. In Russian.Google Scholar
Baranskaya, AV, Romanenko, FA. 2017. Quaternary deposits and paleogeography of the Belyi Island in the Late Pleistocene and Holocene. Voprosy geomorfologii i paleogeografii morskikh poberezhiy i shel’fa. Materialy nauchnoy konferentsii pamyati Pavla Alekseyevicha Kaplina. Geograficheskiy fakul’tet MGU:29–32. In Russian.Google Scholar
Baranskaya, AV, Romanenko, FA, Arslanov, HA, Maksimov, FE, Starikova, AA, Pushina, ZV. 2018. Perennially frozen deposits of Bely Island: stratigraphy, age, depositional environments. Kriosfera Zemli XXII(2):3–15. In Russian.Google Scholar
Bolshiyanov, D, Makarov, A, Savelieva, L. 2015. Lena River delta formation during the Holocene. Biogeoscience 12:579–593.Google Scholar
Bronk Ramsey, C. 2013. OxCal Program v4.2.4. Oxford: Radiocarbon Accelerator Unit, University of Oxford.Google Scholar
Cheng, P, Zhou, W, Wang, H, Lu, X, Du, H. 2013. 14C Dating of soil organic carbon (SOC) in loess-paleosol using sequential pyrolysis and accelerator mass spectrometry (AMS). Radiocarbon 55(2–3):563–570.Google Scholar
Cherkinsky, A, Culp, R, Dvoracek, D, Noakes, J. 2010. Status of the AMS facility at the University of Georgia. Nuclear Instruments and Methods in Physics Research B 268:867–870.Google Scholar
Evseev, AV, Svitoch, AA. 1979. Buried soils and geochemical features of the newest deposits of the island of Aion (Chaun Bay). Pochvovedeniye 11:17–24. In Russian.Google Scholar
FAO-UNESCO Soil Map of the World, Revised Legend, with corrections and updates. 1997. Technical Paper 20. ISRIC. Wageningen.Google Scholar
Gavrilov, AV, Romanovskii, NN, Hubberten, H-W. 2006. Paleogeographic scenario of the postglacial transgression on the Laptev Sea shelf. Kriosfera Zemli X(4):39–50. In Russian.Google Scholar
Gubin, SV. 1996. Late Pleistocene Soil Formation in Northeast Eurasia. Doklady AN SSSR 351(4):544–547. In Russian.Google Scholar
Kaplin, PA. 1975. The recent history of the coasts of the World Ocean. M.:Izd of MGU. 265 p. In Russian.Google Scholar
Kaplin, PA, Selivanov, AO. 1999. Change in the sea level of Russia and the development of the coast. M.:GEOS. 316 p. In Russian.Google Scholar
Kaufman, DS, Ager, TA, Anderson, NJ, Anderson, PM, Andrews, JT, Bartlein, PJ, Brubaker, LB, Coats, LL, Cwynar, LC, Duvall, ML, Dyke, AS, Edwards, ME, Eisner, WR, Gajewski, K, Geirsdóttir, A, Hu, FS, Jennings, AE, Kaplan, MR, Kerwin, MW, Lozhkin, AV, MacDonald, GM, Miller, GH, Mock, CJ, Oswald, WW, Otto-Bliesner, BL, Porinchu, DF, Rühland, K, Smol, JP, Steig, EJ, Wolfe, BB. 2004. Holocene thermal maximum in the western Arctic (0–180°W). Quaternary Science Reviews 23(5–6):529–560.Google Scholar
Khotinskiy, NA. 1977. Holocene of Northern Eurasia: experience of transcontinental correlation of the stages of vegetation and climate development. Nauka. 200 p. In Russian.Google Scholar
Kienast, F, Schirrmeister, TL, Siegert, C, Tarasov, P. 2005. Palaeobotanical evidence for warm summers in the East Siberian Arctic during the last cold stage. Quaternary Research 63:283–300.Google Scholar
MacDonald, GM, Velichko, A, Kremenetski, C, Borisova, O, Goleva, A, Andreev, A, Cwynar, LC, Riding, R, Forman, S, Edwards, T, Aravena, R, Hammarlund, D, Szeicz, J, Gattaulin, V. 2000. Holocene Treeline History and Climate Change Across Northern Eurasia. Quaternary Research 53:302–331.Google Scholar
Moskovchenko, DV, Kurchatova, AN, Fefilov, NN, Yurtaev, AA. 2017. Concentrations of trace elements and iron in the Arctic soils of Belyi Island (the Kara Sea, Russia): patterns of variation across landscapes. Environ Monit Assess 189:210.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Grootes, PM, Guilderson, TP, Haflidason, H, Hajdas, I, Hatt, C, Heaton, TJ, Hoffmann, DL, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Staff, RA, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0-50,000 Years cal BP. Radiocarbon 55(4):1869–1887.Google Scholar
Skripkin, VV, Kovalyukh, NN. 1998. Recent development in the procedures used at the SSCER Laboratory for the routine preparation of lithium carbide. Radiocarbon 40:211–214.Google Scholar
Slagoda, EA, Leibman, MO, Khomutov, AV, Orekhov, PT. 2013. Cryolithologic construction of the firstnterrace at Bely Island, Kara Sea (Part 1). Kriosfera Zemli XVII (4):11–21. In Russian.Google Scholar
Stein, R, Dittmers, KH, Fahl, K, Kraus, M, Matthiessen, J, Niessen, F, Pirrung, M, Polyakova, YeI, Schoster, F, Steinke, T, Fütterer, DK. 2004. Arctic (palaeo) river discharge and environmental change:evidence from the Holocene Kara Sea sedimentary record. Quaternary Science Reviews 23(11–13):1485–1511.Google Scholar
Streletskaya, ID, Vasiliev, AA, Oblogov, GE, Tokarev, IV. 2015. Reconstruction of paleoclimate of Russian arctic in Late Pleistocene-Holocene on the basis of isotope study of ice wedges. Earth’s Cryosphere 19(2):98–106.Google Scholar
Tarasov, PE, Andreev, AA, Romanenko, FA, Sulerzhitskii, LD. 1995. Palynostratigraphy of upper Quaternary deposits of Sverdrup Island, the Kara Sea. Stratigraphy and Geological Correlation 3:190–196. In Russian.Google Scholar
Vasil’chuk, AC. 2017a. Palynological spectra and chronology of poligonalno-zhilnye complexes of Yamal. Arktica and Antarktika 1:84–109. In Russian.Google Scholar
Vasil’chuk, AC. 2017b. Palynological spectra of Holocene poligonalno-zhilnye structures of the Belyi Island and the valley of the Tabmei River of the Yamal Peninsula. Arktica and Antarktika 2:1–24. In Russian.Google Scholar
Vasilchuk, YUK, Petrova, EA, Serova, AK.1983. Some features of the paleogeography of the Holocene of Yamal. Byulleten’ po izucheniyu chetvertichnogo perioda 52:73–89. In Russian.Google Scholar
Velichko, AA, Faustova, MA, Pisareva, VV, Karpukhina, NV. 2017. History of the Scandinavian ice sheet and surrounding landscapes during Valday ice age and the Holocene. Ice and Snow 57(3):391–416. In Russian.Google Scholar
Velichko, AA, Timireva, S N, Kremenetski, KV, MacDonald, G, Smith, L. 2011. West Siberian Plain as a late glacial desert. Quaternary International 237:45–53.Google Scholar
Wacker, L, Němec, M, Bourquin, J. 2010. A revolutionary graphitisation system:fully automated, compact and simple. Nuclear Instruments and Methods in Physics Research B 268(7–8):931–934.Google Scholar
Zazovskaya, E, Mergelov, N, Shishkov, V, Dolgikh, A, Miamin, V, Cherkinsky, A, Goryachkin, S. 2017. Radiocarbon age of soils in oases of East Antarctica. Radiocarbon 59(2):489–503.Google Scholar