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Chronology of Soil Evolution and Climatic Changes in the Dry Steppe Zone of the Northern Caucasus, Russia, During the 3rd Millennium BC

Published online by Cambridge University Press:  18 July 2016

A L Alexandrovskiy ,
J van der Plicht ,
A B Belinskiy  and
O S Khokhlova
A L Alexandrovskiy
Affiliation:
Institute of Geography, Russian Academy of Sciences, Moscow, Russia
A B Belinskiy
Affiliation:
State Department “Nasledie”, Stavropol, Russia
O S Khokhlova
Affiliation:
Institute of Physical, Chemical and Biological Problems of Soil Science, Russian Academy of Sciences, Pushchino, Moscow region, Russia
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Abstract

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Chrono-sequences of paleosols buried under different mounds of the large Ipatovo Kurgan, constructed during the Bronze Age, have been studied to reconstruct climatic changes in the dry steppe zone of the Northern Caucasus, Russia. Abrupt climatic and environmental changes in the third millennium BC have been reconstructed, using morphological and analytical data of the soil. Based on accelerator mass spectrometry (AMS) dates of small charcoal fragments from the soil chrono-sequence, we concluded that two upper paleosols (with the clearest evidence of arid pedogenesis) developed between about 2600–2450 BC.

Type
I. Our ‘Dry’ Environment: Above Sea Level
Information
Radiocarbon , Volume 43 , Issue 2B: Proceedings of the 17th International Radiocarbon Conference (Part 2 of 3), Conference Editors: Israel Carmi, Elisabetta Boaretto , 2001 , pp. 629 - 635
Copyright
Copyright © 2001 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Dalfes, HN, Kukla, G, Weiss, H, editors. 1997. Third Millennium BC. Climate change and Old World collapse. Nato ASI Series. Series I: global environmental change. Vol 49. Springer Verlag.Google Scholar
Demkin, VA. 1997. Paleopochvovedeniye i archeologiya (Paleopedology and archaeology). Pushchino: Pushchino Research Centre Press. 213 p (in Russian).Google Scholar
Fedoroff, N, Demkin, VA, Courty, M-A. 1997. Non-linear behaviour of soil systems during Holocene. Mitteilungen der Osterreichischen Bodenkundlichen Gesellschaft H 55:139–43.Google Scholar
Gerasimenko, NP. 1997. Environmental and climatic changes from 3 to 5ka BP in South-Eastern Ukraine. In: Dalfes, HN, Kukla, G, Weiss, H, editors. “Third Millennium BC. Climate Change and Old World Collapse”. Nato ASI Series. Series I: global environmental change. Vol 49. Springer Verlag. p 371–99.Google Scholar
Ivanov, IV, Alexandrovskiy, AL. 1987. Methods of the study of soil evolution. Soviet Soil Science 19(3):90–101.Google Scholar
Shishov, LL, Tonkonogov, VD, Lebedeva, II, editors. 1997. Russian soil classification. Moscow: V V Dokuchaev Soil Science Institute Press. 236 p. ISBN 5-86921-026-7.Google Scholar
Spiridonova, EA. 1991. Evolution of vegetation cover of the Don basin in the Upper Pleistocene-Holocene. Moscow, Nauka Press (in Russian).Google Scholar
Stuiver, M, Reimer, PJ, Bard, E, Beck, JW, Burr, GS, Hughen, KA, Kromer, B, McCormac, G, van der Plicht, J, Spurk, M. 1998. INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40(3):1041–83.Google Scholar
van der Plicht, J. 1993. The Groningen Radiocarbon Calibration Program. Radiocarbon 35(3):231–7.CrossRefGoogle Scholar
van der Plicht, J, Wijma, S, Aerts, AT, Pertuisot, MH, Meijer, HAJ. 2000. Status report: the Groningen AMS facility. Nuclear Instruments and Methods in Physics Research B172:58–65.CrossRefGoogle Scholar
Weiss, H, Courty, M-A, Wetterstrom, W. 1993. The genesis and collapse of Third Millennium North Mesopotamian civilization. Science 261:995–1004.Google Scholar
[WRB] World Reference Base for Soil Resources. 1994. World soil resources reports 84. 91 p. ISBN 92-5-104141-5.Google Scholar