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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 7
Clim. Past, 13, 795-818, 2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 13, 795-818, 2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Jul 2017

Research article | 06 Jul 2017

Palaeoclimate characteristics in interior Siberia of MIS 6–2: first insights from the Batagay permafrost mega-thaw slump in the Yana Highlands

Kseniia Ashastina et al.
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Cited articles  
Aitken, M. J. and Stokes, S.: Climatostratigraphy, in: Chronometric dating in archaeology, edited by: Taylor, R. E. T. and Aitken, M. J., chap. 1, Springer Science & Business Media, New York, USA, 1–30, 1997.
Andreev, A. A., Grosse, G., Schirrmeister, L., Kuzmina, S. A., Novenko, E. Y., Bobrov, A. A., Tarasov, P. E., Ilyashuk, B. P., Kuznetsova, T. V., Krbetschek, M., and Meyer, H.: Late Saalian and Eemian palaeoenvironmental history of the Bol'shoy Lyakhovsky Island (Laptev Sea region, Arctic Siberia), Boreas, 33, 319–348, 2004.
Andreev, V. N.: Vegetation and Soils of Subarctic Tundra. Academy of science, Siberian Subbrunch Biological Institute, Nauka, Novosibirsk, Russia, 1980.
Ashastina, K., Reinecke, J., Wesche, K., and Kienast, F.: A newly formed permafrost outcrop in Batagay, Arctic Siberia sheds light on the Eemian vegetation of Beringia, 1st Central European Polar Meeting, 10–13 November 2015, Vienna, Austria, 2015.
Ashastina, K., Schirrmeister, L., Fuchs, M. C., and Kienast, F.: OSL age determination and sedimentological characteristics of the Batagay thaw slump, Northeastern Siberia,, 2017. 
Publications Copernicus
Short summary
We present the first detailed description and sedimentological analyses of an 80 m permafrost sequence exposed in a mega-thaw slump near Batagay in the Yana Highlands, Russia, and attempt to deduce its genesis. First dating results (14C, OSL) show that the sequence represents a continental climate record spanning from the Middle Pleistocene to the Holocene. We suggest that the characteristics of the studied deposits are a result of various seasonally controlled climatically induced processes.
We present the first detailed description and sedimentological analyses of an 80 m permafrost...