Vegetation of Central Transbaikalia in the Late Glacial period and Holocene

Pleiades Publishing Ltd - Tập 34 - Trang 172-178 - 2013
S. A. Reshetova, E. V. Bezrukova1, V. Panizzo2, A. Henderson3, A. B. Ptitsyn4, A. V. Daryin5, I. A. Kalugin5
1Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia
2Environmental Change Research Centre, University College London, London, UK
3School of Geography, Politics and Sociology, Newcastle University, Newcastle, UK
4Institute of Natural Resources, Ecology, and Cryology, Siberian Branch, Russian Academy of Sciences, Chita, Russia
5Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia

Tóm tắt

Presented are the latest findings from investigating bottom sediments in Lake Arakhlei, containing continuous records of the vegetation evolution in the Beklemishevskaya depression and its mountain surroundings for the last 13 500 years.

Tài liệu tham khảo

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