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Geographica Helvetica
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Volume 48, issue 3
Geogr. Helv., 48, 111-119, 1993
https://doi.org/10.5194/gh-48-111-1993
© Author(s) 1993. This work is distributed under
the Creative Commons Attribution 3.0 License.
Geogr. Helv., 48, 111-119, 1993
https://doi.org/10.5194/gh-48-111-1993
© Author(s) 1993. This work is distributed under
the Creative Commons Attribution 3.0 License.

  30 Sep 1993

30 Sep 1993

Climate and vegetation changes in the Northern Eurasia during the Younger Dryas

M. V. Muratova1, L. R. Serebryanny2, and O. V. Denissenko3 M. V. Muratova et al.
  • 1Department of Geography, Moscow State University, 119899 Moscow, Russia
  • 2Institute of Geography, Russian Academy of Science, 109017 Moscow, Russia
  • 3Department of Geography, Moscow State University 119899 Moscow, Russia

Abstract. The climate development of the Late Glacial/Holocene transition is one of the most riveting problem of environmental change under short-term cooling. This paper is devoted to a special reconstruction of climate and Vegetation in the Northern Eurasia with special reference to chronological level at 10,500 years b. p., i. e. just in the middle of the Younger Dryas . Reconstruction of Vegetation was based on detailed palaeo-climate maps with numeric estimation of temperature and precipitation parameters. Concluding results were affirmed by independent palaeodata.

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