Complex use of the geochemical features of bottom deposits and pollen records for paleoclimate reconstructions (with lake Teletskoe, Altai Republic, as an example)

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• 作者：V. V. Babich ; N. A. Rudaya ; I. A. Kalugin ; A. V. Darin
• 关键词：climate ; paleoreconstruction ; bottom sediments ; pollen analysis ; biomes
• 刊名：Contemporary Problems of Ecology
• 出版年：2015
• 出版时间：July 2015
• 年：2015
• 卷：8
• 期：4
• 页码：405-413
• 全文大小：1,046 KB
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• 作者单位：V. V. Babich (1)
  N. A. Rudaya (2) (3)
  I. A. Kalugin (1)
  A. V. Darin (1)
  
  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
  2. Institute of Archeology and Ethnography, Siberian Branch, Russian Academy of Sciences, pr. Akademika Lavrent鈥檈va 17, Novosibirsk, 630090, Russia
  3. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
  
• 刊物主题：Ecology;
• 出版者：Springer US
• ISSN：1995-4263

文摘

The delayed response of taiga and steppe biomes to climate changes has been detected with Lake Teletskoe as an example. A paleoreconstruction has been made on the basis of the integral use of geochemical features of bottom sediments and pollen records. It showed 100-year mean temperatures to a time depth of 4000 years with the isolation of the assumed boundaries of climate reconstructions in the 14th and 4th centuries B.C. and the 13th and 20th centuries A.D. A comparison of the temperature reconstruction for Lake Teletskoe with the temperature chronologies for the Northern Hemisphere and northeastern Europe has been carried out.