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Radiocarbon Chronology of the Late Pleistocene–Holocene Paleogeographic Events in Lake Baikal Region (Siberia)

Published online by Cambridge University Press:  18 July 2016

Sergey K Krivonogov ,
Hikaru Takahara ,
Yaroslav V Kuzmin ,
Lyobov A Orlova ,
A J Timothy Jull ,
Toshio Nakamura ,
Norio Miyoshi ,
Kimiyasu Kawamuro  and
Elena V Bezrukova
Sergey K Krivonogov
Affiliation:
United Institute of Geology, Geophysics, and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Koptyug Ave. 3, Novosibirsk 630090, Russia. Corresponding author. Email: carpos@uiggm.nsc.ru
Hikaru Takahara
Affiliation:
Kyoto Prefectural University, 1-5 Hangi-cho, Shimogamo, Sakyo-ku, Kyoto 606-8522, Japan
Yaroslav V Kuzmin
Affiliation:
Pacific Institute of Geography, Far Eastern Branch of the Russian Academy of Sciences, Radio St. 7, Vladivostok 690041, Russia
Lyobov A Orlova
Affiliation:
Institute of Geology, Siberian Branch of the Russian Academy of Sciences, Koptyug Ave. 3, Novosibirsk 630090, Russia
A J Timothy Jull
Affiliation:
NSF-Arizona AMS Facility, University of Arizona, Tucson, Arizona 85721-0081, USA.
Toshio Nakamura
Affiliation:
Center for Chronological Research, Nagoya University, Chikusa, Nagoya 464-8602, Japan
Norio Miyoshi
Affiliation:
Okayama University of Science, 1-1 Ridai-cho, Okayama 700-0005, Japan
Kimiyasu Kawamuro
Affiliation:
Kansai Research Center, Forestry and Forest Products Research Institute, Kyoto 612-0855, Japan
Elena V Bezrukova
Affiliation:
Limnological Institute, Siberian Branch of the Russian Academy of Sciences, Ulanbatorskaya St. 3, Irkutsk 664033, Russia
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Abstract

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New radiocarbon dates obtained from Late Pleistocene and Holocene deposits of the southern, eastern, and northern shores of Lake Baikal in 1995–2001 are presented, and the most important results of paleoenvironmental studies based on C data are discussed. The following paleogeographic events were verified with the help of C dating: 1) first Late Pleistocene glaciation (Early Zyryan); 2) Middle Zyryan interstadial; 3) loess formation during the Late Zyryan (Sartan) deglaciation; 4) warm and cold events in the Late Glacial; and 5) vegetation changes and forest successions during the Late Glacial and Holocene.

Type
Part II
Information
Radiocarbon , Volume 46 , Issue 2: Proceedings of the 18th International Radiocarbon Conference (Part 2 of 2), Conference Editors: Nancy Beavan Athfield, Rodger J Sparks , 2004 , pp. 745 - 754
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

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