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

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    Author
    Krivonogov, S. K.
    Takahara, Hikaru
    Kuzmin, Yaroslav V.
    Orlova, Lyobov A.
    Jull, A. J. Timothy cc
    Nakamura, Toshio
    Miyoshi, Norio
    Kawamuro, Kimiyasu
    Bezrukova, Elena V.
    Issue Date
    2004-01-01
    Keywords
    absolute age
    Asia
    Baikal region
    boreholes
    C 14
    carbon
    Cenozoic
    chronostratigraphy
    Commonwealth of Independent States
    cores
    dates
    Holocene
    isotopes
    microfossils
    miospores
    paleoclimatology
    paleoecology
    paleoenvironment
    paleogeography
    palynomorphs
    Pleistocene
    pollen
    Quaternary
    radioactive isotopes
    Russian Federation
    sediments
    Siberia
    Siberian fold belt
    upper Pleistocene
    vegetation
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    Citation
    Krivonogov, S. K., Takahara, H., Kuzmin, Y. V., Orlova, L. A., Jull, A. T., Nakamura, T., ... & Bezrukova, E. V. (2004). Radiocarbon chronology of the Late Pleistocene–Holocene paleogeographic events in Lake Baikal region (Siberia). Radiocarbon, 46(2), 745-754.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 18th International Radiocarbon Conference held in Wellington, New Zealand, September 1-5, 2003.
    URI
    http://hdl.handle.net/10150/654899
    DOI
    10.1017/S0033822200035785
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    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 14C data are discussed. The following paleogeographic events were verified with the help of 14C 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
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200035785
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 2 (2004)

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