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    The Impact of Holocene Climate on the Development of Prehistoric Societies in Southern Siberia

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    Author
    Kulkova, Marianna
    Krasnienko, Sergey
    Issue Date
    2010-01-01
    
    Metadata
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    Citation
    Kulkova, M., & Krasnienko, S. (2010). The impact of holocene climate on the development of prehistoric societies in Southern Siberia. Radiocarbon, 52(4), 1557-1569.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/654036
    DOI
    10.1017/S0033822200056319
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Geochemical data of 10Be, 14C, 18O obtained from natural archives (tree rings, ice sheets, varves, corals) indicates that the climate during the Holocene was not stable. The cosmogenic isotope fluctuations are bound by the periodicity on solar activity and climatic changes. The sharpest and most abrupt climatic deteriorations are registered in the Early and Middle Holocene at 8200, 5800, 5400, 4300, and 2800 cal BP. These events are characterized by cold conditions. The impact of climate on human communities in steppe depressions in southern Siberia (Nazarovo, Minusinsk, and Turano-Uyuk) was noticeable. The differences of local landscape-climatic conditions in these depressions were connected with global climatic changes to determine the processes of occupation, development, and migrations of ancient societies during the Neolithic, Bronze Age, and Iron Age. The chronology of archaeological cultures was also correlated with the local and global climatic changes during the Early and Middle Holocene in southern Siberia. Here, we generalize the literature data about Holocene climatic changes and archaeological cultures in the southern Siberia region.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200056319
    Scopus Count
    Collections
    Radiocarbon, Volume 52, Number 4 (2010)

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