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    Chronology and Possible Links between Climatic and Cultural Change During the First Millennium BC in Southern Siberia and Central Asia

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    Author
    Zaitseva, G. I.
    van Geel, B.
    Bokovenko, N. A.
    Chugunov, K. V.
    Dergahev, V. A.
    Dirksen, V. G.
    Koulkova, M. A.
    Nagler, A.
    Parzinger, G.
    van der Plicht, J.
    Bourova, N. D.
    Lebedeva, L. M.
    Show allShow less
    Issue Date
    2004-01-01
    Keywords
    absolute age
    archaeology
    Arzhan 2 burial mound
    Asia
    Bronze Age
    C 14
    carbon
    Cenozoic
    Central Asia
    climate change
    cores
    geochemistry
    Holocene
    human activity
    humidity
    Iron Age
    isotopes
    Kutuzhekovo Lake
    lacustrine environment
    lake sediments
    microfossils
    Minusinsk Valley
    miospores
    Neolithic
    palynomorphs
    pollen
    pollen diagrams
    Quaternary
    radioactive isotopes
    sediments
    Siberia
    soil profiles
    southern Siberia
    steppes
    Stone Age
    Uyuk Valley
    Show allShow less
    
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    Citation
    Zaitseva, G. I., van Geel, B., Bokovenko, N. A., Chugunov, K. V., Dergachev, V. A., Dirksen, V. G., ... & Lebedeva, L. M. (2004). Chronology and possible links between climatic and cultural change during the first millennium BC in southern Siberia and Central Asia. Radiocarbon, 46(1), 259-276.
    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/10150/654756
    DOI
    10.1017/S0033822200039576
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We reconstructed climate change during the second half of the Holocene for the Minusinsk (southern Siberia) and the Uyuk (Central Asia) valleys in the Eurasian steppe zone. Sediment cores from 2 lakes and a soil profile from the Arzhan-2 burial mount were investigated. We combined pollen and geochemical analyses and radiocarbon dating with the archaeological record. A sharp increase of human population density occurred at the transition from the Bronze Age to Iron Age (about 2700 cal BP). The most representative Scythian culture started in the Uyuk and the Minusinsk valleys after increased humidity and occupation capacity of the steppe zone during the 9th century BC.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200039576
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 1 (2004)

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