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    Temporal Change of Radiocarbon Reservoir Effect in Sugan Lake, Northwest China during the Late Holocene

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    Author
    Zhou, Ai-feng
    Chen, Fa-hu
    Wang, Zong-li
    Yang, Mei-lin
    Qiang, Ming-rui
    Zhang, Jia-wu
    Issue Date
    2009-01-01
    
    Metadata
    Show full item record
    Citation
    Zhou, A., Chen, F., Wang, Z., Yang, M., Qiang, M., & Zhang, J. (2009). Temporal change of radiocarbon reservoir effect in Sugan Lake, northwest China during the late Holocene. Radiocarbon, 51(2), 529-535.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/654344
    DOI
    10.1017/S0033822200055909
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Many lacustrine chronology records suffer from radiocarbon reservoir effects. A continuous, accurate varve chronology, in conjunction with accelerator mass spectrometry (AMS) 14C dating, was used to determine the age of lacustrine sediment and to quantify the past 14C reservoir effect in Sugan Lake (China). Reservoir age varied from 4340 to 2590 yr due to 14C-depleted water in the late Holocene. However, during the Little Ice Age (LIA), 14C reservoir age was relatively stable. According to this study, 14C reservoir age in the late Holocene may be driven by hydrological and climatic changes of this period. Therefore, special caution should be paid to the correction of the 14C reservoir effect by a unique 14C reservoir age in paleoclimatic and paleolimnological study of northwest China.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200055909
    Scopus Count
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    Radiocarbon, Volume 51, Number 2 (2009)

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