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    The Younger Dryas Cold Event—Was it Synchronous Over the North Atlantic Region?

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    Author
    Goślar, Tomasz
    Arnold, Maurice
    Pazdur, Mieczysław F.
    Issue Date
    1995-01-01
    Keywords
    climate
    Lake Holzmaar
    Lake Soppensee
    Poland
    Lake Gościąż
    lacustrine environment
    Arctic region
    Greenland
    ice cores
    planar bedding structures
    sedimentary structures
    varves
    upper Weichselian
    Weichselian
    Younger Dryas
    Atlantic Ocean
    North Atlantic
    Germany
    Central Europe
    Pleistocene
    upper Pleistocene
    time scales
    Europe
    sediments
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    absolute age
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    Citation
    Goślar, T., Arnold, M., & Pazdur, M. F. (1995). The Younger Dryas cold event—was it synchronous over the North Atlantic region?. Radiocarbon 37(1), 63-70.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/653484
    DOI
    10.1017/S003382220001479X
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Determined independently from annually laminated ice cores and lake sediments, and German pines, the calendar ages of Younger Dryas (YD) boundaries significantly disagree with one another. 14C dates, plotted vs. Calendar ages for samples from different sediments, also reveal distinct offsets. The adjustment of varve chronologies to synchronize the boundaries of the YD nearly cancels the discrepancies between 14C data, and supports the synchronism of the YD cold period over the North Atlantic region. However, the exact timing of the event cannot be estimated in this way.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S003382220001479X
    Scopus Count
    Collections
    Radiocarbon, Volume 37, Number 1 (1995)

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