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    Late Glacial 14C Ages from a Floating, 1382-Ring Pine Chronology

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    Author
    Kromer, Bernd
    Friedrich, Michael
    Hughen, Konrad A.
    Kaiser, Felix
    Remmele, Sabine
    Schaub, Matthias
    Talamo, Sahra
    Issue Date
    2004-01-01
    Keywords
    absolute age
    Atlantic Ocean
    C 14
    calibration
    carbon
    Cariaco Basin
    Caribbean Sea
    Cenozoic
    Central Europe
    corrections
    Europe
    geochronology
    Germany
    isotopes
    marine sediments
    North Atlantic
    planar bedding structures
    Pleistocene
    Quaternary
    radioactive isotopes
    sedimentary structures
    sediments
    Switzerland
    tree rings
    upper Pleistocene
    varves
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    Citation
    Kromer, B., Friedrich, M., Hughen, K. A., Kaiser, F., Remmele, S., Schaub, M., & Talamo, S. (2004). Late glacial 14C ages from a floating, 1382-ring pine chronology. Radiocarbon, 46(3), 1203-1209.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    IntCal04: Calibration Issue, 2004.
    URI
    http://hdl.handle.net/10150/654831
    DOI
    10.1017/S0033822200033099
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We built a floating, 1382-ring pine chronology covering the radiocarbon age interval of 12,000 to 10,650 BP. Based on the strong rise of Delta-14C at the onset of the Younger Dryas (YD) and wiggle-matching of the decadal-scale Delta-14C fluctuations, we can anchor the floating chronology to the Cariaco varve chronology. We observe a marine reservoir correction higher than hitherto assumed for the Cariaco site, of up to 650 yr instead of 400 yr, for the full length of the comparison interval. The tree-ring Delta-14C shows several strong fluctuations of short duration (a few decades) at 13,800, 13,600, and 13,350 cal BP. The amplitude of the strong Delta-14C rise at the onset of the YD is about 40 ppm, whereas in the marine data set the signal appears stronger due to a re-adjustment of the marine mixed-layer Delta-14C towards the atmospheric level.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200033099
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 3 (2004)

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