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    IntCal04 Terrestrial Radiocarbon Age Calibration, 0-26 cal kyr BP

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    Author
    Reimer, Paula J.
    Baillie, Mike G. L.
    Bard, Edouard
    Bayliss, Alex
    Beck, J. Warren
    Bertrand, Chanda J. H.
    Blackwell, Paul G.
    Buck, Caitlin E.
    Burr, George S.
    Cutler, Kirsten B.
    Damon, Paul E.
    Edwards, R. Lawrence
    Fairbanks, Richard G.
    Friedrich, Michael
    Guilderson, Thomas P.
    Hogg, Alan G.
    Hughen, Konrad A.
    Kromer, Bernd
    McCormac, Gerry
    Manning, Sturt
    Bronk Ramsey, Christopher
    Reimer, Ron W.
    Remmele, Sabine
    Southon, John R.
    Stuiver, Minze
    Talamo, Sahra
    Taylor, F. W.
    van der Plicht, Johannes
    Weyhenmeyer, Constanze E.
    Show allShow less
    Issue Date
    2004-01-01
    Keywords
    absolute age
    C 14
    calibration
    carbon
    Cenozoic
    corrections
    dates
    errors
    geochronology
    isotopes
    Northern Hemisphere
    Quaternary
    radioactive isotopes
    tree rings
    uncertainty
    upper Quaternary
    Show allShow less
    
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    Citation
    Reimer, P. J., Baillie, M. G. L., Bard, E., Bayliss, A., Beck, J. W., Bertrand, C. J. H., ... & Weyhenmeyer, C. E. (2004). IntCal04 terrestrial radiocarbon age calibration, 0-26 cal kyr BP. Radiocarbon, 46(3), 1029-1058.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    IntCal04: Calibration Issue, 2004.
    URI
    http://hdl.handle.net/10150/654820
    DOI
    10.1017/S0033822200032999
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0-24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0-26 cal kyr BP, but with much higher resolution beyond 11.4 cal kyr BP than IntCal98. Dendrochronologically-dated tree-ring samples cover the period from 0-12.4 cal kyr BP. Beyond the end of the tree rings, data from marine records (corals and foraminifera) are converted to the atmospheric equivalent with a site-specific marine reservoir correction to provide terrestrial calibration from 12.4-26.0 cal kyr BP. A substantial enhancement relative to IntCal98 is the introduction of a coherent statistical approach based on a random walk model, which takes into account the uncertainty in both the calendar age and the 14C age to calculate the underlying calibration curve (Buck and Blackwell, this issue). The tree-ring data sets, sources of uncertainty, and regional offsets are discussed here. The marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed in brief, but details are presented in Hughen et al. (this issue a). We do not make a recommendation for calibration beyond 26 cal kyr BP at this time; however, potential calibration data sets are compared in another paper (van der Plicht et al., this issue).
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200032999
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 3 (2004)

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