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    Marine04 Marine Radiocarbon Age Calibration, 0-26 cal kyr BP

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    Author
    Hughen, Konrad A.
    Baillie, Mike G. L.
    Bard, Edouard
    Beck, J. Warren
    Bertrand, Chanda J. H.
    Blackwell, Paul G.
    Buck, Caitlin E.
    Burr, George S.
    Cutler, Kirsten B.
    Damon, Paul E.
    Edwards, Richard L.
    Fairbanks, Richard G.
    Friedrich, Michael
    Guilderson, Thomas P.
    Kromer, Bernd
    McCormac, Gerry
    Manning, Sturt
    Bronk Ramsey, Christopher
    Reimer, Paula J.
    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
    Anthozoa
    Atlantic Ocean
    C 14
    calibration
    carbon
    Cariaco Basin
    Caribbean Sea
    Cenozoic
    Coelenterata
    corrections
    dates
    geochronology
    Invertebrata
    isotopes
    marine sediments
    models
    North Atlantic
    planar bedding structures
    Quaternary
    radioactive isotopes
    sedimentary structures
    sediments
    Th U
    tree rings
    uncertainty
    upper Quaternary
    varves
    Show allShow less
    
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    Show full item record
    Citation
    Hughen, K. A., Baillie, M. G., Bard, E., Beck, J. W., Bertrand, C. J. H., Blackwell, P. G., ... & Weyhenmeyer, C. E. (2004). Marine04 marine radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon, 46(3), 1059-1086.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    IntCal04: Calibration Issue, 2004.
    URI
    http://hdl.handle.net/10150/654843
    DOI
    10.1017/S0033822200033002
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    New radiocarbon calibration curves, IntCal04 and Marine04, have been constructed and internationally ratified to replace the terrestrial and marine components of IntCal98. The new calibration data sets extend an additional 2000 yr, from 0-26 cal kyr BP (Before Present, 0 cal BP = AD 1950), and provide much higher resolution, greater precision, and more detailed structure than IntCal98. For the Marine04 curve, dendrochronologically-dated tree-ring samples, converted with a box diffusion model to marine mixed-layer ages, cover the period from 0-10.5 cal kyr BP. Beyond 10.5 cal kyr BP, high-resolution marine data become available from foraminifera in varved sediments and U/Th-dated corals. The marine records are corrected with site-specific 14C reservoir age information to provide a single global marine mixed-layer calibration from 10.5-26.0 cal kyr BP. A substantial enhancement relative to IntCal98 is the introduction of 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 marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed here. The tree-ring data sets, sources of uncertainty, and regional offsets are presented in detail in a companion paper by Reimer et al. (this issue).
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200033002
    Scopus Count
    Collections
    Radiocarbon, Volume 46, Number 3 (2004)

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