Marine04 Marine Radiocarbon Age Calibration, 0–26 Cal Kyr Bp

Konrad A Hughen(Woods Hole Oceanographic Institution), Mike Baillie(Queen's University Belfast), Édouard Bard(Centre de Recherche et d’Enseignement de Géosciences de l’Environnement), J Warren Beck(University of Arizona), Chanda Bertrand(Woods Hole Oceanographic Institution), Paul G. Blackwell(University of Sheffield), Caitlin E. Buck(University of Sheffield), George S. Burr(University of Arizona), Kirsten Cutler, Paul E. Damon(University of Arizona), R. Lawrence Edwards(University of Minnesota), Richard G. Fairbanks(Lamont-Doherty Earth Observatory), Michael Friedrich(University of Hohenheim), T. P. Guilderson(Lawrence Livermore National Laboratory), Bernd Kromer(Heidelberg Academy of Sciences and Humanities), Gerry McCormac(Queen's University Belfast), Sturt W. Manning(University of Toronto), Christopher Bronk Ramsey, Paula Reimer(Queen's University Belfast), Ron Reimer(University of California, Santa Cruz), Sabine Remmele(University of Hohenheim), John Southon(University of California, Irvine), Minze Stuiver(University of Washington), Sahra Talamo(Heidelberg Academy of Sciences and Humanities), Frederick W. Taylor(University of Texas Institute for Geophysics), J. van der Plicht(Leiden University), Constanze E. Weyhenmeyer(Lawrence Livermore National Laboratory)
Radiocarbon
January 1, 2004
Cited by 1,206Open Access
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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 14 C 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 14 C 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).


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