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.
Issue Date
2004-01-01Keywords
absolute ageAnthozoa
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
Metadata
Show full item recordCitation
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.Journal
RadiocarbonDescription
IntCal04: Calibration Issue, 2004.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
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200033002