Author
Stuiver, MinzeReimer, Paula J.
Bard, Edouard
Beck, J. Warren
Burr, G. S.
Hughen, Konrad A.
Kromer, Bernd
McCormac, Gerry
van der Plicht, Johannes
Spurk, Marco
Issue Date
1998-01-01Keywords
INTCAL98 Programprograms
ocean circulation
Th U
Anthozoa
Coelenterata
calibration
marine sediments
errors
atmosphere
tree rings
Pleistocene
sediments
Cenozoic
Quaternary
C 14
carbon
dates
isotopes
radioactive isotopes
Invertebrata
absolute age
Metadata
Show full item recordCitation
Stuiver, M., Reimer, P. J., Bard, E., Beck, J. W., Burr, G. S., Hughen, K. A., ... & Spurk, M. (1998). INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon, 40(3), 1041-1083.Journal
RadiocarbonDescription
INTCAL 98: Calibration Issue.Additional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
The focus of this paper is the conversion of radiocarbon ages to calibrated (cal) ages for the interval 24,000-0 cal BP (Before Present, 0 cal BP = AD 1950), based upon a sample set of dendrochronologically dated tree rings, uranium-thorium dated corals, and varve-counted marine sediment. The 14C age-cal age information, produced by many laboratories, is converted to 14C profiles and calibration curves, for the atmosphere as well as the oceans. We discuss offsets in measured 14C ages and the errors therein, regional 14C age differences, tree-coral 14C age comparisons and the time dependence of marine reservoir ages, and evaluate decadal vs. Single-year 14C results. Changes in oceanic deepwater circulation, especially for the 16,000-11,000 cal BP interval, are reflected in the Δ14C values of INTCAL98.Type
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200019123