TY - JOUR
T1 - Intcal09 and Marine09 Radiocarbon Age Calibration Curves, 0-50,000 Years Cal Bp Rid F-4952-2011 Rid B-7298-2008
JF - Radiocarbon
Y1 - 2009
A1 - Reimer, P. J.
A1 - Baillie, M. G. L.
A1 - Bard, E.
A1 - Bayliss, A.
A1 - Beck, J. W.
A1 - Blackwell, P. G.
A1 - Ramsey, C. Bronk
A1 - Buck, C. E.
A1 - Burr, G. S.
A1 - Edwards, R. L.
A1 - Friedrich, M.
A1 - Grootes, P. M.
A1 - Guilderson, T. P.
A1 - Hajdas, I.
A1 - Heaton, T. J.
A1 - Hogg, A. G.
A1 - Hughen, K. A.
A1 - Kaiser, K. F.
A1 - Kromer, B.
A1 - McCormac, F. G.
A1 - Manning, S. W.
A1 - Reimer, R. W.
A1 - Richards, D. A.
A1 - Southon, J. R.
A1 - Talamo, S.
A1 - Turney, C. S. M.
A1 - van der Plicht, J.
A1 - Weyhenmeye, C. E.
AB - The IntCal04 and Marine04 radiocarbon calibration curves have been updated from 12 cal kBP (cal kBP is here defined as thousands of calibrated years before AD 1950), and extended to 50 cal kBP, utilizing newly available data sets that meet the IntCal Working Group criteria for pristine corals and other carbonates and for quantification of uncertainty in both the (14)C and calendar timescales as established in 2002. No change was made to the curves from 0-12 cal kBP. The curves were constructed using a Markov chain Monte Carlo (MCMC) implementation of the random walk model used for IntCal04 and Marine04. The new curves were ratified at the 20th International Radiocarbon Conference in June 2009 and; ire available in the Supplemental Material at www.radiocarbon.org.
VL - 51
SN - 0033-8222
IS - 4
N1 - id: 1983; PT: J; UT: WOS:000274407500002
ER -
TY - JOUR
T1 - High-precision radiocarbon age calibration for terrestrial and marine samples
JF - Radiocarbon
Y1 - 1998
A1 - Stuiver, M.
A1 - Reimer, P. J.
A1 - Braziunas, T. F.
KW - ad 1950-500 bc
KW - c-14 data
KW - decadal calibration
KW - reservoir ages
KW - time scale
AB - Single-year and decadal radiocarbon tree-ring ages are tabulated and discussed in terms of C-14 age calibration. The single-year data form the basis of a detailed 14C age calibration curve for the cal AD 1510-1954 interval ("cal" denotes calibrated). The Seattle decadal data set (back to 11,617 cal sp, with 0 sp = AD 1950) is a component of the integrated decadal INTCAL98 C-14 age curve (Stuiver et al. 1998). Atmospheric C-14 ages can be transformed into C-14 ages of the global ocean using a carbon reservoir model. INTCAL98 C-14 ages, used for these calculations, yield global ocean C-14 ages differing slightly from previously published ones (Stuiver and Braziunas 1993b). We include discussions of offsets, error multipliers, regional C-14 age differences and marine C-14 age response to oceanic and atmospheric forcing.
VL - 40
SN - 0033-8222
IS - 3
N1 - 155qrTimes Cited:705
Cited References Count:31
JO - Radiocarbon
ER -
TY - JOUR
T1 - Large-volume WOCE radiocarbon sampling in the Pacific Ocean
JF - Radiocarbon
Y1 - 1996
A1 - Stuiver, M.
A1 - Ostlund, H. G.
A1 - Key, R. M.
A1 - Reimer, P. J.
KW - geosecs
AB - At the University of Miami Tritium Laboratory and the University of Washington Quaternary Isotope Laboratory, more than 1000 large-volume Pacific Ocean radiocarbon samples were measured for the WOCE program. Here we present a comprehensive data set, and a brief discussion of our findings.
VL - 38
SN - 0033-8222
IS - 3
N1 - Xd080Times Cited:12
Cited References Count:8
JO - Radiocarbon
ER -