Publications
View AllThe IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
ABSTRACT Radiocarbon ( 14 C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age eq...
IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP
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 extende...
Radiocarbon calibration beyond 20,000 <sup>14</sup>C yr B.P. by means of planktonic foraminifera of the Iberian Margin
We present a new set of 14 C ages obtained by accelerator mass spectrometry (AMS) on planktonic foraminifera from a deep-sea core collected off the Iberian Margin (MD952042). Th...
Elastic Tie-Pointing—Transferring Chronologies between Records via a Gaussian Process
We consider a general methodology for the transferral of chronologies from a master reference record containing direct dating information to an undated record of interest that d...
Comparison of <sup>14</sup>C and U-Th Ages in Corals from IODP #310 Cores Offshore Tahiti
Shallow-water tropical corals can be used to calibrate the radiocarbon timescale. In this paper, we present a new data set based on the comparison between 14 C ages and U-Th age...
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- https://ror.org/04ex24z53