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| | Radiocarbon Calibration |
 | | Of practical importance to a wide range of scientific disciplines is the radiocarbon calibration, which is used for converting radiocarbon ages to calendar years; essential for measuring time and rates of change for numerous scientific fields. |
 | | The tree ring atmospheric radiocarbon calibration data set spanning 0 to 12,410 years BP is superior to all other atmospheric radiocarbon calibration data due to the number and quality of the radiocarbon measurements and the accuracy and precision of the tree dendrochronology (Stuiver et al., 1998; Reimer et al., 2004). |
 | | From 14,000 to 26,000 years BP, 80% of the data in the IntCal04 were provided by our laboratory and we have subsequently doubled the amount of data in the 14,000 to 26,000 year BP time interval (Cao et al., 2006; Fairbanks et al., 2005; 2006). |
| radiocarbon.ldeo.columbia.edu /research/radiocarbon.htm (1950 words) |
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