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 C-14 a
ge-cal age information, produced by many laboratories, is converted to Delt
a(14)C profiles and calibration curves, for the atmosphere as well as the o
ceans. We discuss offsets in measured C-14 ages and the errors therein, reg
ional C-14 age differences, tree-coral C-14 age comparisons and the time de
pendence of marine reservoir ages, and evaluate decadal vs. single-year C-1
4 results. Changes in oceanic deepwater circulation, especially for the 16,
000-11,000 cal sp interval, are reflected in the Delta(14)C values of INTCA
L98.