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MJB/EJL
Why is there a difference? Atmospheric carbon can vary from year to year, altering the amount of carbon living things absorb. Even when archeologists adjust their dates to allow for these fluctuations, their calibration programs may differ. In general, the further back in time we go the greater the difference between these scales. Radiocarbon time becomes increasingly too young, or recent, by two thousand or more years during the Paleoindian era. This has profound consequences for our interpretation of the archaeological record. What does the future hold? Increasingly sound calibrations
are being developed which link these two time scales well back in time.
Calendar years, however, should be used whenever possible in interpretations
and analyses. This is because the two time scales are not yet linked,
and there are plateaus, jumps, and reversals in the radiocarbon time
scale at various times in the past.
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