Fluctuating radiocarbon offsets observed in the southern Levant and implications for archaeological chronology debates.
basic_science · Level V
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- Record sourced from PubMed, PMID 29844183.
- Also identified by DOI 10.1073/pnas.1719420115 and PMC identifier 6004441.
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Abstract
Considerable work has gone into developing high-precision radiocarbon (<sup>14</sup>C) chronologies for the southern Levant region during the Late Bronze to Iron Age/early Biblical periods (∼1200-600 BC), but there has been little consideration whether the current standard Northern Hemisphere <sup>14</sup>C calibration curve (IntCal13) is appropriate for this region. We measured <sup>14</sup>C ages of calendar-dated tree rings from AD 1610 to 1940 from southern Jordan to investigate contemporary <sup>14</sup>C levels and to compare these with IntCal13. Our data reveal an average offset of ∼19 <sup>14</sup>C years, but, more interestingly, this offset seems to vary in importance through time. While relatively small, such an offset has substantial relevance to high-resolution <sup>14</sup>C chronologies for the southern Levant, both archaeological and paleoenvironmental. For example, reconsidering two published studies, we find differences, on average, of 60% between the 95.4% probability ranges determined from IntCal13 versus those approximately allowing for the observed offset pattern. Such differences affect, and even potentially undermine, several current archaeological and historical positions and controversies.