We establish a precision accelerator mass spectrometry (AMS) radiocarbon chronology for the Archaic period Tlacuachero shellmound (Chiapas, Mexico) within a Bayesian statistical framework. Carbonized twig samples were sequentially selected from well-defined stratigraphic contexts based on iterative improvements to a probabilistic chronological model. Analytical error for these measurements is ±15 to 20 14C yr. This greater precision and the absence of stratigraphic reversals eclipses previous 14C work at the site. Based on this, we establish a chronological framework for a sequence of 3 clay floors dating to between 4930 and 4270 cal BP and determine that the bedded shell deposits that formed the mound accumulated rapidly during 2 episodes: a lower 2-m section below the floors that accumulated over a 0-150 cal yr period at 5050-4875 cal BP and, an upper 3.5-m section above the floors that accumulated over a 0-80 cal yr period at 4380-4230 cal BP. © 2011 by the Arizona Board of Regents on behalf of the University of Arizona.
CITATION STYLE
Kennett, D. J., Culleton, B. J., Voorhies, B., & Southon, J. R. (2011). Bayesian analysis of high-precision ams 14C dates from a prehistoric Mexican shellmound. Radiocarbon, 53(2), 245–259. https://doi.org/10.1017/S0033822200056526
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