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      Early Agricultural Diet in Eastern North America: Evidence from Two Kentucky Rockshelters

      American Antiquity
      JSTOR

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          Abstract

          Systematic quantitative analysis of desiccated human paleofeces from two rockshelters in eastern Kentucky has yielded new evidence for early agricultural diet in eastern North America. Results indicate that native cultigens (including sumpweed, sunflower, and chenopod) were sometimes significant dietary constituents as early as ca. 1000 B.C., at least a millennium before agricultural economies became widespread across the region. However, variability in the quantity and frequency of cultigen remains suggests a dietary role that was somewhat limited compared to the practices of later Woodland period farmers. The predictions of foraging theory suggest that the utilization of cultigens would have been most advantageous in spring and summer (when many other foods were scarce) or in years of poor production by nut-bearing trees. The causal link between food storage and the development of food production in eastern Kentucky receives some empirical support and warrants further investigation.

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          Origins of agriculture in eastern north america.

          As a result of research carried out over the past decade, eastern North America now provides one of the most detailed records of the origins of agriculture available. Spanning a filll three millennia, the transition from forager to farmer in eastern North America involved the domestication of four North American seed plants during the second millennium B.C., the initial emergence of food production economies based on local crop plants between 250 B.C. and A.D. 200, and the rapid and broad-scale shift to maize-centered agriculture during the three centuries from A.D. 800 to 1100.
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            High-Precision Bidecadal Calibration of the Radiocarbon Time Scale, 500–2500 BC

            The sole purpose of this paper is to present a previously published14C data set to which minor corrections have been applied. All basic information previously given is still applicable (Pearson & Stuiver 1986). The corrections are needed because14C count-rate influences (radon decay in Seattle, a re-evaluation of the corrections applied for efficiency variation with time previously unrecognized in Belfast) had to be accounted for in more detail. Information on the radon correction is given in Stuiver and Becker (1993). The Belfast corrections were necessary because the original correction for efficiency variations with time was calculated using two suspect standards (these were shown to be suspect by recent observations) that overweighted the correction. A re-evaluation (Pearson & Qua 1993) now shows it to be almost insignificant, and the corrected dates (using the new correction) became older by about 16 years.
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              Multiple pathways to farming in precontact eastern North America

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                Author and article information

                Journal
                applab
                American Antiquity
                American Antiquity
                JSTOR
                0002-7316
                July 1996
                January 2017
                : 61
                : 03
                : 520-536
                Article
                10.2307/281838
                eb2f1e66-6605-4142-b186-0cc0636fe035
                © 1996
                History

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