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    A Fresh Water Diet-Derived 14C Reservoir Effect at the Stone Age Sites in the Iron Gates Gorge

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    Author
    Cook, Gordon T.
    Bonsall, C.
    Hedges, Robert E. M.
    McSweeney, K.
    Boronean, V.
    Pettitt, Paul B.
    Issue Date
    2001-01-01
    Keywords
    Danube Valley
    Iron Gates Gorge
    Romania
    Schela Cladovei archaeological site
    Ungulata
    fresh water environment
    Mesolithic
    nitrogen
    N 15 N 14
    Neolithic
    Stone Age
    Hominidae
    Homo
    Primates
    artifacts
    diet
    calibration
    Theria
    Eutheria
    collagen
    Southern Europe
    Mammalia
    archaeology
    isotope ratios
    Holocene
    Chordata
    Tetrapoda
    Vertebrata
    proteins
    organic compounds
    Europe
    bones
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    stable isotopes
    absolute age
    geochemistry
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    Citation
    Cook, G. T., Bonsall, C., Hedges, R. E. M., McSweeney, K., Boronean, V., & Pettitt, P. B. (2001). A freshwater diet-derived 14C reservoir effect at the Stone Age sites in the Iron Gates gorge. Radiocarbon, 43(2A), 453-460.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    Description
    From the 17th International Radiocarbon Conference held in Jerusalem, Israel, June 18-23, 2000.
    URI
    http://hdl.handle.net/10150/654412
    DOI
    10.1017/S0033822200038327
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Human bones from single inhumation burials and artifacts made from terrestrial mammal (ungulate) bone found in direct association with the skeletons were obtained from the Stone Age site of Schela Cladovei situated just below the Iron Gates Gorge of the River Danube. The results of stable isotope analyses of the human bone collagen are consistent with a heavy dependence on aquatic protein while radiocarbon dating of the samples reveals an offset of 300-500 years between the two sample types, indicating a freshwater reservoir effect in the human bone samples. Since protein consumption is by far the major source of nitrogen in the human diet we have assumed a linear relationship between delta-15N and the level of aquatic protein in each individual's diet and derived a calibration for 14C age offset versus delta-15N which has been applied to a series of results from the site at Lepenski Vir within the gorge. The corrected 14C ages (7310-6720 BP) are now consistent with the previous 14C age measurements made on charcoal from related contexts (7360-6560 BP). In addition, the data indicate a change from a primarily aquatic to a mixed terrestrial/aquatic diet around 7100 BP and this may be argued as supporting a shift from Mesolithic to Neolithic. This study also has wider implications for the accurate dating of human bone samples when the possibility exists of an aquatic component in the dietary protein and strongly implies that delta-15N analysis should be undertaken routinely when dating human bones.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200038327
    Scopus Count
    Collections
    Radiocarbon, Volume 43, Number 2A (2001

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