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    The Climate History of the Eastern Mediterranean as Recorded in Mollusk Shells

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    Author
    Kaufman, Aaron
    Magaritz, Mordeckai
    Issue Date
    1980-01-01
    Keywords
    eastern Mediterranean region
    history
    ratios
    O 18 O 16
    oxygen
    Mediterranean region
    Holocene
    biostratigraphy
    stratigraphy
    paleoclimatology
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    shells
    Invertebrata
    Mollusca
    stable isotopes
    absolute age
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    Citation
    Kaufman, A., & Magaritz, M. (1980). The climatic history of the eastern Mediterranean as recorded in mollusk shells. Radiocarbon, 22(3), 778-781.
    Publisher
    American Journal of Science
    Journal
    Radiocarbon
    Description
    From the 10th International Radiocarbon Conference held in Bern, Switzerland and Heidelberg, Germany, August 19-26, 1979.
    URI
    http://hdl.handle.net/10150/652498
    DOI
    10.1017/S0033822200010158
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    An 18O/16O versus 14C age curve was constructed for unrecrystallized Holocene marine shell samples from Israel that were shown to be homogeneous populations. The surprisingly large variation in the oxygen isotopic composition (1.2 per mil) between 2600 and 4000 years ago is most probably due to variations in the isotopic composition of the water. This implies that either the excess of evaporation over precipitation or the Nile river discharge must have varied significantly during the Holocene.
    Type
    Proceedings
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200010158
    Scopus Count
    Collections
    Radiocarbon, Volume 22, Number 3 (1980)

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