Changes in the Isotopic Composition of East Mediterranean Seawater during the Holocene (original) (raw)
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- Published: 01 June 1973
Nature volume 243, pages 462–464 (1973)Cite this article
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Abstract
WHEN molluscs secrete their shells, the _δ_18O in the shell is a function only of the temperature and of the _δ_18O in the water1–4. Thus one can compute the temperature at which an ancient shell was formed by measuring its _δ_18O value if one assumes that of the water in which it grew. For Pleistocene samples there has been a heated discussion as to the degree of change in the _δ_18O of the sea5–7.
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Authors and Affiliations
- Isotope Department, The Weizmann Institute of Science, Rehovot
MORDECHAI MAGARITZ & AARON KAUFMAN
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- MORDECHAI MAGARITZ
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MAGARITZ, M., KAUFMAN, A. Changes in the Isotopic Composition of East Mediterranean Seawater during the Holocene.Nature 243, 462–464 (1973). https://doi.org/10.1038/243462a0
- Received: 16 February 1973
- Published: 01 June 1973
- Issue Date: 22 June 1973
- DOI: https://doi.org/10.1038/243462a0