Reconstructing Pleistocene Climatic Change from the Oxygen Isotope Composition of Sediments: A Review
Keyword(s):
The isotope composition of ocean sediments is the chief data source for Pleistocene climatic changes. It is generally believed that the18O/16O ratio of a sample indicates the global total of glacial ice at the time the sample was deposited. This is roughly correct, but numerous complicating factors limit the accuracy of the isotope proxies.
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1980 ◽
Vol 22
(7)
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pp. 826-830
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2020 ◽
Vol 552
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pp. 109777
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2007 ◽
Vol 41
(6)
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pp. 1870-1876
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