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• W2162224891 endingPage "1125" @default.
• W2162224891 startingPage "1122" @default.
• W2162224891 abstract "The difference in carbon-13 ((13)C) contents of hopane and sterane biomarkers in the Monterey formation (Naples Beach, California) parallels the Miocene inorganic record of the change in (18)O (delta(18)O), reflecting the Miocene evolution from a well-mixed to a highly stratified photic zone (upper 100 meters) in the Pacific. Steranes (delta(13)C = 25.4 +/- 0.7 per mil versus the Pee Dee belemnite standard) from shallow photic-zone organisms do not change isotopically throughout the Miocene. In contrast, sulfur-bound C(35) hopanes (likely derived from bacterial plankton living at the base of the photic zone) have systematically decreasing (13)C concentrations in Middle and Late Miocene samples (delta(13)C = -29.5 to -31.5 per mil), consistent with the Middle Miocene formation of a carbon dioxide-rich cold water mass at the base of the photic zone." @default.
• W2162224891 created "2016-06-24" @default.
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• W2162224891 date "1994-02-25" @default.
• W2162224891 modified "2023-10-14" @default.
• W2162224891 title "A Molecular Organic Carbon Isotope Record of Miocene Climate Changes" @default.
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• W2162224891 doi "https://doi.org/10.1126/science.263.5150.1122" @default.
• W2162224891 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/17831625" @default.
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