Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry
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Peck, V.L.
Yu, Jimin
Kender, S.
Riesselman, C.R.
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American Geophysical Union
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To date, no conclusive evidence has been identified for intermediate or deep water cooling associated with the >1‰ benthic δ18O increase at the Eocene-Oligocene transition (EOT) when large permanent ice sheets first appeared on Antarctica. Interpretati
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Paleoceanography
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2037-12-31
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