Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry

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

Bibliographic Details
Main Authors: Peck, V.L., Yu, Jimin, Kender, S., Riesselman, C.R.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2015
Subjects:
Antarc*
Antarctica
Online Access:http://hdl.handle.net/1885/65281
Description
Summary: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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