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

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Date

2010

Authors

Peck, V.L.
Yu, Jimin
Kender, S.
Riesselman, C.R.

Journal Title

Journal ISSN

Volume Title

Publisher

American Geophysical Union

Abstract

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

Description

Keywords

Keywords: benthic foraminifera; carbonate; deep sea; Eocene-Oligocene boundary; hypothesis testing; ice sheet; isotopic ratio; Last Glacial Maximum; thermocline; water temperature; Antarctica; Foraminifera

Citation

URI

http://hdl.handle.net/1885/65281

Collections

ANU Research Publications

Source

Paleoceanography

Type

Journal article

Book Title

Entity type

Access Statement

License Rights

DOI

10.1029/2009PA001906

Restricted until

2037-12-31

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Description
01_Peck_Shifting_ocean_carbonate_2010.pdf (522.66 KB)

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