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
Published in: | Paleoceanography |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/65281 https://doi.org/10.1029/2009PA001906 https://openresearch-repository.anu.edu.au/bitstream/1885/65281/5/Yu_J_2010_Shifting_ocean.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65281/7/01_Peck_Shifting_ocean_carbonate_2010.pdf.jpg |
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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