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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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 |
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/65281 2024-01-14T10:02:26+01:00 Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry Peck, V.L. Yu, Jimin Kender, S. Riesselman, C.R. 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 unknown American Geophysical Union 0883-8305 http://hdl.handle.net/1885/65281 doi: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 Paleoceanography Keywords: benthic foraminifera carbonate deep sea Eocene-Oligocene boundary hypothesis testing ice sheet isotopic ratio Last Glacial Maximum thermocline water temperature Antarctica Foraminifera Journal article ftanucanberra https://doi.org/10.1029/2009PA001906 2023-12-15T09:32:57Z 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 Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Australian National University: ANU Digital Collections Paleoceanography 25 4 n/a n/a |
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Open Polar |
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Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
topic |
Keywords: benthic foraminifera carbonate deep sea Eocene-Oligocene boundary hypothesis testing ice sheet isotopic ratio Last Glacial Maximum thermocline water temperature Antarctica Foraminifera |
spellingShingle |
Keywords: benthic foraminifera carbonate deep sea Eocene-Oligocene boundary hypothesis testing ice sheet isotopic ratio Last Glacial Maximum thermocline water temperature Antarctica Foraminifera Peck, V.L. Yu, Jimin Kender, S. Riesselman, C.R. Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
topic_facet |
Keywords: benthic foraminifera carbonate deep sea Eocene-Oligocene boundary hypothesis testing ice sheet isotopic ratio Last Glacial Maximum thermocline water temperature Antarctica Foraminifera |
description |
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 |
format |
Article in Journal/Newspaper |
author |
Peck, V.L. Yu, Jimin Kender, S. Riesselman, C.R. |
author_facet |
Peck, V.L. Yu, Jimin Kender, S. Riesselman, C.R. |
author_sort |
Peck, V.L. |
title |
Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
title_short |
Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
title_full |
Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
title_fullStr |
Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
title_full_unstemmed |
Shifting ocean carbonate chemistry during the Eocene-Oligocene climate transition: Implications for deep-ocean Mg/Ca paleothermometry |
title_sort |
shifting ocean carbonate chemistry during the eocene-oligocene climate transition: implications for deep-ocean mg/ca paleothermometry |
publisher |
American Geophysical Union |
url |
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 |
genre |
Antarc* Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctica Ice Sheet |
op_source |
Paleoceanography |
op_relation |
0883-8305 http://hdl.handle.net/1885/65281 doi: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 |
op_doi |
https://doi.org/10.1029/2009PA001906 |
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Paleoceanography |
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25 |
container_issue |
4 |
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n/a |
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1788057455376203776 |