High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation
We obtained global sea-level (eustatic) estimates with a peak of ∼22 m higher than present for the Pliocene interval 2.7–3.2 Ma from backstripping in Virginia (United States), New Zealand, and Enewetak Atoll (north Pacific Ocean), benthic foraminiferal δ18O values, and Mg/Ca-δ18O estimates. Statisti...
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Geological Society of America
2012
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:49554 2023-05-15T13:38:47+02:00 High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation Miller, Kenneth G. Wright, James D. Browning, James V. Kulpecz, Andrew Kominz, Michelle Naish, Tim R. Cramer, Benjamin S. Rosenthal, Yair Peltier, W. Richard Sosdian, Sindia 2012 https://orca.cardiff.ac.uk/id/eprint/49554/ https://doi.org/10.1130/G32869.1 unknown Geological Society of America Miller, Kenneth G., Wright, James D., Browning, James V., Kulpecz, Andrew, Kominz, Michelle, Naish, Tim R., Cramer, Benjamin S., Rosenthal, Yair, Peltier, W. Richard and Sosdian, Sindia https://orca.cardiff.ac.uk/view/cardiffauthors/A185665E.html orcid:0000-0002-4599-5529 orcid:0000-0002-4599-5529 2012. High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation. Geology 40 (5) , pp. 407-410. 10.1130/G32869.1 https://doi.org/10.1130/G32869.1 doi:10.1130/G32869.1 GC Oceanography QE Geology Article PeerReviewed 2012 ftunivcardiff https://doi.org/10.1130/G32869.1 2022-10-27T22:36:30Z We obtained global sea-level (eustatic) estimates with a peak of ∼22 m higher than present for the Pliocene interval 2.7–3.2 Ma from backstripping in Virginia (United States), New Zealand, and Enewetak Atoll (north Pacific Ocean), benthic foraminiferal δ18O values, and Mg/Ca-δ18O estimates. Statistical analysis indicates that it is likely (68% confidence interval) that peak sea level was 22 ± 5 m higher than modern, and extremely likely (95%) that it was 22 ± 10 m higher than modern. Benthic foraminiferal δ18O values appear to require that the peak was <20–21 m. Our estimates imply loss of the equivalent of the Greenland and West Antarctic ice sheets, and some volume loss from the East Antarctic Ice Sheet, and address the long-standing controversy concerning the Pliocene stability of the East Antarctic Ice Sheet. Article in Journal/Newspaper Antarc* Antarctic Greenland Ice Sheet Cardiff University: ORCA (Online Research @ Cardiff) Antarctic East Antarctic Ice Sheet Greenland New Zealand Pacific Geology 40 5 407 410 |
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Open Polar |
collection |
Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
unknown |
topic |
GC Oceanography QE Geology |
spellingShingle |
GC Oceanography QE Geology Miller, Kenneth G. Wright, James D. Browning, James V. Kulpecz, Andrew Kominz, Michelle Naish, Tim R. Cramer, Benjamin S. Rosenthal, Yair Peltier, W. Richard Sosdian, Sindia High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
topic_facet |
GC Oceanography QE Geology |
description |
We obtained global sea-level (eustatic) estimates with a peak of ∼22 m higher than present for the Pliocene interval 2.7–3.2 Ma from backstripping in Virginia (United States), New Zealand, and Enewetak Atoll (north Pacific Ocean), benthic foraminiferal δ18O values, and Mg/Ca-δ18O estimates. Statistical analysis indicates that it is likely (68% confidence interval) that peak sea level was 22 ± 5 m higher than modern, and extremely likely (95%) that it was 22 ± 10 m higher than modern. Benthic foraminiferal δ18O values appear to require that the peak was <20–21 m. Our estimates imply loss of the equivalent of the Greenland and West Antarctic ice sheets, and some volume loss from the East Antarctic Ice Sheet, and address the long-standing controversy concerning the Pliocene stability of the East Antarctic Ice Sheet. |
format |
Article in Journal/Newspaper |
author |
Miller, Kenneth G. Wright, James D. Browning, James V. Kulpecz, Andrew Kominz, Michelle Naish, Tim R. Cramer, Benjamin S. Rosenthal, Yair Peltier, W. Richard Sosdian, Sindia |
author_facet |
Miller, Kenneth G. Wright, James D. Browning, James V. Kulpecz, Andrew Kominz, Michelle Naish, Tim R. Cramer, Benjamin S. Rosenthal, Yair Peltier, W. Richard Sosdian, Sindia |
author_sort |
Miller, Kenneth G. |
title |
High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
title_short |
High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
title_full |
High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
title_fullStr |
High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
title_full_unstemmed |
High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation |
title_sort |
high tide of the warm pliocene: implications of global sea level for antarctic deglaciation |
publisher |
Geological Society of America |
publishDate |
2012 |
url |
https://orca.cardiff.ac.uk/id/eprint/49554/ https://doi.org/10.1130/G32869.1 |
geographic |
Antarctic East Antarctic Ice Sheet Greenland New Zealand Pacific |
geographic_facet |
Antarctic East Antarctic Ice Sheet Greenland New Zealand Pacific |
genre |
Antarc* Antarctic Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic Greenland Ice Sheet |
op_relation |
Miller, Kenneth G., Wright, James D., Browning, James V., Kulpecz, Andrew, Kominz, Michelle, Naish, Tim R., Cramer, Benjamin S., Rosenthal, Yair, Peltier, W. Richard and Sosdian, Sindia https://orca.cardiff.ac.uk/view/cardiffauthors/A185665E.html orcid:0000-0002-4599-5529 orcid:0000-0002-4599-5529 2012. High tide of the warm Pliocene: implications of global sea level for Antarctic deglaciation. Geology 40 (5) , pp. 407-410. 10.1130/G32869.1 https://doi.org/10.1130/G32869.1 doi:10.1130/G32869.1 |
op_doi |
https://doi.org/10.1130/G32869.1 |
container_title |
Geology |
container_volume |
40 |
container_issue |
5 |
container_start_page |
407 |
op_container_end_page |
410 |
_version_ |
1766111072700334080 |