Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean
Ocean sector of the Southern Ocean represents only the second complete, expanded sequence through the Paleocene/Eocene Thermal Maximum (PETM; ~55 Ma) recovered from Antarctic waters. Calcareous nannoplankton at this site underwent an abrupt, fundamental turnover across the PETM as defined by a carbo...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.490.3967 2023-05-15T13:45:37+02:00 Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean Shijun Jiang Sherwood W. Wise The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.3967 http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.3967 http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf text ftciteseerx 2016-01-08T08:28:46Z Ocean sector of the Southern Ocean represents only the second complete, expanded sequence through the Paleocene/Eocene Thermal Maximum (PETM; ~55 Ma) recovered from Antarctic waters. Calcareous nannoplankton at this site underwent an abrupt, fundamental turnover across the PETM as defined by a carbon isotope excursion. Although Chiasmolithus, Discoaster, and Fasciculithus exponentially increase in abundance at the onset, the former abruptly drops but then rapidly recovers, whereas the latter two taxa show opposite trends due to surface-water oligotrophy. These observations confirm previous results from ODP Site 690 on Maud Rise. The elevated pCO2 that accompanied the PETM caused a shoaling of the lysocline and carbonate compensation depth, leading to intensive dissolution of susceptible holococcoliths and poor preservation of the assemblages. Similarities and contrasts between the results of this study and previous work from open-ocean sites and shelf margins further demonstrate that the response to the PETM was consistent in open-ocean environments, but could be localized on continental shelves where nutrient regimes depend on the local geologic setting and oceanographic conditions. Citation: Jiang, S., and S.W. Wise (2007), Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean, in Antarctica: A Keystone in a Changing Text Antarc* Antarctic Antarctica Southern Ocean Unknown Antarctic Indian Kerguelen Maud Rise ENVELOPE(3.000,3.000,-66.000,-66.000) Southern Ocean |
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Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
Ocean sector of the Southern Ocean represents only the second complete, expanded sequence through the Paleocene/Eocene Thermal Maximum (PETM; ~55 Ma) recovered from Antarctic waters. Calcareous nannoplankton at this site underwent an abrupt, fundamental turnover across the PETM as defined by a carbon isotope excursion. Although Chiasmolithus, Discoaster, and Fasciculithus exponentially increase in abundance at the onset, the former abruptly drops but then rapidly recovers, whereas the latter two taxa show opposite trends due to surface-water oligotrophy. These observations confirm previous results from ODP Site 690 on Maud Rise. The elevated pCO2 that accompanied the PETM caused a shoaling of the lysocline and carbonate compensation depth, leading to intensive dissolution of susceptible holococcoliths and poor preservation of the assemblages. Similarities and contrasts between the results of this study and previous work from open-ocean sites and shelf margins further demonstrate that the response to the PETM was consistent in open-ocean environments, but could be localized on continental shelves where nutrient regimes depend on the local geologic setting and oceanographic conditions. Citation: Jiang, S., and S.W. Wise (2007), Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean, in Antarctica: A Keystone in a Changing |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Shijun Jiang Sherwood W. Wise |
spellingShingle |
Shijun Jiang Sherwood W. Wise Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
author_facet |
Shijun Jiang Sherwood W. Wise |
author_sort |
Shijun Jiang |
title |
Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
title_short |
Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
title_full |
Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
title_fullStr |
Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
title_full_unstemmed |
Abrupt turnover in calcareous-nannoplankton assemblages across the Paleocene/Eocene Thermal Maximum: implications for surface-water oligotrophy over the Kerguelen Plateau, Southern Indian Ocean |
title_sort |
abrupt turnover in calcareous-nannoplankton assemblages across the paleocene/eocene thermal maximum: implications for surface-water oligotrophy over the kerguelen plateau, southern indian ocean |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.3967 http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf |
long_lat |
ENVELOPE(3.000,3.000,-66.000,-66.000) |
geographic |
Antarctic Indian Kerguelen Maud Rise Southern Ocean |
geographic_facet |
Antarctic Indian Kerguelen Maud Rise Southern Ocean |
genre |
Antarc* Antarctic Antarctica Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Southern Ocean |
op_source |
http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.490.3967 http://pubs.usgs.gov/of/2007/1047/srp/srp024/of2007-1047srp024.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766228633806962688 |