Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ...
A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios indicate that bottom waters warmed by 4° to 5°C, similar to tropical and subtropical surface ocean waters, implying no amplificati...
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Online Access: | https://dx.doi.org/10.1594/pangaea.738241 https://doi.pangaea.de/10.1594/PANGAEA.738241 |
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ftdatacite:10.1594/pangaea.738241 2024-09-15T18:18:40+00:00 Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... Tripati, Aradhna K Elderfield, Henry 2005 application/zip https://dx.doi.org/10.1594/pangaea.738241 https://doi.pangaea.de/10.1594/PANGAEA.738241 en eng PANGAEA https://dx.doi.org/10.1126/science.1109202 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg74 Leg143 Leg198 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2005 ftdatacite https://doi.org/10.1594/pangaea.73824110.1126/science.1109202 2024-09-02T08:37:33Z A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios indicate that bottom waters warmed by 4° to 5°C, similar to tropical and subtropical surface ocean waters, implying no amplification of warming in high-latitude regions of deep-water formation under ice-free conditions. Intermediate waters warmed before the carbon isotope excursion, in association with downwelling in the North Pacific and reduced Southern Ocean convection, supporting changing circulation as the trigger for methane hydrate release. A switch to deep convection in the North Pacific at the PETM onset could have amplified and sustained warming. ... : Supplement to: Tripati, Aradhna K; Elderfield, Henry (2005): Deep-sea temperature and circulation changes at the Paleocene-Eocene thermal maximum. Science, 308(5730), 1894-1898 ... Article in Journal/Newspaper Methane hydrate Southern Ocean DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg74 Leg143 Leg198 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg74 Leg143 Leg198 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Tripati, Aradhna K Elderfield, Henry Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
topic_facet |
Drilling/drill rig Leg74 Leg143 Leg198 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios indicate that bottom waters warmed by 4° to 5°C, similar to tropical and subtropical surface ocean waters, implying no amplification of warming in high-latitude regions of deep-water formation under ice-free conditions. Intermediate waters warmed before the carbon isotope excursion, in association with downwelling in the North Pacific and reduced Southern Ocean convection, supporting changing circulation as the trigger for methane hydrate release. A switch to deep convection in the North Pacific at the PETM onset could have amplified and sustained warming. ... : Supplement to: Tripati, Aradhna K; Elderfield, Henry (2005): Deep-sea temperature and circulation changes at the Paleocene-Eocene thermal maximum. Science, 308(5730), 1894-1898 ... |
format |
Article in Journal/Newspaper |
author |
Tripati, Aradhna K Elderfield, Henry |
author_facet |
Tripati, Aradhna K Elderfield, Henry |
author_sort |
Tripati, Aradhna K |
title |
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
title_short |
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
title_full |
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
title_fullStr |
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
title_full_unstemmed |
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum ... |
title_sort |
mg/ca and stable isotope record of benthic foraminifera of the paleocene-eocene thermal maximum ... |
publisher |
PANGAEA |
publishDate |
2005 |
url |
https://dx.doi.org/10.1594/pangaea.738241 https://doi.pangaea.de/10.1594/PANGAEA.738241 |
genre |
Methane hydrate Southern Ocean |
genre_facet |
Methane hydrate Southern Ocean |
op_relation |
https://dx.doi.org/10.1126/science.1109202 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.73824110.1126/science.1109202 |
_version_ |
1810456758705979392 |