Age model and stable isotope record of DSDP holes 48-401 and 86-577 ...
Early Paleogene warm climates may have been linked to different modes and sources of deepwater formation. Warm polar temperatures of the Paleocene and Eocene may have resulted from either increased atmospheric trace gases or increased heat transport through deep and intermediate waters. The possibil...
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ftdatacite:10.1594/pangaea.728114 2024-09-15T18:23:32+00:00 Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... Pak, Dorothy K Miller, Kenneth G 1992 application/zip https://dx.doi.org/10.1594/pangaea.728114 https://doi.pangaea.de/10.1594/PANGAEA.728114 en eng PANGAEA https://dx.doi.org/10.1029/92pa01234 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg48 Leg86 Leg113 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1992 ftdatacite https://doi.org/10.1594/pangaea.72811410.1029/92pa01234 2024-09-02T08:37:33Z Early Paleogene warm climates may have been linked to different modes and sources of deepwater formation. Warm polar temperatures of the Paleocene and Eocene may have resulted from either increased atmospheric trace gases or increased heat transport through deep and intermediate waters. The possibility of increasing ocean heat transport through the production of warm saline deep waters (WSDW) in the Tethyan region has generated considerable interest. In addition, General Circulation Model results indicate that deepwater source regions may be highly sensitive to changing basin configurations. To decipher deepwater changes, we examined detailed benthic foraminiferal faunal and isotopic records of the late Paleocene through the early Eocene (~60 to 50 Ma) from two critical regions: the North Atlantic (Bay of Biscay Site 401) and the Pacific (Shatsky Rise Site 577). These records are compared with published data from the Southern Ocean (Maud Rise Site 690, Islas Orcadas Rise Site 702). During the late Paleocene, ... : Supplement to: Pak, Dorothy K; Miller, Kenneth G (1992): Paleocene to Eocene benthic foraminiferal isotopes and assemblages: implications for deepwater circulation. Paleoceanography, 7(4), 405-422 ... Article in Journal/Newspaper North Atlantic Southern Ocean DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg48 Leg86 Leg113 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg48 Leg86 Leg113 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Pak, Dorothy K Miller, Kenneth G Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
topic_facet |
Drilling/drill rig Leg48 Leg86 Leg113 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
Early Paleogene warm climates may have been linked to different modes and sources of deepwater formation. Warm polar temperatures of the Paleocene and Eocene may have resulted from either increased atmospheric trace gases or increased heat transport through deep and intermediate waters. The possibility of increasing ocean heat transport through the production of warm saline deep waters (WSDW) in the Tethyan region has generated considerable interest. In addition, General Circulation Model results indicate that deepwater source regions may be highly sensitive to changing basin configurations. To decipher deepwater changes, we examined detailed benthic foraminiferal faunal and isotopic records of the late Paleocene through the early Eocene (~60 to 50 Ma) from two critical regions: the North Atlantic (Bay of Biscay Site 401) and the Pacific (Shatsky Rise Site 577). These records are compared with published data from the Southern Ocean (Maud Rise Site 690, Islas Orcadas Rise Site 702). During the late Paleocene, ... : Supplement to: Pak, Dorothy K; Miller, Kenneth G (1992): Paleocene to Eocene benthic foraminiferal isotopes and assemblages: implications for deepwater circulation. Paleoceanography, 7(4), 405-422 ... |
format |
Article in Journal/Newspaper |
author |
Pak, Dorothy K Miller, Kenneth G |
author_facet |
Pak, Dorothy K Miller, Kenneth G |
author_sort |
Pak, Dorothy K |
title |
Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
title_short |
Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
title_full |
Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
title_fullStr |
Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
title_full_unstemmed |
Age model and stable isotope record of DSDP holes 48-401 and 86-577 ... |
title_sort |
age model and stable isotope record of dsdp holes 48-401 and 86-577 ... |
publisher |
PANGAEA |
publishDate |
1992 |
url |
https://dx.doi.org/10.1594/pangaea.728114 https://doi.pangaea.de/10.1594/PANGAEA.728114 |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_relation |
https://dx.doi.org/10.1029/92pa01234 |
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.72811410.1029/92pa01234 |
_version_ |
1810463754624696320 |