Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ...
The Middle Eocene Climatic Optimum (MECO; ~ 40 million years ago [Ma]) is one of the most prominent transient global warming events in the Paleogene. Although the event is well documented in geochemical and isotopic proxy records at many locations, the marine biotic response to the MECO remains poor...
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ftdatacite:10.1594/pangaea.828089 2024-09-15T18:22:25+00:00 Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... Witkowski, Jakub Bohaty, Steven M Edgar, Kirsty M Harwood, David M 2014 application/zip https://dx.doi.org/10.1594/pangaea.828089 https://doi.pangaea.de/10.1594/PANGAEA.828089 en eng PANGAEA https://dx.doi.org/10.1016/j.marmicro.2014.01.001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg171B Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2014 ftdatacite https://doi.org/10.1594/pangaea.82808910.1016/j.marmicro.2014.01.001 2024-08-01T10:54:23Z The Middle Eocene Climatic Optimum (MECO; ~ 40 million years ago [Ma]) is one of the most prominent transient global warming events in the Paleogene. Although the event is well documented in geochemical and isotopic proxy records at many locations, the marine biotic response to the MECO remains poorly constrained. We present new high-resolution, quantitative records of siliceous microplankton assemblages from the MECO interval of Ocean Drilling Program (ODP) Site 1051 in the subtropical western North Atlantic Ocean, which are interpreted in the context of published foraminiferal and bulk carbonate stable isotope (d18O and d13C) records. High diatom, radiolarian and silicoflagellate accumulation rates between 40.5 and 40.0 Ma are interpreted to reflect an ~ 500 thousand year (kyr) interval of increased nutrient supply and resultant surface-water eutrophication that was associated with elevated sea-surface temperatures during the prolonged onset of the MECO. Relatively low pelagic siliceous phytoplankton ... : Supplement to: Witkowski, Jakub; Bohaty, Steven M; Edgar, Kirsty M; Harwood, David M (2014): Rapid fluctuations in mid-latitude siliceous plankton production during the Middle Eocene Climatic Optimum (ODP Site 1051, western North Atlantic). Marine Micropaleontology, 106, 110-129 ... Article in Journal/Newspaper North Atlantic DataCite |
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English |
topic |
Composite Core Leg171B Joides Resolution Ocean Drilling Program ODP |
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Composite Core Leg171B Joides Resolution Ocean Drilling Program ODP Witkowski, Jakub Bohaty, Steven M Edgar, Kirsty M Harwood, David M Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
topic_facet |
Composite Core Leg171B Joides Resolution Ocean Drilling Program ODP |
description |
The Middle Eocene Climatic Optimum (MECO; ~ 40 million years ago [Ma]) is one of the most prominent transient global warming events in the Paleogene. Although the event is well documented in geochemical and isotopic proxy records at many locations, the marine biotic response to the MECO remains poorly constrained. We present new high-resolution, quantitative records of siliceous microplankton assemblages from the MECO interval of Ocean Drilling Program (ODP) Site 1051 in the subtropical western North Atlantic Ocean, which are interpreted in the context of published foraminiferal and bulk carbonate stable isotope (d18O and d13C) records. High diatom, radiolarian and silicoflagellate accumulation rates between 40.5 and 40.0 Ma are interpreted to reflect an ~ 500 thousand year (kyr) interval of increased nutrient supply and resultant surface-water eutrophication that was associated with elevated sea-surface temperatures during the prolonged onset of the MECO. Relatively low pelagic siliceous phytoplankton ... : Supplement to: Witkowski, Jakub; Bohaty, Steven M; Edgar, Kirsty M; Harwood, David M (2014): Rapid fluctuations in mid-latitude siliceous plankton production during the Middle Eocene Climatic Optimum (ODP Site 1051, western North Atlantic). Marine Micropaleontology, 106, 110-129 ... |
format |
Article in Journal/Newspaper |
author |
Witkowski, Jakub Bohaty, Steven M Edgar, Kirsty M Harwood, David M |
author_facet |
Witkowski, Jakub Bohaty, Steven M Edgar, Kirsty M Harwood, David M |
author_sort |
Witkowski, Jakub |
title |
Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
title_short |
Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
title_full |
Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
title_fullStr |
Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
title_full_unstemmed |
Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051 ... |
title_sort |
siliceous microfossil assemblage and accumulation rate variations across the middle eocene climatic optimum at odp site 171-1051 ... |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.828089 https://doi.pangaea.de/10.1594/PANGAEA.828089 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1016/j.marmicro.2014.01.001 |
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.82808910.1016/j.marmicro.2014.01.001 |
_version_ |
1810462204554641408 |