Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ...
Planktic foraminifera across the Paleocene-Eocene transition at DSDP Site 401 indicate that the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and Miller (1988), or PS of Berggren et al. (1995) and coincident with a sudden 2.0‰ excursion in 6r3C values. The benthic fo...
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ftdatacite:10.1594/pangaea.681320 2024-09-15T18:22:30+00:00 Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... Pardo, Alfonso Keller, Gerta Molina, Eustoquio Canudo, José I 1997 application/zip https://dx.doi.org/10.1594/pangaea.681320 https://doi.pangaea.de/10.1594/PANGAEA.681320 en eng PANGAEA https://dx.doi.org/10.1016/s0377-8398(96)00035-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg48 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1997 ftdatacite https://doi.org/10.1594/pangaea.68132010.1016/s0377-8398(96)00035-7 2024-08-01T10:51:52Z Planktic foraminifera across the Paleocene-Eocene transition at DSDP Site 401 indicate that the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and Miller (1988), or PS of Berggren et al. (1995) and coincident with a sudden 2.0‰ excursion in 6r3C values. The benthic foraminiferal extinction event (BFEE) and Sr3C excursion was accompanied by a planktic foraminiferal turnover marked by an influx of warm water species (Morozovella and Acarinina), a decrease in cooler water species (Subbotina), a sudden short-term increase in low oxygen tolerant taxa (Chiloguembelina), and no significant species extinctions. These faunal changes suggest climatic warming, expansion of the oxygen minimum zone, and a well stratified ocean water column. Oxygen isotope data of the surface dweller M. subbotina suggest climate warming beginning with a gradual 0.5‰ decrease in delta180 in the 175 cm preceding the benthic foraminiferal extinction event followed by a sudden decrease of 1‰ (4°C) at the BFEE. ... : Supplement to: Pardo, Alfonso; Keller, Gerta; Molina, Eustoquio; Canudo, José I (1997): Planktic foraminiferal turnover across the Paleocene-Eocene transition at DSDP Site 401, Bay of Biscay, North Atlantic. Marine Micropaleontology, 29(2), 129-158 ... Article in Journal/Newspaper North Atlantic DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg48 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Drilling/drill rig Leg48 Glomar Challenger Deep Sea Drilling Project DSDP Pardo, Alfonso Keller, Gerta Molina, Eustoquio Canudo, José I Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
topic_facet |
Drilling/drill rig Leg48 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
Planktic foraminifera across the Paleocene-Eocene transition at DSDP Site 401 indicate that the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and Miller (1988), or PS of Berggren et al. (1995) and coincident with a sudden 2.0‰ excursion in 6r3C values. The benthic foraminiferal extinction event (BFEE) and Sr3C excursion was accompanied by a planktic foraminiferal turnover marked by an influx of warm water species (Morozovella and Acarinina), a decrease in cooler water species (Subbotina), a sudden short-term increase in low oxygen tolerant taxa (Chiloguembelina), and no significant species extinctions. These faunal changes suggest climatic warming, expansion of the oxygen minimum zone, and a well stratified ocean water column. Oxygen isotope data of the surface dweller M. subbotina suggest climate warming beginning with a gradual 0.5‰ decrease in delta180 in the 175 cm preceding the benthic foraminiferal extinction event followed by a sudden decrease of 1‰ (4°C) at the BFEE. ... : Supplement to: Pardo, Alfonso; Keller, Gerta; Molina, Eustoquio; Canudo, José I (1997): Planktic foraminiferal turnover across the Paleocene-Eocene transition at DSDP Site 401, Bay of Biscay, North Atlantic. Marine Micropaleontology, 29(2), 129-158 ... |
format |
Article in Journal/Newspaper |
author |
Pardo, Alfonso Keller, Gerta Molina, Eustoquio Canudo, José I |
author_facet |
Pardo, Alfonso Keller, Gerta Molina, Eustoquio Canudo, José I |
author_sort |
Pardo, Alfonso |
title |
Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
title_short |
Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
title_full |
Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
title_fullStr |
Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
title_full_unstemmed |
Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic ... |
title_sort |
planktic foraminiferal turnover across the paleocene-eocene transition in the bay of biscay, north atlantic ... |
publisher |
PANGAEA |
publishDate |
1997 |
url |
https://dx.doi.org/10.1594/pangaea.681320 https://doi.pangaea.de/10.1594/PANGAEA.681320 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1016/s0377-8398(96)00035-7 |
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.68132010.1016/s0377-8398(96)00035-7 |
_version_ |
1810462367572557824 |