Benthic foraminifera extinctions in the Cenozoic record ...
In the late Pliocene-middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal-abyssal) benthic foraminifera became extinct. This Extinction Group (Ext. Gp), belonging to three families (all the Stilostomellidae and Pleurostomellidae, some of the Nodosariidae), was a...
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ftdatacite:10.1594/pangaea.774877 2024-09-30T14:39:24+00:00 Benthic foraminifera extinctions in the Cenozoic record ... Hayward, Bruce William Johnson, Katherine Sabaa, Ashwaq T Kawagata, Shungo Thomas, Ellen 2010 application/zip https://dx.doi.org/10.1594/pangaea.774877 https://doi.pangaea.de/10.1594/PANGAEA.774877 en eng PANGAEA https://dx.doi.org/10.1016/j.marmicro.2010.01.001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Composite Core Leg33 Leg80 Leg94 Leg143 Leg162 Leg167 Leg172 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2010 ftdatacite https://doi.org/10.1594/pangaea.77487710.1016/j.marmicro.2010.01.001 2024-09-02T08:36:09Z In the late Pliocene-middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal-abyssal) benthic foraminifera became extinct. This Extinction Group (Ext. Gp), belonging to three families (all the Stilostomellidae and Pleurostomellidae, some of the Nodosariidae), was a major component (20-70%) of deep-sea foraminiferal assemblages in the middle Cenozoic and subsequently declined in abundance and species richness before finally disappearing almost completely during the mid-Pleistocene Climatic Transition (MPT). So what caused these declines and extinction?In this study 127 Ext. Gp species are identified from eight Cenozoic bathyal and abyssal sequences in the North Atlantic and equatorial Pacific Oceans. Most species are long-ranging with 80% originating in the Eocene or earlier. The greatest abundance and diversity of the Ext. Gp was in the warm oceanic conditions of the middle Eocene-early Oligocene. The group was subjected to significant changes in the composition of the ... : Supplement to: Hayward, Bruce William; Johnson, Katherine; Sabaa, Ashwaq T; Kawagata, Shungo; Thomas, Ellen (2010): Cenozoic record of elongate, cylindrical, deep-sea benthic foraminifera in the North Atlantic and equatorial Pacific Oceans. Marine Micropaleontology, 74(3-4), 75-95 ... Article in Journal/Newspaper North Atlantic DataCite Hayward ENVELOPE(167.350,167.350,-78.117,-78.117) Pacific |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Composite Core Leg33 Leg80 Leg94 Leg143 Leg162 Leg167 Leg172 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Composite Core Leg33 Leg80 Leg94 Leg143 Leg162 Leg167 Leg172 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Hayward, Bruce William Johnson, Katherine Sabaa, Ashwaq T Kawagata, Shungo Thomas, Ellen Benthic foraminifera extinctions in the Cenozoic record ... |
topic_facet |
Drilling/drill rig Composite Core Leg33 Leg80 Leg94 Leg143 Leg162 Leg167 Leg172 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP |
description |
In the late Pliocene-middle Pleistocene a group of 95 species of elongate, cylindrical, deep-sea (lower bathyal-abyssal) benthic foraminifera became extinct. This Extinction Group (Ext. Gp), belonging to three families (all the Stilostomellidae and Pleurostomellidae, some of the Nodosariidae), was a major component (20-70%) of deep-sea foraminiferal assemblages in the middle Cenozoic and subsequently declined in abundance and species richness before finally disappearing almost completely during the mid-Pleistocene Climatic Transition (MPT). So what caused these declines and extinction?In this study 127 Ext. Gp species are identified from eight Cenozoic bathyal and abyssal sequences in the North Atlantic and equatorial Pacific Oceans. Most species are long-ranging with 80% originating in the Eocene or earlier. The greatest abundance and diversity of the Ext. Gp was in the warm oceanic conditions of the middle Eocene-early Oligocene. The group was subjected to significant changes in the composition of the ... : Supplement to: Hayward, Bruce William; Johnson, Katherine; Sabaa, Ashwaq T; Kawagata, Shungo; Thomas, Ellen (2010): Cenozoic record of elongate, cylindrical, deep-sea benthic foraminifera in the North Atlantic and equatorial Pacific Oceans. Marine Micropaleontology, 74(3-4), 75-95 ... |
format |
Article in Journal/Newspaper |
author |
Hayward, Bruce William Johnson, Katherine Sabaa, Ashwaq T Kawagata, Shungo Thomas, Ellen |
author_facet |
Hayward, Bruce William Johnson, Katherine Sabaa, Ashwaq T Kawagata, Shungo Thomas, Ellen |
author_sort |
Hayward, Bruce William |
title |
Benthic foraminifera extinctions in the Cenozoic record ... |
title_short |
Benthic foraminifera extinctions in the Cenozoic record ... |
title_full |
Benthic foraminifera extinctions in the Cenozoic record ... |
title_fullStr |
Benthic foraminifera extinctions in the Cenozoic record ... |
title_full_unstemmed |
Benthic foraminifera extinctions in the Cenozoic record ... |
title_sort |
benthic foraminifera extinctions in the cenozoic record ... |
publisher |
PANGAEA |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.774877 https://doi.pangaea.de/10.1594/PANGAEA.774877 |
long_lat |
ENVELOPE(167.350,167.350,-78.117,-78.117) |
geographic |
Hayward Pacific |
geographic_facet |
Hayward Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1016/j.marmicro.2010.01.001 |
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.77487710.1016/j.marmicro.2010.01.001 |
_version_ |
1811641995163074560 |