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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Main Authors: Hayward, Bruce William, Johnson, Katherine, Sabaa, Ashwaq T, Kawagata, Shungo, Thomas, Ellen
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.774877
https://doi.pangaea.de/10.1594/PANGAEA.774877
id ftdatacite:10.1594/pangaea.774877
record_format openpolar
spelling 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
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