Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...

Twenty percent (19 genera, 95 species) of cosmopolitan, deep-sea (500-4000 m), benthic foraminiferal species became extinct during the late Pliocene-Middle Pleistocene (3-0.12 Ma), with the peak of extinctions (76 species) occurring during the mid-Pleistocene Climate Transition (MPT, 1.2-0.55 Ma). O...

Full description

Bibliographic Details
Main Authors: Hayward, Bruce William, Kawagata, Shungo, Grenfell, Hugh R, Sabaa, Ashwaq T, O'Neill, Tanya
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.746497
https://doi.pangaea.de/10.1594/PANGAEA.746497
id ftdatacite:10.1594/pangaea.746497
record_format openpolar
spelling ftdatacite:10.1594/pangaea.746497 2024-09-30T14:26:52+00:00 Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ... Hayward, Bruce William Kawagata, Shungo Grenfell, Hugh R Sabaa, Ashwaq T O'Neill, Tanya 2007 application/zip https://dx.doi.org/10.1594/pangaea.746497 https://doi.pangaea.de/10.1594/PANGAEA.746497 en eng PANGAEA https://dx.doi.org/10.1029/2007pa001424 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg160 Leg161 Leg167 Leg172 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.74649710.1029/2007pa001424 2024-09-02T08:37:33Z Twenty percent (19 genera, 95 species) of cosmopolitan, deep-sea (500-4000 m), benthic foraminiferal species became extinct during the late Pliocene-Middle Pleistocene (3-0.12 Ma), with the peak of extinctions (76 species) occurring during the mid-Pleistocene Climate Transition (MPT, 1.2-0.55 Ma). One whole family (Stilostomellidae, 30 species) was wiped out, and a second (Pleurostomellidae, 29 species) was decimated with just one species possibly surviving through to the present. Our studies at 21 deep-sea core sites show widespread pulsed declines in abundance and diversity of the extinction group species during more extreme glacials, with partial interglacial recoveries. These declines started in the late Pliocene in southern sourced deep water masses (Antarctic Bottom Water, Circumpolar Deep Water) and extending into intermediate waters (Antarctic Intermediate Water, North Atlantic Deep Water) in the MPT, with the youngest declines in sites farthest downstream from high-latitude source areas for ... : Supplement to: Hayward, Bruce William; Kawagata, Shungo; Grenfell, Hugh R; Sabaa, Ashwaq T; O'Neill, Tanya (2007): Last global extinction in the deep sea during the mid-Pleistocene climate transition. Paleoceanography, 22(3), PA3103 ... Article in Journal/Newspaper Antarc* Antarctic North Atlantic Deep Water North Atlantic DataCite Antarctic Hayward ENVELOPE(167.350,167.350,-78.117,-78.117)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg160
Leg161
Leg167
Leg172
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg160
Leg161
Leg167
Leg172
Joides Resolution
Ocean Drilling Program ODP
Hayward, Bruce William
Kawagata, Shungo
Grenfell, Hugh R
Sabaa, Ashwaq T
O'Neill, Tanya
Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
topic_facet Drilling/drill rig
Leg160
Leg161
Leg167
Leg172
Joides Resolution
Ocean Drilling Program ODP
description Twenty percent (19 genera, 95 species) of cosmopolitan, deep-sea (500-4000 m), benthic foraminiferal species became extinct during the late Pliocene-Middle Pleistocene (3-0.12 Ma), with the peak of extinctions (76 species) occurring during the mid-Pleistocene Climate Transition (MPT, 1.2-0.55 Ma). One whole family (Stilostomellidae, 30 species) was wiped out, and a second (Pleurostomellidae, 29 species) was decimated with just one species possibly surviving through to the present. Our studies at 21 deep-sea core sites show widespread pulsed declines in abundance and diversity of the extinction group species during more extreme glacials, with partial interglacial recoveries. These declines started in the late Pliocene in southern sourced deep water masses (Antarctic Bottom Water, Circumpolar Deep Water) and extending into intermediate waters (Antarctic Intermediate Water, North Atlantic Deep Water) in the MPT, with the youngest declines in sites farthest downstream from high-latitude source areas for ... : Supplement to: Hayward, Bruce William; Kawagata, Shungo; Grenfell, Hugh R; Sabaa, Ashwaq T; O'Neill, Tanya (2007): Last global extinction in the deep sea during the mid-Pleistocene climate transition. Paleoceanography, 22(3), PA3103 ...
format Article in Journal/Newspaper
author Hayward, Bruce William
Kawagata, Shungo
Grenfell, Hugh R
Sabaa, Ashwaq T
O'Neill, Tanya
author_facet Hayward, Bruce William
Kawagata, Shungo
Grenfell, Hugh R
Sabaa, Ashwaq T
O'Neill, Tanya
author_sort Hayward, Bruce William
title Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
title_short Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
title_full Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
title_fullStr Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
title_full_unstemmed Pliocene/Pleistocene benthic foraminiferal abundances from six drilling cores ...
title_sort pliocene/pleistocene benthic foraminiferal abundances from six drilling cores ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.746497
https://doi.pangaea.de/10.1594/PANGAEA.746497
long_lat ENVELOPE(167.350,167.350,-78.117,-78.117)
geographic Antarctic
Hayward
geographic_facet Antarctic
Hayward
genre Antarc*
Antarctic
North Atlantic Deep Water
North Atlantic
genre_facet Antarc*
Antarctic
North Atlantic Deep Water
North Atlantic
op_relation https://dx.doi.org/10.1029/2007pa001424
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.74649710.1029/2007pa001424
_version_ 1811632985664913408