Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years

We report changes of deep-sea ostracod fauna during the last 370,000 yr from the Ocean Drilling Program (ODP) Hole 704A in the South Atlantic sector of the Southern Ocean. The results show that faunal changes are coincident with glacial/interglacial-scale deep-water circulation changes, even though...

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Published in:Journal of Paleontology
Main Authors: Hunt, G, Yasuhara, M, Hodell, DA, Cronin, TM
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
Online Access:https://doi.org/10.1666/08-149.1
http://hdl.handle.net/10722/132786
id ftunivhongkonghu:oai:hub.hku.hk:10722/132786
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spelling ftunivhongkonghu:oai:hub.hku.hk:10722/132786 2023-05-15T17:13:54+02:00 Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years Hunt, G Yasuhara, M Hodell, DA Cronin, TM 2009 https://doi.org/10.1666/08-149.1 http://hdl.handle.net/10722/132786 eng eng Journal of Paleontology http://www.scopus.com/mlt/select.url?eid=2-s2.0-70450231484&selection=ref&src=s&origin=recordpage Journal Of Paleontology, 2009, v. 83 n. 6, p. 914-930 doi:10.1666/08-149.1 930 WOS:000272012800005 0022-3360 6 eid_2-s2.0-70450231484 914 http://hdl.handle.net/10722/132786 83 Quaternary Deep-sea Ostracoda Deep-water circulation Paleoecology Southern Ocean Article 2009 ftunivhongkonghu https://doi.org/10.1666/08-149.1 2023-01-14T15:36:33Z We report changes of deep-sea ostracod fauna during the last 370,000 yr from the Ocean Drilling Program (ODP) Hole 704A in the South Atlantic sector of the Southern Ocean. The results show that faunal changes are coincident with glacial/interglacial-scale deep-water circulation changes, even though our dataset is relatively small and the waters are barren of ostracods until mid-MIS (Marine Isotope Stage) 5. Krithe and Poseidonamicus were dominant during the Holocene interglacial period and the latter part of MIS 5, when this site was under the influence of North Atlantic Deep Water (NADW). Conversely, Henryhowella and Legitimocythere were dominant during glacial periods, when this site was in the path of Circumpolar Deep Water (CPDW). Three new species (Aversovalva brandaoae, Poseidonamicus hisayoae, and Krithe mazziniae) are described herein. This is the first report of Quaternary glacial/interglacial scale deep-sea ostracod faunal changes in the Southern and South Atlantic Oceans, a key region for understanding Quaternary climate and deep-water circulation, although the paucity of Quaternary ostracods in this region necessitates further research. © 2009 The Paleontological Society. link_to_subscribed_fulltext Article in Journal/Newspaper NADW North Atlantic Deep Water North Atlantic Southern Ocean University of Hong Kong: HKU Scholars Hub Southern Ocean Journal of Paleontology 83 6 914 930
institution Open Polar
collection University of Hong Kong: HKU Scholars Hub
op_collection_id ftunivhongkonghu
language English
topic Quaternary
Deep-sea Ostracoda
Deep-water circulation
Paleoecology
Southern Ocean
spellingShingle Quaternary
Deep-sea Ostracoda
Deep-water circulation
Paleoecology
Southern Ocean
Hunt, G
Yasuhara, M
Hodell, DA
Cronin, TM
Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
topic_facet Quaternary
Deep-sea Ostracoda
Deep-water circulation
Paleoecology
Southern Ocean
description We report changes of deep-sea ostracod fauna during the last 370,000 yr from the Ocean Drilling Program (ODP) Hole 704A in the South Atlantic sector of the Southern Ocean. The results show that faunal changes are coincident with glacial/interglacial-scale deep-water circulation changes, even though our dataset is relatively small and the waters are barren of ostracods until mid-MIS (Marine Isotope Stage) 5. Krithe and Poseidonamicus were dominant during the Holocene interglacial period and the latter part of MIS 5, when this site was under the influence of North Atlantic Deep Water (NADW). Conversely, Henryhowella and Legitimocythere were dominant during glacial periods, when this site was in the path of Circumpolar Deep Water (CPDW). Three new species (Aversovalva brandaoae, Poseidonamicus hisayoae, and Krithe mazziniae) are described herein. This is the first report of Quaternary glacial/interglacial scale deep-sea ostracod faunal changes in the Southern and South Atlantic Oceans, a key region for understanding Quaternary climate and deep-water circulation, although the paucity of Quaternary ostracods in this region necessitates further research. © 2009 The Paleontological Society. link_to_subscribed_fulltext
format Article in Journal/Newspaper
author Hunt, G
Yasuhara, M
Hodell, DA
Cronin, TM
author_facet Hunt, G
Yasuhara, M
Hodell, DA
Cronin, TM
author_sort Hunt, G
title Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
title_short Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
title_full Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
title_fullStr Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
title_full_unstemmed Deep-sea ostracods from the South Atlantic sector of the Southern ocean during the Last 370,000 years
title_sort deep-sea ostracods from the south atlantic sector of the southern ocean during the last 370,000 years
publishDate 2009
url https://doi.org/10.1666/08-149.1
http://hdl.handle.net/10722/132786
geographic Southern Ocean
geographic_facet Southern Ocean
genre NADW
North Atlantic Deep Water
North Atlantic
Southern Ocean
genre_facet NADW
North Atlantic Deep Water
North Atlantic
Southern Ocean
op_relation Journal of Paleontology
http://www.scopus.com/mlt/select.url?eid=2-s2.0-70450231484&selection=ref&src=s&origin=recordpage
Journal Of Paleontology, 2009, v. 83 n. 6, p. 914-930
doi:10.1666/08-149.1
930
WOS:000272012800005
0022-3360
6
eid_2-s2.0-70450231484
914
http://hdl.handle.net/10722/132786
83
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container_title Journal of Paleontology
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container_issue 6
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