(Appendix) Ostracodes at DSDP Leg 72 Holes ...
From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed between the formation of the deep water masses (mid-bathyal ± 2000 m) and those of intermediate depths (upper bathyal ± 1000 m)....
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ftdatacite:10.1594/pangaea.811745 2024-09-15T17:44:44+00:00 (Appendix) Ostracodes at DSDP Leg 72 Holes ... Benson, Richard H Peypouquet, Jean Pierre 1983 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.811745 https://doi.pangaea.de/10.1594/PANGAEA.811745 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.72.137.1983 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event Sample code/label Stage Nannofossil zone Zone Poseidonamicus sp. Henryhowella sp. Bythocythere sp. Cytheropteron sp. Argilloecia sp. Atlanticythere sp. Ambocythere sp. Bradleya sp. Krithe sp. Trachyleberis sp. Echinocythereis ericea Rockallia sp. Cytherella sp. Thalassocythere sp. Abyssocythere sp. Eucythere sp. Bairdia sp. Oxycythereis sp. Suhmicythere sp. Bythocypris sp. Parakrithe sp. Cythereis sp. Paracypris sp. Agrenocythere sp. Cyprideis sp. Ostracoda indeterminata Hyphalocythere sp. Pelecocythere sp. Drilling/drill rig DSDP/ODP/IODP sample designation Leg72 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1983 ftdatacite https://doi.org/10.1594/pangaea.81174510.2973/dsdp.proc.72.137.1983 2024-08-01T11:15:14Z From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed between the formation of the deep water masses (mid-bathyal ± 2000 m) and those of intermediate depths (upper bathyal ± 1000 m). The ostracode faunas suggest that while the Antarctic Intermediate Water (O2 = 4.5 to 5 ml/l) was flowing through the Vema Trough to fill the northern basins, the returning less-dense, warmer water (O2 = 3.5 to 5 ml/l) originating in Tethys was being gradually displaced upslope. Efforts to identify shallow (less than 200 m) faunas were unsuccessful. No evidence of significant changes in paleodepth or close proximity to islands could be found that could not be better explained by water-mass changes. Studies of the genera Poseidonamicus and Krithe suggest an important water mass change at about 14 Ma (late-middle Miocene), but the cause of this event is not yet understood. ... : ? = species uncertain. ... Dataset Antarc* Antarctic DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Elevation of event Sample code/label Stage Nannofossil zone Zone Poseidonamicus sp. Henryhowella sp. Bythocythere sp. Cytheropteron sp. Argilloecia sp. Atlanticythere sp. Ambocythere sp. Bradleya sp. Krithe sp. Trachyleberis sp. Echinocythereis ericea Rockallia sp. Cytherella sp. Thalassocythere sp. Abyssocythere sp. Eucythere sp. Bairdia sp. Oxycythereis sp. Suhmicythere sp. Bythocypris sp. Parakrithe sp. Cythereis sp. Paracypris sp. Agrenocythere sp. Cyprideis sp. Ostracoda indeterminata Hyphalocythere sp. Pelecocythere sp. Drilling/drill rig DSDP/ODP/IODP sample designation Leg72 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Event label Latitude of event Longitude of event Elevation of event Sample code/label Stage Nannofossil zone Zone Poseidonamicus sp. Henryhowella sp. Bythocythere sp. Cytheropteron sp. Argilloecia sp. Atlanticythere sp. Ambocythere sp. Bradleya sp. Krithe sp. Trachyleberis sp. Echinocythereis ericea Rockallia sp. Cytherella sp. Thalassocythere sp. Abyssocythere sp. Eucythere sp. Bairdia sp. Oxycythereis sp. Suhmicythere sp. Bythocypris sp. Parakrithe sp. Cythereis sp. Paracypris sp. Agrenocythere sp. Cyprideis sp. Ostracoda indeterminata Hyphalocythere sp. Pelecocythere sp. Drilling/drill rig DSDP/ODP/IODP sample designation Leg72 Glomar Challenger Deep Sea Drilling Project DSDP Benson, Richard H Peypouquet, Jean Pierre (Appendix) Ostracodes at DSDP Leg 72 Holes ... |
topic_facet |
Event label Latitude of event Longitude of event Elevation of event Sample code/label Stage Nannofossil zone Zone Poseidonamicus sp. Henryhowella sp. Bythocythere sp. Cytheropteron sp. Argilloecia sp. Atlanticythere sp. Ambocythere sp. Bradleya sp. Krithe sp. Trachyleberis sp. Echinocythereis ericea Rockallia sp. Cytherella sp. Thalassocythere sp. Abyssocythere sp. Eucythere sp. Bairdia sp. Oxycythereis sp. Suhmicythere sp. Bythocypris sp. Parakrithe sp. Cythereis sp. Paracypris sp. Agrenocythere sp. Cyprideis sp. Ostracoda indeterminata Hyphalocythere sp. Pelecocythere sp. Drilling/drill rig DSDP/ODP/IODP sample designation Leg72 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed between the formation of the deep water masses (mid-bathyal ± 2000 m) and those of intermediate depths (upper bathyal ± 1000 m). The ostracode faunas suggest that while the Antarctic Intermediate Water (O2 = 4.5 to 5 ml/l) was flowing through the Vema Trough to fill the northern basins, the returning less-dense, warmer water (O2 = 3.5 to 5 ml/l) originating in Tethys was being gradually displaced upslope. Efforts to identify shallow (less than 200 m) faunas were unsuccessful. No evidence of significant changes in paleodepth or close proximity to islands could be found that could not be better explained by water-mass changes. Studies of the genera Poseidonamicus and Krithe suggest an important water mass change at about 14 Ma (late-middle Miocene), but the cause of this event is not yet understood. ... : ? = species uncertain. ... |
format |
Dataset |
author |
Benson, Richard H Peypouquet, Jean Pierre |
author_facet |
Benson, Richard H Peypouquet, Jean Pierre |
author_sort |
Benson, Richard H |
title |
(Appendix) Ostracodes at DSDP Leg 72 Holes ... |
title_short |
(Appendix) Ostracodes at DSDP Leg 72 Holes ... |
title_full |
(Appendix) Ostracodes at DSDP Leg 72 Holes ... |
title_fullStr |
(Appendix) Ostracodes at DSDP Leg 72 Holes ... |
title_full_unstemmed |
(Appendix) Ostracodes at DSDP Leg 72 Holes ... |
title_sort |
(appendix) ostracodes at dsdp leg 72 holes ... |
publisher |
PANGAEA |
publishDate |
1983 |
url |
https://dx.doi.org/10.1594/pangaea.811745 https://doi.pangaea.de/10.1594/PANGAEA.811745 |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
https://dx.doi.org/10.2973/dsdp.proc.72.137.1983 |
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.81174510.2973/dsdp.proc.72.137.1983 |
_version_ |
1810492393083895808 |