Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...

Benthic foraminiferal delta13C data from site 502 in the Caribbean Sea (sill depth ?1800 m) indicate that throughout the past 2.6 m.y., glacial delta13C values in the middepth Atlantic were higher during glaciations than interglaciations. This is interpreted as indicating a greater proportion of Upp...

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Main Authors: Oppo, Delia W, Raymo, Maureen E, Lohmann, Gerrit, Mix, Alan C, Wright, James D, Prell, Warren L
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1995
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.729936
https://doi.pangaea.de/10.1594/PANGAEA.729936
id ftdatacite:10.1594/pangaea.729936
record_format openpolar
spelling ftdatacite:10.1594/pangaea.729936 2023-12-31T10:20:23+01:00 Stable isotope record of benthic foraminifera from DSDP Site 68-502 ... Oppo, Delia W Raymo, Maureen E Lohmann, Gerrit Mix, Alan C Wright, James D Prell, Warren L 1995 application/zip https://dx.doi.org/10.1594/pangaea.729936 https://doi.pangaea.de/10.1594/PANGAEA.729936 en eng PANGAEA https://dx.doi.org/10.1029/95pa00332 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Composite Core Leg68 Glomar Challenger Deep Sea Drilling Project DSDP Supplementary Publication Series of Datasets article Collection 1995 ftdatacite https://doi.org/10.1594/pangaea.72993610.1029/95pa00332 2023-12-01T11:50:33Z Benthic foraminiferal delta13C data from site 502 in the Caribbean Sea (sill depth ?1800 m) indicate that throughout the past 2.6 m.y., glacial delta13C values in the middepth Atlantic were higher during glaciations than interglaciations. This is interpreted as indicating a greater proportion of Upper North Atlantic Deep Water (UNADW) relative to southern source waters during glaciations. The contribution of UNADW during interglaciations to the middepth Atlantic remained approximately constant, and the contribution during glaciations may have been as much as 10 % higher in the late Pleistocene than in the late Pliocene. This small increase is in striking contrast to the much larger decrease in glacial Lower North Atlantic Deep Water (LNADW) contribution relative to southern sources, from about 80% to about 20%, that occurred over the past 2.6 m.y. Glacial intensification over the past 2.6 m.y. was probably coupled with a decrease in northward heat transport by the upper limb of the North Atlantic circulation ... : Supplement to: Oppo, Delia W; Raymo, Maureen E; Lohmann, Gerrit; Mix, Alan C; Wright, James D; Prell, Warren L (1995): A d13C record of Upper North Atlantic Deep Water during the past 2.6 million years. Paleoceanography, 10(3), 373-394 ... Article in Journal/Newspaper North Atlantic Deep Water North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Composite Core
Leg68
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Composite Core
Leg68
Glomar Challenger
Deep Sea Drilling Project DSDP
Oppo, Delia W
Raymo, Maureen E
Lohmann, Gerrit
Mix, Alan C
Wright, James D
Prell, Warren L
Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
topic_facet Drilling/drill rig
Composite Core
Leg68
Glomar Challenger
Deep Sea Drilling Project DSDP
description Benthic foraminiferal delta13C data from site 502 in the Caribbean Sea (sill depth ?1800 m) indicate that throughout the past 2.6 m.y., glacial delta13C values in the middepth Atlantic were higher during glaciations than interglaciations. This is interpreted as indicating a greater proportion of Upper North Atlantic Deep Water (UNADW) relative to southern source waters during glaciations. The contribution of UNADW during interglaciations to the middepth Atlantic remained approximately constant, and the contribution during glaciations may have been as much as 10 % higher in the late Pleistocene than in the late Pliocene. This small increase is in striking contrast to the much larger decrease in glacial Lower North Atlantic Deep Water (LNADW) contribution relative to southern sources, from about 80% to about 20%, that occurred over the past 2.6 m.y. Glacial intensification over the past 2.6 m.y. was probably coupled with a decrease in northward heat transport by the upper limb of the North Atlantic circulation ... : Supplement to: Oppo, Delia W; Raymo, Maureen E; Lohmann, Gerrit; Mix, Alan C; Wright, James D; Prell, Warren L (1995): A d13C record of Upper North Atlantic Deep Water during the past 2.6 million years. Paleoceanography, 10(3), 373-394 ...
format Article in Journal/Newspaper
author Oppo, Delia W
Raymo, Maureen E
Lohmann, Gerrit
Mix, Alan C
Wright, James D
Prell, Warren L
author_facet Oppo, Delia W
Raymo, Maureen E
Lohmann, Gerrit
Mix, Alan C
Wright, James D
Prell, Warren L
author_sort Oppo, Delia W
title Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
title_short Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
title_full Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
title_fullStr Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
title_full_unstemmed Stable isotope record of benthic foraminifera from DSDP Site 68-502 ...
title_sort stable isotope record of benthic foraminifera from dsdp site 68-502 ...
publisher PANGAEA
publishDate 1995
url https://dx.doi.org/10.1594/pangaea.729936
https://doi.pangaea.de/10.1594/PANGAEA.729936
genre North Atlantic Deep Water
North Atlantic
genre_facet North Atlantic Deep Water
North Atlantic
op_relation https://dx.doi.org/10.1029/95pa00332
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.72993610.1029/95pa00332
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