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...
Main Authors: | , , , , , |
---|---|
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 |
_version_ |
1786830722437218304 |