Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ...
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major changes in Eocene-Oligocene benthic foraminiferal oxygen isotopes were enrichment of up to 1 per mil in 18O associated wit...
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ftdatacite:10.1594/pangaea.719183 2024-09-15T18:31:03+00:00 Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... Keigwin, Lloyd D Corliss, Bruce H 1986 application/zip https://dx.doi.org/10.1594/pangaea.719183 https://doi.pangaea.de/10.1594/PANGAEA.719183 en eng PANGAEA ftp://rock.geosociety.org/pub/reposit/1986/8605.pdf https://dx.doi.org/10.1130/0016-7606(1986)97<335:siilme>2.0.co;2 ftp://rock.geosociety.org/pub/reposit/1986/8605.pdf Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg2 Leg3 Leg9 Leg10 Leg12 Leg17 Leg22 Leg23 Leg26 Leg29 Leg31 Leg39 Leg40 Leg41 Leg48 Leg80 Leg90 Leg95 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1986 ftdatacite https://doi.org/10.1594/pangaea.71918310.1130/0016-7606(1986)97<335:siilme>2.0.co;2 2024-08-01T10:54:59Z Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major changes in Eocene-Oligocene benthic foraminiferal oxygen isotopes were enrichment of up to 1 per mil in 18O associated with the middle/late Eocene boundary and the Eocene/Oligocene boundary at locations which range from 1- to 4-km paleodepth. Although the synchronous Eocene-Oligocene 18O enrichment began in the latest Eocene, most of the change occurred in the earliest Oligocene. The earliest Oligocene enrichment in 18O is always larger in benthic foraminifera than in surface-dwelling planktonic foraminifera, a condition that indicates a combination of deep-water cooling and increased ice volume. Planktonic foraminiferal d18O does not increase across the middle/late Eocene boundary at our one site with the most complete record (Deep Sea Drilling Project Site 363, Walvis Ridge). This pattern suggests that benthic foraminiferal d18O ... : Supplement to: Keigwin, Lloyd D; Corliss, Bruce H (1986): Stable isotopes in late middle Eocene to Oligocene foraminifera. Geological Society of America Bulletin, 97(3), 335-345 ... Article in Journal/Newspaper Planktonic foraminifera DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg2 Leg3 Leg9 Leg10 Leg12 Leg17 Leg22 Leg23 Leg26 Leg29 Leg31 Leg39 Leg40 Leg41 Leg48 Leg80 Leg90 Leg95 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Drilling/drill rig Leg2 Leg3 Leg9 Leg10 Leg12 Leg17 Leg22 Leg23 Leg26 Leg29 Leg31 Leg39 Leg40 Leg41 Leg48 Leg80 Leg90 Leg95 Glomar Challenger Deep Sea Drilling Project DSDP Keigwin, Lloyd D Corliss, Bruce H Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
topic_facet |
Drilling/drill rig Leg2 Leg3 Leg9 Leg10 Leg12 Leg17 Leg22 Leg23 Leg26 Leg29 Leg31 Leg39 Leg40 Leg41 Leg48 Leg80 Leg90 Leg95 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major changes in Eocene-Oligocene benthic foraminiferal oxygen isotopes were enrichment of up to 1 per mil in 18O associated with the middle/late Eocene boundary and the Eocene/Oligocene boundary at locations which range from 1- to 4-km paleodepth. Although the synchronous Eocene-Oligocene 18O enrichment began in the latest Eocene, most of the change occurred in the earliest Oligocene. The earliest Oligocene enrichment in 18O is always larger in benthic foraminifera than in surface-dwelling planktonic foraminifera, a condition that indicates a combination of deep-water cooling and increased ice volume. Planktonic foraminiferal d18O does not increase across the middle/late Eocene boundary at our one site with the most complete record (Deep Sea Drilling Project Site 363, Walvis Ridge). This pattern suggests that benthic foraminiferal d18O ... : Supplement to: Keigwin, Lloyd D; Corliss, Bruce H (1986): Stable isotopes in late middle Eocene to Oligocene foraminifera. Geological Society of America Bulletin, 97(3), 335-345 ... |
format |
Article in Journal/Newspaper |
author |
Keigwin, Lloyd D Corliss, Bruce H |
author_facet |
Keigwin, Lloyd D Corliss, Bruce H |
author_sort |
Keigwin, Lloyd D |
title |
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
title_short |
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
title_full |
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
title_fullStr |
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
title_full_unstemmed |
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and benthic foraminifera from DSDP sediments ... |
title_sort |
oxygen and carbon isotopic composition in eocene and oligocene planktonic and benthic foraminifera from dsdp sediments ... |
publisher |
PANGAEA |
publishDate |
1986 |
url |
https://dx.doi.org/10.1594/pangaea.719183 https://doi.pangaea.de/10.1594/PANGAEA.719183 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
ftp://rock.geosociety.org/pub/reposit/1986/8605.pdf https://dx.doi.org/10.1130/0016-7606(1986)97<335:siilme>2.0.co;2 ftp://rock.geosociety.org/pub/reposit/1986/8605.pdf |
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.71918310.1130/0016-7606(1986)97<335:siilme>2.0.co;2 |
_version_ |
1810472645974556672 |