Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...

Stable isotopic analyses of Middle Miocene to Quaternary foraminiferal calcite from east equatorial and central north Pacific DSDP cores have provided much new informatlon on the paleoceanography of the Pacific Neogene The history of delta18O change in planktonic foraminifera reflects the changing I...

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Bibliographic Details
Main Author: Keigwin, Lloyd D
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1979
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.710854
https://doi.pangaea.de/10.1594/PANGAEA.710854
id ftdatacite:10.1594/pangaea.710854
record_format openpolar
spelling ftdatacite:10.1594/pangaea.710854 2024-09-15T17:47:51+00:00 Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ... Keigwin, Lloyd D 1979 application/zip https://dx.doi.org/10.1594/pangaea.710854 https://doi.pangaea.de/10.1594/PANGAEA.710854 en eng PANGAEA https://dx.doi.org/10.1016/0012-821x(79)90137-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg16 Leg32 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1979 ftdatacite https://doi.org/10.1594/pangaea.71085410.1016/0012-821x(79)90137-7 2024-07-03T13:10:33Z Stable isotopic analyses of Middle Miocene to Quaternary foraminiferal calcite from east equatorial and central north Pacific DSDP cores have provided much new informatlon on the paleoceanography of the Pacific Neogene The history of delta18O change in planktonic foraminifera reflects the changing Isotopic composition and temperature of seawater at the time of test formation. Changes in the isotopic composition of benthonic foraminifera largely reflect changes m the volume of continental ice. Isotopic data from these cores indicates the following sequence of events related to continental glaciation(1) A permanent Antarctic ice sheet developed late in the Middle Miocene (about 13 to 11.5 m.y. ago)(2) The Late Miocene (about 11.5 to 5 m.y. ago) is marked by significant variation in delta18O of about 0.5‰ throughout, indicating instability of Antarctic ice cap size or bottom-water temperatures(3) The early Pliocene (5 to about 3 m.y. ago) was a time of relative stability in ice volume and bottom-water ... : Supplement to: Keigwin, Lloyd D (1979): Late Cenozoic stable isotope stratigraphy and paleoceanography of DSDP sites from the east equatorial and central north Pacific Ocean. Earth and Planetary Science Letters, 45(2), 361-382 ... Article in Journal/Newspaper Antarc* Antarctic Ice cap Ice Sheet Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg16
Leg32
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg16
Leg32
Glomar Challenger
Deep Sea Drilling Project DSDP
Keigwin, Lloyd D
Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
topic_facet Drilling/drill rig
Leg16
Leg32
Glomar Challenger
Deep Sea Drilling Project DSDP
description Stable isotopic analyses of Middle Miocene to Quaternary foraminiferal calcite from east equatorial and central north Pacific DSDP cores have provided much new informatlon on the paleoceanography of the Pacific Neogene The history of delta18O change in planktonic foraminifera reflects the changing Isotopic composition and temperature of seawater at the time of test formation. Changes in the isotopic composition of benthonic foraminifera largely reflect changes m the volume of continental ice. Isotopic data from these cores indicates the following sequence of events related to continental glaciation(1) A permanent Antarctic ice sheet developed late in the Middle Miocene (about 13 to 11.5 m.y. ago)(2) The Late Miocene (about 11.5 to 5 m.y. ago) is marked by significant variation in delta18O of about 0.5‰ throughout, indicating instability of Antarctic ice cap size or bottom-water temperatures(3) The early Pliocene (5 to about 3 m.y. ago) was a time of relative stability in ice volume and bottom-water ... : Supplement to: Keigwin, Lloyd D (1979): Late Cenozoic stable isotope stratigraphy and paleoceanography of DSDP sites from the east equatorial and central north Pacific Ocean. Earth and Planetary Science Letters, 45(2), 361-382 ...
format Article in Journal/Newspaper
author Keigwin, Lloyd D
author_facet Keigwin, Lloyd D
author_sort Keigwin, Lloyd D
title Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
title_short Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
title_full Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
title_fullStr Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
title_full_unstemmed Late Cenozoic stable isotope record of benthic and planktonic foraminifera from the Pacific Ocean ...
title_sort late cenozoic stable isotope record of benthic and planktonic foraminifera from the pacific ocean ...
publisher PANGAEA
publishDate 1979
url https://dx.doi.org/10.1594/pangaea.710854
https://doi.pangaea.de/10.1594/PANGAEA.710854
genre Antarc*
Antarctic
Ice cap
Ice Sheet
Planktonic foraminifera
genre_facet Antarc*
Antarctic
Ice cap
Ice Sheet
Planktonic foraminifera
op_relation https://dx.doi.org/10.1016/0012-821x(79)90137-7
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.71085410.1016/0012-821x(79)90137-7
_version_ 1810497498607779840