Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...

High-resolution delta18O records from the equatorial Pacific (site 503B), equatorial Atlantic (site 665A), and North Atlantic (site 606A) based on the benthic foraminifera Cibicidoides wuellerstorfi show the 2.4 Ma onset of major northern hemispheric glaciation to be a package of three events occurr...

Full description

Bibliographic Details
Main Authors: Sikes, Elisabeth L, Keigwin, Lloyd D, Curry, William B
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1991
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.733972
https://doi.pangaea.de/10.1594/PANGAEA.733972
id ftdatacite:10.1594/pangaea.733972
record_format openpolar
spelling ftdatacite:10.1594/pangaea.733972 2023-05-15T17:33:57+02:00 Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ... Sikes, Elisabeth L Keigwin, Lloyd D Curry, William B 1991 application/zip https://dx.doi.org/10.1594/pangaea.733972 https://doi.pangaea.de/10.1594/PANGAEA.733972 en eng PANGAEA https://dx.doi.org/10.1029/90pa02499 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg68 Leg94 Leg108 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1991 ftdatacite https://doi.org/10.1594/pangaea.73397210.1029/90pa02499 2023-04-03T13:12:12Z High-resolution delta18O records from the equatorial Pacific (site 503B), equatorial Atlantic (site 665A), and North Atlantic (site 606A) based on the benthic foraminifera Cibicidoides wuellerstorfi show the 2.4 Ma onset of major northern hemispheric glaciation to be a package of three events occurring at 2.39, 2.35, and 2.31 Ma in which a periodicity of about 40 kyr is evident. The amplitude of the signals at the three sites indicates that these events were 1/2 to 2/3 the size of the latest Quaternary glaciation and also indicates cooling of northern source bottom water by 2.7°-4.1°C relative to southern source water during glaciations. Carbon isotopes indicate that southern source waters were less oxygenated than in the Quaternary and that there was reduced production of northern source water during glacial intervals. The dominant presence of southern source water in the eastern basin of the equatorial Atlantic, regardless of climatic cycles, throughout the late Pliocene indicates a greater influence of ... : Supplement to: Sikes, Elisabeth L; Keigwin, Lloyd D; Curry, William B (1991): Pliocene paleoceanography: circulation and oceanographic changes associated with the 2.4 Ma glacial event. Paleoceanography, 6(2), 245-257 ... Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg68
Leg94
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg68
Leg94
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Sikes, Elisabeth L
Keigwin, Lloyd D
Curry, William B
Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
topic_facet Drilling/drill rig
Leg68
Leg94
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description High-resolution delta18O records from the equatorial Pacific (site 503B), equatorial Atlantic (site 665A), and North Atlantic (site 606A) based on the benthic foraminifera Cibicidoides wuellerstorfi show the 2.4 Ma onset of major northern hemispheric glaciation to be a package of three events occurring at 2.39, 2.35, and 2.31 Ma in which a periodicity of about 40 kyr is evident. The amplitude of the signals at the three sites indicates that these events were 1/2 to 2/3 the size of the latest Quaternary glaciation and also indicates cooling of northern source bottom water by 2.7°-4.1°C relative to southern source water during glaciations. Carbon isotopes indicate that southern source waters were less oxygenated than in the Quaternary and that there was reduced production of northern source water during glacial intervals. The dominant presence of southern source water in the eastern basin of the equatorial Atlantic, regardless of climatic cycles, throughout the late Pliocene indicates a greater influence of ... : Supplement to: Sikes, Elisabeth L; Keigwin, Lloyd D; Curry, William B (1991): Pliocene paleoceanography: circulation and oceanographic changes associated with the 2.4 Ma glacial event. Paleoceanography, 6(2), 245-257 ...
format Article in Journal/Newspaper
author Sikes, Elisabeth L
Keigwin, Lloyd D
Curry, William B
author_facet Sikes, Elisabeth L
Keigwin, Lloyd D
Curry, William B
author_sort Sikes, Elisabeth L
title Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
title_short Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
title_full Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
title_fullStr Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
title_full_unstemmed Stable carbon and oxygen isotope record of Cibicidoides from DSDP/ODP holes ...
title_sort stable carbon and oxygen isotope record of cibicidoides from dsdp/odp holes ...
publisher PANGAEA
publishDate 1991
url https://dx.doi.org/10.1594/pangaea.733972
https://doi.pangaea.de/10.1594/PANGAEA.733972
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1029/90pa02499
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.73397210.1029/90pa02499
_version_ 1766132628299186176