Global cooling during the Eocene Oligocene Transition ...

About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's temperature changed during this climate transition remains poorly understood, and evidence for Northern Hem...

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Main Authors: Liu, Zhonghui, Pagani, Mark, Zinniker, David, DeConto, Robert M, Huber, Matthew, Brinkhuis, Henk, Shah, Sunita R, Leckie, R Mark, Pearson, Ann
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.771853
https://doi.pangaea.de/10.1594/PANGAEA.771853
id ftdatacite:10.1594/pangaea.771853
record_format openpolar
spelling ftdatacite:10.1594/pangaea.771853 2024-09-30T14:26:14+00:00 Global cooling during the Eocene Oligocene Transition ... Liu, Zhonghui Pagani, Mark Zinniker, David DeConto, Robert M Huber, Matthew Brinkhuis, Henk Shah, Sunita R Leckie, R Mark Pearson, Ann 2009 application/zip https://dx.doi.org/10.1594/pangaea.771853 https://doi.pangaea.de/10.1594/PANGAEA.771853 en eng PANGAEA https://dx.doi.org/10.1126/science.1166368 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Composite Core Leg29 Leg38 Leg71 Leg95 Leg101 Leg151 Leg165 Leg177 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2009 ftdatacite https://doi.org/10.1594/pangaea.77185310.1126/science.1166368 2024-09-02T08:37:33Z About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's temperature changed during this climate transition remains poorly understood, and evidence for Northern Hemisphere polar ice is controversial. Here, we report proxy records of sea surface temperatures from multiple ocean localities and show that the high-latitude temperature decrease was substantial and heterogeneous. High-latitude (45 degrees to 70 degrees in both hemispheres) temperatures before the climate transition were ~20°C and cooled an average of ~5°C. Our results, combined with ocean and ice-sheet model simulations and benthic oxygen isotope records, indicate that Northern Hemisphere glaciation was not required to accommodate the magnitude of continental ice growth during this time. ... : Supplement to: Liu, Zhonghui; Pagani, Mark; Zinniker, David; DeConto, Robert M; Huber, Matthew; Brinkhuis, Henk; Shah, Sunita R; Leckie, R Mark; Pearson, Ann (2009): Global cooling during the Eocene-Oligocene climate transition. Science, 323(5918), 1187-1190 ... Article in Journal/Newspaper Antarc* Antarctica Ice Sheet DataCite Leckie ENVELOPE(66.007,66.007,-70.439,-70.439)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Composite Core
Leg29
Leg38
Leg71
Leg95
Leg101
Leg151
Leg165
Leg177
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Composite Core
Leg29
Leg38
Leg71
Leg95
Leg101
Leg151
Leg165
Leg177
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Liu, Zhonghui
Pagani, Mark
Zinniker, David
DeConto, Robert M
Huber, Matthew
Brinkhuis, Henk
Shah, Sunita R
Leckie, R Mark
Pearson, Ann
Global cooling during the Eocene Oligocene Transition ...
topic_facet Drilling/drill rig
Composite Core
Leg29
Leg38
Leg71
Leg95
Leg101
Leg151
Leg165
Leg177
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's temperature changed during this climate transition remains poorly understood, and evidence for Northern Hemisphere polar ice is controversial. Here, we report proxy records of sea surface temperatures from multiple ocean localities and show that the high-latitude temperature decrease was substantial and heterogeneous. High-latitude (45 degrees to 70 degrees in both hemispheres) temperatures before the climate transition were ~20°C and cooled an average of ~5°C. Our results, combined with ocean and ice-sheet model simulations and benthic oxygen isotope records, indicate that Northern Hemisphere glaciation was not required to accommodate the magnitude of continental ice growth during this time. ... : Supplement to: Liu, Zhonghui; Pagani, Mark; Zinniker, David; DeConto, Robert M; Huber, Matthew; Brinkhuis, Henk; Shah, Sunita R; Leckie, R Mark; Pearson, Ann (2009): Global cooling during the Eocene-Oligocene climate transition. Science, 323(5918), 1187-1190 ...
format Article in Journal/Newspaper
author Liu, Zhonghui
Pagani, Mark
Zinniker, David
DeConto, Robert M
Huber, Matthew
Brinkhuis, Henk
Shah, Sunita R
Leckie, R Mark
Pearson, Ann
author_facet Liu, Zhonghui
Pagani, Mark
Zinniker, David
DeConto, Robert M
Huber, Matthew
Brinkhuis, Henk
Shah, Sunita R
Leckie, R Mark
Pearson, Ann
author_sort Liu, Zhonghui
title Global cooling during the Eocene Oligocene Transition ...
title_short Global cooling during the Eocene Oligocene Transition ...
title_full Global cooling during the Eocene Oligocene Transition ...
title_fullStr Global cooling during the Eocene Oligocene Transition ...
title_full_unstemmed Global cooling during the Eocene Oligocene Transition ...
title_sort global cooling during the eocene oligocene transition ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.771853
https://doi.pangaea.de/10.1594/PANGAEA.771853
long_lat ENVELOPE(66.007,66.007,-70.439,-70.439)
geographic Leckie
geographic_facet Leckie
genre Antarc*
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctica
Ice Sheet
op_relation https://dx.doi.org/10.1126/science.1166368
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.77185310.1126/science.1166368
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