Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...

The cold upwelling 'tongue' of the eastern equatorial Pacific is a central energetic feature of the ocean, dominating both the mean state and temporal variability of climate in the tropics and beyond. Recent evidence for the development of the modern cold tongue during the Pliocene-Pleisto...

Full description

Bibliographic Details
Main Authors: Martínez‐García, Alfredo, Rosell-Melé, Antoni, McClymont, Erin L, Gersonde, Rainer, Haug, Gerald H
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.771708
https://doi.pangaea.de/10.1594/PANGAEA.771708
id ftdatacite:10.1594/pangaea.771708
record_format openpolar
spelling ftdatacite:10.1594/pangaea.771708 2024-09-15T17:45:27+00:00 Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ... Martínez‐García, Alfredo Rosell-Melé, Antoni McClymont, Erin L Gersonde, Rainer Haug, Gerald H 2010 application/zip https://dx.doi.org/10.1594/pangaea.771708 https://doi.pangaea.de/10.1594/PANGAEA.771708 en eng PANGAEA https://dx.doi.org/10.1126/science.1184480 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Piston corer BGR type Leg145 Leg177 ANT-XI/2 Joides Resolution Polarstern International Polar Year 2007-2008 IPY Ocean Drilling Program ODP Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.77170810.1126/science.1184480 2024-07-03T13:10:33Z The cold upwelling 'tongue' of the eastern equatorial Pacific is a central energetic feature of the ocean, dominating both the mean state and temporal variability of climate in the tropics and beyond. Recent evidence for the development of the modern cold tongue during the Pliocene-Pleistocene transition has been explained as the result of extratropical cooling that drove a shoaling of the thermocline. We have found that the sub-Antarctic and sub-Arctic regions underwent substantial cooling nearly synchronous to the cold tongue development, thereby providing support for this hypothesis. In addition, we show that sub-Antarctic climate changed in its response to Earth's orbital variations, from a subtropical to a subpolar pattern, as expected if cooling shrank the warm-water sphere of the ocean and thus contracted the subtropical gyres. ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper Antarc* Antarctic International Polar Year IPY DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Piston corer BGR type
Leg145
Leg177
ANT-XI/2
Joides Resolution
Polarstern
International Polar Year 2007-2008 IPY
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Composite Core
Piston corer BGR type
Leg145
Leg177
ANT-XI/2
Joides Resolution
Polarstern
International Polar Year 2007-2008 IPY
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Martínez‐García, Alfredo
Rosell-Melé, Antoni
McClymont, Erin L
Gersonde, Rainer
Haug, Gerald H
Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
topic_facet Composite Core
Piston corer BGR type
Leg145
Leg177
ANT-XI/2
Joides Resolution
Polarstern
International Polar Year 2007-2008 IPY
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The cold upwelling 'tongue' of the eastern equatorial Pacific is a central energetic feature of the ocean, dominating both the mean state and temporal variability of climate in the tropics and beyond. Recent evidence for the development of the modern cold tongue during the Pliocene-Pleistocene transition has been explained as the result of extratropical cooling that drove a shoaling of the thermocline. We have found that the sub-Antarctic and sub-Arctic regions underwent substantial cooling nearly synchronous to the cold tongue development, thereby providing support for this hypothesis. In addition, we show that sub-Antarctic climate changed in its response to Earth's orbital variations, from a subtropical to a subpolar pattern, as expected if cooling shrank the warm-water sphere of the ocean and thus contracted the subtropical gyres. ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...
format Article in Journal/Newspaper
author Martínez‐García, Alfredo
Rosell-Melé, Antoni
McClymont, Erin L
Gersonde, Rainer
Haug, Gerald H
author_facet Martínez‐García, Alfredo
Rosell-Melé, Antoni
McClymont, Erin L
Gersonde, Rainer
Haug, Gerald H
author_sort Martínez‐García, Alfredo
title Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
title_short Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
title_full Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
title_fullStr Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
title_full_unstemmed Sea surface temperature estimates and alkenone C37:4 abundances in ODP Site 145-882 and 177-1090 ...
title_sort sea surface temperature estimates and alkenone c37:4 abundances in odp site 145-882 and 177-1090 ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.771708
https://doi.pangaea.de/10.1594/PANGAEA.771708
genre Antarc*
Antarctic
International Polar Year
IPY
genre_facet Antarc*
Antarctic
International Polar Year
IPY
op_relation https://dx.doi.org/10.1126/science.1184480
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.77170810.1126/science.1184480
_version_ 1810493282421047296