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...
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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 |