Abrupt temperature changes in the Western Mediterranean over the past 250,000 years

5 pages, 2 figures.-- PMID: 15576615 [PubMed].-- Supporting information available at: www.sciencemag.org/cgi/content/full/306/5702/1762/DC1 A continuous high-resolution Western Mediterranean sea surface temperature (SST) alkenone record spanning the past 250,000 years shows that abrupt changes were...

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Published in:Science
Main Authors: Martrat, Belen, Grimalt, Joan O., López-Martínez, Constancia, Cacho, Isabel, Sierro, Francisco Javier, Flores, José Abel, Zahn, Rainer, Canals, Miquel, Curtis, Jason H., Hodell, David A.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science 2004
Subjects:
SST
MIS
Online Access:http://hdl.handle.net/10261/16405
https://doi.org/10.1126/science.1101706
id ftcsic:oai:digital.csic.es:10261/16405
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/16405 2024-02-11T10:03:18+01:00 Abrupt temperature changes in the Western Mediterranean over the past 250,000 years Martrat, Belen Grimalt, Joan O. López-Martínez, Constancia Cacho, Isabel Sierro, Francisco Javier Flores, José Abel Zahn, Rainer Canals, Miquel Curtis, Jason H. Hodell, David A. 2004-12-03 22195 bytes application/pdf http://hdl.handle.net/10261/16405 https://doi.org/10.1126/science.1101706 en eng American Association for the Advancement of Science http://dx.doi.org/10.1126/science.1101706 Science 306(5702): 1762-1765 (2004) 0036-8075 http://hdl.handle.net/10261/16405 doi:10.1126/science.1101706 none Sea surface temperature SST Marine isotope stages MIS Climate change Climate cycles Abrupt temperature changes artículo http://purl.org/coar/resource_type/c_6501 2004 ftcsic https://doi.org/10.1126/science.1101706 2024-01-16T09:23:26Z 5 pages, 2 figures.-- PMID: 15576615 [PubMed].-- Supporting information available at: www.sciencemag.org/cgi/content/full/306/5702/1762/DC1 A continuous high-resolution Western Mediterranean sea surface temperature (SST) alkenone record spanning the past 250,000 years shows that abrupt changes were more common at warming than at cooling. During marine isotope stage (MIS) 6, SST oscillated following a stadial-interstadial pattern but at lower intensities and rates of change than in the Dansgaard/Oeschger events of MIS 3. Some of the most prominent events occurred over MISs 5 and 7, after prolonged warm periods of high stability. Climate during the whole period was predominantly maintained in interglacial-interstadial conditions, whereas the duration of stadials was much shorter. This work was supported by the Pole-Ocean-Pole (EVK2-2000-00089) and Coordinated European Surface Ocean Palaeoestimation (EVRI1-2001-00009) projects funded by the European Union. Peer reviewed Article in Journal/Newspaper Dansgaard-Oeschger events Digital.CSIC (Spanish National Research Council) Science 306 5702 1762 1765
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Sea surface temperature
SST
Marine isotope stages
MIS
Climate change
Climate cycles
Abrupt temperature changes
spellingShingle Sea surface temperature
SST
Marine isotope stages
MIS
Climate change
Climate cycles
Abrupt temperature changes
Martrat, Belen
Grimalt, Joan O.
López-Martínez, Constancia
Cacho, Isabel
Sierro, Francisco Javier
Flores, José Abel
Zahn, Rainer
Canals, Miquel
Curtis, Jason H.
Hodell, David A.
Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
topic_facet Sea surface temperature
SST
Marine isotope stages
MIS
Climate change
Climate cycles
Abrupt temperature changes
description 5 pages, 2 figures.-- PMID: 15576615 [PubMed].-- Supporting information available at: www.sciencemag.org/cgi/content/full/306/5702/1762/DC1 A continuous high-resolution Western Mediterranean sea surface temperature (SST) alkenone record spanning the past 250,000 years shows that abrupt changes were more common at warming than at cooling. During marine isotope stage (MIS) 6, SST oscillated following a stadial-interstadial pattern but at lower intensities and rates of change than in the Dansgaard/Oeschger events of MIS 3. Some of the most prominent events occurred over MISs 5 and 7, after prolonged warm periods of high stability. Climate during the whole period was predominantly maintained in interglacial-interstadial conditions, whereas the duration of stadials was much shorter. This work was supported by the Pole-Ocean-Pole (EVK2-2000-00089) and Coordinated European Surface Ocean Palaeoestimation (EVRI1-2001-00009) projects funded by the European Union. Peer reviewed
format Article in Journal/Newspaper
author Martrat, Belen
Grimalt, Joan O.
López-Martínez, Constancia
Cacho, Isabel
Sierro, Francisco Javier
Flores, José Abel
Zahn, Rainer
Canals, Miquel
Curtis, Jason H.
Hodell, David A.
author_facet Martrat, Belen
Grimalt, Joan O.
López-Martínez, Constancia
Cacho, Isabel
Sierro, Francisco Javier
Flores, José Abel
Zahn, Rainer
Canals, Miquel
Curtis, Jason H.
Hodell, David A.
author_sort Martrat, Belen
title Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
title_short Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
title_full Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
title_fullStr Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
title_full_unstemmed Abrupt temperature changes in the Western Mediterranean over the past 250,000 years
title_sort abrupt temperature changes in the western mediterranean over the past 250,000 years
publisher American Association for the Advancement of Science
publishDate 2004
url http://hdl.handle.net/10261/16405
https://doi.org/10.1126/science.1101706
genre Dansgaard-Oeschger events
genre_facet Dansgaard-Oeschger events
op_relation http://dx.doi.org/10.1126/science.1101706
Science 306(5702): 1762-1765 (2004)
0036-8075
http://hdl.handle.net/10261/16405
doi:10.1126/science.1101706
op_rights none
op_doi https://doi.org/10.1126/science.1101706
container_title Science
container_volume 306
container_issue 5702
container_start_page 1762
op_container_end_page 1765
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