Age determination and paleotemperatures of western Mediterranean Sea sediments ...

Sea surface temperature (SST) profiles over the last 25 kyr derived from alkenone measurements are studied in four cores from a W-E latitudinal transect encompassing the Gulf of Cadiz (Atlantic Ocean), the Alboran Sea, and the southern Tyrrhenian Sea (western Mediterranean). The results document the...

Full description

Bibliographic Details
Main Authors: Cacho, Isabel, Grimalt, Joan O, Canals, Miquel, Sbaffi, Laura, Shackleton, Nicholas J, Schönfeld, Joachim, Zahn, Rainer
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735765
https://doi.pangaea.de/10.1594/PANGAEA.735765
id ftdatacite:10.1594/pangaea.735765
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735765 2024-09-15T18:21:29+00:00 Age determination and paleotemperatures of western Mediterranean Sea sediments ... Cacho, Isabel Grimalt, Joan O Canals, Miquel Sbaffi, Laura Shackleton, Nicholas J Schönfeld, Joachim Zahn, Rainer 2001 application/zip https://dx.doi.org/10.1594/pangaea.735765 https://doi.pangaea.de/10.1594/PANGAEA.735765 en eng PANGAEA https://dx.doi.org/10.1029/2000pa000502 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Gravity corer Kiel type Calypso Corer M39/1 MD101 Meteor 1986 Marion Dufresne 1995 article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.73576510.1029/2000pa000502 2024-07-03T13:10:33Z Sea surface temperature (SST) profiles over the last 25 kyr derived from alkenone measurements are studied in four cores from a W-E latitudinal transect encompassing the Gulf of Cadiz (Atlantic Ocean), the Alboran Sea, and the southern Tyrrhenian Sea (western Mediterranean). The results document the sensitivity of the Mediterranean region to the short climatic changes of the North Atlantic Ocean, particularly those involving the latitudinal position of the polar front. The amplitude of the SST oscillations increases toward the Tyrrhenian Sea, indicating an amplification effect of the Atlantic signal by the climatic regime of the Mediterranean region. All studied cores show a shorter cooling phase (700 years) for the Younger Dryas (YD) than that observed in the North Atlantic region (1200 years). This time diachroneity is related to an intra-YD climatic change documented in the European continent. Minor oscillations in the southward displacement of the North Atlantic polar front may also have driven this ... : For akenone-derived Holocene sea-surface temperures of sediment core MD95-2043 see Cacho et al. (1999) datasets: doi:10.1594/PANGAEA.735759 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer
Gravity corer Kiel type
Calypso Corer
M39/1
MD101
Meteor 1986
Marion Dufresne 1995
spellingShingle Gravity corer
Gravity corer Kiel type
Calypso Corer
M39/1
MD101
Meteor 1986
Marion Dufresne 1995
Cacho, Isabel
Grimalt, Joan O
Canals, Miquel
Sbaffi, Laura
Shackleton, Nicholas J
Schönfeld, Joachim
Zahn, Rainer
Age determination and paleotemperatures of western Mediterranean Sea sediments ...
topic_facet Gravity corer
Gravity corer Kiel type
Calypso Corer
M39/1
MD101
Meteor 1986
Marion Dufresne 1995
description Sea surface temperature (SST) profiles over the last 25 kyr derived from alkenone measurements are studied in four cores from a W-E latitudinal transect encompassing the Gulf of Cadiz (Atlantic Ocean), the Alboran Sea, and the southern Tyrrhenian Sea (western Mediterranean). The results document the sensitivity of the Mediterranean region to the short climatic changes of the North Atlantic Ocean, particularly those involving the latitudinal position of the polar front. The amplitude of the SST oscillations increases toward the Tyrrhenian Sea, indicating an amplification effect of the Atlantic signal by the climatic regime of the Mediterranean region. All studied cores show a shorter cooling phase (700 years) for the Younger Dryas (YD) than that observed in the North Atlantic region (1200 years). This time diachroneity is related to an intra-YD climatic change documented in the European continent. Minor oscillations in the southward displacement of the North Atlantic polar front may also have driven this ... : For akenone-derived Holocene sea-surface temperures of sediment core MD95-2043 see Cacho et al. (1999) datasets: doi:10.1594/PANGAEA.735759 ...
format Article in Journal/Newspaper
author Cacho, Isabel
Grimalt, Joan O
Canals, Miquel
Sbaffi, Laura
Shackleton, Nicholas J
Schönfeld, Joachim
Zahn, Rainer
author_facet Cacho, Isabel
Grimalt, Joan O
Canals, Miquel
Sbaffi, Laura
Shackleton, Nicholas J
Schönfeld, Joachim
Zahn, Rainer
author_sort Cacho, Isabel
title Age determination and paleotemperatures of western Mediterranean Sea sediments ...
title_short Age determination and paleotemperatures of western Mediterranean Sea sediments ...
title_full Age determination and paleotemperatures of western Mediterranean Sea sediments ...
title_fullStr Age determination and paleotemperatures of western Mediterranean Sea sediments ...
title_full_unstemmed Age determination and paleotemperatures of western Mediterranean Sea sediments ...
title_sort age determination and paleotemperatures of western mediterranean sea sediments ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.735765
https://doi.pangaea.de/10.1594/PANGAEA.735765
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1029/2000pa000502
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.73576510.1029/2000pa000502
_version_ 1810460066231353344