Sea surface temperature estimation for the Iberian Margin

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Hauptverfasser: Martrat, Belén, Grimalt, Joan O, Shackleton, Nicholas J, de Abreu, Lucia, Hutterli, Manuel A, Stocker, Thomas F
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2007
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author Martrat, Belén
Grimalt, Joan O
Shackleton, Nicholas J
de Abreu, Lucia
Hutterli, Manuel A
Stocker, Thomas F
author_facet Martrat, Belén
Grimalt, Joan O
Shackleton, Nicholas J
de Abreu, Lucia
Hutterli, Manuel A
Stocker, Thomas F
collection Datos científicos de ciencias marinas y ambientales
contents Centennial climate variability over the last ice age exhibits clear bipolar behavior. High-resolution analyses of marine sediment cores from the Iberian margin trace a number of associated changes simultaneously. Proxies of sea surface temperature and water mass distribution, as well as relative biomarker content, demonstrate that this typical north-south coupling was pervasive for the cold phases of climate during the past 420,000 years. Cold episodes after relatively warm and largely ice-free periods occurred when the predominance of deep water formation changed from northern to southern sources. These results reinforce the connection between rapid climate changes at Mediterranean latitudes and century-to-millennial variability in northern and southern polar regions.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_771894
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Sea surface temperature estimation for the Iberian Margin
Martrat, Belén
Grimalt, Joan O
Shackleton, Nicholas J
de Abreu, Lucia
Hutterli, Manuel A
Stocker, Thomas F
161-977A; Alboran Sea; CALYPSO; Calypso Corer; DRILL; Drilling/drill rig; GEOSCIENCES, MARMARCORE; IMAGES I; Joides Resolution; Leg161; Marge Ibérique; Marion Dufresne (1995); MD01-2444; MD101__Campaign; MD123; MD952042; MD95-2042; Ocean Drilling Program; ODP
Centennial climate variability over the last ice age exhibits clear bipolar behavior. High-resolution analyses of marine sediment cores from the Iberian margin trace a number of associated changes simultaneously. Proxies of sea surface temperature and water mass distribution, as well as relative biomarker content, demonstrate that this typical north-south coupling was pervasive for the cold phases of climate during the past 420,000 years. Cold episodes after relatively warm and largely ice-free periods occurred when the predominance of deep water formation changed from northern to southern sources. These results reinforce the connection between rapid climate changes at Mediterranean latitudes and century-to-millennial variability in northern and southern polar regions.
title Sea surface temperature estimation for the Iberian Margin
topic 161-977A; Alboran Sea; CALYPSO; Calypso Corer; DRILL; Drilling/drill rig; GEOSCIENCES, MARMARCORE; IMAGES I; Joides Resolution; Leg161; Marge Ibérique; Marion Dufresne (1995); MD01-2444; MD101__Campaign; MD123; MD952042; MD95-2042; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.771894