Paleotemperatures and paleosalinities from the Celtic Margin (Bay of Biscay)

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Auteurs principaux: Eynaud, Frédérique, Malaizé, Bruno, Zaragosi, Sebastien, de Vernal, Anne, Scourse, James D, Pujol, Claude, Cortijo, Elsa, Grousset, Francis E, Penaud, Aurélie, Toucanne, Samuel, Turon, Jean-Louis, Auffret, Gérard A
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Langue:en
Publié: PANGAEA 2012
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author Eynaud, Frédérique
Malaizé, Bruno
Zaragosi, Sebastien
de Vernal, Anne
Scourse, James D
Pujol, Claude
Cortijo, Elsa
Grousset, Francis E
Penaud, Aurélie
Toucanne, Samuel
Turon, Jean-Louis
Auffret, Gérard A
author_facet Eynaud, Frédérique
Malaizé, Bruno
Zaragosi, Sebastien
de Vernal, Anne
Scourse, James D
Pujol, Claude
Cortijo, Elsa
Grousset, Francis E
Penaud, Aurélie
Toucanne, Samuel
Turon, Jean-Louis
Auffret, Gérard A
collection Datos científicos de ciencias marinas y ambientales
contents During the late Quaternary, both external and internal forcings have driven major climatic shifts from glacial to interglacial conditions. Nonlinear climatic steps characterized the transitions leading to these extrema, with intermediate excursions particularly well xpressed in the dynamics of the Northern Hemisphere cryosphere. Here we document the impact of these dynamics on the north-eastern North Atlantic Ocean, focussing on the 35-10 ka interval. Sea-surface salinities have been reconstructed quantitatively based on two independent methods from core MD95-2002, recovered from the northern Bay of Biscay adjacent to the axis of the Manche paleoriver outlet and thus in connection with proximal European ice sheets and glaciers. Quantitative reconstructions deriving from dinocyst and planktonic foraminiferal analyses have been combined within a robust chronology to assess the amplitude and timing of hydrological changes in this region. Our study evidences strong pulsed freshwater discharges which may have impacted the North Atlantic Meridional Overturning Circulation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_810296
institution PANGAEA
language en
publishDate 2012
publisher PANGAEA
record_format pangaea
spellingShingle Paleotemperatures and paleosalinities from the Celtic Margin (Bay of Biscay)
Eynaud, Frédérique
Malaizé, Bruno
Zaragosi, Sebastien
de Vernal, Anne
Scourse, James D
Pujol, Claude
Cortijo, Elsa
Grousset, Francis E
Penaud, Aurélie
Toucanne, Samuel
Turon, Jean-Louis
Auffret, Gérard A
CALYPSO; Calypso Corer; Climate Change: Learning from the past climate; IMAGES I; Marion Dufresne (1995); MD101__Campaign; MD952002; MD95-2002; Meriadzec; Past4Future
During the late Quaternary, both external and internal forcings have driven major climatic shifts from glacial to interglacial conditions. Nonlinear climatic steps characterized the transitions leading to these extrema, with intermediate excursions particularly well xpressed in the dynamics of the Northern Hemisphere cryosphere. Here we document the impact of these dynamics on the north-eastern North Atlantic Ocean, focussing on the 35-10 ka interval. Sea-surface salinities have been reconstructed quantitatively based on two independent methods from core MD95-2002, recovered from the northern Bay of Biscay adjacent to the axis of the Manche paleoriver outlet and thus in connection with proximal European ice sheets and glaciers. Quantitative reconstructions deriving from dinocyst and planktonic foraminiferal analyses have been combined within a robust chronology to assess the amplitude and timing of hydrological changes in this region. Our study evidences strong pulsed freshwater discharges which may have impacted the North Atlantic Meridional Overturning Circulation.
title Paleotemperatures and paleosalinities from the Celtic Margin (Bay of Biscay)
topic CALYPSO; Calypso Corer; Climate Change: Learning from the past climate; IMAGES I; Marion Dufresne (1995); MD101__Campaign; MD952002; MD95-2002; Meriadzec; Past4Future
url https://doi.org/10.1594/PANGAEA.810296