Age model, isotope analyses, geochemical measurements and grain size analyses of sediment core GeoB9508-5 from the Senegal River Mouth

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Hauptverfasser: Mulitza, Stefan, Prange, Matthias, Stuut, Jan-Berend W, Zabel, Matthias, von Dobeneck, Tilo, Itambi, Achakie C, Nizou, Jean, Schulz, Michael, Wefer, Gerold
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Sprache:en
Veröffentlicht: PANGAEA 2009
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author Mulitza, Stefan
Prange, Matthias
Stuut, Jan-Berend W
Zabel, Matthias
von Dobeneck, Tilo
Itambi, Achakie C
Nizou, Jean
Schulz, Michael
Wefer, Gerold
author_facet Mulitza, Stefan
Prange, Matthias
Stuut, Jan-Berend W
Zabel, Matthias
von Dobeneck, Tilo
Itambi, Achakie C
Nizou, Jean
Schulz, Michael
Wefer, Gerold
collection Datos científicos de ciencias marinas y ambientales
contents The influence of the large-scale ocean circulation on Sahel rainfall is elusive because of the shortness of the observational record. We reconstructed the history of eolian and fluvial sedimentation on the continental slope off Senegal during the past 57,000 years. Our data show that abrupt onsets of arid conditions in the West African Sahel were linked to cold North Atlantic sea surface temperatures during times of reduced meridional overturning circulation associated with Heinrich Stadials. Climate modeling suggests that this drying is induced by a southward shift of the West African monsoon trough in conjunction with an intensification and southward expansion of the midtropospheric African Easterly Jet.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_726789
institution PANGAEA
language en
publishDate 2009
publisher PANGAEA
record_format pangaea
spellingShingle Age model, isotope analyses, geochemical measurements and grain size analyses of sediment core GeoB9508-5 from the Senegal River Mouth
Mulitza, Stefan
Prange, Matthias
Stuut, Jan-Berend W
Zabel, Matthias
von Dobeneck, Tilo
Itambi, Achakie C
Nizou, Jean
Schulz, Michael
Wefer, Gerold
293; Center for Marine Environmental Sciences; GeoB9508-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL
The influence of the large-scale ocean circulation on Sahel rainfall is elusive because of the shortness of the observational record. We reconstructed the history of eolian and fluvial sedimentation on the continental slope off Senegal during the past 57,000 years. Our data show that abrupt onsets of arid conditions in the West African Sahel were linked to cold North Atlantic sea surface temperatures during times of reduced meridional overturning circulation associated with Heinrich Stadials. Climate modeling suggests that this drying is induced by a southward shift of the West African monsoon trough in conjunction with an intensification and southward expansion of the midtropospheric African Easterly Jet.
title Age model, isotope analyses, geochemical measurements and grain size analyses of sediment core GeoB9508-5 from the Senegal River Mouth
topic 293; Center for Marine Environmental Sciences; GeoB9508-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL
url https://doi.org/10.1594/PANGAEA.726789