Rock magnetic, element, and color data of three sediment cores along the Senegalese continental margin

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Main Authors: Itambi, Achakie C, von Dobeneck, Tilo, Mulitza, Stefan, Bickert, Torsten, Heslop, David
Format: Dataset Open Access
Language:en
Published: PANGAEA 2010
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author Itambi, Achakie C
von Dobeneck, Tilo
Mulitza, Stefan
Bickert, Torsten
Heslop, David
author_facet Itambi, Achakie C
von Dobeneck, Tilo
Mulitza, Stefan
Bickert, Torsten
Heslop, David
collection Datos científicos de ciencias marinas y ambientales
contents We present a suite of new high-resolution records (0-135 ka) representing pulses of aeolian, fluvial, and biogenic sedimentation along the Senegalese continental margin. A multiproxy approach based on rock magnetic, element, and color data was applied on three cores enclosing the present-day northern limit of the ITCZ. A strong episodic aeolian contribution driven by stronger winds and dry conditions and characterized by high hematite and goethite input was revealed north of 13°N. These millennial-scale dust fluxes are synchronous with North Atlantic Heinrich stadials. Fluvial clay input driven by the West African monsoon predominates at 12°N and varies at Dansgaard-Oeschger time scales while marine productivity is strongly enhanced during the African humid periods and marine isotope stage 5. From latitudinal signal variations, we deduce that the last glacial ITCZ summer position was located between core positions at 12°26' and 13°40'N. Furthermore, this work also shows that submillennial periods of aridity over northwest Africa occurred more frequently and farther south than previously thought.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_734826
institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle Rock magnetic, element, and color data of three sediment cores along the Senegalese continental margin
Itambi, Achakie C
von Dobeneck, Tilo
Mulitza, Stefan
Bickert, Torsten
Heslop, David
291; 301; 312; Center for Marine Environmental Sciences; GeoB9506-1; GeoB9516-5; GeoB9527-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL
We present a suite of new high-resolution records (0-135 ka) representing pulses of aeolian, fluvial, and biogenic sedimentation along the Senegalese continental margin. A multiproxy approach based on rock magnetic, element, and color data was applied on three cores enclosing the present-day northern limit of the ITCZ. A strong episodic aeolian contribution driven by stronger winds and dry conditions and characterized by high hematite and goethite input was revealed north of 13°N. These millennial-scale dust fluxes are synchronous with North Atlantic Heinrich stadials. Fluvial clay input driven by the West African monsoon predominates at 12°N and varies at Dansgaard-Oeschger time scales while marine productivity is strongly enhanced during the African humid periods and marine isotope stage 5. From latitudinal signal variations, we deduce that the last glacial ITCZ summer position was located between core positions at 12°26' and 13°40'N. Furthermore, this work also shows that submillennial periods of aridity over northwest Africa occurred more frequently and farther south than previously thought.
title Rock magnetic, element, and color data of three sediment cores along the Senegalese continental margin
topic 291; 301; 312; Center for Marine Environmental Sciences; GeoB9506-1; GeoB9516-5; GeoB9527-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL
url https://doi.org/10.1594/PANGAEA.734826