Potassium measurements and ages of sediment cores GeoB5546-2 and GeoB6007-2

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Auteurs principaux: Kuhlmann, Holger, Meggers, Helge, Freudenthal, Tim, Wefer, Gerold
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2004
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author Kuhlmann, Holger
Meggers, Helge
Freudenthal, Tim
Wefer, Gerold
author_facet Kuhlmann, Holger
Meggers, Helge
Freudenthal, Tim
Wefer, Gerold
collection Datos científicos de ciencias marinas y ambientales
contents The northward extent of the influence of the W African monsoon during humid periods of interglacials is subject to investigations highlighting feedback mechanisms, such as vegetation. To detect this regional variation and the climate system acting farther to the north will be the aim of this paper focussing on the Holocene. We present two very high-resolution Holocene sediment records off NW Africa located at 31°N and 27°N. The well-known mid-Holocene climate change from the "African Humid Period" to present arid conditions is well reflected by the terrigenous input in the southern core. In contrast, in the northern core spectral and wavelet analyses indicate a periodic oscillation of about 900 years of the terrigenous input throughout the last 9000 years B.P. We conclude that the W African monsoonal influence characterized by the abrupt climatic change at 5000 years B.P. can be separated from the influence of the N Atlantic climate system reflected by a periodic oscillation throughout the Holocene.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_779104
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle Potassium measurements and ages of sediment cores GeoB5546-2 and GeoB6007-2
Kuhlmann, Holger
Meggers, Helge
Freudenthal, Tim
Wefer, Gerold
Center for Marine Environmental Sciences; GeoB; GeoB5546-2; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); KL; M42/4b; M45/5a; MARUM; Meteor (1986); Piston corer (BGR type); SL
The northward extent of the influence of the W African monsoon during humid periods of interglacials is subject to investigations highlighting feedback mechanisms, such as vegetation. To detect this regional variation and the climate system acting farther to the north will be the aim of this paper focussing on the Holocene. We present two very high-resolution Holocene sediment records off NW Africa located at 31°N and 27°N. The well-known mid-Holocene climate change from the "African Humid Period" to present arid conditions is well reflected by the terrigenous input in the southern core. In contrast, in the northern core spectral and wavelet analyses indicate a periodic oscillation of about 900 years of the terrigenous input throughout the last 9000 years B.P. We conclude that the W African monsoonal influence characterized by the abrupt climatic change at 5000 years B.P. can be separated from the influence of the N Atlantic climate system reflected by a periodic oscillation throughout the Holocene.
title Potassium measurements and ages of sediment cores GeoB5546-2 and GeoB6007-2
topic Center for Marine Environmental Sciences; GeoB; GeoB5546-2; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); KL; M42/4b; M45/5a; MARUM; Meteor (1986); Piston corer (BGR type); SL
url https://doi.org/10.1594/PANGAEA.779104