Terrigenous sedimentation of sediment core GeoB6007-2

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Autori principali: Holz, Christine, Stuut, Jan-Berend W, Henrich, Rüdiger, Meggers, Helge
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2007
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author Holz, Christine
Stuut, Jan-Berend W
Henrich, Rüdiger
Meggers, Helge
author_facet Holz, Christine
Stuut, Jan-Berend W
Henrich, Rüdiger
Meggers, Helge
collection Datos científicos de ciencias marinas y ambientales
contents Variations in deposition of terrigenous fine sediments and their grain-size distributions from a high-resolution marine sediment record offshore northwest Africa (30°51.0'N; 10°16.1'W) document climate changes on the African continent during the Holocene. End-member grain-size distributions of the terrigenous silt fraction, which are related to fluvial and aeolian dust transport, indicate millennial-scale variability in the dominant transport processes at the investigation site off northwest Africa as well as recurring periods of dry conditions in northwest Africa during the Holocene. The terrigenous record from the subtropical North Atlantic reflects generally humid conditions before the Younger Dryas, during the early to mid-Holocene, as well as after 1.3 kyr BP. By contrast, continental runoff was reduced and arid conditions were prevalent at the beginning of the Younger Dryas and during the mid- and late Holocene. A comparison with high- and low-latitude Holocene climate records reveals a strong link between northwest African climate and Northern Hemisphere atmospheric circulation throughout the Holocene. Due to its proximal position, close to an ephemeral river system draining the Atlas Mountains as well as the adjacent Saharan desert, this detailed marine sediment record, which has a temporal resolution between 15 and 120 years, is ideally suited to enhance our understanding of ocean-continent-atmosphere interactions in African climates and the hydrological cycle of northern Africa after the last deglaciation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_738416
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Terrigenous sedimentation of sediment core GeoB6007-2
Holz, Christine
Stuut, Jan-Berend W
Henrich, Rüdiger
Meggers, Helge
GeoB; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M45/5a; Meteor (1986); SL
Variations in deposition of terrigenous fine sediments and their grain-size distributions from a high-resolution marine sediment record offshore northwest Africa (30°51.0'N; 10°16.1'W) document climate changes on the African continent during the Holocene. End-member grain-size distributions of the terrigenous silt fraction, which are related to fluvial and aeolian dust transport, indicate millennial-scale variability in the dominant transport processes at the investigation site off northwest Africa as well as recurring periods of dry conditions in northwest Africa during the Holocene. The terrigenous record from the subtropical North Atlantic reflects generally humid conditions before the Younger Dryas, during the early to mid-Holocene, as well as after 1.3 kyr BP. By contrast, continental runoff was reduced and arid conditions were prevalent at the beginning of the Younger Dryas and during the mid- and late Holocene. A comparison with high- and low-latitude Holocene climate records reveals a strong link between northwest African climate and Northern Hemisphere atmospheric circulation throughout the Holocene. Due to its proximal position, close to an ephemeral river system draining the Atlas Mountains as well as the adjacent Saharan desert, this detailed marine sediment record, which has a temporal resolution between 15 and 120 years, is ideally suited to enhance our understanding of ocean-continent-atmosphere interactions in African climates and the hydrological cycle of northern Africa after the last deglaciation.
title Terrigenous sedimentation of sediment core GeoB6007-2
topic GeoB; GeoB6007-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M45/5a; Meteor (1986); SL
url https://doi.org/10.1594/PANGAEA.738416