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Autores principales: Deplazes, Gaudenz, Lückge, Andreas, Stuut, Jan-Berend W, Pätzold, Jürgen, Kuhlmann, Holger, Husson, Dorothée, Fant, Mara, Haug, Gerald H
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2014
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Acceso en línea:https://doi.org/10.1594/PANGAEA.831498
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author Deplazes, Gaudenz
Lückge, Andreas
Stuut, Jan-Berend W
Pätzold, Jürgen
Kuhlmann, Holger
Husson, Dorothée
Fant, Mara
Haug, Gerald H
author_facet Deplazes, Gaudenz
Lückge, Andreas
Stuut, Jan-Berend W
Pätzold, Jürgen
Kuhlmann, Holger
Husson, Dorothée
Fant, Mara
Haug, Gerald H
collection Datos científicos de ciencias marinas y ambientales
contents The Dansgaard-Oeschger oscillations and Heinrich events described in North Atlantic sediments and Greenland ice are expressed in the climate of the tropics, for example, as documented in Arabian Sea sediments. Given the strength of this teleconnection, we seek to reconstruct its range of environmental impacts. We present geochemical and sedimentological data from core SO130-289KL from the Indus submarine slope spanning the last ~ 80 kyr. Elemental and grain size analyses consistently indicate that interstadials are characterized by an increased contribution of fluvial suspension from the Indus River. In contrast, stadials are characterized by an increased contribution of aeolian dust from the Arabian Peninsula. Decadal-scale shifts at climate transitions, such as onsets of interstadials, were coeval with changes in productivity-related proxies. Heinrich events stand out as especially dry and dusty events, indicating a dramatically weakened Indian summer monsoon, potentially increased winter monsoon circulation, and increased aridity on the Arabian Peninsula. This finding is consistent with other paleoclimate evidence for continental aridity in the northern tropics during these events. Our results strengthen the evidence that circum-North Atlantic temperature variations translate to hydrological shifts in the tropics, with major impacts on regional environmental conditions such as rainfall, river discharge, aeolian dust transport, and ocean margin anoxia.
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language en
publishDate 2014
publisher PANGAEA
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spellingShingle Elemental analyses (XRF), total organic carbon (TOC), grain size analyses, lamination index of sediment core SO130-289KL
Deplazes, Gaudenz
Lückge, Andreas
Stuut, Jan-Berend W
Pätzold, Jürgen
Kuhlmann, Holger
Husson, Dorothée
Fant, Mara
Haug, Gerald H
Center for Marine Environmental Sciences; MARUM
The Dansgaard-Oeschger oscillations and Heinrich events described in North Atlantic sediments and Greenland ice are expressed in the climate of the tropics, for example, as documented in Arabian Sea sediments. Given the strength of this teleconnection, we seek to reconstruct its range of environmental impacts. We present geochemical and sedimentological data from core SO130-289KL from the Indus submarine slope spanning the last ~ 80 kyr. Elemental and grain size analyses consistently indicate that interstadials are characterized by an increased contribution of fluvial suspension from the Indus River. In contrast, stadials are characterized by an increased contribution of aeolian dust from the Arabian Peninsula. Decadal-scale shifts at climate transitions, such as onsets of interstadials, were coeval with changes in productivity-related proxies. Heinrich events stand out as especially dry and dusty events, indicating a dramatically weakened Indian summer monsoon, potentially increased winter monsoon circulation, and increased aridity on the Arabian Peninsula. This finding is consistent with other paleoclimate evidence for continental aridity in the northern tropics during these events. Our results strengthen the evidence that circum-North Atlantic temperature variations translate to hydrological shifts in the tropics, with major impacts on regional environmental conditions such as rainfall, river discharge, aeolian dust transport, and ocean margin anoxia.
title Elemental analyses (XRF), total organic carbon (TOC), grain size analyses, lamination index of sediment core SO130-289KL
topic Center for Marine Environmental Sciences; MARUM
url https://doi.org/10.1594/PANGAEA.831498