Age determination and clay content of sediment core GeoB5804-4 ...

Paleosalinity and terrigenous sediment input changes reconstructed on two sediment cores from the northernmost Red Sea were used to infer hydrological changes at the southern margin of the Mediterranean climate zone during the Holocene. Between approximately 9.25 and 7.25 thousand years ago, about 3...

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Main Authors: Arz, Helge Wolfgang, Lamy, Frank, Pätzold, Jürgen, Müller, Peter J, Prins, Maarten Arnoud
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.736624
https://doi.pangaea.de/10.1594/PANGAEA.736624
id ftdatacite:10.1594/pangaea.736624
record_format openpolar
spelling ftdatacite:10.1594/pangaea.736624 2024-09-09T19:25:11+00:00 Age determination and clay content of sediment core GeoB5804-4 ... Arz, Helge Wolfgang Lamy, Frank Pätzold, Jürgen Müller, Peter J Prins, Maarten Arnoud 2003 application/zip https://dx.doi.org/10.1594/pangaea.736624 https://doi.pangaea.de/10.1594/PANGAEA.736624 en eng PANGAEA https://dx.doi.org/10.1126/science.1080325 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M44/3 Meteor 1986 Center for Marine Environmental Sciences MARUM article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.73662410.1126/science.1080325 2024-07-03T13:10:33Z Paleosalinity and terrigenous sediment input changes reconstructed on two sediment cores from the northernmost Red Sea were used to infer hydrological changes at the southern margin of the Mediterranean climate zone during the Holocene. Between approximately 9.25 and 7.25 thousand years ago, about 3 per mil reduced surface water salinities and enhanced fluvial sediment input suggest substantially higher rainfall and freshwater runoff, which thereafter decreased to modern values. The northern Red Sea humid interval is best explained by enhancement and southward extension of rainfall from Mediterranean sources, possibly involving strengthened early-Holocene Arctic Oscillation patterns and a regional monsoon-type circulation induced by increased land-sea temperature contrasts. We conclude that Afro-Asian monsoonal rains did not cross the subtropical desert zone during the early to mid-Holocene. ... : For age determination and results of sediment core GeoB5844-2 see Arz et al. (2003) datasets: doi:10.1594/PANGAEA.736623 ... Article in Journal/Newspaper Arctic DataCite Arctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
M44/3
Meteor 1986
Center for Marine Environmental Sciences MARUM
spellingShingle Gravity corer Kiel type
M44/3
Meteor 1986
Center for Marine Environmental Sciences MARUM
Arz, Helge Wolfgang
Lamy, Frank
Pätzold, Jürgen
Müller, Peter J
Prins, Maarten Arnoud
Age determination and clay content of sediment core GeoB5804-4 ...
topic_facet Gravity corer Kiel type
M44/3
Meteor 1986
Center for Marine Environmental Sciences MARUM
description Paleosalinity and terrigenous sediment input changes reconstructed on two sediment cores from the northernmost Red Sea were used to infer hydrological changes at the southern margin of the Mediterranean climate zone during the Holocene. Between approximately 9.25 and 7.25 thousand years ago, about 3 per mil reduced surface water salinities and enhanced fluvial sediment input suggest substantially higher rainfall and freshwater runoff, which thereafter decreased to modern values. The northern Red Sea humid interval is best explained by enhancement and southward extension of rainfall from Mediterranean sources, possibly involving strengthened early-Holocene Arctic Oscillation patterns and a regional monsoon-type circulation induced by increased land-sea temperature contrasts. We conclude that Afro-Asian monsoonal rains did not cross the subtropical desert zone during the early to mid-Holocene. ... : For age determination and results of sediment core GeoB5844-2 see Arz et al. (2003) datasets: doi:10.1594/PANGAEA.736623 ...
format Article in Journal/Newspaper
author Arz, Helge Wolfgang
Lamy, Frank
Pätzold, Jürgen
Müller, Peter J
Prins, Maarten Arnoud
author_facet Arz, Helge Wolfgang
Lamy, Frank
Pätzold, Jürgen
Müller, Peter J
Prins, Maarten Arnoud
author_sort Arz, Helge Wolfgang
title Age determination and clay content of sediment core GeoB5804-4 ...
title_short Age determination and clay content of sediment core GeoB5804-4 ...
title_full Age determination and clay content of sediment core GeoB5804-4 ...
title_fullStr Age determination and clay content of sediment core GeoB5804-4 ...
title_full_unstemmed Age determination and clay content of sediment core GeoB5804-4 ...
title_sort age determination and clay content of sediment core geob5804-4 ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.736624
https://doi.pangaea.de/10.1594/PANGAEA.736624
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation https://dx.doi.org/10.1126/science.1080325
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73662410.1126/science.1080325
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