A drop in Sahara dust fluxes records the northern limits of the African Humid Period
Marine sediment cores from east of Africa show that Sahara dust fluxes decreased by at least 50% between the last deglaciation and the mid Holocene, while the Northern Sector of the Red Sea remained unchanged. This constrains the African Humid Period impact to have extended up to ca. 22°N, across a...
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Format: | Article |
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Nature Portfolio
2019-08-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-019-11701-z |
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author | Daniel Palchan Adi Torfstein |
author_facet | Daniel Palchan Adi Torfstein |
author_sort | Daniel Palchan |
collection | DOAJ |
description | Marine sediment cores from east of Africa show that Sahara dust fluxes decreased by at least 50% between the last deglaciation and the mid Holocene, while the Northern Sector of the Red Sea remained unchanged. This constrains the African Humid Period impact to have extended up to ca. 22°N, across a more limited region than previously thought. |
first_indexed | 2024-12-14T15:46:59Z |
format | Article |
id | doaj.art-e43041eaa8d7406a8c744fe49b8829d0 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-14T15:46:59Z |
publishDate | 2019-08-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
spelling | doaj.art-e43041eaa8d7406a8c744fe49b8829d02022-12-21T22:55:29ZengNature PortfolioNature Communications2041-17232019-08-011011910.1038/s41467-019-11701-zA drop in Sahara dust fluxes records the northern limits of the African Humid PeriodDaniel Palchan0Adi Torfstein1The Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat RamThe Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, The Edmond J. Safra Campus, Givat RamMarine sediment cores from east of Africa show that Sahara dust fluxes decreased by at least 50% between the last deglaciation and the mid Holocene, while the Northern Sector of the Red Sea remained unchanged. This constrains the African Humid Period impact to have extended up to ca. 22°N, across a more limited region than previously thought.https://doi.org/10.1038/s41467-019-11701-z |
spellingShingle | Daniel Palchan Adi Torfstein A drop in Sahara dust fluxes records the northern limits of the African Humid Period Nature Communications |
title | A drop in Sahara dust fluxes records the northern limits of the African Humid Period |
title_full | A drop in Sahara dust fluxes records the northern limits of the African Humid Period |
title_fullStr | A drop in Sahara dust fluxes records the northern limits of the African Humid Period |
title_full_unstemmed | A drop in Sahara dust fluxes records the northern limits of the African Humid Period |
title_short | A drop in Sahara dust fluxes records the northern limits of the African Humid Period |
title_sort | drop in sahara dust fluxes records the northern limits of the african humid period |
url | https://doi.org/10.1038/s41467-019-11701-z |
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