Articles | Volume 21, issue 6
https://doi.org/10.5194/cp-21-1025-2025
https://doi.org/10.5194/cp-21-1025-2025
Research article
 | 
13 Jun 2025
Research article |  | 13 Jun 2025

Controls of aeolian and fluvial sediment influx to the northern Red Sea over the last 220 000 years

Werner Ehrmann, Paul A. Wilson, Helge W. Arz, and Gerhard Schmiedl

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AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (19 Mar 2025) by Antje Voelker
AR by Werner Ehrmann on behalf of the Authors (24 Mar 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (24 Mar 2025) by Antje Voelker
AR by Werner Ehrmann on behalf of the Authors (25 Mar 2025)  Manuscript 
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Short summary
We report palaeoclimate and sediment provenance records for the last 220 kyr from a sediment core from the northern Red Sea. They comprise high-resolution grain size, clay mineral, and geochemical data, together with Nd and Sr isotope data. The data sets document a strong temporal variability in dust influx on glacial–interglacial timescales and several shorter-term strong fluvial episodes. A key finding is that the Nile delta became a major dust source during glacioeustatic sea-level lowstands.
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