Controls of aeolian and fluvial sediment influx to the northern Red Sea over the last 220 000 years
<p>Present-day sediment influx to the northern Red Sea is dominated by aeolian dust because of its position between the large deserts of northern Africa, the Arabian Peninsula, and the Levant, as well as the absence of discharge from perennial rivers. However, sediment cores retrieved from th...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-06-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/21/1025/2025/cp-21-1025-2025.pdf |
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