Articles | Volume 20, issue 1
https://doi.org/10.5194/cp-20-267-2024
https://doi.org/10.5194/cp-20-267-2024
Research article
 | 
02 Feb 2024
Research article |  | 02 Feb 2024

Changes in the Red Sea overturning circulation during Marine Isotope Stage 3

Raphaël Hubert-Huard, Nils Andersen, Helge W. Arz, Werner Ehrmann, and Gerhard Schmiedl

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Short summary
We have studied the geochemistry of benthic foraminifera (micro-fossils) from a sediment core from the Red Sea. Our data show that the circulation and carbon cycling of the Red Sea during the last glacial period responded to high-latitude millennial-scale climate variability and to the orbital influence of the African–Indian monsoon system. This implies a sensitive response of the Red Sea to climate changes.