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

Viewed

Total article views: 1,425 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,087 265 73 1,425 117 67 72
  • HTML: 1,087
  • PDF: 265
  • XML: 73
  • Total: 1,425
  • Supplement: 117
  • BibTeX: 67
  • EndNote: 72
Views and downloads (calculated since 08 Aug 2023)
Cumulative views and downloads (calculated since 08 Aug 2023)

Viewed (geographical distribution)

Total article views: 1,425 (including HTML, PDF, and XML) Thereof 1,390 with geography defined and 35 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 12 Jul 2025
Download
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.
Share