Articles | Volume 22, issue 6
https://doi.org/10.5194/cp-22-1223-2026
https://doi.org/10.5194/cp-22-1223-2026
Research article
 | 
22 Jun 2026
Research article |  | 22 Jun 2026

The Marine Isotopic Stage 7: a relic of the “41 ka world”? Perspectives from a global-scale sea-surface temperature synthesis

Etienne Legrain, Nathan Stevenard, Emilie Capron, Frédéric Parrenin, and Natalia Vazquez Riveiros

Viewed

Total article views: 3,635 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,306 1,122 207 3,635 466 132 142
  • HTML: 2,306
  • PDF: 1,122
  • XML: 207
  • Total: 3,635
  • Supplement: 466
  • BibTeX: 132
  • EndNote: 142
Views and downloads (calculated since 28 Nov 2025)
Cumulative views and downloads (calculated since 28 Nov 2025)

Viewed (geographical distribution)

Total article views: 3,635 (including HTML, PDF, and XML) Thereof 3,617 with geography defined and 18 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 22 Jun 2026
Download
Short summary
To better understand climate drivers during a warm period ~200,000 years ago, we reconstructed global surface temperature using 132 marine records placed on a common timeline. We found strong hemispheric differences and showed that the warmest phase occurred despite lower CO2 levels. In addition, we suggest that extreme orbital forcing temporarily shifted the climate into the older 41,000-year rhythm, resulting in a hybrid warm period shaped by both 100,000-year and 41,000-year climate dynamics.
Share