Articles | Volume 22, issue 2
https://doi.org/10.5194/cp-22-357-2026
https://doi.org/10.5194/cp-22-357-2026
Research article
 | 
12 Feb 2026
Research article |  | 12 Feb 2026

Decoding the North Atlantic Ocean circulation breakthrough in the Aptian–Albian transition

João M. F. Ramos, Jairo F. Savian, Daniel R. Franco, Milene F. Figueiredo, Rodolfo Coccioni, and Fabrizio Frontalini

Viewed

Total article views: 2,342 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,079 213 50 2,342 70 67
  • HTML: 2,079
  • PDF: 213
  • XML: 50
  • Total: 2,342
  • BibTeX: 70
  • EndNote: 67
Views and downloads (calculated since 27 Aug 2025)
Cumulative views and downloads (calculated since 27 Aug 2025)

Viewed (geographical distribution)

Total article views: 2,342 (including HTML, PDF, and XML) Thereof 2,243 with geography defined and 99 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 04 Mar 2026
Download
Short summary
During the Aptian–Albian interval of the Cretaceous, Earth's climate changed significantly due to volcanism, atmospheric shifts, and reorganised ocean circulation. These changes influenced marine sediments, especially reddish Cretaceous oceanic red beds (CORBs), which reflect intervals of deep-ocean oxygenation. This study analysed sediment cores from ODP Site 1049 (North Atlantic) to determine when CORBs formed and whether similar patterns occurred in other basins, such as the Tethys.
Share