Articles | Volume 21, issue 11
https://doi.org/10.5194/cp-21-2115-2025
https://doi.org/10.5194/cp-21-2115-2025
Research article
 | 
11 Nov 2025
Research article |  | 11 Nov 2025

Oligocene-early Miocene paradox of pCO2 inferred from alkenone carbon isotopic fractionation and sea surface temperature trends

José Guitián, Samuel Phelps, Reto S. Wijker, Pratigya J. Polissar, Laura Arnold, and Heather M. Stoll

Viewed

Total article views: 1,746 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,303 364 79 1,746 132 82 99
  • HTML: 1,303
  • PDF: 364
  • XML: 79
  • Total: 1,746
  • Supplement: 132
  • BibTeX: 82
  • EndNote: 99
Views and downloads (calculated since 18 Oct 2024)
Cumulative views and downloads (calculated since 18 Oct 2024)

Viewed (geographical distribution)

Total article views: 1,746 (including HTML, PDF, and XML) Thereof 1,698 with geography defined and 48 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 09 Jan 2026
Download
Short summary
We reconstructed from sediments of different ocean sites phytoplankton carbon isotopic fractionation (εp), mainly linked to CO2 variations, during the Oligocene to early Miocene. Data confirm Cenozoic long-term CO2 record but show contrasting relationships with the sea surface temperatures evolution. We evaluate the role of non-CO2 environmental factors such as temperature and nutrients at each site εp, highlighting the complexity of interpreting climate dynamics and CO2 reconstructions.
Share