Articles | Volume 21, issue 8
https://doi.org/10.5194/cp-21-1405-2025
https://doi.org/10.5194/cp-21-1405-2025
Research article
 | 
01 Aug 2025
Research article |  | 01 Aug 2025

The Eocene–Oligocene Transition in the Paratethys: boreal water ingression and its paleoceanographic implications

Mustafa Yücel Kaya, Henk Brinkhuis, Chiara Fioroni, Serdar Görkem Atasoy, Alexis Licht, Dirk Nürnberg, and Taylan Vural

Viewed

Total article views: 598 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
429 148 21 598 43 18 26
  • HTML: 429
  • PDF: 148
  • XML: 21
  • Total: 598
  • Supplement: 43
  • BibTeX: 18
  • EndNote: 26
Views and downloads (calculated since 18 Feb 2025)
Cumulative views and downloads (calculated since 18 Feb 2025)

Viewed (geographical distribution)

Total article views: 598 (including HTML, PDF, and XML) Thereof 581 with geography defined and 17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 02 Aug 2025
Download
Short summary
The Eocene–Oligocene Transition (EOT) marked global cooling and Antarctic glaciation, but its impact on marginal seas is less known. This study analyzes the Karaburun section in the eastern Paratethys, using biostratigraphy and geochemistry to reveal boreal water ingress due to Arctic–Atlantic gateway closure. Findings highlight the interplay of global and regional climate dynamics in shaping marginal marine environments.
Share