Articles | Volume 19, issue 9
https://doi.org/10.5194/cp-19-1743-2023
https://doi.org/10.5194/cp-19-1743-2023
Research article
 | 
05 Sep 2023
Research article |  | 05 Sep 2023

Carbon isotope chemostratigraphy, geochemistry, and biostratigraphy of the Paleocene–Eocene Thermal Maximum, deepwater Wilcox Group, Gulf of Mexico (USA)

Glenn R. Sharman, Eugene Szymanski, Rebecca A. Hackworth, Alicia C. M. Kahn, Lawrence A. Febo, Jordan Oefinger, and Gunnar M. Gregory

Viewed

Total article views: 2,779 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,742 945 92 2,779 172 98 125
  • HTML: 1,742
  • PDF: 945
  • XML: 92
  • Total: 2,779
  • Supplement: 172
  • BibTeX: 98
  • EndNote: 125
Views and downloads (calculated since 09 Dec 2022)
Cumulative views and downloads (calculated since 09 Dec 2022)

Viewed (geographical distribution)

Total article views: 2,779 (including HTML, PDF, and XML) Thereof 2,760 with geography defined and 19 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 06 Dec 2025
Download
Short summary
This study examines deepwater deposits within the Gulf of Mexico (USA) that record an episode of pronounced global warming that occurred ∼56 million years ago. We show that the supply of sand and silt into the basin shut off after a delay of about 30 000 years, followed by an influx of clay derived from deep erosion of central North America. Our results are consistent with other studies that indicate rapid sea-level rise, ocean acidification, and decreased oxygen during this warming event
Share