| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6443804 | Journal of African Earth Sciences | 2014 | 34 Pages |
Abstract
The combined data emphasize that most of the Chouabine Formation in the Gafsa Basin was deposited during the late Paleocene. The most negative isotopic values from marls are believed to represent the onset of PETM or pre-PETM record, and the related perturbation of the carbon cycle in shallow water deposits in Tunisia.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
László Kocsis, Anouar Ounis, Claudia Baumgartner, Claudius Pirkenseer, Ian C. Harding, Thierry Adatte, Fredj Chaabani, Salah Mohamed Neili,