| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4690309 | Sedimentary Geology | 2009 | 19 Pages |
Abstract
As for many other Tethyan localities the carbon isotope record from Tulong is characterized by a late Griesbachian-Dienerian positive δ13Ccarb excursion (2â°), and a very prominent positive excursion (5â°) at the Smithian-Spathian boundary, thus confirming the well-documented perturbations of the global carbon cycle following the Permian-Triassic mass extinction event.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Thomas Brühwiler, Nicolas Goudemand, Thomas Galfetti, Hugo Bucher, Aymon Baud, David Ware, Elke Hermann, Peter A. Hochuli, Rossanna Martini,