Paleotethys seawater temperature rise and an intensified hydrological cycle following the end-Permian mass extinction.

Journal article


Publication Details

Author(s): Schobben M, Joachimski M, Korn D, Leda L, Korte C
Journal: Gondwana Research
Publisher: Elsevier
Publication year: 2014
Volume: 26
Pages range: 675-683
ISSN: 1342-937X


FAU Authors / FAU Editors

Joachimski, Michael Prof. Dr.
Lehrstuhl für Geologie (Exogene Dynamik)


External institutions
Leibniz Institute for Evolution and Biodiversity Science / Leibniz-Institut für Evolutions- und Biodiversitätsforschung
University of Copenhagen


How to cite

APA:
Schobben, M., Joachimski, M., Korn, D., Leda, L., & Korte, C. (2014). Paleotethys seawater temperature rise and an intensified hydrological cycle following the end-Permian mass extinction. Gondwana Research, 26, 675-683. https://dx.doi.org/10.1016/j.gr.2013.07.019

MLA:
Schobben, Martin, et al. "Paleotethys seawater temperature rise and an intensified hydrological cycle following the end-Permian mass extinction." Gondwana Research 26 (2014): 675-683.

BibTeX: 

Last updated on 2018-09-08 at 16:39