Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction

Journal article
(Original article)


Publication Details

Author(s): Buggisch W, Joachimski M
Journal: Geology
Publisher: Geological Society of America
Publication year: 2002
Volume: 30
Journal issue: 8
Pages range: 711-714
ISSN: 0091-7613


FAU Authors / FAU Editors

Buggisch, Werner Prof. Dr.
Naturwissenschaftliche Fakultät
Joachimski, Michael Prof. Dr.
Lehrstuhl für Geologie (Exogene Dynamik)


How to cite

APA:
Buggisch, W., & Joachimski, M. (2002). Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction. Geology, 30(8), 711-714. https://dx.doi.org/10.1130/0091-7613(2002)030<0711:CAOSIC>2.0.CO;2

MLA:
Buggisch, Werner, and Michael Joachimski. "Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction." Geology 30.8 (2002): 711-714.

BibTeX: 

Last updated on 2018-26-12 at 13:50