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

Buggisch W, Joachimski M (2002)

Publication Type: Journal article, Original article

Publication year: 2002

Journal

Geology Geological Society of America

Publisher: Geological Society of America

Book Volume: 30

Pages Range: 711-714

Journal Issue: 8

DOI: 10.1130/0091-7613(2002)030<0711:CAOSIC>2.0.CO;2

Authors with CRIS profile

Werner Buggisch Naturwissenschaftliche Fakultät Michael Joachimski 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.

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