Climatic and biotic upheavals following the end-Permian mass extinction-Reference-Cited by-同舟云学术

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Climatic and biotic upheavals following the end-Permian mass extinction

Published:2012-12-21 Issue:1 Volume:6 Page:57-60
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Romano Carlo,Goudemand Nicolas,Vennemann Torsten W.,Ware David,Schneebeli-Hermann Elke,Hochuli Peter A.,Brühwiler Thomas,Brinkmann Winand,Bucher Hugo

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo1667.pdf

Reference31 articles.

1. Meyer, K. M., Yu, M., Jost, A. B., Kelley, B. M. & Payne, J. L. δ13C evidence that high primary productivity delayed recovery from end-Permian mass extinction. Earth Planet. Sci. Lett. 302, 378–384 (2011).

2. Payne, J. L. & Kump, L. R. Evidence for recurrent Early Triassic massive volcanism from quantitative interpretation of carbon isotope fluctuations. Earth Planet. Sci. Lett. 256, 264–277 (2007).

3. Wignall, P. B. The end-Permian mass extinction—how bad did it get? Geobiology 5, 303–309 (2007).

4. Brayard, A. et al. The Early Triassic ammonoid recovery: Paleoclimatic significance of diversity gradients. Palaeogeogr. Palaeoclimatol. Palaeoecol. 239, 374–395 (2006).

5. Brühwiler, T., Bucher, H., Brayard, A. & Goudemand, N. High-resolution biochronology and diversity dynamics of the Early Triassic ammonoid recovery: The Smithian faunas of the Northern Indian Margin. Palaeogeogr. Palaeoclimatol. Palaeoecol. 297, 491–501 (2010).

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