Marine ostracod faunas through the Late Devonian extinction events. Part I: The Kellwasser event

Author:

Guillam Elvis,Forel Marie-Béatrice,Crasquin Sylvie

Publisher

Elsevier BV

Reference188 articles.

1. Contributions to Palaeozoic Ostracod Classification [POC], N° 41. “Non kloedenellacean” ostracods - 1. Family Geisinidae Sohn, 1961. Assured podocopines;Adamczak;Neues Jahrb. Geol. Palaontol. Abh.,2006

2. Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events;Algeo;Philos. Trans. R. Soc. B,1998

3. Land plant evolution and weathering rate changes in the Devonian;Algeo;J. Earth Sci.,2010

4. Late Devonian oceanic anoxic events and biotic crises: "rooted" in the evolution of vascular land plants?;Algeo;Geol. Soc. America, GSAToday,1995

5. Effects of the middle to late Devonian spread of vascular land plants on weathering regimes, marine biotas, and global climate;Algeo,2001

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