The role of sea-level change and marine anoxia in the Frasnian–Famennian (Late Devonian) mass extinction

Author:

Bond David P.G.,Wignall Paul B.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference82 articles.

1. Terrestrial–marine teleconnections in the Devonian; links between the evolution of land plants, weathering processes, and marine anoxic events;Algeo;Philosophical Transactions of the Royal Society of London, Series B,1998

2. Late Devonian oceanic anoxic events and biotic crises: ‘rooted’ in the evolution of vascular land plants?;Algeo;GSA Today,1995

3. Mountain building-enhanced continental weathering and organic carbon burial as major causes for climatic cooling at the Frasnian–Famennian boundary (c. 376 Ma)?;Averbuch;Terra Nova,2005

4. Stratigraphische Gliederung und Ammonoideen-Faunen im Nehdenium (Oberdevon II) von Europa und Nord-Afrika;Becker;Courier Forschung-Institut Senckenberg,1993

5. Kellwasser events and goniatite successions in the Devonian of the Montagne Noire with comments on possible causations;Becker;Courier Forschung-Institut Senckenberg,1994

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