The Cenomanian–Turonian boundary mass extinction (Late Cretaceous): New insights from ammonoid biodiversity patterns of Europe, Tunisia and the Western Interior (North America)

Author:

Monnet Claude

Publisher

Elsevier BV

Subject

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

Reference176 articles.

1. La géochimie isotopique du carbone (δ13C) comme outil stratigraphique. Application à la limite Cénomanien/Turonien en Tunisie centrale;Accarie;C. R. Acad. Sci. Paris,1996

2. Position de la limite Cénomanien–Turonien dans la Formation Bahloul de Tunisie centrale: apports intégrés des ammonites et des isotopes du carbone (δ13C);Amédro;Eclogae Geol. Helv.,2005

3. Variations in the global carbon cycle during the Cretaceous related to climate, volcanism, and changes in atmospheric CO2;Arthur,1985

4. The Cenomanian–Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation;Arthur;Spec. Publ. Geol. Soc. Lond.,1987

5. Geochemical effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary;Arthur;Nature,1988

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