The demise of the rudist-bearing carbonate platforms at the Cenomanian/Turonian boundary: a global control

Author:

Philip J. M.,Airaud-Crumiere C.

Publisher

Springer Science and Business Media LLC

Subject

Aquatic Science

Reference50 articles.

1. Abdallah H (1989) Les transgressions du Crétacé moyen entre les jeux tectoniques et les montées eustatiques (Sud Tunisien). In: Cotillon P (ed) Les événements de la partie moyenne du Crétacé (Aptien à Turonien), vol 11. Géobios, Lyon, pp 83?94

2. Arthur MA, Schlanger SO, Jenkins HC (1987) The cenomanian-Turonian oceanic anoxic event, II. Palaeoceanographic controls on organic matter production and preservation. In: Brooks J, Fleet A (eds) Marine petroleum source rocks. Spec Pub Geol Soc 26:401?420

3. Arthur MA, Dean WE, Pratt LM (1988) Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turoniam boundary. Nature 335:714?717

4. Barron EJ, Washington WM (1982) Cretaceous climate: a comparison of atmospheric simulations with the geologic record. Palaeogeogr Palaeoclimatol Palaeoecol 40:103?133

5. Berthou PY (1984) Albian-Turonian stage boundaries and subdivisions in the Western Portuguese Basin, with special emphasis on the Cenomanian-Turonian boundary in the ammonite facies and rudist facies. Bull Geol Soc Denmark 33:41?55

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