By Hart M.B. (Ed.)
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Extra resources for 8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume
With a detailed lithostratigraphic subdivision of the midSantonian to uppermost Maastrichtian available now, stratigraphic ranges of the various species can be determined in much more detail than in Bosquet's days. In addition, recent fieldwork has yielded a few species unknown to Bosquet. A sound taxonomic frame is now being worked out. I firmly believe that on the basis of cirripedes, assemblage zones can be established, similar to what has been achieved in the Upper Cretaceous and Eocene of the United States.
K. , Hart, M. , Leary, P. , Tocher, B. , Home, D. & Rosenfeld, A. 1988. Microfossil assemblages and the Cenomanian-Turonian (Late Cretaceous) oceanic anoxic event. Cretaceous Research, 9, 3-103. Whatley, R. 1991. The platycopid signal: a means of detecting kenoxic events using Ostracoda. Journal of Micropalaeontology, 10(2), 181-185. Whatley, R. C , Pyne, R. S. & Wilkinson , I. P. 2003. Ostracoda and palaeo-oxygen levels, with particular reference to the Upper Cretaceous of East Anglia. Palaeogeography, Palaeoclimatology, Palaeoecology, 194, 355-386.
Geochemistry of Lower Cretaceous limestones of the Mural Formation of the Bisbee Group, Sonora, Mexico  1 1 Madhavaraju, J . , Gonzalez-Leon, C M . & Yong II Lee 2 1 Estaci6n Regional del Noroeste, Instituto de Geologia, Universidad Nacional Autonoma de Mexico, Apartado Postal 1039 Hermosillo, Sonora 83000, Mexico. com The Aptian-Albian limestones of Mural Formation well exposed in a 300 km long transect which extends from Sierra El Chanate (westernmost part) to Cerro El Caloso Pitaycachi.
8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume by Hart M.B. (Ed.)