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By Hart M.B. (Ed.)

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Extra info for 8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume

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2009. An Early Albian Arctic-type ammonite Arcthoplites from Hokkaido, northern Japan, and its paleobiogeographic and paleoclimatological implications. Journal of Asian Earth Sciences, 34, 4 6 - 5 0 . Iba, Y. & Sano, S. 2007. Mid-Cretaceous step-wise demise of the carbonate platform biota in the Northwest Pacific and establishment of the North Pacific biotic province. Palaeogeography, Palaeoclimatology, Palaeoecology, 245, 462-482. Iba, Y. & Sano, S. 2008. Paleobiogeography of the pectinid bivalve Neithea, and its pattern of step­ wise demise in the Albian Northwest Pacific.

S. 1994. Strontium isotope stratigraphy for Late Cretaceous time: Direct numerical calibration of the Sr isotopic curve based on the US Western Interior. Palaeogeography, Palaeoclimatology, Palaeoecology, 108, 95-119. Late Cretaceous (Campanian-Maastrichtian) scaphitid ammonites from the Pierre Shale and Bearpaw Shale of North America [841] 1 2 3 4 Landman, N. H. , Kennedy, W. J . , Cobban, W. A. & Larson, N. com Scaphitid ammonites (Scaphites) are common in the Upper Cretaceous Pierre Shale and Bearpaw Shale of the Western Interior of North America.

Garcfa-Mondejar, J . 1 1 Departamento 2 Geological de Estratigrafia y Paleontologia, Facultad de Ciencia y Technologia, Universidad del Pais Vasco, Apartado 644, 48080 Bilbao, Spain Institute, Swiss Federal Institute of Technology Zurich, Sonneggstr. es The Early Aptian is known as a period of major carbon cycle perturbations, which are recorded in the 6 C r b and 5 C values. A pronounced negative carbon-isotope excursion and a major positive excursion have been observed worldwide. The beginning of OAE1a coincides with the negative spike in the carbon isotope curve, and is followed by a positive carbon isotope excursion.

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