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Extra resources for 4th Symposium IGCP-506, University of Bristol, 4-8 July 2007, Abstracts
Later attempts to fix a Neocomian base in marine successions have brought suggested ammonite bases that fluctuated up anddown, or remained vague. What were later recognised as Tithonian faunas were used to define the Berriasian: and Toucas even placed the stage in the Jurassic. And the facies and fossils that defined Berriasian in its type area were at the outset known to be far from global. It is possible now to go beyond the two Cretaceous colloquia, gatherings of specialists who predominantly worked in the western Mediterranean and founded their decision on consideration ofTethyan ammonites only.
Aff. tol e G. ;;:==tl: = tl: U Gowerianus Elatmae Herveyi e Calloviense 35 S. calloviense, C. aff. geerzense 34 G. galilaeii, C. coriniense? 33 G. gowerianus, C. aff. sokolovi ? C. geerzense viense Koenigi S. calloviense, East Greenland Ammonites Zone FH Subpatruus Subzone Camptus Subzone r.. ~ C. sokolovi C. sokolovi, Ch. buckmani, G. curtilobus Ch. buckmani, G. owerianus Ch. stuckenbergi, G. aff. toricelli Ch. subpatruus, G. russiensis Ch. surensis, G. russiensis C. stupachenkoi, G. russiensis Ch.
Box 106, Bratislava 45,84005, Slovak Republic. sk The NorianlRhaetian boundary ofthe Fatra basin in the Western Carpathians is known as a transition from the lagoonal or limnic environments to the typical marine conditions. The marine transgression recorded in these deposits represents onset of new live habits, with bivalves being the early successional organisms which inhabited the sea bottom. The section Kardolina exposes Norian-Rhaetian sediments rich in fossils, which pass into the Lower Jurassic.