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Additional info for 4th Symposium IGCP-506, University of Bristol, 4-8 July 2007, Abstracts

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It allows to offer a specified variant ofthis interval correlation (see the table). For simplification only cardioceratids and kosmoceratid taxa are shown on the scheme, though all the groups of ammonites (Macrocephalitidae, Perisphinctidae, Oppeliidae and Spiroceratidae) were involved for correlation. Intervals without kosmoceratids are displayed by color - in most cases these lacunas couldn't be explained by the incompleteness of geological annals or collections. The initial Kepplerites (Kepplerites) appeared at first in Greenland, then in Russia, and only after that- in Western Europe; the extinction of this subgenus [the last of species - K.

In the lower part ofthe unit there is the lowest oil shale Bed IH with the highest heat of combustion. 9m. The total thickness ofthe unit ranges from 3-4m up to l2m. 29 The upper unit is composed of dark grey claystones, kerogen enriched clays tones and oil shales. There are two oil shale beds: the Bed II and the Bed I. They both consist of series of thin OS bands separated with kerogen-enriched clays. The total thickness of the unit exceeds 10m. The fauna in the D. panderi Zone is represented by abundant molluscs (bivalves, gastropods,cephalopods) and rare by lingulid brachiopods.

Cranocephaloide, K. P. Wimbledon Dept. uk In other parts of the Phanerozoic, subcommissions have taken radical actions, and have simply dropped traditional stratotype sections, choosing new GSSPs, and in some cases placed them on the other side ofthe world. But, it seems reasonable to try to define a J-K boundary while maintaining continuity with more recent historical understanding of the scope of the uppermost Jurassic and the lowest Cretaceous - thus to choose somewhere a GSSP that is close to the traditional biozonal definition of a Berriasian base, and one therefore in the marine sequences.

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4th Symposium IGCP-506, University of Bristol, 4-8 July 2007, Abstracts by Wimbledon W.A.P. (coord.)

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