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Thus, both the Bimammatum and Hauffianum Subzones of - FIFTH INTERNATIONAL SYMPOSIUM OF IGCP 506 Hammamet (Tunisia). March. 28-31, 2008 the Submediterranean Bimammatum Zone, and the Planula Zone should be accommodated in the Kimmeridgian. This stratigraphical interval of the Submediterranean Succession with upper boundary at the base of the Galar Subzone correlates with the Boreal Bauhini Zone. Because of this, and its well defined character of ammonite fauna, it is proposed here as the Lower Kimmeridgian Substage.
The recent studies of the Unzha River sections on the Russian Platform about 500 km NE from Moscow, and about 3000 km from the Staffin Bay section have revealed a thin, but stratigraphically fairly complete succession of ammonites indicating the presence of nearly all the Boreal and Subboreal standard ammonite zones of the Middle-Upper Oxfordian and lowest Kimmeridgian (Glowniak, Kiselev, Rogov, Wierzbowski, Wright in preparation). The OxfordianlKimmeridgian boundary can be recognised using almost the same faunistic criteria as in the Staffin Bay section: the appearance of the first representatives of Pictonia (but additionally with closely related representatives of Vineta) (M), and Prorasenia (m), as well as of the first Amoeboceras (Plasmatites).
SEISMIC SEQUENCE STRATIGRAPHY OF THE JURASSIC OF THE CENTRAL ATLAS, TUNISIA f '~Bpartementdes Sciences de la Term, Facult6 des Scieoces de Gafsa. Gafsa 2112. 2050 Hammam-Lit. Tunisie The compilation of outcrop and available subsurface data provided by wells drilled in the Tunisian Atlasic zone has permitted the establishment of a general palaeogeographical reconstruction showing the Jurassic basin and platform distribution. New seismic interpretation also helped in characterizing several seismic sequences within the buried Jurassic series and in setting up several seismic stratigraphic sections, isochron and isopach maps.