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By Martire L. (Ed.)

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Aveiro, 261pp. Canérot J. et al. (1995): C. R. Acad. Sei. Paris, Série lia, 320, 523-530 Eder W. (1999): N. Jb. Geol. Paläont. , 214, 1/2, 353-358 Fürsich F. & Werner W. (1986): N. Jb. Geol. Paläont. , 172, 3, 271-329 Leinfelder R. (1996): Geol. Runschau, 76/2, 599-631 Martin T. & Krebs B. (2000): Ed. Verlag Dr. Friedrich Pfeil, München, 155pp. Pena dos Reis R. et ai. (2000): GeoResearch Forum, 6, 345-356. Ravnas R. et al. , 114, 237-266 Ricqles A. et al. (2001): Compt. Rend. Académie Sciences - Série lia, 332, 10, 647-656 Wilson R.

This datum is in agreement with the ages provided by radiolarians and allows to assign for the first time a Bathonian age (probably early Bathonian) to the lower part of the Radiolaritic unit, not excluding a Bajocian age for its basalmost zone. The underlying unit of basaltic pillow lavas and hyaloclastites records a magmatic event that predates the onset of the biosiliceous sedimentation in this sector, leading to the deposition of siliceous limestones and radiolarites. This unit locally overlies Lower Toarcian pelagic radiolarian cherty limestones (Calcari di Santa Maria del Bosco).

The types of long and broad dominate the coniferous group both the South China flora and North China Flora. It seems that the palaeoclimate in China during EarlyMiddle Jurassic is warm and humid. 47 VI INTERNATIONAL SYMPOSIUM ON THE JURASSIC SYSTEM, PALERMO 12-22 SEPTEMBER 2002 was converted to a gradually steepening slope. , 2002). As indicated by an intense brittle deformational event that dissected the upper levels of the Rosso Ammonitico inferiore, during Late Callovian to Mid Oxfordian times synsedimentary tectonics intensified resulting in an increase of the inclination of the slope.

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6th International Symposium on the Jurassic System, September 12-22 2002, Palermo. Abstracts and program by Martire L. (Ed.)


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