The Upper Jurassic biostratigraphy, so far limited to the J. Zaress, is ext
ended to the ranges of the Tunisian Dorsale. The AR facies (Fm Zaress) begi
ns as early as the Middle/Upper Callovian and ranges up into the Lower Kimm
eridgian (Planula Zone). Above, the grey limestones and overlying beds (Res
sas Fm) span the rest of the Kimmeridgian and the Tithonian. Compared to th
e north-south axis, the Ammonitico Rosso facies develops earlier in the Dor
sale on starving shoals while AR of J. El Haouareb are slope deposits fed f
rom the north-south axis heights, where Callovian and Oxfordian are reduced
or absent. ((C) Academie des sciences / Elsevier, Paris.).