The Antalya nappes (western Taurides-Turkey)*consist of several tectonic units which document the*Southern Neotethyan paleomargin from the Arabo-African*shallow shelf to the oceanic crust.*The Kerner Gorge Units (Upper Antalya nappes)*show a full stratigraphical succession from Ordovician*to Late Cretaceous. A carbonate platform regime*appeared during Late Permian times and existed up*to the early Middle Triassic. For detailed investigations*on the Permo-Triassic boundary, two lithostratigraphic*profiles have been selected: the Curuk*dag and the Kerner Gorge sections.*The main results presented in this paper are : 1) the Late Permian Pamucak Formation (Midian-*Dzhulfian) consists of calcareous algae-foraminiferae*bearing black limestones, locally rich in*brachiopods, crinoids and bryozoae : 2) this black limestone is overlain by an oolitic*grainstone. In the Curuk dag section, the oolitic horizon*is capped by a thin level of calcrete type; emersive*conditions are also inferred by a strong diagenetic*change within the oolitic deposit : 3) the first Early Triassic fossils, appearing*within or above the oolitic grainstone, are microforaminifera*and Pseudoclaraia wangi (late Griesbachian*in age). In the Curuk dag, a rich Early Triassic*microforaminifera association seems linked to a microbiallite*boundstone facies : 4) the overlying unfossiliferous lime mudstone,*the oolitical thick bedded grainstone, the variegated*marly limestone and the vermicular limestone facies*are present. not only in southern Turkey but seem*constant through ' the entire peri arabo-african platform.*Striking similarities appear between the studied*profiles and the Bellerophon-Werfen succession in the*Southern Alps..