Abstract: In the area studied Cambrian to Triassic systems are distinguished by the use of conodonts and their fauna isdeseribed briefly. It is believed that the metamorphic Alanya massif overlays the Sedre Triassic as a nappe, forming atectonic window. Hadimopanella oezgueli n. gen. n. sp. (incertae sedis) and three new conodont species are established.