FIGURE 2. 2.1. Type locality of Cladocyclus pankowskii sp. nov. The holotype was not found in situ, and the locality may only be identified as the Taouz area. 2.2. Section through Kem Kem beds. The holotype and jaw specimen described here undoubtedly come from the ferruginous sandstone horizon. After Forey and Grande (1998).