The Souar Formation dates to the end of the Eocene and is made up of marine clay, marl, sand and gypsum. The Fortuna Formation in the Cap Bon area records the Oligocene with sandy limestone and marls, overlain by coarse sandstones and quartz pebbles, although it fades out in southern Tunisia. Other Cenozoic units include the Ain Grab Group and Oum Domil Formation.