Abstract
Sharks at the cladodont and hybodont level (Paleozoic and Mesozoic) have blunt fangs and crushing teeth. These are covered by a thin sculptured uniform “enamel” cap, with a high compressive strength. The radiation of the modern sharks in the middle Mesozoic leads primarily to a broad spectrum of different sharks with a fang, or cutting tooth dentition. This radiation is accompanied by modifications of anatomical characters of the shark's body but also by the development of three new “enamel” types, which give the teeth bending and compressive strength.