Über den Kieferapparat der Lytoceratacea (Ammonoidea)

The jaw apparati of Paleozoic and Triassic ammonoids are simìlar in shape to parrots’ beaks; they possess sharp cutting-edges and consist of chitinous material. Together with the similar jaw apparati of recent Coleoids, they constitute the Normal-Type of cephalopod jaws. The jaw apparati of the Jurassic-Cretaceous ammonites possess wide, shovel-like lower jaws without cutting-edges. They consist either of an undivided chitinous plate (Anaptychus) or of this and two additional calcitic plates (Aptychi) on its outer flanks. Jaw apparati of this type are here called Aptychus-Type jaws. New finds in the Upper Cretaceous of Japan suggest the existence of a third type of jaw apparatus which is here called the Rhynchaptychus-Type. Jaws of this type are mainly characterized by possession of calcitic rostra on the tips of the jaws. They seem to be restricted to members of the order Lytoceratacea (excluding the Heteromorphs).