20566 - Top Rare 1.12 Inch Foulonia sp Lower Ordovician Trilobite Fezouata Formation Coprolites Enchodus oxytomus

Enchodus oxytomus

It has some glued fractures al the tip of one tooth

Some authors have proposed this species as the predecessor of the current white shark (Great White-Carcharodon carcharias) and the great Carcharodon megalodon

The serrations in its edges are very similar to the ones that would later acquire the Great White Shark

20566 - Top Rare 1.12 Inch Foulonia sp Lower Ordovician Trilobite Fezouata Formation Coprolites Enchodus oxytomusFoulonia sp, Pribyl and Vanek 1985 (trilobite) Trilobita Phacopida The Fezouata Formation occurs in the lower part of the Lower to lower Middle Ordovician Outer Feijas Group, in the western, central and eastern Anti Atlas Mountains, southern Morocco (Destombes et al. 1985; Gutierrez Marco & Martin 2016). It comes from The Konservat Lagersttten of Lower Fezouata Fm that spans the entire Tremadoc stage of the Ordovician system and is only present in the