20566 - Top Rare 1.12 Inch Foulonia sp Lower Ordovician Trilobite Fezouata Formation Coprolites The serrations in its edges

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

Well preserved specimen

Its orange colors come from the limonite (iron oxide) that is the product of the oxidation of the original pyrite that mineralized these fossils

Reptilia - Loricata - Dyrosauridae

Rooted teeth

20566 - Top Rare 1.12 Inch Foulonia sp Lower Ordovician Trilobite Fezouata Formation Coprolites The serrations in its edgesFoulonia 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