20568 - Insane Association Foulonia sp + Ampyx sp Lower Ordovician Trilobites Fezouata Formation Corals organic debris and other sediments

organic debris and other sediments that can form when lightning discharges into ground

• Jurassic to Cretaceous of France

Parent taxon: Enchodontidae according to C

From the proximal end to the tip of the distal end

Ga 58 μg/g

20568 - Insane Association Foulonia sp + Ampyx sp Lower Ordovician Trilobites Fezouata Formation Corals organic debris and other sedimentsFoulonia sp, Pribyl and Vanek 1985 (trilobite) Trilobita Phacopida Ampyx sp, Dalman 1827 (trilobite) Trilobita Asaphida Raphiophoridae 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