21127 - Rare Bavarilla zemmourensis Lower Ordovician Trilobite Fezouata Fm Carboniferous Plants Evolution of the side-necked turtles:

Evolution of the side-necked turtles: The families Bothremydidae

These areas of alteration are visible by dark areas on the cut and polished surface

anatomical comparisons demonstrate that the aglaspidids cannot be accommodated within the chelicerates

France (1)

083g of this RARE type of MARTIAN Shergottite METEORITE

21127 - Rare Bavarilla zemmourensis Lower Ordovician Trilobite Fezouata Fm Carboniferous Plants Evolution of the side-necked turtles:Bavarilla sp, Barrande 1868 (trilobite) Trilobita Phacopida Bavarillidae Positive Negative specimen. 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