Here is a inexpensive Vendian Ediacara fossil of the species Kimberella quadrata a from the Verkhovka Formation of the Solza River fossil site. Unfortunately, the Kimberella is not completely preserved, but the plate still shows some grazing traces. This ichnospeices can be described as Kimberichnus teruzzii.

This Trilobite belongs to the species Asaphellus fezouataensis and it was found in the Ordovician Fezouata Shale of Morocco.

Here is a trilobite of the species Asaphellus fezouataensis from the Ordovician Fezouata Shale of Morocco.
 

This is a trilobite of the species Asaphellus fezouataensis from the Ordovician Fezouata Shale of Morocco. Also on the plate are some fossil snails of the species Pelecyogyra fezouataensis Ebbestad & Lefebvre, 2015
 

Here is a very nice preserved Conularia from the upper Ordovician of the Tafilalt in Morocco. Conulariids are relative rare fossils even they are geographically wide distributed. This specimen shows a striking similairety to Archaeoconularia consobrina, that is known from the Ordovician of the Czech Republic.

This piece shows a very nice Trilobite Track of the species Cruziana furcifera from the Ordovician period in Portugal. The traces originate from a temporary outcrop in the vicinity of Penha Garcia. Cruziana furcifera is characteristic of the Armorican Quartzite. Similar findings are also known in Spain.
 

This is an excellent display piece with two fossils of shark teeth of the species Otodus obliquus from Morocco.
The two shark tooth fossils offer top preservation and are also very large. With a length of about 78 and 79 mm, these compete with many a megalodon tooth. This is an impressive piece that is rare to find.

This slab displays several trilobite trace fossils of species Cruziana furcifera from the Ordovician period in Portugal.

Here is a prone specimen of a Paralejurus spatuliformis from the Lower Devonian of Atchana.

This is a beautiful and detailed Morocco trilobite of the species Hollardops burtandmimiae on a decorative matrix.

This beautiful and authentic heteromorphic ammonite belongs to the species Acrioceras tabarelli and originates from the Lower Cretaceous period in Morocco.

This is a rare specimen of an Odontochile hausmanni from the Pragian of Prague.
This Trilobite is by no means perfect but articulated specimens from this classical site where rarely been found even back in the days. Today this site is not accessible anymore. This is a large and inexpensive specimen from of a interesting species from a very classical paleontological site. Fully prone would this Odontochile hausmanni be about 100 mm long.

Here is a decorative tooth of Mosasaurus beaugei on a beautiful matrix.

This is a beautiful mosasaur tooth of the species Mosasaurus beaugei on matrix.

Here is a godd fossil Mosasaurus tooth from Morokko.

Here is a fossil shark tooth from Morocco of the species Otodus obliquus on a nice matrix.
The fossil shark tooth presents itself on a displayable piece of authentic matrix and shows a good preservation

This is a detailed specimen of a fossilized brittle star from the Upper Ordovician of Morocco. These specimens are commonly offered as “Ophiura sp.”

This is a detailed specimen of a fossilized brittle star from the Upper Ordovician of Morocco. These specimens are commonly offered as “Ophiura sp.”

Here is a highly detailed specimen of a fossilized brittle star from the Upper Ordovician of Morocco. These specimens are commonly offered as “Ophiura sp.”

This is a inexpensive example of  the just now in 2017  by van Viersen A.P., Holland D., Koppka described species Morocops spinifer.

Here is a beautiful tiger's eye sample from the Proterozoic era of South Africa. Tiger's eye is a marine microbialite found in the Banded Iron Formation, which formed approximately 3.8 to 1.8 billion years ago during the Great Oxidation Event through the precipitation of iron in seawater.

Here is a beautiful tiger's eye sample from the Proterozoic era of South Africa. Tiger's eye is a marine microbialite found in the Banded Iron Formation, which formed approximately 3.8 to 1.8 billion years ago during the Great Oxidation Event through the precipitation of iron in seawater.

Here is a beautiful tiger's eye sample from the Proterozoic era of South Africa. Tiger's eye is a marine microbialite found in the Banded Iron Formation, which formed approximately 3.8 to 1.8 billion years ago during the Great Oxidation Event through the precipitation of iron in seawater.

Here is a beautiful tiger's eye sample from the Proterozoic era of South Africa. Tiger's eye is a marine microbialite found in the Banded Iron Formation, which formed approximately 3.8 to 1.8 billion years ago during the Great Oxidation Event through the precipitation of iron in seawater.

Here is a beautiful tiger's eye sample from the Proterozoic era of South Africa. Tiger's eye is a marine microbialite found in the Banded Iron Formation, which formed approximately 3.8 to 1.8 billion years ago during the Great Oxidation Event through the precipitation of iron in seawater.