This is a polished section of an exotic and decorative rock known as Bumble Bee Jasper. It is a carbonate microbialite that was partially formed under the influence of extremophile microorganisms.

This is a polished section of an exotic and decorative rock known as Bumble Bee Jasper. It is a carbonate microbialite that was partially formed under the influence of extremophile microorganisms.

This is a polished section of an exotic and decorative rock known as Bumble Bee Jasper. It is a carbonate microbialite that was partially formed under the influence of extremophile microorganisms.

Here is a beautiful and detailed specimen of a solitary coral of the species Montlivaltia obconica from late Jurassic  Nattheim. 

Here is a beautiful matrix piece of a fossil coral of the species Montlivaltia obconica from the Jura of Nattheim.

This detailed fossil Bivalve from the Jurassic of Portugal belongs to the species Myophorella (Clavotrigonia) lusitanica. This species is also still often identified as Trigonia lusitanica.

This double-valved fossilized shell from the Jurassic period of Portugal belongs to the species Myophorella (Clavotrigonia) lusitanica.
This species is also often referred to as Trigonia lusitanica.

This fossilized bivalve shell from the Jurassic period of Portugal belongs to the species Myophorella (Clavotrigonia) lusitanica. It is often referred to by its alternate name, Trigonia lusitanica.

This is a large and interesting plate with numerous Ediacara fossils of the species Nemiana simplex. 

Here is a Precambrian fossil plate with the Ediacaran fossil Nemiana simplex.

This is a Precambrian fossil plate with the Ediacaran fossil Nemiana simplex.

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

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.

Plaffeiite is a rare alpine amber from the Paleocene, found in the Gurnigel Flysch of the Swiss Alps.
It shows strong UV fluorescence, contains no succinic acid, and derives from fossil conifers.
Due to tectonic fracturing, it's unsuitable for jewelry.