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.

This is a  Agraulos ceticephalus with a nice contrast from the classical Czech Trilobite site Skryje.
The trilobite is about 15 mm long.

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.

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

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

This is a rare soft-bodied marrellomorph arthropod of the species Furca mauretanica, originating from the Fezouata Shale Lagerstätte in Morocco.