Crab - Fossil skeleton - 105 mm - 115 mm (No reserve price)





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Potamon sp., a natural fossil crab specimen from Turkey, dating to the Pleistocene of the Quaternary, preserved as a three‑dimensional outer cast in travertine, with a width of 115 mm, height 105 mm, depth 35 mm and a weight of 756 g.
Description from the seller
Rare example.
SPECIES
Potamon sp.
AGE
Pleistocene (400.000+ years)
LOCATION
Denizli Basin, Southwest Turkey
FORMATION
Travertine Deposits
WEIGHT 756 Gr.
SIZE
Crab 45 mm * 35 mm * 19 mm
Rock 115 mm x 105 mm x 35 mm
This is a spectacular fossil freshwater crab (Potamon sp) preserved in travertine from the Denizli Basin in Southwest Turkey. The crab itself is 4.5 cm wide and exhibits amazingly detailed, 3d preservation. It's totally coated and preserved as a three-dimensional outer cast within a natural cavity of a white travertine matrix. It is covered by an inorganic film of calcium carbonate.
Travertine is a type of limestone that forms around mineral springs. It is often quarried for use as a building material, and that is how these crabs were discovered, during the quarrying of the stone slabs. The travertine deposits in the Denizli Basin are Pleistocene in age, having been formed within the past 400,000 years.
Rare example.
SPECIES
Potamon sp.
AGE
Pleistocene (400.000+ years)
LOCATION
Denizli Basin, Southwest Turkey
FORMATION
Travertine Deposits
WEIGHT 756 Gr.
SIZE
Crab 45 mm * 35 mm * 19 mm
Rock 115 mm x 105 mm x 35 mm
This is a spectacular fossil freshwater crab (Potamon sp) preserved in travertine from the Denizli Basin in Southwest Turkey. The crab itself is 4.5 cm wide and exhibits amazingly detailed, 3d preservation. It's totally coated and preserved as a three-dimensional outer cast within a natural cavity of a white travertine matrix. It is covered by an inorganic film of calcium carbonate.
Travertine is a type of limestone that forms around mineral springs. It is often quarried for use as a building material, and that is how these crabs were discovered, during the quarrying of the stone slabs. The travertine deposits in the Denizli Basin are Pleistocene in age, having been formed within the past 400,000 years.

