Fossilized Bivalve (Mussel or Clam)

Indeterminate species, cf. Mytilidae gen. et sp. indet.Body fossil, invertebrate, specifically a bivalve mollusk

Fossilized Bivalve (Mussel or Clam)

Geological Period

Likely Cretaceous to Neogene

Estimated Age

Approx. 5 to 100 million years

Preservation Type

Permineralization or replacement; the original shell material has likely been replaced by minerals like silica or phosphate, resulting in a dark, stony texture.

Condition Assessment

Fair; the specimen is worn (water-rolled), likely collected as beach float, with significant erosion of the hinge and fine morphological details.

Taxonomic Classification

Phylum: Mollusca, Class: Bivalvia, Order: Pteriomorphia (potential), Genus: cf. Mytilus or similar marine bivalve

Morphological Description

Small, fan-shaped to elongated shell fragment showing distinct radial ribbing and concentric growth lines. The specimen appears moderately convex with a dark, weathered surface and worn edges.

Rock Matrix

Mostly free of matrix, but showing traces of fine-grained silty or phosphatic sediment within crevices.

Formation & Location

Possible origin from coastal formations such as the Chesapeake Group (USA) or similar marine deposits in Europe or North Africa.

Size & Dimensions

Approximately 2-3 cm in length; typical for small adult or juvenile marine bivalves of this clade.

Value & Rarity

Estimated Market Value

$5 - $15 USD

Auction Estimate

$10 - $30 USD (usually sold as part of a lot)

Rarity Assessment

Common; bivalve fossils of this nature are abundant in marine fossil-bearing strata worldwide.

Scientific Significance

Provides evidence of local paleoenvironment (marine) and can contribute to understanding regional molluscan biodiversity and paleobiogeography.

Preparation Recommendations

No further mechanical preparation required. Store in a dry, stable environment. Can be cleaned gently with a soft brush and distilled water if necessary.

Notable Features

Heavy mineralization and dark coloration suggest it may have been found in a phosphatic bed or an area high in manganese/iron, resulting in its weathered, 'river-worn' appearance.

Identified on 6/6/2026