Ostrea bellovacina
Ostrea bellovacina
View age-specific evidence and explanation
| Age | Recorded Occurrences | Localities | Rarity |
|---|---|---|---|
| Thanetian | 1 | 1 | Not yet established |
| Ypresian | 1 | 1 | Not yet established |
These counts describe published LBPS Occurrence records with directly assigned, unambiguous geological-unit mappings—not specimen abundance. Records at restricted Localities and ambiguous or unsupported ages are excluded. Species-level age labels are not used as proof of an age-specific Occurrence.
Specimen-based rarity requires comparable, correctly identified physical fossils, geological provenance and publication permissions. It does not estimate your chance of finding a fossil or collecting access.
Quick Identification
Look for: a thick, irregular oyster valve with a deep attached lower valve, a flatter opposing valve, layered shell growth and a simple toothless hinge.
Summary
Ostrea bellovacina was a sessile oyster with two unequal calcitic valves. Like living oysters, it attached one valve to a firm object and filtered suspended food particles from the water with its gills.
Its irregular shell could change shape as it grew against the substrate or neighbouring shells, so hinge and shell construction are more useful than outline alone.
Diagnostic Features
- Shell strongly inequivalve, with one valve typically deeper and more convex than the other.
- Outline irregular and variable rather than consistently symmetrical.
- Shell thick and built from conspicuous laminated calcitic layers.
- Hinge lacks the interlocking cardinal teeth seen in many clams.
- Concentric growth lamellae dominate the exterior rather than regular radial cockle-like ribs.
Fossil Details
Similar Species
Recorded Fossil Sites
Lambeth Group
Lessness Shell Bed
Reading Formation
Reculver Sand Member
Synonyms & Previous Names
References
- Rundle, A. J. (1970). Report of a Field Meeting to Abbey Wood, Kent. Tertiary Times, 1, 20–23 View reference
- Ward, D.J. (1978). The Lower London Tertiary (Palaeocene) succession of Herne Bay, Kent. Report of the Institute of Geological Sciences. Institute of Geological Sciences View reference
