Pholadomya konincki

Pholadomya konincki

Nyst, 1845

Common name Clam
Fossil group Molluscs
Order Pholadomyoida
Family Pholadomyidae
Genus Pholadomya
Taxonomic status Accepted
Geological age Thanetian

Summary

Pholadomya konincki was an infaunal clam that probably lived deeply buried in soft marine sediment. Like other pholadomyids, it was most likely a suspension feeder, using siphons to maintain contact with the water above while the rest of the animal remained protected within the seabed.

A deep-burrowing lifestyle would have reduced exposure to many surface predators and physical disturbance. Its ecology is inferred from the broader pholadomyid body plan because the fossils preserve the shell or moulds rather than the soft siphons and feeding organs.

Quick Identification

Look for: an inflated, inequilateral pholadomyid shell or mould with a subtrigonal-to-ovate form, prominent close umbones and preserved shell sculpture; complete outline and ornament are needed for a confident species-level identification.

Diagnostic Features

  • Shell is inflated and inequilateral, with a subtrigonal to ovate overall outline.
  • Umbones are prominent, close together and stand above the dorsal margin.
  • Anterior end is comparatively short while the posterior part is more produced.
  • Shell is relatively thin and may preserve concentric and radial surface sculpture where not decalcified.
  • Species-level identification requires the combined shell proportions and ornament; feature-poor internal moulds are not diagnostic.

Fossil Details

Fossil material
Shell, Internal Mould / Cast
Preservation
The thin shell is prone to crushing and decalcification, so specimens may survive mainly as internal or external moulds. Compression can alter the apparent outline and abrasion can erase sculpture, making incomplete specimens difficult to separate from other Pholadomya.

Similar Species

Recorded Fossil Sites

Reculver Sand Member

Thanet Formation
Confirmed

References

  • MolluscaBase Editorial Board. (2026). MolluscaBase: Pholadomya konincki Nyst, 1845. MolluscaBase 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
Last Reviewed
22 August 2026 Reviewed by Sam Harris