Sharnia burnhamensis

Sharnia burnhamensis

Collins & Saward, 2006

Common name Crab
Fossil group Crustaceans
Order Decapoda
Family Etyidae
Genus Sharnia
Taxonomic status Accepted
Geological age Ypresian

Summary

Sharnia burnhamensis was a rare true crab from the Essex London Clay. It would have lived on the seabed as a mobile benthic animal, probably feeding opportunistically on small invertebrates and scavenged food.

Rare species such as Sharnia are important because they show that the London Clay ecosystem contained more than just the familiar common crabs and lobsters. Even unusual or locally scarce forms contributed to the remarkable variety of early Eocene crustacean life.

Quick Identification

Look for: a distinctive elongated crab carapace with strongly defined dorsal regions matching the Sharnia type morphology; do not identify incomplete Essex crab fragments solely from locality.

Diagnostic Features

  • Carapace relatively elongate for a true crab.
  • Dorsal regions are strongly and clearly defined.
  • Overall outline is distinct from broad Portunites and Zanthopsis carapaces.
  • Surface and groove pattern match the unusual Sharnia morphology.
  • Species-level identification requires a substantial, diagnostic part of the carapace.

Fossil Details

Typical size
Centimetre-scale carapace; the species is rare and a robust population range is not available.
Fossil material
Carapace, Claw / Chela
Preservation
Rare specimens are commonly incomplete. Breakage of the margins or compression of the elongated carapace can obscure the features needed to recognise Sharnia.

Similar Species

Recorded Fossil Sites

References

  • Collins, J.S.H.; Saward, J. (2006). Three new genera and species of crabs from the Lower Eocene London Clay of Essex, England. Bulletin of the Mizunami Fossil Museum, 33, 67–76 View reference
  • J. S. H. Collins; C. J. T. Mellish; A. J. Ross; P. R. Crabb; S. K. Donovan. (2020). A guide to the fossil Decapoda (Crustacea: Axiidea, Anomura, Brachyura) of the British Isles. Proceedings of the Geologists' Association, 131(1), 19–50 View reference
Last Reviewed
16 August 2026 Reviewed by Sam Harris