Bucklandium diluvii
Bucklandium diluvii
Summary
Bucklandium diluvii is an enigmatic London Clay ray-finned fish known from a cranium with associated pectoral-arch material. It was historically interpreted as a catfish and compared with living siluriforms, but later re-examination of the type material has questioned that assignment. Its exact position therefore remains unresolved, and it should not be reconstructed as a conventional catfish with a confidently known ecology.
The fossil is nevertheless substantial enough to show a strongly ossified, heavily sculptured head and shoulder region. Because the jaws, soft tissues and complete body are poorly known, diet and lifestyle cannot be inferred securely; the most useful biological message is that it represents a distinctive large-bodied teleost cranial type within the London Clay fauna whose relationships still need clarification.
Quick Identification
Look for: a thick, strongly ossified cranial or pectoral-arch fragment with coarse sculpturing and heavy ridges; the known material is robust three-dimensional head-and-shoulder bone rather than an otolith, isolated tooth or delicate rostral fragment.
Diagnostic Features
- Known type material includes a substantial cranium associated with part of the pectoral arch.
- Dermal cranial bones are thick and strongly ossified.
- External skull surfaces carry coarse relief rather than fine parallel striation.
- Raised bony ridges separate broad sculptured areas on the cranial roof.
- Pectoral-arch elements are robust and closely associated with the posterior skull in the type specimen.
Fossil Details
Recorded Fossil Sites
No fossil-site occurrences have yet been recorded for this species.
References
- Casier, E. (1966). Faune ichthyologique du London Clay. 496 pp.. Trustees of the British Museum (Natural History), London View reference
- Friedman, M.; Beckett, H. T.; Close, R. A.; Johanson, Z. (2016). The English Chalk and London Clay: two remarkable British bony fish Lagerstätten. Geological Society, London, Special Publications, 430(1), 165–200. Geological Society of London, London View reference