Gymnosarda prisca
Gymnosarda prisca
Summary
Gymnosarda prisca was a tuna-like scombrid known from the caudal skeleton rather than the skull. Its identification rests on the structure of the hypural plates that supported the tail fin. This makes the species unusual among London Clay fishes, many of which are diagnosed from three-dimensional crania.
The preserved tail region indicates a powerful caudal apparatus consistent with an active pelagic swimmer. A fast, predatory lifestyle is a reasonable inference from its scombrid relationships, but jaw structure and diet are not directly known for this species. The fossil is important because it records an early branch of the bonito–tuna radiation through one of the body regions most closely tied to propulsion.
Quick Identification
Look for: a compact scombrid caudal skeleton dominated by broad hypural plates, with a distinct notch in the posterior margin of the fused hypural complex; identification is based on the tail-supporting bones rather than teeth or skull fragments.
Diagnostic Features
- Hypural plates form a broad, compact support for the caudal fin.
- Posterior margin of the hypural complex bears a distinct caudal notch.
- Upper and lower hypural regions are strongly expanded laterally.
- Hypural elements are closely united into a stiff plate-like complex.
- Caudal peduncle skeleton is robust and strongly ossified relative to the thin fin-ray supports.
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
- Monsch, K. A. (2005). Revision of the scombroid fishes from the Cenozoic of England. Transactions of the Royal Society of Edinburgh: Earth Sciences, 95(3–4), 445–489 View reference