Xiphiorhynchus priscus
Xiphiorhynchus priscus
Summary
Xiphiorhynchus priscus was a large long-snouted predatory teleost and the best-known member of an extinct Eocene billfish-like family. Both upper and lower jaws were extended into a long rostral apparatus, producing a very different skull from the single-bill arrangement of living swordfish. Fine teeth along the elongated jaws indicate that the rostrum remained part of the feeding surface rather than becoming completely toothless.
The long head and predatory dentition suggest an active marine fish pursuing smaller nekton. Exactly how the rostrum was used is unknown, so comparisons with modern billfish striking behaviour remain speculative. London Clay skull and rostral remains show that highly specialised long-jawed predators were already established in early Eocene pelagic ecosystems.
Quick Identification
Look for: an extremely elongate rostral skull in which both upper and lower jaws project forward, with fine abrasive teeth along the rostral margins, radiating ornament on the frontals and a strongly ossified sclerotic ring around the eye.
Diagnostic Features
- Both upper and lower jaws are greatly elongated into the rostral apparatus.
- Rostral jaw margins carry numerous tiny closely spaced teeth.
- Frontal bones show strong radiating surface ornament.
- Sclerotic ring is conspicuous and strongly ossified.
- Rostrum is long and comparatively fragile, tapering gradually from the cranial base.
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