Otodus obliquus
Otodus obliquus
Summary
Otodus obliquus was one of the major marine predators of the Palaeocene and early Eocene and an early member of the otodontid lineage that later gave rise to the giant megatooth sharks. It was a large, powerful lamniform with a feeding apparatus built for tackling substantial prey.
Its thick triangular teeth had smooth cutting edges and strong lateral cusplets. Working together, they formed a robust grasping-and-cutting dentition capable of penetrating flesh and retaining large prey. Fishes and other marine vertebrates are likely food sources, although direct evidence of individual prey is rare.
O. obliquus was widespread across warm seas and was not simply a local London Clay animal. Its occurrence there places a major open-water predator alongside a remarkably diverse community of smaller sharks and rays.
Quick Identification
Look for: a large, thick triangular tooth with smooth cutting edges, one or more strong lateral cusplets and a massive two-lobed root; complete basal corners are important for separating it from related Otodus species.
Diagnostic Features
- Main cusp is broad, thick and triangular with smooth cutting edges.
- Strong lateral cusplets are present on well-preserved teeth.
- Crown is labiolingually thick compared with most sand-tiger-type teeth.
- Root is massive, bilobed and broadly spread.
- No true crown serration is present in the typical O. obliquus morphology.
Fossil Details
Similar Species
Recorded Fossil Sites
Beltinge Fish Bed
London Clay Formation
Walton Member
References
- Casier, E. (1966). Faune ichthyologique du London Clay. 496 pp.. Trustees of the British Museum (Natural History), London View reference
- Dineley, D. & Metcalf, S. (1999). Fossil Fishes of Great Britain. Geological Conservation Review Series, 675 pp.. Joint Nature Conservation Committee, Peterborough View reference
- Rayner, D.; Mitchell, T.; Rayner, M. (2009). London Clay Fossils of Kent and Essex. 228 pp.. Medway Fossil and Mineral Society, Rochester, Kent 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
- Ward, D.J. (1980). The distribution of sharks, rays and chimaeroids in the English Palaeogene. Tertiary Research, 3(1), 13–19 View reference