Palaeophis toliapicus
Palaeophis toliapicus
Summary
Palaeophis toliapicus was a highly aquatic palaeophiid snake from the early Eocene seas. Its trunk vertebrae are tall and strongly compressed from side to side, part of an ‘advanced’ aquatic body construction in which the trunk was specialised for swimming. The animal probably propelled itself by strong lateral undulation of the body and tail through warm coastal water.
Palaeophiids were predators, and fishes or other small aquatic vertebrates are the most plausible prey for P. toliapicus, although direct gut contents or feeding traces are not known. The species is represented overwhelmingly by vertebrae, so its aquatic adaptations are read principally from the architecture of the spinal column rather than from a complete skeleton.
Quick Identification
Look for: a tall, strongly side-compressed snake trunk vertebra with well-developed upward-projecting pterapophyses, low-set rib articulations and ball-and-socket ends lying on an almost horizontal axis. The prezygapophyses do not flare strongly sideways, and ventral processes or a haemal keel may be present beneath the centrum.
Diagnostic Features
- Trunk vertebrae are tall and strongly laterally compressed.
- Prezygapophyses do not show the massive lateral projection seen in less specialised aquatic palaeophiids.
- Pterapophyses are well developed through the precloacal vertebral series.
- Posterior hypapophysis becomes reduced to a haemal keel in the posterior precloacal region.
- An anterior hypapophysis persists through the precloacal series, sometimes only as a small ventral bump.
Fossil Details
Recorded Fossil Sites
London Clay Formation
References
- Georgalis, G.L.; Del Favero, L.; Delfino, M. (2020). Italy’s largest snake: Redescription of Palaeophis oweni from the Eocene of Monte Duello, near Verona. Acta Palaeontologica Polonica, 65(3), 523–533 View reference
- Owen, R. (1841). Description of some ophidiolites (Palaeophis toliapicus) from the London Clay of Sheppey, indicating an extinct species of serpent. Transactions of the Geological Society of London, Second Series, 6, 209–210 View reference