Temporal range: Late Permian 270Ma
L. I. Price, 1948
The fragmentary remains of this animal have been found in the Pedra do Fogo Formation in the Parnaiba Basin of Northeastern Brazil, and it was described by L.I. Price in 1948. Reaching an estimated length of 4.5 m (14.75 ft) and a weight of 363 kg (800 lb), Prionosuchus is one of the largest amphibians ever found.
With an elongated and tapered snout, numerous sharp teeth, long body, short legs, and a tail adapted for swimming, its general appearance was very similar to a modern crocodile, particularly to the gharial, and it probably had a similar lifestyle as an ambush aquatic predator feeding on fish and other aquatic animals.
It has been classified as an archegosaurian by Carroll. The genus is monotypic with P. plummeri being the only species described. The archegosaurs were a group of temnospondyli that occupied the ecological niche of crocodiles and alligators during the Permian, and of which the European genus Archegosaurus is typical. The group went extinct at the end of the Permian and the niche was subsequently filled by other, new temnospondyls, later joined by reptiles such as the phytosaurs in the Triassic period.
Cox and Hutchinson re-evaluated Prionosuchus in 1991 and synonymized it with the genus Platyoposaurus from Russia. On the basis of this study, the Pedra do Fogo Formation was reevaluated to be of Middle to Late Permian age. However, Platyoposaurus was comparatively smaller, reaching a total length of only 2.5 meters (8.2 ft), indicating that the two animals are distinct at least at the species level. Alternative studies based on plants and pollens indicate that this formation is rather of Early Permian age, making Prionosuchus not contemporary with Platyoposaurus. Most paleontologists consider Prionosuchus as a valid genus.
Prionosuchus lived in a humid and tropical environment as indicated by the petrified forest of the Pedra do Fogo formation in which the fossil has been found. The strata composed of siltstones, shales and limestones were deposited in lagoonal and fluvial environments. Other animals discovered in the same rocks include fish (primitive sharks, palaeoniscids, and lungfishes) and amphibians.
- L.I. Price, 1948, Um anfibio Labirinthodonte da formacao Pedra de Fogo, Estado do Maranhao: Ministerio da Agricultura, Departamento Nacional da Producao ineral Divisao de Geologia e Mineralogia, Boletim n. 124, p. 7-32.
- R. L. Carroll, 1988,Vertebrate Paleontology and Evolution. W.H. Freeman and Company
- Cox, C. B. and Hutchinson, P., 1991. Fishes and amphibians from the Late Permian Pedrado Fogo Formation of northern Brazil. Palaeontology, 34: 561-573
- Mussa D & Coimbra AM., 1987, Novas perspectivas de comparação entre as tafofloras permianas (de lenhos) das Bacias do Parnaíba e do Paraná. X Congresso brasileiro de Paleontologia. Rio de Janeiro. Anais da Academia Brasileira de Ciencias, 2: 901-922.
- Caldas EB, Mussa D, Lima Filho FP & Roesler O., 1989, Nota sobre a ocorrência de uma floresta petrificada de idade permiana em Teresina, Piauí. Bol IG-USP, Publ Esp 7: 69-87.
- Schobbenhaus, C., Campos, D. A., Derze, G. R., and Asmus, H. E., 1984, Geologia do Brasil: Brasõlia, D.N.P.M., Brasília, 501 pp.