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Sauroctonus

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Sauroctonus
Temporal range: Late Permian
Sauroctonus parringtoni
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Therapsida
Clade: Gorgonopsia
Family: Gorgonopsidae
Genus: Sauroctonus
Bystrow, 1955
Species
  • S. parringtoni (von Huene, 1950)
  • S. progressus (Hartmann-Weinberg, 1938)(type)

Sauroctonus is an extinct genus of therapsids. Sauroctonus progressus was a large (2 m long) gorgonopsid that lived in the Late Permian epoch before the Permian-Triassic extinction event that wiped out many life forms on Earth (259-254 million years ago). Its fossils have been found in the Usili Formation (Songea Group) of Tanzania and the Sokolki Assemblage Zone of the Volga Basin of Russia.

Description

Sauroctonus's flattened, triangular skull was about 25 cm (9.8 in) long, with a parietal eye, a primitive character, on the crown. The upper and lower jaw each contained one pair of massive canine teeth (the upper pair was larger); the other teeth were smaller, but were also sharp and pointed. In addition, minute, blunt teeth were present on the palatine bones. The lower jaw was widened to form a kind of chin. The long, lightly built, five-toed limbs bore a resemblance to mammals' limbs, but despite its 'mammalian' characteristics, Sauroctonus was not one of the ancestors of mammals. Based on its cranial and skeletal features, Sauroctonus was not as specialized as other gorgonopsids such as Rubidgea or Inostrancevia.[1]

Species

There are two recognized species of Sauroctonus: S. progressus and S. parringtoni.[2]

See also

References

  1. ^ Anton, Mauricio (2013). Sabertooth.
  2. ^ Gebauer E I, 2014. Re-assessment of the taxonomic position of the specimen GPIT/RE/7113 (Sauroctonus parringtoni comb. nov., Gorgonopsia). In: Kammerer C F, Angielczyk K D, Fröbisch J eds. Early Evolutionary History of the Synapsida. Dordrecht: Springer. 185−207.

Further reading

  • Benes, Josef. Prehistoric Animals and Plants. Pg. 95. Prague: Artia, 1979.