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Scarrittia

From Wikipedia, the free encyclopedia
(Redirected from Scarrittia canquelensis)

Scarrittia
Temporal range: Late Oligocene (Deseadan)
~28.4–23.03 Ma
S. canquelensis fossil
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Infraclass: Placentalia
Order: Notoungulata
Family: Leontiniidae
Genus: Scarrittia
Simpson 1934
Type species
Scarrittia canquelensis
Simpson 1934
Species
  • S. barranquensis Ribeiro et al. 2010
  • S. canquelensis Simpson 1934
  • S. robusta Ubilla et al. 1994

Scarrittia is an extinct genus of hoofed mammal of the family Leontiniidae, native to South America during the Late Oligocene epoch (Deseadan in the SALMA classification).

Description

[edit]
Restoration

Scarrittia was about 2 metres (6.6 ft) in body length, and resembled a rhinoceros with a relatively long body and neck. It had three hoofed toes on each foot, and a very short tail. Due to a fused tibia and fibula, Scarrittia would have been unable to turn its legs sideways. The short skull had 44 poorly specialized teeth.[1]

Natural history

[edit]

This was a very successful genus with various known species, such as Scarrittia robusta, S. barranquensis and S. canquelensis, which lived around 30 million years ago. They lived in moist forest, near the coast, in wetlands, lakes, swamps, etc. and they ate soft vegetation, grasses, fruits and trees. Some species were omnivorous, eating also eggs and small mammals. They were not adapted for running, though their large size meant they had few enemies.[citation needed]

Distribution

[edit]

Fossils of Scarrittia have been found in:[2]

References

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  1. Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 252. ISBN 1-84028-152-9.
  2. Scarrittia at Fossilworks.org
  3. Ubilla, Martín; Perea, Daniel; Bond, Mariano (1994). "The deseadan land mammal age in Uruguay and the report of Scarrittia robusta nov. sp. (Leontiniidae, Notoungulata) in the Fray Bentos Formation (Oligocene-?Lower miocene)". Geobios. 27 (1): 95–102. doi:10.1016/S0016-6995(06)80217-2. ISSN 0016-6995.