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Dicynodontoides

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Also known as Kingoria

Dicynodontoides is a genus of small to medium-bodied, herbivorous, emydopoid dicynodonts from the Late Permian. The name Dicynodontoides references its “dicynodont-like” appearance (dicynodont = two-dog-tooth) due to the caniniform tusks featured by most members of this infraorder. Kingoria, a junior synonym, has been used more widely in the literature than the more obscure Dicynodontoides, which is similar-sounding to another distantly related genus of dicynodont, Dicynodon. Three species are recognized: D. recurvidens from South Africa, and D. nowacki and D. kubwa from Tanzania.

Wikidata facts

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KingoriaDB.jpg
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taxon name
Dicynodontoides
start time
260000000-
end time
251000000-
Commons category
Dicynodontoides
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16 sections
Contents
  • History and discovery
  • Description
  • Skull
  • Post-cranial skeleton
  • Paleobiology
  • Feeding ecology
  • Locomotion
  • Metabolism and thermoregulation
  • Histology
  • Species
  • Classification
  • Stratigraphic and geographic range
  • Paleoenvironment
  • See also
  • References
  • External links

Dicynodontoides is a genus of small to medium-bodied, herbivorous, emydopoid dicynodonts from the Late Permian. The name Dicynodontoides references its “dicynodont-like” appearance (dicynodont = two-dog-tooth) due to the caniniform tusks featured by most members of this infraorder. Kingoria, a junior synonym, has been used more widely in the literature than the more obscure Dicynodontoides, which is similar-sounding to another distantly related genus of dicynodont, Dicynodon. Three species are recognized: D. recurvidens from South Africa, and D. nowacki and D. kubwa from Tanzania.

Dicynodontoides is primarily known from fossil localities in South Africa and Tanzania, though several specimens unidentified to the species level are known from Zambia, Malawi, and India. Unlike several other members of the remarkably disparate emydopoid clade, Dicynodontoides did not survive into the Triassic, and its temporal distribution is restricted to the Late Permian.

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