Sinornithomimus

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iSinornithomimus
Fossil range: Late Cretaceous

Extinct (fossil)

Scientific classification

Kingdom:	Animalia
Phylum:	Chordata
Class:	Sauropsida
Superorder:	Dinosauria
Suborder:	Theropoda
Infraorder:	Coelurosauria
Family:	Ornithomimidae
Genus:	Sinornithomimus Kobayashi & Lu, 2003

Species

Sinornithomimus dongi

Sinornithomimus was an ornithomimid theropod dinosaur found in 1997^[1], in the early Late Cretaceous strata of the Ulansuhai Formation located at Alshanzuo Banner, Nei Mongol Autonomous Region, Northern China. The fossil remains consist of at least fourteen skeletons found in close association, nine of which are nearly complete and relatively uncrushed. The find was comprised of 3 sub-adult to adult specimens and 11 juveniles, described by Kobayashi et al. in 2003. The unweathered state of the bones, preserved in siltstone interspersed with layers of clay and the absence of evidence for post-mortem movement, argue for a catastrophic event that killed all the individuals present in the find simultaneously and instantaneously.

The generic name means “Chinese bird mimic” while the specific epithet honours the discoverer of the fossils.

Sinornithomimus is a two-meter-long ornithomimine, possessing quadrate fenestra, with a dividing vertical bony lamina, included in a quadrate fossa and a depression on the posterior process of the parietal bone. The herbivory of this species is supported by gastrolith characteristics^[2], as such stones were found forming conspicuous masses in the stomach areas of the fossil skeletons. This species was gregarious, which is corroborated by the arrangement of the fossil remains in a small bonebed with the juvenile individuals being approximately of the same age. This is furthermore supported by the increase of running ability as the animal progressed in its ontogeny, thus shown in the more cursorial proportions of the adults. It is assumed by the describers that adults protected themselves and their juveniles from predators by forming familial groups.

S. dongi is a basal ornithomimid that was considered by its describers a more derived form than Archaeornithomimus, though more recent analyses reverse the situation. The structure of the hand is similar to that of Archaeornithomimus representing thus an intermediate between the primitive condition of the ornithomimosaur Harpymimus and the one of the more derived ornithomimids. Sinornithomimus dongi renders some synapomorphies of ornithomimids plesiomorphic, while also differentiating Asian ornithomimid rhamphothecae from North American ones, based on maxillary vascular foramina found in the latter.

[edit] References

Kobayashi, Y. and Lü, J.−C. 2003. A new ornithomimid dinosaur with gregarious habits from the Late Cretaceous of China. Acta Palaeontologica Polonica 48 (2): 235–259.

[edit] Notes

↑ Kobayashi, Y., Lü, J.−C., Azuma, Y., Dong, Z.−M., and Barsbold, R. 2001.

Bonebed of a new gastrolith−bearing ornithomimid dinosaur from the Up− perCretaceous Ulansuhai Formation ofNei Mongol Autonomous Region, China. Journal of Vertebrate Paleontology 21 (Supplement to 3): 68–69.