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Sinobaatar

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Sinobaatar is a genus of extinct mammal from the Lower Cretaceous of China. It is categorized within the also extinct order Multituberculata and among these it belongs to the plagiaulacid lineage (a possible infraorder). Sinobaatar was a small herbivore during the Mesozoic era, commonly called "the age of the dinosaurs". The genus was named by Hu Y. and Wang Y. in 2002. Three species have been described.

In the Vinony graph

Within Vinony's link graph, Sinobaatar is referenced by 152 other articles, and connects out to Eobaataridae, Pinheirodontidae and Loxaulax valdensis.

It sits within the topics Cretaceous mammals, Multituberculata and Prehistoric animals of China.

Its subject is documented across 6 Wikipedia language editions.

Wikidata facts

Parent taxon
Eobaataridae
Image
Sinobaatar & Zhangheotherium.jpg
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taxon name
Sinobaatar
taxon rank
genus
Commons category
Sinobaatar
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Encyclopedic overview

2 sections
Contents
  • Etymology
  • References

Sinobaatar is a genus of extinct mammal from the Lower Cretaceous of China. It is categorized within the also extinct order Multituberculata and among these it belongs to the plagiaulacid lineage (a possible infraorder). Sinobaatar was a small herbivore during the Mesozoic era, commonly called "the age of the dinosaurs". The genus was named by Hu Y. and Wang Y. in 2002. Three species have been described.

It has been found in Lower Cretaceous strata of the Yixian Formation in Liaoning, China. According to Hu & Wang (2002), "[t]he dental features of Sinobaatar show again that eobaatarids are obviously intermediate between Late Jurassic multituberculates and the later forms". Many Multituberculata are only known from teeth, but the type specimen of Sinobaatar is a reasonably complete skeleton.

Excerpted from Wikipedia’s “Sinobaatar” article, available under the CC BY-SA 4.0 licence.

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