Yubaatar

Yubaatar Temporal range: Late Cretaceous
Holotype fossil; the skull and forelimbs are displaced in relation to the rest of the skeleton
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Order:	†Multituberculata
Superfamily:	†Taeniolabidoidea
Genus:	†Yubaatar Xu et al., 2015
Species
Y. qianzhouensis Hu & Han, 2021[1] Y. zhongyuanensis Xu et al., 2015

Yubaatar is a genus of multituberculate, an extinct order of rodent-like mammals, which lived in what is now China during the Late Cretaceous. The first specimen was discovered in the Qiupa Formation of Luanchuan County, in the Henan Province. The specimen consists of a partial skeleton with a nearly complete skull, and was made the holotype of the new genus and species Yubaartar zhongyuanensis by the Chinese palaeontologist Li Xu and colleagues in 2015. The generic name consists of the word Yu, which is the pinyin spelling of the Chinese character for the Henan Province, and the Mongolian word baatar, which means "hero", a word commonly used as suffix in the names of Asian multituberculates. The specific name comes from Zhongyuan, an ancient name for the geographic area of the province.^[2]

Yubaatar is the first known and southernmost Late Cretaceous multituberculate outside of the Mongolian plateau (most multituberculate specimens mainly consist only of teeth and jaws, and are rarely found in eastern Asia). With a skull 7 cm long, Yubaatar is estimated to have been the size of a black-footed ferret, and was the largest member of the group known from Eurasia (larger members are known from North America). Sphenopsalis was similar in size, but most other Mesozoic multituberculates were the size of a shrew or rat. Yubaatar had a unique feature among multituberculates in that its last upper premolar was replaced. The holotype specimen had a palaeopathology unique among known Mesozoic mammal, a severely broken right tibia bone, which was probably damaged in an accident, but had healed.^[2][3]

Yubaatar was found to be basal to the clade Taeniolabidoidea, which consists of North American and Asian multituberculates; this indicates there was a faunal interchange between Asia and North America before the Cretaceous–Paleogene transition. The morphology of Yubaatar indicates that diversity in the complexity of the teeth of multituberculates, relating to their diets, increased with the number of genera and difference in body size, and that there was a shift in adaptations towards increased herbivory in the group across the Cretaceous–Paleogene boundary.^[2]