Xu Li, Zhang Xingliao, Pu Hanyong, Jia Songhai, Zhang Jiming, Lü Junchang, Meng Jin
Henan Geological Museum, Zhengzhou, Henan 450016, China.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 10037, China.
Sci Rep. 2015 Oct 22;5:14950. doi: 10.1038/srep14950.
A new multituberculate, Yubaartar zhongyuanensis gen. and sp. nov., is reported from the Upper Cretaceous of Luanchuan County, Henan Province, China. The holotype of the new taxon is a partial skeleton with nearly complete cranium and associated lower jaws with in situ dentitions. The new species is the southern-most record of a Late Cretaceous multituberculate from outside of the Mongolian Plateau in Asia and represents the largest known Mesozoic multituberculate from Eurasia. The new specimen displays some intriguing features previously unknown in multituberculates, such as the first evidence of replacement of the ultimate upper premolar and a unique paleopathological case in Mesozoic mammals in which the animal with a severely broken right tibia could heal and survive in natural condition. The phylogenetic analysis based on craniodental characters places Yubaartar as the immediate outgroup of Taeniolabidoidea, a group consisting of a North American clade and an Asian clade. This relationship indicates at least a faunal interchange of multituberculates before the K-Pg transition. The new evidence further supports the hypothesis that disparity in dental complexity, which relates to animal diets, increased with generic richness and disparity in body size, and that an adaptive shift towards increased herbivory across the K-Pg transitional interval.
在中国河南省栾川县上白垩统中发现了一种新的多瘤齿兽类,即中原豫巴兽(Yubaartar zhongyuanensis),新属新种。新分类单元的模式标本是一具部分骨骼,带有近乎完整的颅骨以及相连的下颌骨和原位齿列。该新物种是亚洲蒙古高原以外地区白垩纪晚期多瘤齿兽最南端的记录,也是已知欧亚大陆最大的中生代多瘤齿兽。新标本展现出一些多瘤齿兽类此前未知的有趣特征,比如首次发现最后一枚上前臼齿替换的证据,以及中生代哺乳动物中一个独特的古病理学案例,即一只右胫骨严重骨折的动物能够在自然条件下愈合并存活。基于颅齿特征的系统发育分析将豫巴兽置于绦齿兽超科(Taeniolabidoidea)的直接外类群位置,绦齿兽超科由一个北美分支和一个亚洲分支组成。这种关系表明在白垩纪-古近纪过渡之前多瘤齿兽类至少发生过一次动物群的交流。新证据进一步支持了以下假说:与动物饮食相关的牙齿复杂性差异随着属的丰富度和体型差异而增加,并且在白垩纪-古近纪过渡期间向食草性增强发生了适应性转变。