Kammerer Christian F
North Carolina Museum of Natural Sciences, Raleigh, NC, USA.
PeerJ. 2019 Aug 22;7:e7420. doi: 10.7717/peerj.7420. eCollection 2019.
A single species of the dicynodontoid dicynodont is currently recognized from the late Permian Usili Formation of Tanzania: Haughton, 1932. Restudy of the known Tanzanian materials of . demonstrates that they represent two distinct morphotypes, here considered separate taxa. The holotype of . is not referable to and instead is transferred to the genus (but retained as a valid species, comb. nov.). A number of published dicynodontoid specimens from the Usili Formation, however, are referable to , and are here recognized as a new species ( sp. nov.) can be distinguished from its South African congener by the presence of an expansion of the squamosal and jugal beneath the postorbital bar and a curved, posterolateral expansion of the squamosal behind the temporal fenestra. Inclusion of and . in a phylogenetic analysis supports their referral to and (respectively). These results indicate higher basinal endemism in large late Permian dicynodonts than previously thought, a sharp contrast to the cosmopolitanism in the group in the earliest Triassic.
霍顿,1932年。对坦桑尼亚已知材料的重新研究表明,它们代表两种不同的形态类型,在此被视为不同的分类单元。[此处原文有缺失,可能是某个物种名]的正模标本不能归属于[此处原文有缺失,可能是某个物种名],而是被转移到[此处原文有缺失,可能是某个属名]属(但保留为一个有效物种,[此处原文有缺失,可能是某个物种名],新组合)。然而,一些来自乌西利组已发表的二齿兽类标本可归属于[此处原文有缺失,可能是某个物种名],并在此被确认为一个新物种([此处原文有缺失,可能是某个物种名],新物种)。[此处原文有缺失,可能是某个物种名]可通过眶后棒下方鳞骨和颧骨的扩展以及颞孔后方鳞骨的弯曲后外侧扩展与它的南非同类物种相区分。将[此处原文有缺失,可能是某个物种名]和[此处原文有缺失,可能是某个物种名]纳入系统发育分析支持它们分别归属于[此处原文有缺失,可能是某个属名]和[此处原文有缺失,可能是某个属名]。这些结果表明,晚二叠世大型二齿兽的盆地特有性比以前认为的更高,这与三叠纪早期该类群的世界性分布形成鲜明对比。