首页> 外文期刊>Journal of vertebrate paleontology >A REEVALUATION OF BRACHYPROSOPUS BROOMI AND CHELYDONTOPS ALTIDENTALIS, DICYNODONTS (THERAPSIDA, ANOMODONTIA) FROM THE MIDDLE PERMIAN TAPINOCEPHALUS ASSEMBLAGE ZONE OF THE KAROO BASIN, SOUTH AFRICA
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A REEVALUATION OF BRACHYPROSOPUS BROOMI AND CHELYDONTOPS ALTIDENTALIS, DICYNODONTS (THERAPSIDA, ANOMODONTIA) FROM THE MIDDLE PERMIAN TAPINOCEPHALUS ASSEMBLAGE ZONE OF THE KAROO BASIN, SOUTH AFRICA

机译:南非卡鲁盆地中二叠系TAP蛇头刺聚集区的臂突臂猿和斜齿象甲,双齿类(兽脚类,无羊膜)的评价

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Brachyprosopus broomi was described in 1937 based on a specimen from the Tapinocephalus Assemblage Zone (Karoo Basin, South Africa), but it was largely overlooked by subsequent workers. We have identified several new specimens that show that Brachyprosopus is a valid taxon. An autapomorphy for the taxon is a curled lateral edge of the squamosal that forms a lateral wall of the external adductor fossa. Other important characters are absence of anterior median palatal ridges; maxillary tooth rows bounded laterally by a shelf; unfused vomers; raised margins of the interpterygoid vacuity; broad intertemporal region; pineal boss; dentary tables; and a long, wide posterior dentary sulcus that extends posterior to the dentary teeth. Chelydontops altidentalis is a junior synonym of B. broomi. A phylogenetic analysis places Brachyprosopus among basal dicynodonts, not as a close relative of Endothiodon. It is noteworthy that some characters, such as well-developed medial maxillary tooth rows and the shape of the palatines, are shared by Brachyprosopus, Pristerodon, Endothiodon, and Niassodon, hinting that a final resolution of relationships among toothed dicynodonts remains to be achieved. Most Brachyprosopus specimens are from the upper Abrahamskraal Formation (Moordenaars and Karelskraal members). One specimen is from low in the Koonap Formation, just above the lowermost maroon mudrocks of the Beaufort Group, and an exact correlation between this level and the strata of the Abrahamskraal Formation is uncertain. Therefore, it is likely that the stratigraphic range of Brachyprosopus extends throughout the Tapinocephalus zone and possibly down into the Eodicynodon Assemblage Zone. SUPPLEMENTAL DATASupplemental materials are available for this article for free at www.tandfonline.com/UJVP Citation for this article: Angielczyk, K. D., B. S. Rubidge, M. O. Day, and F. Lin. 2016. A reevaluation of Brachyprosopus broomi and Chelydontops altidentalis, dicynodonts (Therapsida, Anomodontia) from the middle Permian Tapinocephalus Assemblage Zone of the Karoo Basin, South Africa. Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2016.1078342.
机译:Brachyprosopus broomi于1937年基于Tapinocephalus集合区(南非Karoo盆地)的标本进行了描述,但随后的工人在很大程度上忽略了它。我们发现了几个新样本,表明Brachyprosopus是有效的分类单元。分类单元的共形是鳞状细胞的卷曲的侧边缘,其形成了外收肌窝的侧壁。其他重要特征是前median中absence的缺失。上颌齿排由架子横向限制;未融合的vomers;翼状间隔增加的边缘;广泛的跨地区松果老板牙齿表;以及一个长而宽的后牙槽,延伸到牙齿的后方。 Chelydontops altidentalis是B. broomi的初级同义词。系统发育分析表明,Brachyprosopus位于基棘突类动物中,而不是Endothiodon的近亲。值得注意的是,Brachyprosopus,Pristerodon,Endothiodon和Niassodon具有某些特征,例如发达的上颌内侧齿排和rows骨的形状,这暗示着有齿双齿齿关系之间的最终解决仍有待实现。大多数短吻鳄标本来自上亚伯拉罕斯克拉尔地层(Moordenaars和Karelskraal成员)。一个标本来自库纳普组的低层,就在博福特群的最下层栗色泥岩之上,该水平与亚伯拉罕克拉尔组地层之间的确切相关性尚不确定。因此,很可能Brachyprosopus的地层范围会延伸到整个Tapinocephalus区,甚至可能向下延伸到Eodicynodon组合区。补充数据可在www.tandfonline.com/UJVP上免费获得本文的补充材料。本文的引用文献:Angielczyk,K。D.,B。S. Rubidge,M。O. Day和F. Lin。 2016年。对南非卡鲁盆地中部二叠纪塔头龙集合区的短臂龙(Brachyprosopus broomi)和虎嘴兰(Chelydontops altidentalis),双齿龙(Therapsida,Anomodontia)进行了重新评估。脊椎动物古生物学杂志。 DOI:10.1080 / 02724634.2016.1078342。

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