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首页> 外文期刊>Canadian journal of earth sciences >A new centrosaurine ceratopsid from the Oldman Formation of Alberta and its implications for centrosaurine taxonomy and systematics
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A new centrosaurine ceratopsid from the Oldman Formation of Alberta and its implications for centrosaurine taxonomy and systematics

机译:来自亚伯达省奥尔德曼组的一种新的角龙碱角藻,及其对角龙碱分类学和系统学的影响

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摘要

Centrosaurus brinktnani (sp. nov) is distinguished from Centrosaurus apertus by key features of its cranial ornamentation, including the shape and orientation of the postorbital horn and parietal ornamentation at parietal locus 3, the shape of the parietal ornamentation at locus 2, and the possession of accessory parietal ossifications developed as short spines on the caudal parietal ramus. This species is restricted to the Oldman Formation of southern Alberta and is the oldest ceratopsid represented by diagnostic material in Canada. Phylogenetic analysis of the Centrosaurinae suggests that the development of spike-like ornamentation at the parietal locus 3 parietal locus is inversely related to the development of the Pi parietal ornamentation.
机译:颅缘龙(Centroosaurus brinktnani)(sp。nov)与颅内角龙(Centosaurus apertus)的主要区别在于其颅骨装饰,包括眶后角的形状和方向和顶位3的顶饰,顶位2的顶饰形状以及占有。顶壁副骨化发展为尾顶骨上的短刺。该物种仅限于艾伯塔省南部的奥尔德曼组,是加拿大诊断材料所代表的最古老的角藻。对Centosaurinae的系统发育分析表明,在顶位3顶位的穗状装饰的发展与Pi顶饰的发展成反比。

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