...
首页> 外文期刊>Acta Palaeontologica Polonica >The enamel microstructure of Manidens condorensis: New hypotheses on the ancestral state and evolution of enamel in Ornithischia
【24h】

The enamel microstructure of Manidens condorensis: New hypotheses on the ancestral state and evolution of enamel in Ornithischia

机译:Manidens Condorensis的牙釉质微观结构:对奥尼斯奇亚祖先州的新假设和牙釉质的演变

获取原文
获取原文并翻译 | 示例
           

摘要

Previous studies on enamel microstructure in Ornithischia have focused on derived lineages of this Glade based on species from the northern hemisphere. Here we describe the enamel microstructure of Manidens condorensis from the late Early Jurassic of Argentina that belongs to Heterodontosauridae (interpreted as the basal-most Glade of Omithischia). Enamel microstructure in the cheek teeth lacks a basal unit layer, presents incipient divergent crystallite as the dominant enamel type and parallel crystallite enamel type (with or without incrementing lines). Enamel of maxillary and dentary teeth differs from each other in enamel distribution (asymmetric vs. symmetric), structure (presence vs. absence of tubules, and less vs. more abundant parallel crystallite enamel with incrementing lines) and ordering (regular ordering of enamel types vs. in patches). The enamel microstructure of Manidens is the simplest of all known Ornithischia, and is more similar to that of the sauropodomorph Plateosaurus than to the one reported for the basal theropod Coelophysis. Similarities within Ornithischia are present with pachycephalosaurids and, to a lesser extent, with ankylosaurs. Phylogenetic optimization of enamel characters in Ornithischia allows the inference of new ancestral states for the internal nodes of the major lineages and to highlight evolutionary transformations: (i) absence of a basal unit layer and presence of parallel crystallite and incipient divergent columnar enamel as the ancestral state for Omithischia; (ii) the shared presence of incipient divergent columnar units or poorly developed divergent columnar enamel in Pachycephalosauridae and Thyreophora represents a retention of the plesiomorphic omithischian condition; (iii) the wavy enamel of Dryomozpha evolved from the ancestral incipient divergent columnar units present in Omithopoda and; (iv) enamel thickness and asymmetry has independently evolved at least four times in Ornithischia.
机译:以前关于牙癣菌的牙釉质微观结构的研究专注于基于来自北半球的物种的该沼泽的衍生谱系。在这里,我们描述了来自阿根廷已故侏罗纪的Manidens Condorensis的搪瓷微观结构,属于Heterodontosauridae(被解释为omithischia的基础最沼泽)。脸颊牙齿中的搪瓷微观结构缺乏基底单元层,呈初始发散微晶作为主要牙釉质型和平行微晶搪瓷型(有或不递增线)。上颌和凹形牙齿的搪瓷在牙釉质分布(非对称与对称)中彼此不同,结构(具有小管的缺失,较少的与递增线的更丰富的平行晶体搪瓷)和订购(定期排序牙釉质类型vs.在补丁中)。领域的搪瓷微观结构是最简单的所有已知的鸟癣,而且与Sauropodomorph Plateaurus更类似于据报道的基底opopo ope脱水的牙龙。奥纳里斯奇亚内的相似性伴有嗜久症和较小程度的血管龙。牙龈上的搪瓷性状的系统发育优化允许新的祖先州的内部节点推断主要谱系的内部节点,并突出进化转化:(i)缺乏基础单元层和平行微晶的存在和初期的分歧柱状牙釉质作为祖先迄今为止的国家; (ii)在Pachycephalosauridae和硫代酚肽中发出的初期发出柱状单位或发育不良发达的发出柱状牙釉质的共同存在代表了Plesiomorphic omithischian条件的保留; (iii)Dryomozpha的波浪珐琅质从omithopoda和祖先初期发出的柱状单位演变而来; (iv)牙釉质厚度和不对称性在奥纳里斯奇亚的至少四次独立地发展。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号