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Upper Ordovician chondrichthyan-like scales from North America

机译:来自北美的上奥陶纪软骨类鳞片

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摘要

Studies of Ordovician micromeric fish scales from the Sandbian of North America have identified a number of scale-based taxa potentially referable to the chondrichthyans and therefore can be among the stratigraphically oldest representatives of the clade described to date. Two of these, Tezakia hardingensis gen. et sp. nov. and Canyonlepis smithae gen. et sp. nov., are formally described herein. Tezakia gen. nov. scales are composed exclusively of tubular dentine and possess polyodontocomplex crowns with a characteristically large primordial odontode. Similar scale crown architecture has been reported only in the reputed chondrichthyan Altholepis composita (Lower Devonian of Podolia, Ukraine), and on these grounds, the two are united within the newly erected Altholepidiformes ordo nov. Multiple odontocomplexes are also a feature of Canyonlepis gen. nov. scale crowns; however, the latter do not demonstrate prominent primordial odontodes and are supported by a base composed of acellular bone. Additional data suggest that both taxa possess a combination of characteristics (areal crown growth, scale symmetry, linear odontocomplex architecture and absence of enamel, osteons, cancellous bone and hard-tissue resorption) previously documented to occur only in chondrichthyan scales. This study contributes to a growing body of evidence that reveals the presence of diverse tissue types (bone, tubular and atubular dentine) and morphogenetic patterns (odontocomplex and non-odontocomplex type of scale crown growth) in the dermal skeleton of putative Ordovician chondrichthyans.
机译:对来自北美桑德比亚的奥陶纪鱼类鱼类鳞片的研究已经发现了一些可能基于软骨鱼类的鳞片类群,因此可以成为迄今为止描述的进化枝中最古老的代表之一。其中两个是手足草海丁属。等。十一月和Canyonlepis smithae gen。等。 nov。,在本文中正式描述。特崎市十一月鳞片仅由管状牙本质组成,并具有带有特征性的大原始齿状牙齿的多齿复合冠。仅在著名的软骨鱼纲Altholepis composita(乌克兰波多利亚的下泥盆纪)中,才报道过类似规模的皇冠建筑,并且基于这些理由,两者在新近建成的Altholepidiformes ordo nov中结合在一起。多种牙本质复合体也是Canyonlepis gen的特征。十一月刻度冠然而,后者并没有显示出明显的原始齿状突,而是由无细胞骨骼组成的基底支撑。其他数据表明,这两个类群都具有以前记录的仅在软骨鱼类鳞片中出现的特征组合(区域冠生长,鳞片对称,线性齿状复杂结构以及缺少牙釉质,骨质,松质骨和硬组织吸收)。这项研究为越来越多的证据做出了贡献,这些证据揭示了假定的奥陶纪软骨鱼类的真皮骨架中存在着多种组织类型(骨骼,管状和小管牙本质)和形态发生模式(鳞状冠生长的牙本质和非牙本质复杂类型)。

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