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首页> 外文期刊>Scottish Journal of Geology >A large, anatomically primitive tristichopterid (Sarcopterygii: Tetrapodomorpha) from the Late Devonian (Frasnian) Alves Beds, Upper Old Red Sandstone, Moray, Scotland
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A large, anatomically primitive tristichopterid (Sarcopterygii: Tetrapodomorpha) from the Late Devonian (Frasnian) Alves Beds, Upper Old Red Sandstone, Moray, Scotland

机译:来自晚泥盆纪(弗拉斯尼亚人)阿尔维斯床,上部老红砂岩,海鳗,苏格兰的大型解剖原始三栖类(Sarcopterygii:Tetrapodomorpha)

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摘要

A nearly complete mandible of a large tetrapodomorph sarcopterygian from the Frasnian Alves Beds is studied with the aid of computed tomography. The absence of cosmine, a small parasymphysial dental plate bearing dentition that is discontinuous with that of the coronoids, and the presence of an elongated posterior coronoid that bears two fang pairs restrict placement of the tetrapodomorph from the Alves Beds to Tristichopteridae, and suggest that is a member of the clade that is sister to the anatomically primitive Givetian genus Tristichopterus. Taxa from this segment of tristichopterid phylogeny include the Givetian-Frasnian Eusthenopteron and Frasnian Jarvikina, but the tristichopterid from the Alves Beds is distinguished from both by the presence of an organized row of well-developed teeth on the posterior coronoid. This character has been proposed as a synapomorphy of taxa crownward of Trischopteridae, but is widely distributed among tetrapodomorph fishes. Our reinterpretation of lower jaw material of Tinirau clackae suggests this species is a member of the Tristichopteridae rather than the 'Elpistostegalia', and likely includes material assigned to a second species and genus of tetrapodomorph from the Red Hill site, Bruehnopteron murphyi. Proposal of a formal taxonomic name for the tristichopterid from the Alves Beds is withheld pending the discovery or analysis of further material from these deposits.
机译:借助计算机断层扫描技术,研究了来自弗拉斯尼亚阿尔维斯河床的大型四足类食肉动物的下颌骨。缺少胭脂红,没有一个与副冠突不连续的小副共齿牙板,并且存在一个带有两个齿对的细长的后冠突,限制了四足纲动物从阿尔维斯床到腕足科的定位。属于解剖学上的吉维恩属Tristichopterus的进化枝成员。来自该三翅类系统发育的这一部分的分类单元包括Givetian-Frasnian Eusthenopteron和Frasnian Jarvikina,但来自阿尔维斯河床的三翅类动物的区别在于后冠上有排排的发育良好的牙齿。该特征已被提出为Trischopteridae的类群冠状突触的同形,但是在四形体鱼类中广泛分布。我们对Tinirau clackae的下颌材料的重新解释表明,该物种是Tristichopteridae的一个成员,而不是'Elpistostegalia',并且可能包括来自红山遗址Bruehnopteron murphyi的第二种和四足类属的材料。在发现或分析这些矿床中的其他物质之前,暂不建议从Alves床获得直翅类的正式生物分类名称。

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