首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >Phyllodont tooth plates of Bobasatrania scutata (GERVAIS, 1852) (Actinoperygii, Bobasatraniiformes) from the Middle Triassic (Longobardian) Grenzbonebed of southern Germany and eastern France, with an overview of Triassic and Palaeozoic phyllodont tooth plates
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Phyllodont tooth plates of Bobasatrania scutata (GERVAIS, 1852) (Actinoperygii, Bobasatraniiformes) from the Middle Triassic (Longobardian) Grenzbonebed of southern Germany and eastern France, with an overview of Triassic and Palaeozoic phyllodont tooth plates

机译:来自德国南部和法国东部的中三叠纪(Longobardian)Grenzbonebed的Bobasatrania scutata的齿状齿盘(GERVAIS,1852年)(Actinoperygii,Bobasatraniiformes),并概述了三叠纪和古生代的齿齿牙盘

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摘要

Phyllodont tooth plates from the Longobardian Grenzbonebed of southern Germany known for more than 170 years are described in detail for the first time. They consist of up to eight layers of superimposed rounded to conical teeth, each layer with up to 300 teeth. An upper and a lower tooth plate can be differentiated with different outlines and reliefs of the chewing surface. Identical dentitions have been described by GERVAIS (1852) under the names Colobodus scutatus (upper tooth plate) and C. hogardi (lower tooth plate) from the uppermost Muschelkalk of Lorraine, France. The superposition of the teeth and the missing of a wart on top of the teeth support the transfer of C. scutatus to the genus Bobasatrania known by complete skeletons with phyllodont tooth plates from the Early Triassic of Madagascar, Greenland and further localities. Bobasatrania scutata represents the youngest record of the genus. The tooth plates are best documented of all Bobasatrania dentitions and are compared with all known Early Mesozoic and Late Palaeozoic phyllodont tooth plates. An up to now unmentioned record of a Bobasatrania tooth plate from the Early Triassic of the Salt Range, Pakistan, is described. The tooth plates of Bobasatrania act as a tongue-bite apparatus known from osteoglossomorph fishes.
机译:首次详细介绍了来自德国南部Longobardian Grenzbonebed已有170多年历史的Phyllodont齿板。它们由多达八层的叠加成圆形的圆锥齿组成,每层最多有300个齿。上齿板和下齿板可以通过咀嚼表面的不同轮廓和凸纹来区分。 GERVAIS(1852)已从法国洛林最上层的Muschelkalk以名称Colobodus scutatus(上牙板)和C. hogardi(下牙板)描述了相同的牙列。牙齿的重叠以及牙齿顶部的疣的缺失支持了梭状芽胞杆菌向Bobasatrania属的转移,Bobasatrania属由马达加斯加早期三叠纪,格陵兰及其他地方的完整具骨架的齿状齿牙板已知。 Bobasatrania scutata代表该属的最年轻记录。牙盘最好记录在所有博巴拉斯坦齿列中,并与所有已知的早期中生代和晚期古生代齿齿牙盘进行比较。描述了巴基斯坦盐岩山脉早期三叠纪的一个波巴萨变迁牙盘的迄今未提及的记录。 Bobasatrania的牙齿板起着舌状骨鱼类已知的舌咬装置的作用。

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