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A new omalodontid-like shark from the Late Devonian (Famennian) of western Siberia, Russia

机译:来自俄罗斯西伯利亚西伯利亚的晚德文尼亚(芬元)的新omalodontid样鲨

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Teeth belonging to a new chondrichthyan, Siberiodus mirabilis gen. et sp. nov., are described from the Famennian Pescherka and Podonino Formations of the Kuznetsk Basin, and the Cheybekkiol' Formation of Gorniy Altay, western Siberia. The Pescherka Formation is early Famennian based on conodonts (crepida-marginifera conodont zones), and the Podonino Formation is late Famennian (trachytera-expansa zones). The Cheybekkiol' Formation is also early Famennian (Middle triangularis-Ea?y rhomboidea zones). The teeth of the several omalodontid-like taxa are characterised by a base with a labial extension, and a reduced lingual part, and most show asymmetry of the crown. The new taxon differs from other such forms in the external and histological structures of the crown, and the type ofvascularisation system. It is suggested that chondrichthyan teeth with a labial base extension could have arisen separately in several shark groups.
机译:牙齿属于新的Chondrichthyan,西伯利亚米拉巴里斯根。等SP。 11月。,由古筝盆栽盆地的Famennian Pescherka和Podonino形成,以及Cheybekkiol'在西伯利亚的Gorniy Altay的形成。 Pescherka形成是基于Conodonts(Crepida-Margifera Conodont区)的初期神话人,并且Podonino的形成是已故的Famennian(Trachytera-Beakea区)。 Cheybekkiol'的形成也是神的神仙(中间Triangularis-EA?Y菱形区域)。几个omalodontid样的齿株的牙齿的特征在于底部具有唇延伸的底座,以及减少的舌部件,并且大多数显示冠部的不对称性。新的分类群不同于冠部的外部和组织学结构中的其他形式,以及血管体系的类型。建议在几个鲨鱼组中可以分别出现具有唇缘延伸的软骨菌牙齿。

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