Kazakhstanosaurus efimovi Yakupova et Akhmedenov sp. nov. (Ichthyosauria, Undorosauridae), a New Species from the Upper Jurassic Deposits of the Middle Volga Region
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引用次数: 0
Abstract
The skeleton fragments of a new ichthyosaur species, Kazakhstanosaurus efimovi Yakupova et Akhmedenov sp. nov., from the Middle Volgian substage of the Upper Jurassic of the Middle Volga region (Ulyanovsk region, Gorodishche section) are described. The species is assigned to the genus Kazakhstanosaurus V. Efimov Akhmedenov et Yakupova, 2019 (fam. Undorosauridae), which has been recently described from the same-age deposits of Kazakhstan. The new species is diagnosed by the following characters: the subquadrate shape of the trunk vertebrae; the structure of the shoulder girdle and forelimbs, which have a two-facet distal end of the humerus and a weak articulation of the first finger; an increased size of all parts of the skeleton; the costal facets positioned on the sides of the end of the ribs; the connection of the costal facets with a bone crest. The facets of the ribs are connected by a bony ridge. The discovery of Kazakhstanosaurus efimovi confirms the connection of the Russian Sea during the Late Jurassic with the warm waters of the Tethys Ocean. Probably, the progenitors of undorosaurids descended from the Triassic and Early Jurassic ichthyosaurs that lived in the tropical regions of the eastern part of the Tethys Ocean. In the Late Jurassic, these ichthyosaurs migrated to the territory of modern Kazakhstan and Eastern Europe, settled in the shallow Russian Sea, and gave rise to representatives of the families Undorosauridae and Platypterygius.
哈萨克斯坦stanosaurus efimovi Yakupova et Akhmedenov sp. 11 .(鱼龙目,下龙科),中伏尔加河地区上侏罗统沉积新种
描述了中伏尔加地区上侏罗统中伏尔加亚期(乌里扬诺夫斯克地区Gorodishche剖面)的一种新鱼龙——Kazakhstanosaurus efimovi Yakupova et Akhmedenov p. nov.)的骨骼碎片。该物种归属于Kazakhstanosaurus V. Efimov Akhmedenov et Yakupova, 2019 (fam)。Undorosauridae),最近在哈萨克斯坦的同年龄矿床中被描述。新种的诊断依据如下特征:躯干椎骨呈近方形;肩带和前肢的结构,其肱骨远端有一个双关节面和第一指的弱关节;骨骼的所有部分都增大了;肋面位于肋骨末端两侧的肋面;肋面与骨嵴的连接肋骨的各面由骨脊连接。“Kazakhstanosaurus efimovi”的发现证实了晚侏罗纪时期的俄罗斯海与特提斯洋的温暖水域之间的联系。也许,下龙的祖先是生活在特提斯洋东部热带地区的三叠纪和早侏罗世鱼龙的后代。在晚侏罗世,这些鱼龙迁移到现代哈萨克斯坦和东欧的领土,定居在俄罗斯海的浅海,并产生了Undorosauridae和Platypterygius家族的代表。