墨西哥科阿韦拉Cerro del Pueblo Formation (Campanian)的La Parrita地区发现的第一个鳄鱼形化石

Héctor E. Rivera-Sylva, Gerardo Carbot-Chanona, Rafael Vivas-González, Lizbeth Nava-Rodríguez, Fernando Cabral-Valdéz
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引用次数: 2

摘要

科阿韦拉Cerro del Pueblo组(晚白垩纪,坎帕尼亚)陆地四足动物的记录包括海龟、翼龙、恐龙和鳄鱼形动物。最后一组以角叶类、不确定真叶类和蒙大拿州短叶类为代表。鳄鱼形目是一种已灭绝的鳄鱼形目,是一种已灭绝的鳄鱼形目,是一种已灭绝的鳄鱼形目,是一种已灭绝的鳄鱼形目,是一种已灭绝的鳄鱼形目,是一种已灭绝的鳄鱼形目。鳄鱼形目、海龟、恐龙和cariofite卵母细胞的组合为白垩纪晚期Cerro del Pueblo形成的热带三角洲平原的河流环境提供了证据。在科阿韦拉的Cerro del Pueblo组(晚白垩纪,坎帕尼亚)的陆地四足动物记录包括海龟、翼龙、恐龙和鳄鱼类。= =地理= =根据美国人口普查,这个县的总面积是,其中土地和(1.694平方公里)水。In this work we report the first crocodyliform仍然from帕里locality地层,based on one属于人民,希尔牙、vertebrae和osteoderms。鳄鱼类、海龟、恐龙和oogonia charophyte的结合为白垩纪晚期Cerro del Pueblo形成的热带三角洲平原上的河流环境提供了证据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The first crocodyloform remains from the La Parrita locality, Cerro del Pueblo Formation (Campanian), Coahuila, Mexico
espanolEl registro de tetrapodos terrestres en la Formacion Cerro del Pueblo (Cretacico tardio, Campaniano) en Coahuila, incluye tortugas, pterosaurios, dinosaurios y crocodyliformes. Este ultimo grupo esta representado por goniofolididos, eusuquios indeterminados y Brachychampsa montana. En este trabajo se reportan los primeros restos de crocodyliformes de la localidad La Parrita, Formacion Cerro del Pueblo, con base en un diente aislado, vertebras y osteodermos. La asociacion de crocodyliformes, tortugas, dinosaurios y oogonias de cariofitas, proporcionan evidencia de ambientes fluviales en una llanura deltaica de tipo tropical para la Formacion Cerro del Pueblo durante el Cretacico tardio. EnglishThe record of land tetrapods of the Cerro del Pueblo Formation (Late Cretaceous, Campanian), in Coahuila, includes turtles, pterosaurs, dinosaurs, and crocodyliforms. This last group is represented only by goniopholidids, indeterminate eusuchians, and Brachychampsa montana. In this work we report the first crocodyliform remains from La Parrita locality, Cerro del Pueblo Formation, based on one isolated tooth, vertebrae, and osteoderms. The association of crocodyliforms, turtles, dinosaurs, and charophyte oogonia provide evidence for stagnant to fluvial environments on a delta plain with tropical climate for the Cerro del Pueblo Formation during the Late Cretaceous.
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