Coahuilasaurus lipani, a New Kritosaurin Hadrosaurid from the Upper Campanian Cerro Del Pueblo Formation, Northern Mexico

Diversity Pub Date : 2024-09-01 DOI:10.3390/d16090531
Nicholas R. Longrich, Angel Alejandro Ramirez Velasco, Jim Kirkland, Andrés Eduardo Bermúdez Torres, Claudia Inés Serrano-Brañas
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Abstract

The Late Cretaceous of Western North America (Laramidia) supported a diverse dinosaur fauna, with duckbilled dinosaurs (Hadrosauridae) being among the most speciose and abundant members of this assemblage. Historically, collecting and preservational biases have meant that dinosaurs from Mexico and the American Southwest are poorly known compared to those of the northern Great Plains. However, evidence increasingly suggests that distinct species and clades inhabited southern Laramidia. Here, a new kritosaurin hadrosaurid, represented by the anterior part of a skull, is reported from the late Campanian of the Cerro del Pueblo Formation, ~72.5 Ma, in Coahuila, Mexico. The Cerro del Pueblo Formation kritosaur was originally considered to represent the same species as a saurolophine from the Olmos Formation of Sabinas, but the Sabinas hadrosaur is now considered a distinct taxon. More recently, the Cerro del Pueblo Formation kritosaur has been referred to Kritosaurus navajovius. We show it represents a new species related to Gryposaurus. The new species is distinguished by its large size, the shape of the premaxillary nasal process, the strongly downturned dentary, and massive denticles on the premaxilla’s palatal surface, supporting recognition of a new taxon, Coahuilasaurus lipani. The dinosaur assemblage of the Cerro del Pueblo Formation shows higher diversity than the contemporaneous fauna of the Horseshoe Canyon Formation in Alberta. Furthermore, Kritosaurini, Lambeosaurini, and Parasaurolophini all persist into the latest Campanian in southern Laramidia after disappearing from northern Laramidia. These patterns suggest declining herbivore diversity seen at high latitudes may be a local, rather than global phenomenon, perhaps driven by cooling at high latitudes in the Late Campanian and Maastrichtian.
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墨西哥北部上坎帕尼亚Cerro Del Pueblo地层出土的一种新的角龙类巨龙--Coahuilasaurus lipani
北美洲西部的晚白垩世(Laramidia)拥有多种多样的恐龙动物群,其中鸭嘴龙(Hadrosauridae)是这一动物群中种类最多、数量最大的成员。从历史上看,由于采集和保存上的偏差,墨西哥和美国西南部的恐龙与大平原北部的恐龙相比鲜为人知。然而,越来越多的证据表明,拉拉米迪亚南部栖息着独特的物种和支系。本文报告了墨西哥科阿韦拉州Cerro del Pueblo地层坎盆纪晚期(约72.5Ma)的一种新的克利龙类剑龙,其头骨的前半部分为代表。塞罗德尔普韦布洛地层的克利龙最初被认为与萨比纳斯奥尔莫斯地层的栉龙代表同一物种,但萨比纳斯栉龙现在被认为是一个独立的类群。最近,Cerro del Pueblo Formation 的剑龙被称为 Kritosaurus navajovius。我们证明它是与蝼蛄龙有关的一个新物种。该新种的特点是体型巨大、前颌鼻突的形状、强烈下翘的齿槽以及前颌腭面上的巨大齿列,从而支持了新类群 Coahuilasaurus lipani 的认定。Cerro del Pueblo地层的恐龙组合比阿尔伯塔省马蹄峡谷地层的同期动物群显示出更高的多样性。此外,Kritosaurini、Lambeosaurini和Parasaurolophini在拉腊米迪亚北部消失后,在拉腊米迪亚南部一直持续到坎盆纪晚期。这些模式表明,在高纬度地区出现的食草动物多样性下降可能是一种局部现象,而不是全球性现象,其原因可能是在晚钟元世和马斯特里赫特世的高纬度地区出现了降温。
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