Coahuilasaurus lipani, a New Kritosaurin Hadrosaurid from the Upper Campanian Cerro Del Pueblo Formation, Northern Mexico
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Published:2024-09-01
Issue:9
Volume:16
Page:531
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ISSN:1424-2818
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Container-title:Diversity
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language:en
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Short-container-title:Diversity
Author:
Longrich Nicholas R.1ORCID, Ramirez Velasco Angel Alejandro2ORCID, Kirkland Jim3, Bermúdez Torres Andrés Eduardo4, Serrano-Brañas Claudia Inés45ORCID
Affiliation:
1. Department of Life Sciences, University of Bath, Bath BA2 7AY, UK 2. Instituto Nacional de Antropología e Historia, Córdoba 45, Roma Norte, Cuauhtémoc, Mexico City 06700, Mexico 3. Utah Geological Survey, Salt Lake City, UT 84114, USA 4. Benemérita Escuela Normal de Coahuila, Calzada de los Maestros 858, Zona Centro Poniente, Saltillo 25000, Mexico 5. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 37012, USA
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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