Hadrosaurs from Cañada Ancha (Cerro del Pueblo Formation; upper Campanian-?lower Maastrichtian), Coahuila, northeastern Mexico
At Cañada Ancha, about 15 km northwest of Saltillo, northeastern Mexico, deposits of the upper Campanian-?lower Maastrichtian Cerro del Pueblo Formation exhibit bone clusters of disarticulated hadrosaurids, tentatively assigned here based on maxillary features to Velafrons coahuilensis and a second...
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| Main Authors: | , |
|---|---|
| Format: | Article (Journal) |
| Language: | English |
| Published: |
7 August 2019
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| In: |
Cretaceous research
Year: 2019, Volume: 104 |
| ISSN: | 0195-6671 |
| DOI: | 10.1016/j.cretres.2019.104199 |
| Online Access: | Verlag, Volltext: https://doi.org/10.1016/j.cretres.2019.104199 Verlag: http://www.sciencedirect.com/science/article/pii/S0195667119301648 |
| Author Notes: | Sandra Rybakiewicz, Héctor E. Rivera-Sylva, Wolfgang Stinnesbeck, Eberhard Frey, José Rubén Guzmán-Gutiérrez, Rafael Vivas González, Rosalba Lizbeth Nava Rodríguez, José M. Padilla-Gutiérrez |
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| 520 | |a At Cañada Ancha, about 15 km northwest of Saltillo, northeastern Mexico, deposits of the upper Campanian-?lower Maastrichtian Cerro del Pueblo Formation exhibit bone clusters of disarticulated hadrosaurids, tentatively assigned here based on maxillary features to Velafrons coahuilensis and a second yet undetermined taxon. We discuss the taphonomy of the material as transported and buried on a delta plain. Orientation and breakage of bones as well as absence of strong abrasion indicate short-distance and high-energy transport by a viscose ‘flash flood’ or debris flow. | ||
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