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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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Bibliographische Detailangaben
Hauptverfasser: Rybakiewicz, Sandra (VerfasserIn) , Stinnesbeck, Wolfgang (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: 7 August 2019
In: Cretaceous research
Year: 2019, Jahrgang: 104
ISSN:0195-6671
DOI:10.1016/j.cretres.2019.104199
Online-Zugang:Verlag, Volltext: https://doi.org/10.1016/j.cretres.2019.104199
Verlag: http://www.sciencedirect.com/science/article/pii/S0195667119301648
Volltext
Verfasserangaben: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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