Huehuecanauhtlus tiquichensis, a new hadrosauroid dinosaur (Ornithischia: Ornithopoda) from the Santonian (Late Cretaceous) of Michoacán, Mexico

Author:

Ramírez-Velasco Angel Alejandro1,Benammi Mouloud2,Prieto-Márquez Albert3,Ortega Jesús Alvarado4,Hernández-Rivera René4

Affiliation:

1. Facultad de Medicina Veterinaria y Zootecnia UNAM, Circuito de Investigación Científica, Ciudad Universitaria, Delegación de Coyoacán, 04510 Mexico D.F., Mexico.

2. Instituto de Geofísica UNAM, Circuito de Investigación Científica, Ciudad Universitaria, Delegación de Coyoacán, 04510 Mexico D.F., Mexico.

3. Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, D-80333 Munich, Germany.

4. Instituto de Geología UNAM, Circuito de Investigación Científica, Ciudad Universitaria, Delegación de Coyoacán, 04510 Mexico D.F., Mexico.

Abstract

Huehuecanauhtlus tiquichensis gen. et sp. nov. is the southernmost diagnostic basal hadrosauroid in the Americas. The holotype and referred material of this taxon came from Santonian strata in the Michoacán State, southwestern Mexico. Huehuecanauhtlus tiquichensis is diagnosed on the basis of a combination of dental, axial, and appendicular characters, including the following: at least two teeth exposed on the occlusal plane of the dentary and maxilla; seven sacral vertebrae; tall neural spines of caudal vertebrae; supraacetabular process long; and short and trapezoidal (in lateral view) postacetabular process. It differs from other hadrosauroids in having an ilium with extreme ventral deflection of the preacetabular process. Maximum parsimony cladistic analysis placed H. tiquichensis as a closely related outgroup to Hadrosauridae. The occurrence of H. tiquichensis in the Santonian of North America may be explained as a dispersal event from Asia to North America that occurred no later than the Albian or, alternatively, as a vicariant event of a most recent common ancestor widespread in both landmasses.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

Reference57 articles.

1. Altamira-Areyán, A. 2002. Las litofacies y sus implicaciones de la Cuenca sedimentaria Cutzamala–Tiquicheo, Estado de Guerrero y Michoacán, México. M.Sc. thesis, Instituto de Geología, Universidad Nacional Autónoma de México, Mexico.

2. Altamira-Areyán, A., Martínez-Hernández, E., and Centeno-García, E. 2000. Facies, paleoambientes y paleoclimas del Paleoceno–Eoceno de la zona norte de Tierra Caliente, estados de Michoacán y Guerrero. In 2a Reunión Nacional de Ciencias de la Tierra: Unión Geofísica Mexicana, Geos, época II 20 [Abstract]: 157.

3. Maximum Agreement Subtree in a Set of Evolutionary Trees: Metrics and Efficient Algorithms

4. Benammi, M., Mariscal-Ramos, C., Centeno-García, E., Morales-Gámez, M., Tolson, G., and Urrutia-Fucugauchi, J. 2006. Preliminary magnetostratigraphic study of the Upper Cretaceous Dinosaur Site from La Barranca Los Bonetes, Tiquicheo (Michoacan State, Southern Mexico). European Geosciences Union, Vienne, Austria. [Abstract.]

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