Huehuecanauhtlus

Huehuecanauhtlus is an extinct genus of hadrosauroid dinosaur known from the Late Cretaceous (Santonian stage) of Michoacán, western Mexico. It contains a single species, Huehuecanauhtlus tiquichensis.
Etymology.
"Huehuecanauhtlus" was first described and named by Angel Alejandro Ramírez-Velasco, Mouloud Benammi, Albert Prieto-Márquez, Jesús Alvarado Ortega and René Hernández-Rivera in 2012 and the type species is "Huehuecanauhtlus tiquichensis". The generic name is derived from Náhuatl (group of dialects related to the Aztecan languages) "huehuetl", meaning "ancient" and "canauhtli", meaning "duck" in reference to its hadrosauroid affinities. The correct pronunciation of the generic name is "UEUE-CANA-UHh-TLUS". The specific name, "tiquichensis", honors the town of Tiquicheo, for the generosity and hospitality of its people during the fieldwork season.
Discovery.
"Huehuecanauhtlus" is known only from two individuals. The holotype IGM 6253 represented by fragmentary skull (partial left maxilla and dentary fragment) and postcranial skeleton including four cervical vertebrae, nine dorsal vertebrae, four dorsal neural spines, one dorsal diapophysis, five right dorsal ribs, seven left dorsal ribs, seven sacral neural spines, seven sacral diapophyses, one caudal diapophysis, three caudal vertebrae, two caudal neural spine, eight fragmentary ossified tendons, left and right partial ilium, and left and right partial pubis. The smaller paratype, IGM 6254, is represented by fragment of left dentary, two teeth, and one cervical prezygapophysis.
Both specimens were collected at the Barranca Los Bonetes locality in Tuzantla, Michoacán. The holotype came from the sixth fossiliferous spot, whereas the paratype came from the third spot, of an unnamed formation, dating to the Santonian stage of the Late Cretaceous period, about 85.8-83.5 million years ago.
Description.
Ramírez-Velasco "et al." (2012) diagnosed "Huehuecanauhtlus" by a unique combination of characters. For example, two teeth exposed on the occlusal plane of the rostral third and the posterior third of the dentary and maxilla, respectively. It had seven sacral vertebrae and tall neural spines of posterior vertebrae, being between 3.5 and 4 times taller than their corresponding centra. As in "Claosaurus", its supraacetabular process is as long as 75% of the length of the central iliac plate, with an apex located above the posteroventral corner of the ischiac tuberosity. It differs from other hadrosauroids in possessing an extremely deflected preacetabular process of the ilium, so that the bisecting long axis of the process forms an angle less than 130° with the horizontal plane defined by the ischiac and pubic peduncles. It can be differentiated from basal hadrosauroids in having a very deep concave profile of the dorsomedial margin of the iliac plate, adjacent to the supraacetabular process. A phylogenetic analysis performed by Ramírez-Velasco "et al." (2012) found a big polytomy of all hadrosauroids which are more derived than "Probactrosaurus" but less derived than Hadrosauridae. The exclusion of "Claosaurus", "Jeyawati", "Levnesovia", "Nanyangosaurus", "Shuangmiaosaurus" and "Telmatosaurus" from the polytomy resulted in a more resolved topology. The cladogram below shows "Huehuecanauhtlus" phylogenetic position among other hadrosauroids following this topology (the relationships within Hadrosauridae are not shown).