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Cerro del Pueblo Formation | |
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Stratigraphic range: Campanian ~ | |
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Type | Geological formation |
Unit of | Difunta Group |
Underlies | Cerro Huerta Formation |
Overlies | Parras Shale |
Thickness | 160 m (520 ft) |
Lithology | |
Primary | Mudstone, sandstone |
Other | Siltstone, conglomerate, limestone |
Location | |
Coordinates | 26°06′N101°06′W / 26.1°N 101.1°W |
Approximate paleocoordinates | 32°12′N75°30′W / 32.2°N 75.5°W |
Region | Coahuila |
Country | ![]() |
Extent | Parras Basin |
The Cerro del Pueblo Formation is a geological formation in Coahuila, Mexico, whose strata date back to the latest Campanian of the Late Cretaceous, just before the Campanian-Maastrichtian boundary. Dinosaur remains are among the fossils that have been recovered from the formation. [1] The formation is believed to correlate with the Baculites reesidesi and Baculites jenseni ammonite zones, which dates it to 73.63-72.74 Ma. [2]
The Cerro del Pueblo Formation includes marine, brackish, and non-marine environments, and was laid down in a coastal lowland environment, with Coahuila being on the edge of the Western Interior Seaway at the time. Fossils are abundant in the Cerro del Pueblo Formation, and include dinosaurs and other vertebrates, plants and seeds, and invertebrates including oysters, snails, and other molluscs. The formation is underlain by the Parras Shale and is overlain by the Cerro Huerta Formation.
Remains of the following ornithischians have been found in the formation: [3]
Ankylosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Ankylosauria [3] | Indeterminate [3] | A femur fragment, phalanx and a possible osteoderm. [3] | Indeterminate ankylosaur remains. [3] | |
Ankylosauridae [3] | Indeterminate [3] | Osteoderms. [3] | Indeterminate ankylosaurid remains. [3] | |
Nodosauridae [3] | Indeterminate [3] | A caudal vertebra, osteoderms and a tooth. [3] | Indeterminate nodosaurid remains. [3] | |
Ceratopsians of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Centrosaurinae [3] | Indeterminate [3] | A partial right squamosal. [3] | Probably represents a new taxon. [3] | |
Ceratopsidae [3] | Indeterminate [3] | Squamosal fragment, metatarsal, metacarpal, sacral vertebrae, proximal end of femora, proximal end of ulna, possible frill fragments and teeth. [3] | Indeterminate ceratopsid remains. [3] | |
Chasmosaurinae [3] | Indeterminate [3] | Supraorbital horncores, an orbit, dorsal vertebra, indeterminate cranial fragments, limb bones, and unspecified postcranial elements pertaining to juvenile specimens. [3] | Indeterminate chasmosaurine remains belonging to juvenile specimens. [3] | |
Ornithopods of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Coahuilasaurus [4] | C. lipani [3] | A kritosaurin hadrosaurid | ![]() ![]() ![]() ![]() | |
Hadrosauridae [3] | Indeterminate [3] | A braincase, postorbital, quadrate, laterosphenoid, dentaries, mandibles, maxillae, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, neural spines, ribs, ilium, femora, fibulae, tibiae, humeri, ulnae, metatarsals, metacarpals, pedal phalanxes, pedal phalanges, pedal ungula, phalanges, phalanxes, various bone fragments, fibulae, scapulae, radii, coracoids, astragali, indeterminate pelvic bones, ossified tendons, isolated teeth and integumentary impressions. [3] | Indeterminate hadrosaurid remains from numerous specimens. [3] | |
Kritosaurus [5] | K. navajovius [5] | Predentary, symphyseal processes, rostral portion of dental battery of dentaries, rostral region of premaxillae, and fragments of maxilla. [5] | A kritosaurin hadrosaurid, originally referred to K. navajovius, [5] but reclassified to Coahuilasaurus . | |
Lambeosaurinae [3] | Indeterminate [3] | Maxillae, premaxillae, quadrate, partial braincase, dentaries, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, neural spines, ribs, ilia, ischium, femora, fibulae, tibiae, humeri, ulnae, metatarsals, metacarpals, pedal phalanges, phalanges, pedal unguals, astragali, radii, scapulae, pubes and other unprepared elements. [3] | Indeterminate lambeosaurine remains from numerous specimens, including a large hadrosaurid. [3] | |
Latirhinus [6] | L. uitstlani [6] | Caudal vertebrae, scapulae, humeri, ulnae, coracoid, metacarpals, manual ungual, ilia, ischia, femora, tibiae, fibula, and astragalus. [6] | Holotype specimen is chimeric as it consists of multiple individuals. Some material from the holotype specimen is assigned to Lambeosaurinae indet. and Saurolophinae indet.. [7] | |
Saurolophinae [3] | Indeterminate [3] | A braincase, brain endocast, dentaries, maxillae, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, chevrons, neural spines, ribs, ilium fragments, femora, fibulae, tibiae, humeri, ulnae, metatarsals, phalanges, phalanxes, scapulae, a possible coracoid, radii, ossified tendons, and undescribed juvenile specimens. [3] | Indeterminate saurolophine remains from numerous specimens, including juvenile individuals. [3] | |
Tlatolophus [8] | T. galorum [8] | An almost complete skull, mandible, partial ilium, partial ischium, a femur, scapula, coracoid, sacral vertebrae, caudal vertebrae, and chevrons. [8] | A parasaurolophin hadrosaur, closely related to Charonosaurus and Blasisaurus . [8] | |
Velafrons [9] | V. coahuilensis [9] | Dentaries, predentaries, ceratobranchial, premaxillae, maxillae, jugal, quadrate, nasal, skull roof, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, neural arches, cervical ribs, ribs, chevrons, scapula, coracoids, humeri, ulnae, radii, metacarpals, manual phalanges, ilium, ischia, pubes, femora, tibiae, astragalus, metatarsals and pedal phalanges. [9] | A lambeosaurine hadrosaurid known only from a juvenile specimen. [9] | |
Thescelosaurids of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Thescelosauridae [10] | Indeterminate [10] | A right premaxillary tooth and a posterior sacral vertebral centrum. [10] | Indeterminate thescelosaurid remains. [10] | |
Remains of the following saurischians have been found in the formation: [3]
Coelurosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
cf. Richardoestesia [3] | Indeterminate [3] | A tooth. [3] | A taxon only known from teeth. [3] | |
Dromaeosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Dromaeosaurinae [3] | Indeterminate [3] | A pedal ungual and dentary teeth. [3] | Indeterminate dromaeosaurine remains. [3] | |
Saurornitholestinae [3] | Indeterminate [3] | A pedal ungual, manual unguals and teeth. [3] | Indeterminate saurornitholestine remains. [3] | |
Oviraptorosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Caenagnathidae | 3 tibia fragments, distal, proximal and medial shaft elements respectively. [11] | An oviraptorosaur. Two different morphotypes are suggested, a small one, less than a meter in length. And a big morphotype, almost reaching two meters. | ||
Ornithomimosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Mexidracon [12] | M. longimanus [3] | A partial skeleton | A ornithomimid theropod | ![]() |
Paraxenisaurus [13] | P. normalensis [13] | Caudal vertebrae, femur, peses, manual phalanxes, manual ungual, tarsals, metatarsals, metacarpals, pedal phalanx, pedal phalanges, and pedal unguals. [13] | Represents the first known deinocheirid from North America. [13] | ![]() |
"Saltillomimus" | "S. rapidus" | Partial skeleton. [14] | An informally named ornithomimosaur. [14] | ![]() |
Tyrannosaurs of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Labocania [15] | L. aguillonae [3] | A teratophonein tyrannosaurine | ![]() | |
Tyrannosauridae [3] | Indeterminate [3] | A caudal vertebra, indeterminate vertebrae, tibia, fibula, fragments of ungual phalanges, phalanges, and teeth. [3] | Indeterminate tyrannosaurid remains. [3] | |
Theropods of the Cerro del Pueblo Formation | ||||
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Genus | Species | Material | Notes | Images |
Theropoda [3] | Indeterminate [3] | A neural arch, complete and fragmented pedal and manual phalanxes, manual unguals, unspecified vertebra, complete and fragmented caudal vertebrae, chevron, proximal end of femur, and unidentified bone fragments. [3] | Indeterminate theropod remains. [3] | |
Troodontidae [3] | Indeterminate [3] | A pedal phalanx and a tooth. [3] | Indeterminate troodontid remains. [3] | |
Pterosaurs of the Cerro del Pueblo Formation | ||||
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Taxa | Presence | Description | Images | |
Ichnogenus: | Saltillo, Coahuila [16] | Specimens kept at the Dinosaur Tracks Museum, of the University of Colorado at Denver and the Secretaría de Educación Pública de Coahuila, Mexico; [16] might also represent Haenamichnus . [17] | ||
Turtles of the Cerro del Pueblo Formation | ||||||
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Genus | Species | Material | Notes | Images | ||
Mexichelys [18] | M. coahuilaensis | New genus for Euclastes coahuilaensis, sea turtle | ||||
Chedighaii [19] | C. hutchisoni | A bothremydid turtle | ||||
Yelmochelys [20] | Y. rosarioae | A stem-kinosternid turtle | ||||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Fish of the Cerro del Pueblo Formation | ||||||
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Genus | Species | Material | Notes | Images | ||
Lepisosteus | L. sp. | |||||
Amiidae | Indet. | |||||
Mammals of the Cerro del Pueblo Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
Cimolomyidae indet. | A cimolomyid multituberculate. [14] | |||||
Pediomys | P. cf. elegans | A pediomyid tribosphenidan. [14] | ||||
Taeniolabidoidae indet. | A taeniolabidoid multituberculate. [14] | |||||
Turgidodon | T. cf. russelli | An alphadontid marsupialiform. [14] | ||||
Kritosaurus is an incompletely known genus of hadrosaurid (duck-billed) dinosaur. It lived about 74.5-66 million years ago, in the Late Cretaceous of North America. The name means "separated lizard", but is often mistranslated as "noble lizard" in reference to the presumed "Roman nose".
Labocania is a genus of carnivorous theropod dinosaur of disputed affinities from the Late Cretaceous of Mexico. Initially regarded as an indeterminate theropod, later studies mentioned possible affinities with tyrannosaurids, abelisaurids, or carcharodontosaurids. More recent research based on additional fossil material found support for a position within the tyrannosaurine clade Teratophoneini. Two species have been proposed: L. anomala, likely from the La Bocana Roja Formation, and L. aguillonae from the Cerro del Pueblo Formation.
Naashoibitosaurus is a genus of hadrosaurid dinosaur that lived about 73 million years ago, in the Late Cretaceous, and was found in the Kirtland Formation of the San Juan Basin in New Mexico, United States. Only a partial skeleton has been found to date. It was first described as a specimen of Kritosaurus by Jack Horner, and has been intertwined with Kritosaurus since its description.
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Velafrons is a genus of lambeosaurine hadrosaurid dinosaur from the Late Cretaceous of Mexico. It is known from a mostly complete skull and partial skeleton of a juvenile individual, with a bony crest on the forehead. Its fossils were found in the late Campanian-age Cerro del Pueblo Formation, near Rincon Colorado, Coahuila, Mexico. The type specimen is CPC-59, and the type species is V. coahuilensis.
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Coahuilaceratops is a genus of chasmosaurine ceratopsian dinosaur that lived during the early Maastrichtian age of the Late Cretaceous epoch, about 71.5 to 70.5 million years ago in what is now northern Mexico. It contains a single species, Coahuilaceratops magnacuerna.
Scott Donald Sampson is a Canadian-American paleontologist and science communicator. Sampson is currently the Executive Director of California Academy of Sciences in San Francisco, California. He was previously Vice President of Research & Collections and Chief Curator at the Denver Museum of Nature & Science. Sampson is notable for his work on the carnivorous theropod dinosaurs Majungasaurus and Masiakasaurus and his extensive research into the Late Cretaceous Period, particularly in Madagascar. He is also known as the presenter of the PBS Kids show Dinosaur Train.
Mexichelys is an extinct monotypic genus of sea turtle which lived in Mexico during the Cretaceous. The only species is Mexichelys coahuilaensis. Mexichelys was erected in 2010 as a replacement name for Euclastes coahuilaensis, a species named in 2009.
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Latirhinus is an extinct genus of lambeosaurine hadrosaurid dinosaur from the Late Cretaceous of Mexico. The type species, Latirhinus uitstlani, was named in 2012 on the basis of a partial skeleton from the Campanian-age Cerro del Pueblo Formation. The specific name uitstlani means "southern" in the Náhuatl language of Mexico, a reference to the species' southern occurrence in the Cretaceous landmass Laramidia.
Lindsay E. Zanno is an American vertebrate paleontologist and a leading expert on theropod dinosaurs and Cretaceous paleoecosystems. She is the Head of Paleontology at the North Carolina Museum of Natural Sciences and an Associate Research Professor in the Department of Biological Sciences at North Carolina State University.
This timeline of hadrosaur research is a chronological listing of events in the history of paleontology focused on the hadrosauroids, a group of herbivorous ornithopod dinosaurs popularly known as the duck-billed dinosaurs. Scientific research on hadrosaurs began in the 1850s, when Joseph Leidy described the genera Thespesius and Trachodon based on scrappy fossils discovered in the western United States. Just two years later he published a description of the much better-preserved remains of an animal from New Jersey that he named Hadrosaurus.
Yehuecauhceratops [jɛhwɛkaoʔkɛratops] is a genus of horned centrosaurine ceratopsid dinosaur from the Late Cretaceous of Coahuila, Mexico. It contains a single species, Y. mudei, described from two partial specimens by Rivera-Sylva et al. in 2016 and formally named by Rivera-Sylva et al. in 2017. It was a small centrosaurine with a body length of 3 metres (9.8 ft), making it smaller than Agujaceratops and Coahuilaceratops, the other two ceratopsids in its environment; the three may have been ecologically segregated. A ridge bearing a single roughened projection near the bottom of the squamosal bone, which probably supported a small horn, allows Yehuecauhceratops to be distinguished from other centrosaurines. Its affinities to nasutoceratopsin centrosaurines, such as Avaceratops and Nasutoceratops, are supported by various morphological similarities to the former.
Paraxenisaurus is an extinct genus of ornithomimosaurian theropod from the Late Cretaceous Cerro del Pueblo Formation of Coahuila in Mexico. The genus contains a single species, P. normalensis, which is known from a few bones of tail, hips, hands, and feet. The specific epithet was given in honor of the Benemérita Normal School of Coahuila, a teacher training institution, where the fossils were reposited. It is a member of the family Deinocheiridae and is the only member of that clade known from Laramidia.
Coahuilasaurus is an extinct genus of kritosaurin ornithopod dinosaur from the Late Cretaceous (Campanian) Cerro del Pueblo Formation of Coahuila, Mexico. The genus contains a single species, C. lipani, known from the associated tips of the upper and lower jaw and other fragmentary skull bones. It is a large kritosaurin with an estimated body length of 8 metres (26 ft).
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