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Cerro del Pueblo Formation | |
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Stratigraphic range: Campanian ~ | |
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 | Mexico |
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 | ||||
---|---|---|---|---|
Genus | Species | Material | Notes | Images |
Coahuilasaurus [4] | C. lipani [5] | 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 [6] | K. navajovius [6] | Predentary, symphyseal processes, rostral portion of dental battery of dentaries, rostral region of premaxillae, and fragments of maxilla. [6] | A kritosaurin hadrosaurid, originally referred to K. navajovius, [6] 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 [7] | L. uitstlani [7] | Caudal vertebrae, scapulae, humeri, ulnae, coracoid, metacarpals, manual ungual, ilia, ischia, femora, tibiae, fibula, and astragalus. [7] | Holotype specimen is chimeric as it consists of multiple individuals. Some material from the holotype specimen is assigned to Lambeosaurinae indet. and Saurolophinae indet.. [8] | |
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 [9] | T. galorum [9] | An almost complete skull, mandible, partial ilium, partial ischium, a femur, scapula, coracoid, sacral vertebrae, caudal vertebrae, and chevrons. [9] | A parasaurolophin hadrosaur, closely related to Charonosaurus and Blasisaurus . [9] | |
Velafrons [10] | V. coahuilensis [10] | 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. [10] | A lambeosaurine hadrosaurid known only from a juvenile specimen. [10] | |
Thescelosaurids of the Cerro del Pueblo Formation | ||||
---|---|---|---|---|
Genus | Species | Material | Notes | Images |
Thescelosauridae [11] | Indeterminate [11] | A right premaxillary tooth and a posterior sacral vertebral centrum. [11] | Indeterminate thescelosaurid remains. [11] | |
Remains of the following saurischians have been found in the formation: [3]
Theropods of the Cerro del Pueblo Formation | ||||
---|---|---|---|---|
Genus | Species | Material | Notes | Images |
Caenagnathidae | 3 tibia fragments, distal, proximal and medial shaft elements respectively. [12] | An oviraptorosaur. Two different morphotypes are suggested, a small one, less than a meter in length. And a big morphotype, almost reaching two meters. | ||
Dromaeosaurinae [3] | Indeterminate [3] | A pedal ungual and dentary teeth. [3] | Indeterminate dromaeosaurine remains. [3] | |
Labocania [13] | L. aguillonae [14] | A teratophonein tyrannosaurine | ||
Ornithomimidae [3] | Indeterminate [3] | Dorsal vertebrae, caudal vertebrae, femora, fibulae, tibiae, metatarsals, ungual manuals, ungual pedals, phalanxes, manual phalanxes, manual phalanges, pedal phalanges, pedal phalanxes, pubes and tarsals. [3] | Indeterminate ornithomimid remains. [3] | |
Paraxenisaurus [15] | P. normalensis [15] | Caudal vertebrae, femur, peses, manual phalanxes, manual ungual, tarsals, metatarsals, metacarpals, pedal phalanx, pedal phalanges, and pedal unguals. [15] | Represents the first known deinocheirid from North America. [15] | |
cf. Richardoestesia [3] | Indeterminate [3] | A tooth. [3] | A taxon only known from teeth. [3] | |
Saurornitholestinae [3] | Indeterminate [3] | A pedal ungual, manual unguals and teeth. [3] | Indeterminate saurornitholestine remains. [3] | |
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] | |
Tyrannosauridae [3] | Indeterminate [3] | A caudal vertebra, indeterminate vertebrae, tibia, fibula, fragments of ungual phalanges, phalanges, and teeth. [3] | Indeterminate tyrannosaurid 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] | ||
Turtles of the Cerro del Pueblo Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Material | Notes | Images | ||
Mexichelys [17] | M. coahuilaensis | New genus for Euclastes coahuilaensis, sea turtle | ||||
Chedighaii [18] | C. hutchisoni | A bothremydid 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 | ||
Multituberculata | Indet. | |||||
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.
Anasazisaurus is a genus of saurolophine hadrosaurid ("duckbill") ornithopod dinosaur that lived about 74 million years ago, in the Late Cretaceous Period. It was found in the Farmington Member of the Kirtland Formation, in the San Juan Basin of New Mexico, United States. Only a partial skull 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. It is known for its short nasal crest, which stuck out above and between its eyes for a short distance.
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.
The Judith River Formation is a fossil-bearing geologic formation in Montana, and is part of the Judith River Group. It dates to the Late Cretaceous, between 79 and 75.3 million years ago, corresponding to the "Judithian" land vertebrate age. It was laid down during the same time period as portions of the Two Medicine Formation of Montana and the Oldman Formation of Alberta. It is an historically important formation, explored by early American paleontologists such as Edward Drinker Cope, who named several dinosaurs from scrappy remains found here on his 1876 expedition. Modern work has found nearly complete skeletons of the hadrosaurid Brachylophosaurus.
The Horseshoe Canyon Formation is a stratigraphic unit of the Western Canada Sedimentary Basin in southwestern Alberta. It takes its name from Horseshoe Canyon, an area of badlands near Drumheller.
Lambeosaurinae is an extinct group of crested hadrosaurid dinosaurs.
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.
The Aguja Formation is a geological formation in North America, exposed in Texas, United States and Chihuahua and Coahuila in Mexico, whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. Fossil palms have also been unearthed here.
The El Gallo Formation is a geological formation in Mexico whose strata date back to the Late Cretaceous, from the Santonian to the Maastrichtian. Dinosaur remains are among the fossils that have been recovered from the formation.
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.
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.
Magnapaulia is a genus of herbivorous lambeosaurine hadrosaurid dinosaurs known from the Latest Cretaceous Baja California, of northwestern Mexico. It contains a single species, Magnapaulia laticaudus. Magnapaulia was first described in 1981 as a possible species of Lambeosaurus by William J. Morris, and was given its own genus in 2012 by Prieto-Márquez and colleagues.
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.
Yehuecauhceratops 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.
Leptorhynchos is an extinct genus of caenagnathid theropod from the Late Cretaceous of what is now the US state of Texas, although it has been suggested to also exist in Alberta and South Dakota. The type species is L. gaddisi, and it is currently the only widely accepted valid species. The generic name of Leptorhynchos comes from the Greek "leptos" meaning "small" and "rhynchos" meaning "beak". The specific epithet is in honor of the Gaddis family, who owned the land on which the holotype was discovered.
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.
Tlatolophus is a genus of hadrosaurid dinosaur belonging to the tribe Parasaurolophini. The only species is the type species, Tlatolophus galorum.
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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