Polyodontosaurus

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Polyodontosaurus
Temporal range: Campanian, 75.5  Ma
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Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Family: Troodontidae
Genus: Polyodontosaurus
Gilmore, 1932
Species:
P. grandis
Binomial name
Polyodontosaurus grandis
Gilmore, 1932
Synonyms

Polyodontosaurus (meaning "many-toothed lizard") is a potentially dubious genus of troodontid dinosaur named in 1932 by Charles W. Gilmore for a left dentary from the Dinosaur Park Formation. [1] It had been considered a synonym of Stenonychosaurus or Troodon for a significant time, before being declared a nomen dubium . The only known species is the type, P. grandis.

Contents

History of discovery

The holotype and only known specimen of Polyodontosaurus was collected in 1928 by Charles Mortram Sternberg, and includes only a left dentary, lacking any teeth. Sternberg presented the dentary to Charles Gilmore, who identified it as a lizard. Gilmore thus named the binomial Polyodontosaurus grandis for the new taxon in 1932. [1] Sternberg revisited the material in 1951 and determined that it represented a carnivorous dinosaur based on the general morphology of the bone, as well as the anatomy of the Meckelian groove, multiple nutrient foramina, and separation of teeth into multiple sockets. Sternberg compared this dentary to one referred to Troodon by Russel in 1948, and decided that they belonged to the same family, and potentially the same genus. While similar, there were a few differences, that might be shown to relate to age or variation within the genus. Sternberg, therefore, referred Polyodontosaurus to the family Troodontidae, until further material could be found. [2] The name Polyodontosaurus has been misspelled as "Polydontosaurus" by some authors. [3]

Polyodontosaurus, represented by the holotype CMN 8540, was found in the Steveville area in the Dinosaur Park Formation. It was found about 37 m (121 ft) below the highest layer of the formation, and comes from the MAZ (Megaherbivore assemblage zone)-2 portion of the fauna, which existed after MAZ-1. This exact stratigraphic location cannot be verified. MAZ-2 spans from 75.9 to 75.3 million years ago, CMN 8540 is from slightly above (younger) than the middle of the formation. [3]

In 1969 Dale Russell described a new specimen of Stenonychosaurus , a troodontid closely related to Saurornithoides . This specimen, CMN 12340, was from the Oldman Formation of Alberta, which lies directly above the Dinosaur Park Formation. [4] This specimen was later named Latenivenatrix and comes from the MAZ-2 level of the formation. [3] Because of the similarities between Polyodontosaurus, Stenonychosaurus, and more complete Saurornithoides, Russell concluded that Polyodontosaurus was a junior synonym of Stenonychosaurus, and that they both might be synonyms of the tooth-taxon Troodon, although the material of Troodon is very incomplete. [4]

Classification

After being initially named as a lizard, Polydontosaurus was reclassified as a troodontid, a classification which stands today. [2] [3] Since 1969 Polyodontosaurus has been considered a synonym of Stenonychosaurus, and later its senior synonym Troodon. [4] [3] Polyodontosaurus is potentially a synonym of the taxon Latenivenatrix, named in 2017, but they may come from separate regions of the formation. Van der Reest & Currie in 2017 determined that due to the lack of sufficient material in the holotype, and that the dentaries of troodontids to not bear unique, autapomorphic features, Polyodontosaurus was a nomen dubium , and could not be considered senior synonym of Latenivenatrix. [3]

Below is the phylogenetic analysis of van der Reest & Currie (2017). Polyodontosaurus has been considered a synonym of the "Two Medicine troodontid" and Latenivenatrix previously. [3]

Troodontidae

Sinovenator

Anchiornis

Mei

Talos

Byronosaurus

MPC-D 100/44

Sinornithoides

Troodontinae

Urbacodon

Gobivenator

Latenivenatrix

Philovenator

Linhevenator

Two medicine troodontid

Saurornithoides

Zanabazar

Paleoecology

Megafaunal dinosaurs of the Dinosaur Park Formation Dinosaur park formation fauna.png
Megafaunal dinosaurs of the Dinosaur Park Formation

The single specimen of Polyodontosaurus was found in the central level of the Dinosaur Park Formation, and was a member of a diverse and well-documented fauna of prehistoric animals that included such well-known dinosaurs as the horned Centrosaurus , Styracosaurus , and Chasmosaurus , fellow duckbills Prosaurolophus , Gryposaurus , Corythosaurus, and Parasaurolophus , tyrannosaurid Gorgosaurus , and armored Edmontonia and Euoplocephalus . [3] [5] The Dinosaur Park Formation is interpreted as a low-relief setting of rivers and floodplains that became more swampy and influenced by marine conditions over time as the Western Interior Seaway transgressed westward. [6] The climate was warmer than present-day Alberta, without frost, but with wetter and drier seasons. Conifers were apparently the dominant canopy plants, with an understory of ferns, tree ferns, and angiosperms. [7]

Related Research Articles

<i>Troodon</i> Extinct genus of dinosaurs

Troodon is a former wastebasket taxon and a potentially dubious genus of relatively small, bird-like theropod dinosaurs definitively known from the Campanian age of the Late Cretaceous period. It includes at least one species, Troodon formosus, known from Montana. Discovered in October 1855, T. formosus was among the first dinosaurs found in North America, although it was thought to be a lizard until 1877. Several well-known troodontid specimens from the Dinosaur Park Formation in Alberta were once believed to be members of this genus. However, recent analyses in 2017 have found this genus to be undiagnostic and referred some of these specimens to the genus Stenonychosaurus some to the genus Latenivenatrix, and some to the genus Pectinodon. The genus name is Ancient Greek for "wounding tooth", referring to the teeth, which were different from those of most other theropods known at the time of their discovery. The teeth bear prominent, apically oriented serrations. These "wounding" serrations, however, are morphometrically more similar to those of herbivorous reptiles, and suggest a possibly omnivorous diet.

<i>Stenonychosaurus</i> Theropod dinosaur

Stenonychosaurus is a genus of troodontid dinosaur from the Late Cretaceous Dinosaur Park Formation of Alberta, Canada, as well as possibly the Two Medicine Formation. The type and only species, S. inequalis, was named by Charles Mortram Sternberg in 1932, based on a foot, fragments of a hand, and some caudal vertebrae from the Late Cretaceous of Alberta. S. inequalis was reassigned in 1987 by Phil Currie to the genus Troodon, which was reverted by the recognition of Stenonychosaurus as a separate genus from the possibly dubious Troodon in 2017 by Evans et al. and also later in the same year by Van der Reest and Currie.

<i>Chasmosaurus</i> Extinct genus of dinosaurs

Chasmosaurus is a genus of ceratopsid dinosaur from the Late Cretaceous Period in North America. Its given name means 'opening lizard', referring to the large openings (fenestrae) in its frill. With a length of 4.3–4.8 metres (14.1–15.7 ft) and a weight of 1.5–2 tonnes —or anywhere from 2,200 to nearly 5,000 lbs., give or take—Chasmosaurus was of a slightly smaller to ‘average’ size, especially when compared to larger ceratopsians. The Chasmosaurs were similar, in overall build and weight, to a white rhinoceros or an Indian rhinoceros; just like rhinos, and all other ceratopsians, they were purely herbivorous, needing to consume around 54 kilograms, or 120 lbs., of plant matter each day.

<i>Saurornitholestes</i> Extinct genus of dinosaurs

Saurornitholestes is a genus of carnivorous dromaeosaurid theropod dinosaur from the late Cretaceous of Canada (Alberta) and the United States.

<i>Ornithomimus</i> Ornithomimid dinosaur genus from the Late Cretaceous Period

Ornithomimus is a genus of ornithomimid theropod dinosaurs from the Campanian and Maastrichtian ages of Late Cretaceous Western North America. Ornithomimus was a swift, bipedal dinosaur which fossil evidence indicates was covered in feathers and equipped with a small toothless beak that may indicate an omnivorous diet. It is usually classified into two species: the type species, Ornithomimus velox, and a referred species, Ornithomimus edmontonicus. O. velox was named in 1890 by Othniel Charles Marsh on the basis of a foot and partial hand from the Denver Formation of Colorado. Another seventeen species have been named since then, though almost all of them have been subsequently assigned to new genera or shown to be not directly related to Ornithomimus velox. The best material of species still considered part of the genus has been found in Alberta, representing the species O. edmontonicus, known from several skeletons from the Horseshoe Canyon Formation. Additional species and specimens from other formations are sometimes classified as Ornithomimus, such as Ornithomimus samueli from the earlier Dinosaur Park Formation.

<i>Saurornithoides</i> Extinct genus of dinosaurs

Saurornithoides is a genus of troodontid maniraptoran dinosaur, which lived during the Late Cretaceous period. These creatures were predators, which could run fast on their hind legs and had excellent sight and hearing. The name is derived from the Greek stems saur~ (lizard), ornith~ (bird) and eides (form), referring to its bird-like skull.

<i>Stegoceras</i> Genus of reptiles (fossil)

Stegoceras is a genus of pachycephalosaurid (dome-headed) dinosaur that lived in what is now North America during the Late Cretaceous period, about 77.5 to 74 million years ago (mya). The first specimens from Alberta, Canada, were described in 1902, and the type species Stegoceras validum was based on these remains. The generic name means "horn roof", and the specific name means "strong". Several other species have been placed in the genus over the years, but these have since been moved to other genera or deemed junior synonyms. Currently only S. validum and S. novomexicanum, named in 2011 from fossils found in New Mexico, remain. The validity of the latter species has also been debated.

<span class="mw-page-title-main">Philip J. Currie</span> Canadian paleontologist and curator

Philip John Currie is a Canadian palaeontologist and museum curator who helped found the Royal Tyrrell Museum of Palaeontology in Drumheller, Alberta and is now a professor at the University of Alberta in Edmonton. In the 1980s, he became the director of the Canada-China Dinosaur Project, the first cooperative palaeontological partnering between China and the West since the Central Asiatic Expeditions in the 1920s, and helped describe some of the first feathered dinosaurs. He is one of the primary editors of the influential Encyclopedia of Dinosaurs, and his areas of expertise include theropods, the origin of birds, and dinosaurian migration patterns and herding behavior. He was one of the models for palaeontologist Alan Grant in the film Jurassic Park.

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<span class="mw-page-title-main">Dinosaur Park Formation</span> Uppermost member of the Belly River Group geologic unit in Alberta, Canada

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<i>Zanabazar junior</i> Extinct species of dinosaur

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<i>Latenivenatrix</i> Extinct genus of dinosaurs

Latenivenatrix, meaning "hiding huntress", is a genus of large troodontid known from a single species, L. mcmasterae. Along with the contemporary Stenonychosaurus, it is known from non-tooth fossils that were formerly assigned to the now potentially dubious genus Troodon. Although described as separate, it has been considered a junior synonym of Stenonychosaurus.

<i>Citipes</i> Genus of reptiles (fossil)

Citipes is an extinct genus of caenagnathid theropod from the Late Cretaceous Dinosaur Park Formation in Alberta, Canada. The genus contains only one species, the type species, C. elegans. The generic name of Citipes is Latin for "fleet-footed", and the specific epithet "elegans" is Latin for "elegant". The type specimen of Citipes has a convoluted taxonomic history, and has been previously assigned to the genera Ornithomimus, Macrophalangia, Elmisaurus, Chirostenotes, and Leptorhynchos before being given its own genus in 2020.

References

  1. 1 2 Gilmore, C. W. (1932). A new fossil lizard from the Belly River Formation of Alberta. Transactions of the Royal Society of Canada, section 4, series 3 16:117-119
  2. 1 2 Sternberg, C.M. (1951). "The lizard Chamops from the Wapiti Formation of Northern Alberta: Polyodontosaurus grandis is not a lizard". Annual Report of the National Museum of Canada Bulletin. 123: 256–258.
  3. 1 2 3 4 5 6 7 8 van der Reest, A.J.; Currie, P.J. (2017). "Troodontids (Theropoda) from the Dinosaur Park Formation, Alberta, with a description of a unique new taxon: implications for deinonychosaur diversity in North America". Canadian Journal of Earth Sciences. 54 (9): 919–935. Bibcode:2017CaJES..54..919V. doi:10.1139/cjes-2017-0031. hdl: 1807/78296 .
  4. 1 2 3 Russell, D.A. (1969). "A new specimen of Stenonychosaurus from the Oldman Formation (Cretaceous) of Alberta". Canadian Journal of Earth Sciences. 6 (4): 595–612. Bibcode:1969CaJES...6..595R. doi:10.1139/e69-059.
  5. Weishampel, D.B.; Barrett, P.M.; Coria, R.A.; Le Loeuff, J.; Xu, X.; Zhao, X.; Sahni, A.; Gomani, E.M.P.; Noto, C.R. (2004). "Dinosaur Distribution". In Weishampel, D.B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria (Second ed.) . University of California Press. pp.  517–606. ISBN   978-0-520-24209-8.
  6. Eberth, D.A. (2005). "The geology". In Currie, P.J.; Koppelhus, E.B. (eds.). Dinosaur Provincial Park: A Spectacular Ancient Ecosystem Revealed. Indiana University Press. pp.  54–82. ISBN   978-0-253-34595-0.
  7. Braman, D.R.; Koppelhus, E.B. (2005). "Campanian palynomorphs". In Currie, P.J.; Koppelhus, E.B. (eds.). Dinosaur Provincial Park: A Spectacular Ancient Ecosystem Revealed. Indiana University Press. pp.  54–82. ISBN   978-0-253-34595-0.