Chirostenotes

Chirostenotes

Chordata

Chirostenotes
Temporal range: Late Cretaceous, 76.5–75 Ma
Illustration of the type specimen
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Superfamily: Caenagnathoidea
Family: Oviraptoridae
Subfamily: Elmisaurinae
Genus: Chirostenotes
Gilmore, 1924
Type species
Chirostenotes pergracilis
Gilmore, 1924
Species
  • C. pergracilis Gilmore, 1924
  • C. elegans (Parks, 1933) [originally Ornithomimus]
Synonyms
  • Macrophalangia Sternberg, 1932

Chirostenotes (pronounced /ˌkaɪrɵˈstɛnɵtiːz/ ky-ro-sten-ə-teez, named from Greek 'narrow-handed') is a genus of oviraptorosaurian dinosaur from the late Cretaceous (about 75 million years ago) of Alberta, Canada. The type species is Chirostenotes pergracilis. Some researchers recognize a second species, C. elegans.

Contents

Description

Chirostenotes was characterized by a toothless beak, long arms ending in slender relatively straight claws, long powerful legs with slender toes. In life, the animal was about 2 metres (6.6 ft) long. Chirostenotes was probably an omnivore or herbivore, although the beak is not as heavily constructed as in the Asian Oviraptoridae. It likely ate small reptiles and mammals, as well as plants, eggs and insects.

In 2005 Phil Senter and J. Michael Parrish published a study on the hand function of Chirostenotes and found that its elongated second finger with its unusually straight claw may have been an adaptation to crevice probing. They suggested that Chirostenotes may have fed on soft-bodied prey that could be impaled by the second claw, such as grubs, as well as unarmored amphibians, reptiles, and mammals.[1] However, if Chirostenotes possessed the large primary feathers on its second finger that have been found in other oviraptorosaurs such as Caudipteryx, it would not have been able to engage in such behavior.[2]

Taxonomic history

Chirostenotes has a confusing history of discovery and naming. The first fossils of Chirostenotes, a pair of hands, were in 1914 found by George Fryer Sternberg near Little Sandhill Creek in the Campanian Dinosaur Park Formation of Canada, which has yielded the most dinosaurs of any Canadian formation. The specimens were studied by Lawrence Morris Lambe who deceased however, before being able to formally name them. In 1924, Charles Whitney Gilmore adopted the name he found in Lambe's notes and described and named the type species Chirostenotes pergracilis. The generic name is derived from Greek cheir, "hand", and stenotes, "narrowness". The specific name means "throughout", per~, "gracile", gracilis, in Latin. The holotype is NMC 2367, the pair of hands[3]

Chirostenotes was but the first name assigned. Feet were then found, specimen CMN 8538, and in 1932 Charles Mortram Sternberg gave them the name Macrophalangia canadensis, meaning 'large toes from Canada'.[4] Sternberg correctly recognized them as part of a meat-eating dinosaur but thought they belonged to an ornithomimid. In 1936, its lower jaws, specimen CMN 8776, were found by Raymond Sternberg near Steveville and in 1940 he gave them the name Caenagnathus collinsi. The generic name means 'recent jaw' from Greek kainos, "new", and gnathos, "jaw"; the specific name honours William Henry Collins. The toothless jaws were first thought to be those of a bird.[5]

Slowly the precise relationship between the finds became clear. In 1960 Alexander Wetmore concluded that Caenagnathus was not a bird but a ornithomimid.[6] In 1969 Edwin Colbert and Dale Russell suggested that Chirostenotes and Macrophalangia were one and the same animal.[7] In 1976 Halszka Osmólska described Caenagnathus as an oviraptosaurian.[8] In 1981 the announcement of Elmisaurus, an Asian form of which both hand and feet had been preserved, showed the soundness of Colbert and Russell's conjecture.

In 1988, a specimen from storage since 1923 was discovered and studied by Philip Currie and Dale Russell. This fossil helped link the other discoveries into a single dinosaur. Since the first name applied to any of these remains was Chirostenotes, this were the only name that was recognized as valid.[9]

Currie and Russell also addressed the complicating issue of a possible second form being present in the material. In 1933 William Arthur Parks had named Ornithomimus elegans, based on specimen ROM 781, another foot from Alberta.[10] In 1971, Joël Cracraft, still under the assumption Caenagnathus was a bird, had named a second species of Caenagnathus: Caenagnathus sternbergi, based on specimen CMN 2690, a small lower jaw. In 1988 Russell and Currie concluded that these fossils might present a more gracile morph of Chirostenotes pergracilis. In 1989 however, Currie thought that they represented a separate smaller species, and named this as a second species of the closely related Elmisaurus: Elmisaurus elegans.[11] In 1997, this was renamed to Chirostenotes elegans by Hans-Dieter Sues.[12] This remains contentious.

Reconstructed head and neck of an undescribed Hell Creek Formation species

Several larger skeletons from the early Maastrichtian Horseshoe Canyon Formation of Alberta and Hell Creek Formation of Montana and South Dakota have been referred to Chirostenotes in the past, though more recent studies concluded that they represent several new species.[13] The Horseshore Canyon formation specimen was renamed Epichirostenotes in 2011, while the Hell Creek Formation specimens are still being studied.[13] The latter specimens are more complete and of a considerable size: in 2010 Gregory S. Paul estimated the length of the South Dakotan Hell Creek specimens at 4 metres (13 ft), the weight at 350 kilograms (770 lb).[14]

In 2007 a cladistic study by Philip Senter cast doubt on the idea that all of the large Dinosaur Park Formation fossils belonged to the same creature: coding the original hand and jaw specimens separately showed that while the Caenagnathus holotype remained in the more basal position in the Caenagnathidae commonly assigned to it, the Chirostenotes pergracilis holotype was placed as an advanced oviraptorosaurian and an oviraptorid.[15][16]

Another fossil connected to Chirostenotes is specimen CMN 8776, a set of jaws with strange teeth, which were originally referred by Gilmore to Chirostenotes pergracilis. Now that it is known that Chirostenotes was a toothless oviraptorosaur, the jaws have been renamed Richardoestesia and are from an otherwise unknown dinosaur, likely a dromaeosaurid.[17]

Synonyms

  • Macrophalangia canadensis Sternberg, 1932
  • Caenagnathus collinsi Sternberg, 1940
  • Ornithomimus elegans Parks, 1933
  • Elmisaurus elegans (Parks, 1933) Currie, 1989
  • Caenagnathus sternbergi Cracraft, 1971
  • Chirostenotes sternbergi (Cracraft, 1971) Eberth & Currie & Brinkman & Ryan & Braman & Gardner & Lam & Spivak & Neuman, 2001

Paleopathology

In 2001, Bruce Rothschild and others published a study examining evidence for stress fractures and tendon avulsions in theropod dinosaurs and the implications for their behavior. They found that only one of the 17 Chirostenotes foot bones checked for stress fractures actually had them.[18]

References

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  1. ^ Senter, P.; Parrish, J.M. (2005) Functional analysis of the hands of the theropod dinosaur Chirostenotes pergracilis: evidence for an unusual paleoecological role. PaleoBios 25: 9–19
  2. ^ Naish, D. (2007). Feathers and Filaments of Dinosaurs, Part II Tetrapod Zoology, April 23, 2011.
  3. ^ Gilmore, C.W. (1924). A new coelurid dinosaur from the Belly River Cretaceous of Alberta. Canada Department of Mines Geological Survey Bulletin (Geological Series) 38(43):1-12.
  4. ^ Sternberg, C.M. (1932). Two new theropod dinosaurs from the Belly River Formation of Alberta. Canadian Field-Naturalist 46(5):99-105.
  5. ^ Sternberg, R.M. (1940). A toothless bird from the Cretaceous of Alberta. Journal of Paleontology 14(1):81-85.
  6. ^ Wetmore, A. 1960. A classification for the birds of the world. Smithsonian Miscellaneous Collections 139 (11): 1–37
  7. ^ E.H. Colbert and D.A. Russell, 1969, "The small Cretaceous dinosaur Dromaeosaurus", Amer. Mus. Novit., No. 2380, pp. 1-49
  8. ^ Osmólska, H. 1976. "New light on the skull anatomy and systematic position of Oviraptor". Nature 262: 683–684
  9. ^ Currie, P.J., and Russell, D.A. (1988). Osteology and relationships of Chirostenotes pergracilis (Saurischia, Theropoda) from the Judith River (Oldman) Formation of Alberta, Canada. Canadian Journal of Earth Sciences 25:972-986.
  10. ^ Parks, W.A. (1933). New species of dinosaurs and turtles from the Upper Cretaceous formations of Alberta. University of Toronto Studies, Geological Series 34:1-33.
  11. ^ Currie, P.J. (1989). The first records of Elmisaurus (Saurischia, Theropoda) from North America. Canadian Journal of Earth Sciences 26(6):1319-1324.
  12. ^ Sues, H.D., 1997, "On Chirostenotes, a Late Cretaceous oviraptorosaur (Dinosauria: Theropoda) from Western North America", Journal of Vertebrate Paleontology 17(4): 698-716
  13. ^ a b Robert M. Sullivan, Steven E. Jasinski and Mark P.A. Van Tomme (2011). "A new caenagnathid Ojoraptorsaurus boerei, n. gen., n. sp. (Dinosauria, Oviraptorosauria), from the Upper Ojo Alamo Formation (Naashoibito Member), San Juan Basin, New Mexico". Fossil Record 3. New Mexico Museum of Natural History and Science Bulletin 53: 418–428. http://www.robertmsullivanphd.com/uploads/169._Sullivan_et_al.__Ojoraptorsaurus__COLOR.pdf. 
  14. ^ Paul, G.S., 2010, The Princeton Field Guide to Dinosaurs, Princeton University Press p. 151
  15. ^ Senter, P. 2007. "A new look at the phylogeny of Coelurosauria (Dinosauria: Theropoda)". Journal of Systematic Palaeontology 5: 429-463
  16. ^ Holtz, Thomas R. Jr. (2010) Dinosaurs: The Most Complete, Up-to-Date Encyclopedia for Dinosaur Lovers of All Ages, Winter 2010 Appendix.
  17. ^ Currie, P.J., Rigby, Jr., J.K., and Sloan, R.E. (1990). Theropod teeth from the Judith River Formation of southern Alberta, Canada. In: Carpenter, K., and Currie, P.J. (eds.). Dinosaur Systematics: Perspectives and Approaches. Cambridge University Press:Cambridge, 107-125. ISBN 0-521-36672-0.
  18. ^ Rothschild, B., Tanke, D. H., and Ford, T. L., 2001, Theropod stress fractures and tendon avulsions as a clue to activity: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, p. 331-336.

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