Edmontonia
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An artist's depiction of Edmontonia
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Edmontonia was an armoured dinosaur, a part of the nodosaur family from the Late Cretaceous Period. It is named after the Edmonton Formation (now the Horseshoe Canyon Formation), the unit of rock it was found in. Edmontonia fossils have never been found in Edmonton, Alberta.
[edit] Discovery and species
The type species of Edmontonia, E. longiceps was discovered in 1924 by George Paterson. It wasn't named until 1928 by C. M. Sternberg. E. rugosidens, formally named by Gilmore in 1930, is reported from the Aguja formation in Texas. Edmontonia species include:
- E. longiceps (type);
- E. rugosidens, which is sometimes given its own genus, Chassternbergia, first coined as a subgenus by Dr. Robert T. Bakker in 1988 (Edmontonia (Chassternbergia) rugosidens) and based on differences in skull proportion from E. longiceps.[1][2] This subgenus or genus is not generally accepted;[3][4][Etymology of Chassternbergia: In honor of Charles Mortram Sternberg (1885-1981), a Canadian paleontologist who, in 1928, named and described Edmontonia longiceps, a nodosaurid ankylosaur which Robert Bakker would later use as the basis for proposing the new nodosaurid family Edmontoniidae, which would include a new subgenus, Chassternbergia as well as the new genus Denversaurus schlessmani. Sternberg, honored for his earlier work on Edmontonia longiceps.[5]]
- And E. australis,[2] which is known from cervical scutes only, and usually is considered to be a dubious name.[3]
Usually included in this genus is Denversaurus schlessmani ("Schlessman's Denver lizard"). This taxon was erected by Bakker in 1988 for a skull from the Late Maastrichtian Upper Cretaceous Lance Formation of South Dakota,[1] but considered by later workers to belong to Edmontonia rugosidens.[4] The type specimen of Denversaurus is in the collections of the Denver Museum of Natural History (now the Denver Museum of Nature and Science), Denver, Colorado (for which the genus was named).
[edit] Paleobiology
Edmontonia was bulky and tank-like at roughly 7m (23 ft) long and 2m (6 ft) high. It had bony plates on its back and head, many sharp spikes along its back and tail and four large spikes jutting out from its shoulders on each side, two of which were split into subspines. These large spikes were probably used in contests of strength. To protect itself from predators, it probably would have crouched down on the ground to minimize the possibility of attack to its defenseless underbelly.
[edit] References
- ^ a b Bakker, R.T. (1988). Review of the Late Cretaceous nodosauroid Dinosauria: Denversaurus schlessmani, a new armor-plated dinosaur from the Latest Cretaceous of South Dakota, the last survivor of the nodosaurians, with comments on Stegosaur-Nodosaur relationships. Hunteria 1(3):1-23.(1988).
- ^ a b Ford, T.L. (2000). A review of ankylosaur osteoderms from New Mexico and a preliminary review of ankylosaur armor. In: Lucas, S.G., and Heckert, A.B. (eds.). Dinosaurs of New Mexico. New Mexico Museum of Natural History and Science Bulletin 17:157-176.
- ^ a b Carpenter K (2001). "Phylogenetic analysis of the Ankylosauria", in Carpenter, Kenneth(ed): The Armored Dinosaurs. Indiana University Press, 455–484. ISBN 0-253-33964-2.
- ^ a b Vickaryous, M.K., Maryańska, T., and Weishampel, D.B., (2004). "Ankylosauria", in Weishampel, D. B., Dodson, P., and Osmólska, H. (eds.): The Dinosauria (Second Edition). University of California Press, 363–392. ISBN 0-520-24209-2.
- ^ Chassternbergia etymology, courtesy of www.dinosaurnames.net