Denversaurus (meaning "Denver lizard") is a genus of panoplosaurin nodosaurid dinosaur from the late Maastrichtian of Late Cretaceous Western North America. Although at one point treated as a junior synonym of Edmontonia by some taxonomists, current research indicates that it is its own distinct nodosaurid genus.
| Denversaurus Temporal range: Late Cretaceous,
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| Skeleton cast of Denversaurus ("Tank"), Houston Museum of Natural Science | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | †Ornithischia |
| Clade: | †Thyreophora |
| Clade: | †Ankylosauria |
| Family: | †Nodosauridae |
| Subfamily: | †Nodosaurinae |
| Clade: | †Panoplosaurini |
| Genus: | †Denversaurus Bakker, 1988 |
| Type species | |
| †Denversaurus schlessmani Bakker, 1988
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Discovery and naming
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In 1922, Philip Reinheimer, a collector and technician employed by the Colorado Museum of Natural History, the predecessor of the present Denver Museum of Nature and Science, near the Twito Ranch in Corson County, South Dakota discovered the fossil of an ankylosaurian in a Maastrichtian age terrestrial horizon of the Lance Formation. In 1943, Barnum Brown referred the find to Edmontonia longiceps.[1]
In 1988, Robert Thomas Bakker decided to split the genus Edmontonia. The species Edmontonia rugosidens was made into a separate genus named Chassternbergia and the Denver fossil was named and described as a new genus and species. The type species of this genus was Denversaurus schlessmani. The generic name referred to the Denver Museum of Natural History at Denver, Colorado. The specific name honoured Lee E. Schlessman, a major benefactor of the museum and the founder of the Schlessman Family Foundation.[2]
The fossil the species is based on, holotype specimen DMNH 468, was discovered in an aforementioned layer of the late Maastrichtian-age Lance Formation of South Dakota. It consists of a skull without the lower jaws and a number of osteoderms of the body armour. It is part of the collection of the Denver Museum of Nature and Science after which the genus was named. Bakker referred a second fossil to the species, specimen AMNH 3076, a skull found by Brown and American Museum of Natural History paleontologist Roland T. Bird at the Tornillo Creek in Brewster County, Texas, in a layer of the poorly dated Upper Cretaceous Aguja Formation, possibly from the Maastrichtian too.[2]
Fossil hunters found a nodosaurid skeleton in Niobrara County, Wyoming, nicknamed "Tank", which has been identified as Denversaurus. The specimen contains the lower jaws, parts of the torso, and about a hundred osteoderms. It is part of the collection of the Rocky Mountain Dinosaur Resource Center under inventory number BHI 127327.[3]
The validity of Denversaurus was disputed in a 1990 paper on ankylosaurian systematics by Kenneth Carpenter, who noted that Bakker's diagnosis of Denversaurus was based primarily on Bakker's artistic restoration of the holotype in an uncrushed state. Since DMNH 468 was found crushed, Carpenter assigned Denversaurus to an Edmontonia sp., even though he noted its similarity to Edmontonia rugosidens.[4] A number of workers treated Denversaurus as synonymous with either E. rugosidens[5] or E. longiceps,[6] or alternatively as a valid species of Edmontonia: E. schlessmani.[7][8]
In an SVP 2015 abstract, Michael Burns revisited the systematics of latest Cretaceous nodosaurids from the Western Interior. According to Burns, Denversaurus is a valid taxon based on its phylogenetic position.[9]
Description
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In 2010, American paleontologist Gregory S. Paul estimated the length of Denversaurus at 6 metres (20 ft) and its body mass at 3 tonnes (3.3 short tons).[8]
Robert T. Bakker considered Denversaurus distinct from Edmontonia and Chassternbergia in having a skull that was wide at the rear and a more rearward position of the eye sockets.[2] The holotype skull has a length of 496 millimetres and a rear width of 346 millimetres. In the referred specimen AMNH 3076, these proportions are less extreme, measuring 395 millimetres long with a rear width of 220 millimetres. According to American paleontologist Kenneth Carpenter, the greater width of both the holotype and the referred specimen was due to crushing.[4]
In 2015, vertebrate anatomist and paleontologist Michael Burns published an abstract concluding that Denversaurus was different from Edmontonia, but similar to Panoplosaurus in having inflated, convex, cranial sculpturing with visible sulci, or troughs, between individual top skull armour elements, but is distinct from Panoplosaurus in having a relatively wider snout.[9]
Classification
editIn 1988, Bakker placed Denversaurus within Edmontoniidae, the presumed sister group of Nodosauridae within Nodosauroidea that would not have been Ankylosauria, but the last surviving Stegosauria.[2] However, these hypotheses have not been confirmed by modern cladistic analysis. Whether it presents a separate species or is identical to E. rugosidens or E. longiceps, Denversaurus material is considered nodosaurid and ankylosaurian. Paul suggested that it was the direct descendant of E. longiceps.[8] Burns recovered Denversaurus as the sister species of Panoplosaurus.[9] Denversaurus is the latest known member of Thyreophora.[2]
References
edit- ^ B. Brown and E.M. Schlaikjer, 1943, "A study of the troödont dinosaurs with the description of a new genus and four new species", Bulletin of the American Museum of Natural History 82(5): 115-150
- ^ a b c d e 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).
- ^ Carpenter K., DiCroce T., Kinneer B., Simon R., 2013, "Pelvis of Gargoyleosaurus (Dinosauria: Ankylosauria) and the Origin and Evolution of the Ankylosaur Pelvis", PLoS ONE 8(11): e79887. doi:10.1371/journal.pone.0079887
- ^ a b Carpenter, K. 1990. "Ankylosaur systematics: example using Panoplosaurus and Edmontonia (Ankylosauria: Nodosauridae)", In: Carpenter, K. & Currie, P.J. (eds) Dinosaur Systematics: Approaches and Perspectives, Cambridge University Press, Cambridge, pp. 281-298
- ^ W. P. Coombs and T. A. Deméré. 1996. A Late Cretaceous nodosaurid ankylosaur (Dinosauria: Ornithischia) from marine sediments of coastal California. Journal of Paleontology 70(2):311-326
- ^ M. K. Vickaryous, T. Maryanska, and D. B. Weishampel. 2004. Ankylosauria. In D. B. Weishampel, P. Dodson, and H. Osmolska (eds.), The Dinosauria (second edition). University of California Press, Berkeley 363-392
- ^ Hunt, A.P. and Lucas, S.G., 1992, "Stratigraphy, Paleontology and age of the Fruitland and Kirkland Formations (Upper Cretaceous), San Juan Basin, New Mexico", New Mexico Geological Society Guidebook, 43rd Field Conference, San Juan Basin, volume 4, p. 217-240
- ^ a b c Paul, G.S. (2010). The Princeton Field Guide to Dinosaurs, Princeton University Press.
- ^ a b c Burns, ME. Intraspecific Variation in Late Cretaceous Nodosaurids (Ankylosauria: Dinosauria). Journal of Vertebrate Paleontology, Program and Abstracts, 2015, 99–100.