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Temporal range: Late Cretaceous, 74.2 Ma
Achelousaurus holotype.jpg
Type specimen MOR 485, Museum of the Rockies
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Order: Ornithischia
Family: Ceratopsidae
Tribe: Pachyrhinosaurini
Subtribe: Pachyrostra
Genus: Achelousaurus
Sampson, 1995
Type species
Achelousaurus horneri
Sampson, 1995

Achelousaurus (pronunciation: /əˌklˈsɔːrəs/, less commonly: /ˌækˌləˈsɔːrəs/;[1] "Achelous's lizard") is a genus of centrosaurine ceratopsid dinosaurs from the Late Cretaceous Period of what is now North America, dated to 74.2 million years ago.[2]


Life restoration

They were quadrupedal herbivores with parrot-like beaks, rough bosses (raised bony areas) on their snouts and one pair behind their eyes, and a pair of horns on the end of their long bony frills. With body lengths of up to six meters (20 feet) and a weight of three tonnes,[3] Achelousaurus were medium-sized ceratopsians.

History of discovery[edit]

The genus and the one named species (A. horneri) were both named by paleontologist Scott Sampson in 1995. The specific name honors Jack Horner, an influential American paleontologist famous for his Montana dinosaur discoveries, who in 1987 headed the team that excavated the holotype skull of Achelousaurus, MOR 485. The generic name Achelousaurus is a complex reference to Greek mythology. Achelous, an important Greek river deity, had one of his horns torn off by Hercules, in a mythological fight with the legendary hero. All three known skulls of Achelousaurus have rough bosses in the same places where other ceratopsians have horns, giving them the appearance of having had the horns ripped off. Achelous was also celebrated for his shapeshifting ability, just as Achelousaurus appear to combine features of other ceratopsian dinosaurs.

Achelousaurus horneri are known from the U.S. state of Montana, in the Two Medicine Formation, which preserves sediments dated from the Campanian stage of the Late Cretaceous Period, between 83 and 74 million years ago. Achelousaurus specimens are found in the highest levels of the formation, probably closer to the end of that timeframe, 74 mya.[4] Contemporary dinosaur species included Prosaurolophus blackfeetensis, Scolosaurus cutleri, Hypacrosaurus stebingeri, Einiosaurus procurvicornis, and tyrannosaurids of uncertain classification.

Scientists have so far recovered three skulls and some postcranial material from the Two Medicine, all housed at the Museum of the Rockies in Bozeman, Montana. The skull of a full-grown Achelousaurus (including the frill horns) is over 5 feet (1.6 meters) long.


Early reports suggested that Achelousaurus represented a transitional form, "Type C", between ceratopsians with modified horns like Einiosaurus, "Type B" (with which A. horneri shares two horns on the end of the frill), and the derived, hornless Pachyrhinosaurus (Horner et al., 1992). While they may or may not form a direct line of descent, all three of these genera are at least closely related, and are often united in the tribe Pachyrhinosaurini, inside the subfamily Centrosaurinae and the family Ceratopsidae (Sampson, 1995; Dodson et al., 2004).

Parietal bones
Side view of holotype skull

The cladogram below shows the phylogenetic position of Achelousaurus following Ryan et al. (2016):[5]


Diabloceratops eatoni


Avaceratops lammersi (ANSP 15800)

MOR 692

CMN 8804

Nasutoceratops titusi

Malta new taxon

Xenoceratops foremostensis

Albertaceratops nesmoi

Sinoceratops zhuchengensis

Wendiceratops pinhornensis


Rubeosaurus ovatus

Styracosaurus albertensis

Spinops sternbergorum

Centrosaurus apertus

Coronosaurus brinkmani


Einiosaurus procurvicornis

Achelousaurus horneri


Pachyrhinosaurus canadensis

Pachyrhinosaurus lakustai

Pachyrhinosaurus perotorum

See also[edit]


  1. ^ "Since the scientific name Achelousaurus was formed by arbitrarily combining Achelous (/ˌækˈləs/) and saurus instead of using the stem-form Achelo-, the "u" needs to be pronounced."[1]
  2. ^ Andrew T. McDonald & John R. Horner, (2010). "New Material of "Styracosaurus" ovatus from the Two Medicine Formation of Montana". Pages 156–168 in: Michael J. Ryan, Brenda J. Chinnery-Allgeier, and David A. Eberth (eds), New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium, Indiana University Press, Bloomington and Indianapolis, IN.
  3. ^ Paul, G.S., 2010, The Princeton Field Guide to Dinosaurs, Princeton University Press p. 263
  4. ^ Michael J. Ryan, David A. Eberth, Donald B. Brinkman, Philip J. Currie, and Darren H. Tanke. (2010). "A New Pachyrhinosaurus-Like Ceratopsid from the Upper Dinosaur Park Formation (Late Campanian) of Southern Alberta, Canada." New Perspectives on Horned Dinosaurs.
  5. ^ Ryan, M.J.; Holmes, R.; Mallon, J.; Loewen, M.; Evans, D.C. (2017). "A basal ceratopsid (Centrosaurinae: Nasutoceratopsini) from the Oldman Formation (Campanian) of Alberta, Canada". Canadian Journal of Earth Sciences. 54. doi:10.1139/cjes-2016-0110. 
  • Dodson, P., Forster, C.A., & Sampson, S.D. 2004. Ceratopsidae. In Weishampel, D.B., Dodson, P. & Osmolska, H. (Eds.) The Dinosauria (2nd Edition). Berkeley: University of California Press. Pp. 494–513.
  • Horner, J.R., Varricchio, D.J. & Goodwin, M.B. 1992. Marine transgressions and the evolution of Cretaceous dinosaurs. Nature 358: 59-61.
  • Sampson, S.D. 1995. Two new horned dinosaurs from the Upper Cretaceous Two Medicine Formation of Montana; with a phylogenetic analysis of the Centrosaurinae (Ornithischia: Ceratopsidae). Journal of Vertebrate Paleontology 15(4): 743-760.

External links[edit]