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VAGACERATOPS

a plant-eating chasmosaurine ceratopsian dinosaur from the Late Cretaceous of North America.
Vagaceratops
Pronunciation: VAH-guh-SEH-ruh-tops
Meaning: Wandering Horn Face
Author/s: Sampson et al. (2010)
Synonyms: Chasmosaurus irvinensis
First Discovery: Alberta, Canada
Discovery Chart Position: #718

Vagaceratops irvinensis

Vagaceratops differs from almost all of its horn-faced relatives by not having any horns on its face. Well, not very impressive ones, anyway. It has a small stump on its snout and two nubbins of bone on its brow where horns would normally be. But its short and wide skull frill with two windows (parietal fenestrae) does sport ten forwards and downwards curving "hornlets" (epoccipitals) in the style of, but more modest than those seen in, Kosmoceratops to whom it is closely related. Unlike Kosmoceratops, however, its current name wasn't its original name.

Vagaceratops was initially identified as the common as muck Chasmosaurus belli in 1958, so lay ignored for many years. Heck, preparation didn't begin until 1980, and it was done in instalments until completely free of fossil-obscuring matrix in 2003, by which point it had already been sporting a shiny new name—Chasmosaurus irvinensis—for two years, courtesy of Robert Holmes. Holmes returned in 2007 to restudy what turned out to be one of the most complete and articulated ceratopsians known, and one which had, unusually, perished in an upright position with both right limbs tucked neatly beneath its torso. This was good news, as it could answer an age-old question of whether ceratopsian dinosaurs held their front legs upright like an elephant's or bent outwards at the knees like a crocodile's. Or, at least, that was the hope. The conclusion, however, was that ceratopsian forelimbs were neither one nor the other but somewhere in between and have no comparison amongst extant critters.

As well as a lack of horns, Chasmosaurus irvinensis had a wider snout, a more modest frill, and a broader chest than any known specimen of Chasmosaurus, so Sampson et al. renamed it Vagaceratops in 2010. Unusual pathologies of its vertebrae and hands suggest Vagaceratops was very old and had perhaps been taken quietly by Father Time as it slept or was unable to move. It seems even ceratopsian pensioners could succumb to arthritis.
(The wandering Horn Face from Irvine)Etymology
Vagaceratops is derived from the Latin "vagus" (wanderer) and the Greek "keras" (horn) and "-ops" (face), in reference to its presence in Alberta (northern Laramidia) during the Late Campanian while its closest relative, Kosmoceratops, was living in Utah (southern Laramidia) during the same period.
The species epithet, irvinensis, is derived from "Irvine" (for the town of Irvine: population of 350), close to where the skeleton was found, and the Latin "ensis" (from).
ZooBank registry: urn:lsid:zoobank.org:act:0A2138B8-E59C-4D24-A221-B59529C4A402.
Discovery
The remains of Vagaceratops were discovered in the Dinosaur Park Formation (Belly River Group), Southwest of Irvine, Alberta, Canada, by Mr. Luke Lindoe and collected by a team led by Wann Langston in 1958. Preparation was initiated in the late 1980s by Drs. Wann Langston and Dale Russell to address the ongoing debate surrounding forelimb posture in ceratopsians.
The holotype (NMC 41357) is a partial skull.
Referred material includes TMP 87.45.1 (a partial skull found 4.8 km NW of Iddesleigh) and TMP 98.102.8 (a partial skull found near the village of Onefour).
Another skull (TMP 2011.053.0046, from Manyberries) was assigned to Vagaceratops in 2018.
Estimations
Timeline:
Era: Mesozoic
Epoch: Late Cretaceous
Stage: Campanian
Age range: 84-71 mya
Stats:
Est. max. length: 7 meters
Est. max. hip height: 2 meters
Est. max. weight: 3.5 tons
Diet: Herbivore
References
• Holmes RB, Forster CA, Ryan MJ, and Shepherd KM (2001) "A new species of Chasmosaurus from the Dinosaur Park Formation of southern Alberta". Canadian Journal of Earth Science, 38(10): 1423-1438. DOI: 10.1139/cjes-38-10-1423.
• Thompson S and Holmes R (2007) "Forelimb stance and step cycle in Chasmosaurus irvinenesis (Dinosauria: Neoceratopsia)". Palaeontologia Electronica, 10(1): 1-17.
• Rega E, Holmes RB and Tirabaso A (2010) "Habitual locomotor behaviour inferred from manual pathology in two Late Cretaceous chasmosaurine ceratopsid dinosaurs, Chamsosaurus irvinensis (CMN 41357) and Chasmosaurus belli (ROM 843)" in Ryan, Chinnery-Allgeier and Eberth (eds.) "New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium".
• Sampson SD, Loewen MA, Farke AA, Roberts EM, Forster CA, et al. (2010) "New Horned Dinosaurs from Utah Provide Evidence for Intracontinental Dinosaur Endemism". [image credit] PLoS One, 5(9): e12292. DOI: 10.1371/journal.pone.0012292.
• Holmes RB (2014) "The postcranial skeleton of Vagaceratops irvinensis (Dinosauria, Ceratopsidae)". Vertebrate Anatomy Morphology Palaeontology, 1: 1-21.
• Longrich NR (2014) "The horned dinosaurs Pentaceratops and Kosmosaurus from the upper Campanian of Alberta and implications for dinosaur biogeography". Cretaceous Research, 51: 292-308.
• Campbell JA, Ryan MJ, Schröder-Adams CJ, Evans DC and Holmes RB (2018) "New insights into chasmosaurine (Dinosauria: Ceratopsidae) skulls from the Upper Cretaceous (Campanian) of Alberta, and an update on the distribution of accessory frill fenestrae in Chasmosaurinae". PeerJ, 6: e5194. DOI: 10.7717/peerj.5194.
• Campbell JA, Ryan MJ, Schröder-Adams CJ, Evans DC and Holmes RB (2018) "Temporal range extension and evolution of the chasmosaurine ceratopsid ‘Vagaceratopsirvinensis (Dinosauria: Ornithischia) in the Upper Cretaceous (Campanian) Dinosaur Park Formation of Alberta". Vertebrate Anatomy Morphology Palaeontology, 7: 83-100. DOI: 10.18435/vamp29356.
• Fowler DW and Freedman Fowler EA (2020) "Transitional evolutionary forms in chasmosaurine ceratopsid dinosaurs: evidence from the Campanian of New Mexico". PeerJ, 8: e9251. DOI: 10.7717/peerj.9251.
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To cite this page:
Atkinson, L. "VAGACERATOPS :: from DinoChecker's dinosaur archive".
›. Web access: 07th Mar 2026.
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