Styracosaurus albertensis Lambe, 1913
A dramatic centrosaurine ceratopsian of Late Cretaceous Canada bearing a single long nasal horn and six long frill spikes.

Scientific reconstruction of Styracosaurus (Styracosaurus albertensis Lambe, 1913) in its native Geological period: Cretaceous Period.
Image Credit: AI-generated scientific paleoart reconstruction synthesized from species-specific osteological profiles and peer-reviewed descriptions. (AI-Generated / Open Educational Media (DinoOrigin Spec))
Phylogenetic classification of Styracosaurus albertensis Lambe, 1913 based on peer-reviewed cladistic analyses of diagnostic skeletal synapomorphies.
| Taxonomic Rank | Taxon / Clade | Diagnostic Context |
|---|---|---|
| Kingdom | Animalia | Monophyletic prehistoric clade |
| Phylum | Chordata | Monophyletic prehistoric clade |
| Clade | Dinosauria | Monophyletic prehistoric clade |
| Order | Ornithischia (Bird-Hipped Dinosaurs) | Characterized by a pelvis with a backwards-pointing pubis parallel to the ischium. |
| Infraorder | Ceratopsia | Ornithischian dinosaurs characterized by beaks, rostral bones, facial horns, and elaborate neck frills. |
| Genus | Styracosaurus | Monophyletic prehistoric clade |
| Species | Styracosaurus albertensis Lambe, 1913 | Specific authority designation |
Styracosaurus albertensis was a spectacularly adorned ceratopsian from the Dinosaur Park Formation of Alberta. Its distinguishing feature was its elaborate cranial armature: a single straight nasal horn measuring up to 60 centimeters in length and 4 to 6 long spikes protruding radially from the upper margin of the parietosquamosal neck frill.
Bonebed deposits containing multiple individuals demonstrate that Styracosaurus lived in cohesive herds that traveled across river valleys, where flash floods occasionally preserved dozens of individuals simultaneously.
Stout quadrupedal ceratopsian with a massive nasal horn, small brow hornlets, and an expansive frill crowned with long, outward-radiating spikes.
Anatomical dimensions relative to an average adult human (1.8 m / 6 ft tall)
Tough, fibrous plants such as palms, cycads, and ferns clipped by a sharp keratinous beak and shredded by dental batteries.
Prominently spiked centrosaurine ceratopsian possessing an impressive frill adorned with long horns and spikes. In the Dinosaur Park Formation, Styracosaurus lived sympatrically with closely related horned dinosaurs like Centrosaurus and crested hadrosaurs like Corythosaurus.
Lowland river delta forests and marshes bordering the Western Interior Seaway.
Holotype CMN 344 consists of a nearly complete skull; multiple partial skeletons recovered from mass mortality bonebeds.
Discovered by Charles M. Sternberg; described by Lawrence Lambe in 1913.
The longest and final period of the Mesozoic Era, characterized by the rise of flowering plants, ceratopsians, hadrosaurs, tyrannosaurids, and concluding with the Chicxulub asteroid impact.
During the Mesozoic Era, continental drift progressively reconfigured land bridges, atmospheric currents, and regional precipitation regimes. Fossils of Styracosaurus evidence its adaptation to the paleoenvironments of North America.
Home to the fossil-rich Morrison Formation of the Late Jurassic and the Hell Creek and Dinosaur Park Formations of the Late Cretaceous.
The anatomical architecture of Styracosaurus serves as a crucial benchmark in vertebrate paleontology, illustrating key adaptive radiations within Ceratopsia.
Scientifically verified answers based on peer-reviewed paleontological evidence.
Styracosaurus lived during the Cretaceous Period Period, approximately 75.5–75 Ma (million years ago). This places it within the Mesozoic Era.
Paleontological estimates place Styracosaurus at a length of 5–5.8 m (16.4–19.0 ft), a hip/standing height of 1.8–2.2 m (5.9–7.2 ft), and a body mass of 2.5–3.2 metric tons (5,512–7,055 lbs).
Classified as a herbivore, Styracosaurus specialized in consuming Tough, fibrous plants such as palms, cycads, and ferns clipped by a sharp keratinous beak and shredded by dental batteries..
Fossil specimens of Styracosaurus have been recovered from Red Deer River, Alberta, Canada, with notable historic specimens documented in 1913. Discovered by Charles M. Sternberg; described by Lawrence Lambe in 1913.
Authoritative citations establishing the factual taxonomy, biometrics, and anatomy of Styracosaurus.
Lambe, L. M. (1913). A new genus and species of Ceratopsia from the Belly River Formation of Alberta. The Ottawa Naturalist, 27(9), 109-116.
Curated & Verified: 2026-09-24Deposited in Mesozoic sedimentary strata preserving skeletal remains, teeth, or trace trackways.
Styracosaurus provides critical insights into the evolutionary radiation of Ceratopsia. Holotypes and fossil evidence indicate: Holotype CMN 344 consists of a nearly complete skull; multiple partial skeletons recovered from mass mortality bonebeds.
CeratopsiaCentrosaurus apertus Lambe, 1904
A prominent centrosaurine ceratopsid from Alberta featuring a forward-curved nasal horn and hooked frill spikes.
CeratopsiaDiabloceratops eatoni Kirkland & DeBlieux, 2010
The 'devil-horned face', a basal centrosaurine featuring long curved brow horns and majestic frill spikes.
CeratopsiaPachyrhinosaurus canadensis Sternberg, 1950
The 'thick-nosed lizard', an Arctic-adapted ceratopsid that replaced horns with massive bony bosses.