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CretaceousherbivoreFossil completeness: excellent

Corythosaurus casuarius

Pronunciation: koh-RITH-oh-SORE-us cass-you-AIR-ee-us

A large Canadian duck-billed dinosaur whose hollow, helmet-shaped crest enclosed long looping nasal passages and whose holotype preserves skin impressions.

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Corythosaurus casuarius

The page URL and title are included automatically. Optional contact details are used only to discuss this report. Do not submit private information or precise sensitive fossil-site coordinates.

Last updated 16 July 2026

Field guide

Overview

Corythosaurus casuarius is a lambeosaurine hadrosaur from Alberta's Dinosaur Park Formation. Its tall semicircular crest contains paired nasal passages that loop through the crest before entering the airway, making it both a visual structure and a plausible acoustic resonator. Numerous skulls and skeletons reveal how the crest changed as animals grew. The celebrated holotype is an articulated skeleton with skin impressions and calcified tendons, providing unusually direct evidence for body outline as well as bone anatomy.

Its fossils occur between approximately 76.6 and 75.5 million years ago. Values shown here are approximate and reflect the current curated seed dataset.

Form and function

Anatomy

AMNH 5240 preserves an articulated skeleton, skin impressions and a meshwork of calcified tendons that stiffened the back and tail. The hollow crest is formed chiefly by the nasal and premaxillary bones and houses elongated airways. Hundreds of tightly packed teeth formed dental batteries that replaced worn teeth continuously. Robust forelimbs and hoof-like finger bones supported quadrupedal walking, while longer hind limbs also permitted bipedal movement, especially during faster travel.

  • Tall semicircular hollow crest containing looping nasal passages
  • Dental batteries with continuously replaced grinding teeth
  • Skin impressions preserved with the holotype
  • Calcified tendons stiffening the back and tail
  • Forelimbs suited to walking and longer hind limbs capable of bipedal movement

Evolutionary position

Scientific classification

  1. 1Dinosauriaclade
  2. 2Ornithischiaclade
  3. 3Neornithischiaclade
  4. 4Ornithopodaclade
  5. 5Iguanodontiaclade
  6. 6Hadrosauridaefamily
  7. 7Lambeosaurinaesubfamily
  8. 8Corythosaurusgenus
  9. 9Corythosaurus casuariusspecies

This simplified classification path shows one placement from Dinosauria to this species. Each step is clickable, and other analyses may support alternative relationships.

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Scale

Size comparison

Scientific record

Discovery and naming

Barnum Brown and his American Museum field team collected the holotype beside Alberta's Red Deer River in 1912. Brown named Corythosaurus casuarius in 1914. Corythosaurus combines Greek korythos, helmet, with sauros, lizard; casuarius compares the crest with that of a cassowary. The original skeleton remains a prominent specimen in the American Museum of Natural History's Hall of Ornithischian Dinosaurs in New York.

Discovery credit: Barnum Brown, American Museum of Natural History field team.

Naming authors: Barnum Brown.

Palaeoenvironment

Habitat and behaviour

The Dinosaur Park Formation records river channels, coastal-plain floodplains, ponds and forested lowlands near the western shore of the Western Interior Seaway. Conifers, flowering plants, ferns and horsetails supplied diverse browse. Other hadrosaurs, horned dinosaurs, armoured dinosaurs and tyrannosaurids occur in the formation, but its fossil record spans many habitats and hundreds of thousands of years.

Dental batteries and a broad beak identify Corythosaurus as a plant eater able to crop and grind vegetation. The crest's internal passages could alter vocal resonance, and its conspicuous external shape likely also carried visual information. Models support acoustic potential but do not reveal a specific call. Differences among crest shapes once attributed to sex are now known to be strongly affected by growth and species identity.

Worth knowing

Field notes

  • The holotype still preserves patches of the animal's skin outline.
  • Its nasal passages travelled through the crest before reaching the throat.
  • The American Museum displays the original 1912 skeleton on Floor 4.
  • Young individuals had much smaller crests that expanded dramatically during growth.

Fossil distribution

Fossil locations

Dinosaur Provincial Park region

Alberta, Canada

Dinosaur Park Formation

regional marker

Markers are deliberately approximate. They identify published fossil areas without exposing sensitive excavation coordinates.

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Fossil specimen record

Museums and research collections

American Museum of Natural History

verified

New York, United States

Original articulated skeleton with skin impressions and calcified tendons, on public display in the Hall of Ornithischian Dinosaurs on Floor 4.

Record type: originalChecked 16 July 2026Institution website

A research repository is not necessarily a public exhibit. Loan and display status can change, so check with the institution before visiting.

Scientific uncertainty

  • Length and mass vary among individuals and reconstruction methods; ten metres represents the upper end of common estimates.
  • The crest was acoustically capable of resonance, but its exact calls and social meanings cannot be recovered.
  • The displayed specimen count is a conservative rounded summary of articulated skulls and skeletons, not every isolated element.
  • Some historic species assigned to Corythosaurus have been synonymized or moved as growth-related variation became clearer.
  • Artwork colour is speculative even though skin impressions constrain parts of the body outline.

Evidence

References and sources

  1. 01
    Corythosaurus casuarius, a new crested dinosaur from the Belly River Cretaceous

    Barnum Brown · Bulletin of the American Museum of Natural History 33 · 1914

    Open source
  2. 02
    Corythosaurus: Duck Billed Dinosaur Skeleton

    American Museum of Natural History

    Open source