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CretaceousherbivoreFossil completeness: good

Sauropelta edwardsorum

Pronunciation: SORE-oh-PEL-tah ed-WARD-so-rum

A heavily armored Cloverly nodosaur with rows of bony plates and enormous paired spines projecting from its shoulders.

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Sauropelta edwardsorum

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 26 July 2026

Field guide

Overview

Sauropelta edwardsorum was a large nodosaurid ankylosaur from the Early Cretaceous of Montana and Wyoming. A mosaic of bony plates protected its neck, back and tail, while two pairs of especially long spines guarded the shoulder region. Unlike later ankylosaurids, Sauropelta lacked a tail club. Several partial skeletons preserve much of its armor in place, making it one of the clearest examples of early nodosaurid defence.

Its fossils occur between approximately 115 and 108 million years ago. Values shown here are approximate and reflect the current curated seed dataset.

Form and function

Anatomy

The small, low skull ended in a broad plant-cropping beak. The neck carried half-rings of armor, and rows of rounded and keeled osteoderms covered the broad back. Large triangular spines projected sideways from the shoulders. Stout limbs supported a low, wide body, while the long tail remained flexible and lacked a terminal club.

  • Two pairs of very large shoulder spines
  • Armored neck half-rings
  • Rows of keeled and rounded osteoderms
  • Broad beak and small leaf-shaped teeth
  • Long tail without a terminal club
  • Stout, weight-bearing limbs

Evolutionary position

Scientific classification

  1. 1Dinosauriaclade
  2. 2Ornithischiaclade
  3. 3Thyreophoraclade
  4. 4Ankylosauriaclade
  5. 5Nodosauridaefamily
  6. 6Sauropeltagenus
  7. 7Sauropelta edwardsorumspecies

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 collected the holotype, AMNH 3032, from the Cloverly Formation of Montana during the early 1930s but did not formally describe it. John Ostrom combined Brown's material with discoveries from Yale expeditions and named Sauropelta edwardsi in 1970. The grammatically corrected spelling edwardsorum is now widely used and honours Nell and Tom Edwards.

Discovery credit: Barnum Brown, American Museum field crews.

Naming authors: John H. Ostrom.

Palaeoenvironment

Habitat and behaviour

Sauropelta inhabited the same Cloverly floodplains and seasonal woodlands as Tenontosaurus. It browsed among conifers, cycads, ferns and early flowering plants while large theropods such as Acrocanthosaurus occupied the ecosystem.

Low jaws and small teeth suit selective browsing on ground-level vegetation. Armor and shoulder spines provided passive protection and may also have served for display. There is no direct evidence for herd size, combat behaviour or parental care.

Worth knowing

Field notes

  • Its longest shoulder spines approached half a metre in length.
  • Unlike Ankylosaurus, it had no tail club.
  • Barnum Brown informally called the fossils Peltosaurus before Ostrom published the name Sauropelta.
  • Much of its armor was found close to its original position on the skeleton.

Fossil distribution

Fossil locations

Bighorn Basin fossil region

Montana and Wyoming, United States

Cloverly 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

The museum houses holotype AMNH 3032 and additional material collected by Barnum Brown.

Record type: originalChecked 26 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

  • Older literature commonly uses the original spelling edwardsi rather than edwardsorum.
  • The precise arrangement of isolated armor elements requires comparison among several specimens.
  • The visual role of the shoulder spines is hypothetical.
  • Colour and soft tissues in the reconstruction are interpretive.

Evidence

References and sources

  1. 01
    The Paleobiology Database

    Open source
  2. 02
    Stratigraphy and paleontology of the Cloverly Formation (Lower Cretaceous) of the Bighorn Basin area, Wyoming and Montana

    John H. Ostrom · Bulletin of the Peabody Museum of Natural History 35 · 1970

    Open source
  3. 03
    Sauropelta

    Natural History Museum, London

    Open source