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CretaceousherbivoreFossil completeness: excellent

Protoceratops andrewsi

Pronunciation: PRO-toh-SER-ah-tops an-DROO-see

A sheep- to pig-sized, four-legged ceratopsian from Mongolia’s Late Cretaceous dune fields, known from abundant skulls and skeletons, a juvenile nest and the extraordinary ‘Fighting Dinosaurs’ fossil.

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Protoceratops andrewsi

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 13 July 2026

Field guide

Overview

Protoceratops andrewsi was a small, stout neoceratopsian that lived in the Djadokhta dune fields of Late Cretaceous Mongolia. Its skull combined a deep beak, a modest nasal boss and a broad fenestrated frill, but lacked the long horns of later ceratopsids. Numerous skulls from small juveniles to large adults document dramatic growth: the snout deepened and the frill expanded disproportionately as the animal matured. The skeleton indicates mainly quadrupedal locomotion, with some capacity to rear. Exceptional fossils add rare behavioural context. Fifteen juveniles were preserved together in a bowl-shaped nest, and another individual died entangled with Velociraptor mongoliensis. Neither occurrence tells a complete life story, but together they make P. andrewsi one of the most behaviourally informative non-ceratopsid ceratopsians.

Its fossils occur between approximately 75 and 71 million years ago. Values shown here are approximate and reflect the current curated seed dataset.

Form and function

Anatomy

A narrow, down-curved rostral bone supported a keratinous beak at the front of the upper jaw, opposed by the predentary beak below. Behind it, closely packed cheek teeth formed slicing surfaces for vegetation. The skull broadened toward a parietal-squamosal frill pierced by two large openings that reduced its weight. Adults developed a low nasal boss rather than a long horn and prominent jugal projections at the cheeks. The neck and trunk were robust, the forelimbs weight-bearing and the hind limbs longer and more powerful. Mature shoulder, elbow and forearm anatomy is consistent with habitual quadrupedalism, while some retained features may have allowed occasional rearing on the hind legs.

  • Deep skull with a narrow, down-curved rostral beak core
  • Broad parietal-squamosal frill pierced by paired openings
  • Low nasal boss rather than a long facial horn
  • Prominent jugal projections on the cheeks
  • Closely packed cheek teeth forming plant-slicing wear surfaces
  • Robust shoulder and forelimb anatomy adapted for weight bearing
  • Longer hind limbs retaining some capacity for rearing
  • Frill size and shape changing strongly through growth

Evolutionary position

Scientific classification

  1. 1Dinosauriaclade
  2. 2Ornithischiaclade
  3. 3Neornithischiaclade
  4. 4Marginocephaliaclade
  5. 5Ceratopsiaclade
  6. 6Protoceratopsidaefamily
  7. 7Protoceratopsgenus
  8. 8Protoceratops andrewsispecies

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

Open interactive position

Scale

Size comparison

Scientific record

Discovery and naming

James Blaine Shackelford found the partial juvenile skull AMNH 6251 during the American Museum’s 1922 Central Asiatic Expedition in Mongolia. Walter W. Granger and William King Gregory named Protoceratops andrewsi in 1923, honouring expedition leader Roy Chapman Andrews. The following expeditions recovered many additional skulls and skeletons at the Flaming Cliffs, producing an unusually broad growth series. Eggs discovered there in 1923 were assigned to Protoceratops largely because it was the common dinosaur nearby. That attribution collapsed in 1994 when an embryo inside the same egg type proved to be an oviraptorid, a correction now incorporated into the museum’s own account.

Discovery credit: James Blaine Shackelford.

Naming authors: Walter W. Granger, William King Gregory.

Palaeoenvironment

Habitat and behaviour

Protoceratops lived among the wind-built dunes and sandy interdune areas recorded by the Djadokhta Formation. The climate was arid to semi-arid, but episodic moisture and patches of vegetation supported a diverse small-bodied fauna. Velociraptor, Oviraptor, Saurornithoides and the armored Pinacosaurus occupied the same broad formation, alongside lizards, mammals and other reptiles. Burial in collapsing or rapidly shifting sand helps explain the three-dimensional skeletons, nests and close associations for which the unit is famous, although no single death mechanism explains every specimen.

The beak and cheek-tooth wear establish herbivory, while the deep jaws supplied leverage for cropping and slicing plants. Adult limb anatomy indicates mainly four-legged travel; rearing to feed, display or defend is mechanically possible but is not directly recorded. The ‘Fighting Dinosaurs’ specimen MPC-D 100/25 preserves P. andrewsi locked against Velociraptor mongoliensis, providing exceptional evidence of a direct physical encounter even though the precise sequence of attack, defence and burial remains debated. A separate nest with fifteen similarly sized juveniles shows that young animals remained together after hatching. It is compatible with extended nest use, but without an adult it does not by itself prove parental care. Strong positive growth of the frill is consistent with a visual social or sexual signal, not proof of one exclusive function.

Worth knowing

Field notes

  • The holotype AMNH 6251 is a juvenile skull, so the much larger adult head became known only from later expeditions.
  • The 1971 ‘Fighting Dinosaurs’ fossil preserves a Velociraptor foot at the Protoceratops throat while the ceratopsian’s beak grips the predator’s forelimb.
  • A bowl-shaped nest from Tugriken Shireh contains fifteen articulated juveniles rather than a clutch of eggs.
  • The famous Flaming Cliffs eggs were called Protoceratops eggs for decades, but an oviraptorid embryo overturned that identification in 1994.
  • Modern morphometric work finds strong growth-related frill change but no clean split into male and female skull shapes.

Fossil distribution

Fossil locations

Flaming Cliffs (Bayn Dzak)

Gobi Desert, Mongolia

Djadokhta Formation

approximate site marker

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

Open interactive map

Fossil specimen record

Museums and research collections

American Museum of Natural History

verified

New York, United States

The museum currently lists Protoceratops andrewsi among its dinosaur displays and shows original skeletons and a growth series from the Mongolian expeditions. Its current egg explainer also corrects the historical Protoceratops assignment: the nearby classic egg type is oviraptorid, not evidence for this species.

Record type: partial originalChecked 13 July 2026Institution website

American Museum of Natural History

verified

New York, United States

Repository of the original expedition series, including holotype skull AMNH 6251 and articulated skeletons such as AMNH 6416. The museum archive verifies catalogue numbers and historic displays; individual specimens may rotate between research and exhibition use.

Record type: originalChecked 13 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

  • Protoceratops andrewsi is exceptionally well represented, but the Djadokhta specimens still span growth stages, deformation and individual variation that complicate comparisons.
  • Published body masses vary widely because estimates use different skeletons and scaling methods; the broad range shown here is more honest than one exact figure.
  • The frill’s positive allometry supports a signalling role but does not identify the signal’s audience, the animal’s sex or other simultaneous functions.
  • A 29-skull analysis did not strongly support the traditional male-versus-female division based on frill and nasal prominence.
  • Fifteen juveniles together in a nest demonstrate prolonged juvenile association, not the presence or behaviour of a caring parent.
  • The classic Flaming Cliffs egg type belongs to oviraptorids; it must not be used as direct evidence for Protoceratops eggs or brooding.
  • Filament-like tail bristles in the gallery reconstruction are speculative for Protoceratops and are not preserved with this species.

Evidence

References and sources

  1. 01
    The Paleobiology Database

    Open source
  2. 02
    The Fighting Dinosaurs: The position of their bodies before and after death

    Rinchen Barsbold · Paleontological Journal · 2016

    Open source
  3. 03
    Fighting Dinosaurs

    American Museum of Natural History

    Open source
  4. 04
    A Theropod Dinosaur Embryo and the Affinities of the Flaming Cliffs Dinosaur Eggs

    Mark A. Norell, James M. Clark, Demberelyin Dashzeveg and 6 coauthors · Science · 1994

    Open source
  5. 05
    Dinosaur Eggs

    American Museum of Natural History

    Open source
  6. 06
    Protoceratops andrewsi, a pre-ceratopsian dinosaur from Mongolia

    Walter W. Granger, William King Gregory · American Museum Novitates 72 · 1923

    Open source
  7. 07
    A nest of Protoceratops andrewsi (Dinosauria, Ornithischia)

    David E. Fastovsky, David B. Weishampel, Mahito Watabe and 3 coauthors · Journal of Paleontology · 2011

    Open source
  8. 08
    Males Resemble Females: Re-Evaluating Sexual Dimorphism in Protoceratops andrewsi (Neoceratopsia, Protoceratopsidae)

    Leonardo Maiorino, Andrew A. Farke, Tassos Kotsakis, Paolo Piras · PLOS ONE · 2015

    Open source
  9. 09
    Three-dimensional geometric morphometric analysis of the skull of Protoceratops andrewsi supports a socio-sexual signalling role for the ceratopsian frill

    Andrew Knapp, Robert J. Knell, David W. E. Hone · Proceedings of the Royal Society B · 2021

    Open source
  10. 10
    Appendicular skeleton of Protoceratops andrewsi (Dinosauria, Ornithischia): comparative morphology, ontogenetic changes, and the implications for non-ceratopsid ceratopsian locomotion

    Justyna Słowiak, Victor S. Tereshchenko, Łucja Fostowicz-Frelik · PeerJ · 2019

    Open source
  11. 11
    Fossil skeleton of Protoceratops andrewsi, AMNH 6416

    American Museum of Natural History Digital Collections

    Open source