Ceratopsidae
Ceratopsidae is a family of ceratopsian dinosaurs including Triceratops, Centrosaurus, and Styracosaurus. All known species were quadrupedal herbivores from the Upper Cretaceous. All but one species are known from western North America, which formed the island continent of Laramidia during most of the Late Cretaceous. Ceratopsids are characterized by beaks, rows of shearing teeth in the back of the jaw, elaborate nasal horns, and a thin parietal-squamosal shelf that extends back and up into a frill. The group is divided into two subfamilies—Chasmosaurinae and Centrosaurinae. The chasmosaurines are generally characterized by long, triangular frills and well-developed brow horns. The centrosaurines had well-developed nasal horns or nasal bosses, shorter and more rectangular frills, and elaborate spines on the back of the frill.

Kurt McKee shankar s. EvaK Jens Lallensack · CC BY 2.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Also called
- ceratopsidPBDB
- Sits inside
- CeratopsiaPBDB
- Diet
- herbivorePBDB, for Ceratopsia
- Life habit
- ground dwellingPBDB, for Ceratopsia
- Motility
- actively mobilePBDB, for Ornithischia
- Environment
- terrestrialPBDB, for Ceratopsia
Time the record covers
At least 17 million years on record.
The record covers at least 89.8 Mya to 72.2 Mya. No occurrence read is dated outside 100.5 Mya to 66 Mya.
754 occurrences of Ceratopsidae on record, most of them in the Late Cretaceous. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
754 occurrences- Late Cretaceous100%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
57 formations
- Hell Creek Formation · Montana Group163
- Dinosaur Park Formation · Belly River Group127
- Lance Formation · Montana Group79
- Oldman Formation · Belly River Group41
- Kirtland Formation26
- Ferris Formation26
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The named rock units Ceratopsidae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 33 further formations hold fewer occurrences each and are not listed. 13 occurrences have no formation on record, which is common for older literature.
Ceratopsidae and its relatives
Late CretaceousWhere Ceratopsidae and its relatives were recorded in the Late Cretaceous.
Found in the same rock
573 taxa- Trionychidae75 sites
- Hadrosauridae74 sites
- Scapherpeton tectum71 sites
- Baenidae67 sites
- Myledaphus bipartitus67 sites
- Lepisosteus occidentalis64 sites
- Champsosaurus62 sites
- Chelydridae56 sites
- Opisthotriton kayi50 sites
- Teleostei47 sites
- Paronychodon44 sites
- Adocus42 sites
- Anura42 sites
- Borealosuchus sternbergii40 sites
- Theropoda40 sites
- Crocodylia39 sites
- Multituberculata39 sites
- Tyrannosauridae39 sites
- Brachychampsa montana38 sites
- Saurornitholestes langstoni37 sites
- Aves35 sites
- Compsemys victa35 sites
- Cyclurus fragosus32 sites
- Coriops amnicolus31 sites
The Paleobiology Database records 717 sites for Ceratopsidae, and this reads 240 of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
283 references- Vertebrate biostratigraphy of the Hell Creek Formation in southwestern North Dakota and northwestern South Dakota59
- Vertebrate faunal changes through Lancian and Puercan time in southern Wyoming25
- Fossil Vertebrate Collections24
- Late Cretaceous dinosaurs from the Denver Basin, Colorado24
- A revision of the Ceratopsia or horned dinosaurs21
- The paleogeographic and stratigraphic distribution of ceratopsids (Ornithischia) in the Upper Judith River Group of western Canada20
- Vertebrate microsite assemblages (exclusive of mammals) from the Foremost and Oldman Formations of the Judith River Group (Campanian) of southeastern Alberta: an illustrated guide19
- Diversity of Late Cretaceous dinosaurs from Mexico16
- Ceratopsian bonebeds: occurrence, origins, and significance15
- Paleontology of the Judith River Formation (Campanian) of Dinosaur National Park, Alberta, Canada: evidence from vertebrate microfossil locality15
- A centrosaurine mega-bonebed from the Upper Cretaceous of southern Alberta: implications for behavior and death events14
- The geographic and stratigraphic distribution of articulated and associated dinosaur remains14
Each of the 754 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 271 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content3
Picture of Ceratopsidae
- Source
- Wikipedia/Commons
- Credit
- Kurt McKee shankar s. EvaK Jens Lallensack
- Licence
- CC BY 2.0
- Commercial use
- the licence allows it
Structured light scan
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Ceratopsidae indet. · RSKM:RSKM P3217.561
3D model
- Source
- Sketchfab
- Licence
- CC Attribution-NonCommercial
- Commercial use
- the licence does not allow it
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itCeratopsia through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Marsh 1888