Chamops
Chamops is an extinct genus of polyglyphanodontian lizard from the Late Cretaceous-Early Eocene of North America. Fossils have been found in the Hell Creek Formation, Judith River Formation and Polecat Bench Formation of Montana, the Milk River Formation of Alberta, Canada and possibly also the Laramie Formation of Colorado. It is known from only one species, C. segnis. Unlike other polyglyphanodonts, Chamops had a more blunt snout. Chamops belonged to the Chamopsiid family of polyglyphanodontian lizards that lived in the Northern Hemisphere during the Late Cretaceous, although there are some possible Chamopsiid genera from South America and the Kem Kem Bone Beds in Morocco. It was originally thought Chamops and kin are related to whiptails, although it is now thought they are more closely related to iguanas.

Othniel Charles Marsh (1831-1889) · Public Domain · via Wikidata/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- Sits inside
- ChamopsiidaePBDB
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Amniota
Time the record covers
At least 32 million years on record.
The record covers at least 89.8 Mya to 57.5 Mya. No occurrence read is dated outside 93.9 Mya to 56 Mya.
33 occurrences of Chamops 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
33 occurrencesThese 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
11 formations
- Lance Formation11
- Hell Creek Formation · Montana Group6
- Kaiparowits Formation3
- Wahweap Formation2
- Frenchman Formation2
- Scollard Formation2
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The named rock units Chamops has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Chamops and its relatives
Late CretaceousWhere Chamops and its relatives were recorded in the Late Cretaceous.
Found in the same rock
426 taxa- Cimolodon nitidus16 sites
- Meniscoessus robustus14 sites
- Odaxosaurus piger14 sites
- Leptochamops denticulatus13 sites
- Lonchidion selachos13 sites
- Mesodma thompsoni13 sites
- Albanerpetontidae12 sites
- Pediomys elegans12 sites
- Scapherpeton tectum12 sites
- Champsosaurus11 sites
- Didelphodon vorax11 sites
- Habrosaurus dilatus11 sites
- Mesodma formosa11 sites
- Opisthotriton kayi11 sites
- Paronychodon11 sites
- Theropoda11 sites
- Anura10 sites
- Brachychampsa montana10 sites
- Cimolomys gracilis10 sites
- Gypsonictops hypoconus10 sites
- Lepisosteus occidentalis10 sites
- Mesodma hensleighi10 sites
- Myledaphus bipartitus10 sites
- Protolambda hatcheri10 sites
The Paleobiology Database records 32 sites for Chamops, and this reads all 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
16 references- Taxonomy and evolution of Late Cretaceous lizards (Reptilia: Squamata) from western Canada5
- Fossil Vertebrate Collections4
- Fossil vertebrates from the Late Cretaceous Lance Formation, eastern Wyoming4
- Teiid-like scincomorphan lizards from the Late Cretaceous (Campanian) of southern Utah3
- Fossil lizards of North America3
- Vertebrate paleoecology from microsites, Talley Mountain, Upper Aguja Formation (Late Cretaceous), Big Bend National Park, Texas, USA2
- Non-dinosaurian lower vertebrates across the Cretaceous-Tertiary boundary in northeastern Montana2
- The Lower Vertebrates of the Hell Creek Formation, Harding County, South Dakota2
- Lizards and snakes from the Cenomanian through Campanian of southern Utah: filling the gap in the fossil record of Squamata from the Late Cretaceous of the Western Interior of North America1
- Taxonomic composition of the Alamo Wash local fauna from the Upper Cretaceous Ojo Alamo Formation (Naashoibito Member), San Juan Basin, New Mexico1
- A teiid lizard in the early Tertiary of North America1
- Vertebrate paleontology of the Upper Cretaceous rocks of the Markagunt Plateau, southwestern Utah1
Each of the 33 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. 4 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 content1

Picture of Chamops
- Source
- Wikidata/Commons
- Credit
- Othniel Charles Marsh (1831-1889)
- Licence
- Public Domain
- Commercial use
- the licence allows it
No 3D scan of Chamops was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Source
- Wikipedia, “Chamops”
- 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 itChamopsiidae through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Marsh 1892