AnimaliaacceptedfamilyAccepted
Cimolomyidae

Cimolomyidae

GBIF:159397328

ABOUT

Descriptions(4)

C. gracilis Marsh, 1889 b Meniscoessus major (Russell, 1937) M. robustus (Marsh, 1889 b) M. conquistus Cope, 1882 M. borealis Simpson, 1927 a
Sahni, Ashok (1972): The vertebrate Fauna of the Judith River formation, Montana. Bulletin of the American Museum of Natural History 147 (6): 319-416, DOI: 10.5281/zenodo.3382461, Hdl: http://hdl.handle.net/2246/1099
Cimolomys clarki, new species
Sahni, Ashok (1972): The vertebrate Fauna of the Judith River formation, Montana. Bulletin of the American Museum of Natural History 147 (6): 319-416, DOI: 10.5281/zenodo.3382461, Hdl: http://hdl.handle.net/2246/1099
The Cimolomyidae comprise medium- to large-sized multituberculates, with a tendency to increase in size in later forms. P 4 is a high, arcuate tooth, with fewer serrations than in most contemporary allotherians. The posterior two or three serrations of P 4 s in both genera are more distinct than the other serrations and may be deflected posteriorly; on the labial sides, grooves are present on or between these serrations and lead ventrally to a prominent posterolabial ledge containing one to three cuspules. P 4 differs in the two genera. It is long and low in Cimolomys, but in Meniscoessus it is short and high. The internal row of Ml is well developed, terminating at or near the second cusp from the anterior end of the medial row. The species of these genera from the Judith River Formation are more similar to each other than they are to later species.
Sahni, Ashok (1972): The vertebrate Fauna of the Judith River formation, Montana. Bulletin of the American Museum of Natural History 147 (6): 319-416, DOI: 10.5281/zenodo.3382461, Hdl: http://hdl.handle.net/2246/1099
The family was proposed by Marsh (1 889 c) but never defined. Clemens (1 963 b) preferred to place the genus in the Ptilodontidae, incertae sedis. Material from the Judith River Formation, however, indicates that the genera Cimolomys and Meniscoessus are closely related and should be included in the family Cimolomyidae. The affinity of the two genera as cimolomyids had already been anticipated by Sloan and Van Valen (1965) in their discussion of the Hell Creek multituberculates. The family as here defined contains two genera, Cimolomys and Meniscoessus, and the following six species:
Sahni, Ashok (1972): The vertebrate Fauna of the Judith River formation, Montana. Bulletin of the American Museum of Natural History 147 (6): 319-416, DOI: 10.5281/zenodo.3382461, Hdl: http://hdl.handle.net/2246/1099

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Source Information

The vertebrate Fauna of the Judith River formation, Montana

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article Sahni, Ashok (1972): The vertebrate Fauna of the Judith River formation, Montana. Bulletin of the American Museum of Natural History 147 (6): 319-416, DOI: 10.5281/zenodo.3382461, Hdl: http://hdl.handle.net/2246/1099

GEOLOGIC INVESTIGATION of the Late Cretaceous Judith River Formation in the area just north of the Judith River on the Missouri River in north-central Montana has resulted in the discovery of varied vertebrate forms. The beds are mainly freshwater continental deposits consisting of crossbedded channel sandstones, gray siltstones, and carbonaceous shales with occasional seams of lignitic coal. The stratigraphic sequence consists of the Marias River Shale overlain by the Eagle, Claggett, Judith River, and Bearpaw formations. The last four constitute the Montana Group. The Judith River Formation is Campanian in age as determined by its position between the fossiliferous marine Claggett and Bearpaw shales.

The fauna was obtained from the upper 50 feet of the formation. The bone concentration in the productive sandstone is the result of size sorting leading to underrepresentation of the larger dinosaurs. Three orders of mammals are represented, the Eutheria by a single genus, the Allotheria by five, and the Metatheria by at least three genera. Teiid and parasaniwid lizards are frequent. Only a fraction of the large number of described dinosaur genera, however, is represented in the collection by isolated teeth. Fish and amphibians form a sizable portion of the fauna.

Vertebrates from the Judith River Formation are more primitive than, but generally similar to, later Maestrichtian species. The mammals differ from their descendants in the Lance Formation at the species level. The community structure and the paleoecology of the fauna of the Judith River Formation resemble those of the Lance Formation. The greatest difference between the two communities is the greater variety of dinosaurs in the earlier formation.

Sahni A, plazi (1972). The vertebrate Fauna of the Judith River formation, Montana. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.5281/zenodo.3382461 accessed via GBIF.org on 2026-06-15.

CC0Published 12/31/1972View dataset
GBIF Usage Key
159397328
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
4831393
Taxon ID
1A7187CFFFDF176BFAAFFB4DE119580A.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026