AnimaliaacceptedfamilyAccepted
Stagodontidae

Stagodontidae

Marsh, 1889

GBIF:159397346

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ABOUT

Descriptions(1)

The family Stagodontidae was proposed by Marsh (1889 c, p. 178) for the inclusion of Stagodon nitor, the genotypic species, and S. tumidus. The type specimen of S. nitor, a worn premolar, however, was later shown by Clemens (1966, p. 55) to belong to Didelphodon Marsh (1889 b). In accordance with the rules established by the International Code of Zoological Nomenclature [Art. 23 (d) and 40], Clemens (1966) retained the family Stagodontidae in preference to the other family group names, Thlaeodontinae Cope (1892), Didelphodontinae Simpson (1927 b), and Thlaeodontinae Hay (1930). The family Stagodontidae as redefined by Clemens (1966, p. 55) consists of " Large, late Cretaceous, North American marsupials in which the trigonids are anteroposteriorly shortened and paraconid and protoconid are of subequal height, and higher than the metaconid. Epitympanic sinus is large and of complex structure. Alisphenoid lacks an entoglenoid process. Bullae are well developed, apparently formed of both alisphenoid and petrosal elements. " Boreodon and Didelphodon are included in the family Stagodontidae in the present paper, but Eodelphis is excluded.
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
159397346
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
4831511
Taxon ID
1A7187CFFFAE171BFB0DF95BE0245829.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026