AnimaliaNot EvaluatedacceptedspeciesAccepted
Pediomys clemensi

Pediomys clemensi

Sahni, 1972

GBIF:159397360

0year

ABOUT

Descriptions(6)

DISTRIBUTION: Judith River Formation, Montana.
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
DESCRIPTION: Two labial fragments of upper molars, AMNH 77373 and 77374, are similar to each other. Specimen AMNH 77373, however, has conules (fig. 13 P), whereas the other, AMNH 77374, lacks conules and is slightly larger. The stylar shelf in the specimens is not bilobate and the stylar shelf is weakly developed. Cusp A is better developed than in the other contemporary metatherian genera, and a crest connects it to the paraconule. Cusp B is small and posterolabial to the paracone. The stylar shelf narrows labial to the paracone, and the external rim of the paracone extends to the shelf. Cusp C is posterior to cusp B and slightly larger. The stylar shelf widens posteriorly just lingual to the prominent stylar cusp D, which is the largest stylar cusp. The metastyle is weakly developed and linked to the metacone by a high ridge. The paracone is situated more labial to the metacone and is about the same height. There are five lower molars that can be referred to Pediomys by use of the criterion developed by Clemens (1966), which is the position of the crista obliqua on the posterior wall of the trigonid. The crista obliqua in pediomyid molars intersects the trigonid wall at the protoconid, a position labial to the usual position in other Cretaceous marsupials. These pediomyid lower molars are small, ranging in length from 1.8 to 2.6 mm. The paraconid is a slender, conical, anteriorly directed cusp in AMNH 77377 (fig. 13 S, T). It is only slightly smaller than the metaconid and well separated from it. The protoconid is anterior and taller than the metaconid, and has a small anterobasal cingulum. The talonid is wide, and the hypoconid is a large, high cusp, which is well separated from the twinned hypoconulid and the broken entoconid. The hypoconulid is a small pointed cusp, directed posteriorly and linked to the entoconid by a short ridge. A broad cingulum is present on the posterolabial side of the crown. AMNH 77376 (fig. 13 Q, R) is a larger lower molar than AMNH 77377.
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
Figure 13 P-T
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
DIAGNOSIS: A small Campanian pediomyid most closely similar to P. elegans from the Maestrichtian. Stylar cusp A (parastyle) and D are well developed. Cusp B is feebly formed and is situated posterolabial to the paracone, close to the equally small stylar cusp C.
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
ETYMOLOGY: For W. A. Clemens, University of California, Berkeley.
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
HOLOTYPE: AMNH 77373, an upper molar (M 2 or M 3). TYPE LOCALITY: Clambank Hollow, Chouteau County, Montana.
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

Export occurrence data

Darwin Core Archive (ZIP)

CLASSIFICATION

Taxonomic Classification Tree

Occurrences with images

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
159397360
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
9076441
Taxon ID
1A7187CFFFA91719FAC6F957E3DC5254.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026