AnimaliaacceptedfamilyAccepted
Pediomydae

Pediomydae

GBIF:159397344

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Figure 130
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 pediomyid affinities of the right upper molar, AMNH 77375, from Clambank Hollow, are indicated by the prominence of stylar cusp D, the narrowing of the stylar shelf labial to the paracone, and the presence of an anterolingual cingulum which often occurs as a variation in later Maestrichtian species, particularly in P. elegans. AMNH 77375 (fig. 130) is small and as transverse as M 3 of P. elegans Clemens (1966, p. 37). A ridge connects the apex of the paracone to the parastyle. It is likely that AMNH 77375 belongs with the other small lower and upper molars assigned to Pediomys clemensi but such an association cannot be demonstrated. DISCUSSION: Pediomys clemensi is a relatively rare member of the fauna from the Judith River Formation, and is closest morphologically to P. elegans from the Lance Formation of Wyoming. Pediomys elegans is the Maestrichtian species that Clemens (1966, p. 34) regarded as most primitive of those then known. Only one species of Pediomys appears to be present as ascertained from the upper molars. Unfortunately, there is not a single complete upper molar of Pediomys; thus there is no way of determining whether the three upper molar fragments belong to the same species. The pediomyid stylar shelf is radically different from that of other marsupials not only in the nonuniform width of the stylar shelf but also in the relative development of the stylar cusps. Buccal to the paracone, the stylar shelf narrows considerably and is little more than a narrow cingulum. The shelf in some later Maestrichtian species may even be absent and discontinuous in this area. Posteriorly, the shelf widens buccal to the metacone. Stylar cusp B is feebly formed and situated closer to cusp C than to cusp A. Cusp D is the largest stylar cusp. The paracone is more labial than the metacone.
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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FIG. 13. Alphadon praesagus (Russell), new combination. A. AMNH 77342, occlusal view of right maxilla with M3, M4. B. AMNH 77343, occlusal view of right M2. C. AMNH 77344, occlusal view of right M'. D. AMNH 77355, lingual view of right P3. E. Occlusal view. F. AMNH 77361, occlusal view of left M4. G. Lingual view. H. AMNH 77356, occlusal view of left mandible with M3. I. Labial view. J. Lingual view. K.?Alphadon praesagus (Russell), new combination, AMNH 77398, occlusal view of DP3. L. Lingual view. M. Alphadon praesagus (Russell), new combination, AMNH 77358, lingual view of right mandible with M2 and P3 talonid. N. Occlusal view. 0.?Pediomyidae, AMNH 77375, occlusal view of right upper molar. Pediormys clemensi, new species. P. AMNH 77373, occlusal view of left upper molar. Q. AMNH 77376, occlusal view of right lower molar. R. Lingual view. S. AMNH 77377, occlusal view of right lower molar. T. Lingual view. Alphadon halleyi, new species. U. AMNH 77367, occlusal view of left lower molar. V. Lingual view. W. AMNH 77370, occlusal view of left upper molar. All x 10.

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The vertebrate Fauna of the Judith River formation, Montana

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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
159397344
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Taxon ID
1A7187CFFFAE1719FE6EF7C2E5515CE8.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026