AnimaliaNot EvaluatedacceptedspeciesAccepted
Alphadon halleyi

Alphadon halleyi

Sahni, 1972

GBIF:159397355

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ABOUT

Descriptions(4)

DESCRIPTION: Several lower molars from Clambank Hollow show morphological differences from teeth that can be assigned to A. praesagus. AMNH 77367 is significantly smaller (length 2.1 mm., fig. 13 U, V) than lower molars of A. praesagus. Its paraconid is a conical cusp and it is slightly medial to the metaconid. The metaconid is anteroposteriorly elongated, particularly at its base, and tapers toward the apex. The protoconid is taller than the metaconid and situated anterior to it. The talonid is deep and basined and the crista obliqua is oriented in the manner characteristic of Alphadon. The hypoconid is a well-developed cusp, and the hypoconulid is directed posteriorly and more separated from the entoconid than in most contemporary marsupials. The width of the talonid (1.2 mm.) is equal to that of the trigonid. A partial upper molar, AMNH 77370, is small enough to be included within A. halleyi (fig. 13 W). The width of the crown is 1.7 mm. and it is approximately equal to the estimated length. The stylar shelf anterior to stylar cusp C is broken. Stylar cusp D is well developed and larger than stylar cusp C. The metacone is as high as the paracone and separated from it by a narrow valley. Both conules are present, and the protocone is a low cusp. Alphadon halleyi is a possible ancestor to the Maestrichtian A. lulli.
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: Smaller than Alphadon praesagus but larger than A. lulli from the Lance Formation. Upper molars with stylar cusp D well developed and larger than stylar cusp C; metaconule and protoconule distinct, protocone low.
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: Named in honor of the Warren Halley family on whose ranch most of our prospecting was done.
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 77367, a lower molar. TYPE LOCALITY: Clambank Hollow, Chouteau County, Montana. KNOWN 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

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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
159397355
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
4975114
Taxon ID
1A7187CFFFAA171DFE91F896E52B5FE2.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026