AnimaliaNot EvaluatedacceptedspeciesAccepted
Belonostomus longirostris

Belonostomus longirostris

(Lambe, 1902) Lambe, 1902

GBIF:159397231

0year

ABOUT

Descriptions(2)

A broken rostrum and a few scales that are referable to Belonostomus longirostris have been recovered during the present investigation. Although the genus does not occur commonly in the formation, it was first reported by Lambe (1902) from the Oldman Formation as Diphyodus longirostris. It was identified three years later (Stanton and Hatcher, 1905, p. 57) from the Judith River Formation of Montana. The genus Diphyodus was put in synonymy with Belonostomus by Estes (1964, p. 25) on the basis of the similarity of the rostrum and the fragmentary scales of the lateral line system. The fragment of the rostrum (AMNH 10111) from Clambank Hollow shows the presence of two rows of teeth along the outer margin. The width of the rostrum is about 3.6 mm. The dimensions compare closely with those of the type specimen described by Lambe (1902, p. 30) in which the anterior end of the dentary is 3.5 mm. wide and the posterior width is slightly larger (4.0 mm.). The occurrence of this marine fish in these coastal plain deposits can only be attributed to the proximity of the sediments to the sea.
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
Diphyodus longirostris LAMBE, 1902, p. 30. Belonostomus longirostris: ESTES, 1964, p. 25.
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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CLASSIFICATION

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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 2026-06-16.

CC0Published 12/31/1972View dataset
GBIF Usage Key
159397231
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
4964357
Taxon ID
1A7187CFFFF61741FB27FA52E56050A2.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026