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Alphadon praesagus

Alphadon praesagus

(Russell, 1972) Sahni, 1972

GBIF:159397353

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Descriptions(5)

DESCRIPTION: M 1; specimen AMNH 77344, an M 1, is assigned to Alphadonpraesagus (fig. 13 C). It is less transverse than the other upper molars. The tooth is only slightly wider than it is long and the stylar shelf is wide. Stylar cusp A is well developed but smaller than the other stylar cusps. A narrow, short valley separates it from stylar cusp B, and it is connected to the paraconule by a crest. Stylar cusp B is a large cusp with at least three distinct ridges leading from its apex. One ridge extends anteriorly, another low ridge joins the paracone, and a third trends posteriorly toward stylar cusp C. Stylar cusp C is situated centrally on the incipiently bilobate stylar shelf. Its elongate orientation is not anteroposterior, but at an angle to this direction, leaving a small, flat shelf between itself and stylar cusp B. Stylar cusp D is smaller than stylar cusp C. The paracone and metacone are well separated by a broad valley, as in A. marshi, and the metacone is noticeably taller than the paracone. No anterolingual cingulum is present. Both conules are well developed. Although the roots are broken, it is possible to make out an interradicular crest that joins the lingual side of the labial roots together. M 2; an M 2, AMNH 77343 (fig. 13 B), is relatively more transverse than M 1 but is relatively less transverse than M 3. The stylar shelf of M 2 is asymmetrically bilobate. Stylar cusp A is situated at the anterolabial corner of the crown on an expanded shelf area, and is separated from stylar cusp B by a valley similar to that found in M'. Stylar cusp B is well developed, and joined by a ridge to the paracone, and the cusp is farther separated from the paracone than the corresponding cusp in M 1. An indistinct ridge arises from the apex of stylar cusp B and joins the smaller stylar cusp C, situated at the stylar cleft. Stylar cusp D, although slightly worn, still appears to have been smaller than stylar cusp C. The paracone and metacone are separated by a broad valley and there does not seem to be much difference in the relative heights of these cusps. The protocone is a low cusp. The lingual portion of the crown is broken, but there appears to be a small anterolingual cingulum. An interradicular crest is present as in M 1. M 3 and M 4; a maxilla fragment containing M 3 and M 4, AMNH 77342 (fig. 13 A), has been recovered. The stylar shelf on its M 3 is worn, but stylar cusp B seems to have been well developed as indicated by the labial expansion of the stylar shelf in that area. Stylar cusp A is much smaller than cusp B and is separated from it by a short valley. Stylar cusp C is smaller than cusp B, and is situated on the labial margin of the stylar shelf at the stylar cleft. Stylar cusp D is present and is smaller than cusp C. A high, worn ridge links the metastyle to the metacone, and the paracone is broken and missing. Both conules are present, and the premetaconular wing terminates at the rounded anterolingual side of the metacone. The protocone is relatively low. A short but distinct anterior cingulum is present, and extends from about the base of the paraconule to the anteroventral side of the protocone. M 4; few M 4 s have been found in association with other teeth of Alphadon and consequently their assignment to the genus is tentative. Two M 4 s of A. rhaister were described by Clemens (1966), and a complete maxilla with M 1 - M 4 of A. marshi from the upper Edmonton Formation of Alberta was described by Lillegraven. M 4 is smaller than M 3 and is characterized by an anterolabial expansion of its stylar shelf. Stylar cusp A is present and a well-developed cingulum connects this cusp to the paraconule. Stylar cusp B is the best-developed stylar cusp. It is connected by a high ridge to the conical paracone, which is much larger and taller than the metacone. Stylar cusp C is present on the labial side of the crown and is smaller than cusp B. Posterior to cusp C, the stylar shelf rapidly narrows and forms the posterolabial part of the metacone. Both the paraconule and the metaconule are present, and the protocone is a low cusp. An anterior cingulum, similar to that found on M 3, occurs on M 4. Russell (1952) described an incomplete lower jaw with M 3 collected below the mouth of Berry Creek, southeast of Steveville, in the Oldman Formation, as Delphodon? praesagus. Clemens (1966, p. 109) suggested that this molar pertained to the genus Alphadon but, in the absence of upper molars, the assignment could not be certain. A large number of isolated teeth and two jaw fragments with teeth, from Clambank Hollow, confirm Clemens's suggestion. This is the most common marsupial from the Judith River Formation. Dimensions of the complete lower molars are given in table 1. Fragmentary molars are useful only in establishing the relative frequency of occurrence of Alphadon praesagus. Comparisons of lengths of the upper and lower molars of A. praesagus agree with the general principle proposed by Clemens (1966, p. 83) that in didelphoid marsupials the lengths of the " lower molars tend to be equal to or greater than the lengths of their upper counterparts. " P 3; some premolars have been found that most likely belong to A. praesagus. It is not possible to clearly distinguish between isolated P 2 and P 3 because they are morphologically and dimensionally very similar. Only a few differences can be made out, principally in the degree and development of the lingual and labial cingula adjacent to the posterior accessory cusp. Specimen AMNH 77355 (fig. 13 D, E) is tentatively identified as P 3 on the basis of a large anterior " spirelike " cusp (protoconid), the development of cingula that are lingual and labial to the posterior accessory cusp, and on the basis of size. The mean length of P 3 in Alphadon marshi is 1.75 mm. (Clemens, 1966), whereas the length of AMNH 77355 is much greater (2.4 mm.). This difference is in keeping with size of molars of A. praesagus, which are larger than those of A. marshi. The primary cusp on P 3 is a large, transversely compressed cusp with steep anterior and more gentle posterior margins. A short anterolingual cingulum is present at the base of the cusp. The posterior accessory cusp is much smaller but well separated from the larger anterior cusp by the presence of a short valley. Two ridges, one originating from the apex of the large primary cusp, and the other from the apex of the posterior accessory cusp, terminate in this valley. Two other ridges arising from the posterior accessory cusp extend lingually and labially. The lingual ridge is higher and longer than the labial one. A basal cingulum is present on the posterolabial corner of the crown. The tooth is two rooted. DP 3; a left DP 3, AMNH 77398. is similar to the deciduous premolar figured by Clemens (1966, p. 108). This tooth is tentatively assigned to Alphadon praesagus on the basis of size (length 2.5 mm.). Its trigonid is anteroposteriorly elongated, and the protoconid is situated anterior to the metaconid. The talonid cusps are distinct and well separated (fig. 13 K, L). MI; two teeth have been tentatively identified as M 1 s. They are smaller but otherwise similar to M 2 s. M 2; there are at least four isolated lower molars similar in size and morphology to M 2 in the mandible of Alphadon praesagus (AMNH 77358, illustrated in fig. 13 M, N). A comparison with UCMP 50299 and 50300, a right and left mandible, respectively, of A. marshi (Clemens, 1966, p. 89) reveals that they are significantly smaller but otherwise morphologically very similar to the Campanian mandible, AMNH 77358. The posterior extension of the symphysis in both Lance species, Alphadon lulli and A. marshi, is below P 2, and a similar condition is present in the Campanian mandible. A prominent mental foramen occurs ventral to M 1 in the Lance mandibles, and also in the Campanian specimen. These features confirm identification of the preserved teeth as P 3 and M 2. The molar has a well-developed, anteriorly projecting paraconid. The paraconid is the smallest cusp of the trigonid and is well separated from the metaconid. All trigonid cusps are conical with broad bases. An anterobasal cingulum extends ventrolabially from the paraconid. The talonid is slightly wider than the trigonid, and the crista obliqua connects the prominent hypoconid to the posterior wall of the trigonid, ventral to the notch separating the protoconid from the metaconid. The hypoconulid and the entoconid are twinned, and the hypoconulid is posterior to the lingually situated entoconid. A broad cingulum extends posterolabially to the hypoconid. M 3; an isolated M 3, AMNH 77356, is assigned to Alphadon praesagus (fig. 13 H-J). Its trigonid is anteroposteriorly compressed, and the protoconid is the tallest cusp and is situated slightly anterior to the metaconid. The metaconid is only slightly higher than the paraconid. An anterior cingulum is feebly developed. The width of the trigonid (2.0 mm.) of AMNH 77356 is greater than that of the talonid (1.8 mm.). The hypoconid is well developed and separated from the other two talonid cusps. A prominent posterolabial cingulum is present at its base. Entoconid and the hypoconulid are elevated in position and situated close to each other. The entoconid is completely lingual in position. Specimen AMNH 77356 and an additional M 3, AMNH 77366, resemble the type specimen of Alphadon praesagus. Length and width of AMNH 77356 is 3.2 mm. and 2.0 mm., respectively, whereas in the type specimen, NMC 114, the corresponding dimensions are 3.3 mm. and 2.2 mm., respectively. M 4; an isolated molar, AMNH 77361, is probably an M 4, as based on its trigonid / talonid width ratio and on its large anteroposteriorly elongated posterior root (fig. 13 F, G). The protoconid is the highest trigonid cusp, and the metaconid is equal to, or slightly taller than, the paraconid. An anterobasal cingulum is present. The hypoconid is a prominent cusp with a posterolabial cingulum, and the hypoconulid is twinned with the lingual entoconid. The crista obliqua intersects the protoconid-metaconid ridge at a point posterior to the metaconid.
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 A-N
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
REVISED DIAGNOSIS: A common Campanian didelphid with close similarities to the slightly smaller A. marshi. The type specimen, NMC 114, from the Oldman Formation, is a partial right lower mandible with M 3, roots of M 4, and an alveolus for the posterior root of M 2. The stylar shelf of M 3 is broad, and the stylar cusp is better developed than in most contemporary marsupials. It is separated from stylar cusp B by a short valley. Stylar cusp B is the largest stylar cusp, with a low ridge joining the only slightly higher paracone, another ridge extends to stylar cusp C. This latter elongate cusp is variously oriented, it may be inclined to the anteroposterior direction (Ml) or less inclined (M 2) or situated on the labial margin (M 3 and M 4). Cusp C is smaller than stylar cusp B but larger than stylar cusp D. A high ridge links the metastyle to the metacone. The metacone is as tall or slightly taller than the paracone. The protocone is a low cusp. The lower teeth have a crista obliqua that intersects the protoconid-metaconid wall just ventral to the notch separating the posterior trigonid cusps.
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
Delphodon? praesagus RUSSELL, 1952, p. 11 3. Delphodon? praesagus: CLEMENS, 1966, p. 109.
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: NMC 114, a right mandible with M 3 and roots of M 4. TYPE LOCALITY: Four miles below the mouth of Berry Creek, southeast of Steveville, Alberta. KNOWN DISTRIBUTION: Oldman Formation, Alberta; 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

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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
159397353
Dataset Key
fd03f669-c046-46cd-861a-6bf56b7fc989
Origin
source
Backbone Key
11198881
Taxon ID
1A7187CFFFD7171DFA86FB69E1F25CA0.taxon
Last Crawled
6/10/2026
Last Interpreted
6/10/2026