Dsungarodon, Pfretzschner & Martin, 2005

Pfretzschner, Hans-Ulrich, Martin, Thomas, Maisch, Michael W., Matzke, Andreas T. & Sun, Ge, 2005, A new docodont mammal from the Late Jurassic of the Junggar Basin in Northwest China, Acta Palaeontologica Polonica 50 (4), pp. 799-808 : 800-802

publication ID

https://doi.org/ 10.5281/zenodo.13625285

persistent identifier

https://treatment.plazi.org/id/039C8792-A905-BA69-F569-FC0700D3FEE2

treatment provided by

Felipe

scientific name

Dsungarodon
status

 

Genus Dsungarodon nov. Pfretzschner and Martin Derivation of the name: Named after the Junggar Basin (formerly Dsungar) and OÔO v, stem of OÔOÓÇ (Greek) tooth. Dsungarodon (masculine), tooth from the Junggar Basin.

Type species: Dsungarodon zuoi sp. nov.

Diagnosis.—Upper molar characters: (1) cusp X hook shaped and recurved buccally; (2) basin developed between cusps A−C−Y−X; (3) cusps A and C high and slender and considerably higher than cusps X and Y; (4) buccal crests forming a cutting edge; (5) lingual portion mesial to the A−X−crest is reduced; (6) distal margin C−Y of the lingual portion of the tooth not deeply indented; (7) strong ectoflexus; (8) outline of the tooth crown triangular.

Lower molar primitive (–) and derived (+) characters: (1) cusp e and f reduced (+); (2) crest b−e well developed (–); (3) crest b−e protruding to the mesial end of the tooth (+); (4) crest e−g missing (–); (5) crest b−g well developed (–); (6) enlarged anterior basin (pseudotalonid) (+); (7) cusp g enlarged, similar in height to cusp c (+); (8) region distal to cusps a and c reduced (+).

Differential diagnosis.—The upper molar of the new taxon differs from those of Haldanodon exspectatus by the following characters: (1) cusp X hook−shaped and recurved buccally; (2) basin developed between cusps A−C−Y−X; (3) cusps A and C high and slender; (4) buccal crests forming a cutting edge; (5) lingual portion mesial to the A−X−crest reduced; (6) distal margin C−Y of the lingual portion of the tooth not deeply indented; (7) strong ectoflexus. Dsungarodon differs from Simpsonodon oxfordensis by the following upper molar characters: (1) buccal cusps A and C much more slender and considerably higher than cusps X and Y; (2) lingual part of the tooth more narrow and more constricted; (3) outline of the tooth crown more triangular.

At the lower molars, the new taxon differs from Tegotherium , Sibirotherium , and Tashkumyrodon by exclusion of

PFRETZSCHNER ET AL.— NEW JURASSIC DOCODONT FROM CHINA 801

1 mm

cusp e from the border of the “pseudotalonid” and by retaining a well developed crest b−g. From Docodon , Haldanodon , and Borelalestes it differs by reduction of cusps f, presence of a large anterior basin (“pseudotalonid”), reduction of a c−d crest, large cusp b, and cusps c and g being of equal height. From Simpsonodon it differs by a straight, mesio−lingually oriented crest b−e that is accompanied by a straight transversal valley between the crests b−g and b−e. Furthermore, the pattern of enamel ridges in the region distal to cusp a and c is less complex. Dsungarodon is clearly distinct from Krusatodon by the following characters: (1) crest b−e runs straight forward in a mesio−lingual direction; (2) a distinct cusp e is not developed; (3) crest b−g is straight and not S−shaped; (4) cusp g does not bulge more lingually than cusp c; (5) crest c−d is almost straight; (6) a distinct cusp f is not developed.

Distribution and stratigraphical range.—Upper part of Qigu Formation at Liuhuanggou, 40 km southwest of Urumqi in the Junggar Basin (Xinjiang Autonomous Region, NW China). Early Late Jurassic (Oxfordian).

ET

East Texas State University

NEW

University of Newcastle

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