Dissacus zanabazari, Geisler & Mckenna, 2007

Geisler, Jonathan H. & Mckenna, Malcolm C., 2007, A new species of mesonychian mammal from the lower Eocene of Mongolia and its phylogenetic relationships, Acta Palaeontologica Polonica 52 (1), pp. 189-212 : 190

publication ID

https://doi.org/ 10.5281/zenodo.13742027

persistent identifier

https://treatment.plazi.org/id/33098317-5A7F-4441-4A7F-FB0BDD3AED06

treatment provided by

Felipe

scientific name

Dissacus zanabazari
status

sp. nov.

Dissacus zanabazari sp. nov.

Figs. 1–11 View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig , Tables 1–4.

Holotype: MAE−BU−97−13786 ( Figs. 1–11 View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig View Fig ), partial skeleton including skull with mandibles; 5 vertebrae:atlas, axis, 2 posterior lumbar, and the first sacral; partial right humerus and ulna; right radius; complete distal left forelimb except for distal phalanges; pelvis, complete right hind limb except for distal ends of metatarsals and distal phalanges; proximal end of left femur. Collected on August 23, 1997 by the joint expedition of the Mongolian Academy of Sciences and the American Museum of Natural History.

Type locality: Tsagaan Khushuu (Tsagan Khushu), Nemegt Basin, Omnogov Aimag (Province), Mongolia.

Derivation of name: In honor of Undur Geghen Zanabazar (1635– 1723), a renowned leader of Mongolia who initiated a renaissance in Mongolian religious art, literature, and architecture.

Age and distribution.— The holotype and only known specimen of Dissacus zanabazari was found several meters above the base of the Bumban Member of the Naran−Bulak Formation. Dashzeveg (1988) correlated the mammalian fauna of the Bumban Member with early Eocene faunas of North America and Europe. An early Eocene age for the Bumban fauna is also supported by the faunal cluster analysis of Meng and McKenna (1998) .

Diagnosis.—Short face; trilobed lower incisors; no diastemata between lower premolars and molars except between p1 and p2; m3 metaconid subequal to protoconid; lingual face of M3 protocone nearly vertical; foramen for superior ramus of stapedial artery entirely within petrosal; anterior halves of 3 rd and 4th metacarpals abut each other; medial edge of lesser trochanter of femur not thickened. In addition to the above listed autapomorphies, Dissacus zanabazari differs from D. argenteus in having a wider talonid basin on m3; differs from D. europaeus in having lower hypoconids on p4 and m1–m3, a transversly wider and mesodistally shorter talonid on m3; differs from Yantanglestes feiganensis (originally assigned to Dissacus ) in having a double−rooted p2, the anterior edge of the orbit over M1 not M2; differs from D. indigenus in having a higher hypoconid and cristid obliqua on lower molars, less retroflexed p4 protoconid; differs from D. serratus in having higher and less recurved protoconids on p3 and p4, shorter talonid basin on p3; differs from D. magushensis in lacking an entoconid on m1; differs from D. navajovius in having better developed talonid basins on p3 and p4, molar protoconids more distal than metaconids, protocone more mesial than paracone on P4; differs from D. praenuntius in lacking ento− and ectocingula on m3 and a well−developed metastyle on M3; differs from D. rotundus in having a much wider talonid basin on m3; differs from D. willwoodensis in having a much wider m3, mandibular ramus that does not deepen posteriorly; differs from D. argenteus in having a wider talonid basin on m3; differs from D. zengi in being larger and in having a lower hypoconid on m2.

Kingdom

Animalia

Phylum

Chordata

Class

Mammalia

Order

Cetacea

Family

Mesonychidae

Genus

Dissacus

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