Bienotheroides shartegensis, Watabe & Tsubamoto & Tsogtbaatar, 2007

Watabe, Mahito, Tsubamoto, Takehisa & Tsogtbaatar, Khishigjav, 2007, A new tritylodontid synapsid from Mongolia, Acta Palaeontologica Polonica 52 (2), pp. 263-274 : 264-265

publication ID

https://doi.org/ 10.5281/zenodo.13741917

persistent identifier

https://treatment.plazi.org/id/038E879A-FFEF-FFE0-FCE8-FCD2FF7B7BAB

treatment provided by

Felipe

scientific name

Bienotheroides shartegensis
status

sp. nov.

Bienotheroides shartegensis sp. nov.

Figs. 3–6 View Fig View Fig View Fig View Fig , 7C View Fig .

Holotype and only known specimen: MPC−Nd 10 /301, an incomplete skull associated with right and left lower jaws. Casts of MPC−Nd 10 /301 are deposited in HMNS ( HMNS 1486 View Materials and 1491).

Type locality: Ulaan Malgait Hills, Shar Teg locality, Gobi−Altai Aimag, southwestern Mongolia ( Fig. 2 View Fig ; Gubin and Sinitza 1996).

Formation and age: From a red mudstone bed of the lower part of the Ulaan Malgait Beds (about 10 meters above the boundary between the Ulaan Malgait Beds and the underlying Shar Teg Beds); Upper Jurassic ( Gubin and Sinitza 1996).

Derivation of the name: Named after the type locality.

Diagnosis.—Differs from the other species of Bienotheroides in having a much smaller M1 cusp. Differs from Bienotheroides zigongensis and Bienotheroides ultimus in

having proportionally shorter and wider PC/pc. Differs from B. ultimus in lacking a projection on the middle part of the mesial margin of PC. Differs from Bienotheroides wansienensis in lacking B0 cusp and a diastema between upper I1 and I2.

HMNS

Houston Museum of Natural Science

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