Bienotheroides shartegensis, Watabe & Tsubamoto & Tsogtbaatar, 2007
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 |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.