Olbitherium
Olbitherium is an extinct mammal of the order Perissodactyla (an early ancestor of modern-day horses, rhinos, and tapirs) from the early Eocene epoch of Shandong, China.
| Olbitherium | |
|---|---|
Scientific classification  | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | Perissodactyla |
| Genus: | †Olbitherium Tong et al., 2004 |
| Type species | |
| Olbitherium millenariusum | |
Description and Classification
Olbitherium was originally described from lower and upper jaw fragments and several teeth found in the Wutu Formation of Shandong Province.[1] The limited material of Olbitherium shares similarities with several ungulate groups. According to Tong et al., the upper cheek teeth show similarities to early Perissodactyls, as well as the hyracoid Seggeurius, while the lower cheek teeth more closely resemble those of phenacodontids, such as Ectocion, Phenacodus, and Copecion. Due to these conflicting similarities, Tong et al. placed Olbitherium as incertae sedis within the Phenacodonta, a grouping of Perissodactyla, "Condylarthra", and Hyracoidea in McKenna's 1975 classification, and suggested that Olbitherium represents an intermediate stage in the evolution of perissodactlys from Phenacodus-like ancestors. [1] In 2010, a skull and post-cranial remains were described, and Olbitherium was assigned to the Perissodactyla, closely related to basal members of the extinct family Isectolophidae such as Homogalax and Cardiolophus.[2]
See also
References
- Y.-S. Tong; J.-W. Wang; J. Meng (2004). "Olbitherium millenariusum, a new perissodactyl-like archaic ungulate (Mammalia) from the Early Eocene Wutu Formation, Shandong". Vertebrata PalAsiatica. 42 (1): 27–38.
- Smith, T.; Missiaen, P. & Li, C.-S (2010). "A new specimen of the enigmatic perissodactyl-like archaic ungulate mammal Olbitherium from the Early Eocene of Wutu coal mine, Shandong province, China". Abstract: Annual Meeting of the Palaeontological Association.