Raranimus
Raranimus is an extinct genus of therapsids of the Middle Permian. It was described in 2009 from a partial skull found in 1998 from the Dashankou locality of the Xidagou Formation, outcropping in the Qilian Mountains of Gansu, China. The genus is the most basal known member of the clade Therapsida, to which the later Mammalia belong. Description. "Raranimus" shares a number of features with later therapsids and ancestral Sphenacodontia. The skull consists of a well preserved rostrum. The teeth suggest a carnivorous lifestyle for "Raranimus", as the incisors are recurved and the second canines are serrated on their  posterior edges. The incisors are morphologically similar to those seen in more derived theriodonts. The presence of two linguo−labially compressed canines is a diagnostic feature of "Raranimus". The presence of two functional canines is characteristic of sphenacodontids, and this condition is seen in no other therapsid other than "Rananimus". However, the slender, compressed shape of these canines is a derived characteristic of therapsids, with the canines of similarly sized sphenacodontids being more massively built. The precanines are small and anteriorly serrated, similar to what is seen in the synapsids "Dimetrodon" and "Tetraceratops". In the palate region of the skull, the  anterior process of the vomer ventrally overlies the premaxilla at the anterior margin of the choana. This overlap is also seen in dinocephalians. However, unlike any other therapsid, the choanae are short and extend only from the level of the fourth incisor back to the first canine. Phylogenetics. According to a phylogenetic analysis conducted along with its initial description, "Raranimus" is considered to be the basalmost therapsid. There has been some controversy as to whether "Tetraceratops" is a therapsid or a more basal pelycosaur. If "Tetraceratops" is a therapsid, as has recently been proposed, it would be the oldest and  most basal one known, surpassing "Raranimus" in age by several million years. However, later studies have questioned the placement of "Tetraceratops" within Therapsida, and the 2009 phylogenetic analysis using "Raranimus" places the genus outside of the clade. "Raranimus" occurs in strata that were deposited during the early Roadian stage of the Middle Permian. The sphenacodontids were most diverse before the Roadian in the Early Permian, yet therapsids did not appear as a diverse group until near the Roadian-Wordian boundary. This has left a morphological and temporal gap in the fossil record during which the origin of therapsids must have  occurred called Olson’s Extinction. With the general absence of therapsid remains from Olson's Extinction, different hypotheses have developed in order to explain the group's origins and initial diversification. One theory suggests that therapsids diversified quickly through rapid apomorphy accumulation sometime during the gap, while the other proposes that therapsids evolved gradually over the course of up to 35 Ma. Only recently have remains of basal therapsids such as "Raranimus" been found from China that occur during Olson's Extinction. Other therapsids that are known to have existed during the gap include "Sinophoneus" and "Stenocybus". Below is a  cladogram modified from Liu "et al.", 2009 depicting the phylogenetic relationships of "Raranimus" with therapsids that occur in Olson's Gap highlighted: