In 2015, a bonebed designated as Z183 was discovered within of the approximate location described by Parrington. This bonebed contained at least three individuals of different sizes, represented by 27 bones, all of which were mixed in with the remains of an allokotosaurian; new elements not known previously included the maxilla, quadrate, braincase, axis, sacral vertebrae, humeri, ischia, and calcaneum. They were stored at the National Museum of Tanzania. It is quite possible, given the proximity, that this bonebed represents the same site that the original specimens were recovered from. In 2017, these remains, along with the holotype, were described by a study published in "Nature", co-authored by Sterling Nesbitt and others. They formally named the genus "Teleocrater", and the type and only species "T. rhadinus". The late Charig was honoured as a co-author on this study.