The remains of
Avimimus were recovered by Russian paleontologists and officially described by Dr.
Sergei Kurzanov in 1981. The
Avimimus fossils were initially described as having come from the
Djadokta Formation by Kurzanov; however, in a 2006 description of a new specimen, Watabe and colleagues noted that Kurzanov was probably mistaken about the provenance, and it is more likely that
Avimimus hailed from the more recent
Nemegt Formation. The
type species is
A. portentosus. A variety of isolated bones that have been attributed to
Avimimus were considered to be distinct from
A. portentosus, and were initially referred to as
Avimimus sp. In 2008, a team of Canadian, American, and Mongolian paleontologists headed by Phil Currie reported in 2006 an extensive bonebed of
Avimimus sp. fossils. The bonebed is in the Nemegt Formation, 10.5 meters above the
Barun Goyot Formation, in the Gobi Desert. The team reported finding abundant bones of at least ten individuals of
Avimimus, but the deposit may hold more. All individuals were either adult or subadult, and the adults showed little variation in size, suggesting
determinate growth. The team also suggests that the individuals were found together because they were
gregarious in life, providing possible indications that
Avimimus formed age-segregated groups for either
lekking or flocking purposes. The adults showed a greater degree of skeletal fusion in the tarsometatarsus and tibiotarsus, and also more prominent muscle scars. The preservation of the bonebeds suggest that they were buried rapidly, uncovered by rapid flow of water, and then buried again a short distance away. In 2018,
Avimimus sp. was formally described as a new species,
A. nemegtensis. ==Description==