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Conchoraptor

Conchoraptor (meaning 'conch plunderer') is a genus of oviraptorid dinosaur from the late Cretaceous Period of what is now Asia. Conchoraptor was a small dinosaur, only 1–2 meters (3.3-6.6 feet) in length. Unlike many other oviraptorids, Conchoraptor lacked a head crest. Like its relatives, it lacked teeth. Instead of teeth, oviraptorids had powerful beaks, possibly adapted to crushing mollusk shells. The skull of Conchoraptor was heavily pneumatised, with most of the bones hollow. Internal connections between both ears functioned as resonance chambers and improved hearing. When first discovered in the Red Beds of Hermiin Tsav of the Early Maastrichtian Nemegt Formation by a Polish-Mongolian expedition in 1971, scientists believed that Conchoraptor was a juvenile Oviraptor and that the animal's missing crest would have begun to grow when the animal reaching sexual maturity. Further study of multiple skeletons showed that Conchoraptor belonged in a new genus. The hands of Conchoraptor were a major reason that scientists decided to split it off from Oviraptor. Anatomically the hands seemed to be an evolutionary intermediate between those of Ajancingenia and Oviraptor, making it obvious that this animal was not a member of a known species. The type species of this new genus, Conchoraptor gracilis, was described and named by Barsbold, in 1986. The generic name is derived from Greek konkhè, 'mussel', and Latin raptor, 'plunderer'. This name reflects Barsbold's hypothesis that oviraptorids, rather than preying primarily upon eggs as had been traditionally thought, may have been specialized to feed on mollusks. The specific name means 'gracile' in Latin. The holotype is IGM 100/20, a partial skeleton with skull. Later about two dozen specimens were formally referred to the species. Conchoraptor was by Barsbold assigned to the Oviraptoridae in 1986. Recent analyses show it was a member of the oviraptorid subfamily Ingeniinae. The cladogram below follows an analysis by Fanti et al., 2012. The Nemegt Formation of Mongolia, is estimated to date back to the Maastrichtian stage, between 70 and 66 million years ago of the Late Cretaceous period. During the Late Cretaceous period, the land that is now the Nemegt Formation had an arid environment with fields of sand dunes and only intermittent streams. It is slightly younger than the nearby Djadochta Formation, and seems to have been slightly wetter. This formation is noteworthy for the exquisite preservation of small and fragile dinosaur skeletons, a rare occurrence considering that these fossils are typically broken up and dispersed when found in other rock formations.

[ "Oviraptorosauria", "Theropoda" ]
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