The fossil is from Late Cretaceous Bissekty Formation (Coniacian, 89–86 MYA) in the Kyzylkum, Uzbekistan. Another partial coracoid (PO 4605) is very similar and is referred to as Abavornis sp.
The fossil originates from the Late Cretaceous Bissekty Formation (Coniacian, 89–86 MYA) in the Kyzylkum, Uzbekistan. Another partial coracoid (PO 4605) is very similar and is identified as Abavornis sp.