and then entered Africa around the
Oligocene-Miocene boundary.
Probably earlier, if _Struthio coppensi_ (or
_Struthioolithus coppensi_) is good: Namibia, 20 mya,
osteologically rather "modern".
Kurochkin summed up the Asian record in 1976
(Smiths.Contrib.Paleobiol.27) and here he lists 5
sites that I'd call reasonably good candidates based
on date and location alone*, notably a good Middle
Oligocene record. Ratites? Not even a bit of eggshell.
Ergilornithids, ecologically somewhat convergent?
Numerous.