Bathornis is noted for its high number of species, and is the most speciose of all
Cariamiformes, extinct or extant.
Bathornis veredus The type species, whose discovery and etymology is mentioned above. It is known from
Eocene and
Oligocene deposits of the
Chadron Formation in
Colorado and
Nebraska. It is known from multiple tibiotarsal material, depicting an animal roughly the size of a modern
emu, something that earned it the description of "one of the most remarkable of recent additions to our fossil avifauna." Skull material from this species is also known.), further examination has shown it to belong to
Bathornis. There is some doubt about whereas it represents a different species or a younger morph of
B. veredus.; known from a similar tibiotarsus that differs in several respects from its contemporary.
Bathornis grallator B. grallator is known from the late
Eocene Washakie Formation of
Wyoming; similar fossils have been described from the
Willwood Formation, but their status as Cariamiformes, let alone bathornithids, are unclear. Originally interpreted as a terrestrial
cathartid,
Storrs Olson reassigned it to
Bathornis in 1985: The reconstruction published with the original description of
Neocathartes has often been reprinted and has now made the "terrestrial vulture" an integral part of the lore of avian paleontology. Well, forget it.
Neocathartes is just our old friend
Bathornis in another guise. Since then, posterior researchers have flip-flopped in their evaluation of
Neocathartes as a
junior synonym of
Bathornis, but most recent studies consistently refer to it within this genus.
Other forms Several undescribed remains from the late
Eocene and
Oligocene have been putatively assigned to
Bathornis. ==Palaeobiology==