The quercymegapodiid hypothesis is supported by paleornithologist Sylvia Hope's (2002) paper on Mesozoic neornithines. This is based on the humeral facet of the coracoid having a large, free lateral flange, the reduced size of the procoracoid process, and a long, raised, ragged scar within the supracoracoid sulcus and parallel to the scapular facet. However, she also noted it differs from quercymegapodiids and more derived
galliforms in retaining a supracoracoid foramen. Altogether, the most satisfying and quite robust hypothesis is that if
P. retusus was not actually an early quercymegapodiid, it was just
basal to that group. The quercymegapodiids, an
extinct group of prehistoric Galliformes, lived apparently on both sides of the
Atlantic, which by then was narrower, with only a few straits separating Europe and North America in the temperate
Greenland region. They seem to have been inhabitants of warm regions as they seem also have to occurred in
Brazil, and it is quite likely that they were also found in or even originated in
Africa from where almost no contemporary bird fossils are known. Their undisputed fossil record starts in the
Eocene. Given that
Anseriformes are now known to have
radiated into the families still present today, it is suspected that by the end of the Cretaceous, at least 4 lineages of
Galliformes existed as distinct:
Megapodiidae,
Cracidae,
Phasianidae and the Quercymegapodiidae. Consequently, the possibility that the present species was also a quercymegapodiid is well in agreement with the
phylogenetic and
biogeographic data. ==Footnotes==