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Through Bird, Seed and Asia

As previously defined, they were paraphyletic as the genus Pternistis, which was previously included in Francolinus, is more closely related to Old World quails than it is to the other francolins. Beginning in 2004, various ornithologists have recommended that it would be clearer to use "spurfowl" for all members of the genus Pternistis and restrict the use of "francolin" to the other species presently or formerly classified in Francolinus. When Pternistis is excluded, the francolins form a monophyletic clade that is a sister group to a clade comprising the junglefowl (Gallus) and the bamboo partridges (Bambusicola); together, these clades compose the tribe Gallini.

Although formerly classified in the partridge subfamily Perdicinae, this classification is no longer supported, and they are now classified in the subfamily Pavoninae.

Francolins are terrestrial (though not flightless) birds that feed on insects, vegetable matter and seeds. Most of the members have a hooked upper beak, well-suited for digging at the bases of grass tussocks and rootballs. They have wide tails with fourteen rectrix feathers. Most species exhibit spurs on the tarsi.

Distribution

Of the approximately 17 extant species, the natural range of five (composing the genus Francolinus and Ortygornis) are restricted to Asia, while the remaining genera are restricted to Africa. Several species have been introduced to other parts of the world, notably Hawaii.

Twelve of the species which occur in Africa are found in the subcontinental region of southern Africa; of these, seven occur in varying proportions within the political boundaries of Namibia and Zambia. Six southern African francolins are considered endemic to the subcontinent, of which three are found in Namibia and Zambia (the Hartlaub's, red-billed and Orange River francolins).

The Cape spurfowl, endemic to the Cape Province of South Africa, occurs marginally in southern Namibia and southwestern Zambia. A fossil francolin, Francolinus capeki, has been described from Late Pliocene deposits of Hungary; the contemporary fossil galliforms "Francolinus" minor and "F." subfrancolinus are now placed in Palaeocryptonyx.

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