THE Malawi Rift and Pliocene palaeofaunas, which include a hominid man
dible attributed to Homo rudolfensis, provide a biogeographical link b
etween the better known Plio-Pleistocene faunal records of East and So
uthern Africa. The Malawi Rift is in a latitudinal position suitable f
or recording any hominid and faunal dispersion towards the Equator tha
t was brought on by increased aridity of the Late Pliocene African lan
dscape. The evidence suggests that Pliocene hominids originated in the
eastern African tropical domain and dispersed to southern Africa only
during more favourable ecological circumstances.