Causes of perceived faunal change in the later Neogene of East Africa

African terrestrial vertebrate faunas change over the time range from 14 my to 4 my, the period during which hominids are presumed to have diverged from other hominoids. The most complete local sequence showing this is provided by the Tugen Hills, west of Lake Baringo in Kenya. A large component of the pattern of faunal changes seen there, and at other relevant sites, could be explained by local environmental alterations, or by sampling properties of fossil assemblages and collections. It is hard to justify global climatic change as the sole explanation of observed faunal shifts, although such external factors cannot be ruled out and on general grounds are likely to be involved. As yet there is no convincing demonstration of synchronicity in faunal turnover. Evidence of a simple shift from forest conditions to grasslands, an event that has been correlated with the origins of hominid bipedalism, is hard to detect. Existing data suggest a more patchy distribution of forest and grassland in both space and time.