Excavations at Duinefontein (DFT) 2 near Cape Town, South Africa have recov
ered numerous stone artefacts and animal bones on an ancient surface sealed
within iron-stained eolian sands. U-series analysis of an overlying calcre
te places the sands before 150 ka ago, while the large mammal taxa imply an
age between 400 and 200 ka ago. The artefacts include a classic Acheulean
handaxe and probable biface shaping flakes that support this age estimate.
The principal mammalian species are long-homed buffalo, black wilde-beest,
greater kudu, Cape zebra, and grysbok/steenbok, which imply a grass-and-bus
h mosaic instead of the historic small-leafed shrubland.
Hippopotamus and reedbuck indicate that water stood nearby, probably in dun
e swales. The large mammal bones are mostly vertebrae and other axial eleme
nts, often in near-anatomical order. Both proximal and distal appendicular
elements are rare. Bones with carnivore damage are common, but ones with st
one tool marks are scarce. The sum suggests a water-edge attritional death
site where people played a minimal role and carcasses were disarticulated m
ainly by carnivore feeding and by trampling. Stone tool marks tend to be eq
ually rare at other Acheulean attritional death sites, and the implication
may be that Acheulean people rarely obtained large mammals, whether by hunt
ing or scavenging. Human scavengers at DFT2 would not have encountered a di
sproportionate number of distal (versus proximal) limb elements, and it fol
lows that the tendency for distal elements to dominate many archeological a
ssemblages need not reflect scavenging versus hunting. Even if DFT2 was not
itself a locus of intense human activity, it provides useful baseline for
evaluating bone damage, skeletal part representation, and other variables a
t sites where people were deeply involved. (C) 1999 Academic Press.