A new hominid skeleton from Sterkfontein Member 2 attaches to foot bones re
covered from loose blocks during the 1980s and first described in 1995. Sev
eral flowstone horizons are present above and below the skeleton and have g
iven clear palaeomagnetic signatures. Five changes in magnetic polarity hav
e been identified; when constrained by the available biostratigraphy, this
sequence can be placed confidently between 3.22 and 3.58 Ma. Interpolation
of sedimentation rates over the small intervals between reversals allows th
is range to be reduced to 3.30-3.33 Ma. The skeleton is thus the oldest yet
discovered and is considered to belong to a species of Australopithecus ot
her than africanus. Copyright (C) 1999 John Wiley & Sons, Ltd.