[1] The Olifantshoek Group in southern Africa contains Paleoproterozoic red beds that are exceptionally well preserved, lying unconformably atop a regionally extensive lateritic paleoweathering profile.We studied the basal unit of this succession, known as theGamagara or Mapedi Formation, and the lateritized substrate (so-called ‘‘Drakenstein’’ or ‘‘Wolhaarkop’’ paleosol) on which it developed....