The Permo-Carboniferous Dwyka Formation of Southern Africa: Deposition by a predominantly subpolar marine ice sheet
Abstract The 800-m thick glacigene Dwyka Formation was deposited along the northern margin of the Permo-Carboniferous Dwyka Basin which covered an area of approximately 2 × 10 6 km 2 in southwestern Gondwana. The palaeogeographic setting, geochemical data of the mudrocks and diamictites, and the palaeontology indicate marine conditions during sedimentation. Ice lobes from spreading centres in the north, east and south coalesced in the basin to form an extensive ice cover from the Westphalian to the late Sakmarian. Lodgement, rain-out and subaqueous debris-flow diamictons, subaqueous and subglacial melt-water sands, suspended mud, and turbidity current sands and silts accumulated in the Dwyka Basin. Sedimentation started on the continental shelf during a grounded ice sheet stage (predominantly lodgement processes), then a floating ice stage (predominantly debris rain-out), and finally an ice sheet disintegration stage (debris rain-out, sand fall-out and suspension settling of mud). The palaeogeographic setting, presence of marine conditions in the basin and the scale of glaciation indicate deposition from a predominantly mid-latitudinal marine ice sheet. The overall characteristics of the glacial sequence are neither typical of a polar nor a temperate setting and for such ancient glaciations a subpolar setting with the presence of unstable ice shelves is suggested.