EARTHS OLDEST REPORTED GLACIATION - PHYSICAL AND CHEMICAL EVIDENCE FROM THE ARCHEAN MOZAAN GROUP (SIMILAR-TO-2.9 GA) OF SOUTH-AFRICA

The Pongola Supergroup is a thick succession of Archean (similar to 2. 9 Ga) supracrustal rocks in the eastern part of the Kaapvaal craton of southern Africa. Its upper part, the Mozaan Group (similar to 5000 m- thick) includes diamictites with a highly varied suite of clasts, some of which are striated and faceted. Clasts in associated stratified si ltstones are interpreted as ice-rafted debris. A glacial origin is als o supported by geochemical investigation of diamictite matrix material s and associated mudstones. Plots of SiO2:Al2O3 and TiO2:Al2O3 suggest that these rocks underwent little chemical weathering, an interpretat ion confirmed by calculation of a Chemical Index of Alteration with lo w values, typical of other glacial deposits. The analyzed rocks are ri ch in Fe (average Fe2O3(T) is similar to 24% wt %), like rocks of many other glaciomarine successions. The diamictites and associated mudsto nes of the Mozaan Group have low Th/Sc ratios, suggesting preferential incorporation of mafic materials into the diamictite matrix material. Previous studies suggest that this part of the Kaapvaal craton underw ent early cratonization, involving tectonic and plutonic events that m ay have contributed to the drawdown of atmospheric CO2 and eventually provided a suitable substrate for development of continental glaciers.