Abstract The Late Archaean-Early Proterozoic Transvaal Sequence is preserved within the
Transvaal, Kanye and Griqualand West basins, with the 2050 Ma Bushveld Complex …

The 15 000 m of relatively unmetamorphosed clastic and chemical sedimentary and
volcanic rocks of the 2550-2050 Ma Transvaal Sequence as preserved within the Transvaal …

The unique and evolving nature of the Precambrian geological environment in many ways
was responsible for significant differences between Precambrian clastic sedimentary …

Microbially mediated calcification can be traced back for at least 2.6 billion years. Although
morphological comparison of fossil and recent microbial carbonates suggests that …

Stilpnomelane-rich tuffaceous mudrocks are an important component of the
Palaeoproterozoic Kuruman and Griquatown Iron Formations in the Northern Cape …

Calculation of sedimentation rates of Neoarchaean and Palaeoproterozoic siliciclastic and
chemical sediments covering the Kaapvaal craton imply sedimentation rates comparable to …

The precipitation of calcite and aragonite as encrustations directly on the seafloor was an
important platform‐building process during deposition of the 2560–2520 Ma Campbellrand …

Concentrically rolled-up silty mudrock laminae, 1–2 mm thick, are found in the uppermost of
four, 40–110 cm thick interdune beds within a thick aeolian succession of the c. 1.8 Ga …

Recent radiometric dating of carbonates and banded iron-formations on the Kaapvaal
Craton, southern Africa, has suggested that late Archaean and Palaeoproterozoic carbonate …

The oldest filament-and colonial coccoid-containing microbial fossil assemblage now known
is described here from drill core samples of stromatolitic cherty limestones of the …