Paleomagnetism of a Neoarchean-Paleoproterozoic carbonate ramp and carbonate platform succession (Transvaal Supergroup) from surface outcrop and drill core, Griqualand West region, South Africa

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Genesis: early life survived in the Polar Circles by precipitating banded iron formation (~ 3.7–1.85 Ga) followed by stratified ferruginous siliciclasts until ~ 580 Ma, when tectonically shifted to lower latitudes initiating the ‘Cambrian Explosion’

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