Abstract
Current thoughts on the early history of the earth have been greatly influenced by the models of Cloud (1972, 1976). These models have attempted to explain, in an internally consistent fashion, the evolution of the atmosphere, hydrosphere, biosphere and crust of the earth. Our concepts of the origin of one of the most enigmatic rock types in the geologic record — the early Precambrian banded iron formations — have also been greatly influenced by Cloud’s models. During the past several years, many advances have been made in the fields of isotopic age dating, geochemistry and sedimentology which are significant to our understanding of the early history of the earth and to the origin of early Precambrian banded iron formations. In this context, a review of some of these advances and their implications seems warranted.
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McLennan, S.M. (1980). Timing and Relationships Among Precambrian Crustal and Atmospheric Evolution and Banded Iron-Formations. In: Trudinger, P.A., Walter, M.R., Ralph, B.J. (eds) Biogeochemistry of Ancient and Modern Environments. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-48739-2_8
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