Precambrian solution photochemistry, inverse segregation, and banded iron formations

Physics

Scientific paper

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Scientific paper

SOLAR radiation on an early Precambrian sea would generate short-lived excited species near the surface of the water. Many of the species would be powerful oxidising or reducing agents. Despite back-reactions, net reducing power would be lost to the atmosphere. This effect would be the opposite of present day photosynthesis and can be termed `inverse segregation'. Its possible relevance to banded iron formation is discussed here.

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