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The mountains that triggered the Late Neoproterozoic increase in oxygen: The second great oxidation event

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Campbell, Ian; Squire, Richard J.

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The consensus view is that the O2 concentration of the Archean atmosphere was very low and that it rose to its present level of 21% in a series of steps, two of which dwarf the others in importance. The first, known as the Great Oxidation Event, occurred

CollectionsANU Research Publications
Date published: 2010
Type: Journal article
URI: http://hdl.handle.net/1885/55656
Source: Geochimica et Cosmochimica Acta
DOI: 10.1016/j.gca.2010.04.064

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