Enhanced weathering as a trigger for the rise of atmospheric O 2 level from the late Ediacaran to the early Cambrian
Scientific reports, pp. 106302019.
A shift toward a higher oxygen level in both ocean and atmosphere systems during the late Ediacaran to the early Cambrian has been suggested from multiple indirect proxies. However, the mechanism and magnitude of this oxidation remain unclear. To solve this issue, we measured carbon isotopes in both carbonate and organic matter as well as...More
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