Manganese geochemical cycling driven by fluctuating redox chemocline in the Ediacaran ocean
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The oceanic redox configuration was stratified and oscillational in continental marginal slope during the deposition of Ediacaran Doushantuo FormationThe paleoclimate variations influenced basin hydrochemistry and organism activity to trigger the fluctuations of redox chemoclineThe fluctuations of the redox chemocline in slope regulated the unique Mn cycling and mineralization in the late Ediacaran ocean
创建时间：
2024-11-09
