Manganese geochemical cycling driven by fluctuating redox chemocline in the Ediacaran ocean

<p dir="ltr">The oceanic redox configuration was stratified and oscillational in continental marginal slope during the deposition of Ediacaran Doushantuo Formation</p><p dir="ltr">The paleoclimate variations influenced basin hydrochemistry and organism activity to trigger the fluctuations of redox chemocline</p><p dir="ltr">The fluctuations of the redox chemocline in slope regulated the unique Mn cycling and mineralization in the late Ediacaran ocean</p>