High Mn concentrations provide unique indicators of water-rich environments and their redox states. Very high-potential oxidants are required to oxidize Mn to insoluble, high-valence oxides that concentrate Mn in rocks and sediments; these redox potentials are much higher than those needed to oxidize Fe or S.
|Number of pages||2|
|Publication status||Published - Mar 2015|
|Event||46th Lunar and Planetary Science Conference - The Woodlands, United States|
Duration: 16 Mar 2015 → 20 Mar 2015
|Conference||46th Lunar and Planetary Science Conference|
|Period||16/03/15 → 20/03/15|