Scientists know that manganese, in its various oxide forms, plays a significant role in Earth’s geochemical cycles. However, the exact forms of manganese, their abundance and the mechanisms behind these cycles that occur in Earth’s deep, high-pressure interior are not well understood. But, a recent study, published in Physical Review B, reports on a newly discovered manganese rich compound that might help shed light on manganese’s behavior in Earth’s interior and explain why seismic waves slow down in certain regions.
While Earth’s mantle mostly consists of oxygen, magnesium, silicon, and iron, other elements, like manganese, also play an important role. Manganese oxides, such as MnO, Mn3O4, Mn2O3, MnO2, are known to exist in Earth’s interior and have been studied in the context of their stability in the high-pressure conditions of Earth’s mantle, but researchers think there may be additional manganese oxides involved.
These compounds have the ability to react with other compounds (and oxidize) depending on the surrounding pressure and temperature. They often act as powerful, pressure-sensitive redox agents, actively participating in deep-Earth geochemical cycling by reacting with and oxidizing subducted iron-bearing minerals.









