Recreating manganese minerals

How should we interpret ancient manganese deposits?

Due to the modern dependence of manganese on O2 and oxygen-derived species, manganese deposits have long been interpreted as reflecting changes in the redox state of the local or global environment. However, surprisingly little is constrained about the formation processes behind the dominant manganese minerals in the geologic record. We are working to recreate important manganese minerals like the manganese silicate braunite and manganese-rich carbonates in controlled experiments to better interpret what these minerals are signaling about past environments and (bio)geochemistry.

The giant Hotazel manganese deposit in South Africa, comprised of the minerals braunite and kutnohorite.

Contact

Jena E Johnson

Assistant Professor
Earth and Environmental Sciences

University of Michigan
1100 N. University Ave.
Ann Arbor, MI 48109-1005

Email: jenaje@umich.edu
Office: 3006 C.C. Little Building