Dr. Maximilian Halama

PhD Student, University of Tübingen



Max worked to define the minerals produced during thermochemical Fe(III) reduction in sediments, relavant to origin of banded iron formation (BIF) mineral assemblages. He also performed experiments related to preservation of elemental signatures sorbed to Fe(III) (oxyhydr)oxides during diagenesis, and partitioning and isotopic composition of carbon during thermochemical Fe(III) reduction.

Funding: Deutsche Forschungsgemeinschaft (DFG) grant