Ferrihydrite associated organic matter (OM) stimulates reduction by Shewanella oneidensis MR-1 and a complex microbial consortia Rebecca E. Cooper1, Karin Eusterhues2, Carl-Eric Wegner1, Kai Uwe Totsche2, Kirsten Küsel1,3 1Aquatic Geomicrobiology, Friedrich Schiller University, Jena, 07743, Germany 5 2Department of Hydrogeology, Institute of Geosciences, Friedrich Schiller University, Jena, 07743, Germany 3The German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Leipzig, 07743, Germany Correspondence to: Kirsten Küsel (
[email protected]) Abstract. The formation of Fe(III) oxides in natural environments occurs in the presence of natural organic matter (OM), resulting in the formation of OM-mineral complexes that form through adsorption or coprecipitation processes. Thus, 10 microbial Fe(III) reduction in natural environments most often occurs in the presence of OM-mineral complexes rather than pure Fe(III) minerals. This study investigated to what extent the content of adsorbed or coprecipitated OM on ferrihydrite influences the rate of Fe(III) reduction by Shewanella oneidensis MR-1, a model Fe(III)-reducing microorganism, in comparison to a microbial consortium extracted from the acidic, Fe-rich Schlöppnerbrunnen fen. We found that increased OM content led to increased rates of microbial Fe(III) reduction by S. oneidensis MR-1 in contrast to earlier findings with the 15 model organism Geobacter bremensis. Ferrihydrite-OM coprecipitates were reduced slightly faster than ferrihydrites with adsorbed OM. Surprisingly, the complex microbial consortia stimulated by a mixture of electrons donors (lactate, acetate, and glucose) mimics S. oneidensis under the same experimental Fe(III)-reducing conditions suggesting similar mechanisms of electron transfer whether or not the OM is adsorbed or coprecipitated to the mineral surfaces.