Orange leads to black: evaluating the efficacy of co‐culturing iron‐oxidizing and sulfate‐reducing bacteria to discern ecological relationships

Summary Two global cycles, iron and sulfur, are critically interconnected in estuarine environments by microbiological actors. To this point, the methods of laboratory study of this interaction have been limited. Here we propose a methodology for co‐culturing from numerous coastal environments, from the same source inocula, iron‐oxidizing and sulfate‐reducing bacteria. The use of same source inocula is largely beneficial to understand real‐world interactions that are likely occurring in situ. Through the use of this methodology, the ecological interactions between these groups can be studied in a more controlled environment. Here, we characterize the oxygen and hydrogen sulfide concentrations using microelectrode depth profiling in the co‐cultures of iron‐oxidizing bacteria and sulfate‐reducing bacteria. These results suggest that while oxygen drives the relationship between these organisms and sulfate‐reducers are reliant on iron‐oxidizers in this culture to create an anoxic environment, there is likely another environmental driver that also influences the interaction as the two remain spatially distinct, as trends in FeS precipitation changed within the anoxic zone relative to the presence of Fe(III) oxyhydroxides. Understanding the relationship between iron‐oxidizing and sulfate‐reducing bacteria will ultimately have implications for understanding microbial cycling in estuarine environments as well as in processes such as controlling microbially influenced corrosion.