Several mineral-reducing microbes have been shown to utilize solid-phase minerals as terminal electron acceptors, by extracellular electron transport (EET) processes that conduct electrons to the exterior of the cell via redox enzymes1. EET is critical, not only for microbe-mineral processes but also applied energy and environmental technologies, such as microbial fuel cells2, electrode synthesis3, and bioremediation4. New EET-capable bacteria are highly sought after, and have been extensively studied from a fundamental or applied perspective5. However, we only have limited insight into the ecological or biogeochemical significance of these bacteria. The majority of EET-capable microbes have been isolated following enrichment from aqua, sediment, or anaerobic digesters using solid electron acceptors such as MnO2, Fe2O3 or poised electrodes in laboratory6,7,8. However, these methods often produce similar consortia and potentially miss more sensitive taxa that may dominate low energy or low biomass systems, biasing the ability of these microbes to adapt to the lab or axenic culture environment9. Usually for low biomass environments, large quantities of water from a site are filtered to concentrate bacterial cells. However, EET-capable bacteria often exhibit anaerobic metabolisms and therefore oxygen exposure may further inhibit or prevent their cultivation. Alternative on-site methodologies to concentrate cells without exposing them to oxygen could facilitate the isolation of EET-capable bacteria. Here, we report setup details for an on-site electrochemical technique to enrich EET-capable microbe over a long period of time without the need for an external power source.
Using our electrocultivation experiments from a highly alkaline spring in Northern California, the Cedars10, we describe this on-site electrochemical technique. The geochemistry of the springs at The Cedars are impacted by serpentinization in the subsurface. The springs are highly reductive, with oxygen concentrations below the limit of detection under the air water interface highlighting the potential for microbial energy production via EET in this functionally anoxic environment11. However, there is no evidence to support EET-capable microbes from the Cedars (in either 16S rRNA or Metagenomic analysis). Even though this environment has been characterized as electron acceptor limited, the potential for using insoluble minerals as terminal electron acceptors, including minerals such as the iron baring minerals that result from serpentinization (i.e., magnetite), has not been extensively investigated12. We, therefore, deployed our electrochemical system at Campsite Spring, a high pH spring at the Cedars, to enrich for EET-capable microbes (Figure1)13.