“…Analysis has shown that a geochemical gradient develops within the bioreactor, going from oxic, to suboxic, to reducing with depth. The redox change is concomitant with distinct reaction layers, including an upper allochthonous sediment zone, an iron-rich oxidized zone, an aluminum-rich zone, and a lower, unreacted shell material zone at the bottom (DiLoreto et al, 2016a). Bacterial communities in the reducing zone are hypothesized to contribute to metal removal (primarily Zn, Tl, and Ni) via biogenic sulfide precipitation, however this biotic mechanism has yet to be explored thoroughly within the bioreactor.…”