“…A very similar situation was found in monitoring wells PV-214 and PV-217, where facultative or strictly anaerobic bacteria were detected, including sulfate-, iron-or nitrate-reducing bacteria represented by the genera Geobacter, Sulfuritalea and families Desulfobacteraceae, Desulfobulbaceae, Comamonadaceae, Oxalobacteraceae, Holophagaceae, Rhodocyclaceae, Nitrospinaceae, Catabacteriaceae [39,40,41]. The detected genera and families indicate that the Cr(VI) reducing process could be mediated by iron-reducing and sulfate-reducing bacteria that are known to react up to 100 times faster than chromium-reducing bacteria from other laboratory studies [10]. This conclusion is also supported by the elevated concentration of soluble Fe (see Figure 4), the Pourbaix stability diagrams (see Figure 5) during the biotic phase that remained even after the decrease in bacterial biomass (see Figure 7) and depletion of TOC during the two last sampling campaigns (see Supplementary Information Figure S2).…”