The photo-irradiation of natural organic matter (NOM) is a well-documented pathway of •OH production in surface waters. Using humic acid (HA) as a model compound, we show that the perturbation of NOM-bearing oxic environments by naturally occurring reduced species, sulfide, contributes to •OH production under dark conditions. Sulfide concentration had a more prominent influence on •OH production than HA. When HA was controlled at 16 mM C under oxic and neutral pH conditions, the increase of sulfide concentration from 0 to 5 mM increased the cumulative •OH concentration from <2 to 72.2 μM within 120 min. When sulfide was maintained at 2.5 mM, the increase of HA concentration from 0 to 16 mM C increased the cumulative •OH concentration from <0.6 to 44.8 μM. •OH accumulation showed good consistency with sulfide removal and O2 consumption. O2 consumption increased with increasing HA concentration at a fixed sulfide concentration, and also increased with increasing sulfide concentration at a fixed HA concentration. UV–Vis and FTIR characterizations suggested that the reduced HA moieties resulting from sulfide interaction with HA acted as the redox-active moieties responsible for •OH production. Additionally, 3DEEM fluorescence suggested the reaction of sulfide with oxic HA as a partially reversible reduction-oxidation process with production of labile HA fluorophoric intermediates. Our findings implicate that the perturbation of NOM-bearing oxic environments by sulfide, i.e., from the discharge of anoxic groundwater, springs, seafloor black smokers, and hydrothermal vents, is another important source of •OH in natural environments in addition to photo-irradiation.