“…In addition, the phases of iron sulfide in nature include mackinawite (FeS), pyrrhotite (Fe 1−x S), pyrite (FeS 2 ), and greigite (Fe 3 S 4 ), etc., which exhibit more variability than iron oxide containing only Fe 2 O 3 and Fe 3 O 4 . The band gap in iron sulfide is smaller than that of iron oxide, leading to the former having more appropriate electron transfer and conductivity (Wadia et al, 2009 ; Jin et al, 2017 ; Zhang et al, 2018 ). Importantly, iron-sulfur clusters are important cofactors in many enzymes which serve as active centers for electron transfer in catalytic processes and respiratory chain reactions (Qi and Cowan, 2011 ).…”