Iron sulfide minerals, including mackinawite (FeS), are relevant in origin of life theories, due to their potential catalytic activity towards the reduction and conversion of carbon dioxide (CO 2 ) to organic molecules, which may be applicable to the production of liquid fuels and commodity chemicals. However, the fundamental understanding of CO 2 adsorption, activation, and dissociation on FeS surfaces remains incomplete. Here, we have used density functional theory calculations, corrected for long-range dispersion interactions (DFT-D2), to explore various adsorption sites and configurations for CO 2 on the low-index mackinawite (001), (110), and (111) surfaces. We found that the CO 2 molecule physisorbs weakly on the energetically most stable (001) surface but adsorbs relatively strongly on the (011) and (111) FeS surfaces, preferentially at Fe sites. The adsorption of the CO 2 on the (011) and (111) surfaces is shown to be characterized by significant charge transfer from surface Fe species to the CO 2 molecule, which causes a large structural transformation in the molecule (i.e., forming a negatively charged bent CO 2 −δ species, with weaker C-O confirmed via vibrational frequency analyses). We have also analyzed the pathways for CO 2 reduction to CO and O on the mackinawite (011) and (111) surfaces. CO 2 dissociation is calculated to be slightly endothermic relative to the associatively adsorbed states, with relatively large activation energy barriers of 1.25 eV and 0.72 eV on the (011) and (111)