Sulfate reduction is one of the earliest types of energy metabolism used by ancestral organisms to sustain life. Despite extensive studies, many questions remain about the way respiratory sulfate reduction is associated with energy conservation. A crucial enzyme in this process is the dissimilatory sulfite reductase (dSiR), which contains a unique siroheme-[4Fe4S] coupled cofactor. Here, we report the structure of desulfoviridin from Desulfovibrio vulgaris, in which the dSiR DsrAB (sulfite reductase) subunits are bound to the DsrC protein. with its conserved C-terminal cysteine reaching the distal side of the siroheme. We propose a novel mechanism for the process of sulfite reduction involving DsrAB, DsrC, and the DsrMKJOP membrane complex (a membrane complex with putative disulfide/thiol reductase activity), in which two of the six electrons for reduction of sulfite derive from the membrane quinone pool. These results show that DsrC is involved in sulfite reduction, which changes the mechanism of sulfate respiration. This has important implications for models used to date ancient sulfur metabolism based on sulfur isotope fractionations.The dissimilatory reduction of sulfur compounds is one of the earliest energy metabolisms detected on earth, at ϳ3.5 billion years ago (1, 2). At the end of the Archean (ϳ2.7 billion years ago), the advent of oxygenic photosynthesis led to a gradual increase in the levels of atmospheric oxygen, which in turn caused an increasing flux of sulfate to the oceans from weathering of sulfide minerals on land (3). As a consequence of this process, reduction of sulfate became a dominant biological process in the oceans, resulting in sulfidic anoxic conditions from about 2.5 to 0.6 billion years ago (3, 4). During this extended period, sulfate-reducing prokaryotes were main players in marine habitats where most evolutionary processes were taking place. Today, these organisms are still major contributors to the biological carbon and sulfur cycles, and their activities have important environmental and economic consequences.A key enzyme in sulfur-based energy metabolism is the dissimilatory sulfite reductase (dSiR), 3 which is present in organisms that reduce sulfate, sulfite, and other sulfur compounds. This enzyme is also found in some phototrophic and chemotrophic sulfur oxidizers, where it is proposed to operate in the reverse direction (reverse sulfite reductase, rSiR). The dSiR is minimally composed of two subunits, DsrA and DsrB, in an ϳ200-kDa ␣ 2  2 arrangement. The dsrA and dsrB genes are paralogous and most likely arose from a very early gene duplication event that preceded the separation of the archaea and bacteria domains (5-8), in agreement with a very early onset of biological sulfite reduction. The dSiR belongs to a family of proteins that also include the assimilatory sulfite (aSiR) and nitrite (aNiR) reductases, the monomeric low molecular mass aSiRs, and other dSiRs like asrC and Fsr (9 -11). This family has in common a characteristic cofactor assembly that includes an iro...