Sulfur is the tenth most abundant element on Earth (Steudel & Chivers, 2019) and is cycled dynamically between the geosphere and biosphere. Sulfate or sulfide in water and soil and sulfur dioxide in the atmosphere constitute the majority of sulfur in nature (Middelburg, 2000) with the oceans as a major reservoir. Here, sulfur is present in very large quantities as dissolved sulfate and also as sedimentary minerals like gypsum (Sievert et al., 2007). Among sulfur-containing minerals, pyrite (FeS 2) is especially ubiquitous (Johnson et al., 2012; Muyzer & Stams, 2008). Sulfur exhibits high reactivity in reduced forms and occurs in several stable oxidation states, ranging from −2 (as in sulfide or reduced organic sulfur) to +6 in sulfate. The most stable form of sulfur in the presence of oxygen is sulfate, while the reduced inorganic forms of sulfur with oxidation states of −2 and zero (as in elemental sulfur) are quite common in anoxic environments. Smaller but significant roles are played by polysulfide, polythionates, thiosulfate, sulfoxides as well as elemental sulfur. Sulfur compounds of mixed valence states like thiosulfate or tetrathionate occur transiently. Organic sulfur compounds like the volatile dimethylsulfide are also important on a global scale. The latter transports sulfur from the oceans to terrestrial regions, and it also affects atmospheric chemistry and the climate system (Charlson et al., 1987; Kettle & Andreae, 2000).