“…Multiple S-isotope ( 32 S, 33 S, 34 S, and 36 S) analysis has proven to be useful for a wide array of applications. − In general, the isotope ratios of any two isotopes can be scaled to each other based on the mass i.e., “mass-dependent fractionation (MDF)” model. , The S-isotopic compositions vary with sources and cycling pathways e.g., in geochemical, biological, and atmospheric processes. − However, the main sulfur emissions within a specific regional reservoir possess distinctive characteristics of sulfur isotopic values, making it feasible to conduct source tracing, e.g., refs − . The δ 34 S (see the Materials and Methods section) signatures of various sources of atmospheric sulfate are disparate (SI Figure S1) and, as such, can be used for determining the origin of atmospheric sulfate e.g., refs − . However, an inherent issue is the broad diversity in the regional S-isotopic signatures for the two likely drivers of anthropogenic SO 2 emissions i.e., coal combustion (e.g., thermal power plants) and oil combustion (e.g., vehicular emissions) (SI Table S1).…”