Mass-independent fractionation of sulfur isotopes by isotope-selective photodissociation of SO2

A quantitative understanding the origin of sulfur isotope mass-independent fractionation (MIF) is essential to a full interpretation of the Archean sulfur geochemical record. Laboratory experiments have demonstrated that a MIF signature is present in elemental sulfur produced during SO2 photolysis, but the underlying mechanism remains unknown. Here, I report the results of atmospheric chemistry modeling of isotope-selective photodissociation of SO2 in the (C) over tilde B-1(2) - (X) over tilde (1)A(1) bands from 190 to 220 nm. This band system is dominated by a bending mode progression that produces shifts in the absorption spectrum upon sulfur isotope substitution. Self-shielding in the rotationally-resolved lines of (SO2)-S-32 produces MIF signatures in SO and residual SO2. A self-shielding origin for sulfur MIF implies that the variations observed in Delta S-33 in Archean rocks reflect variation in atmospheric SO2 concentration, and demonstrates that MIF in terrestrial rocks can be derived from photochemistry independent of molecular symmetry. Citation: Lyons, J.R. ( 2007), Mass-independent fractionation of sulfur isotopes by isotope-selective photodissociation of SO2, Geophys. Res. Lett., 34, L22811, doi: 10.1029/ 2007GL031031.