Reconstruction of secular variation in seawater sulfate concentrations

Long-term secular variation in seawater sulfate concentrations ([SO42-](SW)) is of interest owing to its relationship to the oxygenation history of Earth's surface environment. In this study, we develop two complementary approaches for quantification of sulfate concentrations in ancient seawater and test their application to late Neoproterozoic (635 Ma) to Recent marine units. The rate method is based on two measurable parameters of paleomarine systems: (1) the S-isotope fractionation associated with microbial sulfate reduction (MSR), as proxied by Delta S-34(CAS-PY), and (2) the maximum rate of change in seawater sulfate, as proxied by partial derivative delta S-34(CAS) / partial derivative t(max). The MSR-trend method is based on the empirical relationship of Delta S-34(CAS-PY) to aqueous sulfate concentrations in 81 modern depositional systems. For a given paleomarine system, the rate method yields an estimate of maximum possible [SO42-](SW) (although results are dependent on assumptions regarding the pyrite burial flux, F-PY), and the MSR-trend method yields an estimate of mean [SO42-](SW). An analysis of seawater sulfate concentrations since 635 Ma suggests that [SO42-](SW) was low during the late Neoproterozoic (< 5 mM), rose sharply across the Ediacaran-Cambrian boundary (similar to 5-10 mM), and rose again during the Permian (similar to 10-30 mM) to levels that have varied only slightly since 250 Ma. However, Phanerozoic seawater sulfate concentrations may have been drawn down to much lower levels (similar to 1-4 mM) during short (< similar to 2 Myr) intervals of the Cambrian, Early Triassic, Early Jurassic, and Cretaceous as a consequence of widespread ocean anoxia, intense MSR, and pyrite burial. The procedures developed in this study offer potential for future high-resolution quantitative analyses of paleo-seawater sulfate concentrations.