Stable Isotope Signatures of Authigenic Minerals from Methane Seeps

Abstract

Authigenic minerals forming at marine seeps constitute an excellent archive of past methane seepage and biogeochemical processes. Over the past two decades, authigenic carbonate and sulfur-bearing minerals from methane seeps of the South China Sea (SCS) have been widely investigated, providing insight into fluid sources and seepage dynamics and facilitating the establishment of geochemical proxies to trace sulfate-driven anaerobic oxidation of methane (SD-AOM). Authigenic carbonates from all seep sites in the SCS commonly exhibit low δ13C and high δ18O values, confirming the incorporation of methane-derived carbon and oxygen from a pore water pool probably affected by gas hydrate dissociation. Pyrite is a common authigenic mineral at methane seeps, also forming at low methane flux where authigenic carbonate tends to be absent. The identification of methane seepage and SD-AOM activity consequently benefited from the advancement of sulfur isotope geochemistry, particularly from in situ measurements of δ34Spyrite values using nanoSIMS and multiple sulfur isotopes. Quantification of carbon and sulfur fluxes in the course of SD-AOM in modern and ancient marine sedimentary environments remains challenging, highlighting the need for more field-based research and modeling work. Furthermore, other elemental cycles and biogeochemical processes at methane seeps archived in authigenic minerals, such as nitrogen-based metabolisms, remain largely unknown. We highlight that SCS seeps are fascinating natural laboratories to better understand methane-driven biogeochemical processes and their signatures in authigenic minerals, representing a rewarding but also challenging object of research in the field of geomicrobiology.