Sulfide Dissolution and Awaruite Formation in Continental Serpentinization Environments and Its Implications to Supporting Life
Vrijmoed, J. C.
Engelmann, J. M.
Liesegang, M.
Wiechert, U.
Rohne, R.
Plümper, O.
DOI: https://doi.org/10.23689/fidgeo-4378
Engelmann, J. M.; 1 Institute of Geological Sciences Freie Universität Berlin Berlin Germany
Liesegang, M.; 1 Institute of Geological Sciences Freie Universität Berlin Berlin Germany
Wiechert, U.; 1 Institute of Geological Sciences Freie Universität Berlin Berlin Germany
Rohne, R.; 1 Institute of Geological Sciences Freie Universität Berlin Berlin Germany
Plümper, O.; 2 Department of Earth Sciences Utrecht University Utrecht The Netherlands
Abstract
Serpentinization environments are key locations that support microbial communities by the abiogenic formation of reduced species associated with peridotite alteration. Here we studied partially serpentinized peridotites from the Chimaera seeps (Turkey), an active continental serpentinization system that vents highly methane‐rich fluids, to investigate the impact of water‐rock interaction on the sulfide and metal mineralogy and its implications on supporting microbial communities. Using high‐resolution scanning electron microscopy, electron microprobe analysis, and transmission electron microscopy we found diverse pentlandite decomposition features with precipitation of secondary sulfides including millerite, heazlewoodite, as well as Cu‐bearing sulfides, native Cu, and awaruite (Ni3Fe). Awaruite forms dense veinlets to single crystal platelets tens of nanometers in size, which is formed by desulphurization of pentlandite. In addition, the nanometer‐sized awaruite platelets are intimately intergrown with serpentine suggesting its growth during peridotite alteration by a dissolution‐precipitation process, likely associated with the interaction of methane‐ and H2‐rich but highly sulfur‐undersaturated fluids. Based on sulfur isotope signatures we infer a mantle and mid‐ocean ridge origin of the sulfide minerals associated with the first stage of partial serpentinization and awaruite formation. Subsequent and ongoing continental fluid‐rock interaction causes significant sulfide decomposition resulting in the formation of porosity and the release of, amongst others, H2S and Fe. These species may likely provide a source of nutrients for active microbial communities in these comparatively nutrient‐starved, low‐temperature continental serpentinization environments.
Key Points:
High disequilibrium conditions induce skeletal awaruite growth during continental serpentinization.
Pentlandite dissolution creates fluid pathways and nutrients for microbial life.
Sulfur isotope compositions document ocean floor and subsequent continental serpentinization processes.