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TraceS - Tracing sulphur cycling in the Iceland crust

Subject Area Mineralogy, Petrology and Geochemistry
Geology
Term since 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 554985741
 
Despite the large impact of human activity on the global S cycle, the natural S fluxes from oceans and lithosphere to atmosphere may be still poorly constrained. Especially in mid-ocean ridges (MOR), estimating the mantle-derived S flux to the surface remains a challenge due to (1) a lack of data on S concentrations in basaltic glasses, (2) variable S sources obscuring a possible mantle origin and (3) unknown amounts of S sequestrated in the oceanic crust upon fluid-rock interaction. This project aims to determine the sources and fluxes of S within a MORs using the Icelandic crust as an analogue. In conjunction with geochemical isotope modelling and state-of-the-art mass spectrometric techniques, S concentrations, along with S isotope compositions and trace element data of thermal fluids, bulk rock, sulphides and sulphates will be used to constrain the fluxes from different sources (e.g. seawater, rock leaching) of S at MORs. Furthermore, the potential of fluid-rock interaction in hydrothermal systems along MORs of permanently fixing S by mineral formation upon fluid-rock interaction will be investigated. Remelting of such modified oceanic crust within subduction zones might greatly affect the S isotopic values of melts, volcanic gasses and geothermal fluids in volcanic arcs. Findings of this study will also have an impact on ongoing research on sequestration of anthropogenic S within the Earth’s crust.
DFG Programme Research Grants
International Connection Iceland, USA
 
 

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