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Gypsum desert & atmospheric deposition (C04)

Subject Area Mineralogy, Petrology and Geochemistry
Term since 2016
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 268236062
 
Despite much effort, an exclusive mineralogical mechanism by which the water-free calcium sulfate anhydrite can be formed or being transformed from gypsum could not be established experimentally suggesting that microbial life plays a critical role in initiating and/or catalyzing this mineralization process. We plan to investigate both the exact nature and connection of non-classical or biologically driven nucleation processes and the impact on geochemical archives by comparative analysis and controlled lab experiments. Experiments involving biogeochemical processes include precipitation of natural Ca-sulfates and trace-element fractionation processes mediated by organic substances, microorganisms and plants.
DFG Programme Collaborative Research Centres
Applicant Institution Universität zu Köln
 
 

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