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Earth in dependence of continental growth and how geochemical mineral-water reactions controlled the composition of the first ocean. These processes involve forward weathering (dissolution of primary
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life emerged. As a PhD candidate, you will evaluate scenarios through numerical modelling of mantle dynamic and lithosphere (de)formation processes, using the range of possible Hadean compositions and
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observational conditions in this area. In this 4-year study, you will reconstruct ISM precipitation changes over the past ~100-1000 years, based on lipid biomarkers and their isotopic composition stored in lake
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