| Summary: | Earth’s oxygen-rich atmosphere and its capacity to sustain complex life is the most paramount feature that distinguishes Earth from all other planets. The irreversible oxygenation of atmosphere occurred about half way through Earth’s history at ~2.3 Ga (the Great Oxidation Event – GOE) when for the first-time photosynthetic oxygen production surpassed the consumption by chemical reactions allowing it to accumulate in the atmosphere. Consequently, the GOE had a profound impact on the atmosphere-ocean system, intensifying continental weathering, and prompting an increase in the riverine inputs of phosphate, sulfate and metals to the oceans. Increased availability of macro- and micronutrients may have opened new ecological niches to be exploited by complex microbial communities who, in turn, impact biogeochemichal cycles leaving metabolic signatures in the sedimentary rocks. However, there has been significant debate about the exact nature of the GOE, the environmental changes that followed and how these changes are recorded in the rock record. The focus of this thesis is the ~2.0 Ga Zaonega Formation in the Russian Karelia. This formation is one of the finest archives from which to decipher the physical and chemical conditions, as well as the role of local- vs. global-scale processes in the aftermath of the GOE. The study applies organic carbon and sulfur isotope results to assess organic carbon fluxes, sulfur cycling and depositional conditions that indicate restructuring of the microbial communities at different stages of basin evolution. The results indicate that following the establishment of a substantial seawater sulfate reservoir after the GOE, its size and isotope composition may have remained stable for few 100s Ma. The thesis highlights the importance of evaluating spatial and temporal geochemical variability in the context of individual basinal history before reaching global-scale conclusions.
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