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This study investigates carbonate-hosted manganese deposits in the South China Block, revealing that some manganese carbonates form through direct synsedimentary precipitation under anoxic conditions. The findings suggest that these deposits can serve as proxies for ancient oceanic redox fluctuations, particularly during periods of well-oxygenated oceans, and may be linked to significant biotic crises. The research provides new insights into the geochemical and sedimentological processes that influenced man

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makae2021

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EN