4.7 Article

Organic matter diagenesis and precipitation of Mg-rich carbonate and dolomite in modern hypersaline lagoons linked to climate changes

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Summary: The Dolomite Problem, a century-old controversy, involves the formation of low-temperature dolomite in ancient rocks despite favorable geochemical conditions. Microbes and their exopolymeric substances (EPS) have been found to play a role in nucleating dolomite, with a shift in microbial communities affecting the EPS suited for dolomite precipitation. The turnover of organic material under anoxic conditions is identified as an important driver of the process, shedding new light on the interpretation of dolomite throughout Earth's history.

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