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Dolomite is besides calcite the most abundant carbonate mineral in the geological record. However, the conditions and mechanisms of its formation are poorly understood. Most dolomite is considered to have formed at elevated temperatures when sediments became deeply buried over geological time scales. Abundant dolomite occurs in shallow marine carbonate deposits of the ancient Triassic Tethys margi ...

The goal of this project is to understand the causes and modes of microbialite formation in critical periods of Earth history, typified by changing environments using the example of the Permian-Triassic-Boundary mass extinction event, the most fatal ever. In the aftermath of this mass extinction, microbialite-forming microbes became major components of the marine ecosystem, whereas >90% of marine ...