Some of Earth’s oldest sedimentary rocks exposed in the Pilbara area of Western Australia include a mixed carbonate-evaporite-siliciclastic coastal sabkha. In the present day such sabkhas are widely colonized by microbial mats. Interacting with sedimentary processes such as erosion or evaporate crystal growth the microbial mats generate biogenic structures such as stromatolites or MISS.
In the Pilbara area of Western Australia stromatolites occur which belong to the oldest fossils in Earth history. However, there also exists a plethora of well preserved MISS. These structures represent an entire ecosystem of surprising diversity. Actualistic comparison of fossil and modern biogenic structures and their facies-related distribution in sabkha settings points towards the presence of microbial communities in the Paleoarchean time highly similar to those we are familiar with today.
Preferred Presentation Type: Oral