Barite quarry in the “Dresser Formation” of the Pilbara Craton. This rocks are around 3.5 million years old and contain evidence of microbial life. (IMAGE)

University of Göttingen

Barite quarry in the “Dresser Formation” of the Pilbara Craton. This rocks are around 3.5 million years old and contain evidence of microbial life.

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Barite quarry in the “Dresser Formation” of the Pilbara Craton. This rocks are around 3.5 million years old and contain evidence of microbial life.

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Jan-Peter Duda

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