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1.64 billion years ago, hydrocarbon biomarkers from a northern Australian basin reveal the ecological structure of mid-Proterozoic marine communities. The data indicate an anoxic, sulphidic, and permanently stratified marine environment, supporting evidence that oxygen levels remained below modern levels for a long period after the Great Oxidation Event. This dataset provides molecular fossil evidence for the co-existence of phototrophic purple and green sulphur bacteria.
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