Late Proterozoic rise in atmospheric oxygen concentration inferred from phylogenetic and sulphur-isotope studies
@article{Canfield1996LatePR, title={Late Proterozoic rise in atmospheric oxygen concentration inferred from phylogenetic and sulphur-isotope studies}, author={D. Canfield and A. Teske}, journal={Nature}, year={1996}, volume={382}, pages={127-132} }
The evolution of non-photosynthetic sulphide-oxidizing bacteria was contemporaneous with a large shift in the isotopic composition of biogenic sedimentary sulphides between 0.64 and 1.05 billion years ago. Both events were probably driven by a rise in atmospheric oxygen concentrations to greater than 5–18% of present levels—a change that may also have triggered the evolution of animals.
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