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We have recently reported non-mass-dependent 17 O depletion in sulfate deposited after the Marinoan glacial meltdown at ca. 635 million years ago. Further investigation linking the Δ 17 O of barite to its sedimentological–geological context in Marinoan South China reveals that the 17 O depletion in sulfate is most pronounced at sites near paleo-continents, supporting the hypothesis...
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