Scientists have unveiled important information on The Great Oxidation Event by studying apatite inclusions in zircon crystals from old magmas (IMAGE)
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Sulphur speciation in apatite inclusions in zircon acquired at the ESRF’s ID21 beamline. The spectrum of sulphur changed from reduced (S2-) to oxidised (S6+) from pre- to post- Great Oxidation Event. Authors argue that atmospherically-altered sediments infiltrated the mantle and changed the redox state of magmas.
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Hugo Moreira / Nature Geoscience
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