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Geochemical evidence for widespread euxinia in the Later Cambrian ocean - Nature

3d ago1 min readNews
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From the article

Our study looks at the Tl isotope composition of two organic-rich shales deposited during an extinction & the SPICE (Steptoean Positive Carbon Isotope Excursion) in the later Cambrian (~494 million year ago). This event potentially represents a deoxygenation event in the ocean at the time. (5/7) 🧪⚒️
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