A highly redox-heterogeneous ocean in South China during the early Cambrian (∿29-514 Ma): Implications for biota-environment co-evolution
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文摘

We study Fe–S–C–Al-trace element data from eight early-Cambrian sections from South China.

We found a low sulfate and highly redox-heterogeneous ocean in South China in early Cambrian.

We found a clear pattern that more complex biotas lived in more oxygenated waters by comparison.

We propose that the “Cambrian Explosion” was likely a consequence of local oceanic oxygenation.

Our results suggest that the influence of animals on early Cambrian ocean chemistry was limited.

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