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.