Two pulses of oceanic environmental disturbance during the Permian-Triassic boundary crisis
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文摘

Fe–S system was studied in a deepwater P–Tr boundary section (Xiakou, central China).

Redox conditions changed from stably euxinic to fluctuating during the end-Permian.

The onset of Fe–S system perturbations preceded the mass extinction by ∼10 kyr.

Two euxinic pulses coincided with mass extinction episodes and volcanic eruptions.

These relationships favor volcanism as the trigger for the end-Permian crisis.

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