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Rapid recovery of life at ground zero of the end-Cretaceous mass extinction.
Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2.
Thallium isotopes reveal protracted anoxia during the Toarcian (Early Jurassic) associated with volcanism, carbon burial, and mass extinction.
Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event.