BRIEF OXYGENATION EVENT DURING EXTENSIVE ANOXIA ACROSS THE PERMIAN-TRIASSIC TRANSITION AS REVEALED BY THALLIUM ISOTOPES
Recently, thallium (Tl) isotopes have been used to constrain global-ocean anoxia during several major Mesozoic oceanic anoxic events (OAEs). This isotopic system is a useful tool for constraining global variations in seawater oxygenation. Tl isotopes are primarily affected by Mn-oxides during burial, which Tl adsorbs onto, one of the first processes affected by changes in ocean oxygenation. In addition, Tl’s relatively short seawater residence time, 18,500 years, allows for tracking detailed changes in oceanic oxygen content during major events.
Here, we use sedimentary records from three P-Tr sections to better constrain the global extent and timing of ocean anoxia in relation to the mass extinction event. Their Tl isotopic profiles document a significant perturbation in the global-ocean redox state during the P-Tr transition. This isotopic shift suggests that widespread seafloor anoxia developed prior to the extinction event, expanded at the start of the event, and remained anoxic long after the end of the event, similar to the observed record for two Mesozoic OAEs. The event’s onset is marked by. These sections also document a punctuated return to more negative Tl values at the event’s onset, which suggests widespread Mn-oxide burial, possibly due to a better oxygenated ocean. These data provide a unique window into understanding the development of oceanic anoxia during the P-Tr transition, a likely result of increased volcanic CO2 emissions, and a brief, but potentially important, oxygenation event at its onset.