Earth system instability amplified biogeochemical oscillations following the end-Permian mass extinction.

ABSTRACT: After the end-Permian mass extinction, the Earth system underwent extreme ecological and environmental fluctuations, including high temperatures, recurrent oceanic anoxia, and carbon cycle oscillations as demonstrated by the geochemical isotope proxy records. However, the underlying mechanism behind these oscillations remains poorly understood. Here we propose that they were produced by a coupled oscillation mode of marine phosphorus (P) and atmosphere-ocean carbon (A), driven by nonlinear redox controls on marine phosphorus burial. Our modeling demonstrates that the initial emplacement of the Siberian Traps and the mass extinction (on land and in the ocean) directly led to an early Triassic greenhouse. More importantly, it homogenized the ocean floor redox condition towards anoxia, activa

SUBMITTER: Li ZH 

PROVIDER: S-EPMC12008425 | biostudies-literature | 2025 Apr

REPOSITORIES: biostudies-literature