https://pimsignaling.com/index.....php/high-fidelity-c
Here, we present carbonate-associated sulfate δ34S data from sections spanning the Late Triassic-Early Jurassic change, which document synchronous large positive trips on a global scale occurring in ~50 thousand many years. Biogeochemical modeling shows that this S isotope perturbation is better explained by a fivefold boost in international pyrite burial, in keeping with large-scale development of marine anoxia on the Pa
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