Multiple Sulfur Isotope Geochemistry during the Permian-Triassic Transition
نویسندگان
چکیده
The end-Permian mass extinction was the largest biodiversity crisis in Phanerozoic. Based on characteristic negative ?33S signals of sedimentary pyrite, previous multiple sulfur isotope studies suggested shoaling anoxic/sulfidic deep-waters onto a shelf, leading to shallow-marine extinction. However, validity this model has been controversial. I compiled previously-reported records during Permian-Triassic transition interval, and examined stratigraphic relationship between horizon, redox oscillation depositional settings, record each studied section. compilation shows that do not correspond clearly horizon or benthic anoxia/euxinia sections. also documents are substantially variable, were observed various types sediments including carbonates, carbonates/siltstones relatively deep-water facies, abyssal deep-sea cherts. Those observations allow me infer signal is robust indicator shoaling. Rather, isotopic may reflect substantial heterogeneity controlled by local factors.
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ژورنال
عنوان ژورنال: Geosciences
سال: 2021
ISSN: ['2076-3263']
DOI: https://doi.org/10.3390/geosciences11080327