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The Permian–Triassic time interval is associated with major perturbations in the biogeochemical cycling of several redox-sensitive elements. In particular, sulphur isotope ratios (δ34S) reveal substantial perturbations in sedimentary sulphates. De
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e286e0d2eefe08e6a4b8670d31905b35
https://doi.org/10.5194/egusphere-egu23-12950
https://doi.org/10.5194/egusphere-egu23-12950
