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54. Temporal evolution of shallow marine diagenetic environments: Insights from carbonate concretions S. Loyd et al. 10.1016/j.gca.2023.04.022
55. An evaporite-based high-resolution sulfur isotope record of Late Permian and Triassic seawater sulfate S. Bernasconi et al. 10.1016/j.gca.2017.01.047
56. Carbonate-associated sulfate as an archive of sulfur and oxygen stable isotope composition of seawater sulfate: Evidence from reef carbonate rocks of the southern South China Sea P. Di et al. 10.1016/j.chemgeo.2023.121699
57. Oceanic anoxia through the late Permian Changhsingian Stage in the Lower Yangtze region, South China: Evidence from sulfur isotopes and trace elements Z. Liao et al. 10.1016/j.chemgeo.2019.119371
58. Taphonomic experiments on caridean shrimp elucidate the timing and influence of organic matter on diagenetic pyritization and sulfurization G. Odin et al. 10.1016/j.chemgeo.2023.121858
59. Hydrothermally induced 34S enrichment in pyrite as an alternative explanation of the Late-Devonian sulfur isotope excursion in South China H. Yan et al. 10.1016/j.gca.2020.05.017
60. Volatile earliest Triassic sulfur cycle: A consequence of persistent low seawater sulfate concentrations and a high sulfur cycle turnover rate? M. Schobben et al. 10.1016/j.palaeo.2017.02.025
61. Petrographic and geochemical characteristics of the lacustrine black shales from the Upper Triassic Yanchang Formation of the Ordos Basin, China: Implications for the organic matter accumulation C. Wang et al. 10.1016/j.marpetgeo.2017.05.016
62. Petrography and sulfur isotopic compositions of SEDEX ores in the early Cambrian Nanhua Basin, South China T. Han et al. 10.1016/j.precamres.2020.105757
63. Reconstructing the redox environment of the Cambrian Harkless Formation, Nevada, USA: Navigating the effects of iron-rich clay minerals on the iron speciation redox proxy A. Hagen et al. 10.1016/j.chemgeo.2024.122453
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83. Negative δ13Ccarb shifts in Upper Ordovician (Hirnantian) Guanyinqiao Bed of South China linked to diagenetic carbon fluxes C. Chen et al. 10.1016/j.palaeo.2017.09.030
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