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Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery

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Figure

Figure 1 | Geological information. (geological map of Oman and UAEDienerian (not to scale) showing estimated palaeo-depths (based on facies) and site numbers as inslope, (4) Wadi Wasit South and Radio Tower; distal slope, (5) Ba’id; seamount, (6) Buday’ah;
Figure 2 | Distribution of Fe-speciation data as a function of total Fe.Samples are coloured by lithology (blackalso be a decrease in precision, leading to excessively high Fehave Fedata for these samples cannot be interpreted
Figure 3 | Summary of Fe-speciation and Fe/Al records for the Arabian Margin. Samples where FePalaeontological informationfor Fe-speciation regardless of lithologyresultshelp interpret FeFigs 1–7
Figure 4 | S-isotope systematics. Comparison of newpublished values ofrecordsinference of ferruginous conditions from Fe-speciation and suggests low d34Spy data with d34Sseawater from Late Permian and Early Triassic CAS40,41
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