S5: Global and local climate change during a Late Paleozoic glacial cycle revealed by conodont and sedimentary geochemistry from the Midcontinent, USA
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Supplemental Table 4: Results of inverse modeling using the freshwater values which are the measured values minus the 2SD of conodont Sr isotopic composition and organic matter C/N. Italics means the difference between the calculated and measured value (estSrtest, estCNtest) is beyond than the 2SD of the measured value.
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2025-10-21
