S4: Global and local climate change during a Late Paleozoic glacial cycle revealed by conodont and sedimentary geochemistry from the Midcontinent, USA
Supplemental Table 3: Results of inverse modeling using measured 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
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