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.