S6: Global and local climate change during a Late Paleozoic glacial cycle revealed by conodont and sedimentary geochemistry from the Midcontinent, USA

Supplemental Table 5: Results of inverse modeling using the saltwater values which are the measured values plus 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 greater than the 2SD of the measured value.