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.

补充表5：采用以牙形石（conodont）锶同位素组成与有机质碳氮比的实测值加上其2倍标准偏差（2SD）得到的盐水端元值开展反演模型计算的结果。其中，斜体格式代表计算值与实测值的差值（estSrtest、estCNtest）大于实测值的2倍标准偏差。