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Reliable carbonate carbon isotopes (d13Ccarb) mirror differences in global carbon cycling, and thus the paleoclimate and paleoceanographic conditions

United statesPanthalassic oceanWenli yangJitao chenMegan craigInstitute of geologyChinese academy of sciencesSedimentary responsesNanjing instituteChinese academySouth chinaPlanetary changeon januarySouth china blockPaleo tethys oceanLuodian basinLate paleozoic ice