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Revealing the Sedimentary Responses to Glacio-Eustatic Changes

Published: February 21, 2023

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

Source: azocleantech.com

Related Topics:

United StatesPanthalassic OceanWenli YangJitao ChenMegan CraigInstitute Of GeologyChinese Academy Of SciencesSedimentary ResponsesNanjing InstituteChinese AcademySouth ChinaPlanetary Changeon JanuarySouth China BlockPaleo Tethys OceanLuodian BasinLate Paleozoic IceUpper CarboniferousLower Permian