Δ17O of O2 during Termination II and Termination V from EPICA Dome C ice core...
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Significant changes in atmospheric CO2 over glacial-interglacial cycles have mainly been attributed to the Southern Ocean through physical and biological processes. However,...
冰期-间冰期旋回期间大气二氧化碳的显著变化，既往多被归因于南大洋通过物理及生物过程介导的调控作用。然而，……
