Figure 5. Trace metal analysis of sediment core PS1506-1
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An increase in whole ocean alkalinity during glacial periods could account, in part, for the drawdown of atmospheric CO2 into the ocean. Such an increase was inevitable due to...
冰期阶段全海洋碱度（whole ocean alkalinity）的升高，可部分解释大气二氧化碳向海洋的固存过程。此类碱度提升本就不可避免，其根源在于……
