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The response of marine carbon and nutrient cycles to ocean acidification: Large uncertainties related to phytoplankton physiological assumptions

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Academic year: 2021

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Figure 4. The relationship between the percentage change in CEX and (a) denitrification and (b) ocean suboxia (using results from the years 2000 and 2100).
Figure 6), with the suboxic volume increasing by 15% in Exp PP‐PSiFe or declining by 7% in Exp PP‐N (Table 2)

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