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Reconsidering the role of carbonate ion concentration in calcification by marine organisms

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Academic year: 2017

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Figure 1. Change of di ff erent surface ocean carbonate chemistry parameters under “business- “business-as-usual” climate change scenario SRES A2 with (a) increasing atmospheric pCO 2 and (b) over time
Figure 2. Correlations between calcification related measurements and [CO 2− 3 ] (left panel) or [HCO − 3 ]/[H + ] (right panel)
Figure 3. Ratio of [CO 2 3 − ] and [HCO − 3 ]/[H + ] compared to the ratio of [CO 2 3 − ] and DIC/[H + ].
Figure 4. Relative change of [CO 2− 3 ], Ω CaCO 3 , and [HCO − 3 ]/[H + ] on (a) a pressure gradient, (b) a salinity gradient, and (c) a temperature gradient.
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