Dissecting the impact of CO 2 and pH on the mechanisms of photosynthesis and calcification in the coccolithophore Emiliania huxleyi

Summary Coccolithophores are important calcifying phytoplankton predicted to be impacted by changes in ocean carbonate chemistry caused by the absorption of anthropogenic CO 2 . However, it is difficult to disentangle the effects of the simultaneously changing carbonate system parameters ( CO 2 , bicarbonate, carbonate and protons) on the physiological responses to elevated CO 2 . Here, we adopted a multifactorial approach at constant pH or CO 2 whilst varying dissolved inorganic carbon (DIC) to determine physiological and transcriptional responses to individual carbonate system parameters. We show that Emiliania huxleyi is sensitive to low CO 2 (growth and photosynthesis) and low bicarbonate (calcification) as well as low pH beyond a limited tolerance range, but is much less sensitive to elevated CO 2 and bicarbonate. Multiple up‐regulated genes at low DIC bear the hallmarks of a carbon‐concentrating mechanism (CCM) that is responsive to CO 2 and bicarbonate but not to pH . Emiliania huxleyi appears to have evolved mechanisms to respond to limiting rather than elevated CO 2 . Calcification does not function as a CCM , but is inhibited at low DIC to allow the redistribution of DIC from calcification to photosynthesis. The presented data provides a significant step in understanding how E. huxleyi will respond to changing carbonate chemistry at a cellular level.