H+-driven increase in CO2 uptake and decrease in HCO3− uptake explain coccolithophores' acclimation responses to ocean acidification

Recent ocean acidification (OA) studies revealed that seawater [H+] rather than [CO2] or [HCO3-] regulate short-term responses in carbon fluxes of Emiliania huxleyi. Here, we investigated whether acclimation to altered carbonate chemistry modulates this regulation pattern and how the carbon supply f... View More