Biomineralization control related to population density under ocean acidification

Anthropogenic CO₂ is a major driver of current environmental change in most ecosystems¹, and the related ocean acidification (OA) is threatening marine biota². With increasing pCO₂, calcification rates of several species decrease³, although cases of up-regulation are observed⁴. Here, we show that biological control over mineralization relates to species abundance along a natural pH gradient. As pCO₂ increased, the mineralogy of a scleractinian coral (Balanophyllia europaea) and a mollusc (Vermetus triqueter) did not change. In contrast, two calcifying algae (Padina pavonica and Acetabularia acetabulum) reduced and changed mineralization with increasing pCO₂, from aragonite to the less soluble calcium sulphates and whewellite, respectively. As pCO₂ increased, the coral and mollusc abundance was severely reduced, with both species disappearing at pH < 7.8. Conversely, the two calcifying and a non-calcifying algae (Lobophora variegata) showed less severe or no reductions with increasing pCO₂, and were all found at the lowest pH site. The mineralization response to decreasing pH suggests a link with the degree of control over the biomineralization process by the organism, as only species with lower control managed to thrive in the lowest pH.