Plasticity of coral physiology under ocean acidification

Coral reefs are oases of life in the oceans, harbouring more than a quarter of all marine species. These vibrant ecosystems are founded on reef structures that are built by the CaCO3 skeletons of “stony” scleractinian corals. While productive and biodiverse, coral reef ecosystems are sensitive to many elements of global environmental change, including “ocean acidification” which impairs the capacity of corals to build their skeletons by calcification [1]. Ocean acidification is driven by seawater-uptake of rising atmospheric pCO2 and involves changes in seawater carbonate chemistry associated with decreasing seawater pH. Meta-analysis of published data suggests that ocean acidification will cause a worrying decline in reef coral calcification rates by the end of the 21st century [2], but exactly how and why ocean acidification affects coral calcification isn’t well understood at a physiological level. Improving our understanding of the effects of ocean acidification on corals hinges on achieving a mechanistic understanding of the coral calcification process, yet relatively few cellular-level studies have addressed this topic [3]. Corals are diploblastic animals, characterised by a relatively thin layer of tissue overlying a complex CaCO3 skeleton. The calcifying cell layer that deposits the skeleton regulates ion supply to an internal calcifying fluid where the skeleton forms, and also produces an organic matrix which is incorporated into the skeleton’s structure (Figure 1). Ions used for calcification arrive in the calcifying fluid via a paracellular pathway characterised by septate junctions, and via transcellular pathways involving ion transporters and channels in the calcifying cells. Certain of these ion transporters act to regulate conditions in the calcifying fluid, notably by elevating pH and boosting dissolved inorganic carbon (DIC) concentrations, to promote the precipitation of CaCO3 [4]. To better understand how ocean acidification affects coral calcification, we need to look for clues in both the coral tissues and the skeleton itself. In our recent work, published in Nature Communications [5], we carried out a controlled laboratory study on a model stony coral species, Stylophora pistillata, which can tolerate longterm exposure to low seawater pH. After more than a year at a low seawater pH that should favour dissolution of CaCO3, our corals continued to calcify, albeit at slower rates than controls. Interestingly however, the coral skeletons that formed at lower pH were significantly more porous and less dense than their counterparts at normal seawater pH. Our analyses ruled-out the possibility that physicochemical dissolution of the skeleton by low seawater pH had caused the observed increases in porosity. Indeed, pH measurements by confocal microscopy showed that the calcifying cell layer regulated calcifying fluid pH to elevated values that should favour CaCO3 precipitation, not dissolution. Rather, the explanation underlying why coral skeletons became more porous lay in a biologicallycontrolled shift in the coral skeleton’s architecture, pointing to morphological plasticity of S. pistillata under seawater acidification. These findings raise numerous questions about the molecular and cellular mechanisms controlling calcification, and we are currently employing genomic, transcriptomic and post-genomic approaches to get insight into the cellular physiology of corals under ocean acidification. For example how do corals control the chemistry of the calcifying fluid when the pH and carbonate chemistry of the surrounding seawater changes? Are genes coding for transporters involved in pH regulation responsive to acidification and/or do we see changes in transporter activity? Furthermore, separation of the calcifying fluid from the external seawater relies Editorial