Interactive effects of ocean acidification and temperature on two scleractinian corals from Moorea, French Polynesia

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Fast coral reef calcifiers are more sensitive to ocean acidification in short‐term laboratory incubations (2014, methodology): “The thickened tissue of perforate corals may enhance the potential for chemically modified internal microenvironments, which is a further reason to expect this functional group of corals to be more tolerant of external physical conditions (Edmunds et al. 2012).”
The responses of eight coral reef calcifiers to increasing partial pressure of CO2 do not exhibit a tipping point (2013, background): “…measurements establishing the functional relationship between the partial pressure of CO2 (PCO2; and hence, Varag and the saturation state of calcite, Vcalc) and the calcification rates of important functional groups of calcifying taxa on tropical reefs (Erez et al. 2011; Edmunds et al. 2012).”
The physiological and molecular responses of larvae from the reef-building coral Pocillopora damicornis exposed to near-future increases in temperature and pCO2 (2012, background): “Future research needs Currently, a large portion of our knowledge of the effects of ocean acidification on corals comes from relatively short exposure times (reviewed by Edmunds et al. 2012) and single point sampling.”