Hysteresis between coral reef calcification and the seawater aragonite saturation state
Some predictions of how ocean acidification (OA) will effect coral reefs assume a linear functional relationship between the ambient seawater aragonite saturation state (Ωa) and net ecosystem calcification (NEC). We quantified NEC in a healthy coral reef lagoon in the Great Barrier Reef during different times of the day. Our observations revealed a diel hysteresis pattern in the NEC versus Ωa relationship, with peak NEC rates occurring before the Ωa peak and relatively steady night-time NEC in spite of variable Ωa. Net ecosystem production had stronger correlations with NEC than light, temperature, nutrients, pH, and Ωa. The observed hysteresis may represent an overlooked challenge for predicting the effects of OA on coral reefs. If widespread in coral reefs, the hysteresis could prevent the use of a linear extrapolation to determine critical Ωa threshold levels required to shift coral reefs from a net calcifying to a net dissolving state.
McMahon A., Santos I. R., Cyronak T. & Eyre B. D., in press. Hysteresis between coral reef calcification and the seawater aragonite saturation state. Geophysical Research Letters. Article (subscription required).