Global carbon emissions continue to acidify the oceans, motivating growing concern for the ability of coral reefs to maintain net positive calcification rates. Efforts to develop robust relationships between coral reef calcification and carbonate parameters such as aragonite saturation state (Ωarag) aim to facilitate meaningful predictions of how reef calcification will change in the face of ocean acidification. Here, we investigate natural trends in carbonate chemistry of a coral reef flat over diel cycles and relate these trends to benthic carbon fluxes by quantifying net community calcification and net community production. We find that, despite an apparent dependence of calcification on Ωarag seen in a simple pairwise relationship, if the dependence of net calcification on net photosynthesis is accounted for, knowing Ωarag does not add substantial explanatory value. This suggests that, over short timescales, the control of Ωarag on net calcification is weak relative to factors governing net photosynthesis.
Albright R., Benthuysen J., Cantin N., Caldeira K. & Anthony K., in press. Coral reef metabolism and carbon chemistry dynamics of a coral reef flat. Geophysical Research Letters. Article (subscription required).
