Articles | Volume 10, issue 7
Biogeosciences, 10, 4897–4909, 2013

Special issue: The ocean in a high-CO2 world III

Biogeosciences, 10, 4897–4909, 2013

Research article 19 Jul 2013

Research article | 19 Jul 2013

Benthic buffers and boosters of ocean acidification on coral reefs

K. R. N. Anthony3,1, G. Diaz-Pulido2, N. Verlinden3, B. Tilbrook4, and A. J. Andersson5 K. R. N. Anthony et al.
  • 1Australian Institute of Marine Science, Townsville, Qld 4810 Australia
  • 2Griffith School of Environment and Australian Rivers Institute – Coasts & Estuaries, Nathan Campus, Griffith University, Nathan, Queensland 4111, Australia
  • 3Biological Sciences, The University of Queensland, St Lucia, Q4072, Australia
  • 4Marine and Atmospheric Research, CSIRO, Hobart, Tasmania 7000, Australia
  • 5Scripps Institution of Oceanography, University of California San Diego, 9500 Gilman Drive, La Jolla, CA 92093-0202, USA

Abstract. Ocean acidification is a threat to marine ecosystems globally. In shallow-water systems, however, ocean acidification can be masked by benthic carbon fluxes, depending on community composition, seawater residence time, and the magnitude and balance of net community production (NCP) and calcification (NCC). Here, we examine how six benthic groups from a coral reef environment on Heron Reef (Great Barrier Reef, Australia) contribute to changes in the seawater aragonite saturation state (Ωa). Results of flume studies using intact reef habitats (1.2 m by 0.4 m), showed a hierarchy of responses across groups, depending on CO2 level, time of day and water flow. At low CO2 (350–450 μatm), macroalgae (Chnoospora implexa), turfs and sand elevated Ωa of the flume water by around 0.10 to 1.20 h−1 – normalised to contributions from 1 m2 of benthos to a 1 m deep water column. The rate of Ωa increase in these groups was doubled under acidification (560–700 μatm) and high flow (35 compared to 8 cm s−1). In contrast, branching corals (Acropora aspera) increased Ωa by 0.25 h−1 at ambient CO2 (350–450 μatm) during the day, but reduced Ωa under acidification and high flow. Nighttime changes in Ωa by corals were highly negative (0.6–0.8 h−1) and exacerbated by acidification. Calcifying macroalgae (Halimeda spp.) raised Ωa by day (by around 0.13 h−1), but lowered Ωa by a similar or higher amount at night. Analyses of carbon flux contributions from benthic communities with four different compositions to the reef water carbon chemistry across Heron Reef flat and lagoon indicated that the net lowering of Ωa by coral-dominated areas can to some extent be countered by long water-residence times in neighbouring areas dominated by turfs, macroalgae and carbonate sand.

Final-revised paper