Optimising reef-scale CO2 removal by seaweed to buffer ocean acidification
The equilibration of rising atmospheric CO 2 with the ocean is lowering pH in tropical waters by about 0.01 every decade. Coral reefs and the ecosystems they support are regarded as one of the most vulnerable ecosystems to ocean acidification, threatening their long-term viability. In response to th...
| Published in: | Environmental Research Letters |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Institute of Physics Publishing Ltd.
2016
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| Subjects: | |
| Online Access: | https://doi.org/10.1088/1748-9326/11/3/034023 http://ecite.utas.edu.au/118105 |
| Summary: | The equilibration of rising atmospheric CO 2 with the ocean is lowering pH in tropical waters by about 0.01 every decade. Coral reefs and the ecosystems they support are regarded as one of the most vulnerable ecosystems to ocean acidification, threatening their long-term viability. In response to this threat, different strategies for buffering the impact of ocean acidification have been proposed. As the pH experienced by individual corals on a natural reef system depends on many processes over different time scales, the efficacy of these buffering strategies remains largely unknown. Here we assess the feasibility and potential efficacy of a reef-scale (a few kilometers) carbon removal strategy, through the addition of seaweed (fleshy multicellular algae) farms within the Great Barrier Reef at the Heron Island reef. First, using diagnostic time-dependent age tracers in a hydrodynamic model, we determine the optimal location and size of the seaweed farm. Secondly, we analytically calculate the optimal density of the seaweed and harvesting strategy, finding, for the seaweed growth parameters used, a biomass of 42gNm -2 with a harvesting rate of up 3.2gNm -2 d -1 maximises the carbon sequestration and removal. Numerical experiments show that an optimally located 1.9km 2 farm and optimally harvested seaweed (removing biomass above 42gNm -2 every 7d) increased aragonite saturation by 0.1 over 24km 2 of the Heron Island reef. Thus, the most effective seaweed farm can only delay the impacts of global ocean acidification at the reef scale by 7-21 years, depending on future global carbon emissions. Our results highlight that only a kilometer-scale farm can partially mitigate global ocean acidification for a particular reef. |
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