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1.
Mar Pollut Bull ; 133: 448-459, 2018 Aug.
Article in English | MEDLINE | ID: mdl-30041336

ABSTRACT

A 3D ecosystem model was used to quantify changes in water quality brought about by salmon aquaculture in the D'Entrecasteaux Channel and Huon Estuary in southeast Tasmania. Macroalgae-based integrated multitrophic aquaculture (IMTA) was simulated and showed that IMTA is capable of reducing the increased chlorophyll concentration attributable to fish farming by up to 10-15% in large areas of the region, during the season of highest production. Kelp farms (Macrocystis pyrifera) recovered between 6 and 11% of the dissolved inorganic nitrogen (DIN) input by salmon aquaculture over a nine month period, with DIN remediation increasing linearly with farm size. Under a ten-fold increase in aquaculture to very high loads, a much lower remediation effect was found for both chlorophyll and DIN. Model results indicate that IMTA could have an important impact on reducing negative effects of finfish aquaculture on water quality providing that stocking rates are not too high.


Subject(s)
Aquaculture/methods , Estuaries , Models, Theoretical , Nitrogen/metabolism , Seaweed/growth & development , Animals , Chlorophyll/metabolism , Ecosystem , Food Chain , Kelp , Salmon , Tasmania
2.
Nat Commun ; 7: 10732, 2016 Feb 23.
Article in English | MEDLINE | ID: mdl-26907171

ABSTRACT

The Great Barrier Reef (GBR) is founded on reef-building corals. Corals build their exoskeleton with aragonite, but ocean acidification is lowering the aragonite saturation state of seawater (Ωa). The downscaling of ocean acidification projections from global to GBR scales requires the set of regional drivers controlling Ωa to be resolved. Here we use a regional coupled circulation-biogeochemical model and observations to estimate the Ωa experienced by the 3,581 reefs of the GBR, and to apportion the contributions of the hydrological cycle, regional hydrodynamics and metabolism on Ωa variability. We find more detail, and a greater range (1.43), than previously compiled coarse maps of Ωa of the region (0.4), or in observations (1.0). Most of the variability in Ωa is due to processes upstream of the reef in question. As a result, future decline in Ωa is likely to be steeper on the GBR than currently projected by the IPCC assessment report.


Subject(s)
Anthozoa/metabolism , Calcium Carbonate/metabolism , Coral Reefs , Seawater/chemistry , Animals , Hydrodynamics , Hydrogen-Ion Concentration , Models, Biological , Models, Chemical , Oceans and Seas
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