Flow of organic carbon (OC) and nitrogen through a sea cage trout farm was calculated on the basis of detailed studies of the farming operation, water circulation, OC and nutrient transport and recycling processes in sediment. A third of the OC and nitrogen provided by fish food was incorporated into fish biomass, which is more than has been found in previous studies. Most OC input was respired by the fish (52 to 70%), and ~63% of the associated nitrogen was lost as dissolved inorganic nitrogen (DIN), potentially stimulating pelagic primary production. Approx. 6% of carbon and 5% of nitrogen derived from fish food settled on the seabed, where it was either mineralized or accumulated in the sediment. Based on transect measurements of diagenetic activity, the farm footprint was found to cover an area ~10 times the farm area. OC mineralization in the sediment increased linearly with increasing food input; the divergence between carbon efflux and oxygen uptake in sediment likewise increased with increasing food input, reflecting an increasing level of sediment reduction. Directly below the farm, the dissolved organic carbon (DOC) efflux was high (on average 53% of dissolved inorganic carbon efflux), indicating that DOC efflux is an important pathway for benthic carbon release below aquaculture farms. Overall, microbial processes removed 56 and 38% of OC and nitrogen, respectively, that settled to the seabed. During a 39 d break in farming activity, due to the combined effect of mineralization and resuspension of surface sediment, sediment conditions improved considerably.
KEY WORDS:Fish farming · Sediment · Organic enrichment · Nutrient enrichment · Organic matter mineralization · Carbon budget · Sedimentation · Benthic recovery
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 431: [223][224][225][226][227][228][229][230][231][232][233][234][235][236][237][238][239][240][241] 2011 2003, Islam 2005, Pitta et al. 2006), but increased nutrient loading from fish farming may cause such effects on a regional scale (Karakassis et al. 2005). Pelagic effects are highly dependent on hydrographic and nutrient status in the farming area.Models have shown little effect on primary production in a Norwegian fjord (Skogen et al. 2009). However in oligotrophic waters in southern Tasmania, theoretical models indicate significant impact on primary production, especially during summer and autumn when surface waters are otherwise nutrientdepleted (Wild-Allen et al. 2010).Particulate waste products in the form of fish food and faeces quickly sink to the seafloor (Cromey et al. 2002). The sedimentation of organic carbon (OC) below fish farms has been found to be from 4 to 27 times higher than at unaffected sites, declining rapidly with distance from the farm (Hall et al. 1990, Chamberlain & Stucchi 2007, Holmer et al. 2007, Kutti et al. 2007). The high deposition of waste particles in the sediment near aquaculture operations stimulates metabolic activity in the sediment and hence...