Sedimentation from mussel (Perna canaliculus) culture in the Firth of Thames, New Zealand: Impacts on sediment oxygen and nutrient fluxes

Shellfish aquaculture is growing worldwide and previous studies have shown a range of associated environmental impacts. In the Firth of Thames, New Zealand, there are more than 2000 ha of existing and approved farm area with applications pending for approximately another 6000 ha, however, no previous studies have examined the impacts of mussel culture in this region. To determine the impact of a mussel farm (45 ha) in the Firth of Thames we measured sedimentation rates by deploying sediment traps, sediment characteristics by collecting sediment cores and sediment oxygen and nutrient fluxes by deploying benthic chambers in four seasons. Sedimentation under the farm was increased by 106 g m^− 2 d^− 1 compared to the reference site. Similarly sediments under the farm had elevated organic carbon, nitrogen, chlorophyll a and phaeopigment concentrations indicative of the additional organic input due to bivalve biodeposition. Oxygen consumption was higher under the farm compared to a reference site (1.1-2.1×) but this increase was only significant (p < 0.001) in summer when rates reached 3083 μmol m^− 2 h^− 1 under the farm. Ammonia release rates ranged from 80 to 319 μmol m^− 2 h^− 1 and were higher under the farm compared to the reference site in spring (1.8×, non-significant p = 0.588) and autumn (3×, significant p = 0.006) but in summer release rates at the reference site (275 μmol m^− 2 h^− 1) were 1.4× higher than those under the farm. Nitrate fluxes (3.1 to 21.8 μmol m^− 2 h^− 1) were significantly (p = 0.001) higher at the farm site. Oxygen and nutrient fluxes generally demonstrated the typical response to increased organic input due to sedimentation from mussel culture. Unusually low nitrogen release rates in summer may indicate enhanced denitrification under the farm. Benthic regeneration at the reference site could supply 74% of nitrogen required by pelagic primary producers whereas under the farm it could account for 94%. This demonstrates the importance of benthic nutrient regeneration in this region and that mussel culture can lead to a redistribution of nutrients. The farm we studied is small and located in a high-energy environment and impacts from larger farms or in areas where biodeposit dispersal is limited are likely to be even more significant and we suggest that site-specific hydrodynamic and biogeochemical conditions have to be taken into account when planning new mussel farms to prevent excessive modifications of nutrient dynamics.