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Application 124771 - Ministry of Fisheries

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MAY 2012 REPORT NO. 2134 | CAWTHRON INSTITUTE<br />

26<br />

enrichment, together with the accumulation <strong>of</strong> debris beneath coastal mussel farms,<br />

increases both the food available for scavengers and habitat heterogeneity. This in<br />

turn can lead to significant increases in the diversity <strong>of</strong> infauna and epibiota (Inglis et<br />

al. 2000, Wong & O’Shea 2011). However, in shell- and sand-dominated benthic<br />

habitats, shifts in epibiota feeding and living on mussels and changes to enrichment<br />

tolerant infauna taxa can occur (Keeley et al. 2010).<br />

Clumps <strong>of</strong> mussels beneath the reference farm sites had been colonised by a range<br />

<strong>of</strong> organisms and provided a reef-like habitat for a variety <strong>of</strong> small fishes and mobile<br />

fauna. Elsewhere, biodeposits beneath mussel farms have been are known to attract<br />

large numbers <strong>of</strong> predatory fish, seastars, crabs, sea urchins and other echinoderms<br />

(Mattsson & Lindén 1983, Kaspar et al. 1985, Cole & Grange 1996). Furthermore,<br />

exclusion <strong>of</strong> trawling by the farm infrastructure also means that species which are<br />

regularly harvested or damaged by trawling in open areas <strong>of</strong> seabed, such as scallops<br />

(Pecten novaezelandiae) and horse mussels (Atrina zealandica), are occasionally<br />

abundant beneath the farms. The extent to which protection for these species is<br />

occurring beneath Coromandel mussel farms however is unknown; scallops were rare<br />

at all sites and occasional beds <strong>of</strong> horse mussels were observed beneath three<br />

reference farm sites and at four control sites.<br />

In general, mussel farming is unlikely to result in irreversible ecological effects<br />

(Forrest 1995, Keeley et al. 2010). Farms placed over mud / silt habitat, as were the<br />

majority <strong>of</strong> farm sites in this study, would likely return to pre-farm conditions within one<br />

to two years <strong>of</strong> farm removal. However, this would depend on the level <strong>of</strong> shell cover<br />

at each site. In extreme cases, banks <strong>of</strong> sediment and shell material up to 2 m high<br />

have been observed beneath Coromandel mussel farms (e.g. C<strong>of</strong>fey 2001), but the<br />

accumulation and extent <strong>of</strong> shell material depends on processes such as water<br />

movement and bioturbation which tends to disperse and modify deposited materials<br />

(Morrisey et al. 2000). Overall, the enrichment effects <strong>of</strong> inshore mussel farms on the<br />

benthic environment in the Coromandel were minor; while shell deposition and related<br />

effects on diversity and abundance <strong>of</strong> epibiota, while considerable, were not<br />

necessarily negative (Keeley et al. 2010).<br />

6.2. Water column effects<br />

The water column properties measured at reference farm sites and control sites were<br />

broadly similar and no clear patterns in differences were observed. Water column<br />

turbidity in the top 1-2 m <strong>of</strong> the water column was similar between farm and control<br />

sites, but farm sites were less turbid between 3-5 m and below 7 m depth. This lower<br />

turbidity may be attributed to the filtering effect <strong>of</strong> the mussels on the farm droppers,<br />

but this effect will depend greatly on the state <strong>of</strong> the tide and the water velocities at<br />

each site, which are known to influence the residence time <strong>of</strong> water passing through<br />

mussel farms (Plew 2011).

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