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Aquatic Environment and Biodiversity Annual Review 2012

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AEBAR <strong>2012</strong>: Ecosystem effects: L<strong>and</strong>-based effects<br />

duration, frequency <strong>and</strong> magnitude of exposure, temperature, <strong>and</strong> other environmental variables<br />

(Servizi <strong>and</strong> Martens 1992).<br />

Increased nutrient addition to the aquatic environment can initially increase production, but with<br />

increasing nutrients there is an increasing likelihood of harmful algal blooms <strong>and</strong> cascades of effects<br />

damaging to most communities above the level of the plankton (Kennish 2002; Heisler et al. 2008).<br />

This excess of nutrients is termed eutrophication. Eutrophication can stimulate phytoplankton growth<br />

which can decrease the light availability <strong>and</strong> subsequently lead to losses in benthic production from<br />

seagrass, microalgae or macroalgae <strong>and</strong> their associated animal communities. Algal blooms then die<br />

<strong>and</strong> their decay depletes oxygen <strong>and</strong> blankets the seafloor. The lack of oxygen in the bed <strong>and</strong> water<br />

column can lead to losses of finfish <strong>and</strong> benthic communities. These effects are likely to be location<br />

specific <strong>and</strong> are influenced by a number of factors including: water transparency, distribution of<br />

vascular plants <strong>and</strong> biomass of macroalgae, sediment biogeochemistry <strong>and</strong> nutrient cycling, nutrient<br />

ratios <strong>and</strong> their regulation of phytoplankton community composition, frequency of toxic/harmful algal<br />

blooms, habitat quality for metazoans, reproduction/growth/survival of pelagic <strong>and</strong> benthic<br />

invertebrates, <strong>and</strong> subtle changes such as shifts in the seasonality of ecosystems (Cloern 2001). These<br />

effects of eutrophication abound in the literature, for example, the formation of dead (or anoxic) zones<br />

is exacerbated by eutrophication, although oceanographic conditions also play a key role (Diaz <strong>and</strong><br />

Rosenberg 2008). Dead zones have now been reported from more than 400 systems, affecting a total<br />

area of more than 245,000 square kilometres (Diaz <strong>and</strong> Rosenberg 2008). This includes anoxic events<br />

from New Zeal<strong>and</strong> in coastal north-eastern New Zeal<strong>and</strong> <strong>and</strong> Stewart Isl<strong>and</strong> (Taylor et al. 1985,<br />

Morrissey 2000).<br />

Other pollutants such as heavy metals <strong>and</strong> organic chemicals can have severe effects, but are more<br />

localised in extent than sediment or nutrient pollution (Castro <strong>and</strong> Huber 2003, Kennish 2002).<br />

Fortunately the concentration of these pollutants in most New Zeal<strong>and</strong> aquatic environments is<br />

relatively low, with a few known exceptions. Examples of this include naturally elevated levels of<br />

arsenic in Northl<strong>and</strong> 27 , Cadmium levels in Foveaux Strait oysters (Frew et al. 1996) <strong>and</strong> levels of<br />

Nickel <strong>and</strong> chromium within the Motueka river plume in Tasman Bay (Forrest et al. 2007). The<br />

Cadmium levels have caused market access issues for Foveaux Strait Oysters. Some<br />

anthropogenically generated pollutants such as copper, lead, zinc <strong>and</strong> PCBs are high in localised<br />

hotspots within urban watersheds. In the Auckl<strong>and</strong> region these hotspots tend to be in muddy<br />

estuarine sites <strong>and</strong> tidal creeks that receive runoff from older urban catchments 28 . There is a lack of<br />

knowledge on the impacts of these pollutants upon fisheries.<br />

Climate change is likely to interact with the effect of l<strong>and</strong>-based impacts as the main delivery of l<strong>and</strong>based<br />

influences is through rainfall <strong>and</strong> subsequent freshwater flows. Global climate change<br />

projections include changes in the amount <strong>and</strong> regional distribution of rainfall over New Zeal<strong>and</strong><br />

(IPCC 2007). More regional predictions include increasing frequency of heavy rainfall events over<br />

New Zeal<strong>and</strong> (Whetton et al. 1996). This is likely to exacerbate the impact of some l<strong>and</strong>-based<br />

influences as delivery peaks at times of high rainfall, e.g. sediment delivery (Morrison et al. 2009).<br />

Physical alterations of the coast are generally, but not exclusively (i.e. wetl<strong>and</strong> reclamation for<br />

agriculture), concentrated around urban areas <strong>and</strong> can have a number of consequences on the marine<br />

environment (Bulleri <strong>and</strong> Chapman 2010). Changes in diversity, habitat fragmentation or loss <strong>and</strong><br />

increased invasion susceptibility have all been identified as consequences of physical alteration. The<br />

effects of physical alterations upon fisheries remain largely unquantified; however the habitat loss or<br />

alteration portion of physical alterations will be dealt with under the habitats of particular significance<br />

for fisheries management (HPSFM) section.<br />

27 Accessible on the www.os2020.org.nz website.<br />

28 Available from the State of the Auckl<strong>and</strong> Region report 2010, Chapter 4.4 Marine, at<br />

http://www.arc.govt.nz/albany/index.cfm?FD6A3403-145E-173C-986A-A0E3C199B8C5<br />

219

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