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1 1.10 Application of estuarine and coastal classifications in marine ...

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Government Department <strong>of</strong> Climate Change <strong>in</strong> order to support an <strong>in</strong>itial vulnerability<br />

assessment for the whole <strong>of</strong> the Australian coastl<strong>in</strong>e, <strong>and</strong> to contribute to the development <strong>of</strong><br />

mar<strong>in</strong>e ‘ecoregions’ or bioregional subregions. Before NISB, there was no consistently-classified<br />

habitat mapp<strong>in</strong>g <strong>of</strong> the entire Australian coastl<strong>in</strong>e, except at very broad scales that were not <strong>of</strong><br />

practical use <strong>in</strong> a <strong>coastal</strong> vulnerability assessment. The NISB habitat classes <strong>in</strong>clude: mangroves,<br />

saltmarsh, seagrass, macroalgae, coral reef, rock-dom<strong>in</strong>ated, sediment-dom<strong>in</strong>ated <strong>and</strong> filter<br />

feeders (such as sponges). These habitats occur between the approximate position <strong>of</strong> the highest<br />

astronomical tide mark <strong>and</strong> the location <strong>of</strong> the outer limit <strong>of</strong> the photic benthic zone (usually at<br />

the 50 to 70 meter depth contour). High spatial resolution polygons with thematic attributes<br />

based on NISB are also available <strong>in</strong> Ozcoasts, together with national, state <strong>and</strong> regional summary<br />

maps for each habitat (Figure 5). The NISB Classification Scheme has been adopted as a<br />

st<strong>and</strong>ard by S<strong>in</strong>clair Knight Mertz, one <strong>of</strong> Australia’s largest environmental consult<strong>in</strong>g<br />

companies. In addition, it will be used by the CSIRO climate adaptation branch <strong>in</strong> the <strong>coastal</strong><br />

version <strong>of</strong> their Impacts <strong>of</strong> Climate Change on Australian Mar<strong>in</strong>e Life studies (Hobday et al.,<br />

2006).<br />

Coastal environments can also be classified accord<strong>in</strong>g to levels <strong>of</strong> physical disturbance<br />

from extreme storm events that mobilize <strong>and</strong> transport sediments across the shelf, a characteristic<br />

feature <strong>of</strong> many shelf ecosystems. Research has shown that storms <strong>and</strong> strong currents can cause<br />

widespread sediment erosion <strong>and</strong> deposition, some <strong>of</strong> which can bury or remove seagrasses <strong>and</strong><br />

can cause extensive physical damage to coral reefs (Puot<strong>in</strong>en 2007). Harris (unpublished<br />

manuscript) proposes the development <strong>of</strong> a framework for classify<strong>in</strong>g Australia’s cont<strong>in</strong>ental<br />

shelf relative to disturbance based on a central tenet that biodiversity will be highest at<br />

<strong>in</strong>termediate levels <strong>of</strong> disturbance follow<strong>in</strong>g Connell’s Intermediate Disturbance Hypothesis.<br />

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