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

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In a hierarchical framework for the Scotian Shelf, R<strong>of</strong>f et al. (2003) classified pelagicbenthic<br />

seascapes by comb<strong>in</strong><strong>in</strong>g a classification <strong>of</strong> benthic seascapes (based on temperature,<br />

bottom temperature, exposure, slope <strong>and</strong> sediment types), with a classification <strong>of</strong> pelagic<br />

seascapes (based on water temperature, depth classes <strong>and</strong> stratification classes) (Figure 2A).<br />

These layers were then used to calculate a derivative map to show relative seascape<br />

heterogeneity (Figure 2B) <strong>in</strong> order to identify areas with high heterogeneity as potential focal<br />

areas for mar<strong>in</strong>e conservation. Further utility can be ga<strong>in</strong>ed by quantify<strong>in</strong>g the seascape<br />

composition <strong>of</strong> exist<strong>in</strong>g or proposed mar<strong>in</strong>e protected areas, for l<strong>in</strong>k<strong>in</strong>g to key faunal populations<br />

or behavioral patterns such as migratory corridors for megafauna <strong>and</strong> addresses questions about<br />

habitat use <strong>and</strong> preferences at scales that may be more mean<strong>in</strong>gful to the highly mobile<br />

organisms (Box 3). Furthermore, such <strong>in</strong>formation can help underst<strong>and</strong> mar<strong>in</strong>e species<br />

distributions <strong>and</strong> characterize essential fish habitat <strong>in</strong>clud<strong>in</strong>g nursery <strong>and</strong> spawn<strong>in</strong>g areas.<br />

Us<strong>in</strong>g similar organizational frameworks, seascapes have been classified <strong>and</strong> del<strong>in</strong>eated <strong>in</strong><br />

Australia (Harris 2007); the Gulf <strong>of</strong> Ma<strong>in</strong>e (CLF/WWF 2006); the Irish Sea (V<strong>in</strong>cent et al.<br />

2004), <strong>and</strong> the Baltic Sea (Al-Hamdani et al. 2007). In the UK, four ma<strong>in</strong> categories <strong>of</strong> seascape<br />

types (or mar<strong>in</strong>e l<strong>and</strong>scapes) have been def<strong>in</strong>ed (Connor et al. 2006). These are:<br />

1.) Coastal (physiographic) features, such as fjords <strong>and</strong> estuaries, where the seabed <strong>and</strong> water<br />

body are closely <strong>in</strong>terl<strong>in</strong>ked.<br />

2.) Topographic <strong>and</strong> bed-form features, occurr<strong>in</strong>g away from the coast <strong>and</strong> form<strong>in</strong>g dist<strong>in</strong>ct<br />

raised or deepened features <strong>of</strong> the seabed at various scales;<br />

3.) Broad-scale seabed habitats, def<strong>in</strong>ed through model<strong>in</strong>g <strong>and</strong> broadly equivalent to EUNIS<br />

higher level habitat classes;<br />

17

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