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lack of apparent correlation must be treated with caution due to different sampling<br />

regimes for the sediments and fauna. There were significant positive correlations of<br />

P. elegans density with high levels of % organic content, % silt/clay, Md 4) and sorting<br />

coefficient in the 8m and 40m surveys. Tube-building polychaetes have been shown<br />

to affect these sediment properties (Noji, 1994; Morgan, 1997) and, therefore, the<br />

sediments may not have been responsible for the generation of P. elegans patchiness<br />

but vice versa. This will be discussed further for P. elegans on Drum Sands in<br />

Chapter 8.<br />

Drum Sands is a relatively high energy sandflat with frequent sediment movement<br />

(pers. obs.) and macroalgal mats are capable of forming during the summer (summer<br />

of 1996 for example). Therefore, the mosaic of species patches observed in this study<br />

may have been generated by disturbances. The role of disturbance in structuring<br />

macrobenthic populations on Drum Sands will be addressed in Chapters 4, 5 and 6.<br />

This study revealed spatial patterns of many common intertidal macrobenthic species<br />

found in European sandflats at various scales using regular grid-sampling techniques.<br />

This sampling design is simple to carry out, is capable of covering a range of scales<br />

and spatial patterns can be easily detected and displayed. This study revealed the<br />

presence of patches of 1-2m2 in many species.<br />

The effect of a dominant biogenic species on the spatial patterns of other<br />

invertebrate species on an intertidal sandflat.<br />

One of the most conspicuous biological features on an intertidal sandflat are the<br />

mounds or plateaus formed by high densities of tube-building polychaetes. On Drum<br />

Sands, P. elegans forms areas of smooth, raised sediment, approximately 1-1.5m2,<br />

within an otherwise wave-rippled sandflat. These areas are characterised by increased<br />

densities of P. elegans. Many studies have reported different sediment characteristics<br />

within dense arrays of tube-building polychaetes (Dupont, 1975; Featherstone and<br />

Risk, 1977; Noji, 1994; Morgan, 1997; Chapter 8) and these have resulted in different<br />

faunal assemblages (Sanders et al., 1962; Fager, 1964; Ragnarsson, 1996; Chapter 8).<br />

None of these studies, however, have assessed to what extent the spatial pattern<br />

56

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