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8m survey - spatial patterns Figures 2.7(i-viii) present the interpolated density maps of the non-randomly distributed species from the 8m survey while Figures 2.8(i-v) display the significant correlograms. The distance classes 1-6 for these correlograms represent inter-sample distances of 0-8m, 8-12m, 12-16m, 16-20m, 20-24m and 24-28m, respectively. The density maps suggest that 2 species appeared to form patches less than 8m 2 (E. cf flava and G. duebeni; both of which produced non-significant correlograms) while the other species either formed patches between 8-24m 2 (C. capitata, S. martinensis and L. conchilega) or patches of various sizes (P. elegans). The correlograms do not appear to support the density plots for all species. For example, while the density plot for L. conchilega (Figure 2.7(iii)) suggests a patch of approximately 20m 2 was present, the correlogram (Figure 2.8(ii)) implies a patch size of only 8-12m2. Areas of increased densities of some species, C. edule and M. balthica for example, were located at the edges of the 56x56m survey area and therefore it is not possible to give an indication of patch sizes from the density plots and one must be cautious when drawing conclusions from their correlograms. Figures 2.7(i-xii) support the results of the correlation analyses (Table 2.5). The non- significant correlations between P. elegans and most of the other species are clearly defended by the maps since high density patches of most species do not seem to have been spatially correlated within the survey area. Furthermore, the significant positive correlation between P. elegans and M. balthica is vindicated by their contour plots, although the locations of moderate M. balthica densities as well as high densities have to be observed to see this. Figures 2.7(ix-xii) suggest that the 4 measured sediment variables were spatially correlated with each other to a certain extent. Increased levels of organic carbon and silt/clay, together with Md 0 and sorting coefficient were mainly found at the top of the 56x56m grid, although high levels of organic carbon content and Md (I) were also found in other small areas. The significant correlograms produced for the distribution of these variables (except % organic content) in Figures 2.8(vi-viii) indicate patch sizes of approximately 20-24m 2. However, since these were located at the edges of 42

the survey area, one must be cautious. The significant positive correlations between P. elegans abundance and the levels % silt/clay, % organics and sorting coefficient are supported by the contour plots. 40m survey - spatial patterns Figures 2.9(i-xi) present the contour maps of the non-randomly distributed species from the 40m survey and Figures 2.10(i-ix) display the significant correlograms. The distance classes 1-6 for these correlograms represent inter-sample distances 0-40m, 40-60m, 60-80m, 80-100m, 100-120m and 120-140m respectively. These Figures suggest that P. elegans, E. cfflava, M. balthica and C. edule formed patches between 40-60m2. Some species, S. martinensis, A. marina, L. conchilega and B. sarsi for example, formed patches which were located at the edge of the survey area and so it is difficult to estimate their patch sizes. Although not formally tested, none of the species appeared to form patches which were spatially correlated with any other species. The significant positive correlation between P. elegans and M. balthica (Table 2.5) is not strongly supported by the contour plots, although their patch sizes were similar they were not spatially correlated. Figure 2.9(xii-xv) show that the sediment variables appear to have had increased levels approximately across the middle region of the survey area. The correlograms indicated that these patches were approximately 80-100m2. The significant positive correlations between P. elegans and % organic carbon, % silt/clay and sorting coefficient (Table 2.5) were better supported by the maps for the 40m survey than they were for the 8m survey with high levels of these variables occurring at approximately the same areas as the P. elegans patches. The contour plots support the significant positive correlations between P. elegans and % silt/clay, % organics and sorting coefficient and suggest that no other species was positively correlated with them. 43

8m survey - spatial patterns<br />

Figures 2.7(i-viii) present the interpolated density maps of the non-randomly<br />

distributed species from the 8m survey while Figures 2.8(i-v) display the significant<br />

correlograms. The distance classes 1-6 for these correlograms represent inter-sample<br />

distances of 0-8m, 8-12m, 12-16m, 16-20m, 20-24m and 24-28m, respectively. The<br />

density maps suggest that 2 species appeared to form patches less than 8m 2 (E. cf<br />

flava and G. duebeni; both of which produced non-significant correlograms) while the<br />

other species either formed patches between 8-24m 2 (C. capitata, S. martinensis and<br />

L. conchilega) or patches of various sizes (P. elegans). The correlograms do not<br />

appear to support the density plots for all species. For example, while the density plot<br />

for L. conchilega (Figure 2.7(iii)) suggests a patch of approximately 20m 2 was<br />

present, the correlogram (Figure 2.8(ii)) implies a patch size of only 8-12m2.<br />

Areas of increased densities of some species, C. edule and M. balthica for example,<br />

were located at the edges of the 56x56m survey area and therefore it is not possible to<br />

give an indication of patch sizes from the density plots and one must be cautious when<br />

drawing conclusions from their correlograms.<br />

Figures 2.7(i-xii) support the results of the correlation analyses (Table 2.5). The non-<br />

significant correlations between P. elegans and most of the other species are clearly<br />

defended by the maps since high density patches of most species do not seem to have<br />

been spatially correlated within the survey area. Furthermore, the significant positive<br />

correlation between P. elegans and M. balthica is vindicated by their contour plots,<br />

although the locations of moderate M. balthica densities as well as high densities have<br />

to be observed to see this.<br />

Figures 2.7(ix-xii) suggest that the 4 measured sediment variables were spatially<br />

correlated with each other to a certain extent. Increased levels of organic carbon and<br />

silt/clay, together with Md 0 and sorting coefficient were mainly found at the top of<br />

the 56x56m grid, although high levels of organic carbon content and Md (I) were also<br />

found in other small areas. The significant correlograms produced for the distribution<br />

of these variables (except % organic content) in Figures 2.8(vi-viii) indicate patch<br />

sizes of approximately 20-24m 2. However, since these were located at the edges of<br />

42

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