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Sediment water, organic and silt/clay contents - There were no statistical differences between patches and non-patches for water content (Figure 8.12(i)), while for the % silt/clay and % organic contents, significantly higher values were found in P. elegans patches throughout the sampling period from April 1997 to August 1998 (Figures 8.12(ii-iii)). Silt/clay content remained at approximately 5% in non-patch samples while it rose to 14.2% ± 0.64% in August 1997 in patches, then slowly decreased to 9.58% ± 0.95% in August 1998. A decreasing trend was observed for the organic content in patches from 3.6% ± 0.19% at the start of the sampling period to 2.4% ± 0.08% in August 1998, although this was always significantly higher than in non-patch sediments, which was consistently around 2%. Redox potentials - Whilst sedimentary variables such as the silt/clay and organic contents showed clear differences between patch and non-patch sediments, the results of the redox measurements were more equivocal. Figures 8.13(i-iii) show that the redox profiles of the two plot types were very similar between April and December 1997. However, during August 1998, the sediments at 1 cm and 2cm depths in P. elegans patches were significantly more reducing than those in non-patch areas, while at the 4cm depth, they were significantly less reducing than non-patch sediments (Figure 8.13(iv)). 223
8 2 1„z 25.5 — 25 — 24.5 — 24 — 23.5 — 23 — 22.5 — 22 — 21.5 — 21 2 1 16 — 14 — 12 — 10 — 8 — 6 — 4 — 3 .5 — 3 — 2 .5 — 2 — 1.5 — — 0.5 — (i) Water content (ii) Silt/clay content 111 Patch Non-patch April August December August April ** August (iii) Organic content * * * December ** E Patch 0 Non-patch August • Patch Non-patch April August December August Figures 8.12(i-iii) : Mean sediment results (±S.E.Mean, n=6) showing the results of statistical tests between patch and non-patch values. ** Denotes a statistical difference between patch and non-patch means using Two-sample t-test at 0.01 level of significance and *** at 0.001. 224
- Page 190 and 191: METHODS Experimental design - A pre
- Page 192 and 193: study. These individuals would not
- Page 194 and 195: RESULTS Pilot survey - The pilot su
- Page 196 and 197: Transect survey - Micro-scale patte
- Page 198 and 199: Month v:m ratio pattern Id pattern
- Page 200 and 201: (i) March 1997, replicate 1 -iAlmiA
- Page 202 and 203: (xix) October 1997, replicate 1 (ra
- Page 204 and 205: The new recruits were only sufficie
- Page 206 and 207: The results of correlation analyses
- Page 208 and 209: cf.) . crt N ,—, Cr) C,1 ,—, Cr
- Page 210 and 211: 1.2 -0.4 "a 0.8 > (i) % Water conte
- Page 212 and 213: examine the micro-scale spatial pat
- Page 214 and 215: Invertebrate larvae, those of polyc
- Page 216 and 217: laboratory observations are needed
- Page 218 and 219: CHAPTER 8 THE FAUNAL COMMUNITIES OF
- Page 220 and 221: Other theories have been postulated
- Page 222 and 223: RESULTS Univariate analysis of spec
- Page 224 and 225: -T. g 80 g 50 40 30 20 10 (i) Adult
- Page 226 and 227: in significant differences in size
- Page 228 and 229: 8.2). This was mainly because of th
- Page 230 and 231: 120 100 80 60 - 40 20 0. cn1 c.n (i
- Page 232 and 233: 3NP 6NP 4NP 1 NP 5NP 2NP : 3P 1P 6P
- Page 234 and 235: 4P 3P 5P 5NP 6P 2P 1P Figure 8.8: T
- Page 236 and 237: Figure 8.10 shows the dendrogram pr
- Page 238 and 239: NP1 NP2 NP2 NP2 NP1 NP1 NP2 NP2 NP2
- Page 242 and 243: 5 350 — 300 250 200 — ISO — 1
- Page 244 and 245: abundances of P. ciliata had more d
- Page 246 and 247: levels of silt/clay and organics. S
- Page 248 and 249: 1973; Noji and Noji, 1991). Competi
- Page 250 and 251: shown to consume up to 68% of a 0-g
- Page 252 and 253: In Chapter 7 the micro-scale spatia
- Page 254 and 255: and positions of patches. Consequen
- Page 256 and 257: epresent those found establishing i
- Page 258 and 259: distribution at the micro-scale. Ad
- Page 260 and 261: provide a rich food source for deme
- Page 262 and 263: Armonies W., 1988. Active emergence
- Page 264 and 265: Cha M.W., in prep. Macroalgal mats
- Page 266 and 267: Dobbs F.C. and Vozarik J.M., 1983.
- Page 268 and 269: Flach E.C., 1996. The influence of
- Page 270 and 271: Hall SI, Raffaeni D.G., Basford DJ.
- Page 272 and 273: Keckler D., 1997. Surfer for Window
- Page 274 and 275: Levin L.A. and Creed E.L., 1986. Ef
- Page 276 and 277: Mileikovsky S.A., 1971. Types of la
- Page 278 and 279: Ong B. and Krishnan S., 1995. Chang
- Page 280 and 281: Raffaelli D.G., Hildrew A.G. and Gi
- Page 282 and 283: Scheltema R.S., 1974. Biological in
- Page 284 and 285: Soulsby P.G., Lowthion D., Houston
- Page 286 and 287: McArdle B.H., Morrisey D., Schneide
- Page 288 and 289: Wharfe J.R., 1977. An ecological su
Sediment water, organic and silt/clay contents - There were no statistical<br />
differences between patches and non-patches for water content (Figure 8.12(i)), while<br />
for the % silt/clay and % organic contents, significantly higher values were found in P.<br />
elegans patches throughout the sampling period from April 1997 to August 1998<br />
(Figures 8.12(ii-iii)). Silt/clay content remained at approximately 5% in non-patch<br />
samples while it rose to 14.2% ± 0.64% in August 1997 in patches, then slowly<br />
decreased to 9.58% ± 0.95% in August 1998. A decreasing trend was observed for the<br />
organic content in patches from 3.6% ± 0.19% at the start of the sampling period to<br />
2.4% ± 0.08% in August 1998, although this was always significantly higher than in<br />
non-patch sediments, which was consistently around 2%.<br />
Redox potentials - Whilst sedimentary variables such as the silt/clay and organic<br />
contents showed clear differences between patch and non-patch sediments, the results<br />
of the redox measurements were more equivocal. Figures 8.13(i-iii) show that the<br />
redox profiles of the two plot types were very similar between April and December<br />
1997. However, during August 1998, the sediments at 1 cm and 2cm depths in P.<br />
elegans patches were significantly more reducing than those in non-patch areas, while<br />
at the 4cm depth, they were significantly less reducing than non-patch sediments<br />
(Figure 8.13(iv)).<br />
223