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oughness elements (Nowell and Church, 1979; Nowell et al., 1981) and/or the indirect effect of increased microbial sediment-binding (Eckman et al., 1981). The altered physical, chemical, physico-chemical and biological conditions encountered within these tube-beds have been shown to result in different infaunal macrobenthic (Sanders et al., 1962; Fager, 1964; Ragnarsson, 1996) and meiobenthic (Reise, 1985; Noji, 1994) communities compared with non-patch areas. The processes responsible for the formation and maintenance of such patches, in contrast to micro-scale patches, have not been explicitly studied. Relating observed patterns to the underlying processes which help to create them is difficult, even at the tractable scale at which manipulative experiments can be conducted (Hall et al., 1993). However, several authors have proposed that sediment disturbance and the appropriate life history characteristics for their particular environment are prerequisites for patch formation. Carey (1987) suggested that there was an association between L. conchilega, macroalgal mat establishment and intermittently high sedimentation rates for L. conchilega mound development on St. Andrews Bay, Scotland. Fager (1964), however, suggested that a period of calm conditions after larval settlement could have led to the formation of the 0. fusiformis patches. Morgan (1997) postulated that in view of the reproductive strategy possessed by the P. elegans population in the Baie de Somme, France, gregarious larval settlement and increased adult immigration into, or lower adult emmigration and/or lower mortality within patches, were important prerequisites for the formation of tube-beds. Many spionid polychaetes are capable of reaching very high numbers following a disturbance and have been described as opportunists (Grassle and Grassle, 1974; Pearson and Rosenberg, 1978). How this relates to formation of the observed patches is not clear. However, it would appear that for spionid tube-bed formation, some sediment disturbance is likely to be an important prerequisite. THE PRESENT STUDY On Drum Sands, Firth of Forth, Scotland, the tube-building, spionid polychaete Pygospio elegans forms small-scale patches which can be seen as areas of smooth, 6
aised sediment within an otherwise wave-rippled sandflat. This study has 3 main aims, these are: • To determine the spatial distribution of P. elegans on Drum Sands; • To investigate the processes affecting P. elegans densities and the possible role of these processes in the formation and maintenance of small-scale patches; • To assess the ecological importance of the spatial distribution of P. elegans on Drum Sands. These 3 aims were addressed by carrying out surveys and experimental manipulations on Drum Sands, these are discussed in more detail below. In Chapter 2, the small- to meso-scale (metres-10's metres) spatial patterns of P. elegans within a relatively homogeneous area of Drum Sands were investigated to explicitly determine the sizes of the P. elegans patches, their position, and worm density within them. The spatial patterns of other common taxa were also determined, together with sediment variables, in order to assess whether interspecific interactions and/or abiotic factors were likely to be important processes affecting the spatial distribution of P. elegans. The population dynamics and reproductive biology of P. elegans on Drum Sands were considered in Chapter 3 together with their possible role in patch formation and maintenance. An understanding of the population dynamics and reproductive biology of this population was necessary in view of the reproductive variability found within this species. The ecological effects of macroalgal mat formation on intertidal sandflats were investigated in Chapters 4 and 5. In these chapters, the potential role of macroalgal mat establishment in the formation and maintenance of P. elegans patches is discussed. This was achieved by both a controlled weed-implantation experiment (Chapter 4) and a descriptive survey (Chapter 5). In Chapter 6, the role of sediment disturbance on intertidal sandflats is addressed. Using small-scale patches of P. elegans, the effects of dense assemblages of biogenic 7
- Page 1 and 2: AN INVESTIGATION INTO THE PROCESSES
- Page 3 and 4: ABSTRACT The spionid polychaete Pyg
- Page 5 and 6: ACKNOWLEDGEMENTS I am indebted to m
- Page 7 and 8: Results. . 65 Size distribution of
- Page 9 and 10: CHAPTER 9. GENERAL DISCUSSION . . 2
- Page 11 and 12: Figure 5.4 Figure 5.5 Figure 6.1 Fi
- Page 13 and 14: LIST OF TABLES Table 2.1 Statistica
- Page 15 and 16: BACKGROUND CHAPTER 1 INTRODUCTION A
- Page 17 and 18: The scales of observation, or the s
- Page 19: systematic sampling design to inves
- Page 23 and 24: Fauchald and Jumars (1979) describe
- Page 25: Dalmeny House and sewage discharged
- Page 28 and 29: E 7— E 6-ac. MHWS MHWN t co 4 —
- Page 30 and 31: variance (TTLQV) techniques (see Lu
- Page 32 and 33: analysis using Moran's and Geary's
- Page 34 and 35: Holme and McIntyre (1984). Percenta
- Page 36 and 37: Pattern Analysis - Grid Surveys Sur
- Page 38 and 39: 57 64 1=1 0 0 0 0 0 0 0 O 0 0 0 0 0
- Page 40 and 41: Maps produced by kriging and other
- Page 42 and 43: 200 180 1160 140 100 1-3 80 g 60 c.
- Page 44 and 45: 2.5 1.5 0.5 0 3 T (i) % Silt/clay%
- Page 46 and 47: v : m pattern Id pattern Ip pattern
- Page 48 and 49: " v : m pattern Id pattern Ip patte
- Page 50 and 51: The results show that at the smalle
- Page 52 and 53: Nephtys hombergii's spatial distrib
- Page 54 and 55: (vii) G. duebeni (ix) % Organic con
- Page 56 and 57: 8m survey - spatial patterns Figure
- Page 58 and 59: (1) P. elegans (iii) L. conchilega
- Page 60 and 61: a) Ts 1.4 0.6 u 0.2 -0.2 1.4 'E5 0.
- Page 62 and 63: 200m 150m 100m 50m (ix) C. edule 56
- Page 64 and 65: 73 ‘a• el 1.4 (ix) G. duebeni 1
- Page 66 and 67: DISCUSSION The main aims of this st
- Page 68 and 69: formed patches less than 1m2 and th
oughness elements (Nowell and Church, 1979; Nowell et al., 1981) and/or the<br />
indirect effect of increased microbial sediment-binding (Eckman et al., 1981). The<br />
altered physical, chemical, physico-chemical and biological conditions encountered<br />
within these tube-beds have been shown to result in different infaunal macrobenthic<br />
(Sanders et al., 1962; Fager, 1964; Ragnarsson, 1996) and meiobenthic (Reise, 1985;<br />
Noji, 1994) communities compared with non-patch areas.<br />
The processes responsible for the formation and maintenance of such patches, in<br />
contrast to micro-scale patches, have not been explicitly studied. Relating observed<br />
patterns to the underlying processes which help to create them is difficult, even at the<br />
tractable scale at which manipulative experiments can be conducted (Hall et al.,<br />
1993). However, several authors have proposed that sediment disturbance and the<br />
appropriate life history characteristics for their particular environment are<br />
prerequisites for patch formation. Carey (1987) suggested that there was an<br />
association between L. conchilega, macroalgal mat establishment and intermittently<br />
high sedimentation rates for L. conchilega mound development on St. Andrews Bay,<br />
Scotland. Fager (1964), however, suggested that a period of calm conditions after<br />
larval settlement could have led to the formation of the 0. fusiformis patches. Morgan<br />
(1997) postulated that in view of the reproductive strategy possessed by the P. elegans<br />
population in the Baie de Somme, France, gregarious larval settlement and increased<br />
adult immigration into, or lower adult emmigration and/or lower mortality within<br />
patches, were important prerequisites for the formation of tube-beds. Many spionid<br />
polychaetes are capable of reaching very high numbers following a disturbance and<br />
have been described as opportunists (Grassle and Grassle, 1974; Pearson and<br />
Rosenberg, 1978). How this relates to formation of the observed patches is not clear.<br />
However, it would appear that for spionid tube-bed formation, some sediment<br />
disturbance is likely to be an important prerequisite.<br />
THE PRESENT STUDY<br />
On Drum Sands, Firth of Forth, Scotland, the tube-building, spionid polychaete<br />
Pygospio elegans forms small-scale patches which can be seen as areas of smooth,<br />
6