Macrophytes, detached by storms and heavy wave actlon, accumulate in the surf zone off King's Beach, Algoa Bay, South Africa. The con~position of these macrophytes, their temporal and spatial occurrence, and their associated fauna were invesbgated. These macrophytes are a transient feature at King's Beach. They are living and actively photosyntheslzlng while in the surf zone, thus breaking down very slowly. Mesh bags contaimng the 2 dominant species of red algae were placed behlnd the breakers and breakdown rates of the algae monitored. In addition, changes in fauna1 biomass values and numbers were analysed. In bags with 10 mm mesh, 50 % breakdown occurred after 8 d and in bags with 2 mm mesh, after 26 d. These algae pass through the beach system rapidly in longshore currents and do not accumulate there. They are neither important in the energetics of the surf zone nor form an important nursery area for juvenile fishes at King's Beach. The fauna associated wlth these algae is derived from their attachment sites of origin and does not colonize them in the surf. Amphipods dominate the epifauna. INTRODUCTION detached macrophytes in a Southern African surf zone by determining whether these algal accumulations are The role of beached macrophytes in coastal food web important in surf zone energetics and/or are utilised as dynamics has been investigated by several authors nursery areas for juvenile fishes, as recorded else(e.g. Gnffiths & Stenton-Dozey 1981, Koop & Field where. 1981). The influence of surf zone accumulations of plants on ecological processes in coastal marine MATERIALS AND METHODS environments has, however, received less attention (Lenanton et al. 1982), particularly in terms of macroStudy area. King's Beach (3358'S, 2539' E) , is an faunal-drift algae associates (Kulczycki et al. 1981). ENE-facing beach, stretching 1.3 km in a southerly Along the western Australian coast large numbers of direction from the harbour of Port Elizabeth (Fig. 1). macrophytes are removed from nearshore seagrass This is a medium energy beach, being less exposed meadows and kelp beds by storms and heavy swells. than other beaches in Algoa Bay, as it is protected from These macrophytes accumulate along the shore formthe prevailing south-westerly winds by the mainland of ing large patches of plant material in the surf zone and Cape Recife (Lasiak 1984). King's Beach experiences wrack banks on beaches and rocks (Lenanton et al. continuous moderate wave action; waves break at a 1982). Similar wrack accumulations were recorded by distance of 50 to 100 m offshore and have an average Zobell (1971). According to Lenanton et al. (1982) a brealung height of 0.7 m (McLachlan 1980). The physinumber of fish species use portions of the open coast of cal, chemical and biological features of King's Beach south-western Australia as an alternative to estuaries have been described by McLachlan (1977, 1979, 1980). as nursery areas. The detached macrophyte accumulaThe temperate waters of Algoa Bay are subjected to tions provide a source of food and shelter for these seasonal fluctuations with a maximum temperature fishes (Lenanton et al. 1982) and also a habitat for range of 11 to 26°C in the surf (Lasiak 1984). However, epifauna (Eiseman & Benz 1975, Hooks et al. 1976, temperature varied between 14 and 18°C during this Cowper 1978, Heck 1979, Gore et al. 1981, Heck & study. Tides are semidiurnal subequal with a maximum Thoman 1981, Kulczycki et al. 1981). spring range of 2.1 m. The aim of this study was to evaluate the role of Field sampling. Algal wrack is most abundant in the O Inter-Research/Printed in F. R. Germany Mar. Ecol. Prog. Ser. 38: 53-63, 1987
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