Abstract

We evaluated relationships between (1) salinity and species richness and (2) frontal zones and community structure for the rocky intertidal macrobenthic community of the Uruguayan coast. A large-scale sampling design (extent ~500 km) covering 9 rocky shores across 3 intertidal levels was performed between September and November 2002. The linear relationship between salinity and species richness (minimum at the freshwater extreme) and the lack of correlation between variation in salinity and richness rejected two previous empirical models, explaining variations in species richness along the salinity gradient. Other factors (e.g. turbidity) may explain this discrepancy. The estuarine front defined two communities—freshwater and estuarine-marine—differing in species composition and richness. The freshwater community was characterised by low richness and few individuals confined to crevices or tide pools, and must be structured by physical processes (e.g. desiccation); the estuarine-marine community, with individuals occupying almost all available substrata, must be structured by both physical and biological processes. A marine front, separating estuarine and marine habitats, had a weak effect on community structure although estuarine and marine assemblages differed according to species characterising different functional groups. We conclude that the position of the estuarine frontal zones is important for explaining large-scale patterns of community structure in the study area.

Highlights

  • The development of most ecological theory relies on the study of small-scale patterns of distributions (Schneider, 1994)

  • Summary: We evaluated relationships between (1) salinity and species richness and (2) frontal zones and community structure for the rocky intertidal macrobenthic community of the Uruguayan coast

  • We explored the relationships between salinity and species richness and investigated whether macrobenthic community structure varied in relation to the estuarine and marine fronts

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Summary

Introduction

The development of most ecological theory relies on the study of small-scale patterns of distributions (Schneider, 1994). In intertidal habitats, research on large-scale variability in populations and communities focuses on latitudinal gradients in coastal oceanic areas, associated with gradients in solar irradiance, temperature, disturbance history or production (Hughes et al, 1999; Bustamante and Branch, 1996; Broitman et al, 2001; Benedetti-Cecchi, 2001). Most studies of gradients in estuarine areas are concerned with small-scale patterns and soft-sediment fauna (but see Wallentinus, 1991). Gradients in species richness are observed along estuaries, with a minimum salinity of around 3-4 (reviewed in Remane and Schlieper, 1971). Macrofaunal richness may reach minimum values (1) at an ecophysiological boundary (horohalinicum) at a salinity of 4-8 (Remane and Schlieper, 1971), or (2) at sites characterised by high variability in salinity (Attrill, 2002)

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