The benthic macrofauna of the St. Lucia Estuary during the 2005 drought year
Introduction
The St. Lucia estuarine lake (hereafter referred to as the St. Lucia Estuary) is the largest estuarine system in Africa (Fielding et al., 1991, Cyrus and Vivier, 2006a) and makes up roughly 80% of the overall estuarine area in the province of KwaZulu-Natal (Begg, 1978). The St. Lucia Estuary forms part of the Greater St. Lucia Wetland Park, which was declared a RAMSAR site in 1991, and granted World Heritage status in 1999, in view of the biological diversity and richness of this ecosystem.
Ecologically, the St. Lucia Estuary functions as a nursery for many fish (Wallace and van der Elst, 1975) and invertebrate species (Begg, 1978, Benfield et al., 1989). From a commercial and socio-economic point of view, the estuary has also supported a commercial prawn bait fishery since 1952 (Fielding et al., 1990), as well as other subsistence and recreational fisheries (Mann, 1995).
The St. Lucia Estuary is a naturally variable system, as large-scale spatial and temporal variations in physical and chemical parameters have been documented through its history (Begg, 1978, Fielding et al., 1991). The system has been typified by intermittent periods of flooding, droughts and mouth closure, but in spite of such disturbances, the system has nevertheless supported rich and diverse fauna and flora (Fielding et al., 1991). Such unpredictability in the physico-chemical habitat, allied with the diversity of biota has resulted in the system being well researched relative to other systems in South Africa. Studies on phytoplankton (Fielding et al., 1991), zooplankton (Grindley and Heydorn, 1970), fish (Blaber, 1979, Cyrus and Vivier, 2006a, Cyrus and Vivier, 2006b) and macrofauna (Forbes and Cyrus, 1992, Owen and Forbes, 1997) have been undertaken in the system.
However, the St. Lucia Estuary has been subjected to severe drought conditions over the last four to five years, which have resulted in the mouth of the estuary being permanently cut off from the Indian Ocean in June 2002 (Cyrus and Vivier, 2006a). Since then, the only link the estuary has had with the ocean is via the adjacent Mfolozi River during a flood event (Cyrus and Vivier, 2006a). Due to high evaporation rates and reduced fresh water inflow into the system, parts of the estuary have became hypersaline, with salinities of 200 and 90 being recorded in the North and South lakes, respectively (Cyrus and Vivier, 2006a).
So far, the only published work documenting the biological effects of this drought has dealt with the fish community, but there is as yet no information available on its effects on invertebrates, specifically macrofauna. The primary aim of this investigation was, therefore, to examine the effects of the prevalent drought conditions on the macrofauna of the St. Lucia system, as no study has specifically addressed this issue. The secondary aim was to update knowledge of benthic macrofauna in the St Lucia Estuary, since the last published work on macrofauna was undertaken roughly a decade ago. From a global perspective, literature regarding the effects of droughts on estuaries and estuarine lakes is scarce, and the mechanisms by which they influence these ecosystems are poorly understood (e.g. Hastie and Smith, 2006). The present study was intended to add to current knowledge of drought effects on estuarine systems, and to understand the fundamental causative mechanisms.
Section snippets
Study area
The St. Lucia Estuary is situated in northern Kwazulu-Natal and lies between 27° 52′S to 28° 24′S and 32° 21′E to 32° 34′E. The system is made up of three shallow lakes connected to the Indian Ocean by a 21 km meandering channel referred to as the Narrows (Fig. 1). In total, the St. Lucia Estuary and lake system cover an area between 300 and 350 km2, depending on water levels (Begg, 1978). The system is sub-divided into the Mouth, Narrows, South Lake, North Lake and False Bay (Fig. 1).
Sampling procedure
Samples
Salinity
A reversed-salinity gradient persisted in the system over the whole survey period, with salinities at the mouth and Narrows ranging from 10.1 to 17.9 and from 5.3 to 16.7, respectively. Salinity ranged from 9.9 to 72 in the South Lake, and from 0 to 125.6 in the North Lake–False Bay area (Table 1). Hypersaline conditions were most extreme in February, when maxima of 113.7 and 125.6 were recorded at Lister's Point and Hell's Gate, respectively.
Temperature
Seasonal variations in temperature were marked
Discussion
The results of this investigation indicate a significant effect of the prevailing drought on the physical environment and macrofauna of the St. Lucia Estuary. The most noteworthy effects on the physical habitat are the reductions in total areas of inhabitable substrate available to macrofauna, as well as the development of hypersaline conditions in parts of the South and North lakes. The 5 year period of mouth closure, and the consequent loss of seawater intrusion into the system, allied with
Acknowledgements
We are grateful to the management and staff of Ezemvelo KZN Wildlife for logistical support during the study, especially to R. Taylor, C. Fox and A. Myeza. M. Desai is gratefully acknowledged for assistance in collecting, sorting and identification of macrofauna samples. A.J. Smit, S. Singh and K. Pillay are thanked for their assistance with field collections, and F. MacKay for help with taxonomic identifications. Funding for the study was provided by the South African Marine and Coastal
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