Stygofauna Diversity and Distribution in Eastern Australian Cave and Karst Areas
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--- - ------------------------------ DOI: 10.18195/issn.0313-122x.64.2001.049-062 Records of the Western Australian Museum Supplement No. 64: 49-62 (2001). Stygofauna diversity and distribution in Eastern Australian cave and karst areas 1 2 3 Mia E. Thurgate *, Jane s. Gough , Arthur K. Clarke , Peter Serov4and Andy Spate! 1 Jenolan Caves Reserve Trust, Locked Bag, Jenolan Caves, New South Wales 2790, Australia e-mail: [email protected] 2 NSW National Parks and Wildlife Service, PO Box 2115, Queanbeyan, New South Wales 2620, Australia 3 School of Zoology, University of Tasmania, GPO Box 252-05, Hobart, Tasmania 7001, Australia 4 Centre for Natural Resources, Biodiversity and Conservation Unit, University of New England, PO Box U245, Armidale, New South Wales 2351, Australia * For correspondence Abstract - This paper reviews the diversity and distribution of the stygofauna of Eastern Australia on a regional basis. Most of the stygofauna is concentrated in the highland karsts of New South Wales and Tasmania. Two hundred and thirty-eight taxa are present and amphipods, syncarids and hydrobiid gastropods are the dominant and most widespread groups. Nearly half of the total fauna are stygobites (82 taxa) and stygophiles (34 taxa). Also present are taxa with Gondwanan and Pangaean affinities, taxa that are phylogenetic and distributional relicts, and locally endemic taxa. Diversity and distribution at the local karst scale is also discussed using a case study of Wombeyan Caves, one of the richest stygofauna sites in Eastern Australia. The paper concludes with suggestions for further research. INTRODUCTION surveys suggest this is also an important region of The presence of a diverse global stygofauna stygofauna diversity (Eberhard et al., 1991; (fauna inhabiting groundwater environments) has Eberhard and Spate, 1995). led to groundwater ecology becoming a major This paper synthesises the available information discipline of scientific endeavour (Gibert et al., on the stygofauna of Eastern Australia inhabiting 1994), particularly in the Northern Hemisphere. In karst and cave areas. We describe patterns in terms of global composition, crustaceans dominate composition, diversity and distribution focussing the fauna, there is a paucity of insects, and particularly on the crustacean and molluscan fauna gastropods are regionally significant (Botosaneanu, of New South Wales and Tasmania. Our intention 1986; Culver and Sket, 2000; Sket, 1999). The is to highlight the stygofauna of Eastern Australia, diversity of these groundwater ecosystems was draw attention to what is known of its significance, recently highlighted by the identification of and encourage further discussion and research. stygofauna 'hotspots' in North America and Europe (Culver and Sket, 2000). Despite considerable continental aridity and a METHODS AND SOURCES OF INFORMAnON paucity of cave and karst areas by world standards, The information presented in this paper is based Australia has been identified as a regional centre of on several databases, unpublished reports and stygofauna diversity (Holsinger, 1993; Knott, 1986; records of the authors'. Published information is Williams, 1986). Support for this statement arises also used for Tasmania (Eberhard et al., 1991; from research in Western Australia, particularly in Clarke, 1997), New South Wales (Eberhard and Cape Range, Barrow Island and Yanchep (e.g. Spate, 1995; Bradbury and Williams, 1997b) and Humphreys, 2000a; Jasinska and Knott, 2000). The South Australia (Zeidler, 1983; Thurgate, 1995). two richest sites in the world for stygal amphipods Details of the locations of specimens and the status are the Ethel Gorge calcrete and Barrow Island, both of taxonomic determinations are available from the in northwestern Australia (Humphreys, 2001; authors. Bradbury, 2000). There are also more stygal dytiscid Most karst and cave areas in Eastern Australia beetles in the Yilgarn region (southwestern have been cursorily sampled, although a few Australia) than in the remainder of the world selected areas in Tasmania (e.g. Ida Bay, Mole combined (Humphreys, 2001). Less attention has Creek) and New South Wales (e.g. Wombeyan, been paid to the stygofauna of Eastern Australia Jenolan) have been more intensively surveyed. (defined herein as east of 138° longitude) but Surveys have employed a mixture of techniques 50 M.E. Thurgate, }.S. Gough, A.K. Clarke, P. Serov, A. Spate . v. NNC wsw FRE DE 250 o 250 500 km i s Figure 1 Distribution of stygofauna sites in Eastern Australia. Each dot on the map represents one or more karst areas. Boundaries for IBRA regions are also shown and follow Thackway and Cresswell (1995). Codes for IBRA regions are given in Table 1, except for MII (Mount Isa Inlier) and MGD (Mitchell Grass Downs). These latter two regions are not included in Table 1 as the diversity and composition of their stygofauna is completely undetermined. -----------------------~....._ ..._--- Stygofauna of Eastern Australia 51 including active searching, nets and aspirators, and relictual and are perched above the water table for trapping with modified baited 'yabbie' pots much of the year. In the Mount Gambier karst (Eberhard et al., 1991; Eberhard and Spate, 1995; (Naracoorte Coastal Plain Region) groundwater is Clarke, 1997). present at shallow depths in many caves. Much of the stygofauna is undetermined, but we In the Einasleigh Uplands Region, the karsts are have included information on these taxa to give a residual tropical forms (karst towers) rising above more complete indication of the diversity of these the surrounding plains. They formed during the ecosystems. Where multiple specimens have not wetter conditions of the Tertiary Oennings, 1982). been clearly assigned to a particular genus or Numerous individual towers are distributed over species, we have treated these as belonging to a several hundred kilometres. Subdued tower karsts single taxon. Given the distribution patterns are also found in the North Coast Region, and these discussed below (i.e. highly localised with many developed in the Cretaceous (Osborne and endemics), improved taxonomic information will Branagan, 1988). This region is a transition zone undoubtedly result in an overall increase in between the tropical karsts described above and diversity. temperate karsts described below. Few caves extend to groundwater in either of these regions. Nature and Extent of Karst Areas At least 90 small karst areas are widely scattered The karsts of Eastern Australia are not uniformly in the South Western Slopes, South East Highlands distributed (Figure 1). Instead, they form a series of and Australian Alps Regions of New South Wales scattered outcrops that are concentrated in the (Figure 1). Often these are ancient karsts, some of southeast of Eastern Australia. The distribution of which developed in the Permian (Osborne and karst styles broadly corresponds to the Branagan, 1988; Osborne, 1993, 1999). These karst biogeographic region boundaries developed under areas are impounded, that is, surrounded by higher- the Interim Biogeographic Regionalisation for lying non-carbonate terrains so groundwater Australia (!BRA: Thackway and Cresswell, 1995). systems are generally small and discontinuous. These regions (Figure 1) are based on similarities in Approximately 80 small karst areas are located in surface climate, geology, landform and biological the Woolnorth, West and South West and attributes. We use the !BRA regions as an D'Entrecasteaux Regions of Tasmania, and are of a organisational framework for discussing the similar age and style to those of southeast New biogeography of the stygofauna, and it is not our South Wales, but are more extensive and deeper intention to infer causality. systems (Kiernan, 1995). In both states, the karsts Most of the Eastern Australian karsts are of small are found throughout a range of climatic and size with limited surface expression (Table 1). altitudinal gradients. Exceptions to this pattern are found in the extensive The impounded karsts of New South Wales and Mitchell Grass Downs and Naracoorte Coastal Plain Tasmania are complex systems, and many of them Regions (Figure 1) where the karsts form broad, have experienced multiple phases of karstification undulating plains in flat-bedded rock. Many of the interspersed with periods of marine transgression, caves in these regions have deep open shafts or burial, infilling and exhumation (Osborne and sinkholes at their entrance. Most caves at Branagan, 1988; Osborne, 1993, 1999; Clarke, 1995). Camooweal (Mitchell Grass Downs Region) are In addition, many karst areas of Tasmania lie Crustacea 130 Gastropoda Other Insecta o 20 40 60 80 100 120 140 No. oftaxa Figure 2 Composition of stygofauna in Eastern Australia. The group designated as 'other' includes protozoans, turbellarians, oligochaetes, nematomorphans, arachnids and bivalves. Table 1 Karst area characteristics and associated stygofauna families occurring within IBRA regions as defined by Thackway and Cresswell (1995). Representative sites Ut include locations in New South Wales and Tasmania with a high stygofauna diversity (ie more than 10 taxa present). Families with five or more taxa present in a N given IBRA region are also indicated. IBRA Region Location, karst styles and climatic regime1 Representative sitesz Characteristic faunaI elements (lBRA Code) (Total no. taxa) Einasleigh QLD: Numerous bluffs (tower karst) over several hundred Mitchell-Palmer (1), ChilIagoe (I), Paramelitidae Uplands (EIU) kilometres. Watertable