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RESEARCH ARTICLE (Open Access)

Inland aquatic systems and their fauna at Two Peoples Bay Nature Reserve, Western Australia, with emphasis on microinvertebrates

Stuart A. Halse A and Andrew W. Storey https://orcid.org/0009-0009-5804-7091 B *
+ Author Affiliations
- Author Affiliations

A Bennelongia Environmental Consultants, 5 Bishop Street, Jolimont, WA 6014, Australia.

B School of Biological Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia.

* Correspondence to: andrew.storey@uwa.edu.au

Handling Editor: Mike Calver

Pacific Conservation Biology 31, PC24094 https://doi.org/10.1071/PC24094
Submitted: 3 December 2024  Accepted: 5 December 2024  Published: 6 January 2025

© 2025 The Author(s) (or their employer(s)). Published by CSIRO Publishing. This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND)

Abstract

Context

Decisions about fauna conservation priorities in a region, and management actions required to facilitate conservation objectives, require as much information as possible about the ecology of fauna species present.

Aims

This paper summarises information on the inland aquatic fauna of Two Peoples Bay Nature Reserve as part of the process of documenting the Reserve’s conservation values.

Key Results

Surveys in the early 1990s, and subsequently, show that rivers, creeks, and lakes of the Reserve support a rich aquatic invertebrate fauna. The microinvertebrate community is unusually rich in rotifers and cladocerans. Probably nine Indigenous fish species occur in the Reserve, including the vulnerable Nannatherina balstoni, restricted Galaxias maculatus and critically endangered Galaxias truttaceus. The installation of a vertical slot fish ladder on the Goodga River weir has likely helped these species by expanding available habitat. Although the low nutrient status and relatively deep water of the lakes limit their waterbird value, considered together the Reserve’s lakes fall just outside the top 10% of nature reserves in Western Australian for number of waterbird species supported.

Conclusions

The richness of aquatic invertebrate species in the Reserve’s lakes contrasted with previous results from rivers in south-western Australia and has led to a changed understanding of both the diversity and conservation significance of the inland aquatic invertebrate fauna in Western Australian lakes.

Implications

Invertebrate community composition and conservation values are not recognised unless surveyed by people with appropriate taxonomic expertise. Without such surveys the focus of conservation effort and management may be, at least partially, misdirected.

Keywords: Cladocera, conservation value, fish, macroinvertebrates, microinvertebrates, Rotifera, waterbirds, wetlands.

Introduction

This paper is part of a collection of Pacific Conservation Biology documenting the natural history of the Two Peoples Bay Nature Reserve in Western Australia (Hopkins et al. 2024) and provides information about the drainage systems and their non-marine aquatic fauna. Wetlands, including creeks, are prominent features of the Reserve. Three distinct drainage systems occur, associated with the Goodga River, Angove River, and the upland streams of the Maardjitup Gurlin/Mt Gardner headland (Fig. 1) (Noongar names are from Knapp et al. 2024). Two of the systems (Angove and Goodga) arise outside the Reserve and are influenced by external land practices.

Fig. 1.

Lakes, rivers, and streams of Two Peoples Bay Nature Reserve and sampling points in the water bodies.


PC24094_F1.gif

Data on water depth, salinity, and discharge of the Goodga and Angove systems have been recorded for a number of years (Lane et al. 2015) and the invertebrate fauna has been surveyed relatively intensively (Storey et al. 1993), with a range of authors sampling fish (current authors in 1990; Morgan et al. 1998, 2006; Morgan and Beatty 2006; N. Coy, unpubl. data). Our paper describes the physico-chemical characteristics and vegetation (emergent and riparian) of the aquatic ecosystems of the Reserve area, provides the results of some surveys of fish and waterbirds, and discusses the significance of the aquatic invertebrate fauna.

The data reported in this paper are mostly several decades old and, with the exception of physico-chemical data for the lakes, were collected to provide an inventory of the biological values of the Reserve, which was gazetted in 1966 and 1967 for the purpose of flora and fauna conservation (Chatfield and Saunders 2024). The protection thus provided to the aquatic systems of the Reserve and their fauna represents early recognition of the value of formal protection processes by government as an effective conservation tool, which is overlooked in much conservation policy-making (Tickner et al. 2020). Detailed inventory of aquatic invertebrates in south-western Australia was in its early stages in 1990 and 1991, when the invertebrate work reported here was undertaken, and the results from the Reserve have been important for highlighting the value of sampling all aquatic invertebrate groups and also in providing taxonomic focus for much of the more recent aquatic invertebrate work in Western Australia.

Background to aquatic fauna surveys in south-western Australia

Biogeographic setting

This review of inland aquatic fauna surveys focuses on south-western Australia, comprising a zone extending approximately from Kalbarri to Esperance and comprising seven bioregions (Fig. 2). Two Peoples Bay Nature Reserve lies in the southern part of the Jarrah Forest bioregion. Permanent or near permanent lakes are mostly restricted to the Swan Coastal Plain, Warren, southern Jarrah Forest, and Esperance bioregions, and are uncommon even in these regions. South-western Australia has a Mediterranean climate, albeit with less pronounced seasonality at Two Peoples Bay on the south coast. Albany, just west of Two Peoples Bay, has a mean monthly maximum temperature of 16°C in the coldest winter month and 23°C in the warmest summer month, and an annual rainfall of 921 mm (Table 1). Across most of the south-west, rivers flow for limited periods in winter and spring but near the coast may contain permanent water, especially in the wetter Warren region.

Fig. 2.

Interim biogeographical regions of south-western Australia and towns/sites used in rainfall statistics.


PC24094_F2.gif
Table 1.Mean monthly maximum temperatures and mean annual rainfall for selected south-western Australian sites (from Bureau of Meteorology).

 July (°C)February (°C)Annual rainfall (mm)
Albany15.922.9920.9
Esperance17.326.2617.4
Kalbarri21.934.1341.8
Perth18.531.7727.3
Southern Cross16.334.5A 295.4
Windy Harbour16.823.71061.1
A January value.
Waterbirds

There is a long history of waterbird surveys at wetlands in Western Australia, often by amateur ornithologists. Large-scale, coordinated surveys with multiple surveys of sites and a clear conservation purpose did not begin until the 1980s. The main surveys have included inventory of waterbirds in nearly all nature reserves containing wetlands in the 1980s (Jaensch et al. 1988), censuses of ducks, coots, and swans across the south-west from 1986 to 1992 (Halse et al. 1995), and surveys of 251 wetlands on the coastal plain around Perth in 1990 and 1991 to assist water allocation planning (Storey et al. 1993). Waterbirds were surveyed across all of Western Australia in 2008 as part of a national census (Kingsford et al. 2012) and regular monitoring of the effects of salinisation at 25 wetlands began in the mid-1990s (Pinder et al. 2023). These broadscale surveys provide a context for the many surveys that have been conducted at individual wetlands or groups of wetlands, including the surveys at Two Peoples Bay Nature Reserve.

Fish

Important contributions to knowledge of inland fish in south-western Australia have been made by Gerry Allen (Allen et al. 2002) and Ian Potter, David Morgan, Luke Pen, and Howard Gill (Pen and Potter 1991; Morgan et al. 1998). Among the many benefits, surveys of fish in the past 30 years have led to new species being discovered (Morgan et al. 2013), the habitats and distributions of south-western Australian inland aquatic fish being known in detail (Morgan and Gill 2000) and fitted into a state-wide picture (Morgan et al. 2014), and managers being able to predict the likely impacts of increasing salinity on different fish species (Beatty et al. 2011). Dryland salinity is extensive in south-western Australia and has affected all aquatic life (Halse et al. 2003). The impact of invasive fish species has also been studied (Lymbery et al. 2010).

Aquatic invertebrates

Several people have made outstanding taxonomic contributions that have supported inventory of aquatic invertebrates across Western Australia. They include Tony Watson for dragonflies (Watson et al. 1991), Chris Watts for beetles (Watts 1978), Peter Cranston and Don Edward for dipterans (Leung et al. 2013; Cranston 2019), Ian Bayly for calanoid copepods (Bayly 1992), Patrick De Deckker for ostracods (De Deckker 1983), Michael Geddes and Brian Timms for anostracans (Geddes 1981; Timms 2012), Adrian Pinder for oligochaetes (Pinder and Brinkhurst 1994), and Russell Shiel for rotifers and cladocerans (Shiel 1995).

Large-scale surveys of aquatic invertebrates have been undertaken on the coastal plain around Perth for water allocation planning (Davis et al. 1993), wetlands across the wheatbelt region of south-western Australia for conservation planning (Pinder et al. 2004), in rivers across Western Australia to provide the basis for using invertebrates as indicators of the ecological health of wetlands (Smith et al. 1999), and in rivers of the forested areas for conservation planning and monitoring of ecological condition (Pennifold et al. 2017). Many smaller scale surveys, including those along the south coast by Edward et al. (1994), Stewart (2009, 2011) and Timms (2008), have provided inventories and examined the effect of water chemistry on the invertebrate species present. Ecological processes in small streams were studied during the 1980s and 1990s in jarrah forest (Bunn 1988; Storey et al. 1990) and karri forest (Trayler and Davis 1998). The invertebrates of granite rock pools have also been a focus of attention (Pinder et al. 2000; Bayly et al. 2011).

Reviews

Several reviews or analyses of the aquatic fauna of the south-west have been undertaken, including a comprehensive review of all groups of aquatic fauna and flora using rivers by Davies and Stewart (2013), who considered 43% of species in rivers to be endemic to south-western Australia. Reviewing stream studies in south-western Australia in the 1980s, Bunn and Davies (1990) highlighted the depauperate nature of the recorded fish and macroinvertebrate faunas and suggested this is associated with the isolation of south-western Australian streams from other stream systems (the south-west is surrounded by arid regions), the occurrence of much greater aridity in the south-west in the past than occurs now (hence the fauna reflects a more arid situation), and a very low level of primary productivity. In an analysis of available information on aquatic invertebrates, fish and frogs in the Warren bioregion (Fig. 2), Trayler et al. (1996) found records of 156 described invertebrate species, 22 frogs, and 14 native fish in lotic and lentic systems and concluded 86% of the species were protected by their occurrence in various forms of nature reserves, although external impacts (including salinisation) may reduce the protection provided by some reserves. Analysing results of sampling for aquatic invertebrates in peatlands and shrublands of southern parts of the Warren and Jarrah Forest bioregions, Horwitz (1997) found endemism to be higher in the coastal plain of the Warren region than elsewhere, perhaps because this area was less impacted by salinity, both currently and historically, than further north. A similar analysis by Horwitz et al. (2009) for aquatic invertebrates in lentic waterbodies around Perth in the Swan Coastal Plain bioregion found 520 species had been recorded, with the coastal wetlands having higher average richness than wetlands further inland in more arid areas. However, only 16% of species recorded by Horwitz et al. (2009) are endemic to south-western Australia.

The aquatic systems at Two Peoples Bay Nature Reserve

The wetland area in the Two Peoples Bay Nature Reserve fluctuates seasonally between ~400 ha (8.5% of the 4745 ha reserve) in normal summer conditions and ~750 ha (15.8%) during average winter/spring flooding in August/September. In very wet winters an estimated 830 ha (17.5%) is inundated, with an additional 170 ha (3.5%) of waterlogged land. The widespread occurrence of peaty sands in the area suggests it was much wetter historically than now. Extraction of water from the Angove River for a potable water supply for Albany (Chatfield and Saunders 2024) and construction of drains on the coastal plain are probably partly responsible for this drying. Components of the wetland systems are described below.

The Goodga drainage system covers 21 km and runs from the headwaters of the Goodga River through Kaiupgidjukgidj/Moates Lake, Juniperina Creek, Tyiurrtmiirity/Gardner Lake and Gardner Creek into the ocean in Two Peoples Bay (Fig. 1). Physico-chemical and depth data for the Goodga system are summarised in Table 2 and Fig. 3; much of this information comes from Lane et al. (2015).

Table 2.Physico-chemical data collected from streams, rivers, and lakes of the Two Peoples Bay area in 1990 when sampling invertebrates (mostly in June) (see Fig. 1 for locations).

Physico-chemical parameterAngove RiverGoodga RiverWest GullyWebster’s GullyAngove LakeGardner LakeMoates Lake
Depth (m)0.50.40.40.31.82.64.4
Salinity (mg/L TDS A)240560440180580880470
pH5.96.36.56.86.87.66.7
Temperature (°C)13.111.410.811.413.310.711.5
Dissolved oxygen (% sat.)7296939396100 B96
Total phosphorus (mg/L)0.030.020.03

Total phosphorus values are the means of samples collected two-monthly between July 1984 and May 1985 by J. A. K. Lane.

A Total dissolved solids.
B Dissolved oxygen was 23% in flooded Melaleuca woodland near Gardner Creek.
Fig. 3.

Long-term data on physico-chemistry of the lakes of Two Peoples Bay Nature Reserve, (a) depth, (b) salinity and (c) pH.


PC24094_F3.gif

The Goodga River arises ~80 m above sea level (a.s.l.) in Water Catchment Reserve No. 13802, which currently has an area of 4006 ha. The Catchment Reserve was first gazetted on 27 October 1911 with an area of 20,000 ha, then gazetted to its present size in 1953 and vested in the Department of Planning, Lands and Heritage.

Water from the headwater swamps in the Catchment Reserve descends 30 m in the first 2 km as it passes between low granite hills before flowing for 6 km in a broad, swampy valley through cleared farmland (Churchward et al. 1988) and being joined by a smaller tributary from the west. One kilometre downstream from this confluence the river enters National Park/Water Reserve No. 24991, which was gazetted on 16 May 1958.

Throughout Reserve No. 24991, what is now the Goodga River is slightly acidic (Table 2) and characterised by a series of long, highly coloured pools with silty substrates that are connected by riffles flowing over laterised rock. Wetland plants along the watercourse include Triglochin procera, Machaerina juncea, Leptocarpus scariosus, Juncus holoschoenus, and Lepyrodia monoica. The Department of Water and Environmental Regulation maintains a V-notch gauging weir 2.5 km upstream from the Two Peoples Bay Road (Fig. 4).

Fig. 4.

V-notch weirs on (a) Angove Creek (Credit: WA Department of Water and Environmental Regulation) and (b) Goodga Creek (Credit: J. Oates).


PC24094_F4.gif

As the river gets closer to Kaiupgidjukgidj/Moates Lake, there are a series of sedge swamps along the water course dominated by Evandra aristata, Leptocarpus scariosus, Hypolaena exsulca, and Xyris lantana. The tannin-stained Kaiupgidjukgidj/Moates Lake is one of the deepest natural lakes in south-western Australia, with depth in September and November varying between 3.6 and 5.0 m over the past 40 years (Fig. 3). Four main rivers/streams flow into the lake: the Goodga River and Black Cat Creek come from the north, a swamp stream that originates north of Two Peoples Bay Road comes from the north-west, and a stream flowing through Black Cat Creek Farm comes from the west (Fig. 1).

Kaiupgidjukgidj/Moates Lake has an area of about 144 ha with 124 ha of open water. Total length of the lake, from east to west, is 2.75 km with a maximum north–south measurement of 0.7 km. Elevation is ~8 m a.s.l. The lake is situated in a depression between a low scarp of sandy laterite to the north and a 300 ha calcareous dune dating from the Holocene to the south. Much of the southern shoreline is a sandy beach, but apart from a few small laterite and sand beaches the northern shoreline is sedge-dominated. Salinity in September and November has varied from 0.1 to 0.8 g/L, with a median of 0.5 g/L. pH has varied from 4.5 to 8.9, with a median of 7.4 (Fig. 3). The major species of sedge in the water are Machaerina articulata in depths up to 1 m and B. juncea close to the shore. Triglochin procera grows in sheltered areas. The marginal sedgeland includes E. aristata, L. scariosus, L. coangustatus, and Anarthria scabra. Behind the sedges are low trees of Taxandria juniperina and A. linearifolia (Halse et al. 1993).

The 2.5 km section of the Goodga system between Kaiupgidjukgidj/Moates and Tyiurrtmiirity/Gardner Lakes is referred to locally as Juniperina Creek. It has a seasonal flow that meanders between lagoons and swamps and through a 1.5 m deep channel to the delta marsh at the western end of Tyiurrtmiirity/Gardner Lake (Fig. 1). There is a fall of 6–7 m in surface level between the two lakes; the gradient varies with fluctuating lake levels. The watercourse and the five or six lagoons between the dunes are locally referred to as the South-East Lagoons. The Machaerina/Juncus sedgelands in the seasonally wet, interdunal swales and along the creek-line are fringed by Taxandria juniperina and Banksia littoralis.

The slightly stained, brackish Tyiurrtmiirity/Lake Gardner receives water mainly from upstream parts of the Goodga drainage system via Juniperina Creek. It may also receive some tidal flow from Gardner Creek, when this is open to the sea, because the lakebed is only ~1.5 m a.s.l. Tyiurrtmiirity/Gardner Lake contains about 186 ha of open water when full but in winter an area of ~350 ha is flooded, with almost half the area densely vegetated. The lake area measures 1.8 km north–south and 1.6 km east–west. Available information, mostly from the 1980s, shows September and November depths of Tyiurrtmiirity/Lake Gardner vary from 2.0 to 2.4 m deep, with salinity ranging from 0.5 to 2.4 g/L and pH from 7.8 to 8.6 (Fig. 3; also see Lane et al. 2015).

Much of the substrate in Tyiurrtmiirity/Gardner Lake is silt over sand and laterite. The emergent sedges around the lake are mainly Machaerina articulata, Juncus krausii, Schoenus brevifolius, and Restio sp. (Fig. 5). In places along the eastern shore they extend 100 m into the water when the lake is full. The seasonally inundated margins support Gahnia trifida, Lepidosperma gladiatum and various shrubs, including Taxandria juniperina, Homalospermum firmum, Hakea sp., Lepyrodia sp., Thysanotis gracilis, and Centella asiatica (Halse et al. 1993).

Fig. 5.

Tyiurrtmiirity/Gardner Lake looking south from road and (a) fringing sedges (Credit: S. Halse).


PC24094_F5.gif

The channel between Tyiurrtmiirity/Gardner Lake and the main beach at Two Peoples Bay is referred to as Gardner Creek. This creek is closed to the sea each summer by a sandbar. In early winter, water in the creek backs up on the landward side of the sandbar, which is opened by mechanical means, usually by the middle of June, to prevent flooding of the small road bridge over Gardner Creek.

As the 2.8 km long Gardner Creek leaves the eastern shore of Tyiurrtmiirity/Gardner Lake, it follows a north-easterly course through a grove of overhanging Melaleuca with little understorey (Fig. 6). Melaleuca cuticularis, M. raphiophylla, M. preissiana, and an undescribed species grow in this seasonally inundated area. The creek then turns south along the landward side of the dune line. Near its mouth, at a break in the dunes adjacent to the Reserve Office, the creek flows past a dense thicket of Phebalium anceps over Lepidosperma gladiatum, with Typha domingensis in a disturbed backwater.

Fig. 6.

Gardner Creek at road crossing (Credit: S. Halse).


PC24094_F6.gif

The Angove drainage system, which is 14 km long, includes the Angove River, Miialyiin/Angove Lake and Angove Drain. The latter joins the Goodga drainage system 1 km inland from the dunes of the main Two Peoples Bay beach. Angove River arises ~90 m a.s.l. in small swamps north of the uncleared Water Catchment Reserve No. 13802 (Fig. 1). The river flows for 8 km through a gently sloping valley into a pipe-head dam that was constructed in 1912–13 to provide water for the town of Albany (Fig. 7). Soils consist of sand over gravels and clay, with mallee-woodland/heath growing on the valley sides and thickets of jarrah Eucalyptus marginata and Allocasuarina on swampy land in the valley (Churchward et al. 1988). Below the dam the stream flows over a sloping granite fault line, with a marked gradient of ~15 m over 1.5 km to a V-notch gauging weir (Fig. 4). Jarrah/Allocasuarina woodland grows on the valley slopes through this section.

Fig. 7.

Miialyiin/Angove Lake looking east (Credit: S. Halse).


PC24094_F7.gif

After leaving the catchment reserve, the river flows more slowly through a stream reserve that is dominated by Melaleuca cuticularis with an understorey that includes the shrubs Pultenaea reticulata, Boronia crenulata, B. gracilipes, and Hypocalymma cordifolium Thresk. Its catchment area and volume are increased by the contribution of four tributaries: two from the north, one flowing from Reservoir Hill in the west across cleared farmland, and a short fast-flowing stream from Boulder Hill in the east (Fig. 1).

Miialyiin/Angove Lake, which is included in a separate ~89 ha northern section of the Nature Reserve, has an area of 22 ha, of which 15.6 ha is open water (Fig. 7). It is complemented by two lagoons to the west (measuring 3 ha and 4 ha respectively), and a third lagoon of 10 ha to the north-east, inland from the dunes at the northern end of Two Peoples Bay (Fig. 7). The total area of swamp and winter-wet land around Miialyiin/Angove Lake is ~100 ha. September and November depths at Angove Lake, mostly from the 1980s, have ranged from 1.8 to 2.8 m. with salinity between 0.3 and 0.9 g/L and pH between 7.8 and 8.6 (Fig. 3; see also Lane et al. 2015).

When settled, water in Miialyiin/Angove Lake is clear but the substrate of black silt is readily suspended by disturbance and settles slowly. Lake margins support extensive stands of Machaerina articulata in deeper water, with B. preisii, Juncus pallidus, J. capitatus, Isolepis prolifera, Triglochin procera, and Cotula coronopifolia in shallow water and on shore. Behind the sedgeland, on the northern side of the lake, the shrubs Taxandria juniperina and Kunzea aff. ericifolia grow, beyond which is a dense thicket of Melaleuca thymoides. Miialyiin/Angove Lake has been invaded by a number of weeds, including Rumex acetosella, Holcus lanatus, Psoralea pinnata, and Vellereophyton dealbatum.

There is a 3 km drain from Miialyiin/Angove Lake to Gardner Creek that is ~1.5 m deep and 10 m wide. It was originally part of a drainage system dug by hand in the late 1920s to allow summer vegetable crops to be grown on the seasonally inundated swamps of the floodplain south of Miialyiin/Angove Lake. The drain was enlarged and deepened to its present size by dragline in the late 1970s.

Where the drain leaves the lake, it contains dense stands of Homalospermum firmum and, for much of its course through farmland, the drain is fringed by a species of Melaleuca, Taxandria linearifolia, Taxandria juniperina, and Kunzea vestita. Close to Gardner Creek the drain follows a natural watercourse, fringed by Hibbertia furfuracea and sedges.

There is a different aquatic system on the Maardjitup Gurlin/Mt Gardner headland, which is drained by 12 small streams that are well-shaded and comparatively cool. The densely vegetated gullies, through which these streams flow, served as a refuge for the noisy scrub-bird Atrichornis clamosus when the species was locally extinct elsewhere (Danks et al. 1996). Streams on the ocean side of the headland rise at ~200 m a.s.l. and flow to the sea with a mean gradient of about 1:7 over their 1.3–1.5 km courses. The four major streams flowing to the ocean – Gardner, Robinson, Webster’s, and West Gullies – hold water permanently, although they recede to pools in dry years.

Robinson Gully is a clear upland stream with a sloping marshland of Schoenus grandiflorus in its middle reaches. Webster’s Gully consists of a series of gravel-bottomed, clearwater pools in its lower reaches with a 10 m drop over granite boulders onto Naarup/Waterfall Beach. The vegetation of this gully is dense eucalypt/Melaleuca forest with a varied understorey that includes Lepidospermum sp. and Anarthria scabra along the stream. West Gully is a rapidly flowing stream with few pools and a dense canopy of low eucalypts along its lower reaches.

Streams on the inland side of the headland arise at ~180 m a.s.l. and descend to the isthmus area where they seep into the dunes and swales. These streams only flow in their upper reaches, where they are seasonal, and are more akin to dry drainage lines for most of their ~2 km courses.

The fauna

Waterbirds

Forty-two species of waterbird were recorded from the three lakes of Two Peoples Bay Nature Reserve between 1973 and 1990 during surveys by the Birdlife Australia and Department of Conservation and Land Management staff (Table 3, see Jaensch et al. 1988 for details). This represents comparatively high species richness for wetlands of south-western Australia: Jaensch et al. (1988) surveyed 197 nature reserves in the south-west during the same time period and ranked Two Peoples Bay 25th in terms of number of species. The individual lakes showed considerable differences in waterbird richness, with Miialyiin/Angove supporting fewer species (17) than Kaiupgidjukgidj/Moates (29) and Tyiurrtmiirity/Gardner (35) (Table 3), although Miialyiin/Angove was surveyed much less often and the lower number of species may be partly attributed to lower survey effort (Jaensch et al. 1988).

Table 3.Waterbird species recorded at Miialyiin/Angove, Tyiurrtmiirity/Gardner, and Kaiupgidjukgidi/Moates lakes during the 1980s (Jaensch et al. 1988).

Scientific nameCommon nameAngoveGardnerMoates
PodicipedidaeGrebes
Podiceps cristatus Great crested grebe61
Poliocephalus poliocephalus Hoary-headed grebe404
Tachybaptus novaehollandiae Australasian grebe67
PelecanidaePelicans
Pelecanus conspicillatus Australian pelican2
AnhingidaeDarters
Anhinga melanogaster Darter2*
PhalacrocoracidaeCormorants
Phalacrocorax carbo Great cormorant110
Phalacrocorax varius Pied cormorant102
Phalacrocorax sulcirostris Little black cormorant168
Phalacrocorax melanoleucos Little pied cormorant399*
ArdeidaeHerons and bitterns
Ardea novaehollandiae White-faced heron11174
Ardea alba Great egret23
Ixobyychus minutus Little bittern11
Botaurus poiciloptilus Australasian bittern111
ThreskornithidaeIbises and spoonbills
Threskiornis aethiopica Sacred ibis181
Threskiornis spinicollis Straw-necked ibis41
Platalea regis Royal spoonbill3
Platalea flavipes Yellow-billed spoonbill3
AnatidaeDucks, geese and swans
Cygnus atratus Black swan24510*
Tadoma tadomoides Australian shelduck25410
Anas superciliosa Pacific black duck65164*13
Anas gibberifrons Grey teal182
Anas rhynchotis Australasian shoveler2
Chenonetta jubatam Maned duck22
Oxyura australis Blue-billed duck531
Biziura lobata Musk duck3*50*4*
AccipitridaeHawks and harriers
Circus aeruginosus Marsh harrier112
RallidaeRails, coots and gallinules
Porzana tabuensis Spotless crake21*3
Porphyrio porphyrio Purple swamphen373*
Fulica atra Eurasian coot216
CharadriidaePlovers and dotterels
Pluvialus squatarola Grey plover1
Erythrogonys cinctus Red-kneed dotterel1
Charadrius ruficapillus Red-capped plover54
Charadrius melanops Black-fronted plover256
ScolopacidaeSnipe and sandpipers
Tringa hypoleucos Common sandpiper1
Tringa nebularia Greenshank62
Calidris ruficollis Red-necked stint60
LaridaeGulls and terns
Larus novaehollandiae Silver gull23
Chlidonias hybrida Whiskered tern2
Hydroprogne caspia Caspian tern2
Sterna bergii Crested tern1
Muscicapidae: SylviinaeOld world warblers
Acrocephalus stentoreus Clamorous reed warbler3
Megalurus gramineus Little grassbird
 Number of surveys52430
 No. of species142524
 No. of breeding species135
 Highest counts totalled10942041

The highest number of birds recorded on a single occasion is shown for each species. Breeding species are indicated by an asterisk.

Waterbird abundance was low in all three lakes. Tyiurrtmiirity/Gardner was ranked 83 in abundance out of the 285 wetlands in the reserves surveyed by Jaensch et al. (1988). Kaiupgidjukgidj/Moates and Miialyiin/Angove support even lower abundance (Table 3). The waterbird conservation value of the lakes lies chiefly in the diversity and composition of species.

Species occurring in highest numbers are Eurasian coot, Pacific black duck, Australian shelduck, blue-billed duck, musk duck, red-necked stint, and red-capped plover (scientific names are given in Table 3). The occurrence of most of these species is sporadic, however. Those most frequently observed in Tyiurrtmiirity/Gardner are musk duck (85% of surveys), black swan (85%), and white-faced heron (70%). The most frequently observed species in Kaiupgidjukgidj/Moates are little pied cormorant (70%), little black cormorant (63%), and spotless crake (53%). There were too few surveys of Miialyiin/Angove for this analysis.

Musk duck, darter, little pied cormorant, Pacific black duck, spotless crake, and purple swamphen have been recorded breeding in the Reserve; musk ducks have bred at all three lakes (Table 3). Several other species may breed around the lakes (Jaensch et al. 1988), including Australasian bittern, which is listed under State and Commonwealth legislation as endangered. Kaiupgidjukgidj/Moates Lake area, in particular, is considered to be important habitat for this comparatively rare species (Department of Biodiversity, Conservation and Attractions 2018).

Fish

The freshwater and estuarine fish populations of Two Peoples Bay Nature Reserve have been surveyed on several occasions (current authors in 1990; Morgan et al. 1998, 2006; Morgan and Beatty 2006; N. Coy, unpubl. data), with fish collected from both the Angove and Goodga drainage systems. No fish have been recorded from the Maardjitup Gurlin/Mt Gardner Headland systems. The above surveys, combined with Western Australian Museum records and anecdotal records from several local people with a long-term interest in the area, suggest nine Indigenous freshwater species occur (Table 4).

Table 4.Distribution of Indigenous inland fish species at Two Peoples Bay Nature Reserve.

Scientific nameCommon nameGRMLGLGRAS
Galaxiidae
Galaxias maculatus (Jenyns)Common jollytailXXXXX
Galaxias truttaceus (Valenciennes)Trout minnowXX
Galaxias occidentalis (OgilbyA )Western minnowXXX
Percichthyidae
Nannoperca vittata (Castelnau)Western pygmy perchXX
Nannatherina balstoni (Regan)Balston’s pygmy perchX
Atherinidae
Leptatherina wallacei (Prince Ivanstoff & Potter)Western hardyheadXXX
Mugilidae
Aldrichetta forsteri (Valenciennes)Yellow-eye mulletXXX
Gobiidae
Pseudogobius olorum (Sauvage)Blue-spot gobyXXXXX
Sparidae
Acanthopagrus butcheri (Munro)Black breamXXX
No. of species63657

GR, Goodga River; ML, Kaiupgidjukgidj/Moates Lake; GL, Tyiurrtmiirity/Gardner Lake; AS, Angove system.

A Although reported by Morgan et al. (1998), has not been recorded since, and record needs to be confirmed.

Although not unique, the fish assemblage of the area is noteworthy for supporting common south-west Western Australian species towards the eastern extent of their range, as well as supporting several galaxiids that are restricted to south coast catchments. Pseudogobius olorum (Swan River goby) and Galaxias maculatus (common jollytail) are the most widely distributed species in the Reserve. Morgan et al. (1998) reported Galaxias occidentalis (western minnow) from six locations in the system, however, a subsequent study on galaxiid passage on the Goodga River (Morgan and Beatty 2006) failed to mention this species and so the previous records may have been an error.

The coastal sections of both river systems appear to be nurseries for the euryhaline Leptatherina wallacei (hardyhead), Aldrichetta forsteri (yellow-eye mullet), and Acanthopagrus butcheri (black bream) (Table 4). Prior to 1980, a local family (the Wilsons) netted 40–60 cm long yellow-eye mullet and a variety of small, unidentified ‘bait fish’ (likely G. maculatus) from Tyiurrtmiirity/Gardner Lake several times each year. Acanthopagrus butcheri has been caught in Tyiurrtmiirity/Gardner Lake and Gardner Creek. Although it has not been collected, it is likely that Geotria australis (pouched lamprey) occurs in the Angove and Goodga systems (Miller et al. 2021). Large spawning runs of this species usually occur each winter in nearby King Creek, Waychinicup River, and the Kalgan River.

The presence of Galaxias truttaceus (trout minnow) and Galaxias maculatus in a relatively landlocked situation in the Goodga and Angove rivers is notable. Studies in the eastern states of Australia on G. truttaceus (Humphries 1989) and G. maculatus (Pollard 1971) have shown the former is usually anadromous (going upstream from the sea to spawn) and the latter catadromous (going downstream to the estuary to spawn), although both species can adapt to landlocked situations.

Galaxias maculatus was formerly known only from rivers and lakes between the Goodga River and the Daley River (50 km east of Esperance), with additional records from the Boat Harbour Lakes (Kent River). An intensive survey extended its distribution east by 50 km (Thomas River), west by approximately 40 km (Walpole River), with outlier records from the Harvey River (400 km north) and the Canning River (a further 100 km north; Western Australian Museum record) (Morgan et al. 2006).

The trout minnow, Galaxias truttaceus Valenciennes, 1846, is known from Western Australia, South Australia, Tasmania, and Victoria, and King, Flinders, and Clarke islands in Bass Strait (Allen et al. 2002). Although Western Australian populations of the species were originally described as a discrete taxon (Galaxias truttaceus hesperius Whitely, 1944), more recent studies synonymise G. truttaceus hesperius with G. truttaceus. Notwithstanding this, G. truttaceus hesperius is listed federally as ‘critically endangered’ under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act), and ‘endangered’ by the Western Australian Government under the Biodiversity Conservation Act 2016 (BC Act). The critically endangered Western Australian population of Galaxias truttaceus has been categorised by Allen (1982) as ‘our rarest species of native minnow’, and is known currently from the Goodga, Angove and King rivers in the south-west, with outlying, more western occurrence in the Kent River catchment (Colman 2010). Additional populations occur in south-eastern Australia but genetic and ecological investigations (Morgan et al. 2016) indicated there is limited contemporary gene flow between the eastern and western populations and concluded that the south-west population should be considered an evolutionary significant unit. In contrast to many eastern populations that are diadromous, all western populations are potamodromous. Adults live and spawn in riverine habitats and larvae drift downstream to coastal lakes, where they spend several months, before undertaking a distinct upstream recruitment migration as juveniles to colonise riverine habitats (Morgan and Beatty 2006; Morgan et al. 2016).

Goodga River also harbours the scarce Nannatherina balstoni (Balston’s pygmy perch) (Allen 1982, 1989), listed as ‘vulnerable’ under both the BC and EPBC Acts. This is another species that has experienced range contraction. Christensen (1982) collected it at only four of 120 sampling sites along the south coast hinterland between Augusta and Albany.

There are no confirmed records, but there are anecdotal reports of both Oncorhynchus mykiss (rainbow trout) and Perca fluviatilis (redfin perch) occasionally breaking the surface of Kaiupgidjukgidj/Moates Lake. Rainbow trout were first introduced to the Two Peoples Bay area in 1913 and were sporadically released in the Angove and Goodga systems by the Acclimatisation Society of Western Australia and the Albany, Denmark and Plantagenet Acclimatisation Society until after the Reserve was gazetted in 1967. Both Oncorhynchus mykiss and Salmo trutta (brown trout) maintain self-sustaining populations in nearby King Creek and O. mykiss also occurs in the Kalgan and Waychinicup Rivers (Lenanton 1974).

Both the Angove and Goodga rivers have relatively high V-notch weirs in their upper reaches (Fig. 4), which are barriers to upstream fish passage, with no fish recorded upstream of either the Angove (A. Storey, unpubl. data) or Goodga weirs (Morgan and Beatty 2006) in early surveys. A vertical slot fishway, designed to function during low flows to coincide with the upstream spawning migration of Galaxias truttaceus, was constructed on the Goodga Weir in 2003. Subsequent monitoring showed upstream movement of G. truttaceus and G. maculatus through the fishway and into the upper reaches of the Goodga, providing additional valuable habitat to both species (Morgan and Beatty 2006).

Aquatic invertebrates

Samples of aquatic invertebrates were collected from the major flowing (Angove and Goodga rivers, West and Websters gullies) and standing (Miialyiin/Angove, Tyiurrtmiirity/Gardner, and Kaiupgidjukgidj/Moates lakes) waterbodies in the Two Peoples Bay area in June 1990 and February 1991 (Fig. 1). Additional samples of Cladocera were collected from the three lakes in September 1991 (see Storey et al. 1993 for details of sampling). Standard sampling techniques were used with 250 μm mesh nets in streams and both 50 μm and 250 μm mesh nets in lakes.

Lakes

At least 248 species of aquatic invertebrate were collected (Appendix 1, Fig. 8). The lakes contained more species (171) than streams, with 72 taxa occurring in Tyiurrtmiirity/Gardner Lake, 97 in Miialyiin/Angove and 85, in Kaiupgidjukgidi/Moates Lake (Table 5). Twelve per cent of the invertebrate fauna was common to all three lakes.

Fig. 8.

Microinvertebrates collected at Two Peoples Bay Nature Reserve. (a) Copepod Paracyclops chiltoni, (b) cladoceran Macrothrix cf. breviseta, (c) ostracod Alboa worooa, (d) rotifer Platyais quadricornis, (e) copepod Gladioferans imparipes, (f) cladoceran Dunhevedia crassa. Scale bars = 0.1 mm. (Credit: J. McRae).


PC24094_F8.gif
Table 5.Numbers of aquatic invertebrates (excluding Protozoa) and the percentages of microinvertebrate species collected from lakes and other still waterbodies in different studies in Australia.

 By siteFor survey overall
TotalR + MCMCTotalR + MCMC
This study84 (72–96)53 (49–59)33 (29–39)1655732
Edward et al (1994)39 (22–57)21 (8–43)21115
Davis et al. (1993)53 (18–95)28 (18–45)25329
Pinder et al. (2004)39 (0–107)33 (0–70)27 (0–67)9934829
Halse et al. (2000)4924733
Pinder et al. (2010)10113818
Timms (1993)1063329
Timms (1998)334236

Total, mean (plus range) of number of species collected; R + MC, mean percentage (plus range) of rotifers and microcrustaceans; MC, mean percentage (plus range) of microcrustaceans.

Sampling was sufficiently standardised to show that Tyiurrtmiirity/Gardner Lake contained the greatest biomass of invertebrates (despite lower species richness) and Kaiupgidjukgidi/Moates Lake the least, although biomass in all three lakes was low compared with many wetlands in agricultural parts of the Western Australian Wheatbelt (Pinder et al. 2004) and Swan Coastal Plain (Storey et al. 1993). None of the lakes contained many benthic animals. Chironomids and ostracods, both of which are abundant in most nutrient-enriched lakes, occurred in low numbers. Several species with marine affinities (e.g. Gladioferans imparipes and Schizopera clandestina) occurred in Tyiurrtmiirity/Gardner Lake, reflecting potential seasonal connection to the sea. The occurrence of the harpacticoid copepod S. clandestina is of interest but is perhaps a problematic record; it is the first time this west European species has been recorded in the southern hemisphere. More significantly, the cladoceran Gondwanothrix halsei collected from Miialyiin/Angove Lake represents a new family related to Macrothricidae (Van Damme et al. 2007) and highlights, together with the work of Frey (1998), that endemism in the cladoceran fauna of south-western Australia is much greater than suggested by Smirnov and Timms (1983). Similarly, more recent examination of the rotifers more widely in south-western Australia in the light of the richness of the Reserve’s lakes has shown that what was considered to be a cosmopolitan group has relatively high endemism in the south-west (Segers and Shiel 2003; Suatoni et al. 2006).

There was substantial focus on microinvertebrates when identifying the animals in Reserve’s lake samples and 57% of the fauna identified were rotifers or microcrustaceans (Table 5). Analysis of the results of other surveys in south-western and eastern Australia suggests microinvertebrates nearly always contribute substantially to invertebrate richness in lentic waterbodies and that surveys targeting only macroinvertebrates usually provide a very incomplete picture of inland aquatic biodiversity. For example, sampling in south-western Australia by Pinder et al. (2004) in the Avon Wheatbelt region and Halse et al. (2000) in a semi-arid area north of the Geraldton Sandplain, collected only slightly fewer than 50% microinvertebrates (Table 5). This suggests that the 40 Swan Coastal Plain lakes sampled by Davis et al. (1993), which on average yielded 53 species, would likely have shown similar or greater richness than the Reserve’s lakes if rotifers and harpacticoid copepods had been identified in that study. Similarly, the omission by Edward et al. (1994) of rotifer identifications and lumping of identification of cyclopoid and harpacticoid copepods to order level in the 23 wetlands sampled along the coast in the Warren region would have significantly reduced reported richness in that study. It is likely that the true richness of these lakes is similar to the Reserve’s lakes. Eastern Australian lakes also appear to have substantial proportions of microinvertebrates, based on sampling of saline lakes in southern Queensland at Lake Wyara (Timms 1998) and the Paroo (Timms 1993) (Table 5). Shiel et al. (1998) reported a very large assemblage (252 species) of rotifers from pools on the Murray River floodplain, though most individual sites had relatively low numbers of species and the proportion of rotifers and other microinvertebrates in the pool communities could not be calculated.

Rivers and creeks

Overall, 110 species were collected from the river and creek sites. Eighty-three species were found in the two ‘lowland’ rivers and 56 in the two headland streams. Fifty-three species were collected from Angove River, with 55, 40, and 43 species taken from Goodga River, West and Webster’s Gullies, respectively. Eleven per cent of the invertebrate fauna was common to all four sites, 23% were recorded only from the two headland streams and 49% was restricted to the two lowland rivers.

All the known major components of the aquatic invertebrate fauna of south-western Australian flowing waters were represented in the rivers and streams of Two Peoples Bay Nature Reserve (Bunn et al. 1986; Storey and Edward 1989; Storey et al. 1990; Growns and Davis 1991, 1994). The absence of decapod crustaceans from the headland streams may reflect an absence of suitable habitats, since these streams were fast flowing, possessed few large pools, had small accumulations of organic matter, and a coarse substratum. The lowland rivers were slow flowing, consisted of large deep pools, exhibited large accumulations of fine organic matter, and supported large populations of decapods.

Values for species richness in winter at each flowing water site (23–36 species) were mostly higher than reported by Bunn et al. (1986) for winter samples from 10 perennial ‘stream’ sites in the Wungong and North Dandalup catchments south-east of Perth (18–26 taxa). The higher values may be the result of different sampling methods, particularly since Bunn et al. (1986) sampled only riffle zones, whereas the present study sampled all major habitats, but also reflect the richness of the south coast aquatic fauna.

Introduced species

According to Morrissy (1978), marron Cherax cainii are not indigenous to the drainage systems of Two Peoples Bay Nature Reserve. He reports Fisheries Inspector Goodlad stating in 1939 ‘There are places just outside Albany where marron have been put in by private persons. Angove Creek for instance’ and was told of another translocation from waters west of Albany into Kaiupgidjukgidi/Moates Lake in about 1940. Although marron are now abundant in Goodga River and Kaiupgidjukgidi/Moates Lake, the average size caught by marroners decreased during the 1980s, most likely because of fishing pressure (N. Morrissy, pers. comm.).

The introduced yabby Cherax destructor was not evident in the waters of the Reserve in the early 1990s, but had reputedly been released into nearby farm dams (D. Wilson, pers. comm.). In the long-term this species, with its greater fecundity and environmental tolerance, could replace the Indigenous freshwater crayfishes of the Reserve (Lake and Sokol 1986). According to Morrissy (pers. comm.) most farmers in the region are unaware of the animals’ introduced status and misname it as the endemic koonac (C. plebejus or C. preissii).

Conclusion

The aquatic ecosystems of Two Peoples Bay Nature Reserve are important features. All systems are relatively undisturbed, with the catchments of the streams on Maardjitup Gurlin/Mt Gardner headland being entirely within the Reserve. Long-term collection of data on water chemistry and the aquatic fauna of the rivers, creeks and lakes in the Reserve can provide benchmark information with which to assess impacts of disturbances such as land clearing on aquatic systems elsewhere on the south coast of Western Australia.

Miialyiin/Angove, TyiurrtmiirityGardner, and Kaiupgidjukgidi/Moates Lakes support moderate diversity, albeit low abundance of waterbirds, and provide habitat for the endangered Australasian bittern. The Goodga and Angove systems also provide most of the known habitat for the genetically-distinct Western Australian population of the critically endangered Galaxias truttaceus. The systems contain high numbers of aquatic invertebrate species with high diversity of rotifers and cladocerans, including occurrence of the unusual Gondwanotrichidae family of cladocerans. The collection of a rich microinvertebrate community in the Reserve’s lakes in 1990–1991 has had a major impact on the design of many subsequent aquatic invertebrate surveys in Western Australia (Halse et al. 2000, 2014; Pinder et al. 2004, 2010). Their taxonomic focus was broadened beyond macroinvertebrates to routinely include rotifers, cladocerans, ostracods and copepods and to undertake species level identifications.

The conservation values of the Reserve’s inland aquatic systems are not limited to invertebrates, however, and there is a need for more information about fish as well as microinvertebrates to fully understand conservation values and plan management. The distributions and ecology of Galaxias truttaceus and Nannatherina balstoni should be a focus for fish surveys, and further surveys to complete the list of species in rivers, creeks, and lakes are important for aquatic invertebrates.

Generally in south-western Australia, the greatest threat to the invertebrate, fish, and waterbird faunas of the aquatic systems is a reduction in water quality or quantity (Halse et al. 2003; Atkinson et al. 2021). The headland streams appear to be at no risk from external factors other than fire and changing climate. The likely extent of impacts from future climate change are unclear. Based on data from the Bureau of Meteorology annual rainfall at Albany has shown no significant change since 1877, although there appears to be a slight downward trend (data from Bureau of Meteorology, station 9500). Water quality in Angove and Goodga Rivers and the lakes appears to have been little affected by agricultural clearing. However, further land clearing or intensified agricultural activities in the catchments may impact on water quality. Agricultural development has increased salinity levels in the adjacent Kalgan River, Waychinicup River, and King Creek catchments (Schofield et al. 1988). Another possible impact on the Angove system is reduction of flow as a result of water extractions from the pipe-head dam on the Angove River for Albany’s water supply. This has not been investigated in detail but, while at current levels, probably has at most a small effect (McKay and King 2006; Mbaka and Mwaniki 2015).

Data availability

The data that support this study are available in the article and accompanying Appendix.

Conflicts of interest

The authors declare that they have no conflicts of interest.

Declaration of funding

This research would not have been possible without the assistance of salaries and operating budgets paid for by the Western Australian Government.

Acknowledgements

We thank Russell Shiel and the late Neil Coy for their very substantial contributions to this paper, Adrian Pinder for providing physico-chemical data about the lakes, Jane McRae for invertebrate photographs and Alan Danks for gentlemanly guidance around Two Peoples Bay Nature Reserve and sharing of his knowledge.

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Appendix 1.Aquatic invertebrate species of the Two Peoples Bay area

Species collected from rivers, creeks, and lakes of the Two Peoples Bay area in 1990 and 1991 (see Storey et al. 1993).


 ARGRWGWbGALGLML
PROTOZOA
Arcella sp. A*
Centropyxis sp. A*
 +Difflugia acuminata (Ehrenberg)*
Difflugia sp. A*
Euglypha sp. A*
 +Lesquereusia spiralis (Ehrenberg)**
ROTIFERA
 Bdelloida sp. A*
Brachionus cf. angularis bidens (Plate)**
Brachionus quadridentatus (Hermann)*
 +Dipleuchalnis propatula (Gosse)**
Euchlanis dilatata (Ehrenberg)*
 +Filinia cf. australiensis (Koste)*
 +Filinia cf. pejleri (Hutchinson)*
 +Filinia sp. A*
 +Heterolepadella ehrenbergi (Perty)*
Keratella javana (Hauer)*
Keratella procurva (Thorpe)*
Keratella sp. A*
 +Lecane noobjupi (Segers & Shiel)*
 +Lecane imbricata (Carlin)**
 +Lecane cf. ohioensis (Herrick)*
 +Lecane signifera (Jennings)*
 +Lepadella rottenburgi (Lucks)*
 +Lepadella triptera (Ehrenberg)*
Lepadella sp. A*
 +Macrochaetus collinsi (Gosse)*
Monommata sp. A*
Monostyla bulla (Gosse)***
Monostyla hamata (Stokes)**
Monostyla lunaris (Ehrenberg)*
 +Monostyla crenata (Harring)**
 +Monostyla furcata (Murray)**
 +Monostyla quadridentate (Ehrenberg)*
 +Monostyla rhophalura (Harring & Myers)*
 +Monostyla sp. nov. A*
 +Notommata sp. nov. A*
Platyias quadricornis (Ehrenberg)*
 +Testudinella amphora (Hauer)*
Testudinella insinuata (Hauer)*
Testudinella nr. patina (Hermann)*
 +Testudinella tasmaniensis (Koste & Shiel)*
Trichocerca elongata (Gosse)*
Trichocerca pusilla (Jennings)*
 +Trichocerca rattus carinata (Ehrenberg)*
 +Trichocerca rattus cristata (Harring)*
Trichocerca sp. A1**
Trichocerca sp. A2*
Trichotria tetractis (Ehrenberg)**
 NEMATODA
 Nematoda spp.SSBBB
MOLLUSCA
 GASTROPODA
 Ancylidae
Ferrissia petterdi (Johnston)WBBW
 Planorbidae
Physastra sp. AB
ANNELIDA
 Oligochaeta spp.BBBWBBB
ARTHROPODA
ORIBATIDA
 Oribatida spp.WBB
HYDRACARINA
 Arrenuridae
Arrenurus sp. AS
Arrenurus sp. BS
 Oxidae
Flabellifrontipoda sp.AW
Limnochares australica (Lundblad)S
Oxus sp. AWBB
Frontipoda sp. AS
 Unionicolidae
Koenikea sp. AB
Newmania sp. AS
 Hygrobatidae
Corticarus sp. AW
Gretacarus sp. ASS
Coaustraliobates sp. AS
 Halacaridae
 Halacaridae sp. AW
Soldanellonyx sp. AS
CRUSTACEA
CLADOCERA
 Sididae
Latonopsis cf. brehmi (Petkovski)S
 Chydoridae
Alonella cf. clathratula (Sars)S
Biapertura cf. affinis (Leydig)W
Biapertura cf. rigidicaudis (Smirnov)W
 +Biapertura cf. setigera (Brehm)SS
 +Biapertura sp. M1B
Camptocercus cf. australis (Sars)S
 +Chydorus sp. ABWS
Dunhevedia crassa (King)W
Ephemeroporus barroisi (s. l. Frey)S
 +Euryalona cf. orientalis (Daday)W
Graptoleberis cf. testudinaria (Fischer)W
Monope reticulata (Henry)S
 +cf. Pleuroxus sp. AWW
 +Rhynchochydorus cf. australiensis (Smirnov & Timms)S
 +Chydoridae sp. A1B
 +Chydoriae sp. M2S
 Macrothricidae
Echinisca sp. AW
Ilyocryptus sp. AW
Macrothrix cf. breviseta (Smirnov & Timms)B
Neothrix armata (Gurney)B
 +Gondwanotrichidae
 +Gondwanothrix halsei (Van Damme, Shiel & Dumont)S
 Daphniidae
Scapholeberis cf. kingi (Sars)SS
Simocephalus exspinosus australiensis (Dana)S
Simocephalus sp. AW
 Bosminidae
Bosmina meridionalis (Sars)WB
Bosmina sp. AW
OSTRACODA
 Ostracoda sp. 287S
 Cyprididae
Cypretta baylyi (McKenzie)BW
 +Ilyodromus sp. 255BS
Kennethia cristata (De Deckker)BWW
Alboa worooa (De Deckker)SW
Mesocypris aff. tasmaniensis (De Deckker)S
 Darwinulidae
 Darwinulidae sp.WS
 Limnocytheridae
Gomphodella maia (De Deckker)BB
Limnocythere mowbrayensis (Chapman)W
 +Paralimnocythere sp. nov.BS
 Candonidae
Candonopsis tenuis (Brady)WWS
COPEPODA
 Centropagidae
Calamoecia attenuata (Fairbridge)BB
Calamoecia tasmanica (s. l. Smith)S
Calamoecia tasmanica subattenuata (Fairbridge)BWB
Gladioferens imparipes (Thomson)SB
 Cyclopidae
Eucyclops australiensis (Morton)SSSS
Halicyclops sp. AS
Microcyclops sp. AWWW
Thermocyclops sp. ABWW
Macrocyclops albidus (Jurine)SWWB
Paracyclops chiltoni (Thomson)SS
Paracyclops sp. AWS
 Canthocamptidae
 +Canthocamptidae sp. AWW
 Canthocamptidae sp. 15SS
 Canthocamptidae sp. 16S
 Ameiridae
  Leptomesochra sp. AS
  Nitocra sp. ASB
 Laophontidae
  Onychocamptus bengalensis (Sewell)S
  +Onychocamptus chathamensisWW
 Diosaccidae
  +Schizopera clandestina (Klie)W
DECAPODA
 Parastacidae
Cherax plebejus (Hess)BWW
Cherax quinquecarinatus (Gray)BSWS
Cherax tenuimanus (Smith)WBWS
 Palaemonidae
Palaemonetes australis (Dakin)BBBB
AMPHIPODA
 Ceinidae
Austrochiltonia subtenuis (Hurley)WBB
 Gammaridae
Perthia branchialis (Nicholls)BSBS
Perthia acutitelson (Straskraba)W
Uroctena setosa (Nicholls)B
 Talitroidea
Agilestia sp. ASS
Austrotroides pectinalis (Friend)S
ISOPODA
 Philosciidae
 ?Laevophiloscia sp. AS
 ?Plymophiloscia sp. ASW
 Styloniscidae
Styloniscus australiensis australiensis (Vandel)SW
INSECTA
MEGALOPTERA
 Chauliodidae
Archichauliodes cervulus (Theischinger)B
LEPIDOPTERA
Lepidoptera sp. BS
DIPTERA
 Simuliidae
Cnephia tonnoiri tonnoiri (Drummond)BWWW
Austrosimulium furiosum (Skuse)BW
 Culicidae
Aedes sp. AW
Anopheles annulipes (Walker)S
Culex australicus (Dobrotworsky & Drummond)SS
Culex globocoxitus (Dobrotworsky)W
 Chironomidae
 Tanypodinae
Coelopynia pruinosa (Freeman)S
Paramerina levidensis (Skuse)SSBBSWB
Macropelopia dalyupensis (Freeman)WS
Macropelopia sp. V9W
 ?Ablabesmyia sp. V10B
 Tanypodinae sp. V20S
 Orthocladiinae
Corynoneura ?scutellata (Winnertz)W
Cricotopus annuliventris (Skuse)BBWB
Stictocladius uniserialis (Freeman)W
Nanocladius sp. VCD7W
Thienemanniella sp. V19BWWW
Limnophyes pullulus (Skuse)SBWWB
 ?Limnophyes sp. V31WS
 Orthocladiinae sp. V11BBW
 Orthocladiinae sp. VTPB1WW
 Orthocladiinae sp. VTPB2S
 Orthocladiinae sp. VTPB3S
 Orthocladiinae sp. V59B
 Orthocladiinae sp. AWW
 Chironominae
Cladopelma curtivalva (Kieffer)SSS
 ?Harnischia sp. VTPB4SS
Polypedilum sp. V3BSBWWB
Polypedilum sp. V33BB
Polypedilum sp. AS
Procladius paludicola (Skuse)SSSS
Riethia sp. V4BBSS
Riethia sp. V5BBSS
Cladotanytarsus ?mancus (Walker)SS
Tanytarsus sp. V6BBWBWB
Tanytarsus sp. ASS
Tanytarsus sp. BS
Stempellina ?australiensis (Freeman)BSBS
 ?Paratendipes sp. V12W
Rheotanytarsus sp. V18SWS
Cryptochironomus griseidorsum (Kieffer)BSW
Stenochironomus sp. V27B
Chironomus aff. alternans (Walker)SS
 Tanytarsini sp. AWW
 Chironomini sp. V21S
Dicrotendipes sp. V47S
 Tipulidae
 Limoniinae sp. ASBBW
 Limoniinae sp. BBW
 ?Pedicia sp. AWW
 Tipulinae sp. ASBS
 Ceratopogonidae
 Ceratopogonidae sp. AWWB
 Ceratopogonidae sp. BBSBWBW
 Ceratopogonidae sp. CW
 Ceratopogonidae sp. DW
 Ceratopogonidae sp. FS
 Ceratopogonidae sp. GS
 Ceratoogonidae sp. KS
 Ceratopogonidae sp. OS
 Stratiomyidae
 Stratiomyidae sp. AW
 Stratiomyidae sp. BS
 Dolichopodidae
 Dolichopodidae sp. AW
 Emphididae
 Empididae sp. ASS
 Empididae sp. BSSS
ZYGOPTERA
 Coenagrionidae
Ischnura sp. AWW
Ischnura aurora (Brauer)S
ANISOPTERA
 Aeschnidae
Austroaeschna anacantha (Tillyard)BBBBS
 Corduliidae
Lathrocordulia metallica (Tillyard)S
 Corduliidae sp A (immature)W
Hemicordulia tau (Selys)S
 Gomphidae
Austrogomphus collaris (Hagen)B
 Libellulidae
Diplacodes haematodes (Burmeister)W
 Synthemidae
Synthemis macrostigma occidentalis (Tillyard)W
Synthemis cyanitincta (Tillyard)S
HEMIPTERA
 Veliidae
 Veliidae sp. AW
 Corixidae
Agraptocorixa sp. AS
Micronecta robusta (Hale)W
EPHEMEROPTERA
 Leptophlebiidae
Nyungara bunni (Dean)B
Bibulmena kadjina (Dean)WBB
Neboissophlebia occidentalis (Dean)SS
 Caenidae
Tasmanocoenis tillyardi (Lestage)BW
PLECOPTERA
 Gripopterygidae
Newmanoperla exigua (Kimmins)W
 Gripopterygidae sp. A (immature)W
TRICHOPTERA
 Hydropsychidae
Smicrophylax australis (Ulmer)BB
 Ecnomidae
Ecnomina scindens/trulla/merga groupB
Ecnomus pansus/turgidus complexBWS
 Leptoceridae
Condocerus aptus (Neboiss)BB
Lectrides parilis (Neboiss)BSBB
Oecetis spp.SSSS
Triplectides sp. AW
Triplectides australis (Navas)WWB
Notoperata tenax (Neboiss)S
 Hydroptilidae
Hellyethira malleoforma (Wells)SSSS
Oxyethira retracta (Wells)WS
Maydenoptila ?rupina (Neboiss)W
Hydroptila losida (Mosely)S
 Hydrobiosidae
Taschorema pallescens (Banks)BBBB
 Polycentropodidae
Plectrocnemia ?exima (Neboiss)S
COLEOPTERA
 Dytiscidae
Antiporus femoralis (Boheman)S
Lancetes lanceolatus (Clark)WW
Liodessus dispar (Sharp)W
Megaporus howitti (Clark)W
Megaporus solidus (Sharp)S
Necterosoma darwini (Babington)B
Necterosoma sp. B (larva)SS
Rhantus suturalis (MacLeay)SW
Sternopriscus browni (Sharp)W
Sternopriscus sp. AS
Platynetes decempunctatus (Fabricius)S
 Helodidae
 Helodidae sp. ASSBBW
 Hydrophilidae
 Hydrophilidae sp. IS
No. of species53554043967285

S, summer; W, winter; B, both seasons. *sampled only in summer. First records for Western Australia marked with +. Voucher specimen names are used for some undescribed species (e.g. Biapertura sp. M1). AR, Angove River; GR, Goodga River; WG, West Gully; WbG, Webster’s Gully; AL, Miialyiin/Angove Lake; GL, Tyiurrtmiirity/Gardner Lake; ML, Kaiupgidjukgidj/Moates Lake.