Brian V. Timms

Saline lakes of the Paroo, inland New South Wales, Australia

Twenty-five lakes from fresh to crystallizing brine in the semi-desert of northwestern New South Wales, Australia, were studied regularly for 27 months. The lakes are small, shallow and ephemeral. Chemically waters are mainly of the NaCl type. Seventy-four species of invertebrate occur in saline waters (>3 g 1-1) with crustaceans such as Parartemia minuta, Apocyclops dengizicus, Daphniopsis queenslandensis, Diacypris spp. and Reticypris spp. dominant, particularly at higher salinities. The insects Tartytarsus barbitarsis and Berosus munitipennis are also important in meso- and hypersaline lakes. They are joined in hypo- and mesosaline waters by many others, including more beetles, odonatans, trichopterans, pyralids, notonectids, and corixids. Species richness declines with increasing salinity. There is a prominent inland faunal component mainly of crustaceans, including P. minuta, D. queenslandensis, R. walbu, Trigonocypris globulosa and Moina baylyi.

A study of benthic communities in some shallow saline lakes of western Victoria, Australia

The summer benthos of 24 lakes ranging from 1–204 g l-1 salinity contained 27 species of macroinvertebrates. The worm Antipodrilus timmsi, the ostracod Mytilocypris splendida, the amphipod Austrochiltonia subtenuis, the chironomids Procladius spp. and Chironomus duplex aand the snail Coxiella striata were common at lower salinities (3—ca. 30 g l-1) while the crustaceans Australocypris robusta and Haloniscus searlei, the chironomid Tanytarsus barbitarsis and a ceratopogonid larva dominated in salinities ca. 20–100 g l-1. Small ostracods were common from 40–150 g l-1. Diversity changed little with salinity.Mean dry biomass ranged from 0–3.94 g m-2; distribution between lakes was negatively skewed with a peak around 7 g l-1 salinity. Within many lakes, there was considerable spatial heterogeneity which in some cases seemed to result from different bottom characteristics or to point source enrichment. Many groups contributed to the standing crop at low to moderate salinities, and at high salinities crustaceans were important.The lakes were grouped into two low salinity associations, an association which comprised the Red Rock Lakes and a cluster of highly saline lakes. This reflects the grouping of species into halobiont, halophilic and salt-tolerant freshwater species.

Salt lakes in Australia: present problems and prognosis for the future

Australia is a land of salt lakes and despite low human population density, many lakes are adversely impacted by a range of factors. Secondary salinisation is the most pernicious force degrading lakes, especially in south-west Western Australia where up to 30% of the landscape is predicted to be affected. Mining also impinges on many salt lakes in this state, mainly through the dewatering of saline groundwater. Exploitation of groundwater for irrigation caused some lakes in Victoria, Australia, to dry, especially the significant Red Rock Complex. Global climate change will result in new water balances in endorheic lakes, with most having less water, particularly the seasonal lakes of southern Australia. This has already happened in Lake Corangamite, Victoria, but the prime reason is diversion of inflowing floodwater. Consequently, the lake has retreated and become salinised compromising its status as a Ramsar site. Various other lakes suffer from enhanced sedimentation, have introduced biota or their catchments are being disturbed to their detriment. Enlightened management should be able to maintain some important lakes in an acceptable condition, but, for most others, the future is bleak.

15. Animal communities in three Victorian lakes of differing salinity

In faunal studies on salt lakes, attention is often focused on species distribution patterns with respect to salinity (e.g. Beadle 1943; Hussainy 1969; Rawson & Moore 1944). Yet in any series of lakes, other factors such as depth, size, permanency, stratification, to name a few, may influence distribution and abundance, so that it may be difficult to be sure that any patterns observed are not influenced by factors other than salinity. Further, because of logistic problems such studies are usually based on single qualitative collections from each lake.

Biogeography and ecology of Anostraca (Crustacea) in middle Paroo catchment of the Australian arid-zone

Fourteen species of Branchinella and one each of Parartemia, Streptocephalus (Parastreptocephalus) and an undescribed branchipodid genus occur in a limited area (2000 km2) of the Paroo in northwestern New South Wales and southwestern Queensland. Syntopic coexistence was common (55% of collections) but to a large degree species interactions are minimized by habitat factors of turbidity, salinity and length of the wet phase in decreasing order of importance, and by a species factor of relative size. Discrete habitats such as claypans had a similar species composition each time they filled, but creek pools and other connected sites had variable species composition over time. The high biodiversity is explained by the presence of many distinct types of wetlands, each with their own characteristic anostracans.

The Coastal Dune Lakes of Eastern Australia

Most lakes in siliceous dunes in eastern Australia originated through deflation and organic accumulation to form on perched watertables in otherwise porous sand. Salinity is low (<50 mg 1-1), Na+ and Cl- ions are dominant, Ca2+ and HCO3 - ions are almost absent, and the water is acidic (pH <5·0) and humic. Many of the biota are distinctive, including a sparse, desmid-dominated phytoplankton, the limnetic copepod Calamoecia tasmanica, and a few other microcrustaceans, odonates, trichopterans, chironomids and fish. Planarians, rotifers, ostracods, amphipods and molluscs are rarely present. Biological communities tend to be simple so that the result of predator-prey interactions may be obvious. Energy pathways apparently rely on allochthonous organic matter. Community structure and function vary between lakes according to slight differences in physiographical position and hence water chemistry. Six types of dune lake are recognized at present, though more may exist in poorly known regions. Dune lakes are threatened by mining, mobile sand, cultural eutrophication, and exotic biota.

The fairy shrimp genus Branchinella sayce (Crustacea: Anostraca: Thamnocephalidae) in Western Australia, including a description of four new species

The genus Branchinella is diverse in Western Australia, with 18 species, including four new species described here. B. complexidigitata n. sp. is characterized by an intricate frontal appendage, unlike any within the genus. The other three are less remarkable; B. halsei n. sp. is like B. lyrifera, B. kadjikadji n. sp. belongs to the B. affinis group and B. nana n. sp. is similar to B. simplex; similarities are based on frontal appendage and to a lesser extent on the second antennae and penis. Only two species, B. affinis and B. longirostris, are common and widespread; many of the remainder being localized endemics. The high diversity in Western Australia is explained by broad latitudinal range, habitat diversity, and great age and isolation of the landscape.

Further studies on the saline lakes of the eastern Paroo, inland New South Wales, Australia

Continuing studies of 25 shallow lakes in the semi-desert of northwestern New South Wales during drier years revealed greater physicochemical extremes than previously recorded and wider fluctuations in salinity, even in less saline lakes. Earlier data on species composition and species richness were confirmed, with a few new species reported from either further field collections or the hatching of dried lake muds. A summer filling as against almost regular previous autumn-winter fillings made only a minor difference in faunas, though insects and phyllopods, for different reasons, were less prevalent in the drier years. The fauna of these inland saline lakes is not only biogeographically different from those in southern Australia, but is adapted to a more extreme and irregular environment.

Cyclestheria hislopi (Crustacea: Branchiopoda): A group of morphologically cryptic species with origins in the Cretaceous

Cyclestheria hislopi is thought to be the only extant species of Cyclestherida. It is the sister taxon of all Cladocera and displays morphological characteristics intermediate of Spinicaudata and Cladocera. Using one mitochondrial (COI) and two nuclear (EF1α and 28S rRNA) markers, we tested the hypothesis that C. hislopi represents a single circumtropic species. South American (French Guiana), Asian (India, Indonesia, Singapore) and several Australian populations were included in our investigation. Phylogenetic and genetic distance analyses revealed remarkable intercontinental genetic differentiation (uncorrected p-distances COI>13%, EF1α>3% and 28S>4%). Each continent was found to have at least one distinct Cyclestheria species, with Australia boasting four distinct main lineages which may be attributed to two to three species. The divergence of these species (constituting crown group Cyclestherida) was, on the basis of phylogenetic analyses of COI and EF1α combined with molecular clock estimates using several fossil branchiopod calibration points or a COI substitution rate of 1.4% per million years, dated to the Cretaceous. This was when the South American lineage split from the Asian-Australian lineage, with the latter diverging further in the Paleogene. Todays circumtropic distribution of Cyclestheria may be best explained by a combination of Gondwana vicariance and later dispersal across Asia and Australia when the tectonic plates of the two continents drew closer in the early Miocene. The lack of morphological differentiation that has taken place in this taxon over such a long evolutionary period contrasts with the high level of differentiation and diversification observed in its sister taxon the Cladocera. Further insights into the evolution of Cyclestheria may help us to understand the evolutionary success of the Cladocera.

Toward a Global Phylogeny of the “Living Fossil" Crustacean Order of the Notostraca

Tadpole shrimp (Crustacea, Notostraca) are iconic inhabitants of temporary aquatic habitats worldwide. Often cited as prime examples of evolutionary stasis, surviving representatives closely resemble fossils older than 200 mya, suggestive of an ancient origin. Despite significant interest in the group as ‘living fossils’ the taxonomy of surviving taxa is still under debate and both the phylogenetic relationships among different lineages and the timing of diversification remain unclear. We constructed a molecular phylogeny of the Notostraca using model based phylogenetic methods. Our analyses supported the monophyly of the two genera Triops and Lepidurus, although for Triops support was weak. Results also revealed high levels of cryptic diversity as well as a peculiar biogeographic link between Australia and North America presumably mediated by historic long distance dispersal. We concluded that, although some present day tadpole shrimp species closely resemble fossil specimens as old as 250 mya, no molecular support was found for an ancient (pre) Mesozoic radiation. Instead, living tadpole shrimp are most likely the result of a relatively recent radiation in the Cenozoic era and close resemblances between recent and fossil taxa are probably the result of the highly conserved general morphology in this group and of homoplasy.