Water regime and salinity changes in wetland macroinvertebrate communities

The research successfully showed how biological communities change in wetlands that are affected by salinity and altered water regimes as a result of irrigation and river regulation. As an outcome of the study, recommendations have been made for the future management of wetlands in the Kerang region in northern Victoria.

The evolution of the temporary protection visa regime in Australia

While the Temporary Protection Visa (TPV) regime was formally introduced in October 1999 by the Howard Government, the concept of temporary protection was not totally alien to the Australian humanitarian landscape. Earlier examples reflected a standard use of temporary protection as a complementary or interim protection mechanism, offering short-term group-based protection where individual assessment under the 1951 Convention was both impractical and untimely. This paper focuses on the wider and more controversial changes in the use of temporary protection mechanisms that were to follow with the introduction of the TPV in 1999, which offered substitute protection for individually assessed Convention refugees who had arrived onshore without valid travel documents. It examines the history and evolution of the TPV policy regime from 1999 to the announcement of its abolition in 2008, arguing that the introduction and subsequent development of the policy may be understood as a product of a conservative, exclusionist political climate in Australia, following the unprecedented impact of the populist One Nation party in 1998, and later, the impact of September 11th. It also examines later amendments to the regime as a response to growing domestic disquiet about the impacts of the policy, and the abolition of the TPV policy under a new Australian government elected in late 2007.

Improving our superannuation regime : a post-Henry review look at superannuation taxation, raising superannuation balances and longevity insurance

This paper examines what, if any changes should be made regarding certain aspects of the superannuation system. Specifically, it looks at possible changes to the superannuation tax regime, measures intended at increasing superannuation balances, as well as policies aimed at improving the price and availability of retirement income streams. The recommendations of the final report of the Henry Review on these issues are also critically evaluated. The paper finds that a greater targeting of superannuation tax concessions towards middle and lower income earners would make the system more equitable and achieve other desirable goals such as increasing voluntary savings. Furthermore, the available evidence suggests that the current mandatory contributions rate of 9% is adequate, and a higher contributions rate is likely to have more costs than benefits. On the issue of superannuation income streams, the article finds that whilst taxpayers should continue to be allowed to take their superannuation as a lump sum, policies should be implemented to make lifetime annuities more readily available and better value for money. The Henry Review's recommendations on these issues, with some exceptions, are for the most part sound and based on logic.

Late palaeozoic global changes affecting high-latitude environments and biotas : an introduction

The Late Palaeozoic Ice Age (LPIA), spanning approximately from ~320 Ma (Serpukhovian, late Mississippian) to 290 Ma (mid-Sakmarian, Early Permian), represents the vegetated Earth’s largest and most long-lasting regime of severe and multiple glaciations, involving processes and patterns probably comparable to those of the Last Ice Age. Accompanying the LPIA occurred a number of broadly synchronous global environmental and biotic changes. These global changes, as briefly reviewed and summarized in this introductory paper, comprised (but are not limited to) the following: massive continental reorganization in the lead up to the final assembly of Pangea resulting in profound changes in global palaeogeography, palaeoceanography and palaeobiogeogarphy; substantially lowered global atmospheric carbon dioxide concentrations (pCO₂), coupled with an unprecedented increase in atmospheric oxygen concentrations reaching Earth's all-time high in its last 600 million year history; sharp global temperature and sea-level drops (albeit with considerable spatial and temporal variability throughout the ice age); and apparently a prolonged period of global sluggish macro-evolution with both low extinction and origination rates compared to other times. In the aftermath of the LPIA, the world's climate entered into a transitional climate phase through the late Early to Middle Permian before its transformation into a greenhouse state towards the end-Permian. In recent years, considerable amount of data and interpretations have been published concerning the physical evidence in support of the LPIA, its broad timeframe and eustatic and ecosystem responses from the lower latitudes, but relatively less attention has been drawn to the impact of the ice age on late Palaeozoic high-latitude environments and biotas. It is with this mission in mind that we have organized this special issue, with the central focus on late Palaeozoic high latitude regions of both hemispheres, that is, Gondwana and northern Eurasia. Our aim is to gather a set of papers that not only document the physical environmental changes that had occurred in the polar regions of Gondwana and northern Eurasia during the LPIA, but also review on the biotic responses at different taxonomic, ecological and spatial scales to these physical changes in a refined chronological timeframe.

This introductory paper is designed to provide a global context for the special issue, with a brief review of key late Palaeozoic global environmental changes (including: changes in global land-sea configurations, atmospheric chemistry, global climate regimes, global ocean circulation patterns and sea levels) and large -scale biotic (biogeographic and evolutionary) responses, followed by a summary of what we see as unresolved scientific issues and various working hypotheses concerning late Palaeozoic global changes and, in particular, the LPIA, as a possible reference to future research.

Changes in catch rates and length and age at maturity, but not growth, of an estuarine plotosid (cnidoglanis macrocephalus) after heavy fishing

The hypothesis that heavy fishing pressure has led to changes in the biological characteristics of the estuary cobbler (Cnidoglanis macrocephalus) was tested in a large seasonally open estuary in southwestern Australia, where this species completes its life cycle and is the most valuable commercial fish species. Comparisons were made between seasonal data collected for this plotosid (eeltail catfish) in Wilson Inlet during 2005-08 and those recorded with the same fishery-independent sampling regime during 1987-89. These comparisons show that the proportions of larger and older individuals and the catch rates in the more recent period were far lower, i.e., they constituted reductions of 40% for fish ≥430 mm total length, 62% for fish ≥4 years of age, and 80% for catch rate. In addition, total mortality and fishing-induced mortality estimates increased by factors of ~2 and 2.5, respectively. The indications that the abundance and proportion of older C. macrocephalus declined between the two periods are consistent with the perception of long-term commercial fishermen and their shift toward using a smaller maximum gill net mesh to target this species. The sustained heavy fishing pressure on C. macrocephalus between 1987-89 and 2005-08 was accompanied by a marked reduction in length and age at maturity of this species. The shift in probabilistic maturation reaction norms toward smaller fish in 2005-08 and the lack of a conspicuous change in growth between the two periods indicate that the maturity changes were related to fishery-induced evolution rather than to compensatory responses to reduced fish densities.

Regime change in Australian maternity hospitals

Contemporary attempts to ‘organise’ risk and manage uncertainty are remaking many ‘industrial-era’ institutions – including maternity hospitals. Health policies are encouraging a shift away from hierarchical, medically dominated structures towards new governance systems and ‘women-centred’ care, often led by midwives. To understand the resulting contestation, in this article we argue for a wider conceptual frame than a focus on neo-liberal state regulation of the professions. We utilise theories of the ‘second modernity’, in particular those concerning socio-cultural changes associated with shifts in risk regimes, to interpret findings from qualitative research studies undertaken in Australian maternity hospitals. Whereas analysis confined to macro or institutional levels emphasises stability and hegemony, we demonstrate that when cultural and interactional levels are examined, considerable fluidity and uncertainty in the identification and negotiation of risk is evident, resulting in new work practices with inevitable shifts in professional identities and allegiances.

The effects of topographic variation and the fire regime on coarse woody debris: insights from a large wildfire

Coarse woody debris (CWD) is a common structural component of terrestrial ecosystems, and provides important habitat for biota. Fires modify the distribution of CWD, both spatially and temporally. Changes in fire regimes, such as those arising from prescribed burning and changing climatic conditions, make it critical to understand the response of this resource to fire. We created a conceptual model of the effects of fire on logs and dead trees in topographically diverse forests in which trees often survive severe fire. We then surveyed paired sites, in a damp gully and adjacent drier slope, ~3.5. years after a large wildfire in south-eastern Australia. Sites were stratified by fire severity (unburnt, understorey burnt and severely burnt), and fire history (burnt ≤3. years or ≥20. years prior to the wildfire). Both components of the fire regime influenced CWD availability in gullies. Severe wildfire and fire history ≤3. years reduced the volume of small logs (10-30. cm diameter) in gullies, while severe wildfire increased the number of large dead trees in gullies. CWD on slopes was not affected by fire severity or history at ~3.5. years post-fire. Log volumes on slopes may recover more quickly after wildfire through rapid collapse of branches and trees. Gullies generally supported more logs than slopes, but longer inter-fire intervals in gullies may allow fuel loads to accumulate and lead to comparatively larger fire impacts. Given that fire severity and fire interval are predicted to change in many fire-prone ecosystems in coming decades, this study highlights the importance of understanding the interacting effects of multiple components of the fire regime with landscape structure. In particular, variation in fire interval and fire severity in relation to topographic position will influence the pattern of accumulation of coarse woody debris across the landscape, and therefore the structure and quality of habitats for biota.

Evaluating temporal changes in hydraulic conductivities near karst-terrain dams: Dokan Dam (Kurdistan-Iraq)

Dam sites provide an outstanding opportunity to explore dynamic changes in the groundwater flow regime because of the high hydraulic gradient rapidly induced in their surroundings. This paper investigates the temporal changes of the hydraulic conductivities of the rocks and engineered structures via a thorough analysis of hydrological data collected at the Dokam Dam, Iraq, and a numerical model that simulates the Darcian component of the seepage. Analysis of the data indicates increased seepage with time and suggests that the hydraulic conductivity of the rocks increased as the conductivity of the grout curtain decreased. Conductivity changes on the order of 10-8m/s, in a 20-yr period were quantified using the numerical analysis. It is postulated that the changes in hydraulic properties in the vicinity of Dokan Dam are due to suspension of fine materials, interbedded in small fissures in the rocks, and re-settlement of these materials along the curtain. Consequently, the importance of the grout curtain to minimize the downstream seepage, not only as a result of the conductivity contrast with the rocks, but also as a barrier to suspended clay sediments, is demonstrated. The numerical analysis also helped us to estimate the proportion of the disconnected karstic conduit flow to the overall flow.