Artykuły w czasopismach: „Great Artesian Basin”

1

Dafny, Elad. "The Great Artesian Basin: is it that great?" Hydrogeology Journal 24, nr 6 (14.07.2016): 1329–32. http://dx.doi.org/10.1007/s10040-016-1444-5.

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Mazor, Emanuel. "Stagnant aquifer concept Part 1. Large-scale artesian systems— Great Artesian Basin, Australia". Journal of Hydrology 173, nr 1-4 (grudzień 1995): 219–40. http://dx.doi.org/10.1016/0022-1694(95)02706-u.

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3

Fensham, R. J., R. J. Fairfax i P. R. Sharpe. "Spring wetlands in seasonally arid Queensland: floristics, environmental relations, classification and conservation values". Australian Journal of Botany 52, nr 5 (2004): 583. http://dx.doi.org/10.1071/bt03171.

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The vegetation and environmental setting of permanent spring wetlands are described from a survey of 269 spring complexes throughout seasonally arid Queensland. Wetlands associated with springs in the western and southern discharge areas of the Great Artesian Basin are floristically distinct from other spring wetlands. Ordination analysis suggests that the biogeographic regions and the broad geological substrates that support spring wetlands provide a meaningful representation of floristic range. An existing classificatory system that defines ‘regional ecosystems’ on the basis of the biogeographic region and broad geological substrate is adopted to define 15 spring-wetland types in seasonally arid Queensland. The conservation value of the springs is assessed by a scheme that weights plant species populations on the basis of their endemicity and isolation from other populations, demonstrating that both Great Artesian Basin and non-Great Artesian Basin springs have similar conservation values.

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4

Fensham, R. J., i R. J. Fairfax. "Spring wetlands of the Great Artesian Basin, Queensland, Australia". Wetlands Ecology and Management 11, nr 5 (październik 2003): 343–62. http://dx.doi.org/10.1023/b:wetl.0000005532.95598.e4.

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PONDER, W. F., W. H. ZHANG, A. HALLAN i M. E. SHEA. "New taxa of Tateidae (Caenogastropoda, Truncatelloidea) from springs associated with the Great Artesian Basin and Einasleigh Uplands, Queensland, with the description of two related taxa from eastern coastal drainages". Zootaxa 4583, nr 1 (10.04.2019): 1. http://dx.doi.org/10.11646/zootaxa.4583.1.1.

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Species from artesian springs associated with the Queensland Great Artesian Basin that were previously included in the tateid genus Jardinella are included in three new genera, namely Eulodrobia, with six species, five of them new and all from the Eulo Supergroup; Springvalia, with one species from the Springvale Supergroup; and Carnarvoncochlea with two previously-described species, from the Carnarvon Supergroup. The genus Edgbastonia is extended to include eight previously described species, in addition to the type species, and four new species-group taxa from the Barcaldine Supergroup springs; all but the type species are included in the new subgenus Barcaldinia. Three new species from non-artesian springs in north Queensland are included in Edgbastonia, one of them tentatively. Two additional related new genera, both with a single new species, are described from outside the Great Artesian Basin; Conondalia from southeast Queensland and Nundalia from north-eastern New South Wales. The genus Jardinella, previously used for all the Queensland spring tateids, is here restricted to three species found in coastal rivers and streams in northeast Queensland. A molecular phylogenetic analysis using COI and 16S mitochondrial genes in combination suggests that the Queensland Great Artesian Basin taxa may be more closely related to the tateid genera Austropyrgus, Pseudotricula, Posticobia and Potamopyrgus than to the South Australian GAB taxa, thus indicating the separate origins of these two desert spring faunas.

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Henderson, Robert A., i E. Donald McKenzie. "Idanoceras, a new heteromorph ammonite genus from the Late Albian of eastern Australia". Journal of Paleontology 76, nr 5 (wrzesień 2002): 906–9. http://dx.doi.org/10.1017/s0022336000037574.

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The late Albian marine fossil record from eastern Australia derives from the sedimentary succession of the Great Artesian Basin deposited in a vast epicontinental sea which then covered much of the continent (see Frakes et al., 1987). Ammonites of this age are common but their generic diversity is low. Heteromorph assemblages almost exclusively comprise the taxa Myloceras, Labeceras sensu stricto and Labeceras (Appurdiceras) of the Family Labeceratidae that were widely distributed in higher latitudes of the Southern Hemisphere during Late Albian time (see Aguirre Urreta and Riccardi, 1988; Klinger, 1989). Some 19 endemic species of these genera are recorded from the Great Artesian Basin in the present literature (Etheridge, 1892; Whitehouse, 1926; Reyment, 1964) and there are additional undescribed species (Henderson and McKenzie, unpublished data). The Australian Late Albian epicontinental sea was clearly a site of significant speciation for Labeceras and Myloceras and it has been argued that the Great Artesian Basin represents the evolutionary center for these genera (Henderson, 1990).

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7

Noble, JC, MA Habermehl, CD James, J. Landsberg, AC Langston i SR Morton. "Biodiversity implications of water management in the Great Artesian Basin." Rangeland Journal 20, nr 2 (1998): 275. http://dx.doi.org/10.1071/rj9980275.

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The Great Artesian Basin (GAB) underlies a vast, mainly arid, region where most of the indigenous biota are not dependent upon surface water. In contrast, an important minority is dependent on refuges such as mound springs and their associated wetlands. In some parts of the GAB, such as western New South Wales, many springs have either ceased to flow, or are now barely detectable, because the proliferation of artesian waterbores has reduced groundwater pressures. Because of the rarity of species endemic to mound springs, and the damage they have suffered since pastoral settlement, emphasis should be directed towards conservation and possible rejuvenation of these ecosystems. Provision of artificial sources of water allows more widespread grazing by livestock, larger native and feral herbivores, thereby posing threats to native plants and animals that do not use the water. Because of the proliferation of artificial waters and the grazing they allow, terrestrial grazing-sensitive species now appear to be confined to tiny patches in the landscape. Some nature reserves within the GAB retain numerous artificial sources of water. Most of these should be closed over time to reduce negative impacts on grazing-sensitive plants and animals, especially where these species are inadequately protected elsewhere. In those regions where the ratio of artificial to natural waters is still low, consideration should be given to balancing provision of water for livestock with conservation of biological diversity, by maintaining a patchwork of areas remote from water. In regions where the density of artificial waters is high, conservation of biodiversity on freehold and leasehold lands might be enhanced with a mix of approaches accommodating the needs of the biota and the aspirations of landholders, tailored according to land type and condition. Key words: Great Artesian Basin, biological diversity, mound springs, refuges, rare biota, grazing impact, conservation management, groundwater.

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8

Saruwatari, Kazuko, Yukihiro Mizuochi, Yasunori Mahara, Teruyoshi Hatano, Takuma Hasegawa, Hirohisa Kobayashi, Atsushi Ninomiya i in. "The Great Artesian Basin and the Limestone Mound Springs, Australia". Journal of the Geological Society of Japan 110, nr 4 (2004): VII—VIII. http://dx.doi.org/10.5575/geosoc.110.4.vii_viii.

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9

Ordens, Carlos Miraldo, Neil McIntyre, Jim R. Underschultz, Tim Ransley, Catherine Moore i Dirk Mallants. "Preface: Advances in hydrogeologic understanding of Australia’s Great Artesian Basin". Hydrogeology Journal 28, nr 1 (22.01.2020): 1–11. http://dx.doi.org/10.1007/s10040-019-02107-8.

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10

Herczeg, A. L., T. Torgersen, A. R. Chivas i M. A. Habermehl. "Geochemistry of ground waters from the Great Artesian Basin, Australia". Journal of Hydrology 126, nr 3-4 (wrzesień 1991): 225–45. http://dx.doi.org/10.1016/0022-1694(91)90158-e.

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Harris, Kathryn, Vair Pointon i Ryan Morris. "The presence of natural methane in Great Artesian Basin aquifers of the Surat Basin". APPEA Journal 52, nr 2 (2012): 674. http://dx.doi.org/10.1071/aj11088.

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The Surat Basin portion of the Great Artesian Basin (GAB) in Queensland has long been known to contain natural gas from both conventional and CSG sources. Commercial gas extraction from conventional sources target the Evergreen and Precipice Formations, which are among the lowermost of the Surat Basin stratigraphic units; however, evidence exists of methane occurrences in waterbores, which in most cases, access aquifers much shallower than recognised conventional gas or CSG targets. Large-scale development of CSG in the Surat and southern Bowen basins has highlighted the presence of gas in aquifers overlying and underlying the coal measures. Potential issues associated with gas in waterbores include health and safety risks, and the difficulty of establishing baseline groundwater bore conditions against which potential CSG impacts can be compared. Australia Pacific LNG has been investigating the presence of gas in the aquifers across the basin. The program has involved the routine measurement of wellhead gas concentrations and analysis of dissolved gas in waterbores. Stable isotope analysis of the dissolved methane (δ13C-methane and δD-methane) has been undertaken to ‘fingerprint’ aquifer gasses to ascertain their provenance. More recently, δ13C-CO2 has been added to the suite of isotopes. Initial results confirm the presence of natural methane across the study area and in all of the GAB aquifers sampled. Isotopic analysis indicates a distinct difference in isotopic signatures between the methane from the coal measures and that of the overlying aquifers from which most groundwater is extracted.

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12

Sandiford, Mike, Ken Lawrie i Ross S. Brodie. "Hydrogeological implications of active tectonics in the Great Artesian Basin, Australia". Hydrogeology Journal 28, nr 1 (29.10.2019): 57–73. http://dx.doi.org/10.1007/s10040-019-02046-4.

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13

Powell, O. C. "Song of the Artesian Water: aridity, drought and disputation along Queensland's pastoral frontier in Australia". Rangeland Journal 34, nr 3 (2012): 305. http://dx.doi.org/10.1071/rj12014.

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Following the recent discovery of artesian supplies, the Shearers’ Strike of 1891 and the onset of the Federation drought (1895–1902), A. B. ‘Banjo’ Paterson’s Song of the Artesian Water, published in 1896, was written at a time of profound social and environmental upheaval in the ‘bush’ of Australia. In order to better understand the historical encounters between colonial capitalism and semiarid rangeland environments, this paper unpacks the cultural meaning behind Song of the Artesian Water by exploring the interactions between water, scientific knowledge, drought and environmental transformation along the pastoral frontier of Queensland. Banjo Paterson’s poem is used as a framework to provide an historical interpretation of European exploitation of the Great Artesian Basin as well as a framework for current economic uses and environmental threats.

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14

Italiano, F., G. Yuce, I. T. Uysal, M. Gasparon i G. Morelli. "Insights into mantle-type volatiles contribution from dissolved gases in artesian waters of the Great Artesian Basin, Australia". Chemical Geology 378-379 (czerwiec 2014): 75–88. http://dx.doi.org/10.1016/j.chemgeo.2014.04.013.

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15

Akers, Harry F., i Suzette A. T. Porter. "The 1945 - 1955 Queensland Artesian Fluoride Experience: A Unique Phenomenon within the Australian Wool Industry". Historical Records of Australian Science 18, nr 2 (2007): 177. http://dx.doi.org/10.1071/hr07007.

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Inquiries into the diminishing supply of artesian water within the Queensland aspect of the Great Artesian Basin began in 1939. These investigations produced a Queensland phenomenon without Australian precedent in terms of rationale, geographical diversity, and commitment of resources. In some regions, exposure of herds to fluoride emerged as an urgent issue because fluoride was perceived as an invasive, invisible, and odourless 'contaminant' in artesian water. This paper discusses the scientific background to, and management of, concerns over the consumption by stock of artesian water with a high concentration of natural bioavailable fluoride. The Queensland Department of Agriculture and Stock managed the problem by scientific investigation, methodical field study, and the application of research findings to animal husbandry. The practical solutions arrived at involved rotation of stock on an age-related basis to and from certain bore supplies, fencing young sheep away from the artesian supply, fencing young sheep near the bore-head, and limiting the use of supplements.

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16

Fensham, R. J., R. J. Fairfax, D. Pocknee i J. Kelley. "Vegetation patterns in permanent spring wetlands in arid Australia". Australian Journal of Botany 52, nr 6 (2004): 719. http://dx.doi.org/10.1071/bt04043.

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A transect-based quadrat survey was conducted within 11 spring wetlands fed by permanent groundwater flows from the Great Artesian Basin at Elizabeth Springs in western Queensland. Flow patterns within individual wetlands change with sedimentation associated with mound building, siltation of abandoned drains and changes in aquifer pressure associated with artificial extraction from bores. The pattern of floristic groups for the wetland quadrats was poorly related to soil texture, water pH, slope and topographic position. Patterns were most clearly related to wetland age as determined from aerial photography, with a clear successional sequence from mono-specific stands of Cyperus laevigatus on newly formed wetland areas to more diverse wetland assemblages. However, evidence from other Great Artesian Basin springs suggests that succession can also result in reduced species richness where the palatable tall reed Phragmites australis develops mono-specific stands.

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17

Bethke, Craig M., Xiang Zhao i Thomas Torgersen. "Groundwater flow and the4He distribution in the Great Artesian Basin of Australia". Journal of Geophysical Research: Solid Earth 104, B6 (10.06.1999): 12999–3011. http://dx.doi.org/10.1029/1999jb900085.

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Byers, Helen K., Erko Stackebrandt, Chris Hayward i Linda L. Blackall. "Molecular investigation of a microbial mat associated with the Great Artesian Basin". FEMS Microbiology Ecology 25, nr 4 (kwiecień 1998): 391–403. http://dx.doi.org/10.1111/j.1574-6941.1998.tb00491.x.

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Pogge von Strandmann, P. A. E., B. C. Reynolds, D. Porcelli, R. H. James, P. van Calsteren, M. Baskaran i K. W. Burton. "Assessing continental weathering rates and actinide transport in the Great Artesian Basin". Geochimica et Cosmochimica Acta 70, nr 18 (sierpień 2006): A497. http://dx.doi.org/10.1016/j.gca.2006.06.1457.

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Zhang, Min, Shaun K. Frape, Andrew J. Love, Andrew L. Herczeg, B. E. Lehmann, U. Beyerle i R. Purtschert. "Chlorine stable isotope studies of old groundwater, southwestern Great Artesian Basin, Australia". Applied Geochemistry 22, nr 3 (marzec 2007): 557–74. http://dx.doi.org/10.1016/j.apgeochem.2006.12.004.

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21

Radke, Bruce, i Tim Ransley. "Connectivity between Australia’s Great Artesian Basin, underlying basins, and the Cenozoic cover". Hydrogeology Journal 28, nr 1 (4.12.2019): 43–56. http://dx.doi.org/10.1007/s10040-019-02075-z.

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Torgersen, T., M. A. Habermehl i W. B. Clarke. "Crustal helium fluxes and heat flow in the Great Artesian Basin, Australia". Chemical Geology 102, nr 1-4 (grudzień 1992): 139–52. http://dx.doi.org/10.1016/0009-2541(92)90152-u.

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23

Kaushik, Pankaj R., Christopher E. Ndehedehe, Ryan M. Burrows, Mark R. Noll i Mark J. Kennard. "Assessing Changes in Terrestrial Water Storage Components over the Great Artesian Basin Using Satellite Observations". Remote Sensing 13, nr 21 (6.11.2021): 4458. http://dx.doi.org/10.3390/rs13214458.

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The influence of climate change and anthropogenic activities (e.g., water withdrawals) on groundwater basins has gained attention recently across the globe. However, the understanding of hydrological stores (e.g., groundwater storage) in one of the largest and deepest artesian basins, the Great Artesian Basin (GAB) is limited due to the poor distribution of groundwater monitoring bores. In this study, Gravity Recovery and Climate Experiment (GRACE) satellite and ancillary data from observations and models (soil moisture, rainfall, and evapotranspiration (ET)) were used to assess changes in terrestrial water storage and groundwater storage (GWS) variations across the GAB and its sub-basins (Carpentaria, Surat, Western Eromanga, and Central Eromanga). Results show that there is strong relationship of GWS variation with rainfall (r = 0.9) and ET (r = 0.9 to 1) in the Surat and some parts of the Carpentaria sub-basin in the GAB (2002–2017). Using multi-variate methods, we found that variation in GWS is primarily driven by rainfall in the Carpentaria sub-basin. While changes in rainfall account for much of the observed spatio-temporal distribution of water storage changes in Carpentaria and some parts of the Surat sub-basin (r = 0.90 at 0–2 months lag), the relationship of GWS with rainfall and ET in Central Eromanga sub-basin (r = 0.10–0.30 at more than 12 months lag) suggest the effects of human water extraction in the GAB.

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24

Yan, Jiabao, Shaofeng Jia, Aifeng Lv, Rashid Mahmood i Wenbin Zhu. "Analysis of the spatio-temporal variability of terrestrial water storage in the Great Artesian Basin, Australia". Water Supply 17, nr 2 (16.08.2016): 324–41. http://dx.doi.org/10.2166/ws.2016.136.

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The Great Artesian Basin (GAB) in Australia, the largest artesian basin in the world, is rich in groundwater resources. This study analyzed the spatio-temporal characteristics of terrestrial water storage (TWS) in the GAB for 2003–2014 using satellite (Gravity Recovery and Climate Experiment, GRACE) data, hydrological models’ outputs, and in situ data. A slight increase in TWS was observed for the study period. However, there was a rapid increase in TWS in 2010 and 2011 due to two strong La Nina events. Long-term mean monthly TWS changes showed remarkable agreements with net precipitation. Both GRACE derived and in situ groundwater disclosed similar trend patterns. Groundwater estimated from the PCR-GLOBWB model contributes 26.8% (26.4% from GRACE) to the total TWS variation in the entire basin and even more than 50% in the northern regions. Surface water contributes only 3% to the whole basin but more than 60% to Lake Eyre and the Cooper River. Groundwater, especially deeper than 50 meters, was insensitive to climate factors (i.e., rainfall). Similarly, the groundwater in the northern Cape York Peninsula was influenced by some other factors rather than precipitation. The time-lagged correlation analysis between sea surface height and groundwater storage indicated certain correlations between groundwater and sea level changes.

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Robertson, Hannah L., i Nicholas P. Murphy. "16 microsatellite loci for the Australian Great Artesian Basin spring amphipod, Wangiannachiltonia guzikae". Australian Journal of Zoology 61, nr 2 (2013): 109. http://dx.doi.org/10.1071/zo13011.

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454 Next Generation sequencing was used to develop a set of microsatellite markers for the Great Artesian Basin (GAB) amphipod, Wangiannachiltonia guzikae. Primers were designed for 42 microsatellite loci. A total of 22 loci were successfully amplified and 16 characterised using 30 individuals from a single GAB spring population. Across these 16 loci, observed heterozygosity ranged from 0.000 to 0.818 (mean = 0.445) and the number of alleles per locus ranged from 2 to 12 (mean = 6.688). Of these 16 loci, however, only 10 were in Hardy–Weinberg equilibrium, though all 16 loci should be retained for further studies in the event that stochastic events affected equilibrium of this single population.

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26

Iverach, Charlotte P., Dioni I. Cendón, Karina T. Meredith, Klaus M. Wilcken, Stuart I. Hankin, Martin S. Andersen i Bryce F. J. Kelly. "A multi-tracer approach to constraining artesian groundwater discharge into an alluvial aquifer". Hydrology and Earth System Sciences 21, nr 11 (28.11.2017): 5953–69. http://dx.doi.org/10.5194/hess-21-5953-2017.

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Abstract. Understanding pathways of recharge to alluvial aquifers is important for maintaining sustainable access to groundwater resources. Water balance modelling is often used to proportion recharge components and guide sustainable groundwater allocations. However, it is not common practice to use hydrochemical evidence to inform and constrain these models. Here we compare geochemical versus water balance model estimates of artesian discharge into an alluvial aquifer, and demonstrate why multi-tracer geochemical analyses should be used as a critical component of water budget assessments. We selected a site in Australia where the Great Artesian Basin (GAB), the largest artesian basin in the world, discharges into the Lower Namoi Alluvium (LNA), an extensively modelled aquifer, to convey the utility of our approach. Water stable isotopes (δ18O and δ2H) and the concentrations of Na+ and HCO3− suggest a continuum of mixing in the alluvial aquifer between the GAB (artesian component) and surface recharge, whilst isotopic tracers (3H, 14C, and 36Cl) indicate that the alluvial groundwater is a mixture of groundwaters with residence times of < 70 years and groundwater that is potentially hundreds of thousands of years old, which is consistent with that of the GAB. In addition, Cl− concentrations provide a means to calculate a percentage estimate of the artesian contribution to the alluvial groundwater. In some locations, an artesian contribution of up to 70 % is evident from the geochemical analyses, a finding that contrasts with previous regional-scale water balance modelling estimates that attributed 22 % of all inflow for the corresponding zone within the LNA to GAB discharge. Our results show that hydrochemical investigations need to be undertaken as part of developing the conceptual framework of a catchment water balance model, as they can improve our understanding of recharge pathways and better constrain artesian discharge to an alluvial aquifer.

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Fensham, R. J., T. Doyle, M. A. Habermehl, B. Laffineur i J. L. Silcock. "Hydrogeological assessment of springs in the south-central Great Artesian Basin of Australia". Hydrogeology Journal 29, nr 4 (6.04.2021): 1501–15. http://dx.doi.org/10.1007/s10040-021-02335-x.

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Bentley, Harold W., Fred M. Phillips, Stanley N. Davis, M. A. Habermehl, Peter L. Airey, Graeme E. Calf, David Elmore, Harry E. Gove i Thomas Torgersen. "Chlorine 36 dating of very old groundwater: 1. The Great Artesian Basin, Australia". Water Resources Research 22, nr 13 (grudzień 1986): 1991–2001. http://dx.doi.org/10.1029/wr022i013p01991.

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Collerson, Kenneth D., William J. Ullman i T. Torgersen. "Ground waters with unradiogenic 87Sr/86Sr ratios in the Great Artesian Basin, Australia". Geology 16, nr 1 (1988): 59. http://dx.doi.org/10.1130/0091-7613(1988)016<0059:gwwuss>2.3.co;2.

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Petus, Caroline, Megan Lewis i Davina White. "Monitoring temporal dynamics of Great Artesian Basin wetland vegetation, Australia, using MODIS NDVI". Ecological Indicators 34 (listopad 2013): 41–52. http://dx.doi.org/10.1016/j.ecolind.2013.04.009.

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Jones, Chris, David Stanton, Ned Hamer, Stephen Denner, Kavita Singh, Steven Flook i Madeleine Dyring. "Field investigation of potential terrestrial groundwater-dependent ecosystems within Australia’s Great Artesian Basin". Hydrogeology Journal 28, nr 1 (20.12.2019): 237–61. http://dx.doi.org/10.1007/s10040-019-02081-1.

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Harrington, Glenn A., W. Payton Gardner, Brian D. Smerdon i M. Jim Hendry. "Palaeohydrogeological insights from natural tracer profiles in aquitard porewater, Great Artesian Basin, Australia". Water Resources Research 49, nr 7 (lipiec 2013): 4054–70. http://dx.doi.org/10.1002/wrcr.20327.

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Inverarity, Kent, Michael Hatch i Graham Heinson. "Electrical geophysics of carbonate mound spring complexes of the South- Western Great Artesian Basin". ASEG Extended Abstracts 2013, nr 1 (grudzień 2013): 1–4. http://dx.doi.org/10.1071/aseg2013ab190.

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Priestley, Stacey C., Karl E. Karlstrom, Andrew J. Love, Laura J. Crossey, Victor J. Polyak, Yemane Asmerom, Karina T. Meredith, Ryan Crow, Mark N. Keppel i Marie A. Habermehl. "Uranium series dating of Great Artesian Basin travertine deposits: Implications for palaeohydrogeology and palaeoclimate". Palaeogeography, Palaeoclimatology, Palaeoecology 490 (styczeń 2018): 163–77. http://dx.doi.org/10.1016/j.palaeo.2017.10.024.

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Torgersen, T., B. M. Kennedy, H. Hiyagon, K. Y. Chiou, J. H. Reynolds i W. B. Clarke. "Argon accumulation and the crustal degassing flux of40Ar in the Great Artesian Basin, Australia". Earth and Planetary Science Letters 92, nr 1 (luty 1989): 43–56. http://dx.doi.org/10.1016/0012-821x(89)90019-8.

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Torgersen, T., B. M. Kennedy, H. Hiyagon, K. Y. Chiou, J. H. Reynolds i W. B. Clarke. "Argon accumulation and the crustal degassing flux of40Ar in the great Artesian Basin, Australia". Chemical Geology 70, nr 1-2 (sierpień 1988): 42. http://dx.doi.org/10.1016/0009-2541(88)90299-9.

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Pogge von Strandmann, Philip A. E., Don Porcelli, Rachael H. James, Peter van Calsteren, Bruce Schaefer, Ian Cartwright, Ben C. Reynolds i Kevin W. Burton. "Chemical weathering processes in the Great Artesian Basin: Evidence from lithium and silicon isotopes". Earth and Planetary Science Letters 406 (listopad 2014): 24–36. http://dx.doi.org/10.1016/j.epsl.2014.09.014.

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Fairfax, R., R. Fensham, R. Wager, S. Brooks, A. Webb i P. Unmack. "Recovery of the red-finned blue-eye: an endangered fish from springs of the Great Artesian Basin". Wildlife Research 34, nr 2 (2007): 156. http://dx.doi.org/10.1071/wr06086.

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The red-finned blue-eye (Scaturiginichthys vermeilipinnis) is endemic to a single complex of springs emanating from the Great Artesian Basin, Australia. The species has been recorded as naturally occurring in eight separate very shallow (generally <20 mm) springs, with a combined wetland area of ~0.3 ha. Since its discovery in 1990, five red-finned blue-eye (RFBE) populations have been lost and subsequent colonisation has occurred in two spring wetlands. Current population size is estimated at <3000 individuals. Artesian bores have reduced aquifer pressure, standing water levels and spring-flows in the district. There is evidence of spatial separation within the spring pools where RFBE and the introduced fish gambusia (Gambusia holbrooki) co-occur, although both species are forced together when seasonal extremes affect spring size and water temperature. Gambusia was present in four of the five springs where RFBE populations have been lost. Four out of the five remaining subpopulations of RFBE are Gambusia free. Circumstantial evidence suggests that gambusia is a major threat to red-finned blue-eyes. The impact of Gambusia is probably exacerbated by domestic stock (cattle and sheep), feral goats and pigs that utilise the springs and can negatively affect water quality and flow patterns. Three attempts to translocate RFBE to apparently suitable springs elsewhere within the complex have failed. Opportunities to mitigate threats are discussed, along with directions for future research to improve management of this extremely threatened fish and habitat.

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Flook, Steven, Jon Fawcett, Randall Cox, Sanjeev Pandey, Gerhard Schöning, Jit Khor, Dhananjay Singh, Axel Suckow i Matthias Raiber. "A multidisciplinary approach to the hydrological conceptualisation of springs in the Surat Basin of the Great Artesian Basin (Australia)". Hydrogeology Journal 28, nr 1 (21.01.2020): 219–36. http://dx.doi.org/10.1007/s10040-019-02099-5.

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Rey, P. F. "Opalisation of the Great Artesian Basin (central Australia): an Australian story with a Martian twist". Australian Journal of Earth Sciences 60, nr 3 (kwiecień 2013): 291–314. http://dx.doi.org/10.1080/08120099.2013.784219.

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Ogg, C. D., i B. K. C. Patel. "Caloramator australicus sp. nov., a thermophilic, anaerobic bacterium from the Great Artesian Basin of Australia". INTERNATIONAL JOURNAL OF SYSTEMATIC AND EVOLUTIONARY MICROBIOLOGY 59, nr 1 (1.01.2009): 95–101. http://dx.doi.org/10.1099/ijs.0.000802-0.

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Redburn, A. C., i B. K. C. Patel. "Desulfovibrio longreachiisp. nov., a sulfate-reducing bacterium isolated from the Great Artesian Basin of Australia". FEMS Microbiology Letters 115, nr 1 (styczeń 1994): 33–38. http://dx.doi.org/10.1111/j.1574-6968.1994.tb06610.x.

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Perez, Kathryn E., Winston F. Ponder, Donald J. Colgan, Stephanie A. Clark i Charles Lydeard. "Molecular phylogeny and biogeography of spring-associated hydrobiid snails of the Great Artesian Basin, Australia". Molecular Phylogenetics and Evolution 34, nr 3 (marzec 2005): 545–56. http://dx.doi.org/10.1016/j.ympev.2004.11.020.

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Collon, P., W. Kutschera, H. H. Loosli, B. E. Lehmann, R. Purtschert, A. Love, L. Sampson, D. Anthony, D. Cole i B. Davids. "81Kr in the Great Artesian Basin, Australia: a new method for dating very old groundwater". Earth and Planetary Science Letters 182, nr 1 (15.10.2000): 103–13. http://dx.doi.org/10.1016/s0012-821x(00)00234-x.

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Shand, P., A. J. Love, T. Gotch, M. D. Raven, J. Kirby i K. Scheiderich. "Extreme Acidic Environments Associated with Carbonate Mound Springs in the Great Artesian Basin, South Australia". Procedia Earth and Planetary Science 7 (2013): 794–97. http://dx.doi.org/10.1016/j.proeps.2013.03.055.

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Wolaver, Brad D., Stacey C. Priestley, Laura J. Crossey, Karl E. Karlstrom i Andrew J. Love. "Elucidating sources to aridland Dalhousie Springs in the Great Artesian Basin (Australia) to inform conservation". Hydrogeology Journal 28, nr 1 (23.12.2019): 279–96. http://dx.doi.org/10.1007/s10040-019-02072-2.

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Collon, P., W. Kutschera, B. Davids, M. Fauerbach, R. Harkewics, D. Morrissey, B. Sherrill i in. "First attempt at dating groundwater from the Great Artesian Basin of Australia with81Kr using AMS". Chinese Science Bulletin 43, S1 (sierpień 1998): 27. http://dx.doi.org/10.1007/bf02891400.

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Prescott, J. R., i M. A. Habermehl. "Luminescence dating of spring mound deposits in the southwestern Great Artesian Basin, northern South Australia". Australian Journal of Earth Sciences 55, nr 2 (marzec 2008): 167–81. http://dx.doi.org/10.1080/08120090701689340.

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Torgersen, T., M. A. Habermehl, F. M. Phillips, David Elmore, Peter Kubik, Geoffrey B. Jones, T. Hemmick i H. E. Gove. "Chlorine 36 Dating of Very Old Groundwater: 3. Further Studies in the Great Artesian Basin, Australia". Water Resources Research 27, nr 12 (grudzień 1991): 3201–13. http://dx.doi.org/10.1029/91wr02078.

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Inverarity, K., G. Heinson i M. Hatch. "Groundwater flow underneath mound spring tufas from geophysical surveys in the southwestern Great Artesian Basin, Australia". Australian Journal of Earth Sciences 63, nr 7 (2.10.2016): 857–72. http://dx.doi.org/10.1080/08120099.2016.1261942.

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