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1

Lubiniecki, D. C., R. C. King, S. P. Holford, M. A. Bunch, S. B. Hore, and S. M. Hill. "Cenozoic structural evolution of the Mount Lofty Ranges and Flinders Ranges, South Australia, constrained by analysis of deformation bands." Australian Journal of Earth Sciences 67, no. 8 (February 9, 2020): 1097–115. http://dx.doi.org/10.1080/08120099.2019.1695227.

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2

Paul, E., T. Flöttmann, and M. Sandiford. "Structural geometry and controls on basement‐involved deformation in the northern Flinders Ranges, Adelaide Fold Belt, South Australia." Australian Journal of Earth Sciences 46, no. 3 (June 1999): 343–54. http://dx.doi.org/10.1046/j.1440-0952.1999.00711.x.

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3

Laflamme, Marc, James G. Gehling, and Mary L. Droser. "Deconstructing an Ediacaran frond: three-dimensional preservation of Arborea from Ediacara, South Australia." Journal of Paleontology 92, no. 3 (March 14, 2018): 323–35. http://dx.doi.org/10.1017/jpa.2017.128.

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AbstractExquisitely preserved three-dimensional examples of the classic Ediacaran (late Neoproterozoic; 570–541 Ma) frond Charniodiscus arboreus Jenkins and Gehling, 1978 (herein referred to as Arborea arborea Glaessner in Glaessner and Daily, 1959) are reported from the Ediacara Member, Rawnsley Quartzite of South Australia, and allow for a detailed reinterpretation of its functional morphology and taxonomy. New specimens cast in three dimensions within sandy event beds showcase detailed branching morphology that highlights possible internal features that are strikingly different from rangeomorph and erniettomorph fronds. Combined with dozens of well-preserved two-dimensional impressions from the Flinders Ranges of South Australia, morphological variations within the traditional Arborea morphotype are interpreted as representing various stages of external molding. In rare cases, taphomorphs (morphological variants attributable to preservation) represent composite molding of internal features consisting of structural supports or anchoring sites for branching structures. Each primary branch consists of a central primary branching stalk from which emerge several oval secondary branches, which likely correspond to similar structures found in rare two-dimensional specimens. Considering this new evidence, previous synonymies within the Arboreomorpha are no longer justified, and we suggest that the taxonomy of the group be revised.
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4

Snow, Michael R., Allan Pring, and Nicole Allen. "Minerals of the Wooltana Cave, Flinders Ranges, South Australia." Transactions of the Royal Society of South Australia 138, no. 2 (January 2014): 214–30. http://dx.doi.org/10.1080/03721426.2014.11649009.

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5

Groves, I. M., C. E. Carman, and W. J. Dunlap. "Geology of the Beltana Willemite Deposit, Flinders Ranges, South Australia." Economic Geology 98, no. 4 (June 1, 2003): 797–818. http://dx.doi.org/10.2113/gsecongeo.98.4.797.

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6

Lemon, N. M. "A Neoproterozoic fringing stromatolite reef complex, Flinders Ranges, South Australia." Precambrian Research 100, no. 1-3 (March 2000): 109–20. http://dx.doi.org/10.1016/s0301-9268(99)00071-6.

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7

Walshe, Keryn. "Aboriginal occupation at Hawker Lagoon, southern Flinders Ranges, South Australia." Australian Archaeology 60, no. 1 (January 2005): 24–33. http://dx.doi.org/10.1080/03122417.2005.11681801.

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8

Woon, E., and M. W. Wallace. "Petrogenesis of Neoproterozoic Allochthonous Reef Carbonates, Flinders Ranges, South Australia." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–4. http://dx.doi.org/10.1071/aseg2006ab198.

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9

Jago, J. B., J. G. Gehling, M. J. Betts, G. A. Brock, C. R. Dalgarno, D. C. García-Bellido, P. G. Haslett, et al. "The Cambrian System in the Arrowie Basin, Flinders Ranges, South Australia." Australian Journal of Earth Sciences 67, no. 7 (December 11, 2018): 923–48. http://dx.doi.org/10.1080/08120099.2018.1525431.

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10

Liddle, Nerida R., Matthew C. McDowell, and Gavin J. Prideaux. "Insights into the pre-European mammalian fauna of the southern Flinders Ranges, South Australia." Australian Mammalogy 40, no. 2 (2018): 262. http://dx.doi.org/10.1071/am17035.

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Many Australian mammal species have suffered significant declines since European colonisation. During the first century of settlement, information on species distribution was rarely recorded. However, fossil accumulations can assist the reconstruction of historical distributions. We examine a fossil vertebrate assemblage from Mair’s Cave, one of few known from the southern Flinders Ranges, South Australia. The Mair’s Cave assemblage was dominated by mammals but also included birds and reptiles. Of the 18 mammals recovered, two have not previously been recorded from the southern Flinders Ranges, at least one is extinct and seven are recognised as threatened nationally. Characteristics of the assemblage suggest that it was accumulated by a Tyto owl species. Remains of Tyto delicatula and a larger unidentified owl were recovered from the assemblage. Most mammals identified from the assemblage presently occupy Australia’s semiarid zone, but a single specimen of the broad-toothed rat (Mastacomys fuscus), which primarily occurs in high-moisture, low-temperature environments was also recovered. This suggests either that the southern Flinders Ranges once experienced higher past precipitation, or that M. fuscus can tolerate a broader climatic range than its current distribution suggests. Our study contributes new knowledge on the biogeography and ecology of several mammal species, data useful for helping to refine restoration targets.
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11

Cooke, B. D., and L. P. Hunt. "Practical and economic aspects of rabbit control in hilly semiarid South Australia." Wildlife Research 14, no. 2 (1987): 219. http://dx.doi.org/10.1071/wr9870219.

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Poisoning, ripping of warrens and a combination of both techniques were assessed as means of controlling rabbits in steep areas of the southern Flinders Ranges in semiarid South Australia. The number of active warren entrances was reduced significantly by poisoning and by ripping. One month after treatment, untreated plots contained an average of 72.2 active entrances whereas the poisoned and ripped plots averaged 27.1 and 7.3 active entrances, respectively. A combination of both techniques reduced the number of active warren entrances even further, but this is not recommended because it increases the cost of control substantially. The efficiencies of a large and a small crawler tractor were compared. Costs of ripping were similar, and the suitability of each tractor is discussed. In the southern Flinders Ranges rabbit control is clearly economical in relation to the improvements in sheep production likely to be obtained.
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12

Mahoney, J. A., M. J. Smith, and G. C. Medlin. "A new species of hopping-mouse, Notomys robustus sp. Nov. (Rodentia : Muridae), from cave deposits in the Flinders and Davenport Ranges, South Australia." Australian Mammalogy 29, no. 2 (2007): 117. http://dx.doi.org/10.1071/am07017.

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Notomys robustus sp. nov. is described from skulls found in whole and decomposed owl pellets from caves at Chambers Gorge in the Flinders Ranges, South Australia. The holotype was contained within a complete owl pellet, as were several paratypes. The species is distinguished by the unique conformation of the cusps of the upper first molar teeth. In adults, the anterodorsal region of the zygomatic arch is much wider than in any known species of Notomys. Since the original discoveries were made in 1976, the species has been found in more sites in the Flinders Ranges and at one other site near Mount Margaret in the Davenport Range, some 350 km northwest of the nearest Flinders Ranges site.
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13

Ahmed, Alaa, and Ian Clark. "Groundwater flow and geochemical evolution in the Central Flinders Ranges, South Australia." Science of The Total Environment 572 (December 2016): 837–51. http://dx.doi.org/10.1016/j.scitotenv.2016.07.123.

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14

FULLER, MARGARET, and RICHARD JENKINS. "REEF CORALS FROM THE LOWER CAMBRIAN OF THE FLINDERS RANGES, SOUTH AUSTRALIA." Palaeontology 50, no. 4 (July 2007): 961–80. http://dx.doi.org/10.1111/j.1475-4983.2007.00682.x.

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15

Giddings, J. A., M. W. Wallace, and E. M. S. Woon. "Interglacial carbonates of the Cryogenian Umberatana Group, northern Flinders Ranges, South Australia." Australian Journal of Earth Sciences 56, no. 7 (October 2009): 907–25. http://dx.doi.org/10.1080/08120090903005378.

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16

Chamalaun, F. H. "Geomagnetic deep sounding experiment in the central Flinders Ranges of South Australia." Physics of the Earth and Planetary Interiors 37, no. 2-3 (February 1985): 174–82. http://dx.doi.org/10.1016/0031-9201(85)90050-0.

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17

Gehling, James G., and J. Keith Rigby. "Long expected sponges from the Neoproterozoic Ediacara fauna of South Australia." Journal of Paleontology 70, no. 2 (March 1996): 185–95. http://dx.doi.org/10.1017/s0022336000023283.

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New fossils from the Neoproterozoic Ediacara fauna of South Australia are interpreted as the oldest known hexactinellid sponges. They occur within the Ediacara Member of the Rawnsley Quartzite (Pound Subgroup) from several locations in the Flinders Ranges. The new genus,Palaeophragmodictya, is characterized by disc-shaped impressions preserving characteristic spicular networks and is reconstructed as a convex sponge with a peripheral frill and an oscular disc at the apex.
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18

DONNELLAN, S., M. ANSTIS, L. PRICE, and L. WHEATON. "A new species of Crinia (Anura: Myobatrachidae) from the Flinders Ranges, South Australia." Zootaxa 3499, no. 1 (September 27, 2012): 1. http://dx.doi.org/10.11646/zootaxa.3499.1.1.

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We describe, as a new species, the northern Flinders Ranges populations of the myobatrachid frog Crinia riparia. It isdistinguished from C. riparia sensu stricto on the basis of reciprocal monophyly of mitochondrial genes, absence ofhaplotype sharing in a nuclear gene, fixed differences in allozyme loci and differences in larval oral disc morphologyconsistent with less adaptation to stream habitats. We were not able to reliably distinguish the taxa on the basis of adultmorphology. The geographic range of C. riparia sensu stricto is now reduced to a 75 kilometre section of the southernFlinders Ranges from Napperby Gorge in the south to Mt Brown in the north suggesting that an assessment of its conservation status is warranted.
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19

Mildren, S. D., and M. Sandiford. "Heat refraction and low‐pressure metamorphism in the northern Flinders Ranges, South Australia." Australian Journal of Earth Sciences 42, no. 3 (June 1995): 241–47. http://dx.doi.org/10.1080/08120099508728198.

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20

Williams, Martin, John R. Prescott, John Chappell, Donald Adamson, Bryan Cock, Keith Walker, and Peter Gell. "The enigma of a late Pleistocene wetland in the Flinders Ranges, South Australia." Quaternary International 83-85 (September 2001): 129–44. http://dx.doi.org/10.1016/s1040-6182(01)00035-0.

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21

Stobo-Wilson, Alyson M., Robert Brandle, Christopher N. Johnson, and Menna E. Jones. "Management of invasive mesopredators in the Flinders Ranges, South Australia: effectiveness and implications." Wildlife Research 47, no. 8 (2020): 720. http://dx.doi.org/10.1071/wr19237.

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Abstract ContextSignificant resources have been devoted to the control of introduced mesopredators in Australia. However, the control or removal of one pest species, such as, for example, the red fox (Vulpes vulpes), may inadvertently benefit other invasive species, namely feral cats (Felis catus) and rabbits (Oryctolagus cuniculus), potentially jeopardising native-species recovery. AimsTo (1) investigate the impact of a large-scale, long-term fox-baiting program on the abundance of foxes, feral cats and introduced and native prey species in the Flinders Ranges, South Australia, and (2) determine the effectiveness of a short time period of cat removal in immediately reducing feral cat abundance where foxes are absent. MethodsWe conducted an initial camera-trap survey in fox-baited and unbaited sites in the Flinders Ranges, to quantify the impact of fox baiting on the relative abundance of foxes, feral cats and their prey. We then conducted a secondary survey in sites where foxes were absent, following an intensive, but short, time period of cat removal, in which 40 cats were shot and killed. Key resultsNo foxes were detected within baited sites, but were frequently detected in unbaited sites. We found a corresponding and significant increase in several native prey species in fox-baited sites where foxes were absent. Feral cats and rabbits were also more frequently detected within baited sites, but fox baiting did not singularly predict the abundance of either species. Rather, feral cats were less abundant in open habitat where foxes were present (unbaited), and rabbits were more abundant within one predominantly open-habitat site, where foxes were absent (fox-baited). We found no effect of short-term cat removal in reducing the local abundance of feral cats. In both camera-trap surveys, feral cat detections were positively associated with rabbits. ConclusionsLong-term fox baiting was effective in fox removal and was associated with a greater abundance of native and introduced prey species in the Flinders Ranges. To continue to recover and conserve regional biodiversity, effective cat control is required. ImplicationsOur study showed fox removal has likely resulted in the local release of rabbits and an associated increase in cats. Because feral cat abundance seemingly fluctuated with rabbits, we suggest rabbit control may provide an alternative and more effective means to reduce local feral cat populations than short-term removal programs.
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22

KALLIES, AXEL, and TED EDWARDS. "A new sun moth species from the Flinders Ranges in South Australia (Lepidoptera, Castniidae)." Zootaxa 4369, no. 2 (January 3, 2018): 292. http://dx.doi.org/10.11646/zootaxa.4369.2.9.

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Sun moths (Castniidae) constitute a small family of day-flying butterfly-like moths that have their centers of diversity in South America and Australia. Here we describe a new castniid from the Finders Ranges, South Australia. Synemon arkaroola spec. nov. is similar and related to Synemon brontias Meyrick, 1891 but differs by a number of external and genitalic characters, including the extensive bright orange markings on the hindwings. The new species inhabits dry creek beds and adjacent slopes where the hostplant, Scented Lemon Grass, Cymbopogon ambiguus (Hack.) A. Camus (Poaceae), grows.
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23

Rowan, M. G., T. E. Hearon IV, R. A. Kernen, K. A. Giles, C. E. Gannaway-Dalton, N. J. Williams, J. C. Fiduk, T. F. Lawton, P. T. Hannah, and M. P. Fischer. "A review of allochthonous salt tectonics in the Flinders and Willouran ranges, South Australia." Australian Journal of Earth Sciences 67, no. 6 (February 10, 2019): 787–813. http://dx.doi.org/10.1080/08120099.2018.1553063.

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24

Lafuste, Jean, Françoise Debrenne, Anna Gandin, and David Gravestock. "The oldest tabulate coral and the associated archaeocyatha, Lower Cambrian, Flinders Ranges, South Australia." Geobios 24, no. 6 (January 1991): 697–718. http://dx.doi.org/10.1016/s0016-6995(06)80298-6.

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25

Thomas, Matilda, Jonathan D. A. Clarke, Victor A. Gostin, George E. Williams, and Malcolm R. Walter. "The Flinders Ranges and surrounds, South Australia: a window on astrobiology and planetary geology." Episodes 35, no. 1 (March 1, 2012): 226–35. http://dx.doi.org/10.18814/epiiugs/2012/v35i1/022.

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26

Holden, C., and G. Mutze. "Impact of rabbit haemorrhagic disease on introduced predators in the Flinders Ranges, South Australia." Wildlife Research 29, no. 6 (2002): 615. http://dx.doi.org/10.1071/wr00101.

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The impact of rabbit haemorrhagic disease (RHD) on the population dynamics and diet of foxes and feral cats was studied in the Flinders Ranges, South Australia. Populations of both foxes and cats decreased substantially some 6–10 months after the advent of RHD, when rabbit numbers were reduced by 85%. The diet of foxes changed as a result of reduced rabbit numbers, with much less rabbit and more invertebrates and carrion being eaten. The physical condition of foxes showed little change after RHD. The diet of cats did not change markedly, but their physical condition was substantially poorer than before RHD. Total predation on native fauna is considered to have decreased after RHD.
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27

Jell, P. A., J. B. Jago, and J. G. Gehling. "A new conocoryphid trilobite from the Lower Cambrian of the Flinders Ranges, South Australia." Alcheringa: An Australasian Journal of Palaeontology 16, no. 3 (January 1992): 189–200. http://dx.doi.org/10.1080/03115519208619118.

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28

Brugger, Joël, Ngaire Long, D. C. McPhail, and Ian Plimer. "An active amagmatic hydrothermal system: The Paralana hot springs, Northern Flinders Ranges, South Australia." Chemical Geology 222, no. 1-2 (October 2005): 35–64. http://dx.doi.org/10.1016/j.chemgeo.2005.06.007.

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29

Handley, Heather K., Simon P. Turner, Anthony Dosseto, David Haberlah, and Juan C. Afonso. "Considerations for U-series dating of sediments: Insights from the Flinders Ranges, South Australia." Chemical Geology 340 (February 2013): 40–48. http://dx.doi.org/10.1016/j.chemgeo.2012.12.003.

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30

Betts, Marissa J., Timothy P. Topper, James L. Valentine, Christian B. Skovsted, John R. Paterson, and Glenn A. Brock. "A new early Cambrian bradoriid (Arthropoda) assemblage from the northern Flinders Ranges, South Australia." Gondwana Research 25, no. 1 (January 2014): 420–37. http://dx.doi.org/10.1016/j.gr.2013.05.007.

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31

Eickhoff, K. H., C. C. Von Der Borch, and A. E. Grady. "Proterozoic canyons of the Flinders Ranges (South Australia): submarine canyons or drowned river valleys?" Sedimentary Geology 58, no. 2-4 (August 1988): 217–35. http://dx.doi.org/10.1016/0037-0738(88)90070-x.

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32

Yu, B., and CJ Rosewell. "Rainfall erosivity estimation using daily rainfall amounts for South Australia." Soil Research 34, no. 5 (1996): 721. http://dx.doi.org/10.1071/sr9960721.

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The rainfall erosivity model relating storm erosivity to daily rainfall amounts was tested for 4 sites in South Australia where seasonal rainfall erosivity is generally out of phase with seasonal rainfall because of the predominant winter rainfall. The model worked reasonably well, with the coefficient of efficiency varying from 0.54 to 0.77, and the average discrepancy between actual and estimated monthly distribution was no more than 3%. The model performance in the winter rainfall area is similar to that in the uniform and summer rainfall areas. A set of regional parameter values estimated using a combined dataset is recommended for other sites in the agricultural and viticultural areas of South Australia where the mean annual rainfall ranges from 300 to 500 mm. The R-factor and its seasonal distribution were estimated for 99 sites in South Australia using long-term daily rainfall data. The R-factor varies mostly between 250 and 500 MJ . mm/(ha . h . year). Rainfall erosivity peaks in winter in the southern part of the western agricultural area and the south-east corner of the State, while it peaks in summer in the inland area east of the South Flinders and Mount Lofty Ranges.
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33

Sandiford, Mike, Eike Paul, and Thomas Flottmann. "Sedimentary thickness variations and deformation intensity during basin inversion in the Flinders Ranges, South Australia." Journal of Structural Geology 20, no. 12 (December 1998): 1721–31. http://dx.doi.org/10.1016/s0191-8141(98)00088-1.

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34

Jago, J. B., C. G. Gatehouse, C. McA Powell, T. Casey, and E. M. Alexander. "The Dawson Hill Member of the Grindstone Range Sandstone in the Flinders Ranges, South Australia." Transactions of the Royal Society of South Australia 134, no. 1 (January 2010): 115–24. http://dx.doi.org/10.1080/3721426.2010.10887135.

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35

Schmallegger, Doris, Andrew Taylor, and Dean Carson. "Rejuvenating Outback Tourism through Market Diversification: the Case of the Flinders Ranges in South Australia." International Journal of Tourism Research 13, no. 4 (May 24, 2011): 384–99. http://dx.doi.org/10.1002/jtr.851.

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36

Quigley, Mark, Mike Sandiford, and Matt Cupper. "Landscape expressions of late Quaternary climate change and large flood events, Flinders Ranges, South Australia." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–2. http://dx.doi.org/10.1071/aseg2006ab144.

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37

Hornsby, PE, and EY Corlett. "Differential responses by sympatric macropodids to severe drought." Australian Mammalogy 26, no. 2 (2004): 185. http://dx.doi.org/10.1071/am04185.

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Responses to severe drought by two sympatric macropodids, the yellow-footed rock-wallaby (Petrogale xanthopus) and the euro (Macropus robustus erubescens) were examined at a site in the North Flinders Ranges of South Australia. The results indicate that the two species respond differentially to drought conditions. It was observed that small fluctuations occurred in the P. xanthopus population. In contrast, M. r. erubescens evidenced significant mortality, especially among larger animals.
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38

Reilly, M. R. W., and S. C. Lang. "A PONDED BASIN FLOOR FAN OUTCROP ANALOGUE: BUNKERS SANDSTONE, NORTHERN FLINDERS RANGES, AUSTRALIA." APPEA Journal 43, no. 1 (2003): 537. http://dx.doi.org/10.1071/aj02028.

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The Donkey Bore Syncline in the Northern Flinders Ranges of South Australia contains a generally finegrained deepwater succession of Early Cambrian age (Bunkers Sandstone) that outcrops on three sides of a syncline and flanks an active salt diapir to the east (Wirrealpa Diapir). Within the succession lies a basal sand-prone interval interpreted as a basin floor fan (BFF) ponded within a mini-basin on a topographically complex slope.The BFF comprises over 30 m of section with deposits that are dominantly massive clean sandstone beds (0.1– 3 m thick) that are stacked or interbedded with siltstones and pinch out along strike.Eight stratigraphic sections and accompanying spectral gamma ray logs (using a hand held scintillometer) were measured through the BFF. Using spectral gamma ray log analysis combined with stratigraphic logs, four alternative correlation panels were constructed.Quantitative analysis of sand-prone intervals interpreted in each of the panels provided data on the vertical and horizontal connectivity within the BFF as different correlation methods were explored and the geological model improved. Quantitative analysis of vertical and horizontal connectivity values indicates a high degree of heterogeneity within the BFF, with poor–moderate vertical connectivity, with individual beds rarely correlating >500 m along strike. This heterogeneity is poorly resolved using conventional wireline log suites, but is greatly improved if spectral gamma ray logs are used (especially Thorium).The data set provides a high-resolution analogue for understanding the internal architecture of deepwater hydrocarbon reservoirs.
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39

Haberlah, David. "Loess and floods: late Pleistocene fine-grained valley-fill deposits in the Flinders Ranges, South Australia." Quaternary International 279-280 (November 2012): 183. http://dx.doi.org/10.1016/j.quaint.2012.08.288.

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40

Rajabi, Mojtaba, Mark Tingay, Oliver Heidbach, David Belton, Natalie Balfour, and Betina Bendall. "New constraints on the neotectonic stress pattern of the Flinders and Mount Lofty Ranges, South Australia." Exploration Geophysics 49, no. 1 (February 2018): 111–24. http://dx.doi.org/10.1071/eg16076.

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41

Rajabi, Mojtaba, Mark Tingay, Oliver Heidbach, David Belton, Natalie Balfour, and Betina Bendall. "New constraints on the neotectonic stress pattern of the Flinders and Mount Lofty Ranges, South Australia." Exploration Geophysics 49, no. 1 (February 2018): 125. http://dx.doi.org/10.1071/eg16076_co.

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42

Coutts, Felicity J., James G. Gehling, and Diego C. García-Bellido. "How diverse were early animal communities? An example from Ediacara Conservation Park, Flinders Ranges, South Australia." Alcheringa: An Australasian Journal of Palaeontology 40, no. 4 (October 1, 2016): 407–21. http://dx.doi.org/10.1080/03115518.2016.1206326.

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43

Skovsted, Christian B., Glenn A. Brock, Anna Lindström, John S. Peel, John R. Paterson, and Margaret K. Fuller. "Early Cambrian record of failed durophagy and shell repair in an epibenthic mollusc." Biology Letters 3, no. 3 (April 3, 2007): 314–17. http://dx.doi.org/10.1098/rsbl.2007.0006.

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Predation is arguably one of the main driving forces of early metazoan evolution, yet the fossil record of predation during the Ediacaran–Early Cambrian transition is relatively poor. Here, we present direct evidence of failed durophagous (shell-breaking) predation and subsequent shell repair in the Early Cambrian (Botoman) epibenthic mollusc Marocella from the Mernmerna Formation and Oraparinna Shale in the Flinders Ranges, South Australia. This record pushes back the first appearance of durophagy on molluscs by approximately 40 Myr.
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44

Ahmed, Alaa, Abdullah Alrajhi, and Abdulaziz S. Alquwaizany. "Identification of Groundwater Potential Recharge Zones in Flinders Ranges, South Australia Using Remote Sensing, GIS, and MIF Techniques." Water 13, no. 18 (September 17, 2021): 2571. http://dx.doi.org/10.3390/w13182571.

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In Australia, water resource management is a major environmental, biological, and socio-economic issue, and will be an essential component of future development. The Hawker Area of the central Flinders Ranges, South Australia suffers from a lack of reliable data to help with water resource management and decision making. The present study aimed to delineate and assess groundwater recharge potential (GWRP) zones using an integration between the remote sensing (RS), geographic information system (GIS), and multi-influencing factors (MIF) approaches in the Hawker Area of the Flinders Ranges, South Australia. Many thematic layers such as lithology, drainage density, slope, and lineament density were established in a GIS environment for the purpose of identifying groundwater recharge potential zones. A knowledge base ranking from 1 to 5 was assigned to each individual thematic layer and its categories, depending on each layer’s importance to groundwater recharge potential zones. All of the thematic layers were integrated to create a combined groundwater potential map of the study area using weighting analysis in ArcGIS software. The groundwater potential zones were categorized into three classes, good, moderate, and low. The resulting zones were verified using available water data and showed a relative consistency with the interpretations. The findings of this study indicated that the most effective groundwater potential recharge zones are located where the lineament density is high, the drainage density is low, and the slope is gentle. The least effective areas for groundwater recharge are underlain by shale and siltstone. The results indicated that there were interrelationships between the groundwater recharge potential factors and the general hydrology characteristics scores of the catchment. MIF analysis using GIS mapping techniques proved to be a very useful tool in the evaluation of hydrogeological systems and could enable decision makers to evaluate, better manage, and protect a hydrogeological system using a single platform.
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45

Read, J., P. Copley, and P. Bird. "The distribution, ecology and current status of Pseudomys desertor in South Australia." Wildlife Research 26, no. 4 (1999): 453. http://dx.doi.org/10.1071/wr97051.

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Recent surveys have shown that the desert mouse (Pseudomys desertor), which was once considered to be rare in South Australia, is relatively widespread throughout the north-west of the State. However, historical localities in the Flinders Ranges and Nullarbor Plain were not matched with contemporary records, suggesting a range contraction to the central desert regions. Habitat preferences were determined from 78 captures at 41 sites, which revealed that samphire, sedge and nitrebush habitats, along with spinifex grassland, were favoured. A high tolerance to high rabbit numbers, mining activity, moderate cattle grazing pressures and cohabitation with Mus domesticus was evident. Pseudomys desertor is sometimes diurnal, possibly as a result of the time-consuming and regular foraging requirements of its folivorous diet. High mortality rates, resulting from prolonged exposure to predators, and lack of complex deep burrow systems are offset by its high fecundity and ecological plasticity. We consider that P. desertor is secure in the north-western arid zone of South Australia.
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46

Balfour, N. J., P. R. Cummins, S. Pilia, and D. Love. "Localization of intraplate deformation through fluid-assisted faulting in the lower-crust: The Flinders Ranges, South Australia." Tectonophysics 655 (August 2015): 97–106. http://dx.doi.org/10.1016/j.tecto.2015.05.014.

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47

Bourne, J. A., R. Hillis, M. Rutty, and C. R. Twidale. "Fan, fill or covered pediment? Seismic investigation of alluvial cover thickness, Hayward ``Pediment'', Flinders Ranges, South Australia." Zeitschrift für Geomorphologie 46, no. 2 (July 3, 2002): 193–201. http://dx.doi.org/10.1127/zfg/46/2002/193.

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48

Kernen, R. A., K. A. Giles, P. L. Poe, C. E. Gannaway Dalton, M. G. Rowan, J. C. Fiduk, and T. E. Hearon. "Origin of the Neoproterozoic rim dolomite as lateral carbonate caprock, Patawarta salt sheet, Flinders Ranges, South Australia." Australian Journal of Earth Sciences 67, no. 6 (April 23, 2019): 815–32. http://dx.doi.org/10.1080/08120099.2019.1588695.

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49

Hore, S. B., S. M. Hill, and N. F. Alley. "Early Cretaceous glacial environment and paleosurface evolution within the Mount Painter Inlier, northern Flinders Ranges, South Australia." Australian Journal of Earth Sciences 67, no. 8 (April 15, 2020): 1117–60. http://dx.doi.org/10.1080/08120099.2020.1730963.

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50

Bourne, J. A., and C. R. Twidale. "Pediments and alluvial fans: Genesis and relationships in the western piedmont of the Flinders Ranges, South Australia." Australian Journal of Earth Sciences 45, no. 1 (February 1998): 123–35. http://dx.doi.org/10.1080/08120099808728373.

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