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Journal articles on the topic 'Geology South Australia Lofty'

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Published: 10 December 2022

Last updated: 29 January 2023

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1

Twidale, C. Rowland. "Paul S. Hossfeld and His Contribution to Geomorphology." Historical Records of Australian Science 23, no. 2 (2012): 132. http://dx.doi.org/10.1071/hr12006.

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The received wisdom was and is that landscapes cannot be more than a few millions of years old. Nevertheless, consideration of local geology and age of sediments in adjacent basins convinced Paul S. Hossfeld that the summit surface of low relief preserved on the northern Mount Lofty Ranges of South Australia resulted from long-continued planation and that it is of Cretaceous age; that is, some 70 million years old. Hossfeld's apparently intuitive suggestion that very old landscapes exist, recorded in his graduate thesis but not further pursued by him, is the earliest known statement of this idea.

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2

Paull, D. "The distribution of the southern brown bandicoot (Isoodon obesulus obesulus) in South Australia." Wildlife Research 22, no. 5 (1995): 585. http://dx.doi.org/10.1071/wr9950585.

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This paper describes the South Australian distribution of the southern brown bandicoot (Isoodon obesulus obesulus) on the basis of records of its past occurrence and field surveys undertaken to determine its present distribution. Since European settlement I. o. obesulus has been recorded from four separate regions of the state: the Mount Lofty Ranges, the South East, Kangaroo Island and Eyre Peninsula. Subfossil remains show that I. o. obesulus also once occurred on Yorke Peninsula but there is no evidence that it has existed there in modem times. Field surveys conducted between 1986 and 1993 confirmed that I. o. obesulus still exists in the Mount Lofty Ranges, the South East and on Kangaroo Island. Its status on Eyre Peninsula is uncertain. Isoodon o. obesulus is vulnerable in the South East and Mount Lofty Ranges because of habitat fragmentation and predation by feral carnivores. The Kangaroo Island population is less threatened as large areas of habitat have been preserved and the fox (Vulpes vulpes) has not been introduced. The area of potential bandicoot habitat remaining in these three regions totals approximately 190 000 ha, most of which is already managed for nature conservation. This habitat is highly fragmented, occurring as small remnant patches of native vegetation separated by extensive tracts of cleared and modified land cover. The implications of this habitat configuration for the long-term survival of I. o. obesulus are discussed.

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3

Speight, Natasha, Daniel Colella, Wayne Boardman, David A. Taggart, Julie I. Haynes, and William G. Breed. "Seasonal variation in occurrence of oxalate nephrosis in South Australian koalas (Phascolarctos cinereus)." Australian Mammalogy 41, no. 1 (2019): 92. http://dx.doi.org/10.1071/am17038.

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Many koalas (Phascolarctos cinereus) in the Mount Lofty Ranges, South Australia, are affected by oxalate nephrosis, in which renal calcium oxalate deposition occurs. In other species, suboptimal water intake increases the risk of urinary calcium oxalate crystal formation. Koalas principally rely on eucalypt leaf moisture content to maintain hydration but the Mount Lofty Ranges region has hot, dry summers. This study investigates the association between temperature, rainfall and eucalypt leaf moisture and the occurrence of oxalate nephrosis in this population of koalas. Koalas from the Mount Lofty Ranges population that had died or were euthanased between 2008 and 2016 were necropsied and oxalate nephrosis was determined by histopathology (n=50). Leaf moisture content of Mount Lofty eucalypts was determined seasonally. It was found that increased numbers of koalas with oxalate nephrosis died in the months following high mean maximal temperature and in the months following low rainfall. Eucalypt leaf moisture content was not significantly associated with koala deaths. These findings suggest that hot and dry summer/autumn periods contribute to an increased incidence of koala deaths due to oxalate nephrosis. This is probably due to the effects of evaporative water loss and/or lack of access to supplementary drinking water at this time.

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4

Twidale, C. Rowland. "Charles Fenner and Early Landform Studies in South Australia." Historical Records of Australian Science 21, no. 2 (2010): 149. http://dx.doi.org/10.1071/hr10001.

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Charles Albert Edward Fenner (1884?1955) was educated in Melbourne but spent the major part of his working life in South Australia, first as Superintendent of Technical Education and later as Director of Education, holding the latter post during the difficult years of the Second World War. He is best remembered for his role in the establishment of Geography as a university discipline and for his landform studies. He brought together earlier work on the tectonics of the Gulfs region of South Australia and introduced the term ?shatter belt' to describe the complex of horsts and sunken blocks. He noted evidence pointing to recent and continuing earth movements, and suggested that such earth movements were responsible for the westerly diversion of the River Murray at Chucka Bend. He also conceived a hypothesis of ?double planation' in explanation of the morphology of the Mt Lofty Ranges.

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5

Speight, K. N., W. G. Breed, W. Boardman, D. A. Taggart, C. Leigh, B. Rich, and J. I. Haynes. "Leaf oxalate content of Eucalyptus spp. and its implications for koalas (Phascolarctos cinereus) with oxalate nephrosis." Australian Journal of Zoology 61, no. 5 (2013): 366. http://dx.doi.org/10.1071/zo13049.

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Oxalate nephrosis is a leading disease of the Mount Lofty Ranges koala population in South Australia, but the cause is unclear. In other herbivorous species, a common cause is high dietary oxalate; therefore this study aimed to determine the oxalate content of eucalypt leaves. Juvenile, semimature and mature leaves were collected during spring from eucalypt species eaten by koalas in the Mount Lofty Ranges and compared with those from Moggill, Queensland, where oxalate nephrosis has lower prevalence. Total oxalate was measured as oxalic acid by high-performance liquid chromatography. The oxalate content of eucalypts was low (<1% dry weight), but occasional Mount Lofty leaf samples had oxalate levels of 4.68–7.51% dry weight. Mount Lofty eucalypts were found to be higher in oxalate than those from Queensland (P < 0.001). In conclusion, dietary oxalate in eucalypt leaves is unlikely to be the primary cause of oxalate nephrosis in the Mount Lofty koala population. However, occasional higher oxalate levels could cause oxalate nephrosis in individual koalas or worsen disease in those already affected. Further studies on the seasonal variation of eucalypt leaf oxalate are needed to determine its role in the pathogenesis of oxalate nephrosis in koalas.

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6

Cook, Robert B. "Ataeamite: Moonta Mine, South Australia, Australia." Rocks & Minerals 81, no. 5 (January 2006): 374–78. http://dx.doi.org/10.3200/rmin.81.5.374-378.

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7

Mogoutnov, Alena, and Jackie Venning. "Remnant tree decline in agricultural regions of South Australia." Pacific Conservation Biology 20, no. 4 (2014): 366. http://dx.doi.org/10.1071/pc140366.

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Agricultural landscapes in southern Australia were once dominated by temperate eucalypt woodlands of which only fragmented patches and scattered trees in paddocks remain. This study focuses on the decline of scattered trees in the Mount Lofty Ranges and South East agricultural regions of South Australia. A combination of digitized aerial photography and satellite imagery was used to extend a previous assessment of decline undertaken in the early 1980s and increase the period over which decline was assessed to 58–72 years. A total of 17 049 scattered trees were counted from the earliest time period assessed over 11 sites of which 6 185 trees were lost by 2008 — a 36 % decline. Recruitment of 2 179 trees during this period was evident. Imagery indicates that clearing for agricultural intensification is the primary cause of the decline. A range of management options and policy settings are required to reverse the decline notwithstanding the challenges of implementation at a landscape scale across privately owned land.

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8

Speight, KN, P. Hicks, C. Graham, W. Boardman, WG Breed, E. Manthorpe, O. Funnell, and L. Woolford. "Necropsy findings of koalas from the Mount Lofty Ranges population in South Australia." Australian Veterinary Journal 96, no. 5 (April 24, 2018): 188–92. http://dx.doi.org/10.1111/avj.12690.

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9

Szabo, Judit K., Peter A. Vesk, Peter W. J. Baxter, and Hugh P. Possingham. "Paying the extinction debt: woodland birds in the Mount Lofty Ranges, South Australia." Emu - Austral Ornithology 111, no. 1 (March 2011): 59–70. http://dx.doi.org/10.1071/mu09114.

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10

Main, BY. "Further Studies on Australian Diplurinae: A Review of the Genera of the Teylni ( Araneae: Mygalomorphae: Dipluridae)." Australian Journal of Zoology 33, no. 5 (1985): 743. http://dx.doi.org/10.1071/zo9850743.

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The tribe Teylini is diagnosed. It comprises Teyl Main, Namea Raven (newly placed) and two new monotypic genera, Teyloides and Pseudoteyl. The two new genera and their type-species, T. bakeri and P. vancouveri from Mt Lofty, South Australia, and West Cape Howe, Western Australia, respectively, are described. Affinities within the Teylini and relationships to other diplurine genera are discussed. It is suggested that the spur on the first tibia, a significant diagnostic character of Australian male diplurines, has evolved at least three times.

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11

Bourman, R. P., D. Banerjee, C. V. Murray-Wallace, S. Buckman, D. K. Panda, A. P. Belperio, and C. L. Jayawardena. "Luminescence dating of Quaternary alluvial successions, Sellicks Creek, South Mount Lofty Ranges, southern Australia." Australian Journal of Earth Sciences 67, no. 5 (February 24, 2020): 627–47. http://dx.doi.org/10.1080/08120099.2020.1722967.

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12

Bardsley, D. K., D. Weber, G. M. Robinson, E. Moskwa, and A. M. Bardsley. "Wildfire risk, biodiversity and peri-urban planning in the Mt Lofty Ranges, South Australia." Applied Geography 63 (September 2015): 155–65. http://dx.doi.org/10.1016/j.apgeog.2015.06.012.

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13

Li, You, Melanie L. Lancaster, Susan M. Carthew, Jasmin G. Packer, and Steven J. B. Cooper. "Delineation of conservation units in an endangered marsupial, the southern brown bandicoot (Isoodon obesulus obesulus), in South Australia/western Victoria, Australia." Australian Journal of Zoology 62, no. 5 (2014): 345. http://dx.doi.org/10.1071/zo14038.

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Conservation programs for threatened species are greatly benefiting from genetic data, for their power in providing knowledge of dispersal/gene flow across fragmented landscapes and for identifying populations of high conservation value. The endangered southern brown bandicoot (Isoodon obesulus obesulus) has a disjunct distribution range in South Australia, raising the possibility that populations of the subspecies may represent distinct conservation units. In the current study, we used a combination of 14 microsatellite and two mitochondrial sequence markers to investigate the phylogeography and population structure of I. o. obesulus in South Australia and south-western Victoria, with the aim of identifying any potential evolutionarily significant units and management units relevant to conservation management. Our phylogenetic/population analyses supported the presence of two distinct evolutionary lineages of I. o. obesulus. The first lineage comprised individuals from the Mount Lofty Ranges, Fleurieu Peninsula and Kangaroo Island. A second lineage comprised individuals from the south-east of South Australia and south-western Victoria. We propose that these two lineages represent distinct evolutionarily significant units and should be managed separately for conservation purposes. The findings also raise significant issues for the national conservation status of I. o. obesulus and suggest that the current subspecies classification needs further investigation.

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14

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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15

Guan, Huade, Craig T. Simmons, and Andrew J. Love. "Orographic controls on rain water isotope distribution in the Mount Lofty Ranges of South Australia." Journal of Hydrology 374, no. 3-4 (August 2009): 255–64. http://dx.doi.org/10.1016/j.jhydrol.2009.06.018.

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16

Taylor, G. S. "THE GALL FORMING PSYLLOIDEA OF EUCALYPTUS OBLIQUA IN THE MOUNT LOFTY RANGES OF SOUTH AUSTRALIA." Australian Journal of Entomology 26, no. 3 (August 1987): 223–28. http://dx.doi.org/10.1111/j.1440-6055.1987.tb00290.x.

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17

Merry, RH, KG Tiller, and AF Richards. "Variability in characteristics of some acidic pasture soils in South Australia and implications for lime application." Soil Research 28, no. 1 (1990): 27. http://dx.doi.org/10.1071/sr9900027.

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The variability of soil pH (0.01 M CaCI2), aluminium and manganese (extractable in 0.01 M CaCl2), total carbon and some soil morphological factors have been investigated in the surface and subsoil at seven pasture sites in the southern Mount Lofty Ranges and Kangaroo Island, South Australia. The coefficients of variation of the factors measured were found to be of a similar order, except for soil pH which, being a logarithmic transformation, is much lower. Relationships between pH and soil aluminium, manganese and carbon are used to predict the effects of further acidification, especially with respect to the development of increased extractable aluminium, and to assess the likelihood of problems in selecting appropriate rates of lime application.

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18

VÖRÖS, JUDIT, SKYE WASSENS, LUKE PRICE, DAVID HUNTER, STEVEN MYERS, KYLE ARMSTRONG, MICHAEL J. MAHONY, and STEPHEN DONNELLAN. "Molecular systematic analysis demonstrates that the threatened southern bell frog, Litoria raniformis (Anura: Pelodryadidae) of eastern Australia, comprises two sub-species." Zootaxa 5228, no. 1 (January 11, 2023): 1–43. http://dx.doi.org/10.11646/zootaxa.5228.1.1.

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In south-eastern Australia, the pelodryadid Litoria aurea Group (sensu Tyler & Davies 1978) comprises three species: Litoria aurea (Lesson, 1829), Litoria raniformis (Keferstein, 1867), and Litoria castanea (Steindachner, 1867). All three species have been subject to declines over recent decades and taxonomic uncertainty persists among populations on the tablelands in New South Wales. We address the systematics of the Group by analysing mitochondrial and nuclear DNA sequences to assess divergence in the Litoria raniformis from across its current range in New South Wales (NSW), Victoria, South Australia (SA) and Tasmania. We also included samples of Litoria castanea from a recently rediscovered population in the southern tablelands of NSW. Our phylogenetic and population genetic analyses show that Litoria raniformis comprises northern and southern lineages, showing deep mitochondrial DNA sequence divergence (7% net average sequence divergence) and can be diagnosed by fixed allelic differences at more than 4,000 SNP loci. Samples of the northern lineage were collected from the Murray-Darling Basin while those of the southern lineage were collected from south-eastern South Australia, southern and south-eastern Victoria and Tasmania. Analysis of the morphology and bioacoustics did not unequivocally delineate the two lineages. The presence of a hybrid backcross individual in western Victoria at the northern margin of the southern lineage, leads us to assign sub-species status to the two lineages, L. r. raniformis for the northern lineage and L. r. major for the southern lineage. Our data do not unequivocally resolve the taxonomic status of L. castanea which will require molecular genetic analyses of museum vouchers from those parts of the range where L. castanea and L. raniformis are no longer extant. Our data also suggest that human mediated movement of frogs may have occurred over the past 50 years. Our genotyping of vouchers collected in the 1970s from the Mount Lofty Ranges in South Australia detected mitochondrial haplotypes of both sub-species and SNP analysis showed that a single Tasmanian specimen was a backcross with L. r. raniformis ancestry. Movement of L. r. raniformis into Tasmania and both sub-species into the Mount Lofty Ranges are not likely due to passive movements of animals through agricultural commerce, but due to the attractiveness of the species as pets and subsequent escapes or releases, potentially of the larval life stage.

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19

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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20

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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21

Westphal, Michael I., Scott A. Field, and Hugh P. Possingham. "Optimizing landscape configuration: A case study of woodland birds in the Mount Lofty Ranges, South Australia." Landscape and Urban Planning 81, no. 1-2 (May 2007): 56–66. http://dx.doi.org/10.1016/j.landurbplan.2006.10.015.

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22

Anderson, Thomas A., Erick A. Bestland, Ilka Wallis, and Huade D. Guan. "Salinity balance and historical flushing quantified in a high-rainfall catchment (Mount Lofty Ranges, South Australia)." Hydrogeology Journal 27, no. 4 (January 10, 2019): 1229–44. http://dx.doi.org/10.1007/s10040-018-01916-7.

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23

Wilford, J., and M. Thomas. "Predicting regolith thickness in the complex weathering setting of the central Mt Lofty Ranges, South Australia." Geoderma 206 (September 2013): 1–13. http://dx.doi.org/10.1016/j.geoderma.2013.04.002.

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24

Chandler, Gregory T., and Michael D. Crisp. "Contributions Towards a Revision of Daviesia (Fabaceae: Mirbelieae). IV.* D. ulicifolia sens. lat." Australian Systematic Botany 10, no. 1 (1997): 31. http://dx.doi.org/10.1071/sb96013.

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Following a morphometric and cladistic analysis of the Daviesia ulicifolia Andrews group (Chandler and Crisp 1997), a new species, D. sejugata, is described. It occurs disjunctly in eastern Tasmania and southern Yorke Peninsula, South Australia, and is closely related to D. arthropoda F.Muell., differing in a generally more robust habit, thicker fleshy phyllodes, and larger flowers. Even with this species removed from D. ulicifolia, the latter varies considerably over a wide geographic, edaphic and altitudinal range. Daviesia ulicifolia is divided into six subspecies based on distinct phenetic and phylogenetic groups delimited in the earlier study. These are subsp. aridicola (glaucous plants in arid regions), subsp. incarnata (reddish-flowered plants in the Mt Lofty Range, South Australia), subsp. ruscifolia (plants with ovate-acuminate leaves and orange flowers in Victoria and southern New South Wales (NSW), often at high altitude), subsp. stenophylla (a narrow-leaved form in northern NSW and Queensland), subsp. pilligensis (ovate-leaved plants on sandy soil in western NSW), and subsp. ulicifolia (a paraphyletic residual from south-eastern states).

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25

Bryant, E. A., and R. W. Young. "Bedrock-Sculpturing by Tsunami, South Coast New South Wales, Australia." Journal of Geology 104, no. 5 (September 1996): 565–82. http://dx.doi.org/10.1086/629852.

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26

Matthews, Chris, and Graeme Beardsmore. "New heat flow data from south-eastern South Australia." Exploration Geophysics 38, no. 4 (December 1, 2007): 260–69. http://dx.doi.org/10.1071/eg07028.

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27

Jenkins, Richard J. F. "Chapter 68 Billy Springs glaciation, South Australia." Geological Society, London, Memoirs 36, no. 1 (2011): 693–99. http://dx.doi.org/10.1144/m36.68.

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28

LOTTERMOSER, B. G. "A carbonatitic diatreme from Umberatana, South Australia." Journal of the Geological Society 145, no. 3 (May 1988): 505–13. http://dx.doi.org/10.1144/gsjgs.145.3.0505.

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29

Funnell, Oliver, Lynley Johnson, Lucy Woolford, Wayne Boardman, Adam Polkinghorne, and David McLelland. "Conjunctivitis Associated with Chlamydia pecorum in Three Koalas (Phascolarctos cinereus) in the Mount Lofty Ranges, South Australia." Journal of Wildlife Diseases 49, no. 4 (October 2013): 1066–69. http://dx.doi.org/10.7589/2013-03-066.

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30

Buckman, Solomon, Katherine C. Brownlie, Robert P. Bourman, Colin V. Murray-Wallace, Rowena H. Morris, Terry J. Lachlan, Richard G. Roberts, Lee J. Arnold, and John H. Cann. "Holocene palaeofire records in a high-level, proximal valley-fill (Wilson Bog), Mount Lofty Ranges, South Australia." Holocene 19, no. 7 (October 23, 2009): 1017–29. http://dx.doi.org/10.1177/0959683609340998.

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31

Fitzpatrick, R. W., J. W. Cox, E. Fritsch, and I. D. Hollingsworth. "A soil-diagnostic key to manage saline and waterlogged catchments in the Mt Lofty Ranges, South Australia." Soil Use and Management 10, no. 4 (December 1994): 145–52. http://dx.doi.org/10.1111/j.1475-2743.1994.tb00477.x.

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32

Varcoe, Jon, John A. van Leeuwen, David J. Chittleborough, James W. Cox, Ronald J. Smernik, and Anna Heitz. "Changes in water quality following gypsum application to catchment soils of the Mount Lofty Ranges, South Australia." Organic Geochemistry 41, no. 2 (February 2010): 116–23. http://dx.doi.org/10.1016/j.orggeochem.2009.09.010.

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33

Richards, Jenny, John Tibby, Cameron Barr, and Peter Goonan. "Effect of substrate type on diatom-based water quality assessments in the Mount Lofty Ranges, South Australia." Hydrobiologia 847, no. 14 (June 1, 2020): 3077–90. http://dx.doi.org/10.1007/s10750-020-04316-9.

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34

Oliver, Danielle P., Rai S. Kookana, Jenny S. Anderson, Jim W. Cox, Nigel Fleming, Natasha Waller, and Lester Smith. "Off-site transport of pesticides from two horticultural land uses in the Mt. Lofty Ranges, South Australia." Agricultural Water Management 106 (April 2012): 60–69. http://dx.doi.org/10.1016/j.agwat.2011.06.004.

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35

Newton, Warwick, Sue Daly, Stuart Robertson, Wolfgang Preiss, Colin conor, and Andrew Burtt. "Overview of geology and mineralisation in South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 1–18. http://dx.doi.org/10.1071/asegspec12_01.

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36

Lukasik, J. J., and N. P. James. "Deepening-Upward Subtidal Cycles, Murray Basin, South Australia." Journal of Sedimentary Research 73, no. 5 (September 1, 2003): 653–71. http://dx.doi.org/10.1306/031003730653.

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37

Carr, Paul, Malcolm Southwood, and Jeff Chen. "Fluorapatite from Broken Hill, New South Wales, Australia." Rocks & Minerals 97, no. 1 (December 20, 2021): 16–27. http://dx.doi.org/10.1080/00357529.2022.1989948.

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38

Sandiford, M., G. Eraser, J. Arnold, J. Foden, and T. Farrow. "Some causes and consequences of high‐temperature, low‐pressure metamorphism in the eastern Mt Lofty Ranges, South Australia." Australian Journal of Earth Sciences 42, no. 3 (June 1995): 233–40. http://dx.doi.org/10.1080/08120099508728197.

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39

SMITH, PETER J. "Early mining in South Australia." Geology Today 4, no. 1 (January 1988): 30–34. http://dx.doi.org/10.1111/j.1365-2451.1988.tb00539.x.

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40

Walter, Malcolm. "The geology of South Australia, volume 1. The Precambrian." Precambrian Research 78, no. 4 (June 1996): 298–99. http://dx.doi.org/10.1016/0301-9268(95)00060-7.

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41

Gatehouse, Colin G. "The geology of the Warburton Basin in South Australia." Australian Journal of Earth Sciences 33, no. 2 (June 1986): 161–80. http://dx.doi.org/10.1080/08120098608729357.

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42

Williams, George E., Victor A. Gostin, David M. McKirdy, Wolfgang V. Preiss, and Phillip W. Schmidt. "Chapter 70 The Elatina glaciation (late Cryogenian), South Australia." Geological Society, London, Memoirs 36, no. 1 (2011): 713–21. http://dx.doi.org/10.1144/m36.70.

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43

White, A., and P. R. Milligan. "Geomagnetic variation anomaly on Eyre Peninsula, South Australia." Exploration Geophysics 17, no. 1 (March 1986): 32–34. http://dx.doi.org/10.1071/eg986032.

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44

Sherwood, John E., Jim M. Bowler, Stephen P. Carey, John Hellstrom, Ian J. McNiven, Colin V. Murray-Wallace, John R. Prescott, et al. "The Moyjil site, south-west Victoria, Australia: chronology." Proceedings of the Royal Society of Victoria 130, no. 2 (2018): 32. http://dx.doi.org/10.1071/rs18005.

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An unusual shell deposit at Moyjil (Point Ritchie), Warrnambool, in western Victoria, has previously been dated at 67±10 ka and has features suggesting a human origin. If human, the site would be one of Australia’s oldest, justifying a redetermination of age using amino acid racemisation (AAR) dating of Lunella undulata (syn. Turbo undulatus) opercula (the dominant shellfish present) and optically stimulated luminescence (OSL) of the host calcarenite. AAR dating of the shell bed and four Last Interglacial (LIG) beach deposits at Moyjil and Goose Lagoon, 30 km to the west, confirmed a LIG age. OSL analysis of the host sand revealed a complex mixing history, with a significant fraction (47%) of grains giving an early LIG age (120–125 ka) using a three-component mixing model. Shell deposition following the LIG sea-level maximum at 120–125 ka is consistent with stratigraphic evidence. A sand layer immediately below the shell deposit gave an age of ~240 ka (i.e. MIS 7) and appears to have been a source of older sand incorporated into the shell deposit. Younger ages (~60–80 ka) are due to bioturbation before calcrete finally sealed the deposit. Uranium/thorium methods were not applicable to L. undulata opercula or an otolith of the fish Argyrosomus hololepidotus because they failed to act as closed systems. A U–Th age of 103 ka for a calcrete sheet within the 240 ka sand indicates a later period of carbonate deposition. Calcium carbonate dripstone from a LIG wave-cut notch gave a U–Th age of 11–14 ka suggesting sediment cover created a cave-like environment at the notch at this time. The three dating techniques have collectively built a chronology spanning the periods before and after deposition of the shell bed, which occurred just after the LIG sea-level maximum (120–125 ka).

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45

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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46

Cox, James W., Danielle P. Oliver, Nigel K. Fleming, and Jenny S. Anderson. "Off-site transport of nutrients and sediment from three main land-uses in the Mt Lofty Ranges, South Australia." Agricultural Water Management 106 (April 2012): 50–59. http://dx.doi.org/10.1016/j.agwat.2011.08.014.

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47

Cartwright, I. "Changes in Oxygen Isotope Ratios of Metasediments During Regional-Metamorphic Crustal-Scale Fluid Flow, Mount Lofty Ranges, South Australia." Mineralogical Magazine 58A, no. 1 (1994): 154–55. http://dx.doi.org/10.1180/minmag.1994.58a.1.83.

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48

POPPLE, LINDSAY W., and DAVID L. EMERY. "Five new species of Yoyetta Moulds (Hemiptera: Cicadidae: Cicadettinae) from south-eastern Australia." Zootaxa 5141, no. 5 (May 30, 2022): 401–41. http://dx.doi.org/10.11646/zootaxa.5141.5.1.

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Five new species are described in the genus Yoyetta Moulds, each belonging to the Yoyetta tristrigata (Goding and Froggatt) species group. Yoyetta australicta n. sp. occurs in southern eucalypt woodlands in two separate populations, one extending from the foothills of the Mt Lofty Ranges and southern fringes of Adelaide north to the Flinders Ranges, and the other from Warrumbungle National Park and from Clandulla, near Orange and near Grenfell in New South Wales south to Mt Taylor in the Australian Capital Territory. Yoyetta corindi n. sp. has a restricted, coastal and subcoastal warm temperate distribution in north-eastern New South Wales open forest communities between Trustums Hill and Arrawarra, extending inland from south-west of Grafton to Tyringham. Yoyetta delicata n. sp. has an inland warm temperate distribution in eucalypt woodland and open forest from near Killarney and west of Warwick in south-east Queensland south to Cassilis and near Wyong in central New South Wales. Yoyetta ignita n. sp. is found from Flinders Peak and Mt Tamborine in south-east Queensland, south along the Great Dividing Range (and inland to Mt Kaputar) in New South Wales, with a disjunct population on the eastern slopes of Mt Ainslie in the Australian Capital Territory. Yoyetta robusta n. sp. is found from the Granite Belt in south-east Queensland south to the Glenn Innes area in northern New South Wales. The new species are all small–medium sized cicadas (15–25 mm body length) with male calling songs that are distinguishable from one another and from other species in the genus. In three of the new species (Y. australicta n. sp., Y. corindi n. sp. and Y. robusta n. sp.), the songs are characterised by sharp, high energy ticks or clicks, produced mainly in flight. Each of these species also produces ticks or clicks, sometimes in combination with a short buzz, while stationary. Of the remaining two species, one (Y. delicata n. sp.) produces a soft, coarse buzzing song while stationary and the other (Y. ignita n. sp.) produces a combination of buzzes and clicks while stationary. A key to species in the Y. tristrigata species group is provided.

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49

Smith, John V. "Textures recording transient porosity in synkinematic quartz veins, South Coast, New South Wales, Australia." Journal of Structural Geology 27, no. 2 (February 2005): 357–70. http://dx.doi.org/10.1016/j.jsg.2004.09.003.

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50

Mitchell, GJ, RJ Carter, and SR Chinner. "Studies on the control of water-dropwort (Oenanthe pimpinelloides) in South Australia." Australian Journal of Experimental Agriculture 35, no. 4 (1995): 483. http://dx.doi.org/10.1071/ea9950483.

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Water-dropwort (Oenanthe pimpinelloides L.), a tuberous perennial herb, is currently known in South Australia from only a single locality in the Mount Lofty Ranges. There is little information on water-dropwort control, and 2 experiments were conducted to assess the effects of sowing pasture, with or without presowing herbicides, on the control of this weed. Phalaris (Phalaris aquatica L.) and perennial clovers were successfully introduced into infested pastures by direct drilling in autumn. Water-dropwort regenerated from seed more densely in unsown plots than plots of established perennial pasture, suggesting that upgrading pastures may be a strategy to reduce the rate of spread by seed of this weed. A range of herbicide treatments applied to waterdropwort at the stem elongation stage in spring before autumn sowing of pastures provided effective shortterm control. The best short-term control was provided by glyphosate at 1440 g a.i./ha; metsulfuron methyl at 6, 12, and 36 g a.i./ha; and metsulfuron methyl at 12 g a.i./ha tank-mixed with glyphosate or 2,4-D amine at 720 or 1000 g a.i./ha, respectively. These treatments, and chlorsulfuron at 21 g a.i./ha, also significantly (P<0.05) reduced water-dropwort abundance (relative to untreated areas) for up to 18 months after sowing and initially improved the density of sown pasture species, but these improvements were not evident 14 months after resowing. Although prior season herbicide treatments controlled water-dropwort in newly sown pastures, 2 separate applications of herbicides, in May and October, gave no better control of water-dropwort than a single herbicide application in spring. Water-dropwort infestations do not appear to prevent successful direct drilling of phalaris and perennial clovers. Although pasture renovation did not provide long-term suppression of water-dropwort, the maintenance of vigorous pastures may reduce the rate of population growth from seedlings of this weed. Recropping restrictions may limit the role of chlorsulfuron for water-dropwort control in pasture renovation situations.

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