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Late Pleistocene and Early Holocene aeolian deposits of Tasmania and their climatic implications

Published online by Cambridge University Press:  13 November 2020

Peter D. McIntosh Open the ORCID record for Peter D. McIntosh [Opens in a new window] ,
Christina Neudorf ,
Olav B. Lian Open the ORCID record for Olav B. Lian [Opens in a new window] ,
Adrian J. Slee ,
Brianna Walker ,
Rolan Eberhard ,
Richard Doyle  and
Grant Dixon
Peter D. McIntosh*
Affiliation:
Forest Practices Authority, 30 Patrick Street, Hobart, TAS, 7000, Australia
Christina Neudorf
Affiliation:
Division of Earth and Ecosystem Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, NV, 89512, USA
Olav B. Lian
Affiliation:
School of Land Use and Environmental Change, University of the Fraser Valley, 33844 King Road, Abbotsford, BCV2S 7M8, Canada
Adrian J. Slee
Affiliation:
Forest Practices Authority, 30 Patrick Street, Hobart, TAS, 7000, Australia
Brianna Walker
Affiliation:
Tasmanian Institute of Agriculture, University of Tasmania, Churchill Avenue, Hobart, TAS7005, Australia
Rolan Eberhard
Affiliation:
Department of Primary Industries, Parks, Water and the Environment, 134 Macquarie St., Hobart, TAS, 7000, Australia
Richard Doyle
Affiliation:
Tasmanian Institute of Agriculture, University of Tasmania, Churchill Avenue, Hobart, TAS7005, Australia
Grant Dixon
Affiliation:
Department of Primary Industries, Parks, Water and the Environment, 134 Macquarie St., Hobart, TAS, 7000, Australia
*
*Corresponding author at: Forest Practices Authority, 30 Patrick Street, Hobart, TAS, 7000Australia E-mail address: peter.mcintosh@fpa.tas.gov.au (P. McIntosh)
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Abstract

Late Pleistocene and Early Holocene aeolian deposits in Tasmania are extensive in the present subhumid climate zone but also occur in areas receiving >1000 mm of rain annually. Thermoluminescence, optically stimulated luminescence, and radiocarbon ages indicate that most of the deposits formed during periods of cold climate. Some dunes are remnants of longitudinal desert dunes sourced from now-inundated continental shelves which were previously semi-arid. Others formed near source, often in the form of lunettes east of seasonally-dry lagoons in the previously semi-arid Midlands and southeast of Tasmania, or as accumulations close to floodplains of major rivers, or as sandsheets in exposed areas. Burning of vegetation by the Aboriginal population after 40 ka is likely to have influenced sediment supply. A key site for determining climate variability in southern Tasmania is Maynes Junction which records three periods of aeolian deposition (at ca. 90, 32 and 20 ka), interspersed with periods of hillslope instability. Whether wind speeds were higher than at present during the last glacial period is uncertain, but shells in the Mary Ann Bay sandsheet near Hobart and particle size analysis of the Ainslie dunes in northeast Tasmania suggest stronger winds during the last glacial period than at present.

Keywords

AeolianTasmaniaPalaeoclimateOptically stimulated luminescence (OSL)Thermoluminescence (TL)Thermally-transferred OSL (TT-OSL)Wind speedDuneLunettesSemi-aridLast Glacial Maximum (LGM)
Type
Thematic Set: Southern Hemisphere Last Glacial Maximum (SHeMax)
Information
Quaternary Research , Volume 102 , July 2021 , pp. 91 - 114
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Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020

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References

REFERENCES

Allen, J. (Ed.), 1996. Report of the Southern Forests Archaeological Project. Vol. 1, Site Descriptions, Stratigraphies and Chronologies. Archaeology Publications, School of Archaeology, La Trobe University.Google Scholar
Barrows, T.T., Juggins, S., De Dekker, P., Calvo, E., Pelejero, C., 2007. Long-term sea-surface temperatures and climate change in the Australian-New Zealand region. Paleooceanography 22, 2215.CrossRefGoogle Scholar
Baynes, F.J., 1990. A Preliminary Survey of the Coastal Geomorphology of the World Heritage Area, South West Tasmania. Unpublished Report for the Department of Parks, Wildlife and Heritage, Tasmania.Google Scholar
Blom, W.M., 1988. Late Quaternary sediments and sea levels in Bass basin, southeastern Australia–a preliminary report. Search 19, 94–96.Google Scholar
Bowden, A.R., 1983. Relict terrestrial dunes: legacies of a former climate in coastal northeastern Tasmania. Zeitschrift für Geomophologie Supplement 45, 153–174.Google Scholar
Bowler, J.M., 1998. Willandra lakes revisited: environmental framework for human occupation. Archaeology in Oceania 33, 120–155.CrossRefGoogle Scholar
Bowler, J.M., Price, D.M., 1998. Luminescence dates and stratigrahic analyses at Lake Mungo: review and new perspectives. Archaeology in Oceania 33, 156–168.CrossRefGoogle Scholar
Bowler, J.M., Wasson, R.J., 1984. Glacial age environments of arid Australia. Transactions, Institute of British Geographers 56, 77–110.Google Scholar
Bradbury, J., 1994. Aeolian Landforms in the Lake Ada - Lake Augusta area: A Preliminary Investigation and Management Strategy. Draft Report of National Parks and Wildlife Service. Department of Primary Industries and Water, Tasmania.Google Scholar
Bradbury, J., 2014. A revised geological map of lungtalanana (Clarke Island) and brief explanatory notes. In: Natural and Cultural Heritage Division. lungtalanana (Clarke Island), Natural Values Survey 2014. Hamish Saunders Memorial Trust, New Zealand and Natural and Cultural Heritage Division, DPIPWE, Hobart. Nature Conservation Report Series 15/2, pp. 36–61.Google Scholar
Bragg, F.J., Prentice, I.C., Harrison, S.P., Eglinton, G., Foster, P.N., Rommerskirchen, F., Rullkőtter, J., 2012. Stable isotope and modelling evidence that CO2 drives vegetation changes in the tropics. Biogeosciences Discussions 9, 156699–15722.Google Scholar
Bronk Ramsey, C., 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51, 337–360.CrossRefGoogle Scholar
Bruce, J.G., 1971. Loessial deposits in southern South Island, with a definition of Stewarts Claim formation. New Zealand Journal of Geology and Geophysics 16, 533–548.CrossRefGoogle Scholar
Bureau of Meterology, 2020. Climate statistics for Australian locations. http://www.bom.gov.au/climate/averages/tables/cw_094008_All.shtmlGoogle Scholar
Calver, C.R., 2007. Some notes on the geology of King Island. Tasmania Geological Survey Record 2007/02, Department of Infrastructure, Mineral Resources, Tasmania.Google Scholar
Colhoun, E.A., 1977. A sequence of late Quaternary deposits at Pipe Clay Lagoon, southeastern Tasmania. Papers and Proceedings of the Royal Society of Tasmania 111, 1–12.Google Scholar
Colhoun, E.A., 1985. Glaciations of the West Coast Range, Tasmania. Quaternary Research 24, 39–59.CrossRefGoogle Scholar
Colhoun, E.A., 2002. Periglacial landforms and deposits of Tasmania. South African Journal of Science 98, 55–63.Google Scholar
Colhoun, E.A., Turner, E., van der Geer, G., 1982. Late Pleistocene molluscan faunas from four sites in Tasmania. Papers and Proceedings of the Royal Society of Tasmania 166, 91–96.CrossRefGoogle Scholar
Comfort, M., Eberhard, R., 2011. The Tasmanian geoconservation database: a tool for promoting the conservation and sustainable management of geodiversity. Proceedings of the Linnean Society of New South Wales 132, 27–36.Google Scholar
Compton, J.S., 2011. Pleistocene sea-level fluctuations and human evolution on the southern coastal plain of South Africa. Quaternary Science Reviews 30, 506–527.CrossRefGoogle Scholar
Cosgrove, R., 1985. New evidence for early Holocene Aboriginal occupation in northeast Tasmania. Australian Archaeology 21, 19–36.CrossRefGoogle Scholar
Cullen, P., Dell, M., 2013. Geomorphological evolution of the Prion Beach and New River Lagoon beach barrier system. Nature Conservation Report Series 2013/03. Department of Primary Industries, Parks, Water and Environment, Tasmania.Google Scholar
Delmonte, B, Basile-Doelsch, I., Petit, J.-R., Maggi, V., Revel-Rolland, M., Michard, A., Jagoutz, E., Grousset, F., 2004. Comparing the Epica and Vostok dust records during the last 220,000 years: stratigraphical correlation and provenance in glacial periods. Earth Science Reviews 66, 63–87.CrossRefGoogle Scholar
Dixon, G., 1996. A reconnaissance inventory of sites of geoconservation significance on Tasmanian islands. Report for Parks and Wildlife Service, Tasmania and Australian Heritage Commission, Canberra.Google Scholar
Dixon, G., 1997. A preliminary survey of the distribution and conservation significance of inland aeolian features in the Midlands, Northeast and Southeast Tasmania. Parks and Wildlife Service, Tasmania.Google Scholar
Donaldson, P., 2010. Facies architecture and radar stratigraphy of the Seven Mile Spit complex, Tasmania. Unpublished Honours thesis, School of Earth Sciences, University of Tasmania.Google Scholar
Doyle, R.B., 1993. Soils of the South Esk Sheet Tasmania (southern half). Soil Survey Series of Tasmania No. 1. Department of Primary Industries and Fisheries, Tasmania.Google Scholar
Duller, G.A.T., Augustinus, P., 1997. Luminescence studies of dunes from north-eastern Tasmania. Quaternary Science Reviews (Quaternary Geochronology) 16, 357–365.CrossRefGoogle Scholar
Duller, G.A.T., Augustinus, P., 2006. Reassessment of the record of linear dune activity in Tasmania using optical dating. Quaternary Science Reviews 25, 2608–2618.CrossRefGoogle Scholar
Eberhard, R., 2009. Geodiversity. In: Harris, S., Driessen, M., Bell, P. (Eds). Prime Seal Island Scientific Expedition 2008. Hamish Saunders Memorial Trust, New Zealand and Biodiversity Conservation Branch, DPIPWE, Hobart, Nature Conservation Report Series 09/3, pp. 10–25.Google Scholar
Eberhard, R., 2017. Aspects of geodiversity on Hunter Island: four Quaternary age geosites. In: Natural and Cultural Heritage Division, South Hunter and Stack Island Natural and Cultural Values Survey. Hamish Saunders Memorial Trust, New Zealand and the Natural and Cultural Heritage Division, DPIPWE, Hobart. Nature Conservation Report 17/4, pp. 68–90.Google Scholar
Eberhard, R., Sharples, C., Bowden, N., Comfort, M., 2015. Monitoring the Erosion Status of Oceanic Beaches in the Tasmania Wilderness World Heritage Area: Establishment Report. Nature Conservation Report Series 15/3. Natural & Cultural Heritage Division, Department of Primary Industries, Parks, Water & Environment, Hobart.Google Scholar
Falster, G., Tyler, J., Grant, K., Tibby, J., Turney, C., Lőhr, S., Jacobsen, G., Kershaw, A.P., 2018. Millennial-scale variability in south-east Australian hydroclimate between 30,000 and 10,000 years ago. Quaternary Science Reviews 192, 106–122.CrossRefGoogle Scholar
Fletcher, M-S., Hall, T., Alexandra, A.N., 2020. The loss of an indigenous constructed landscape following British invasion of Australia: an insight into the deep human imprint on the Australian landscape. Ambio. https://doi.org/10.1007/s13280-020-01339-3.CrossRefGoogle Scholar
Fletcher, M-S., Thomas, I., 2010. The origin and temporal development of an ancient cultural landscape. Journal of Biogeography 37, 2183–2196.CrossRefGoogle Scholar
Galbraith, R.F., Roberts, R.G., Laslett, G.M., Yoshida, H., Olley, J.M., 1999. Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia: Part I, experimental design and statistical models. Archaeometry 41, 339–364.CrossRefGoogle Scholar
Gammage, B., 2011. The Biggest Estate on Earth: How Aborigines made Australia. Allen & Unwin, Sydney.Google Scholar
Gardner, T.W., Webb, J., Davis, A.G., Cassel, E.J., Pezzia, C., Merrits, D.J., Smith, B., 2006. Late Pleistocene landscape response to climate change: eolian and alluvial fan deposition, Cape Liptrap, southeastern Australia. Quaternary Science Reviews 25, 1552–1569.CrossRefGoogle Scholar
Gillespie, R., Camens, A.B., Worthy, T.H., Rawlence, N.J., Reid, C., Bertuch, F., Levchenko, V., Cooper, A., 2012. Man and megafauna in Tasmania: closing the gap. Quaternary Science Reviews 37, 38–47.CrossRefGoogle Scholar
Grant, J.C., Laffan, M.D., Hill, R.B., Neilsen, W.A., 1995. Forest Soils of Tasmania. Forestry Tasmania, Hobart.Google Scholar
Hellstrom, J., McCulloch, M., Stone, J., 1998. A detailed 31,000 year record of climate and vegetation change, from isotope geochemistry of two New Zealand speleothems. Quaternary Research 50, 167–178.CrossRefGoogle Scholar
Hesse, P.P., 1994. The record of continental dust from Australia in Tasman Sea sediments. Quaternary Science Reviews 13, 257–272.CrossRefGoogle Scholar
Hesse, P.P., 2016. How do longitudinal dunes respond to climate forcing? Insights from 25 years of luminescence dating of the Australian desert dunefields. Quaternary International 410, 11–29.CrossRefGoogle Scholar
Hesse, P.P., Humphreys, G.S., Smith, B.L., Campbell, J., Peterson, E.K., 2003. Age of loess deposits in the central tablelands of New South Wales. Australian Journal of Soil Research 41, 1115–1131.CrossRefGoogle Scholar
Hesse, P.P., McTainsh, G.H., 1999. Last glacial maximum to early Holocene wind strength in the mid-latitudes of the southern hemisphere from aeolian dust in the Tasman Sea. Quaternary Research 52, 343–349.CrossRefGoogle Scholar
Hesse, P.P., McTainsh, G.H., 2003. Australian dust deposits: modern processes and the Quaternary record. Quaternary Science Reviews 22, 2007–2035.CrossRefGoogle Scholar
Jennings, J.N., 1957. Coastal dune lakes as exemplified from King Island, Tasmania. Geographical Journal 123, 59–70.CrossRefGoogle Scholar
Jennings, J.N., 1959. The coastal geomorphology of King Island, Bass Strait in relation to changes in the relative level of land and sea. Records of the Queen Victoria Museum 11, 1–39.Google Scholar
Johnson, C., 2006. Australia's Mammal Extinctions: A 50 000 year History. Cambridge University Press. Melbourne.Google Scholar
Kershaw, R.C., Sutherland, F.L., 1972. Quaternary geomorphology on Flinders Island. Records of the Queen Victoria Museum 43, 28 pp.Google Scholar
Lambeck, K., Chappell, J., 2001. Sea level change through the last glacial cycle. Science 292, 679–685.CrossRefGoogle ScholarPubMed
Lewis, S.E., Sloss, C.R., Murray-Wallace, C.V., Woodroffe, C.D., Smithers, S.G., 2013. Post-glacial sea-level changes around the Australian margin: a review. Quaternary Science Reviews 74, 115–138.CrossRefGoogle Scholar
Lisiecki, L.E., Raymo, M.E., 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, dx.doi.org/10.1029/2004PA001071.Google Scholar
Lourandos, H., 1970. Coast and Hinterland: The Archaeological Sites of Eastern Tasmania. Thesis, Department of Prehistory and Anthropology, Australian National University, Canberra.Google Scholar
Mackenzie, L., Moss, P., 2014. A late Quaternary record of vegetation and climate change from Hazards Lagoon, eastern Tasmania. Quaternary International 432, 58–65.CrossRefGoogle Scholar
Macphail, M.K., Jackson, W.D., 1978. The late Pleistocene and Holocene history of the Midlands of Tasmania. Proceedings of the Royal Society of Victoria 90, 287–300.Google Scholar
Manaaki Whenua Soils Portal, 2020. https://soils.landcareresearch.co.nz/describing-soils/nzsc/soil-order/pallic-soils (accessed 20 March 2020).Google Scholar
Matthews, W.L., 1975. Geological atlas 1:50,000 series, Lake River. Tasmania Department of Mines, Hobart.Google Scholar
Matthews, W.L., 1983. Geology and groundwater resources of the Longford Tertiary basin. Geological Survey Bulletin 59. Tasmania Department of Mines.Google Scholar
Mazengarb, C., Stevenson, M.D., 2016. Pleistocene coastal terraces in northern Tasmania revisited; what do they tell us about landscape evolution and uplift rates? Presented paper, AESC 2016 – Australian Earth Sciences Convention; Uncover Earth's Past to Discover Our Future, Adelaide Convention Centre. Geological Society of Australia.Google Scholar
McClenaghan, M.P. (Compiler), 2006. Digital Geological Atlas 1:25000 series, Sheet 5447, Waterhouse. Mineral Resources Tasmania, Rosny.Google Scholar
McIntosh, P.D., 1984. Genesis and classification of a sequence of soils formed from aeolian parent materials in East Otago, New Zealand. Australian Journal of Soil Research 22, 219–242.CrossRefGoogle Scholar
McIntosh, P.D., 2012a. Soil characterisation at the Warra Flux Tower supersite. Version 2, with supplementary data. Forest Practices Authority Contract Report, prepared for Forestry Tasmania, 16 pp.Google Scholar
McIntosh, P.D., 2012b. Dated geoconservation sites in the forest estate in Tasmania, 2004–2012. Forest Practices Authority Technical Report 2. Forest Practices Authority, Hobart.Google Scholar
McIntosh, P.D., 2015a. Soils and Land Capability in the Kempton–Melton Mowbray Road Corridor. Contract report for State Growth, April 2015. Forest Practices Authority, Hobart, 19 pp.Google Scholar
McIntosh, P.D., 2015b. Comments on the paper ‘Stratigraphy and geochronology of Quaternary marine terraces of Tasmania, Southeastern Australia: implications on neotectonism by Jaeryul Shin, Geosciences Journal 17, p. 429–443’. Geosciences Journal 19, 575–578.CrossRefGoogle Scholar
McIntosh, P.D., 2018. Dating Wasson's Derwent Valley fans. Quaternary Australasia 35, 9.Google Scholar
McIntosh, P.D., Eberhard, R., Slee, A., Moss, P., Price, D.M., Donaldson, P., Doyle, R., Martins, J., 2012. Late Quaternary extra-glacial cold-climate deposits in low and mid-altitude Tasmania and their climatic implications. Geomorphology 179, 21–39.CrossRefGoogle Scholar
McIntosh, P.D., Kiernan, K., Price, D.M., 2004. An aeolian sediment pulse at c. 28 kyr BP in southern Tasmania. Journal of the Royal Society of New Zealand 34, 369–379.CrossRefGoogle Scholar
McIntosh, P.D., Price, D.M., Eberhard, R., Slee, A., 2008. Late Quaternary erosion chronology in lowland and mid-altitude Tasmania. Forest Practices Authority, Scientific Report 5.Google Scholar
McIntosh, P.D., Price, D.M., Eberhard, R., Slee, A.J., 2009. Late Quaternary erosion events in lowland and mid-altitude Tasmania in relation to climate change and first human arrival. Quaternary Science Reviews 28, 850–872.CrossRefGoogle Scholar
McIntosh, P.D., Price, D.M., Grove, S., Slee, A.J., 2013. ‘Reply to Murray-Wallace et al. (2013): comments on a paper by Slee et al. (2012). A reassessment of last interglacial deposits at Mary Ann Bay, Tasmania’. Quaternary Australasia 30, 4–8.Google Scholar
Murray-Wallace, C.V., Goede, A., 1991. Aminostratigraphy and electron spin resonance dating of late Quaternary sea level change and coastal neotectonics in Tasmania, Australia. Zeitschift für Geomorphologie 35, 129–149.CrossRefGoogle Scholar
Murray-Wallace, C.V., Goede, A., 1995. Aminostratigraphy and electron spin resonance dating of Quaternary coastal neotectonism in Tasmania and the Bass Strait islands. Australian Journal of Earth Sciences 42, 51–67.CrossRefGoogle Scholar
Murray-Wallace, C.V., Woodroffe, C.D., 2014. Quaternary Sea-Level Changes: A Global Perspective. Cambridge University Press. Cambridge, England.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2000. Luminescence dating of quartz using an improved single aliquot regenerative dose protocol. Radiation Measurements 32, 57–73.CrossRefGoogle Scholar
Nanson, G.C., Chen, X.Y., Price, D.M., 1995. Aeolian and fluvial evidence of changing climate and wind patterns during the past 100 ka in the western Simpson Desert, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 113, 87–102.CrossRefGoogle Scholar
Neudorf, C.M., Lian, O.B., McIntosh, P.D., Gingerich, T.B., Augustinus, P.C., 2019. Investigation into the OSL and TT-OSL signal characteristics of ancient (>100 ka) Tasmanian aeolian quartz and its utility as a geochronometer for understanding long-term climate-driven landscape change. Quaternary Geochronology 53, 101005.CrossRefGoogle Scholar
Olley, J., 2010. Peer review of the TASI 10757 Jordan River, Brighton, Tasmania: luminescence chronology (Cupper, May 2010). Unpublished Griffith University Report to Department of Primary Industries, Parks, Water and Environment, Hobart, Tasmania.Google Scholar
Osok, R., Doyle, R., 2004. Soil development on dolerite and its implications for landscape history in southeastern Tasmania. Geoderma 121, 169–186.CrossRefGoogle Scholar
Paton, R., 2010. Draft Final Archaeology Report on the Test Excavations of the Jordan River Levee Site, southern Tasmania. Robert Paton Archaeological Studies Pty Ltd, Tasmania.Google Scholar
Petit, J.-R., Briat, M., Royer, A., 1981. Ice age aerosol content from East Antarctic ice core samples and past wind strength. Nature 293, 391–394.CrossRefGoogle Scholar
Pinkard, G.J., 1980. Land Systems of Tasmania, Region 4. Tasmanian Department of Agriculture, Hobart.Google Scholar
Reffet, E., Courrech du Pont, S., Hersen, P., Douady, S., 2010. Formation and stability of transverse and longitudinal sand dunes. Geology 38, 491–494..CrossRefGoogle Scholar
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Ramsey, C.B., Buck, C.E., et al. , 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887.CrossRefGoogle Scholar
Rule, S., Brook, B.W., Haberle, S.G., Turney, C.S.M., Kershaw, A.P., Johnson, C.N., 2012. The aftermath of megafaunal extinction: ecosystem transformation in Pleistocene Australia. Science 335, 1483–1486.CrossRefGoogle ScholarPubMed
Sharples, C., 1996. A Reconnaissance of Landforms and Geological Sites of Geoconservation Significance in the Murchison Forest District. Report to Forestry Tasmania. (2 vols.)Google Scholar
Sharples, C., 1997. Geoconservation Survey of Bridport - Waterhouse Telstra Cable Route. Report for Telstra Corporation Ltd, Hobart.Google Scholar
Sharples, C., Walford, H., Watson, C., Ellison, J.C., Hua, Q., Bowden, N., Bowman, D., 2020. Ocean Beach, Tasmania: a swell-dominated shoreline reaches climate-induced recessional tipping point? Marine Geology 419, 106081.CrossRefGoogle Scholar
Shepherd, M.J., Price, D.M., 1990. Thermoluminescence dating of late Quaternary dunesand, Manawatu/Horowhenua area, New Zealand, a comparison with 14C age determinations. New Zealand Journal of Geology and Geophysics 33, 535–539.CrossRefGoogle Scholar
Shin, J., 2013. Stratigraphy and geochronology of Quaternary marine terraces of Tasmania, southeastern Australia: implications on neotectonism. Geosciences Journal 17, 429–443.CrossRefGoogle Scholar
Sigleo, W.R., Colhoun, W.A., 1982. Terrestrial dunes, man and the late Quaternary environment in southern Tasmania. Palaeogeography, Palaeoclimatology, Palaeoecology 39, 87–121.CrossRefGoogle Scholar
Slee, A.J., McIntosh, P.D., Price, D.M., Grove, S., 2012. A reassessment of last interglacial deposits at Mary Ann Bay, Tasmania. Quaternary Australasia 29, 4–11.Google Scholar
Sutherland, F.L., Kershaw, R.C., 1971. The Cainozoic geology of Flinders Island, Bass Strait. Papers and Proceedings of the Royal Society of Tasmania 105, 151–176.Google Scholar
Turney, C.S.M., Flannery, T.F., Roberts, R.G., Reid, C., Fifield, L.K., Higham, T.F.G., Jacobs, Z., et al. , 2008. Late-surviving megafauna in Tasmania, Australia, implicate human involvement in their extinction. Proceedings of the National Academy of Sciences 105, 12150–12153.CrossRefGoogle ScholarPubMed
Twidale, C.R., 1957. A reconnaissance of the Corinna-Pieman Heads area – geomorphology. Papers and Proceedings of the Royal Society of Tasmania 91, 9–17.Google Scholar
Vandergoes, M.J., Newnham, R.M., Denton, G. H., Blaauw, M., Barrell, D.J.A., 2013. The anatomy of last glacial maximum climate variations in south Westland, New Zealand, derived from pollen records. Quaternary Science Reviews 74, 215–229.CrossRefGoogle Scholar
Walker, B.J.R., 2016. Late Pleistocene climatic oscillations inferred by soil stratigraphic analysis of southern Tasmanian Quaternary sediments. Honours Thesis, University of Tasmania.Google Scholar
Wasson, R.J., 1977. Catchment processes and the evolution of alluvial fans in the Lower Derwent valley, Tasmania. Zeitschrift für Geomorphologie 21, 147–168.Google Scholar
Wasson, R.J., Hyde, R., 1983. Factors determining desert dune type. Nature 304, 337–339.CrossRefGoogle Scholar
Zhou, L., Williams, M.A.J., Petersen, J.A., 1994. Late Quaternary aeolianites, palaeosols and depositional environments on the Nepean peninsula, Victoria, Australia. Quaternary Science Reviews 13, 225–239.CrossRefGoogle Scholar
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