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Karst evolution of the Nullarbor Plain, Australia.
Geological Society of America Special Paper , 65—78 Sandiford, M. The tilting continent: A new constraint on the dynamic topographic field from Australia. Fujioka, T. History of Australian aridity: chronology in the evolution of arid landscapes. Geological Society , London , Special Publications 3 46 , — Stone, J. Limestone erosion measurements with cosmogenic chlorine in calcite — preliminary results from Australia. Miller, C. Prolonged carbonate diagenesis under an evolving late cenozoic climate: Nullarbor Plain, southern Australia.
Sedimentary Geology , 33—49 Hillis, R. Geological Society, London, Special Publications , 71—89 Stock, G. Pace of landscape evolution in the Sierra Nevada, California, revealed by cosmogenic dating of cave sediments. Geology 32 , — Anthony, D. A Late Tertiary origin for multilevel caves along the western escarpment of the Cumberland Plateau, Tennessee and Kentucky, established by cosmogenic 26 Al and 10 Be. Journal of Cave and Karst Studies 66 , 46—55 Granger, D. Quaternary downcutting rate of the New River, Virginia, measured from differential decay of cosmogenic 26 Al and 10 Be in cave-deposited alluvium.
Geology 25 , — GSA Bulletin , — Lundberg, J. Pleistocene depositional history in a periglacial terrane: A k. Geosphere 3 , — Rixhon, G. Improvements in Th dating, Th and U half-life values, and U—Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry. Earth and Planetary Science Letters — , 82—91 Hellstrom, J. Journal of Analytical Atomic Spectrometry 18 , — Drysdale, R.
Vegetation and climate change in southwestern Australia during the Last Glacial Maximum. G eophysical Research Letters in review. Veizer, J. In Tre atise on Ge ochem istry eds Turekian, K. Elsevier Paton, C. Iolite: Freeware for the visualisation and processing of mass spectrometric data. Journal of Analytical Atomic Spectrometry , Schmitz, M. Derivation of isotope ratios, errors, and error correlations for U-Pb geochronology using Pb- U- U -spiked isotope dilution thermal ionization mass spectrometric data.
Geochemistry, Geophysics, Geosystems 8 , Q Ludwig, K. A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication1a Powell, R. Improving isochron calculations with robust statistics and the bootstrap. U and Pb variability in older speleothems and strategies for their chronology. Quaternary Geochronology 14 , — Cox, R. Chemical Geology , 21—32 Chemical Geology — , — Prideaux, G. An arid-adapted middle Pleistocene vertebrate fauna from south-central Australia.
Download references. Nullarbor speleothem samples were obtained over a period of many years and numerous expeditions by various parties: appropriate sampling permits were in place where applicable.
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Most of the cave systems noted in this study are located on pastoral leases and we thank the many station owners who have over the years allowed access to their properties for research purposes. Gavin Prideaux is thanked for assistance with field logistics. Jon D. Tireless cave exploration efforts by P. Correspondence to Jon D. Reprints and Permissions. The antiquity of Nullarbor speleothems and implications for karst palaeoclimate archives.
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Sci Rep 9, Download citation. Received : 02 September Accepted : 30 November Published : 24 January Geology Geochronology Palaeogeography, Palaeoclimatology, Palaeoecology Chemical Geology The Holocene By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.
Advanced search. Skip to main content Thank you for visiting nature. Download PDF. Subjects Geochemistry Palaeoclimate. Abstract Speleothems represent important archives of terrestrial climate variation that host a variety of proxy signals and are also highly amenable to radiometric age determination. Introduction Speleothems secondary cave calcite deposits including stalagmites, stalactites and flowstones are increasingly recognised as critical sources of climate history. Figure 1. Full size image. We […].
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