D
David M. Price
Researcher at University of Wollongong
Publications - 105
Citations - 4450
David M. Price is an academic researcher from University of Wollongong. The author has contributed to research in topics: Quaternary & Holocene. The author has an hindex of 39, co-authored 105 publications receiving 4172 citations.
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Journal ArticleDOI
Wetting and drying of Australia over the past 300 ka
TL;DR: In this paper, thermoluminescence (TL) dates and 18 U/Th dates from alluvial and eolian sediments have been used to provide evidence of widespread climate and flow-regime changes in Australia.
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Sea-level and environmental changes since the last interglacial in the Gulf of Carpentaria, Australia: an overview
Allan R. Chivas,Adriana García,Sander van der Kaars,Martine J.J. Couapel,Sabine Holt,Jessica M Reeves,David J Wheeler,Adam D. Switzer,Colin V. Murray-Wallace,Debabrata Banerjee,Debabrata Banerjee,David M. Price,Sue X Wang,Grant Pearson,N Terry Edgar,Luc Beaufort,Patrick De Deckker,Ewan Lawson,C. Blaine Cecil +18 more
TL;DR: In this article, a preliminary interpretation of the palaeoenvironments recorded in six sediment cores collected by the IMAGES program in the Gulf of Carpentaria is presented, which includes a record of sea-level/lake-level changes, with particular complexity between 80 and 40 years.
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Chronology of Murrumbidgee River palaeochannels on the Riverine Plain, southeastern Australia
TL;DR: In this paper, the ages of four major periods of palaeochannel activity have been identified on the Murrumbidgee sector of the Riverine Plain of southeastern Australia.
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Aeolian and fluvial evidence of changing climate and wind patterns during the past 100 ka in the western Simpson Desert, Australia
TL;DR: Sediments near Finke in central Australia provide evidence of late Quaternary evolution and the interaction of aeolian and fluvial systems in response to changing climate in the western Simpson Desert.
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Evidence of Tsunami Sedimentation on the Southeastern Coast of Australia
TL;DR: In contrast to storm waves, tsunamis can leave a depositional imprint of their passage characterized by chaotic sort of sediment features as discussed by the authors, which can be used to account for large-scale, anomalous sediment features.