Aeolian-fluvial interaction and climate change: source-bordering dune development over the past ~100 ka on Cooper Creek, central Australia

Article

Maroulis, Jerry C., Nanson, Gerald C., Price, David M. and Pietsch, Tim. 2007. "Aeolian-fluvial interaction and climate change: source-bordering dune development over the past ~100 ka on Cooper Creek, central Australia." Quaternary Science Reviews: the international multidisciplinary research and review journal. 26 (3-4), pp. 386-404. https://doi.org/10.1016/j.quascirev.2006.08.010
Article Title

Aeolian-fluvial interaction and climate change: source-bordering dune development over the past ~100 ka on Cooper Creek, central Australia

ERA Journal ID1756
Article CategoryArticle
AuthorsMaroulis, Jerry C. (Author), Nanson, Gerald C. (Author), Price, David M. (Author) and Pietsch, Tim (Author)
Journal TitleQuaternary Science Reviews: the international multidisciplinary research and review journal
Journal Citation26 (3-4), pp. 386-404
Number of Pages19
Year2007
Place of PublicationOxford, United Kingdom
ISSN0277-3791
1873-457X
Digital Object Identifier (DOI)https://doi.org/10.1016/j.quascirev.2006.08.010
Web Address (URL)https://www.sciencedirect.com/science/article/abs/pii/S027737910600271X
Abstract

This study provides an interpretation of interrelated Quaternary fluvial and aeolian activity related to climate change on Cooper Creek in the Lake Eyre Basin in southwestern Queensland, central Australia. The extensive muddy floodplain is characterised by buried sandy palaeochannels now almost entirely invisible but stratigraphically connected to source-bordering dunes that emerge as distinctive sandy islands through the floodplain surface. Luminescence dating has identified pronounced periods of fluvial activity represented by abundant sandy alluvium from Marine Isotope Stages (MIS) 8–3. While all these sandy fluvial episodes on Cooper Creek were much
more powerful than anything subsequent, they appear to be ranked in order of declining activity. MIS 8–6 saw reworking of almost the entire floodplain whereas subsequent phases of reworking were far less extensive. Source-bordering dunes were derived from active sandy channels in late MIS 5 (85–80 ka) and mid MIS 3 (50–40 ka). After

KeywordsCooper Creek; climate change; quaternary chronology; floodplain; source-bordering dunes; stratigraphy
ANZSRC Field of Research 2020370904. Palaeoclimatology
370905. Quaternary environments
370999. Physical geography and environmental geoscience not elsewhere classified
Byline AffiliationsAustralian Centre for Sustainable Catchments
University of Wollongong
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