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dc.contributor.authorHaberlah, Daviden_US
dc.contributor.authorA.J. Williams, Martinen_US
dc.contributor.authorHalverson, Galenen_US
dc.contributor.authorMcTainsh, Granten_US
dc.contributor.authorM. Hill, Stevenen_US
dc.contributor.authorHrstka, Tomasen_US
dc.contributor.authorJaime, Patricioen_US
dc.contributor.authorR. Butcher, Alanen_US
dc.contributor.authorGlasby, Peteren_US
dc.date.accessioned2017-05-03T14:51:57Z
dc.date.available2017-05-03T14:51:57Z
dc.date.issued2010en_US
dc.date.modified2011-03-29T06:53:28Z
dc.identifier.issn0277-3791en_US
dc.identifier.doi10.1016/j.quascirev.2010.04.014en_AU
dc.identifier.urihttp://hdl.handle.net/10072/37810
dc.description.abstractTerrace remnants of late Pleistocene fine-grained valley-fill deposits (Silts) deeply entrenched by ephemeral traction load streams in arid areas remain a puzzle. They have been attributed to a variety of origins ranging from lacustrine to alluvial floodplains. We here report a centimetre-scale multi-proxy study of a 7 m section of Silts in the semi-arid Flinders Ranges of South Australia, which span the lead-up to and peak of the Last Glacial Maximum (LGM). The results of detailed lithostratigraphic mapping, high-resolution parametric particle-size analysis, Automated Mineralogy, induced magnetic susceptibility, carbon stable isotope geochemistry, and a chronostratigraphy based on 27 AMS radiocarbon and 6 luminescence ages are discussed in terms of sediment provenance, depositional environment and weathering history with the aim of reconstructing the regional palaeo-environment. The data are consistent with a fluctuating aeolian-fluvial interplay dominating the extended LGM environment with a greater impact on the landscape than all combined geomorphic processes since then. Accordingly, weathered slope mantles and loess accessions were eroded and entrained by numerous small and at least a dozen large-scale flood events, and trapped in an intra-montane floodplain extending into Brachina Gorge. Upstream of this narrow constriction, recurrent backflooding is discussed resulting in a thick sequence of layered to laminated slackwater couplets. Aggradation and degradation of valley-fills appear to be largely controlled by fine-sediment supply from the valley slopes, replenished by wind-blown dust from upwind playa lakes and source-bordering dunefields. In conclusion, this study demonstrates how dust storms and flooding rains can account for 'pluvial' features previously explained by the opposing effects of reduced precipitation and evaporation in the colder more arid glacial landscape of southern Australia.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherElsevieren_US
dc.publisher.placeUnited Kingdomen_US
dc.relation.ispartofstudentpublicationNen_AU
dc.relation.ispartofpagefrom2673en_US
dc.relation.ispartofpageto2693en_US
dc.relation.ispartofissue19-20en_US
dc.relation.ispartofjournalQuaternary Science Reviewsen_US
dc.relation.ispartofvolume29en_US
dc.rights.retentionYen_AU
dc.subject.fieldofresearchGeology not elsewhere classifieden_US
dc.subject.fieldofresearchcode040399en_US
dc.titleLoess and floods: High-resolution multi-proxy data of Last Glacial Maximum (LGM) slackwater deposition in the Flinders Ranges, semi-arid South Australiaen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.date.issued2010
gro.hasfulltextNo Full Text


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