The timing and cause of megafauna mass deaths at Lancefield Swamp, south-eastern Australia

dc.contributor.authorDortch, Joe
dc.contributor.authorCupper, Matt
dc.contributor.authorGrün, Rainer
dc.contributor.authorHarpley, Bernice
dc.contributor.authorLee, Kerrie
dc.contributor.authorField, Judith
dc.date.accessioned2016-08-25T05:50:58Z
dc.date.available2016-08-25T05:50:58Z
dc.date.issued2016
dc.description.abstractLancefield Swamp, south-eastern Australia, was one of the earliest sites to provoke interest in Pleistocene faunal extinctions in Sahul (Pleistocene Australia-New Guinea). The systematic investigation of the deposit in the early 1970s identified megafaunal remains dominated by the 100–200 kg kangaroo Macropus giganteus titan. Associated radiocarbon ages indicated that the species was extant until c.30,000 BP, suggesting significant overlap with human settlement of Sahul. This evidence was inconsistent with contemporary models of rapid human-driven extinctions. Instead, researchers inferred ecological tethering of fauna at Lancefield Swamp due to intense drought precipitated localised mass deaths, consistent with Late Pleistocene climatic variability. Later investigations in another part of the swamp, the Mayne Site, remote to the initial investigations, concluded that mass flow disturbed this area, and Electron Spin Resonance (ESR) analyses on megafauna teeth returned wide-ranging ages. To clarify site formation processes and dating of Lancefield Swamp, we excavated new test-pits next to previous trenches in the Classic and Mayne Sites. We compared absolute chronologies for sediments and teeth, sedimentology, palaeo-topography, taphonomy, and macropod age at death across the swamp. Luminescence dating of sediments and ESR analysis of teeth returned ages between c.80,000 and 45,000 years ago. We found no archaeological remains in the bone beds, and evidence of carnivore activity and fluvial action, in the form of reactivated spring flow. The latter disturbed limited parts of the site and substantial areas of the bone beds remained intact. The faunal assemblage is dominated by megafaunal adult Macropus, consistent with mass die-offs due to severe drought. Such droughts appear to have recurred over millennia during the climatic variability of Marine Isotope Stages 4 and 3. These events began tens of millennia before the first appearance of Aboriginal people in Sahul and only the very youngest fossil deposits could be coeval with the earliest human arrivals. Therefore, anthropogenic causes cannot be implicated in most if not all of mass deaths at the site. Climatic and environmental changes were the main factors in site formation and megafauna deaths at Lancefield Swamp.en_AU
dc.description.sponsorshipWe thank members of the Wurundjeri Tribe Land and Heritage Council for the endorsement of our research, which was funded by the Australian Research Council (ARC DP0342843), a University of Sydney Sesquicentenary R&D Grant held by JD, and a Carlyle Greenwell Bequest to BN. We are grateful for the support of the Lancefield Park Management Committee, Office of Aboriginal Affairs Victoria, Department of Environment, Land, Water and Planning (Vic.) and Shire of Macedon Ranges.en_AU
dc.identifier.issn0277-3791en_AU
dc.identifier.urihttp://hdl.handle.net/1885/107306
dc.publisherElsevieren_AU
dc.relationhttp://purl.org/au-research/grants/arc/DP0342843en_AU
dc.rights© 2016 Elsevier Ltd.en_AU
dc.sourceQuaternary Science Reviewsen_AU
dc.subjectMegafaunaen_AU
dc.subjectMacropodsen_AU
dc.subjectExtinctionsen_AU
dc.subjectPleistoceneen_AU
dc.subjectOSLen_AU
dc.subjectESRen_AU
dc.subjectTaphonomyen_AU
dc.subjectLancefield Swampen_AU
dc.titleThe timing and cause of megafauna mass deaths at Lancefield Swamp, south-eastern Australiaen_AU
dc.typeJournal articleen_AU
local.bibliographicCitation.lastpage182en_AU
local.bibliographicCitation.startpage161en_AU
local.contributor.affiliationGrün, R., Earth Environment, Research School of Earth Sciences, The Australian National Universityen_AU
local.contributor.authoruidu9201753en_AU
local.identifier.citationvolume145en_AU
local.identifier.doi10.1016/j.quascirev.2016.05.042en_AU
local.publisher.urlhttp://www.elsevier.com/en_AU
local.type.statusPublished Versionen_AU

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