Climate-human interaction associated with southeast Australian megafauna extinction patterns

被引:0
作者
Frédérik Saltré
Joël Chadoeuf
Katharina J. Peters
Matthew C. McDowell
Tobias Friedrich
Axel Timmermann
Sean Ulm
Corey J. A. Bradshaw
机构
[1] Flinders University,Global Ecology, College of Science and Engineering and ARC Centre of Excellence for Australian Biodiversity and Heritage
[2] UR 1052,Dynamics of Eco
[3] French National Institute for Agricultural Research (INRA),Evolutionary Pattern and ARC Centre of Excellence for Australian Biodiversity and Heritage
[4] University of Tasmania,Center for Climate Physics
[5] University of Hawai’i at Mānoa,ARC Centre of Excellence for Australian Biodiversity and Heritage, College of Arts, Society and Education
[6] Institute for Basic Science,undefined
[7] Pusan National University,undefined
[8] James Cook University,undefined
来源
Nature Communications | / 10卷
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摘要
The mechanisms leading to megafauna (>44 kg) extinctions in Late Pleistocene (126,000—12,000 years ago) Australia are highly contested because standard chronological analyses rely on scarce data of varying quality and ignore spatial complexity. Relevant archaeological and palaeontological records are most often also biased by differential preservation resulting in under-representated older events. Chronological analyses have attributed megafaunal extinctions to climate change, humans, or a combination of the two, but rarely consider spatial variation in extinction patterns, initial human appearance trajectories, and palaeoclimate change together. Here we develop a statistical approach to infer spatio-temporal trajectories of megafauna extirpations (local extinctions) and initial human appearance in south-eastern Australia. We identify a combined climate-human effect on regional extirpation patterns suggesting that small, mobile Aboriginal populations potentially needed access to drinkable water to survive arid ecosystems, but were simultaneously constrained by climate-dependent net landscape primary productivity. Thus, the co-drivers of megafauna extirpations were themselves constrained by the spatial distribution of climate-dependent water sources.
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