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Extinction of eastern Sahul megafauna coincides with sustained environmental deterioration
Scott A Hocknull1,2, Richard Lewis3, Lee J Arnold3
1Geosciences, Queensland Museum, 122 Gerler Rd., Hendra, QLD, 4011, Australia. scott.hocknull@qm.qld.gov.au.
Nature Communications
|May 19, 2020
Summary
Upper Pleistocene megafauna extinctions in Sahul were not human-driven. New fossil evidence suggests extinctions resulted from staggered hydroclimate deterioration and environmental change, not rapid human impact.
Area of Science:
- Paleontology
- Quaternary Science
- Environmental History
Background:
- The extinction of megafauna in Sahul (Australia and New Guinea) during the Upper Pleistocene is poorly understood.
- Existing hypotheses focus on climate or human-driven scenarios, despite limited data for much of the region.
Observation:
- New megafauna fossils from north-eastern Australia date to after 40,100 (±1700) years ago.
- Fossils indicate a sclerophyllous forest environment with diverse megaherbivores and carnivorous reptiles.
- Megafauna species diversity in this region exceeds that of southern sites of similar age.
Findings:
- The findings challenge rapid, continent-wide human-mediated extinction models and proposed extinction timing.
- Megafauna extinctions correlate with regionally varied, long-term hydroclimate decline and environmental shifts.
- Greater species diversity in the north contradicts extinction patterns linked to proposed human migration routes.
Implications:
- This study refutes synchronous human-driven extinction of Sahul's megafauna.
- Environmental factors, specifically hydroclimate changes, played a significant role in megafauna extinctions.
- The research highlights the need for more localized data to understand past extinction events.
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