Discovery Early Career Researcher Award - Grant ID: DE200100890
Funder
Australian Research Council
Funding Amount
$427,082.00
Summary
Rapid climate change, early modern human dispersal, and Neanderthal demise. Why are we the only surviving human species? This project aims to investigate whether seasonal environmental changes associated with rapid climate change events played a role in the expansion of our own species and the demise of Neanderthals between 60,000-30,000 years ago. The project will generate quantitative, sub-seasonal records of past climate variability using novel multi-proxy analyses from key archaeological sit ....Rapid climate change, early modern human dispersal, and Neanderthal demise. Why are we the only surviving human species? This project aims to investigate whether seasonal environmental changes associated with rapid climate change events played a role in the expansion of our own species and the demise of Neanderthals between 60,000-30,000 years ago. The project will generate quantitative, sub-seasonal records of past climate variability using novel multi-proxy analyses from key archaeological sites, offering a framework for understanding early human responses to extreme climate fluctuations. This may inform our strategies for coping with future extreme scenarios. These unparalleled records will also provide data to test and refine climate models, enabling a better understanding of Earth’s climate system. Read moreRead less
Resolving the Maya climate-collapse hypothesis. This project aims to test the climate-collapse theory by developing detailed records of climate and social change from Maya cities that did not collapse, and in doing so identify why some cities were more resilient to the impact of climatic variability than others. Catastrophic climate variability is often invoked to explain the historic collapse of large low-density urban centres in the global tropics. The collapse of the Maya civilisation of Cent ....Resolving the Maya climate-collapse hypothesis. This project aims to test the climate-collapse theory by developing detailed records of climate and social change from Maya cities that did not collapse, and in doing so identify why some cities were more resilient to the impact of climatic variability than others. Catastrophic climate variability is often invoked to explain the historic collapse of large low-density urban centres in the global tropics. The collapse of the Maya civilisation of Central America after the 8th century AD is the archetypal social collapse yet, despite robust evidence for drought across Central America, archaeological evidence suggests a heterogenous social response. This project will reveal what social, material, or environmental properties facilitated resiliency in historic urban centres confronting climatic variability.Read moreRead less