William Paterson University Researcher and his International Team Link Previously Unknown Megadrought More Than 4,000 Years Ago to Major Changes in Human Settlement


Professor Griffiths collects samples from inside caves in Laos

Physical evidence found in caves in Laos shows a connection between the end of the Green Sahara – when once heavily vegetated Northern Africa became a desert landscape – and a previously unknown megadrought that crippled Southeast Asia 4,000 to 5,000 years ago. 

In a paper published in Nature Communications, an international team of researchers led by William Paterson University Professor of Environmental Science and isotope geochemist Michael Griffiths explain how this major climate transformation led to a shift in human settlement patterns in Southeast Asia, which is now inhabited by more than 600 million people.

“What is so critical in what we do in reconstructing the past is highlighting what is possible,” Griffiths says of his work. “No doubt the large climate changes of the past are not a perfect analogue for the observed changes in Earth’s climate today or in the future. However, I think we can say with a high degree of confidence that populated regions like mainland Southeast Asia have the potential to undergo rapid shifts in both the abundance and timing of monsoon precipitation, underscoring the need for reliable climate projections.”

Griffiths and other researchers, including colleagues of more than 10 years—University of California, Irvine’s Kathleen Johnson and University of Pennsylvania’s Joyce White— gathered stalagmite samples from caves in Northern Laos. Then, geochemical properties of the oxygen and carbon isotopes, carbon-14, and trace metals found in the specimens were measured. This helped researchers verify the occurrence of the drought and extrapolate its impacts on the region.

They combined data from the analysis of the stalagmites with a series of climate model simulations, in which Saharan vegetation and dust concentrations were altered, allowing them to investigate the ocean-atmosphere feedbacks associated with such an abrupt shift in precipitation.

The modeling experiments suggested that reduced plant growth in the Sahara led to increased airborne dust that acted to cool the Indian Ocean, among other effects, leading to a large reduction in monsoon moisture across Southeast Asia that lasted more than 1,000 years.

Anthropologists and archaeologists have previously studied the effects of the demise of the Green Sahara on population centers closer to Western Asia and North Africa. But the link to the origin of the Southeast Asia megadrought and lifestyle pattern shifts in that region had not been previously investigated, Griffiths explains.

“Archaeologists and anthropologists have been studying this event for decades now, in terms of societal adaptations and upheavals, but its exact cause has eluded the scientific community,” Griffiths says.

His work suggest that the centuries-long megadrought corresponds to what is called “the missing millennia” in Southeast Asia—between 4,000 and 6,000 years ago—a time characterized by a noticeable lack of archaeological evidence for the region.

Griffiths’ project, which also involved researchers from Oxford University and Northumbria University in the United Kingdom, Los Alamos National Laboratory, and the University of New Mexico, was funded in part by a grant awarded to Griffiths from the National Science Foundation. 

“This study and data from Laos sets a new agenda and trajectory of research that is needed to understand human-environment relationships over the long term,” Griffiths says. “Climate change is not just an issue for today, it was a fact in the deep past, and perhaps studying the past can help illuminate our current situation in new ways.”

08/24/20