In a study published in PNAS, researchers have shown that orbitally induced strengthening of the Asian summer monsoon played a key role in the dispersal of Homo sapiens from Africa to East Asia during the last interglacial period 125,000 to 70,000 years ago.

Led by Professor Ao Hong from the Institute of Earth Environment of the Chinese Academy of Sciences (CAS), the researchers integrated a comprehensive compilation of paleoanthropological site data with new high-resolution reconstructions of the Asian summer monsoon based on Chinese loess data, continuous modeling of the East Asian hydroclimate, and a novel human habitat simulation — all covering the past 280,000 years.

How human ancestors responded to past climate change remains a key question in research on human evolution. Climate variability was a key driver of human evolution and dispersal within Africa during the Pleistocene. However, our understanding of the orbital hydroclimatic influence on the early dispersal of our species, Homo sapiens, from Africa to East Asia, is hampered by the lack of integrated paleoclimatic and paleoanthropological studies from Asia.

Field photograph of the Huanxian loess-paleosol sequence on the central Chinese Loess Plateau [IMAGE: AO HONG]

To reconstruct orbitally resolved Asian summer monsoon variability over the past 280,000 years, the researchers collected 2,066 samples in the field from the rapidly accumulating Huanxian loess-paleosol section on the central Chinese Loess Plateau for measurements in the laboratory.

The resulting unprecedented centennial-resolution reconstructions suggest that the orbital-scale variability of the Asian summer monsoon responds to the combined action of changes in insolation (a so-called external forcing, i.e., one coming from outside Earth), and ice volume and greenhouse gas concentration (examples of what we call internal forcings, i.e., those coming from the Earth system), rather than to their individual actions. This argument is strongly supported by the Ao team’s model-based reconstructions of the East Asian hydroclimate over the past 280,000 years.

“When we integrated proxy- and model-based spatiotemporal paleoclimatic reconstructions with paleoanthropological data compilations from Asia across time and space, we found, to our surprise, that H. sapiens dispersed to East Asia at the same time as the Asian summer monsoon was intensified. This suggests an important influence of the paleo-monsoon on the early dispersal of H. sapiens from Africa to East Asia,” said Professor Ao, lead author of the study.

Homo sapiens dispersed from deteriorating environments in Southeast Africa to more optimal environments in Asia [IMAGE: AO HONG]

“In contrast to the strengthening of the Asian summer monsoon, the climate in much of southeast Africa worsened during the last interglacial. It is possible that these Asian and Southeast African hydroclimate changes acting together spurred the early dispersal of H. sapiens from Africa to East Asia,” said Dr. Thibaut Caley, an author of the study and a paleoclimatologist from the Université de Bordeaux, France. In contrast, the lush vegetation in East Asia at the time would have attracted H. sapiens habitation.

To provide further quantitative evidence of climate effects on H. sapiens dispersal, Dr. Ruan Jiaoyang, corresponding author of the study and assistant researcher at the IBS Center for Climate Physics, South Korea, performed computer simulations of H. sapiens habitats and found that the H. sapiens occupation of East Asia was consistent with a transcontinental increase in simulated habitat suitability.

This study was funded by the Strategic Priority Research Program of CAS, the Second Tibetan Plateau Scientific Expedition and Research Program, and the National Natural Science Foundation of China.

Source: Institute of Earth Environment,

Chinese Academy of Sciences