Habitat and feeding ecology of a Denisovan from Late Pleistocene Taiwan
Abstract
Denisovans, originally identified from ancient genome from Denisova Cave in Altai, were a sister group to the Neanderthals and were once widely distributed across diverse terrains in the north and south of eastern Asia1–5. Genomic studies suggest that there were multiple events of interbreeding between modern humans (Homo sapiens) and Denisovans somewhere in Asia6. However, little is known about Denisovan living environments, diet, ecological niche, the timing of their disappearance, and the possible coexistence with modern humans in different regions. Here we report the radiocarbon age and stable isotopic signature of Penghu 3, a large Denisovan tibia from Penghu Channel, Taiwan7. The results showed that Penghu 3 dates to approximately 45,000 years ago, the time when modern humans were already widespread in southern parts of Asia. This Denisovan individual inhabited a C4-dominated ecosystem, open environments such as savannahs and floodplains, or a mixture of both, and consumed a high proportion of animal protein similar to some European Neanderthals8–10, with no clear evidence for the use of aquatic resources. These findings have implications for the behavioral flexibility, large body size7, and eventual disappearance of the Denisovans.