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Kaifu, Y.

Publications and source records attributed to Kaifu, Y..

2 recordsLinked to original sources

Denisovan leg bones from Taiwan reveal large body size

Denisovans are an extinct archaic Homo group whose lineage diverged from the Neanderthal lineage approximately 550,000 years ago and were widely distributed across eastern Asia until [~]45,000 years ago1-7. Their morphological features are known directly from the existing cranio- dental and phalangeal remains1,2,8-12. However, the body size and postcranial morphology of the Denisovans remain largely unknown. We here report that hominin femoral and tibial fossils recovered from the Penghu Channel, Taiwan, are Denisovans in their proteomic profiles. Morphologically, these specimens are among the largest leg bones known in Pleistocene Homo. They exhibit generally archaic features, but also show some modern human-like morphology, including a strong femoral pilaster. Our findings demonstrate that the Denisovan population at the northern circle had larger body size than earlier Homo erectus as well as Late Pleistocene Homo sapiens in eastern Asia. This challenges the generally held expectation that Pleistocene Homo followed Bergmanns rule that anticipates latitudinal decline of body size, and suggests that the large Denisovan brain resulted from their large body size at least partly. The strong pilaster developed in the Penghu femur suggests some behavioral similarities between the Denisovans and the Upper Palaeolithic modern humans and/or gene flow from the latter to the former.

paleontology↗

Habitat and feeding ecology of a Denisovan from Late Pleistocene Taiwan

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.

paleontology↗