Author
Listed:
- Yingqi Zhang
(Chinese Academy of Sciences
Macquarie University)
- Kira E. Westaway
(Chinese Academy of Sciences
Macquarie University)
- Simon Haberle
(Australian National University)
- Juliën K. Lubeek
(Macquarie University)
- Marian Bailey
(Southern Cross University)
- Russell Ciochon
(University of Iowa)
- Mike W. Morley
(Flinders University)
- Patrick Roberts
(Max Planck Institute for Geoanthropology
Max Planck Institute for Geoanthropology
University of Queensland)
- Jian-xin Zhao
(University of Queensland)
- Mathieu Duval
(National Research Centre on Human Evolution CENIEH
Griffith University)
- Anthony Dosseto
(University of Wollongong)
- Yue Pan
(Chinese Academy of Sciences)
- Sue Rule
(Australian National University)
- Wei Liao
(Shandong University)
- Grant A. Gully
(Flinders University)
- Mary Lucas
(Max Planck Institute for Geoanthropology)
- Jinyou Mo
(Natural History Museum of Guangxi)
- Liyun Yang
(Chongzuo Zhuang Ethnological Musuem)
- Yanjun Cai
(Xi’an Jiaotong University)
- Wei Wang
(Shandong University)
- Renaud Joannes-Boyau
(Chinese Academy of Sciences
Southern Cross University
University of Johannesburg)
Abstract
The largest ever primate and one of the largest of the southeast Asian megafauna, Gigantopithecus blacki1, persisted in China from about 2.0 million years until the late middle Pleistocene when it became extinct2–4. Its demise is enigmatic considering that it was one of the few Asian great apes to go extinct in the last 2.6 million years, whereas others, including orangutan, survived until the present5. The cause of the disappearance of G. blacki remains unresolved but could shed light on primate resilience and the fate of megafauna in this region6. Here we applied three multidisciplinary analyses—timing, past environments and behaviour—to 22 caves in southern China. We used 157 radiometric ages from six dating techniques to establish a timeline for the demise of G. blacki. We show that from 2.3 million years ago the environment was a mosaic of forests and grasses, providing ideal conditions for thriving G. blacki populations. However, just before and during the extinction window between 295,000 and 215,000 years ago there was enhanced environmental variability from increased seasonality, which caused changes in plant communities and an increase in open forest environments. Although its close relative Pongo weidenreichi managed to adapt its dietary preferences and behaviour to this variability, G. blacki showed signs of chronic stress and dwindling populations. Ultimately its struggle to adapt led to the extinction of the greatest primate to ever inhabit the Earth.
Suggested Citation
Yingqi Zhang & Kira E. Westaway & Simon Haberle & Juliën K. Lubeek & Marian Bailey & Russell Ciochon & Mike W. Morley & Patrick Roberts & Jian-xin Zhao & Mathieu Duval & Anthony Dosseto & Yue Pan & Su, 2024.
"The demise of the giant ape Gigantopithecus blacki,"
Nature, Nature, vol. 625(7995), pages 535-539, January.
Handle:
RePEc:nat:nature:v:625:y:2024:i:7995:d:10.1038_s41586-023-06900-0
DOI: 10.1038/s41586-023-06900-0
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