Chinese Science Bulletin

, Volume 56, Issue 33, pp 3590–3595

Enamel carbon isotope evidence of diet and habitat of Gigantopithecus blacki and associated mammalian megafauna in the Early Pleistocene of South China

Authors

    • Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and PaleoanthropologyChinese Academy of Sciences
    • Laboratory of Human Evolution, Institute of Vertebrate Paleontology and PaleoanthropologyChinese Academy of Sciences
    • State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences
  • LiZhao Zhang
    • Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and PaleoanthropologyChinese Academy of Sciences
    • Laboratory of Human Evolution, Institute of Vertebrate Paleontology and PaleoanthropologyChinese Academy of Sciences
  • FuSong Zhang
    • State Key Laboratory of Lithospheric Evolution, Institute of Geology and GeophysicsChinese Academy of Sciences
  • XinZhi Wu
    • Laboratory of Human Evolution, Institute of Vertebrate Paleontology and PaleoanthropologyChinese Academy of Sciences
Open AccessArticle Geology

DOI: 10.1007/s11434-011-4732-4

Cite this article as:
Zhao, L., Zhang, L., Zhang, F. et al. Chin. Sci. Bull. (2011) 56: 3590. doi:10.1007/s11434-011-4732-4

Abstract

Enamel stable carbon isotope analyses were conducted on the large fossil ape Gigantopithecus blacki and an associated mammalian megafauna from Longgudong Cave in Jianshi and Juyuandong Cave in Liucheng, South China. The range in δ13C values (−18.8‰ to −14.1‰) indicates that G. blacki and other large mammals fed on solely C3 biomass, and lived in forest habitats, and not open country or savannas. These results are consistent with other faunal and floral analyses for that time. The diet and habitat of G. blacki were significantly different from those of early hominins (Australopithecus and Paranthropus) from South and East Africa. Extinction of G. blacki probably was a result of forest habitat fragmentation and deterioration.

Keywords

Gigantopithecus blackidietenamel stable carbon isotopeshabitat
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© The Author(s) 2011

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