Mass spectrometric U-series dating of Laibin hominid site in Guangxi, southern China

Nanjing Normal University, Nan-ching, Jiangsu Sheng, China
Journal of Archaeological Science (Impact Factor: 2.14). 12/2007; 34(12):2109-2114. DOI: 10.1016/j.jas.2007.02.008

ABSTRACT The Laibin hominid represents one of the rare finds of modern Homo sapiens in China, rare for its relative completeness and well-established stratigaphic provenance. This paper presents the results of mass spectrometric U-series dating of intercalated calcite samples from the Laibin site. The capping flowstone and the calcite vein, which sandwich the hominid fossil-containing deposits, date to 38.5 ± 1.0 and 44.0 ± 0.8 ka, setting respectively the minimum and maximum ages to the fossils. The second flowstone layer is 112.0 ± 1.4 ka old, indicating that the cultural sequence may possibly extend to somewhere between 44 and 112 ka. Securely dated Laibin finds should be of importance in reconstructing human physical and cultural evolution in the region.

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Available from: Hai Cheng, Aug 22, 2015
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    • "). Problematic Liujiang aside, the fragmentary Laibing specimen, also from Guangxi Province, is dated to between 38,000 and 44,000 BP (Shen et al., 2007). Moving south, a range of other late Pleistocene specimens from Niah Cave in Malaysia (Brothwell, 1960; Kennedy, 1977; Barker et al., 2007), Tabon Cave in the Philippines (Macintosh, 1978; Dizon et al., 2002; D etroit et al., 2004), and Wajak in Indonesia (Dubois, 1922; Storm, 1995; Storm et al., 2013) have secure dates ranging from 40,000 to 16,000 BP. "
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    • "Late Pleistocene (or probably Late Pleistocene) crania: Chilinshan 1 (PA 60), Liujiang 1 (PA 89), Minatogawa 4, Niah Cave 1, ZKD-Upper Cave 101 (AN 71), and Ziyang 1 (PA 58) (Wu, 1958, 1961; Chia and Wu, 1959; Woo, 1959; Brothwell, 1960; Suzuki, 1982; Shen et al., 2007 "
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    • "La deuxième couche de plancher stalagmitique est datée de 112,0 AE 1,4 ka, donnant un a ˆge maximum aux dépôts situés au-dessus. Les coquilles d'eau douce comprises dans les dépôts de ce site peuvent e ˆtre citées comme un témoignage soutenant la présence humaine dans le sud de la Chine entre 39 et 112 ka (Shen et al., 2007). "
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