4.4 Article

TT-OSL and post-IR IRSL dating of the Dali Man site in central China

Journal

QUATERNARY INTERNATIONAL
Volume 434, Issue -, Pages 99-106

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2015.05.027

Keywords

Dali Man; Aeolian deposits; Fluvial deposits; TT-OSL; Post-IR IRSL

Funding

  1. National Natural Science Foundation of China [41202127, 41472138, 41371203]
  2. Specialized Research Fund for the Doctoral Program of Higher Education [20130091130006]
  3. Fundamental Research Funds for the Central Universities
  4. Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD)

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Showing features associated with archaic Homo sapiens and evolved Homo erectus, the Dali skull is a key fossil for understanding human evolution in China. Various dating methods such as U-series, IRSL, ESR, ESR/U-series, and stratigraphical correlation with central Loess Plateau sequence were used to estimate the antiquity the Dali Man site with varying results. In this study, a total of 12 samples were taken in the sequence in the Dali Man site, from the aeolian loess-palaeosol sequence and underlying fluvial deposit layers including the palaeoanthropological level and dated by several optically stimulated luminescence (OSL) methods: coarse-grained quartz SAR OSL, thermally transferred OSL (TT-OSL), and K-feldspar post-IR infrared (IR) stimulated luminescence (post-IR IRSL; pIRIR(290)) methods. Results show that the TT-OSL and pIRIR(290) ages were consistent up to -100 ka. For older samples, the feldspar ages were significantly older. These pIRIR(290) ages increased with the stratigraphy up to 310 ka. The best age estimation of the Dali Man layer providing by the feldspar pIRIR(290) suggested that the Dali Man lived in late period of L3 (MIS 8) stage. Furthermore, correlating the pIRIR(290) ages between 267.7 +/- 13.9 ka and 258.3 +/- 14.2 ka and new pollen analysis, we proposed a new viewpoint that the Dali Man was likely to live during a transitional period from glacial to interglacial climate in the 52/L3 (MIS 7/8) stage. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.

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