RESEARCH PAPER
ESR dating of the Donggutuo Palaeolithic site in the Nihewan Basin, northern China
1
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, 100029, China
2
Key laboratory of Geography Information Science Ministry of Education, East China Normal University, Shanghai, 200062, China
3
Département de Préhistoire, Muséum National d’Histoire Naturelle, UMR7194 du CNRS, 1 rue René Panhard, 75013, Paris, France
4
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Online publication date: 2013-09-27
Publication date: 2013-12-01
Geochronometria 2013;40(4):348-354
KEYWORDS
ABSTRACT
The fluvio-lacustrine sequences in the Nihewan Basin, northern China, provide important terrestrial archives about Palaeolithic settlements and, therefore, about early human occupation in high northern latitude in East Asia. Here we present detailed ESR dating of the Donggutuo Palaeolithic site, located in this basin. Four levels A, B, C and E of the Donggutuo archaeological layer yield ESR ages ranging from 1060±129 ka to 1171±132 ka with a mean of 1119±132 ka. The ages are consistent with the paleomagnetic data, which show that the Donggutuo Palaeolithic site lies just below the onset of the Jaramillo normal subchron (0.99–1.07 Ma). Furthermore, our results indicate that the reliable ESR dating range of bleached quartz using Ti-Li centre can be effectively extended to 1100 ka and the Ti-Li centre was zeroed before the last deposition, which requires improvement of the understanding of the bleaching mechanism conditions.
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