| 古气候与环境变化 |
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| AMS-14C Dating of the Holocene Loess Sequence at Lantian, Shaanxi and Reflected Environmental Change |
| ZHANG Ting1,2,3, ZHU Yi-zhi1, YANG Ya-chang4, SHAO Jing4 |
| 1.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710075, China; 2.Xian Accelerator Mass Spectrometry Center, Xian 710061, China; 3.Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 4.Shaanxi Provincial Institute of Archaeology, Xian 710054, China |
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Abstract AMS-14C dating provides a new way in archaeology studies because of its high precision and speed and applicability in micro-sample dating. It is widely used in late Quaternary and Neolithic archaeological research. Based on AMS-14C dating of loess-paleosol sequence of the Xinjie profile at Lantian County of Shaanxi Province, the archaeological chronology of this sequence was obtained by using Bayesian method. Combining the stratigraphic sequence, magnetic susceptibility and pollen analysis, we got the conclusion that the weather was dry and cold during Malan loess period, and warm in Holocene, humid and warm in Yangshao period, dry and warm in Longshan period, dry and cold in recent Loess forming period.
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Received: 04 October 2010
Published: 20 May 2011
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2011, Vol. 31 
