4.2 Article

Luminescence dating of the Huliu River terraces in the Nihewan Basin, North China

Journal

QUATERNARY GEOCHRONOLOGY
Volume 71, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.quageo.2022.101316

Keywords

Huliu river terraces; Nihewan basin; pIRIR; Single grain measurement; SGC

Funding

  1. Australian Research Council Future Fellowship [FT140100384]
  2. National Natural Science Foundation of China [42071003]
  3. China Scholarship Council
  4. University of Wollongong [201506010345]

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In the Yuxian sub-basin of the Nihewan Basin in North China, the discovery of over 27 new archaeological sites lacking age control has prompted investigation into the fluvial terrace sequence of the Huliu River. Dating using pIRIR on potassium feldspar revealed formation ages for three Huliu River terraces, providing insights into human occupation in the region.
As one of the most important regions for early human occupation in East Asia, Nihewan Basin in North China is well-known for an abundance of archaeological sites with ages spanning the last 2 Ma. In recent 10 years, more than 27 new archaeological localities have been discovered from the Yuxian (sub-basin of Nihewan), and all of them are with no age control. The lack of reliable ages for these localities affects our understanding for the evolution of the stone-tool technology in the Nihewan Basin. As many localities were founded in the river terrace, the fluvial terrace sequence of the Huliu River (main river of the Yuxian) was investigated. Based on single-grain post-infrared infrared stimulated luminescence (pIRIR) procedure on potassium (K-) feldspar, our results reveal that the formation ages of three Huliu River terraces are 139.6-115.7, 19.7-5.5, and <0.9 ka, respectively. On the basis of these pIRIR ages, the formation of the fluvial terrace sequence may provide informative constraints on the human occupation in the Huliu River terrace in the Nihewan Basin, if a clear stratigraphic correlation is established between the archaeological sites and the dated terrace deposits.

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