4.2 Article

A detailed post-IR IRSL dating study of the Niuyangzigou loess site in northeastern China

Journal

BOREAS
Volume 45, Issue 4, Pages 644-657

Publisher

WILEY-BLACKWELL
DOI: 10.1111/bor.12185

Keywords

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Funding

  1. National Natural Science Foundation of China [41371203, 41472138]
  2. China National Science and Technology Basic Work Program [2012FY111700]
  3. Danish Independent Research Council [11-104566]

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In this study, we report standard quartz SAR OSL and post-IR infrared (IR) stimulated luminescence (post-IR IRSL; pIRIR(290)) measurements made on sand-sized quartz and K-feldspar extracts from the loess-palaeosol sequence at Niuyangzigou in northeastern China. The quartz OSL characteristics are satisfactory. Extensive pIRIR(50,290) dose recovery tests were performed by adding doses on top of the natural dose. We found that dose recovery ratios improve significantly when the test dose ranges between similar to 15 and similar to 80% of the total dose, and good dose recovery (within +/- 5% of unity) can be obtained up to approximate to 800Gy. Otherwise, the dose recovery ratio deviates from unity. The D-e values also depend on the test dose size and so we conclude that the effect of test dose size should be routinely considered in pIRIR dating. First IR stimulation plateau pIRIR(290) results are compared with multiple elevated temperature -pIRIR (MET-pIRIR) data. It appears that the low temperature MET-pIRIR data are strongly affected by poor dose recovery, but this is not the case for the pIRIR(290) results. Natural signal measurements at the highest (first IR) stimulation temperature on a sample expected to be in field saturation suggest that similar to 10% signal loss occurs in pIRIR signals. Long-term laboratory bleaching experiments (>80days) show that a constant (or very difficult to bleach) residual pIRIR(290) signal is reached after similar to 300h, corresponding to a dose of 6.2 +/- 0.7Gy. Quartz OSL and feldspar pIRIR(50,290) ages are in good agreement at least back to c.70ka. Beyond this the quartz ages begin to underestimate but the feldspar ages are in agreement with the expected Last Interglacial age palaeosol.

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