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Testing the accuracy of single-grain OSL dating on Eemian quartz samples
被引:0
|作者:
Baumgarten, Frederik H.
[1
]
Thomsen, Kristina J.
[1
]
Guerin, Guillaume
[2
]
Buylaert, Jan-Pieter
[1
]
Murray, Andrew S.
[1
,3
]
机构:
[1] Tech Univ Denmark, Dept Phys, DTU Riso Campus, Roskilde, Denmark
[2] Univ Rennes, CNRS, Geosci Rennes, UMR 6118, F-35000 Rennes, France
[3] Aarhus Univ, Dept Geosci, Nord Lab Luminescence Dating, Aarhus, Denmark
关键词:
Luminescence;
Quartz;
OSL;
Single-grain;
Accuracy;
Multi-grain;
Independent age-control;
Dose models;
OPTICALLY STIMULATED LUMINESCENCE;
JINMIUM ROCK SHELTER;
NORTHERN AUSTRALIA;
SEDIMENT SAMPLES;
PALEOLITHIC SITE;
MULTIPLE GRAINS;
DOSE MODEL;
AGE;
MIDDLE;
AFRICA;
D O I:
10.1016/j.quageo.2024.101602
中图分类号:
P9 [自然地理学];
学科分类号:
0705 ;
070501 ;
摘要:
Single-grain OSL dating of quartz is a popular approach to OSL dating, even when incomplete bleaching is not likely to be significant. However, little testing of the accuracy of single-grain dating has been published; particularly for samples older than 50 ka. In this study, we investigate the accuracy of single-grain quartz OSL dating, when a significant number of individual grains are no longer able to accurately measure the burial dose because of saturation effects. We compare standard multi-grain OSL results with those obtained from single-grain OSL measurements for five OIS substage 5e (Eemian) samples (similar to 128 ka). We show that for these samples, standard multi-grain quartz dose estimation results in dose estimates in good agreement with the predicted doses (four of the five samples recover age control), but that standard frequentist single-grain dating procedures significantly underestimate the age controls, i.e. the measured to predicted dose range between 0.42 +/- 0.03 and 0.84 +/- 0.06, where the underestimation increases with increasing relative number of grains in saturation. Attempting to remove the inevitable bias in the dose estimation resulting from a significant number of saturated grains (by using the D-c criterion) reduced the underestimation, i.e. the measured to predicted dose ratio range between 0.63 +/- 0.05 and 0.94 +/- 0.08, but only the sample with the smallest absorbed dose is consistent with the age control. Using Bayesian analysis ("BayLum") the ratio of measured to predicted dose range between 0.75 +/- 0.07 and 1.14 +/- 0.08, but only two of the five samples agree with the independent age control. Our results have implications for the evaluation of single-grain OSL dating of quartz in the 100-200 Gy natural dose range.
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