Testing the accuracy of single-grain OSL dating on Eemian quartz samples

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL Quaternary Geochronology Pub Date : 2024-07-19 DOI:10.1016/j.quageo.2024.101602
Frederik H. Baumgarten , Kristina J. Thomsen , Guillaume Guérin , Jan-Pieter Buylaert , Andrew S. Murray
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Abstract

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 (∼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 Dc 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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测试对伊玛纪石英样品进行单颗粒 OSL 测定的准确性
对石英进行单颗粒 OSL 测定是一种常用的 OSL 测定方法,即使在不完全漂白可能并不显著的情况下也是如此。然而,对单粒定年法准确性的测试很少发表,尤其是对年代超过 50 ka 的样本。在本研究中,我们研究了单颗粒石英 OSL 测年的准确性,因为在这种情况下,由于饱和效应,相当数量的单个颗粒不再能够准确测量埋藏剂量。我们比较了标准多晶粒 OSL 测定结果与单晶粒 OSL 测定结果,这些结果是对五个 OIS 第 5e(Eemian)亚阶段(128 ka ∼)样本的测量结果。我们的研究表明,对于这些样品,标准的多晶粒石英剂量估算结果与预测剂量估算结果吻合良好(五个样品中有四个样品恢复了年龄控制),但标准的频数主义单晶粒测年程序明显低估了年龄控制,即测量剂量与预测剂量的比值范围在 0.42 ± 0.03 和 0.84 ± 0.06 之间,低估程度随着饱和晶粒相对数量的增加而增加。通过使用 Dc 标准,试图消除大量饱和晶粒导致的剂量估计中不可避免的偏差(即测量剂量与预测剂量之比介于 0.63 ± 0.05 和 0.94 ± 0.08 之间),降低了低估率,但只有吸收剂量最小的样本与年龄对照相符。使用贝叶斯分析法("BayLum"),测量剂量与预测剂量之比介于 0.75 ± 0.07 和 1.14 ± 0.08 之间,但五个样本中只有两个与独立的年龄对照一致。我们的研究结果对评估 100-200 Gy 自然剂量范围内的石英单颗粒 OSL 年代测定具有重要意义。
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来源期刊
Quaternary Geochronology
Quaternary Geochronology 地学-地球化学与地球物理
CiteScore
4.40
自引率
22.20%
发文量
130
审稿时长
20 weeks
期刊介绍: Quaternary Geochronology is an international journal devoted to the publication of the highest-quality, peer-reviewed articles on all aspects of dating methods applicable to the Quaternary Period - the last 2.6 million years of Earth history. Reliable ages are fundamental to place changes in climates, landscapes, flora and fauna - including the evolution and ecological impact of humans - in their correct temporal sequence, and to understand the tempo and mode of geological and biological processes.
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