Optical dating of charcoal kiln remains from WWII: A test of accuracy

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL Quaternary Geochronology Pub Date : 2024-06-28 DOI:10.1016/j.quageo.2024.101582
Nasrin Karimi Moayed , Dimitri Vandenberghe , Koen Deforce , Eva Kaptijn , Karsten Lambers , Wouter Verschoof-van der Vaart , Wim De Clercq , Johan De Grave
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Abstract

The majority of relic charcoal kilns in Europe are more recent than 1650 CE and cannot be precisely dated using radiocarbon dating (14C). Quartz-based optically stimulated luminescence (OSL) dating of the sediments associated with the kiln remains has been suggested as a viable alternative. Owing to the lack of reliable and sufficiently precise independent age information, however, it remains to be established whether OSL dating can yield accurate ages for post-1650 CE features. This is explicitly investigated in this study by applying a commonly adopted quartz OSL methodology to three relic charcoal kilns which are known to have been constructed and operated between December 1941 and March/April 1942 CE.

We first document the quartz luminescence characteristics and show through procedural tests that the adopted single-aliquot regenerative dose procedure should be appropriate for equivalent dose determination. Four samples collected from the uppermost part of the charcoal-rich layers in the three features yield the youngest optical ages and are considered coeval. Their average age is 1928 ± 13 CE (95% probability), which matches the independent age reasonably well. The precision associated with the individual OSL ages ranges between 7 and 14% (1 sigma total uncertainty) and it might ideally be possible to establish relative chronologies with a higher time resolution. Finally, we briefly discuss our entire set of OSL ages in relation to future strategies for sampling charcoal kilns remains. In general, we conclude that OSL dating can be particularly advantageous to help resolving chronometric issues that pertain to post-1650 CE relic charcoal kilns.

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二战时期炭窑遗迹的光学年代测定:准确性测试
欧洲的大多数遗迹木炭窑的年代都在公元 1650 年之前,无法使用放射性碳年代测定法(14C)精确确定其年代。有人建议对与窑炉遗迹相关的沉积物进行石英基光激发发光(OSL)测年,作为一种可行的替代方法。然而,由于缺乏可靠和足够精确的独立年代信息,OSL 测定法是否能够为公元 1650 年后的地貌提供准确的年代仍有待确定。我们首先记录了石英发光特征,并通过程序测试表明,所采用的单等量再生剂量程序应适用于等效剂量测定。从三个地貌中富含木炭层的最上部采集的四个样本得出了最年轻的光学年龄,被认为是共生的。它们的平均年龄为 1928 ± 13 CE(95%概率),与独立年龄相当吻合。单个 OSL 年龄的精确度在 7% 到 14% 之间(总不确定性为 1 sigma),理想情况下可以建立时间分辨率更高的相对年代学。最后,我们简要讨论了与未来炭窑遗迹取样策略有关的整套 OSL 年龄。总之,我们得出的结论是,OSL 测定在帮助解决公元 1650 年后遗留炭窑的年代测定问题方面具有特别的优势。
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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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