Combined different luminescence dating approaches on fluvial gravel deposits from the southern upper Rhine graben

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL Quaternary Geochronology Pub Date : 2024-05-10 DOI:10.1016/j.quageo.2024.101536
Madhurima Marik, Elena Serra, Lukas Gegg, Dominic Wölki, Frank Preusser
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Abstract

In recent years, luminescence dating has witnessed significant advancements to overcome its traditional boundaries. However, methodological challenges persist when dating high-energy fluvial gravel deposits in proglacial settings, because partial bleaching and the scarcity of sand lenses complicate luminescence age estimation through conventional approaches. To address these issues, using rock surfaces of large clasts may overcome the limited availability of sand layers in some deposits and allow clast specific assessment of luminescence signal resetting at the time of deposition through the analyses of bleaching profiles. The Hartheim gravel pit in the southern Upper Rhine Graben of southwest Germany features a sedimentary succession deposited by distal braided river meltwater streams reworked during the late Pleistocene. Different luminescence approaches have been applied to sand lenses, the sandy matrix of gravel deposits and crystalline cobbles. Quartz optically stimulated luminescence (OSL) ages range between ∼19 and 22 ka, which represents the time just after the last glaciation maximum in the region. The OSL ages of the sandy matrix of ∼24–27 ka are in an agreement with the previous estimates, as these are from a stratigraphic lower position. However, post-IR infrared stimulated luminescence (pIRIR) ages of sand layer and sandy matrix both are some 3–6 ka older than the OSL ages, despite being internally very consistent. Luminescence depth profiles show that the signal was deeply reset in some cobbles, whereas in others only the IRSL signal in the surface layer appears to have been reset. The cobble IRSL ages show a relatively large spread, and it remains uncertain, if this is caused by incomplete bleaching or it reflects dosimetric issues. Nevertheless, overall, our results underscore the potential of rock surface luminescence dating to date fluvial deposits from the Upper Rhine Graben and similar settings.

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莱茵河上游地堑南部河道砾石沉积物的不同发光测年方法组合
近年来,发光测年技术取得了重大进展,突破了其传统界限。然而,在对冰期环境中的高能量河流砾石沉积进行年代测定时,方法学上仍然存在挑战,因为部分漂白和砂透镜的稀缺使传统方法的发光年龄估算变得复杂。为了解决这些问题,使用大块岩石表面可以克服某些沉积中砂层有限的问题,并通过分析漂白剖面对沉积时的发光信号重置进行特定的评估。德国西南部上莱茵海盆区南部的哈特海姆砾石坑具有晚更新世期间由远端辫状河融水溪流再加工沉积的沉积演替。对砂粒透镜体、砾石沉积的砂质基质和结晶鹅卵石采用了不同的发光方法。石英光学激发发光(OSL)年龄介于 19 至 22 ka 之间,代表了该地区最后一次冰川作用最大化之后的时间。砂质基质的 OSL 年龄为 ∼24-27 ka,与之前的估计一致,因为这些年龄来自地层较低的位置。然而,砂层和砂质基质的后红外激发发光(pIRIR)年龄都比 OSL 年龄早约 3-6 ka,尽管内部非常一致。发光深度剖面图显示,一些鹅卵石的信号被深度重置,而另一些鹅卵石只有表层的 IRSL 信号被重置。鹅卵石的 IRSL 年龄显示出相对较大的差异,目前还不能确定这是由于漂白不完全造成的,还是反映了剂量测定问题。尽管如此,总的来说,我们的研究结果凸显了岩石表面发光测年法在确定莱茵河上游海湾及类似地区的河流沉积物年代方面的潜力。
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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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