CosmoChron: A versatile age-depth modeling approach using cosmogenic nuclides and direct age constraints

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL
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Abstract

We introduce a novel age-depth modeling approach called CosmoChron that integrates both cosmogenic nuclide concentrations and other age constraints, such as radiocarbon and OSL ages, from different depths in a sedimentary sequence. Based on probabilistic inverse modeling, CosmoChron constrains the age-depth relationship of a sedimentary sequence along with associated uncertainties. Knowledge about the sample origins and the accumulation process is incorporated in the prior model. The 26Al/10Be ratio is computed at different depths in the forward model by accounting for different pre-burial scenarios, radioactive decay and post-burial production of 26Al-10Be, which is directly tied to the age-depth relation itself. Synthetic test cases demonstrate the method's ability to construct accurate age-depth relationships given by the posterior distribution, even for complex scenarios that include slow and varying accumulation rates, complex pre-burial histories, hiatuses, and unconformities. Based on observed unconformities, users have the option to manually input hiatuses into the model at specific depths, which allows estimation of their durations. Application of CosmoChron to real 26Al/10Be data from the Laujunmiao section in China yields ages that are similar to those obtained with conventional burial dating methods for specific stratigraphic layers. However, the associated uncertainties are significantly reduced with CosmoChron (by ∼47 % on average) because it exploits the vertical coupling of data combined with knowledge of the relative age of the samples, which must become younger towards the top of the profile. Additionally, the age-depth model reflets the duration of three hiatuses inferred from unconformities observed in the field. When CosmoChron is applied to OSL-derived ages from Jingbian section A on the Chinese Loess Plateau, covering the last ∼140 ka, the method produces results that are almost identical to those obtained with the well-established Bacon age-depth modeling approach. CosmoChron consequently offers a new, versatile and reliable tool to construct age-depth models for Quaternary sediment sequences.

CosmoChron:利用宇宙成因核素和直接年龄约束的多功能年龄深度建模方法
我们介绍了一种名为 CosmoChron 的新型年龄-深度建模方法,该方法综合了沉积序列中不同深度的宇宙成因核素浓度和其他年龄约束,如放射性碳年龄和 OSL 年龄。CosmoChron 以概率反演模型为基础,对沉积序列的年龄-深度关系以及相关的不确定性进行约束。有关样品来源和堆积过程的知识被纳入先验模型。通过考虑不同的埋藏前情况、26Al-10Be 的放射性衰变和埋藏后生成,在前向模型中计算不同深度的 26Al/10Be 比率,这与年龄-深度关系本身直接相关。合成测试案例表明,该方法能够根据后验分布构建准确的年龄-深度关系,即使是在包括缓慢和变化的累积率、复杂的埋藏前历史、间断和不整合等复杂情况下也是如此。根据观测到的不整合现象,用户可以选择在特定深度手动将间断输入模型,从而估计其持续时间。将 CosmoChron 应用于中国刘军庙剖面的实际 26Al/10Be 数据,得到的年龄与特定地层的传统埋藏年代测定方法相似。然而,由于 CosmoChron 利用了数据的垂直耦合和样品相对年龄的知识,其相关的不确定性大大降低(平均降低 47%),而样品的相对年龄必须向剖面顶部变年轻。此外,年龄-深度模型还反推了根据实地观察到的不整合推断出的三个间断的持续时间。当将 CosmoChron 应用于中国黄土高原靖边 A 段的 OSL 年龄时,该方法得出的结果与培根年龄-深度模型方法得出的结果几乎相同。因此,CosmoChron 为构建第四纪沉积序列的年龄-深度模型提供了一种新的、多功能和可靠的工具。
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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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