泰晤士河阶地序列中更新世哺乳动物珐琅质的氨基酸年代测定:多类群方法

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL
M.R. Dickinson , K. Scott , N.F. Adams , A.M. Lister , K.E.H. Penkman
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引用次数: 0

摘要

氨基酸地质年代学可以为更新世提供有效的相对年代框架,并使陆地沉积与海洋氧同位素记录所描述的全球气候波动相关联。利用为分析牙釉质中结晶内氨基酸而开发的方法,我们的目标是利用不同的哺乳动物分类群:大象、马和野牛,为英国南部泰晤士河谷的阶地沉积构建基于牙釉质的氨基酸地质年代。为此,我们对泰晤士河谷上游 10 个地层、泰晤士河谷下游 3 个地层和莱亚河谷泰晤士河支流 1 个地层中的 58 枚象牙、21 枚马牙和 15 枚野牛牙进行了手性氨基酸分析。我们评估了不同类群之间氨基酸分解率的差异,并确定了哪些物种足够相似,可以用于相对年代测定的比较。河流阶地沉积物的相对年代测定与阶地地层学、生物地层学以及其他对所有三个分类群年龄的独立估计都非常吻合。这些框架证明了基于珐琅质的氨基酸地质年代学在英国中晚更新世沉积物相对年代测定方面的潜力,并建立了一个氨基地层学框架,在此基础上可以完善其他牙齿材料的年代测定。珐琅质为评估没有贝壳材料或贝壳材料保存较差的遗址的年代提供了机会。最重要的是,它还可以为哺乳动物化石提供直接的相对年代测定,而哺乳动物化石往往是研究其进化、分布变化或灭绝的重点。直接测年法避免了哺乳动物化石本身可能被重新加工或与贝壳、沉积物或同一矿床中其他测年材料的年代不同的风险;它还可以对来源不可靠的存档样本(如 17-19 世纪早期的采集样本)进行直接测年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Amino acid dating of pleistocene mammalian enamel from the river thames terrace sequence: A multi-taxon approach

Amino acid geochronology can provide effective relative dating frameworks for the Pleistocene and has enabled correlation of terrestrial deposits to the global climatic fluctuations described by the marine oxygen isotope record. Using methods developed for the analysis of intra-crystalline amino acids in tooth enamel, we aimed to construct an enamel-based amino acid geochronology for the terrace deposits in the valley of the River Thames in southern Britain using different mammalian taxonomic groups: elephant, horse and bison. To achieve this, chiral amino acid analysis was applied to 58 elephantid, 21 horse and 15 bison teeth from 10 horizons in the Upper Thames Valley, three in the Lower Thames Valley and one from a Thames tributary in the Lea Valley. We evaluate differences in the rates of amino acid breakdown between the taxa and establish which species are similar enough to enable comparison for relative dating purposes. The relative dating of the river terrace deposits is in good agreement with the terrace stratigraphy, biostratigraphy, and other independent estimates of age for all three taxonomic groups. These frameworks demonstrate the potential of enamel-based amino acid geochronologies for relative dating of Middle–Late Pleistocene deposits in the UK, and establish an aminostratigraphic framework from which the dating of other tooth material can be refined. Enamel offers an opportunity to evaluate the age of sites where shell material is absent or poorly preserved. It can also, crucially, provide direct relative dating of mammalian fossils, which are often the focus of study in terms of their evolution, distributional changes or extinction. Direct dating negates the risk that the mammal fossils themselves might be reworked, or of different ages to shell, sediments or other dated material in the same deposits; it also enables archived samples with insecure provenance (e.g. from early 17th-19th century collections) to be directly dated.

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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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