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How precise are U-series coral ages?

机译:U系列珊瑚的年龄有多精确?

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摘要

U-series dating of fossil reef corals is a well established and widely applied technique in paleoclimate research. Many fossil corals, however, show evidence for post-depositional diagenetic alteration, and it is generally accepted that the accuracy of U-series coral ages is more limited due to coral diagenesis than analytical precision. In recent years, three models have been published that try to correct the effects of diagenesis and allow the calculation of model ages [Thompson W. G., Spiegelmann M. W., Goldstein S. L., and Speed R. C. (2003) An open-system model for U-series age determinations of fossil corals. Earth and Planetary Science Letters 210, 365-381; Villemant B., and Feuillet N. (2003) Dating open systems by the U-238-U-234-Th-230 method: application to Quaternary reef terraces. Earth and Planetary Science Letters 210, 105-118; Scholz D., Mangini A., and Felis T. (2004) U-series dating of diagenetically altered fossil reef corals. Earth and Planetary Science Letters 218, 163-178]. Here, we assess the age variability of both conventional Th-230/U-dating and the three models by application to different sub-samples of individual coral specimens. The age variability, estimated as the 2 sigma-standard deviation on the individual ages, is compared with the errors quoted by the different methods. Our results show that the errors of conventional Th-230/U-dating as well as those of the method of Thompson et al. (2003) do not account for the true age variability. The age variability of both methods is in the range of the errors given by the models of Villemant and Feuillet (2003) and Scholz et al. (2004). Furthermore, we show that the widely used reliability criteria are not sufficient to identify all diagenetically altered corals. In contrast, analysis of different sub-samples of one coral specimen allows (i) to estimate the real age variability, (ii) to test if the assumptions of the models are fulfilled, and (iii) to investigate the diagenetic processes in more detail. Thus, this method should generally be applied to obtain more reliable U-series coral ages and errors. (c) 2007 Elsevier Ltd. All rights reserved.
机译:U系列化石珊瑚的定年是在古气候研究中已建立并广泛应用的技术。但是,许多化石珊瑚显示出沉积后成岩作用的证据,因此,人们普遍认为,由于珊瑚的成岩作用,U系列珊瑚年龄的准确性比分析精度受到更大的限制。近年来,已经发布了三个模型,这些模型试图纠正成岩作用并允许计算模型年龄[Thompson WG,Spiegelmann MW,Goldstein SL和Speed RC(2003),U系列年龄的开放系统模型。化石珊瑚的决心。地球与行星科学快报210,365-381; Villemant B.和Feuillet N.(2003)通过U-238-U-234-Th-230方法对开放系统进行约会:应用于第四纪礁阶地。地球与行星科学快报210,105-118; Scholz D.,Mangini A.和Felis T.(2004)地磁变化化石珊瑚的U系列年代测定。地球与行星科学快报218,163-178]。在这里,我们通过将其应用于单个珊瑚标本的不同子样本来评估常规Th-230 / U约会和这三个模型的年龄变异性。将年龄变异性(估计为各个年龄段的2 sigma标准偏差)与不同方法引用的误差进行比较。我们的结果表明,常规的Th-230 / U约会以及Thompson等人的方法都存在误差。 (2003年)没有考虑到真实的年龄变异性。两种方法的年龄变异性都在Villemant和Feuillet(2003)模型以及Scholz等人的模型给出的误差范围内。 (2004)。此外,我们表明,广泛使用的可靠性标准不足以识别所有由双数位基因改变的珊瑚。相比之下,对一个珊瑚标本的不同子样本的分析允许(i)估计实际年龄变异,(ii)测试模型的假设是否得到满足,以及(iii)更详细地研究成岩过程。 。因此,通常应采用这种方法来获得更可靠的U系列珊瑚年龄和误差。 (c)2007 Elsevier Ltd.保留所有权利。

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