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Evidence for long-term averaging of strontium in bovine enamel using TIMS and LA-MC-ICP-MS strontium isotope intra-molar profiles.

机译:使用TIMS和LA-MC-ICP-MS锶同位素摩尔内曲线对牛牙釉质中锶进行长期平均的证据。

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摘要

High spatial resolution micro-sampling of tooth enamel offers the possibility of high temporal resolution isotope data to reconstruct climate, environment, diet and mobility. Questions remain about the duration and pattern of the maturation phase of enamel and the existence and direction of chronological 'time-lines'. LA-MC-ICP-MS measurements of c. 400 μm craters and TIMS analyses of transverse enamel sections of an archaeological bovine third molar were undertaken to investigate the long-term averaging of incorporated strontium. The same gradually increasing isotope profile was obtained from both approaches, indicating that the large increase in spatial resolution did not change the response profile obtained. The results suggest that even at the microscopic scale, strontium is incorporated over a period in excess of 12 months. Averaging of the input signal may result from both long-term retention of strontium in the skeleton and recirculation in the body pool, or long-term maturation of enamel on a microscopic scale. Whichever mechanism is responsible, it may not be possible to recover strontium isotope ratios with a high time resolution from cattle molar enamel unless there is a large imbalance in the amount of strontium supplied by different sources. Consequently, strontium isotope profiles may not be synchronous with those of lighter isotope systems. ud
机译:牙釉质的高空间分辨率微采样提供了高分辨率的同位素数据来重建气候,环境,饮食和迁移率的可能性。牙釉质成熟阶段的持续时间和方式,以及时间“时间表”的存在和方向仍然存在疑问。 LA-MC-ICP-MS测量c。进行了400μm陨石坑和考古牛第三磨牙横向釉质截面的TIMS分析,以研究掺入锶的长期平均值。从这两种方法都获得了相同的逐渐增加的同位素分布,这表明空间分辨率的大幅提高并未改变获得的响应分布。结果表明,即使在微观范围内,锶的掺入时间也超过12个月。输入信号的平均可能是由于锶在骨骼中的长期保留和在人体池中的再循环,或者是珐琅质在微观尺度上的长期成熟所致。无论哪种机制起作用,除非从不同来源供应的锶数量存在很大的失衡,否则不可能从牛磨牙珐琅质中以高时间分辨率恢复锶同位素比。因此,锶同位素的分布可能与较轻的同位素系统的分布不同步。 ud

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