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CHANGES IN THE METAL CONTENT OF HUMAN HAIRDURING DIAGENESIS FROM 500 YEARS, EXPOSURE TOGLACIAL AND AQUEOUS ENVIRONMENTS

机译:历年500年来人发性斜向性汗液中金属含量的变化,暴露于冰雹和水的环境

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Scanning electron microscopy, inductively coupled plasma mass spectroscopy and time-of-flight secondary ion mass spectrometry have been used to examine the extent and possiblemechanisms by which the metal content of human hair is altered by exposure to aqueousenvironments. The results, using both modern hair and samples from 500-year-old hairassociated with glacier-entombed remains, show that the metal content has been alteredsufficiently so that the interpretation of the metal signature in terms of diet or disease isproblematic. While endogenous information is difficult to glean from these data, interestingobservations have been made of possible early stages of mineral authigenic deposition. Thechemistry of the outer hair surface was found to he consistent with deposition of Fe and Alsilicates, as well as other mineral phases. The ancient hair was analysed at the root region andincluded a comparison of the internal versus external composition to assist in identifying thediagenetic processes.
机译:扫描电子显微镜,电感耦合等离子体质谱和飞行时间二次离子质谱已用于检查暴露于水环境而改变人发金属含量的程度和可能的机理。使用现代头发和来自500年历史的,与冰川沉陷残骸相关的头发样本的结果表明,金属含量已被充分改变,因此从饮食或疾病方面对金属特征的解释是有问题的。虽然很难从这些数据中收集内源性信息,但人们对矿物自生沉积的可能早期阶段进行了有趣的观察。发现头发外表面的化学性质与铁和铝硅酸盐以及其他矿相的沉积相一致。在根部区域对古发进行了分析,包括内部和外部成分的比较,以帮助识别成岩过程。

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