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Comparing bioapatite carbonate pre-treatments for isotopic measurements: Part 2-Impact on carbon and oxygen isotope compositions

机译:比较用于同位素测量的生物磷灰石碳酸盐预处理:第2部分对碳和氧同位素组成的影响

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Carbon and oxygen isotope measurements (delta C-13, delta O-18) of bioapatite carbonate fractions in archaeological and fossil remains are essential tools to investigate past diets and climates. The reliability of these reconstructions is however dependent on the recovery of the biological signal and the removal of competing sources of carbon and oxygen isotopes, such as remaining organic material and secondary carbonates. Modern, archaeological and fossil bone and tooth specimens have been treated with different chemicals commonly used to pre-treat the samples with the aim of removing these competing sources of isotopes. Results highlight significant shifts in the isotope values of the samples tested, with different isotopic effects according to which pre-treatment was used. This has a clear impact on the data recovered, which may lead to misinterpretations of the results and inferred past diets and climates. The results of this study suggest that both hydrogen peroxide and sodium hypochlorite, the most commonly used oxidising agents employed to remove organic substance, have major problems: hydrogen peroxide is only partially efficient as organic removal agent and causes unwanted bioapatite dissolutions and isotopic shift, while sodium hypochlorite induces the incorporation of exogenous carbonates into the bioapatite, likely from the dissolution of atmospheric CO2 into the test tube. In both cases, there is an impact on the recovered isotope composition. Hydrazine hydrate, a third chemical for organic removal, has the lowest influence on the bioapatite isotopic composition, being also efficient at removing organic matter from bioapatites. The latter is recommended as an organic removal agent if such pre-treatment is deemed necessary. The use of acetic acid also causes isotopic shifts that seem independent on the removal of secondary/diagenetic carbonate, as also occurring in modern samples. Overall, our study clearly shows that any chemical treatment commonly used to remove unwanted contaminants from the bioapatite samples has also unpredictable, often significant effects on the pristine isotopic composition recovered, and corroborates the need for consistency in the pre-treatment of bone and teeth specimens. It also questions the necessity of removing organic matter at all from most skeletal samples prior to isotopic analysis. (C) 2015 Elsevier B.V. All rights reserved.
机译:考古和化石残留物中生物磷灰石碳酸盐馏分的碳和氧同位素测量(δC-13,δO-18)是研究过去饮食和气候的重要工具。然而,这些重建的可靠性取决于生物信号的恢复以及碳和氧同位素的竞争性来源(例如剩余的有机物质和仲碳酸盐)的去除。现代的,考古的和化石的骨骼和牙齿标本已经用通常用于预处理样品的不同化学物质处理过,目的是去除这些竞争的同位素源。结果表明,所测试样品的同位素值发生了显着变化,根据所使用的预处理方法,同位素效应不同。这对回收的数据有明显的影响,可能导致对结果的误解并推断过去的饮食和气候。这项研究的结果表明,过氧化氢和次氯酸钠(用于去除有机物质的最常用氧化剂)都存在主要问题:过氧化氢仅部分有效地用作有机去除剂,并会引起有害的生物磷灰石溶解和同位素迁移,而次氯酸钠可能将外源碳酸盐掺入生物磷灰石中,这可能是由于大气中的二氧化碳溶解在了试管中。在这两种情况下,都会对回收的同位素组成产生影响。水合肼是用于有机物去除的第三种化学物质,对生物磷灰石的同位素组成影响最小,也有效去除了生物磷灰石中的有机物。如果认为需要进行预处理,则建议将后者用作有机去除剂。乙酸的使用还会引起同位素迁移,这似乎与中学/成岩碳酸盐的去除无关,这也发生在现代样品中。总体而言,我们的研究清楚地表明,通常用于从生物磷灰石样品中去除不需要的污染物的任何化学处理方法,对回收的原始同位素组成也具有不可预测的,通常具有显着影响,并证实了在对骨骼和牙齿样品进行预处理时需要保持一致性。它还质疑在同位素分析之前从大多数骨骼样品中完全去除有机物的必要性。 (C)2015 Elsevier B.V.保留所有权利。

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