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首页> 外文期刊>Analytical and bioanalytical chemistry >Novel contribution on the diagenetic physicochemical features of bone and teeth minerals, as substrates for ancient DNA typing
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Novel contribution on the diagenetic physicochemical features of bone and teeth minerals, as substrates for ancient DNA typing

机译:作为古代DNA分型的底物,对骨骼和牙齿矿物质的成岩理化特性的新贡献

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The extraction of DNA from skeletal remains is a major step in archeological or forensic contexts. However, diagenesis of mineralized tissues often compromises this task although bones and teeth may represent preservation niches allowing DNA to persist over a wide timescale. This exceptional persistence is not only explained on the basis of complex organo-mineral interactions through DNA adsorption on apatite crystals composing the mineral part of bones and teeth but is also linked to environmental factors such as low temperatures and/or a dry environment. The preservation of the apatite phase itself, as an adsorption substrate, is another crucial factor susceptible to significantly impact the retrieval of DNA.With the view to bring physicochemical evidence of the preservation or alteration of diagenetic biominerals, we developed here an analytical approach on various skeletal specimens (ranging from ancient archeological samples to recent forensic specimens), allowing us to highlight several diagenetic indices so as to better apprehend the complexity of bone diagenesis. Based on complementary techniques (X-ray diffraction (XRD), Fourier transform infrared (FTIR), calcium and phosphate titrations, SEM-EDX, and gravimetry), we have identified specific indices that allow differentiating 11 biological samples, primarily according to the crystallinity and maturation state of the apatite phase. A good correlation was found between FTIR results from the analysis of the v3(PO4) and v4(PO4) vibrational domains and XRD-based crystallinity features. A maximal amount of information has been sought from this analytical approach, by way of optimized posttreatment of the data (spectral subtraction and enhancement of curve-fitting parameters). The good overall agreement found between all techniques leads to a rather complete picture of the diagenetic changes undergone by these 11 skeletal specimens. Although the heterogeneity and scarcity of the studied samples did not allow us to seek direct correlations with DNA persistence, the physicochemical parameters described in this work permit a fine differentiation of key properties of apatite crystals among postmortem samples. As a perspective, this analytical approach could be extended to more numerous sets of specimens so as to draw statistical relationships between mineral and molecular conservation.
机译:从骨骼遗骸中提取DNA是考古或法医研究的重要一步。但是,矿化组织的成岩作用通常会损害这项任务,尽管骨骼和牙齿可能代表着保存位,从而使DNA可以在很长的时间内持续存在。这种异常的持久性不仅可以通过在组成骨骼和牙齿的矿物部分的磷灰石晶体上进行DNA吸附来进行复杂的有机-矿物相互作用来解释,而且还可以与诸如低温和/或干燥环境之类的环境因素相关联。磷灰石相本身作为吸附底物的保存是另一个重要的因素,很容易显着影响DNA的回收。为了提供成岩生物矿物的保存或改变的理化证据,我们在此开发了一种对各种生物矿物的分析方法。骨骼标本(从古代考古样品到最近的法医标本),使我们能够突出显示几个成岩指数,以便更好地了解骨成岩的复杂性。基于补充技术(X射线衍射(XRD),傅立叶变换红外(FTIR),钙和磷酸盐滴定,SEM-EDX和重量分析法),我们已经确定了可以区分11个生物样品的特定指标,主要根据结晶度和磷灰石相的成熟状态。在对v3(PO4)和v4(PO4)振动域以及基于XRD的结晶度特征进行分析的FTIR结果之间发现了很好的相关性。通过优化的数据后处理(光谱减法和曲线拟合参数的增强),从这种分析方法中寻求了最大的信息量。所有技术之间的良好总体一致性使这11个骨骼标本经历了完整的成岩变化图。尽管研究样品的异质性和稀缺性使我们无法寻求与DNA持久性的直接相关性,但这项工作中描述的物理化学参数可以使尸检样品中的磷灰石晶体的关键特性进行精细区分。从一个角度来看,这种分析方法可以扩展到更多的标本集,以便得出矿物和分子守恒之间的统计关系。

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