首页> 外文OA文献 >Détection d'ADN par spectroscopie SERRS et interactions entre nucléotides et surfaces des minéraux phyllosilicatés ferromagnésiens dans le contexte de l'origine de la Vie
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Détection d'ADN par spectroscopie SERRS et interactions entre nucléotides et surfaces des minéraux phyllosilicatés ferromagnésiens dans le contexte de l'origine de la Vie

机译:在生命起源的背景下,通过SERRS光谱法检测DNA以及叶硅酸铁镁矿物的核苷酸与表面之间的相互作用

摘要

The first goal of this thesis was the development of a non-enzymatic DNA detection method. Current enzymatic techniques such as Polymerase Chain Reaction (PCR) often fail in analyzing ancient or processed samples. Indeed DNA undergoes numerous post-mortem degradations, among which some are known to block the bypass of DNA-polymerases. Our method combines hybridization and SERRS (Surface Enhanced Resonant Raman Scattering) spectroscopy, and allows the detection and quantification of degraded DNA sequences that are refractory to PCR analysis. This novel detection method therefore opens new perspectives, especially in paleogenetics. This thesis also aims at studying the role of mineral surfaces in the origin of nucleic acids. Mineral surfaces might have trapped and concentrated the elementary bricks of those biopolymers, thus contributing in their formation. Previous work has focused on minerals such as montmorillonite, although it might not have been abundant during the Hadean/Archean. The primitive Earth’s mineralogy would have been preferentially dominated by Fe-Mg rich phyllosilicates. We have therefore studied the adsorption of nucleotides on minerals we think are relevant to the geological context, and have varied the environmental conditions. This work allows characterizing the adsorption mechanism of nucleotides on mineral surfaces, as well as environmental conditions of the origin of genetic material.
机译:本文的首要目标是开发一种非酶DNA检测方法。当前的酶促技术,例如聚合酶链反应(PCR),通常无法分析古老或加工过的样品。实际上,DNA经历了许多验尸降解,其中一些已知可以阻止DNA聚合酶的旁路。我们的方法结合了杂交技术和SERRS(表面增强共振拉曼散射)光谱技术,可以检测和定量PCR难以分析的降解DNA序列。因此,这种新颖的检测方法开辟了新的视角,尤其是在古遗传学方面。本论文还旨在研究矿物表面在核酸起源中的作用。矿物表面可能已经捕获并浓缩了这些生物聚合物的基本砖,从而有助于其形成。以前的工作主要集中在诸如蒙脱石等矿物上,尽管在哈代/阿尔奇时期可能并不丰富。原始地球的矿物学原本会以富含铁镁的页硅酸盐为主导。因此,我们研究了核苷酸在我们认为与地质环境有关的矿物上的吸附,并改变了环境条件。这项工作可以表征核苷酸在矿物表面上的吸附机制,以及遗传物质来源的环境条件。

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    Feuillie Cécile;

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  • 年度 2012
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  • 原文格式 PDF
  • 正文语种 fr
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