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Microanalysis and synthesis of calcite. Growth mechanisms on prehistoric paintings in the Large Cave, Arcy-sur-Cure (Yonne, France)

机译:方解石的微分析和合成。阿尔凯河畔库里(Arcy-sur-Cure)大洞穴中史前绘​​画的生长机制(法国约讷)

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The formation of subsequent layers of calcium carbonate (CaCO3) in karst caves is a well-known phenomenon observed especially on the prehistoric paintings in the Large Cave (Grande Grotte) of Arcy-sur-Cure, in France. About 40 natural samples coming from the Large Cave were already investigated in a previous work and classified as a function of their crystal morphology, texture, composition and appearance. The presence of at least two calcite types was revealed on the walls: translucent and opaque white or grey calcites. The latter opaque calcites completely obstruct the paintings. The formation of these different calcites depends on various geochemical and geophysical parameters and could also be influenced by biotic processes. Questions remain about formation mechanisms leading to different calcite types and, in particular, about the role of micro-organisms as well as interactions between prehistoric paint layers and calcite layers. Additional natural calcites were studied in order to confirm the first classification. Various syntheses of abiotic calcite were performed to study the influence of environmental parameters on calcite growth. Moreover, several series of biotic calcite were synthesised in a specific medium with two bacteria isolated from the cave in order to test their calcifying properties. All natural and synthetic samples were analysed using complementary microanalytical laboratory techniques. Micro-x-ray fluorescence analysis (micro-XRF) and x-ray absorption near-edge structure spectroscopy (XANES) based on synchrotron radiation also enabled a more detailed distinguishing of different minerals within the complex biotic and abiotic mixtures and layered synthetic samples at microscopic scale. Comparison of natural and synthetic samples gives more detailed insights into the formation mechanisms of the different calcite types found in the Grande Grotte and allows proposing an adapted conservation strategy of its prehistoric paintings. Copyright (C) 2008 John Wiley & Sons, Ltd.
机译:岩溶洞穴中随后形成的碳酸钙(CaCO3)层是一种众所周知的现象,尤其是在法国Arcy-sur-Cure的大洞穴(Grande Grotte)的史前绘画中观察到。在先前的工作中已经对来自大洞穴的大约40个天然样品进行了研究,并根据其晶体形态,质地,组成和外观进行了分类。墙上发现至少两种方解石类型:半透明和不透明的白色或灰色方解石。后者不透明的方解石完全遮住了绘画。这些不同方解石的形成取决于各种地球化学和地球物理参数,也可能受到生物过程的影响。关于导致方解石类型不同的形成机制,尤其是微生物的作用以及史前涂料层与方解石层之间的相互作用,仍然存在疑问。为了确定第一个分类,还研究了其他天然方解石。进行了各种非生物方解石的合成,以研究环境参数对方解石生长的影响。此外,在特定的介质中合成了一系列生物方解石,并从洞穴中分离出两种细菌,以测试其钙化特性。使用互补的微量分析实验室技术分析了所有天然和合成样品。基于同步加速器辐射的微x射线荧光分析(micro-XRF)和x射线吸收近边缘结构光谱(XANES)还使得能够更详细地区分复杂的生物和非生物混合物以及分层合成样品中的不同矿物微观规模。天然样品和合成样品的比较可以更详细地了解Grande Grotte中发现的不同方解石类型的形成机理,并可以提出对其史前绘画的适应性保存策略。版权所有(C)2008 John Wiley&Sons,Ltd.

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