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首页> 外文期刊>Journal of King Saud University >Spectroscopic studies on Permian plant fossils in the Pedra de Fogo Formation from the Parnaíba Basin, Brazil
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Spectroscopic studies on Permian plant fossils in the Pedra de Fogo Formation from the Parnaíba Basin, Brazil

机译:巴西帕尔纳巴盆地Pedra de Fogo组二叠纪植物化石的光谱学研究

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The Pedra de Fogo Formation dated from the early Permian (approximately 280?Mya), belongs to the sedimentary Parnaíba Basin, located in the northeastern region of Brazil. It is recognized by their well preserved plant fossil contents and it is notable for having several fossilized trunks in the life position. This study presents physical and/or chemical properties of the fossilized plants through vibrational spectroscopies, SEM/EDS spectroscopy and X-ray diffraction techniques. Specimens from different localities were selected for the purpose of identifying and characterizing compounds related to the fossilized materials. These different techniques allowed obtaining information from the molecular spectra in organic and inorganic substances, which are present in these stated fossils and in the atomic elements, as well as the crystalline phases. Based on the results duly obtained, we were able to identify the presence of silica and confirm that the dominant process of the fossilized specimens investigated has occurred through quartz silicification with the contribution of persistence from amorphous carbon.
机译:Pedra de Fogo岩层可追溯至二叠纪早期(约280?Mya),属于巴西东北地区的沉积性Parnaíba盆地。它的保存良好的植物化石含量得到认可,并且在生活中还拥有多个化石树干。这项研究通过振动光谱,SEM / EDS光谱和X射线衍射技术展示了化石植物的物理和/或化学性质。选择了来自不同地区的标本,以鉴定和表征与化石材料有关的化合物。这些不同的技术允许从有机和无机物质的分子光谱中获取信息,这些物质存在于这些化石,原子元素以及晶相中。根据适当获得的结果,我们能够确定二氧化硅的存在,并确认所研究的化石标本的主要过程是通过石英硅化作用而发生的,而非晶碳的持久性也对其产生了影响。

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