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SEM EBSD laser confocal microscopy and FE-SEM data from modern

机译:SEMEBSD激光共聚焦显微镜和现代的FE-SEM数据

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摘要

Here, we provide the dataset associated with the research article “Orientation patterns of aragonitic crossed-lamellar, fibrous prismatic and myostracal microstructures of modern Glycymeris shells” [1]. Based on several tools (SEM, EBSD, laser confocal microscopy and FE-SEM) we present original data relative to the microstructure and texture of aragonite crystallites in all Glycymeris shell layers (crossed-lamellar, complex crossed-lamellar, fibrous prismatic and pedal retractor and adductor myostraca) and address texture characteristics at the transition from one layer to the other, identifying similarities and differences among the different layers. Shells were cut transversely, obliquely and longitudinally in order to obtain different orientated sections of the outer and inner layer and of the myostraca. The identification of major microstructural elements was provided by detailed SEM and laser confocal microscopy images. Microstructure and texture characterization was based on EBSD measurements presented as band contrast images and as color-coded crystal orientation maps with corresponding pole figures. Crystal co-orientation was measured with the MUD value. Finally, the distribution of the organic matrix occluded within the outer crossed-lamellar layer was revealed using FE-SEM. These data, besides providing a modern unaltered Glycymeris reference to detect diagenetic alteration in fossil analogs used for paleoenvironmental reconstructions, are useful to better comprehend the mechanisms of bivalve shell formation.
机译:在这里,我们提供与研究制品相关的数据集“现代甘草壳的纤维状交叉层状,纤维棱柱肌瘤微观组织的研究制品”取向模式“[1]。基于几种工具(SEM,EBSD,激光共聚焦显微镜和FE-SEM),我们在所有甘油系壳层(交叉层叠,复合横梁,纤维棱镜,纤维棱镜和踏板牵发器)中,我们呈现出原始数据相对于化石微晶的微观结构和质地。和联系者myostraca)和地址从一层到另一层转换的纹理特性,识别不同层之间的相似性和差异。壳被横向,倾斜,纵向切割,以获得外层和内层的不同取向部分和肌肌瘤。通过详细的SEM和激光共聚焦显微镜图像提供主要微观结构元件的鉴定。微观结构和纹理表征基于作为带对比图像的EBSD测量,并且作为具有相应极图的彩色编码晶体取向图。用泥浆值测量晶体协调。最后,使用Fe-SEM揭示了在外交叉层层内封闭的有机基质的分布。除了提供现代未改变的甘草粒子的这些数据外,为了检测用于古环境重建的化石类似物中的成岩性改变,可用于更好地理解双撇壳形成的机制。

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