新生代古叠层石:芬诺斯堪地盾东部的 Segosia columnaris 和 Sundosia mira:微观结构和三维建模

Andrew Lyutikov
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引用次数: 0

摘要

本研究的目的是对位于芬诺斯康地盾(卡累利阿克拉通)东部的古新生代叠层石 Segosia columnaris 和 Sundosia mira 的微观结构和三维建模进行研究。研究的前提是研究人员在 20 世纪 50 年代和 80 年代收集的大量古生物材料。研究采用了现代方法,包括扫描电镜分析、三维建模和拉曼光谱结果。通过对叠层石微观结构的研究,发现了参与这些结构形成的蓝藻可能残留物,这可能表明了所研究样本的生物起源。其他作者获得的拉曼光谱结果也表明了所研究样本的生物起源性质。三维可视化软件首次获得了所研究叠层石的空间形状图像,可用于根据形态特征完善叠层石的分类。对叠层石建筑进行三维建模可以恢复其原始形状。
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Paleoproterozoic stromatolites Segosia columnaris and Sundosia mira of the Eastern part of the Fennoscandian Shield: microstructure and 3D modeling
The purpose of this study is to study the microstructure and 3D modeling of Paleoproterozoic stromatolites Segosia columnaris and Sundosia mira in the eastern part of the Fennoscandian shield (Karelian craton). The premise of the study is the extensive paleontological material collected by researchers in the 1950s and 1980s. Modern methods, including SEM analysis, 3D modeling, and the results of Raman spectroscopy are used. As a result of studying the microstructure of stromatolites, possible remnants of cyanobacteria involved in the formation of these structures were identified, which potentially indicated the biogenic origin of the studied samples. The results of Raman spectroscopy obtained by other authors also indicate the biogenic nature of the studied samples. For the first time, images of the spatial shapes of the studied stromatolites were obtained by 3D visualization software, which could be used to refine the classification of stromatolites by morphological features. 3D modeling of stromatolite buildings allowed restoring their original shape.
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