在移动硬基质中对内石古社会发展的新见解,使用来自世 (西南西班牙阿尔梅里亚) 的生物侵蚀的CT成像
Weronika Łaska1,2, Francisco J Rodríguez-Tovar3, Alfred Uchman4
1Faculty of Geography and Geology, Institute of Geological Sciences, Jagiellonian University, Gronostajowa 3a, 30-387, Kraków, Poland. wn.laska@uw.edu.pl.
Die Naturwissenschaften
|February 8, 2024
概括
计算机断层扫描 (CT) 揭示了世碳酸盐石块中复杂的生物侵蚀历史. 虫钻孔占主导地位,这表明频繁的物理干扰影响了这些古代海洋环境中的生态继承.
科学领域:
- 古生物学的古生物学
- 沉积物学的沉积物学
- 鱼类学 鱼类学 鱼类学 鱼类学
背景情况:
- 纪浅海碳酸盐石块中的生物侵蚀结构为过去的生态动态提供了洞察力.
- 了解这些结构有助于古环境的重建和与现代生态系统的比较.
研究的目的:
- 分析二代碳酸盐石块中生物侵蚀结构的3D架构和 ichnotaxonomy.
- 解释生物侵蚀的古老环境意义及其与物理干扰的关系.
- 研究生物和代遗传过程在塑造毛孔网络中的相互作用.
主要方法:
- 计算机断层扫描 (CT) 扫描用于内部结构的详细3D分析.
- 生物侵蚀痕迹的标识和定量.
- 石化分析和手部样本观察以确定基因变化.
主要成果:
- 鉴定了来自5个类中的14个类型,主要由虫 (polychaetes,sipunculids) 占主导地位.
- 揭示了复杂的殖民历史,与重复的生物侵蚀和物理干扰事件.
- 他区分了生物侵蚀的多孔性与代谢性毛孔 (多洛米化,化,溶解),并指出生物侵蚀往往发生晚些时候.
结论:
- 频繁的物理干扰可能有利于早期的连续性虫钻探者,而不是晚期的连续性海绵.
- 代遗传过程创造了菌孔隙,这可能是无聊海绵的初始息地.
- 这项研究表明,生物和非生物过程对内石古社会发展的综合影响.
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