病毒参与了梯形岩的有机矿物化
Mirosław Słowakiewicz1, Edoardo Perri2, Ezher Tagliasacchi3
1Faculty of Geology, University of Warsaw, 02-089, Warsaw, Poland. m.slowakiewicz@gmail.com.
Scientific reports
|July 19, 2023
概括
现代的岩岩构成是各种微生物群落的宿主,包括丰富的菌体 (细菌病毒). 这些病毒在有机矿物化中发挥作用,影响着青.
科学领域:
- 地质微生物学的生物.
- 生物矿物化 生物矿物化
- 环境科学 环境科学
背景情况:
- 梯形岩通常被视为物理化学和微生物沉的产物.
- 病毒在岩形成中的作用尚未得到广泛研究.
研究的目的:
- 为了调查病毒群落在现代岩生物膜中的存在和影响.
- 了解涉及病毒在碳酸盐和环境中的有机矿化过程.
主要方法:
- 来自欧洲和亚洲草遗址的生物膜的元基因组学分析.
- 对类似病毒的颗粒和矿物沉物的显微镜检查.
- 分析病毒社区的组成和分布.
主要成果:
- 在特拉维生物膜中发现了高度多样化的病毒,细菌和考古社区.
- 细菌菌体,特别是二面体类型 (Siphoviridae,Myoviridae,Podoviridae) 是最丰富的病毒.
- 观察到病毒经过矿化,最初是Ca-Si沉,然后形成Ca碳酸盐纳米球体.
结论:
- 病毒,特别是菌体,是现代岩相关微生物群落的重要组成部分.
- 病毒积极参与这些环境中的有机矿物化过程.
- 结合病毒作用对于准确的地质和生态系统模型的岩形成至关重要.
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