细菌中硫化铁矿物的反应序列及其作为生物标志物的使用
M Pósfai1, P R Buseck, D A Bazylinski
1Department of Geology, Arizona State University, Tempe, AZ 85287, USA.
概括
细菌可以在内部制造微小的磁性灰岩石 (Fe3S4) 晶体. 这些晶体在几周内从非磁性前体中形成,影响了对外星矿物的解释.
科学领域:
- 生物矿物化 生物矿物化
- 地质化学 地质化学
- 微生物学 微生物学
背景情况:
- 一些细菌合成细胞内磁性硫化铁晶体,如灰岩石 (Fe3S4).
- 这些生物性磁性晶体影响细菌行为和环境相互作用.
研究的目的:
- 研究细菌中细胞内灰炎的形成途径和前体.
- 为了澄清涉及生物质灰岩合成的矿物质变化.
主要方法:
- 传输电子显微镜 (TEM) 用于观察细胞内晶体的形态和组成.
- 分析的重点是识别前体矿物质和转化过程.
主要成果:
- 观察到铁磁灰岩 (Fe3S4) 从非磁性马基纳岩 (四边形FeS) 和潜在的立方FeS中形成.
- 转化过程涉及铁原子的重新排列,并且发生在几天到几周的时间内.
- 在这种细菌系统中,既没有发现pyrrhotite,也没有发现pyrite是产物或前体.
结论:
- 细菌中灰岩的形成是通过特定的前体矿物质和依赖时间的转变而发生的.
- 了解细菌灰石的形成,可以了解生物矿物化过程.
- 这些发现对解释外星样本中灰岩和岩的存在有影响,比如火星石ALH84001.1.
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