铁 (III) (氧化) 氧化物被热爱的减少铁的细菌Desulfovulcanus ferrireducens减少
Elizabeth C Sklute1,2, Deborah A Leopo3, Kaylee A Neat4
1Planetary Science Institute, Tucson, AZ, United States.
Frontiers in microbiology
|November 6, 2023
概括
热性降铁细菌将铁酸盐等矿物质转化为磁铁. 其他铁矿物质产生难以溶解的纳米圈,显示出各种微生物生物矿化通路.
科学领域:
- 地质微生物学的生物.
- 生物矿物化 生物矿物化
- 深海微生物学 深海微生物学
背景情况:
- 深海通风口中的热友细菌利用铁的减少来生长.
- 了解这些微生物的生物性矿物转化是有限的.
研究的目的:
- 为了研究Desulfovulcanus ferrireducens的矿物转化.
- 为了分析生长在铁酸盐,阿加尼特和勒皮多克罗西特上产生的产物.
主要方法:
- 使用可见近红外 (VNIR),FTIR-ATR,Mössbauer光谱学,XRD和TEM.
- 培养了具有特定铁矿物质作为电子受体的细菌.
- 使用多种光谱和显微技术分析矿产产品.
主要成果:
- 铁酸盐的转化产生了阴离子缺乏磁铁.
- 阿卡尼尼特和勒皮多克罗西特产生了难以溶解的黑色纳米球.
- 与对照组相比,生物降解产品表现出明显的光谱和形态特征.
结论:
- 热友细菌转化各种Fe (III) 矿物质,结果各不相同.
- 矿产产品是由溶解-再沉产生的,而不仅仅是化学平衡.
- 微生物生物矿物化途径复杂且难以预测.
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