在深海铁地地表面的微生物样结构中,Ce和有机物的共同丰富
Ayaka Tokumaru1, Mariko Kouduka1, Hiroki Suga1,2
1Department of Earth and Planetary Science, The University of Tokyo, Bunkyo-ku, Tokyo, Japan.
概括
深海铁地上含有铁氧化物的微生物样结构显示的丰富. 这一发现表明,在含氧海洋中积累的新型微生物过程与早期地球和火星有关.
科学领域:
- 地质化学 地质化学
- 海洋科学 海洋科学
- 天体生物学 天体生物学
背景情况:
- (Ce) 对于了解历史上海洋氧化还原状态至关重要.
- 深海铁甲地是有氧化海洋中重要的Ce沉积点.
- 氧化物的无机氧化传统上解释了Ce的缩.
研究的目的:
- 研究潜在的微生物在深海积累中的作用.
- 描述铁甲皮上发现的类似微生物的结构.
- 确定这些结构中丰富的机制.
主要方法:
- 显微镜和纳米级固态分析.
- 类似微生物的Fe-Mn氧化物结构的表征.
- 对有机物质组成和物种的分析.
主要成果:
- 在地表面发现了与Fe-Mn氧化物矿化的类似微生物的结构.
- 这些结构富含和有机物质.
- 有机物表现出芳香/碳酸; (III) 出现在表面坑中,表明局部减少.
结论:
- 提出了一种用于深海铁甲地中积的新型微生物过程.
- 这一过程涉及到类似微生物的结构和局部化的Ce (III) 稳定性.
- 这些发现对了解古代地球和火星铁氧化物和行星保护有重要意义.
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