一种早期分枝的微生物菌形成了细胞内碳酸盐
Estelle Couradeau1, Karim Benzerara, Emmanuelle Gérard
1Institut de Minéralogie et de Physique de la Matière Condensée, CNRS UMR 7590, Université Pierre et Marie Curie, Paris, France.
概括
蓝藻细菌形成细胞内碳酸含量,揭示了一个新的生物矿物化途径. 这一发现挑战了化仅仅是细胞外的观点,扩大了对微生物在地化学中的作用的了解.
科学领域:
- 地质微生物学的生物.
- 生物矿物化 生物矿物化
- 菌研究 菌研究
背景情况:
- 菌显著影响地球的地化学循环,包括碳,和氧.
- 化,即碳酸的形成,是历史上被视为细胞外的关键过程.
- 微生物体是微生物群落形成的结构,通常涉及化.
研究的目的:
- 为了研究蓝藻细菌中的新化途径.
- 为了识别和描述与现代微生物体内的生物矿物化有关的蓝藻细菌.
- 探索微生物碳酸盐形成中的细胞控制机制.
主要方法:
- 从墨西哥阿尔奇奇卡湖 (Alchichica Lake) 取出微生物的实地采样.
- 蓝藻细菌的分离和遗传学分析.
- 使用显微镜和化学分析对细胞内含的表征.
主要成果:
- 在Gloeobacterales序列中识别一种蓝藻细菌,形成细胞内无形碳酸含量.
- 包含的平均直径为270纳米,含有,,和.
- 构成和结构表明细胞内受控的生物矿物化.
结论:
- 一个以前未知的菌细胞内化的途径已经被发现.
- 这一发现扩大了已知能够形成无形碳酸的有机体的多样性.
- 细胞对蓝藻细菌生物矿物化的控制得到了证明,影响了我们对微生物地球化学的理解.
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