在高温下进行的古 (per) 酸盐还原:生物和非生物反应的相互作用
Martin G Liebensteiner1, Martijn W H Pinkse, Peter J Schaap
1Laboratory of Microbiology, Wageningen University, Dreijenplein 10, 6703 HB Wageningen, Netherlands.
概括
这项研究表明,古生物,特别是Archaeoglobus fulgidus,可以减少甲酸盐和酸盐离子. 这种古老的生物过程可能影响了早期的地球.
科学领域:
- 环境微生物学环境微生物学
- 生物地质化学生物地质化学
- 考古物 (Archaea) 是一种古老的物种.
背景情况:
- 甲酸盐和酸盐离子是环境污染物,细菌利用它们作为电子受体.
- 这些离子的生物降解以前被认为仅限于细菌.
研究的目的:
- 在考古学领域研究酸盐和酸盐降解的潜力.
- 阐明古代 (酸盐) 减少的生化途径和环境影响.
主要方法:
- 用超热的Archaeoglobus fulgidus进行了生长实验.
- 基因组和蛋白质组分析以确定相关的酶和途径.
- 研究化物中间体的命运.
主要成果:
- 考古球体 fulgidus 证明了 (per) 酸盐减少的能力,将这一过程扩展到古生物.
- 该途径涉及与细菌对应物相似的基酶.
- 酸盐不是通过酶分解分解的,而是通过与硫化合物的无生物/生物氧化回氧反应消除.
结论:
- 生物 (甲) 降解不仅限于细菌,而且发生在古生物中.
- 这种古老的考古活动可能在氧化光合作用之前调节了早期地球的氧化还原条件.
- 了解这种途径可以了解早期的生物地球化学循环.
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