在铁限制之前结合铁: siderophore 合成在铁成为限制元素之前早就出现了
Ricardo Soares1,2, Inês B Trindade1,3, Ricardo O Louro1
1Instituto de Tecnologia Química e Biológica da Universidade Nova de Lisboa, Avenida da República (EAN), Oeiras 2780-157, Portugal.
ISME communications
|February 23, 2026
概括
赛德罗的进化发生在大氧化事件 (GOE) 之前,这挑战了以前的理论. 这表明早期的微生物利用 siderophores 进行矿物溶解,而不仅仅是获得铁.
科学领域:
- 生物地质化学生物地质化学
- 分子进化分子进化
- 天体生物学 天体生物学
背景情况:
- 铁结合分子的 siderophores 被认为是在大氧化事件 (GOE) 后出现的,这是由于铁的生物可用性降低.
- 铁对生命至关重要,它的可用性对微生物进化产生了深刻的影响.
研究的目的:
- 为了研究 siderophore 生合成和利用基因的进化时间表.
- 质疑关于 siderophore 起源的既定观点,它只与印度政府有关.
主要方法:
- 对 siderophore 相关基因的分子钟分析.
- 遗传学分析以估计基因出现日期.
主要成果:
- 赛德罗生物合成基因显著早于铁性赛德罗减少酶和酶出现.
- 非核糖体合成酶独立的 siderophore 合成酶的出现早于 GOE 超过10亿年.
- 在 siderophore 合成和利用机器之间存在时间差距.
结论:
- 赛德罗的进化早于GOE,这表明了铁稀缺之外的其他驱动因素.
- 另一个假设是 siderophores 有助于铁矿物质溶解,防止微生物嵌.
- 早期的地球微生物-矿物相互作用是关键的选择性力量,需要重新评估 siderophore 进化.
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