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Updated: Jun 27, 2025

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在地质时代中,利用植物遗传学计算循环酶的进化时间
Joanne S Boden1, Juntao Zhong2, Rika E Anderson3
1School of Earth and Environmental Sciences, University of St. Andrews, Bute Building, Queen's terrace, St. Andrews, Fife, United Kingdom. j.boden@st-andrews.ac.uk.
Nature communications
|May 2, 2024
概括
早期生命可以获得高酸盐水平,这是基因进化所证明的. 减少的使用和较低的酸盐度在地球历史的后期出现,这可能会限制早期的生物生产力.
科学领域:
- 生命的起源和演变.
- 生物地质化学生物地质化学
- 古海洋学是古海洋学.
背景情况:
- 对于生物生产力至关重要,但前坎布里亚时期的海洋酸盐水平是不确定的.
- 早期地球上减少物种的生物可用性是未知的.
- 预坎布里亚时期酸盐度的估计差异很大.
研究的目的:
- 重建生命中的获取和代谢的进化历史.
- 根据基因组数据推断早期地球酸盐度.
- 了解在早期生物进化中的作用.
主要方法:
- 基因演变的族系学重建.
- 对酸盐运输和代谢基因的分析.
- 基因进化与估计的酸盐度的相关性.
主要成果:
- 酸盐运输基因 (pnas) 在古老时代 (>3.6亿年前) 进化,这表明酸盐水平>3微米.
- 低酸盐条件 (pstS) 的基因出现在中古时代 (<1μM).
- 降低的代谢途径后来出现,在2.3亿年后得到广泛使用.
结论:
- 早期地球可能有足够的酸盐来维持生命,但通过阿尔凯时代,酸盐水平在本地下降.
- 减少的物种直到大氧化事件之后才被广泛使用.
- 酸盐水平的下降可能限制了早期的生物生产力.
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