一个窗口进入过渡金属的可用性在早期的古新生代的海水
Ansahmbom Y Nke1, Rosalind E M Rickaby2, Harilaos Tsikos3
1Department of Geological Sciences, University of Cape Town, Rondebosch, 7701, South Africa.
Scientific reports
|December 22, 2025
概括
古代海水的化学成分与今天的化学成分有很大不同,和铁的度很高. 这种金属的可用性可能影响了早期的微生物进化和金属蛋白的发展.
科学领域:
- 地质化学 地质化学
- 古生物学的古生物学.
- 早期地球的条件.
背景情况:
- 所有生命都需要金属来合成金属蛋白质.
- 在无氧海水中金属的可用性在地质时间内发生了巨大的变化.
- 从散装岩石中重建古代海水化学是很困难的.
研究的目的:
- 为了确定古代海水中的过渡金属含量.
- 提供海水化学的高分辨率快照大约2460亿年前.
- 将古代金属度与现代海水和地化学预测进行比较.
主要方法:
- 分析绿岩中的过渡金属含量,这是一个主要的Fe (II) - 酸盐矿物质.
- 使用来自南非库鲁曼山脉的绿岩石微米尺度的线.
- 古代矿物样本的高分辨率地质化学分析.
主要成果:
- (Zn) 和 (V) 在古代海水中稀缺.
- (Ni) 度与现代水平相似.
- (Co) 被丰富, (Mn) 被高度丰富.
- 铁 (Fe) 和 (Mn) 主导着古代海水的组成.
结论:
- 古代海水的化学成分与今天有很大不同,其特点是高和.
- 早期生命可能使用了Fe和Mn,与它们的丰富性相一致.
- 极高的Mn度可能影响了细胞过程并推动了进化速率.
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