在海底热水系统中减少非生态N2可以迅速使非生态海洋受精
Liheng Sun1,2, Kan Li2, Zhen Sun3,4,5
1State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.
Nature communications
|November 28, 2025
概括
在水热系统中,生物降解 (ANR) 在地球早期产生了大量的 (NH4+). 这一过程可能为生命提供了必要的化合物.
科学领域:
- 地质化学 地质化学
- 天体生物学 天体生物学
- 生命的起源研究 生命的起源研究
背景情况:
- 氨 (NH3) 或氨 (NH4+) 对于有机化合物的非生物合成和解决微弱的年轻太阳悖论至关重要.
- 在前生物地球上可持续的NH3 / NH4 + 需要在热水系统中有效的非生物N2减少 (ANR),这一过程缺乏地质证据.
- 实验室研究已经证明了ANR,但其在自然地质环境中的存在仍然未得到证实.
研究的目的:
- 调查在热水系统中的非生物N2降解 (ANR) 的地质证据.
- 量化海洋地水热脉中氨 (NH4+) 的产量和同位素特征.
- 评估ANR对地球早期全球循环的潜在贡献.
主要方法:
- 在海洋地的热液样本中分析氨 (NH4+) 度和同位素比率 (15N/14N).
- 地质化学建模以模拟水热系统中的循环和同位素分离.
- 测量的同位素特征与对非生物和生物变化的预测进行比较.
主要成果:
- 在南中国海盆地海洋地内的水热脉中检测到高度的15N贫的NH4+.
- 同位素数据表明,15N贫的NH4+起源于深水热流体中的ANR.
- 面向15N丰富的NH4+的过渡表明了生物过程的过度打印.
结论:
- 在水热系统中发生了非生物性N2降解 (ANR),产生了大量的15N贫的NH4+.
- 水热系统中的ANR可以向前生物海洋提供大量的NH4+,可能会使它们受精,并提供大气NH3.
- 这些发现为ANR及其在益生菌循环中的作用提供了第一个地质证据.
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