水中脱氧作为行星边界和地球系统稳定的关键调节器
Kevin C Rose1,2, Erica M Ferrer3,4, Stephen R Carpenter5
1Department of Biological Sciences, Rensselaer Polytechnic Institute, Troy, NY, USA. rosek4@rpi.edu.
Nature ecology & evolution
|July 15, 2024
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地球系统科学 地球系统科学
- 环境科学 环境科学
- 生态生态学 生态生态学
背景情况:
- 行星边界定义了影响全球可居住性的地球系统过程的关键值.
- 人类活动正在改变这些过程,可能会破坏地球的稳定.
- 地球系统过程的相互连接意味着跨越一个边界可能会影响其他边界.
研究的目的:
- 建议淡水和海洋生态系统的脱氧化作为一个额外的行星边界.
- 突出氧气水平在地球生态和社会系统中的关键作用.
- 将脱氧纳入行星边界框架,以集中全球努力.
主要方法:
- 审查关于水生息地脱氧的研究.
- 对氧气值和变化速度的分析.
- 评估脱氧化与其他行星边界过程的相互作用.
主要成果:
- 水生生态系统的脱氧正在迅速发生,接近临界值.
- 氧气耗尽的速度与其他公认的行星边界过程相当.
- 脱氧既影响,也受到其他地球系统过程变化的影响.
结论:
- 脱氧代表了对生态和社会完整性至关重要的关键行星边界.
- 扩大行星边界框架,包括去氧化是必要的.
- 迫切需要全球监测,研究和政策努力,以应对脱氧化挑战.
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