红氧受约束的微生物生态学决定了损失与留
Jemma Fadum1, Xin Sun1,2, Emily Zakem1
1Division of Biosphere Sciences and Engineering, Carnegie Institution for Science, Stanford, CA 94305, United States.
ISME communications
|December 15, 2025
概括
幼化将水生微生物从损失转移到留,从而加剧了这个问题. 我们的模型解释了这种转变,为生态系统管理和微生物社区分析提供了预测.
科学领域:
- 微生物生态学 微生物生态学
- 生物地质化学循环过程
- 生态系统建模 生态系统建模
背景情况:
- 微生物是生物地球化学循环的关键驱动力.
- 在深度无毒水域的水生系统中,化会增加表面生产力,影响无氧微生物群落.
- 增加沉沉的有机碳可以将微生物功能从气损失转移到留,创造一个积极的反循环,放大了轻化.
研究的目的:
- 在无氧微生物群落中,开发一个从损失到留过渡的定量,第一原则模型.
- 将微生物生态动力学与微生物代谢的能量学联系起来.
- 了解增加有机碳供应对循环的影响.
主要方法:
- 开发并分析了结合氧化还原化学的生态系统模型.
- 关键无氧循环微生物功能类型的受约束特征:脱化,非仿真性酸盐降解为,和无氧氧化 (anammox).
- 将生态动态与微生物代谢能量学联系起来.
主要成果:
- 该模型成功地捕捉了从损失到保留的过渡,随着有机碳供应的增加.
- 在"净零N损失"点的微生物群体组成的确定特征.
- 提供可测试的假设来测序数据和其他观察.
结论:
- 该模型提供了一种机理性的理解,即对由于环氧化而导致的循环转移.
- 结果提供了一个广泛适用的框架,用于预测诸如缩和脱氧等干扰的生物地质化学影响.
- 将微生物生态与环境化学潜力联系起来,可以提高水生生态系统的预测能力.
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