河岸地区的氧化还原振荡通过增强微生物呼吸来刺激碳损失
Zhenchen Li1, Xiaoyun Li1, Binquan Jiao2
1Key laboratory of the Three Gorges Reservoir Region's Eco-environments, Ministry of Education, Institute of Environment and Ecology, Chongqing University, 174 Shapingba Road, Chongqing 400045, China.
Water research
|March 4, 2026
概括
沿海地区的减氧振荡降低了微生物碳利用效率,加速了碳损失. 铁循环和基激素主要燃烧有机物质,将生态系统变成碳泄漏热点.
科学领域:
- 环境科学 环境科学
- 微生物生态学 微生物生态学
- 生物地质化学生物地质化学
背景情况:
- 沿海生态系统在碳捕获中发挥着至关重要的作用.
- 氧化还原振荡对微生物碳代谢的影响尚不清楚.
- 在波动的氧化还原条件下,非生态驱动因素和微生物反应需要进一步研究.
研究的目的:
- 阐明氧化还原振荡与微生物碳利用效率 (CUE) 之间的机械联系.
- 研究铁循环和有机物转化如何受到氧化还原振荡的影响.
- 了解微生物群落和在氧化还原振荡条件下的代谢转变.
主要方法:
- 控制的化实验模拟氧化还原振荡.
- 对铁物种和无形铁池的分析.
- 矿物相关有机碳 (MAOC) 的量化及其生物降解性.
- 微生物群落和代谢产物的元基因组和代谢组分析.
- 测量基 (•OH) 的产生.
主要成果:
- 氧化还原振荡显著降低了微生物CUE,导致与静态条件相比碳损失增加.
- 在氧化还原振荡下铁循环减少无形Fe,释放可生物降解的MAOC并通过OH去聚合芳香物质.
- 甲基因组和代谢组数据显示了微生物群落和代谢物概况的显著变化.
- 微生物的代谢途径,包括酸途径和TCA循环,被激活用于基质矿化.
结论:
- 确定了一种结合的非生物-生物"燃烧和燃烧"机制,由铁循环和微生物呼吸驱动.
- 反氧振荡区作为重要的碳泄漏热点,影响陆地碳汇.
- 了解这些机制对于预测不断变化的环境中的碳动态至关重要.
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