在季节性淹水沉积物中增加的甲基产量:从DOM分子组成的洞察力
Xian Zhou1, Tianrong He1, Yongguang Yin2
1Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.
Journal of hazardous materials
|January 9, 2025
概括
由于独特的溶解有机物 (DOM) 质量,季节性洪水地区 (SIA) 显示出更高的甲基 (MeHg) 产量. 包括成分和结构在内的SIA DOM特征显著推动了沉积物中的MeHg合成.
科学领域:
- 环境化学环境化学
- 水生生态学 水生生态学
- 生物地质化学生物地质化学
背景情况:
- 季节性洪水地区 (SIA) 是水生生态系统中甲基 (MeHg) 生产的热点.
- 在SIA沉积物中溶解有机物 (DOM) 质量对MeHg生产的具体作用仍然不清楚.
- 了解这些因素对于管理湿地的污染至关重要.
研究的目的:
- 研究DOM在SIA沉积物的分子组成和结构特征.
- 为了确定SIA DOM质量对MeHg产量的影响.
- 阐明DOM属性与金属污染湿地中的MeHg合成之间的关系.
主要方法:
- 在金属污染的高原湿地实地采样,比较SIA和永久淹水地区 (PIA).
- 实验室微观宇宙实验以评估DOM生物降解性,吸附性和对Hg的结合亲和力.
- 通过Desulfomicrobium escambiense对MeHg合成的分析和使用部分最小平方路径建模 (PLS-PM) 的量化.
主要成果:
- 与PIA相比,SIA中的DOM表现出更高的体样分数,分子量和生物可用性,但较低的染色体DOM和蛋白质样分数.
- SIA DOM更容易生物降解,具有更高的Hg (II) 吸附能力和较低的结合亲和力.
- 与SIA DOM相比,MeHg合成高出了29.6倍,而DOM组成强烈影响了沉积物孔水中的MeHg水平.
结论:
- 在SIA沉积物中的DOM分子组成和结构是MeHg产量升高的关键驱动因素.
- 在SIA内部,DOM质量的适应性变化为MeHg合成创造了有利的条件.
- 这些发现为季节性淹水的水生系统中高MeHg水平提供了机械解释.
相关概念视频
Microbial Mats
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
Marine Microbial Ecology
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...


