微生物多面手和溶解有机质组分在长江重金属含量调节中的作用

IF 11.3
Jiayuan Liu, Fude Liu, Yongjiu Cai, Chen Cheng, Zhirui Qin, Xiaolong Wang, Hui Zou, Tao Feng, Kai Peng
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引用次数: 0

摘要

大尺度河流重金属固液分异是河流生态风险评价的重要内容。然而,微生物群落(通才vs专才)和溶解有机物(DOM)组成在调节HMs动态中的作用尚不清楚。通过对长江流域77个水生样点(>1000 km)的调查,分析了水体微生物的分布和DOM组成,并阐明了微生物多能手驱动的水体微生物固液分配机制。HMs主要来源于自然资源,人为影响有限。水体和沉积物中细菌和真核生物的群落结构、多样性和代谢特征存在显著差异。细菌专门型和真核通才型在各自的群落形成中占主导地位。从沉积物到水体,细菌和真核生物代谢丰度的变化是HMs动态和DOM组成的关键驱动因素,不同的类群通过不同的途径影响HMs分布。细菌专家通过蛋白质样物质的中介间接促进HMs在沉积物中的保留。相比之下,真核生物的通才直接驱使HMs迁移到水中。虽然水体的生态风险相对较低,但大多数有机污染物仍存在从沉积物向水体迁移的风险,特别是As、Cd和Hg。本研究强调了微生物和DOM在调节有机污染物动态中的关键作用,促进了对河流有机污染物命运的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Roles of microbial generalists-specialists and dissolved organic matter components in regulating heavy metal(loid)s occurrence in the Yangtze River.

Heavy metal(loid)s (HMs) solid-liquid partitioning is crucial for ecological risk assessment in large-scale rivers. However, the roles of microbial communities (generalists vs. specialists) and dissolved organic matter (DOM) composition in regulating HMs dynamics remain unclear. We investigated 77 aquatic sites across the Yangtze River (>1000 km), analyzed HMs distributions and DOM composition, as well as elucidated the mechanisms of HMs solid-liquid partitioning driven by microbial generalist-specialist. HMs primarily originated from natural sources, with limited anthropogenic influence. Community structures, diversity, and metabolic characteristics of bacteria and eukaryotes differed substantially between water and sediments. Bacterial specialists and eukaryotic generalists dominated their respective community formation. From sediments to water, changes in metabolic abundance of bacteria and eukaryotes are key drivers of HMs dynamics and DOM composition, and different taxa influence HMs distribution via distinct pathways. Bacterial specialists indirectly promote HMs retention in sediments through the mediation of protein-like substances. In contrast, eukaryotic generalists directly drive HMs migration into water. Although ecological risks in water were relatively low, most HMs still pose a migration risk from sediments to water, especially As, Cd, and Hg. This study highlights the key roles of microbes and DOM in regulating HMs dynamics, advancing riverine HMs fate understanding.

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