微生物硫循环决定因素及其对环境的影响。

Chemosphere Pub Date : 2025-03-01 Epub Date: 2025-01-14 DOI:10.1016/j.chemosphere.2025.144084
Felicia Y L Liu, Lauren E Twible, Tara E Colenbrander Nelson, Kelly Whaley-Martin, Yunyun Yan, James L S Arrey, Lesley A Warren
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引用次数: 0

摘要

硫氧化细菌(SOB)在金属矿尾矿库(TI)内出现硫氧化中间体(SOI)化合物的过程中发挥着至关重要的作用,目前可用的非生物处理方法往往难以奏效。由于在处理后不慎排放 SOI 会导致受纳环境的酸化失控,因此,在这些相对缺乏研究的系统中阐明环境对 SOB 特性和硫循环的控制变得越来越重要。在此,通过在安大略省北部分层贱金属 TI 中进行三个夏季(2016 年、2017 年和 2021 年)的综合物理化学、地球化学和微生物现场与实验调查,结果确定了 SOB 群落分化和相关代谢途径发生的控制因素。SOB 群落和硫氧化途径的动态变化主要受[S2O32-]的驱动,并进一步受 pH 值、[O2]和电导率的影响。当[S2O32-]高于 0.03 mM 时,在 pH 值较低和电导率较高的条件下,观察到卤代硫杆菌属(Halothiobacillus spp.当[S2O32-]低于 0.03 mM 时,观察到 SOB 群体(Thiovirga 菌属、Thiobacillus 菌属和 Sediminibacterium 菌属)在较高 pH 值和较低电导率条件下共同占主导地位,这与 SOI 循环途径(不完全 Sox、rDSR、S4I)导致的 SOI 持久性有关。定向 SOB 富集培养证实了 S2O32- 的可用性在推动 SOB 群落变化方面的重要性,以及卤硫杆菌在高氧、高[S2O32-]条件下超越其他 SOB 的能力。利用文献数据,我们发现在更广泛的环境中也出现了与矿井透气层相关的 SOB 趋势,这表明在解释与 SOB 活动相关的结果时,它们具有更广泛的生态相关性。研究结果还为通过控制[S2O32-]、pH值和/或[O2]来改善硫相关风险的生物知情管理提供了新的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Microbial sulfur cycling determinants and implications for environmental impacts.

Sulfur-oxidizing bacteria (SOB) play a vital role in the occurrence of sulfur oxidation intermediate (SOI) compounds often recalcitrant to currently available, abiotic treatment within metal mine tailings impoundments (TI). As inadvertent SOI discharge post-treatment can lead to the uncontrolled acidification of receiving environments, it becomes increasingly important to elucidate the environmental controls on SOB identities and sulfur cycling within these relatively unstudied systems. Here, results identified controlling factors on SOB community differentiation and associated metabolic pathway occurrence through integrated physicochemical, geochemical, and microbial field and experimental investigation across three summers (2016, 2017, 2021) in a stratified Northern Ontario base metal TI. Dynamic shifts in SOB communities and sulfur oxidation pathways were primarily driven by [S2O32-] and further influenced by pH, [O2], and conductivity. At [S2O32-] above 0.03 mM, Halothiobacillus spp. was observed to dominate in lower pH, higher conductivity conditions where complete SOI oxidation, mediated through the complete Sox pathway, is suggested to reduced [SOI] in treated discharge waters. At [S2O32-] below 0.03 mM, an SOB assemblage (Thiovirga spp., Thiobacillus spp., and Sediminibacterium spp.) was observed to collectively dominate under higher pH and lower conductivity, associated with SOI persistence due to SOI recycling pathways (incomplete Sox, rDSR, S4I). Targeted SOB enrichment cultures confirmed the importance of S2O32- availability in driving SOB community shifts and the capability of Halothiobacillus to outcompete other SOB under oxygenated, high [S2O32-] conditions. Trends observed here for mine TI associated SOB were found to also occur across a broader suite of contexts using literature data, indicating their wider ecological relevance in interpreting outcomes associated with SOB activity. Results also provide new insights into improved, biologically informed management of sulfur associated risks with potential SOB manipulation through [S2O32-], pH, and/or [O2] controls.

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