沉积物细菌群落结构和功能对C和Zn修正的响应:城市和非城市河流

S. Perryman, G. Rees, M. Grace
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引用次数: 10

摘要

城市化是河流流域重要的生态调节剂,显著改变了水体系统的C类型、浓度和重金属输入。C和重金属是微生物群落结构(种群动态)和功能(生理过程)的重要决定因素。理解景观尺度上的变化如何影响微观尺度上的关键营养转化过程(如反硝化)和C代谢(如甲烷生成),需要同时确定细菌群落的结构和功能响应。我们比较了添加C和Zn前后城市和非城市河流沉积物中总细菌(16S核糖体核糖核酸[rRNA]基因)和反硝化细菌(nosZ基因)群落结构。在含有水系沉积物的微生态系统中添加蛋白质C或叶片渗滤液C,分别使C含量增加~ 36和130 mg/L。在不添加锌(200 mg/kg)的情况下分别添加C。通过测定各中游群落顶空CO2、N2和CH4积累速率,测定群落功能变化与添加量同时变化。地点对总菌群和反硝化菌群结构的影响最大。添加C对总细菌群落结构的影响虽小但很显著,而对反硝化细菌群落结构没有影响。C富集导致群落功能发生显著而迅速的变化。非城市样地的产甲烷率显著高于城市样地,且受C型(显著站点× C相互作用)的显著影响。反硝化和CO2产量不受碳添加的影响,但在不同地点有所不同。添加Zn改变了总菌群结构,但没有改变反硝化菌群结构。锌对产甲烷速率有影响,但影响程度小于C型。在研究结束时,不同地点之间的群落结构仍然不同,尽管暴露在反映城市化河流条件的Zn浓度和模仿城市或非城市河流条件的C源。我们的研究支持了先前的观察结果,即微生物群落结构受到先前沉积物历史的强烈影响。更广泛的含义是,在我们的研究中,城市化等景观尺度变化改变了水系沉积物的其他物理和化学性质,这些性质比锌或C浓度更能影响群落结构。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sediment bacterial community structure and function in response to C and Zn amendments: urban and nonurban streams
Abstract Urbanization is an important ecological modifier of stream catchments and significantly alters C type and concentration and heavy metal input to aquatic systems. C and heavy metals are important determinants of microbial community structure (population dynamics) and function (physiological processes). Understanding how changes at the landscape scale affect key nutrient-transformation processes (e.g., denitrification) and C metabolism (e.g., methanogenesis) at the micro scale requires simultaneous determination of the structural and functional responses of bacterial communities. We compared total bacterial (16S ribosomal ribonucleic acid [rRNA] gene) and denitrifying bacterial (nosZ gene) community structures in sediments taken from an urban and a nonurban stream before and after C and Zn additions. Microcosms containing stream sediment were supplemented with either proteinaceous or leaf-leachate C, increasing the C content by ∼36 and 130 mg/L, respectively. C was added in the presence and absence of Zn addition (200 mg/kg). Changes in community function were determined simultaneously with additions by measuring the rates of CO2, N2, and CH4 accumulation in the headspace of each mesocosm. Site had the greatest effect on total and denitrifying bacterial community structures. Added C caused a small but significant change in total bacterial community structure, but did not change denitrifying bacterial community structure. C enrichment caused a significant and rapid change in community function. Rates of methanogenesis were significantly higher at the nonurban than at the urban site and were significantly affected by C type (significant site × C interaction). Denitrification and CO2 production were unaffected by C additions but differed between sites. Zn addition changed total bacterial community structure but not denitrifying bacterial community structure. Zn affected the rate of methanogenesis, but the effect size was less than for C type. Community structures remained different between sites at the end of the study despite exposure to Zn concentrations that reflected conditions in urbanized streams and C sources that mimicked those from urban or nonurban streams. Our study supports previous observations that microbial community structure is strongly influenced by prior sediment history. The broader implication is that landscape-scale changes like urbanization alter other physical and chemical properties of the stream sediment that influence community structure more than the Zn or C concentrations in our study.
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来源期刊
Journal of the North American Benthological Society
Journal of the North American Benthological Society 生物-海洋与淡水生物学
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