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Variation in Prokaryotic Community Composition as a Function of Resource Availability in Tidal Creek Sediments

机译:潮河沉积物中原核生物群落组成的变化与资源可利用性的关系

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摘要

In anaerobic coastal sediments, hydrolytic and/or fermentative bacteria degrade polymeric material and produce labile intermediates, which are used by terminal metabolizers to complete the conversion of organic material to CO2. We used molecular approaches to evaluate the response of two bacterial terminal metabolizer groups from a coastal tidal creek sediments, sulfate reducers and methanogens, to controlled changes in carbon resource supply. Tidal creek sediment bioreactors were established in April and August 2004. For each date, intact sediment sections were continuously supplied with flowthrough seawater that was either unamended or amended with the high-molecular-weight polysaccharide dextran. Biogeochemical data indicate that the activity of fermenting bacteria and the terminal metabolizers was limited by organic carbon supply during both experiments, with a significant increase in net volatile fatty acid (VFA) production and rates of sulfate reduction and methanogenesis following dextran addition. Community composition (measured by using terminal restriction fragment length polymorphism analysis, and functional gene [dsrA, mcrA] clone libraries) changed from April to August. However, community composition was not different between amended and unamended cores within each month, despite the change in resource level. Moreover, there was no relationship between community richness and evenness with resource level. This lack of variation in community composition with C addition could be attributed to the dynamic environment these sediment communities experience in situ. Fluctuations in VFA concentrations are most likely very high, so that the dominant bacterial species must be able to outcompete other species at both high and low resource levels.
机译:在厌氧的沿海沉积物中,水解细菌和/或发酵细菌会降解聚合材料并产生不稳定的中间体,终端代谢物会利用这些中间体完成有机物向二氧化碳的转化。我们使用分子方法评估了来自沿海潮汐小溪沉积物,硫酸盐还原剂和产甲烷菌的两个细菌末端代谢物组对碳资源供应受控变化的响应。于2004年4月和2004年8月建立了潮汐小河沉积生物反应器。在每个日期,完整的沉积物部分将不断供应未改性或已用高分子量多糖葡聚糖改性的流通海水。生物地球化学数据表明,在两个实验中,发酵细菌和终末代谢产物的活性都受到有机碳供应的限制,净挥发性脂肪酸(VFA)的产量以及添加右旋糖酐后硫酸盐还原和甲烷化的速率均显着增加。社区组成(通过使用末端限制性片段长度多态性分析和功能基因[dsrA,mcrA]克隆文库测量)从4月到8月。但是,尽管资源水平发生了变化,但每个月内经过修订和未经修订的核心之间的社区组成没有不同。而且,社区的丰富程度与资源水平的均匀性之间没有关系。碳的添加导致群落组成变化的缺乏可能归因于这些沉积物群落在原位经历的动态环境。 VFA浓度的波动很可能非常高,因此优势细菌种必须能够在资源水平高低两方面都胜过其他物种。

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