首页> 美国卫生研究院文献>Frontiers in Microbiology >Selective Pressure of Temperature on Competition and Cross-Feeding within Denitrifying and Fermentative Microbial Communities
【2h】

Selective Pressure of Temperature on Competition and Cross-Feeding within Denitrifying and Fermentative Microbial Communities

机译:温度对反硝化和发酵微生物群落竞争和交叉供料的选择性压力

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

In coastal marine sediments, denitrification and fermentation are important processes in the anaerobic decomposition of organic matter. Microbial communities performing these two processes were enriched from tidal marine sediments in replicated, long term chemostat incubations at 10 and 25°C. Whereas denitrification rates at 25°C were more or less stable over time, at 10°C denitrification activity was unstable and could only be sustained either by repeatedly increasing the amount of carbon substrates provided or by repeatedly decreasing the dilution rate. Metagenomic and transcriptomic sequencing was performed at different time points and provisional whole genome sequences (WGS) and gene activities of abundant populations were compared across incubations. These analyses suggested that a temperature of 10°C selected for populations related to Vibrionales/Photobacterium that contributed to both fermentation (via pyruvate/formate lyase) and nitrous oxide reduction. At 25°C, denitrifying populations affiliated with Rhodobacteraceae were more abundant. The latter performed complete denitrification, and may have used carbon substrates produced by fermentative populations (cross-feeding). Overall, our results suggest that a mixture of competition—for substrates between fermentative and denitrifying populations, and for electrons between both pathways active within a single population –, and cross feeding—between fermentative and denitrifying populations—controlled the overall rate of denitrification. Temperature was shown to have a strong selective effect, not only on the populations performing either process, but also on the nature of their ecological interactions. Future research will show whether these results can be extrapolated to the natural environment.
机译:在沿海海洋沉积物中,反硝化和发酵是有机物厌氧分解的重要过程。在10和25°C的重复长期化学恒温培养中,潮汐海洋沉积物中丰富了执行这两个过程的微生物群落。 25°C时的反硝化速率随时间变化大致稳定,而10°C时的反硝化活性则不稳定,并且只能通过反复增加所提供的碳底物量或通过反复降低稀释率来维持。在不同的时间点进行了元基因组和转录组测序,并比较了整个孵化过程中的临时全基因组序列(WGS)和丰富种群的基因活性。这些分析表明,与振动弧菌/光细菌有关的种群选择的温度为10°C,这有助于发酵(通过丙酮酸/甲酸酯裂解酶)和一氧化二氮的减少。在25°C时,与红细菌科相关的反硝化种群数量更多。后者进行了完全的反硝化作用,可能使用了由发酵菌群产生的碳底物(交叉进料)。总体而言,我们的结果表明,发酵和反硝化种群之间的底物竞争,以及单个种群中活跃的两种途径之间的电子竞争,以及发酵和反硝化种群之间的交叉进料竞争,共同控制了总体反硝化速率。事实证明,温度不仅对进行这两种过程的种群都有强烈的选择性作用,而且对它们的生态相互作用的性质也具有很强的选择性作用。未来的研究将显示这些结果是否可以推断到自然环境中。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号