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Influence of rewetting on microbial communities involved in nitrification and denitrification in a grassland soil after a prolonged drought period

机译:延长干旱期后,重新润湿对草地土壤中硝化和反硝化的影响

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The frequency of extreme drought and heavy rain events during the vegetation period will increase in Central Europe according to future climate change scenarios, which will affect the functioning of terrestrial ecosystems in multiple ways. In this study, we simulated an extreme drought event (40 days) at two different vegetation periods (spring and summer) to investigate season-related effects of drought and subsequent rewetting on nitrifiers and denitrifiers in a grassland soil. Abundance of the microbial groups of interest was assessed by quantification of functional genes (amoA, nirSirK and nosZ) via quantitative real-time PCR. Additionally, the diversity of ammonia-oxidizing archaea was determined based on fingerprinting of the archaeal amoA gene. Overall, the different time points of simulated drought and rewetting strongly influenced the obtained response pattern of microbial communities involved in N turnover as well as soil ammonium and nitrate dynamics. In spring, gene abundance of nirS was irreversible reduced after drought whereas nirK and nosZ remained unaffected. Furthermore, community composition of ammonia-oxidizing archaea was altered by subsequent rewetting although amoA gene abundance remained constant. In contrast, no drought/rewetting effects on functional gene abundance or diversity pattern of nitrifying archaea were observed in summer. Our results showed (I) high seasonal dependency of microbial community responses to extreme events, indicating a strong influence of plant-derived factors like vegetation stage and plant community composition and consequently close plant-microbe interactions and (II) remarkable resistance and/or resilience of functional microbial groups involved in nitrogen cycling to extreme weather events what might indicate that microbes in a silty soil are better adapted to stress situations as expected.
机译:根据未来的气候变化情景,植被期间,植被期间的极端干旱和大雨事件的频率将在多种方面影响陆地生态系统的运作。在这项研究中,我们在两种不同的植被期(春夏)模拟了极端干旱事件(40天),以研究干旱和随后在草地土壤中的硝化液和脱氮剂中的季节性对季节性效果和随后的效果。通过定量实时PCR定量功能基因(AmoA,Nirs / Nirk和NoSz)来评估​​微生物的微生物群体的丰富。另外,基于古氨基氨基基因的指纹识别确定氨氧化archaea的多样性。总体而言,模拟干旱和重载的不同时间点强烈影响了涉及N个营业额和土壤铵和硝酸盐动力学的微生物社区的所得反应模式。在春天,在干旱后,NIRS的基因丰富的鼻子是不可逆转的减少,而NIRK和NOSZ保持不受影响。此外,虽然AmoA基因丰富保持恒定,但随后的重入仍然是恒定的,因此通过随后的再润湿而改变了氨氧化古亚氏的群落组成。相比之下,夏季未观察到对官能基因丰度或硝化古亚硝化亚硝化的多样性模式的干旱/复合效应。我们的结果表明(i)微生物群落对极端事件的高季节性依赖性,表明植物阶段和植物群落组成等植物衍生因子的强烈影响,并因此关闭植物微生物相互作用和(ii)显着的抗性和/或弹性在氮气循环到极端天气事件中涉及的功能微生物组可能表明粉冻土壤中的微生物更好地适应压力情况。

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