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首页> 外文期刊>Global change biology >Four years of experimental climate change modifies the microbial drivers of N2O fluxes in an upland grassland ecosystem.
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Four years of experimental climate change modifies the microbial drivers of N2O fluxes in an upland grassland ecosystem.

机译:四年的实验性气候变化改变了旱地草原生态系统中N 2 O通量的微生物驱动力。

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Emissions of the trace gas nitrous oxide (N2O) play an important role for the greenhouse effect and stratospheric ozone depletion, but the impacts of climate change on N2O fluxes and the underlying microbial drivers remain unclear. The aim of this study was to determine the effects of sustained climate change on field N2O fluxes and associated microbial enzymatic activities, microbial population abundance and community diversity in an extensively managed, upland grassland. We recorded N2O fluxes, nitrification and denitrification, microbial population size involved in these processes and community structure of nitrite reducers (nirK) in a grassland exposed for 4 years to elevated atmospheric CO2 (+200 ppm), elevated temperature (+3.5 degrees C) and reduction of summer precipitations (-20%) as part of a long-term, multifactor climate change experiment. Our results showed that both warming and simultaneous application of warming, summer drought and elevated CO2 had a positive effect on N2O fluxes, nitrification, N2O release by denitrification and the population size of N2O reducers and NH4 oxidizers. In situ N2O fluxes showed a stronger correlation with microbial population size under warmed conditions compared with the control site. Specific lineages of nirK denitrifier communities responded significantly to temperature. In addition, nirK community composition showed significant changes in response to drought. Path analysis explained more than 85% of in situ N2O fluxes variance by soil temperature, denitrification activity and specific denitrifying lineages. Overall, our study underlines that climate-induced changes in grassland N2O emissions reflect climate-induced changes in microbial community structure, which in turn modify microbial processes.
机译:微量气体一氧化二氮(N 2 O)的排放对于温室效应和平流层臭氧耗竭起着重要作用,但气候变化对N 2 O通量的影响潜在的微生物驱动因素仍然不清楚。这项研究的目的是确定持续气候变化对广泛管理的高地草原田间N 2 O通量及相关微生物酶活性,微生物种群数量和群落多样性的影响。我们记录了在暴露于4年的草地中,N 2 O通量,硝化和反硝化,这些过程涉及的微生物种群大小以及亚硝酸盐还原剂( nir K)的群落结构。作为长期的多因素气候变化实验的一部分,大气CO 2 升高(+200 ppm),温度升高(+3.5摄氏度)和夏季降水减少(-20%)。我们的结果表明,变暖和同时应用变暖,夏季干旱和CO 2 升高对N 2 O通量,硝化作用,N 2 <反硝化释放/ sub> O以及N 2 O还原剂和NH 4 氧化剂的种群规模。与温暖的条件下相比,在温暖条件下,原位N 2 O通量与微生物种群的相关性更强。 nir 反硝化菌群落的特定谱系对温度有显着响应。此外, nir K群落组成显示出对干旱的显着变化。路径分析解释了土壤温度,反硝化活性和特定反硝化谱系中超过80%的原位N 2 O通量变化。总体而言,我们的研究强调,气候引起的草原N 2 O排放量变化反映了气候引起的微生物群落结构变化,进而改变了微生物的过程。

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