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Climate Change Induces Shifts in Abundance and Activity Pattern of Bacteria and Archaea Catalyzing Major Transformation Steps in Nitrogen Turnover in a Soil from a Mid-European Beech Forest

机译:气候变化导致中欧山毛榉森林土壤中氮和氮转化的主要转化步骤导致细菌和古细菌的丰度和活动方式发生转变。

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摘要

Ongoing climate change will lead to more extreme weather events, including severe drought periods and intense drying rewetting cycles. This will directly influence microbial nitrogen (N) turnover rates in soil by changing the water content and the oxygen partial pressure. Therefore, a space for time climate change experiment was conducted by transferring intact beech seedling-soil mesocosms from a northwest (NW) exposed site, representing today's climatic conditions, to a southwest (SW) exposed site, providing a model climate for future conditions with naturally occurring increased soil temperature (+0.8°C in average). In addition, severe drought and intense rainfall was simulated by a rainout shelter at SW and manual rewetting after 39 days drought, respectively. Soil samples were taken in June, at the end of the drought period (August), 24 and 72 hours after rewetting (August) and after a regeneration period of four weeks (September). To follow dynamics of bacterial and archaeal communities involved in N turnover, abundance and activity of nitrifiers, denitrifiers, N2-fixing microbes and N-mineralizers was analyzed based on marker genes and the related transcripts by qPCR from DNA and RNA directly extracted from soil. Abundance of the transcripts was reduced under climate change with most pronounced effects for denitrification. Our results revealed that already a transfer from NW to SW without further treatment resulted in decreased cnor and nosZ transcripts, encoding for nitric oxide reductase and nitrous oxide reductase, respectively, while nirK transcripts, encoding for nitrite reductase, remained unaffected. Severe drought additionally led to reduced nirK and cnor transcripts at SW. After rewetting, nirK transcripts increased rapidly at both sites, while cnor and nosZ transcripts increased only at NW. Our data indicate that the climate change influences activity pattern of microbial communities involved in denitrification processes to a different extend, which may impact emission rates of the greenhouse gas N2O.
机译:持续的气候变化将导致更多的极端天气事件,包括严重的干旱时期和剧烈的干湿循环。通过改变水含量和氧分压,这将直接影响土壤中微生物氮(N)的转化率。因此,通过将完整的山毛榉幼苗-土壤中观空间从代表当今气候条件的西北(NW)暴露地点转移到西南(SW)暴露地点,进行了时空气候变化实验,从而为未来的气候条件提供了模型。自然发生的土壤温度升高(平均+ 0.8°C)。此外,西南干旱的避雨棚和干旱39天后的人工重新润湿分别模拟了严重干旱和强降雨。在6月,干旱时期(8月),重新润湿(8月)后24和72小时以及再生期4周(9月)之后,采集了土壤样品。为了跟踪参与氮更新的细菌和古细菌群落的动态,根据标记基因和相关转录本,通过qPCR从直接从土壤中提取的DNA和RNA中,基于标记基因和相关转录本,分析了硝化剂,反硝化剂,固氮微生物和氮矿化剂的丰度和活性。在气候变化下,转录物的丰度降低,反硝化作用最为明显。我们的结果表明,未经进一步处理就已经从西北向西南转移,导致分别编码一氧化氮还原酶和一氧化二氮还原酶的cnor和nosZ转录物减少,而编码亚硝酸盐还原酶的nirK转录物仍然不受影响。严重的干旱还导致SW的nirK和cnor转录物减少。重新润湿后,nirK转录本在两个位点均迅速增加,而cnor和nosZ转录本仅在西北部增加。我们的数据表明,气候变化对反硝化过程中涉及的微生物群落活动模式的影响程度不同,这可能会影响温室气体N2O的排放率。

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