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温度和肥料对土壤氨氧化菌活性及群落结构的影响

Effects of temperature and fertilizer on activity and community structure of soil ammonia oxidizers.

作者信息

Avrahami Sharon, Liesack Werner, Conrad Ralf

机构信息

Max-Planck-Institut für terrestrische Mikrobiologie, Karl-von-Frisch-Str., 35043 Marburg, Germany.

出版信息

Environ Microbiol. 2003 Aug;5(8):691-705. doi: 10.1046/j.1462-2920.2003.00457.x.

Abstract

We investigated the effect of temperature on the activity of soil ammonia oxidizers caused by changes in the availability of ammonium and in the microbial community structure. Both short (5 days) and long (6.5, 16 and 20 weeks) incubation of an agricultural soil resulted in a decrease in ammonium concentration that was more pronounced at temperatures between 10 and 25 degrees C than at either 4 degrees C or 30-37 degrees C. Consistently, potential nitrification was higher between 10 and 25 degrees C than at either 4 degrees C or 37 degrees C. However, as long as ammonium was not limiting, release rates of N2O increased monotonously between 4 and 37 degrees C after short-term temperature adaptation, with nitrification accounting for about 35-50% of the N2O production between 4 and 25 degrees C. In order to see whether temperature may also affect the community structure of ammonia oxidizers, we studied moist soil during long incubation at low and high concentrations of commercial fertilizer. The soil was also incubated in buffered (pH 7) slurry amended with urea. Communities of ammonia oxidizers were assayed by denaturant gradient gel electrophoresis (DGGE) of the amoA gene coding for the alpha subunit of ammonia monooxygenase. We found that a polymerase chain reaction (PCR) system using a non-degenerated reverse primer (amoAR1) gave the best results. Community shifts occurred in all soil treatments after 16 weeks of incubation. The community shifts were obviously influenced by the different fertilizer treatments, indicating that ammonium was a selective factor for different ammonia oxidizer populations. Temperature was also a selective factor, in particular as community shifts were also observed in the soil slurries, in which ammonium concentrations and pH were better controlled. Cloning and sequencing of selected DGGE bands indicated that amoA sequences belonging to Nitrosospira cluster 1 were dominant at low temperatures (4-10 degrees C), but were absent after long incubation at low fertilizer treatment. Sequences of Nitrosospira cluster 9 could only be detected at low ammonium concentrations, whereas those of Nitrosospira cluster 3 were found at most ammonium concentrations and temperatures, although individual clones of this cluster exhibited trends with temperature. Obviously, ammonia oxidizers are able to adapt to soil conditions by changes in the community structure if sufficient time (several weeks) is available.

摘要

我们研究了温度对土壤氨氧化菌活性的影响,这种影响是由铵的有效性变化和微生物群落结构变化引起的。对一种农业土壤进行短期(5天)和长期(6.5、16和20周)培养,均导致铵浓度降低,在10至25摄氏度之间这种降低比在4摄氏度或30 - 37摄氏度时更为明显。相应地,10至25摄氏度之间的潜在硝化作用高于4摄氏度或37摄氏度时。然而,只要铵不成为限制因素,短期温度适应后,在4至37摄氏度之间N2O的释放速率单调增加,在4至25摄氏度之间硝化作用约占N2O产生量的35 - 50%。为了探究温度是否也会影响氨氧化菌的群落结构,我们在低浓度和高浓度商业肥料的长期培养过程中研究了湿润土壤。土壤也在添加尿素的缓冲(pH 7)泥浆中进行培养。通过对编码氨单加氧酶α亚基的amoA基因进行变性梯度凝胶电泳(DGGE)来分析氨氧化菌群落。我们发现使用非简并反向引物(amoAR1)的聚合酶链反应(PCR)系统效果最佳。培养16周后,所有土壤处理中都发生了群落变化。群落变化明显受到不同肥料处理的影响,表明铵是不同氨氧化菌种群的选择因素。温度也是一个选择因素,特别是因为在土壤泥浆中也观察到了群落变化,在土壤泥浆中铵浓度和pH得到了更好的控制。对选定DGGE条带的克隆和测序表明,属于亚硝化螺菌属簇1的amoA序列在低温(4 - 10摄氏度)下占主导,但在低肥料处理的长期培养后消失。亚硝化螺菌属簇9的序列仅在低铵浓度下能检测到,而亚硝化螺菌属簇3的序列在大多数铵浓度和温度下都能找到,尽管该簇的个别克隆呈现出随温度变化的趋势。显然,如果有足够的时间(几周),氨氧化菌能够通过群落结构的变化来适应土壤条件。

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