Wang Yanan, Ke Xiubin, Wu Liqin, Lu Yahai
College of Resources and Environmental Sciences, China Agricultural University, Beijing 100094, China.
Syst Appl Microbiol. 2009 Feb;32(1):27-36. doi: 10.1016/j.syapm.2008.09.007. Epub 2008 Dec 16.
Little information is available on the ecology of ammonia-oxidizing bacteria (AOB) and archaea (AOA) in flooded rice soils. Consequently, a microcosm experiment was conducted to determine the effect of nitrogen fertilizer on the composition of AOB and AOA communities in rice soil by using molecular analyses of ammonia monooxygenase gene (amoA) fragments. Experimental treatments included three levels of N (urea) fertilizer, i.e. 50, 100 and 150 mgNkg(-1) soil. Soil samples were operationally divided into four fractions: surface soil, bulk soil deep layer, rhizosphere and washed root material. NH(4)(+)-N was the dominant form of N in soil porewater and increased with N fertilization. Cloning and sequencing of amoA gene fragments showed that the AOB community in the rice soil consisted of three major groups, i.e. Nitrosomonas communis cluster, Nitrosospira cluster 3a and cluster 3b. The sequences related to Nitrosomonas were predominant. There was a clear effect of N fertilizer and soil depth on AOB community composition based on terminal restriction fragment length polymorphism fingerprinting. Nitrosomonas appeared to be more abundant in the potentially oxic or micro-oxic fractions, including surface soil, rhizosphere and washed root material, than the deep layer of anoxic bulk soil. Furthermore, Nitrosomonas increased relatively in the partially oxic fractions and that of Nitrosospira decreased with the increasing application of N fertilizer. However, AOA community composition remained unchanged according to the denaturing gradient gel electrophoresis analyses.
关于淹水稻田土壤中氨氧化细菌(AOB)和古菌(AOA)的生态学信息较少。因此,进行了一项微观实验,通过对氨单加氧酶基因(amoA)片段进行分子分析,来确定氮肥对稻田土壤中AOB和AOA群落组成的影响。实验处理包括三个氮肥(尿素)水平,即50、100和150 mgNkg(-1)土壤。土壤样本在操作上被分为四个部分:表层土壤、深层土壤、根际土壤和洗根物质。NH(4)(+)-N是土壤孔隙水中氮的主要形态,并随氮肥施用量增加而增加。amoA基因片段的克隆和测序表明,稻田土壤中的AOB群落由三个主要类群组成,即共同亚硝化单胞菌簇、亚硝化螺菌属3a簇和3b簇。与亚硝化单胞菌相关的序列占主导地位。基于末端限制性片段长度多态性指纹图谱分析,氮肥和土壤深度对AOB群落组成有明显影响。亚硝化单胞菌在潜在有氧或微氧部分(包括表层土壤、根际土壤和洗根物质)似乎比深层缺氧的大块土壤中更为丰富。此外,随着氮肥施用量的增加,部分有氧部分的亚硝化单胞菌相对增加,而亚硝化螺菌属则减少。然而,根据变性梯度凝胶电泳分析,AOA群落组成保持不变。