National Institute for Agro-Environmental Sciences, Tsukuba, Ibaraki 305–8604, Japan.
Microbes Environ. 2011;26(3):248-53. doi: 10.1264/jsme2.me11127. Epub 2011 May 17.
Soil type is one of the key factors affecting soil microbial communities. With regard to ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB), however, it has not been determined how soil type affects their community size and soil nitrification activity. Here we quantitatively analyzed the ammonia monooxygenase genes (amoA) of these ammonia oxidizers in fields with three different soil types (Low-humic Andosol [LHA], Gray Lowland Soil [GLS], and Yellow Soil [YS]) under common cropping conditions, and assessed the relationships between soil nitrification activity and the abundance of each amoA. Nitrification activity of LHA was highest, followed by that of GLS and YS; this order was consistent with that for the abundance of AOB amoA. Abundance of AOB amoA showed temporal variation, which was similar to that observed in nitrification activity, and a strong relationship (adjusted R(2)=0.742) was observed between the abundance of AOB amoA and nitrification activity. Abundance of AOA amoA also exhibited a significant relationship (adjusted R(2)=0.228) with nitrification activity, although this relationship was much weaker. Our results indicate that soil type affects the community size of AOA and AOB and the resulting nitrification activity, and that AOB are major contributors to nitrification in soils, while AOA are partially responsible.
土壤类型是影响土壤微生物群落的关键因素之一。然而,关于氨氧化古菌(AOA)和氨氧化细菌(AOB),土壤类型如何影响它们的群落大小和土壤硝化活性还没有确定。在这里,我们在常见的种植条件下,定量分析了三种不同土壤类型(低腐殖质火山灰土[LHA]、灰色低地土壤[GLS]和黄壤[YS])下农田中这些氨氧化菌的氨单加氧酶基因(amoA),并评估了土壤硝化活性与每个 amoA 丰度之间的关系。LHA 的硝化活性最高,其次是 GLS 和 YS;这一顺序与 AOB amoA 的丰度一致。AOB amoA 的丰度表现出时间变化,与硝化活性的变化相似,并且在 AOB amoA 的丰度和硝化活性之间观察到很强的关系(调整后的 R(2)=0.742)。AOA amoA 的丰度也与硝化活性呈显著关系(调整后的 R(2)=0.228),尽管这种关系要弱得多。我们的结果表明,土壤类型影响 AOA 和 AOB 的群落大小以及由此产生的硝化活性,AOB 是土壤硝化作用的主要贡献者,而 AOA 则部分负责。