The influence of soil pH on the diversity, abundance and transcriptional activity of ammonia oxidizing archaea and bacteria

古细菌 生物 温度梯度凝胶电泳 微观世界 氨单加氧酶 土壤微生物学 16S核糖体RNA 自养 土壤pH值 硝化作用 塔玛丘塔 广域古菌界 细菌 土壤水分 环境化学 生态学 化学 遗传学 氮气 有机化学
作者
Graeme W. Nicol,Sven Leininger,Christa Schleper,James I. Prosser
出处
期刊:Environmental Microbiology [Wiley]
卷期号:10 (11): 2966-2978 被引量:1223
标识
DOI:10.1111/j.1462-2920.2008.01701.x
摘要

Summary Autotrophic ammonia oxidation occurs in acid soils, even though laboratory cultures of isolated ammonia oxidizing bacteria fail to grow below neutral pH. To investigate whether archaea possessing ammonia monooxygenase genes were responsible for autotrophic nitrification in acid soils, the community structure and phylogeny of ammonia oxidizing bacteria and archaea were determined across a soil pH gradient (4.9–7.5) by amplifying 16S rRNA and amoA genes followed by denaturing gradient gel electrophoresis (DGGE) and sequence analysis. The structure of both communities changed with soil pH, with distinct populations in acid and neutral soils. Phylogenetic reconstructions of crenarchaeal 16S rRNA and amo A genes confirmed selection of distinct lineages within the pH gradient and high similarity in phylogenies indicated a high level of congruence between 16S rRNA and amoA genes. The abundance of archaeal and bacterial amoA gene copies and mRNA transcripts contrasted across the pH gradient. Archaeal amoA gene and transcript abundance decreased with increasing soil pH, while bacterial amoA gene abundance was generally lower and transcripts increased with increasing pH. Short‐term activity was investigated by DGGE analysis of gene transcripts in microcosms containing acidic or neutral soil or mixed soil with pH readjusted to that of native soils. Although mixed soil microcosms contained identical archaeal ammonia oxidizer communities, those adapted to acidic or neutral pH ranges showed greater relative activity at their native soil pH. Findings indicate that different bacterial and archaeal ammonia oxidizer phylotypes are selected in soils of different pH and that these differences in community structure and abundances are reflected in different contributions to ammonia oxidizer activity. They also suggest that both groups of ammonia oxidizers have distinct physiological characteristics and ecological niches, with consequences for nitrification in acid soils.
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