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Ammonia-Oxidizing Archaea Show More Distinct Biogeographic Distribution Patterns than Ammonia-Oxidizing Bacteria across the Black Soil Zone of Northeast China

机译:在中国东北黑土区氨氧化古细菌比氨氧化细菌具有更明显的生物地理分布格局

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摘要

Black soils (Mollisols) of northeast China are highly productive and agriculturally important for food production. Ammonia-oxidizing microbes play an important role in N cycling in the black soils. However, the information related to the composition and distribution of ammonia-oxidizing microbes in the black soils has not yet been addressed. In this study, we used the amoA gene to quantify the abundance and community composition of ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) across the black soil zone. The amoA abundance of AOA was remarkably larger than that of AOB, with ratios of AOA/AOB in the range from 3.1 to 91.0 across all soil samples. The abundance of AOA amoA was positively correlated with total soil C content (p < 0.001) but not with soil pH (p > 0.05). In contrast, the abundance of AOB amoA positively correlated with soil pH (p = 0.009) but not with total soil C. Alpha diversity of AOA did not correlate with any soil parameter, however, alpha diversity of AOB was affected by multiple soil factors, such as soil pH, total P, N, and C, available K content, and soil water content. Canonical correspondence analysis indicated that the AOA community was mainly affected by the sampling latitude, followed by soil pH, total P and C; while the AOB community was mainly determined by soil pH, as well as total P, C and N, water content, and sampling latitude, which highlighted that the AOA community was more geographically distributed in the black soil zone of northeast China than AOB community. In addition, the pairwise analyses showed that the potential nitrification rate (PNR) was not correlated with alpha diversity but weakly positively with the abundance of the AOA community (p = 0.048), whereas PNR significantly correlated positively with the richness (p = 0.003), diversity (p = 0.001) and abundance (p < 0.001) of the AOB community, which suggested that AOB community might make a greater contribution to nitrification than AOA community in the black soils when ammonium is readily available.
机译:中国东北的黑土(高产土壤)生产力高,对农业生产具有重要的农业意义。氨氧化微生物在黑土的氮循环中起重要作用。但是,有关黑土壤中氨氧化微生物的组成和分布的信息尚未得到解决。在这项研究中,我们使用amoA基因来量化整个黑土区氨氧化古细菌(AOA)和氨氧化细菌(AOB)的丰度和群落组成。 AOA的amoA丰度明显大于AOB,在所有土壤样品中AOA / AOB的比率在3.1到91.0之间。 AOA amoA的丰度与土壤总C含量呈正相关(p <0.001),而与土壤pH却没有正相关(p> 0.05)。相比之下,AOB amoA的丰度与土壤pH呈正相关(p = 0.009),但与土壤总C呈正相关。AOA的α多样性与任何土壤参数均不相关,但是,AOB的α多样性受多种土壤因素影响,例如土壤的pH值,总磷,氮和碳,有效钾含量和土壤水分含量。典型的对应分析表明,AOA群落主要受采样纬度的影响,其次是土壤pH,总磷和碳。而AOB群落主要由土壤pH值,总磷,碳和氮,水分含量和采样纬度决定,这表明AOA群落比AOB群落在中国东北黑土区的地理分布更大。此外,成对分析显示,潜在硝化率(PNR)与α多样性无关,但与AOA群落的丰度呈弱正相关(p = 0.048),而PNR与丰富度呈显着正相关(p = 0.003) ,AOB群落的多样性(p = 0.001)和丰度(p <0.001),这表明在容易获得铵盐的情况下,黑土中AOB群落对硝化的贡献可能大于AOA群落。

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