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Microbial nitrification in throughfall of a Japanese cedar associated with archaea from the tree canopy

机译:与树冠古生菌相关的日本雪松穿透物中的微生物硝化作用

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摘要

To investigate the nitrification potential of phyllospheric microbes, we incubated throughfall samples collected under the canopies of Japanese cedar (Cryptomeria japonica) and analyzed the transformation of inorganic nitrogen in the samples. Nitrate concentration increased in the unfiltered throughfall after 4 weeks of incubation, but remained nearly constant in the filtered samples (pore size: 0.2 and 0.4 µm). In the unfiltered samples, δ18O and δ15N values of nitrate decreased during incubation. In addition, archaeal ammonia monooxygenase subunit A (amoA) genes, which participate in the oxidation of ammonia, were found in the throughfall samples, although betaproteobacterial amoA genes were not detected. The amoA genes recovered from the leaf surface of C. japonica were also from archaea. Conversely, nitrate production, decreased isotope ratios of nitrate, and the presence of amoA genes was not observed in rainfall samples collected from an open area. Thus, the microbial nitrification that occurred in the incubated throughfall is likely due to ammonia-oxidizing archaea that were washed off the tree canopy by precipitation.
机译:为了研究叶际微生物的硝化潜力,我们温育了在日本雪松(Cryptomeria japonica)冠层下收集的穿透样品,并分析了样品中无机氮的转化。孵育4周后,未经过滤的穿透物中的硝酸盐浓度增加,但在过滤后的样品中硝酸盐浓度几乎保持恒定(孔径:0.2和0.4μm)。在未过滤的样品中,硝酸盐的δ 18 O和δ 15 N值在培养期间降低。此外,尽管未检测到β变形杆菌的amoA基因,但在穿透样品中发现了参与氨氧化的古细菌氨单加氧酶亚基A(amoA)基因。从粳稻叶片表面回收的amoA基因也来自古细菌。相反,从空旷地区收集的降雨样品中未观察到硝酸盐的产生,硝酸盐同位素比的降低以及amoA基因的存在。因此,在温育穿透过程中发生的微生物硝化作用可能是由于氨氧化古细菌被沉淀物从树冠上冲洗掉了。

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