Wu Yucheng, Ke Xiubin, Hernández Marcela, Wang Baozhan, Dumont Marc G, Jia Zhongjun, Conrad Ralf
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China.
Appl Environ Microbiol. 2013 May;79(9):3076-84. doi: 10.1128/AEM.00061-13. Epub 2013 Mar 1.
Both bacteria and archaea potentially contribute to ammonia oxidation, but their roles in freshwater sediments are still poorly understood. Seasonal differences in the relative activities of these groups might exist, since cultivated archaeal ammonia oxidizers have higher temperature optima than their bacterial counterparts. In this study, sediment collected from eutrophic freshwater Lake Taihu (China) was incubated at different temperatures (4°C, 15°C, 25°C, and 37°C) for up to 8 weeks. We examined the active bacterial and archaeal ammonia oxidizers in these sediment microcosms by using combined stable isotope probing (SIP) and molecular community analysis. The results showed that accumulation of nitrate in microcosms correlated negatively with temperature, although ammonium depletion was the same, which might have been related to enhanced activity of other nitrogen transformation processes. Incubation at different temperatures significantly changed the microbial community composition, as revealed by 454 pyrosequencing targeting bacterial 16S rRNA genes. After 8 weeks of incubation, [(13)C]bicarbonate labeling of bacterial amoA genes, which encode the ammonia monooxygenase subunit A, and an observed increase in copy numbers indicated the activity of ammonia-oxidizing bacteria in all microcosms. Nitrosomonas sp. strain Is79A3 and Nitrosomonas communis lineages dominated the heavy fraction of CsCl gradients at low and high temperatures, respectively, indicating a niche differentiation of active bacterial ammonia oxidizers along the temperature gradient. The (13)C labeling of ammonia-oxidizing archaea in microcosms incubated at 4 to 25°C was minor. In contrast, significant (13)C labeling of Nitrososphaera-like archaea and changes in the abundance and composition of archaeal amoA genes were observed at 37°C, implicating autotrophic growth of ammonia-oxidizing archaea under warmer conditions.
细菌和古菌都可能参与氨氧化过程,但其在淡水沉积物中的作用仍知之甚少。由于培养的古菌氨氧化菌比细菌氨氧化菌具有更高的最适温度,这些菌群的相对活性可能存在季节性差异。在本研究中,从中国富营养化淡水太湖采集的沉积物在不同温度(4°C、15°C、25°C和37°C)下培养长达8周。我们通过联合稳定同位素探测(SIP)和分子群落分析,研究了这些沉积物微宇宙中活跃的细菌和古菌氨氧化菌。结果表明,尽管铵消耗相同,但微宇宙中硝酸盐的积累与温度呈负相关,这可能与其他氮转化过程的活性增强有关。靶向细菌16S rRNA基因的454焦磷酸测序显示,在不同温度下培养显著改变了微生物群落组成。培养8周后,编码氨单加氧酶亚基A的细菌amoA基因的[(13)C]碳酸氢盐标记以及观察到的拷贝数增加表明所有微宇宙中氨氧化细菌都有活性。在低温和高温下,嗜硝化单胞菌属菌株Is79A3和共同嗜硝化单胞菌谱系分别在CsCl梯度的重相中占主导地位,表明活性细菌氨氧化菌沿温度梯度存在生态位分化。在4至25°C下培养的微宇宙中,氨氧化古菌的(13)C标记较少。相比之下,在37°C下观察到类似亚硝化球形菌属古菌的显著(13)C标记以及古菌amoA基因丰度和组成的变化,这意味着在较温暖的条件下氨氧化古菌的自养生长。