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Ammonia-Oxidizing Archaea and Bacteria Differentially Contribute to Ammonia Oxidation in Sediments from Adjacent Waters of Rushan Bay China

机译:氨氧化古细菌和细菌在中国乳山湾附近水域沉积物中氨氧化中的差异作用

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摘要

Ammonia oxidation plays a significant role in the nitrogen cycle in marine sediments. Ammonia-oxidizing archaea (AOA) and bacteria (AOB) are the key contributors to ammonia oxidation, and their relative contribution to this process is one of the most important issues related to the nitrogen cycle in the ocean. In this study, the differential contributions of AOA and AOB to ammonia oxidation in surface sediments from adjacent waters of Rushan Bay were studied based on the ammonia monooxygenase (amoA) gene. Molecular biology techniques were used to analyze ammonia oxidizers’ community characteristics, and potential nitrification incubation was applied to understand the ammonia oxidizers’ community activity. The objective was to determine the community structure and activity of AOA and AOB in surface sediments from adjacent waters of Rushan Bay and to discuss the different contributions of AOA and AOB to ammonia oxidation during summer and winter seasons in the studied area. Pyrosequencing analysis revealed that the diversity of AOA was higher than that of AOB. The majority of AOA and AOB clustered into Nitrosopumilus and Nitrosospira, respectively, indicating that the Nitrosopumilus group and Nitrosospira groups may be more adaptable in studied sediments. The AOA community was closely correlated to temperature, salinity and ammonium concentration, whereas the AOB community showed a stronger correlation with temperature, chlorophyll-a content (chla) and nitrite concentration. qPCR results showed that both the abundance and the transcript abundance of AOA was consistently greater than that of AOB. AOA and AOB differentially contributed to ammonia oxidation in different seasons. AOB occupied the dominant position in mediating ammonia oxidation during summer, while AOA might play a dominant role in ammonia oxidation during winter.
机译:氨氧化在海洋沉积物中的氮循环中起着重要作用。氨氧化古细菌(AOA)和细菌(AOB)是氨氧化的关键因素,它们对这一过程的相对贡献是与海洋氮循环有关的最重要问题之一。本研究基于氨单加氧酶(amoA)基因研究了乳山湾邻近水域表层沉积物中AOA和AOB对氨氧化的不同贡献。分子生物学技术被用于分析氨氧化剂的群落特征,潜在的硝化温育被用于了解氨氧化剂的群落活动。目的是确定乳山湾相邻水域表层沉积物中AOA和AOB的群落结构和活性,并探讨研究区域夏季和冬季AOA和AOB对氨氧化的不同贡献。焦磷酸测序分析表明,AOA的多样性高于AOB。大部分的AOA和AOB分别聚集成于Nitrosopumilus和Nitrosospira中,这表明Nitrosopumilus组和Nitrosospira组可能更适合于研究的沉积物。 AOA群落与温度,盐度和铵盐浓度密切相关,而AOB群落与温度,叶绿素a含量(chla)和亚硝酸盐浓度表现出更强的相关性。 qPCR结果表明,AOA的丰度和转录本丰度始终大于AOB。 AOA和AOB在不同季节对氨氧化的贡献不同。在夏季,AOB在介导氨氧化中占据主导地位,而在冬季,AOA可能在氨氧化中发挥主导作用。

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