Laboratory of Marine Microbiology, Department of Marine Ecosystem Dynamics, Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba, Japan.
National Institute of Polar Research, Tachikawa, Tokyo, Japan.
PLoS One. 2018 Aug 20;13(8):e0202636. doi: 10.1371/journal.pone.0202636. eCollection 2018.
Planktonic archaea are thought to play an important role in ammonia oxidation in marine environments. Data on the distribution, abundance, and diversity of ammonia oxidizers in the coastal sea-surface microlayer (SML) are lacking, despite previous reports of high abundance of Thaumarchaeota in the SML of estuaries and freshwater lakes. Here, we failed to detect the presence of ammonia-oxidizing bacteria in any of our samples taken from a semi-enclosed marine inlet in Japan. Therefore, we shifted our focus to examine the archaeal community composition as well as the Thaumarchaeota marine group I (MG-I) and ammonia monooxygenase subunit A (amoA) gene copy numbers and composition in the SML and corresponding underlying water (UW, 20 cm). amoA gene copy numbers obtained by quantitative PCR were consistent with the typical values observed in the surface waters of oceanic and coastal environments where nitrification activity has been detected, but the copy numbers were two- to three-fold less than those reported from the surface layers and UW of high mountain lakes. Both amoA and MG-I 16S rRNA gene copy numbers were significantly negatively correlated with chlorophyll-a and transparent exopolymer particle concentrations in the SML. Communities of archaea and ammonia-oxidizing archaea in SML samples collected during low wind conditions (≤5 m s-1) differed the most from those in UW samples, whereas the communities in SML samples collected during high wind conditions were similar to the UW communities. In the SML, low ratios of amoA to MG-I 16S rRNA genes were observed, implying that most of the SML Thaumarchaeota lacked amoA. To our knowledge, our results provide the first comparison of ammonia-oxidizing communities in the coastal SML with those in the UW.
浮游古菌被认为在海洋环境中的氨氧化过程中发挥着重要作用。尽管先前有报道称在河口和淡水湖泊的表 面 微 层 (SML) 中丰度很高,但有关沿海 SML 中氨氧化菌的分布、丰度和多样性的数据仍然缺乏。在这里,我们未能在从日本一个半封闭的海洋入口采集的任何样本中检测到氨氧化细菌的存在。因此,我们将重点转移到检查 SML 和相应的底层水(UW,20 cm)中的古菌群落组成以及 Thaumarchaeota 海洋组 I(MG-I)和氨单加氧酶亚基 A(amoA)基因拷贝数和组成。通过定量 PCR 获得的 amoA 基因拷贝数与在已经检测到硝化作用的海洋和沿海环境的表层水中观察到的典型值一致,但拷贝数比从高山湖泊的表层和 UW 报告的少两到三倍。amoA 和 MG-I 16S rRNA 基因拷贝数与 SML 中叶绿素-a 和透明外聚物颗粒浓度呈显著负相关。在低风速条件(≤5 m s-1)下采集的 SML 样本中,古菌和氨氧化古菌的群落与 UW 样本中的群落差异最大,而在高风速条件下采集的 SML 样本中的群落与 UW 群落相似。在 SML 中,观察到 amoA 与 MG-I 16S rRNA 基因的比例较低,这意味着大多数 SML Thaumarchaeota 缺乏 amoA。据我们所知,我们的研究结果首次比较了沿海 SML 中的氨氧化群落与 UW 中的氨氧化群落。