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首页> 外文期刊>Frontiers in Microbiology >Diazotroph Diversity in the Sea Ice, Melt Ponds, and Surface Waters of the Eurasian Basin of the Central Arctic Ocean
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Diazotroph Diversity in the Sea Ice, Melt Ponds, and Surface Waters of the Eurasian Basin of the Central Arctic Ocean

机译:在中央北冰洋的欧亚盆地的海冰,熔体池塘和地表水域的Diazotrophy多样性

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The Eurasian basin of the Central Arctic Ocean is nitrogen limited, but little is known about the presence and role of nitrogen-fixing bacteria. Recent studies have indicated the occurrence of diazotrophs in Arctic coastal waters potentially of riverine origin. Here, we investigated the presence of diazotrophs in ice and surface waters of the Central Arctic Ocean in the summer of 2012. We identified diverse communities of putative diazotrophs through targeted analysis of the nifH gene, which encodes the iron protein of the nitrogenase enzyme. We amplified 529 nifH sequences from 26 samples of Arctic melt ponds, sea ice and surface waters. These sequences resolved into 43 clusters at 92% amino acid sequence identity, most of which were non-cyanobacterial phylotypes from sea ice and water samples. One cyanobacterial phylotype related to Nodularia sp. was retrieved from sea ice, suggesting that this important functional group is rare in the Central Arctic Ocean. The diazotrophic community in sea-ice environments appear distinct from other cold-adapted diazotrophic communities, such as those present in the coastal Canadian Arctic, the Arctic tundra and glacial Antarctic lakes. Molecular fingerprinting of nifH and the intergenic spacer region of the rRNA operon revealed differences between the communities from river-influenced Laptev Sea waters and those from ice-related environments pointing toward a marine origin for sea-ice diazotrophs. Our results provide the first record of diazotrophs in the Central Arctic and suggest that microbial nitrogen fixation may occur north of 77°N. To assess the significance of nitrogen fixation for the nitrogen budget of the Arctic Ocean and to identify the active nitrogen fixers, further biogeochemical and molecular biological studies are needed.
机译:中部北冰洋的欧亚流域是氮气限制,但对氮素固定细菌的存在和作用很少。最近的研究表明,北极沿海水域潜在潜在的河流起源的发生。在这里,我们在2012年夏天调查了中央北冰洋的冰和地表水中的重氮化存在。我们通过对NiFH基因的靶向分析确定推定的重氮化的多样化社区,其编码硝基酶的铁蛋白。我们从26个北极熔体池,海冰和表面水处理扩增了529个NiFH序列。这些序列在92%的氨基酸序列同一性中升定到43个簇中,其中大部分是来自海冰和水样的非蓝藻属植物。一种与Nodularia sp相关的一种蓝藻型。从海冰中取出,表明这一重要的功能群在中央北冰洋中很少见。海冰环境中的重氮营养群落出现在其他冷适应的真正营养社区中的不同,例如沿海加拿大北极,北极苔原和冰川南极湖泊的那些。 NiFH的分子指纹纹理和RRNA操纵子的非基准间隔区揭示了来自河流影响的Laptev海水的社区与指向海冰二眩晕的海洋起源的与冰相关环境的社区之间的差异。我们的结果提供了中枢性北极中的重氮化的第一条记录,并表明微生物氮固定可能在77°N以后发生。为了评估氮气预算的氮气预算的重要性,并鉴定活性氮固定剂,需要进一步的生物地球化学和分子生物学研究。

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