首页> 外文期刊>Frontiers in Marine Science >Methanotrophic community dynamics in a seasonally anoxic fjord: Saanich Inlet, British Columbia
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Methanotrophic community dynamics in a seasonally anoxic fjord: Saanich Inlet, British Columbia

机译:季节性缺氧峡湾的甲烷营养群落动态:不列颠哥伦比亚省萨尼奇湾

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Marine oxygen minimum zones (OMZs) play disproportionate roles in nutrient and climate active trace gas cycling including nitrous oxide and methane, in the ocean. OMZs are currently expanding due to climate change making it increasingly important to identify microbial controls on trace gas cycling at the individual, population and community levels. Here we present a two-year survey of the microbial community along seasonal redox gradients in Saanich Inlet focused on identifying microbial agents driving methane oxidation. Although methanotrophs were rare, we identified three uncultivated groups affiliated with particulate methane monooxygenase (pMMO) encoding phylogenetic groups (OPU), and methanotrophic symbionts as primary drivers of methane oxidation in Saanich Inlet. Distribution and activity patterns for these three groups were consistent with niche partitioning that became increasingly resolved during water column stratification. Moreover co-occurrence analysis combined with multi-level indicator species analysis revealed significant correlations between operational taxonomic units affiliated with Methylophaga, Methylophilales, SAR324, Verrucomicrobia, and Planctomycetes with OPUs and methanotrophic symbiont groups. Taken together these observations shed new light on the composition, dynamics, and potential interspecific interactions of microbes associated with CH4 cycling in the Saanich Inlet water column, provide a baseline for comparison between coastal and open ocean OMZs and support the potential role of OPUs, and methanotrophic symbiont groups as a widely distributed pelagic sink for CH4 along continental margins.
机译:海洋氧气最低限度区域(OMZs)在海洋中的养分和气候活跃的微量气体循环中(包括一氧化二氮和甲烷)起着不成比例的作用。由于气候变化,OMZ目前正在扩展,这使得在个人,人口和社区各级识别微量气体循环的微生物控制变得越来越重要。在此,我们对Saanich Inlet沿季节性氧化还原梯度对微生物群落进行了为期两年的调查,重点是确定驱动甲烷氧化的微生物。尽管甲烷营养菌很少见,但我们确定了三个未经培养的群体,这些群体与编码系统进化基团(OPU)的颗粒甲烷单加氧酶(pMMO)相关,而甲烷营养菌的共生体是Saanich Inlet中甲烷氧化的主要驱动力。这三组的分布和活动模式与在水柱分层过程中逐渐解决的生态位分配相一致。此外,共现分析与多级指标种类分析相结合,揭示了与甲基邻苯二甲酸酯,甲基邻苯二酚,SAR324,疣状微生物和浮游菌与OPU和甲烷营养共生群相关的可操作分类单位之间的显着相关性。这些观察结果共同为Saanich Inlet水柱中CH4循环相关微生物的组成,动力学和潜在的种间相互作用提供了新的思路,为沿海和开放海洋OMZ之间的比较提供了基线,并支持了OPU的潜在作用,以及甲烷营养共生体群是沿大陆边缘CH4广泛分布的上层水槽。

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