Department of Biology, Concordia University, Montreal, Quebec, Canada.
Department of Fisheries and Oceans, Bedford Institute of Oceanography, Dartmouth, Nova Scotia, Canada.
ISME J. 2014 Jun;8(6):1301-13. doi: 10.1038/ismej.2013.234. Epub 2014 Jan 9.
In this study, we used comparative metaproteomics to investigate the metabolic activity of microbial plankton inhabiting a seasonally hypoxic basin in the Northwest Atlantic Ocean (Bedford Basin). From winter to spring, we observed a seasonal increase in high-affinity membrane transport proteins involved in scavenging of organic substrates; Rhodobacterales transporters were strongly associated with the spring phytoplankton bloom, whereas SAR11 transporters were abundant in the underlying waters. A diverse array of transporters for organic compounds were similar to the SAR324 clade, revealing an active heterotrophic lifestyle in coastal waters. Proteins involved in methanol oxidation (from the OM43 clade) and carbon monoxide (from a wide variety of bacteria) were identified throughout Bedford Basin. Metabolic niche partitioning between the SUP05 and ARCTIC96BD-19 clades, which together comprise the Gamma-proteobacterial sulfur oxidizers group was apparent. ARCTIC96BD-19 proteins involved in the transport of organic compounds indicated that in productive coastal waters this lineage tends toward a heterotrophic metabolism. In contrast, the identification of sulfur oxidation proteins from SUP05 indicated the use of reduced sulfur as an energy source in hypoxic bottom water. We identified an abundance of Marine Group I Thaumarchaeota proteins in the hypoxic deep layer, including proteins for nitrification and carbon fixation. No transporters for organic compounds were detected among the thaumarchaeal proteins, suggesting a reliance on autotrophic carbon assimilation. In summary, our analyses revealed the spatiotemporal structure of numerous metabolic activities in the coastal ocean that are central to carbon, nitrogen and sulfur cycling in the sea.
在这项研究中,我们使用比较宏蛋白质组学来研究栖息在北大西洋(贝德福德盆地)季节性缺氧盆地中的微生物浮游生物的代谢活性。从冬季到春季,我们观察到参与有机底物掠夺的高亲和力膜转运蛋白的季节性增加;红杆菌门转运蛋白与春季浮游植物大量繁殖密切相关,而 SAR11 转运蛋白在底层水中含量丰富。一系列用于有机化合物的转运蛋白与 SAR324 进化枝相似,揭示了沿海水域中活跃的异养生活方式。参与甲醇氧化(来自 OM43 进化枝)和一氧化碳(来自多种细菌)的蛋白质在整个贝德福德盆地中都有发现。SUP05 和 ARCTIC96BD-19 进化枝(它们共同构成了γ-变形菌硫氧化菌群)之间的代谢生态位划分明显。参与有机化合物运输的 ARCTIC96BD-19 蛋白表明,在生产力高的沿海水域,该谱系倾向于异养代谢。相比之下,SUP05 中硫氧化蛋白的鉴定表明,在缺氧底层水中,还原硫被用作能源。我们在缺氧深层中发现了大量海洋 I 组古菌蛋白,包括硝化和碳固定蛋白。在古菌蛋白中未检测到有机化合物的转运蛋白,这表明它们依赖于自养碳同化。总之,我们的分析揭示了沿海海洋中许多代谢活动的时空结构,这些活动是海洋中碳、氮和硫循环的核心。