CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway.
Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway.
Sci Rep. 2019 Jul 5;9(1):9725. doi: 10.1038/s41598-019-46209-5.
Sedimentary biofilms comprising microbial communities mediating the anaerobic oxidation of methane are rare. Here, we describe two biofilm communities discovered in sediment cores recovered from Arctic cold seep sites (gas hydrate pingos) in the north-western Barents Sea, characterized by steady methane fluxes. We found macroscopically visible biofilms in pockets in the sediment matrix at the depth of the sulphate-methane-transition zone. 16S rRNA gene surveys revealed that the microbial community in one of the two biofilms comprised exclusively of putative anaerobic methanotrophic archaea of which ANME-1 was the sole archaeal taxon. The bacterial community consisted of relatives of sulphate-reducing bacteria (SRB) belonging to uncultured Desulfobacteraceae clustering into SEEP-SRB1 (i.e. the typical SRB associated to ANME-1), and members of the atribacterial JS1 clade. Confocal laser scanning microscopy demonstrates that this biofilm is composed of multicellular strands and patches of ANME-1 that are loosely associated with SRB cells, but not tightly connected in aggregates. Our discovery of methanotrophic biofilms in sediment pockets closely associated with methane seeps constitutes a hitherto overlooked and potentially widespread sink for methane and sulphate in marine sediments.
由介导甲烷厌氧氧化的微生物群落组成的沉积生物膜很少见。在这里,我们描述了在巴伦支海西北部的北极冷渗流点(天然气水合物冰丘)中回收的沉积物岩心中发现的两个生物膜群落,这些群落具有稳定的甲烷通量。我们在硫酸盐-甲烷过渡带深度的沉积物基质中的口袋中发现了宏观可见的生物膜。16S rRNA 基因调查显示,两个生物膜之一中的微生物群落完全由假定的厌氧甲烷营养菌组成,其中 ANME-1 是唯一的古菌分类群。细菌群落由属于未培养脱硫杆菌科的硫酸盐还原菌(SRB)的亲缘关系组成,聚类为 SEEP-SRB1(即与 ANME-1 相关的典型 SRB)和 atribacterial JS1 分支的成员。共聚焦激光扫描显微镜表明,这种生物膜由 ANME-1 的多细胞链和斑块组成,与 SRB 细胞松散相关,但不紧密连接成聚集体。我们在与甲烷渗出物密切相关的沉积物口袋中发现的甲烷营养生物膜,构成了迄今为止被忽视的、海洋沉积物中甲烷和硫酸盐的潜在广泛汇。