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High Prevalence of Gammaproteobacteria in the Sediments of Admiralty Bay and North Bransfield Basin Northwestern Antarctic Peninsula

机译:南极半岛西北​​部金钟湾和北布朗斯菲尔德盆地沉积物中γ-变形杆菌的高发生率

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摘要

Microorganisms dominate most Antarctic marine ecosystems, in terms of biomass and taxonomic diversity, and play crucial role in ecosystem functioning due to their high metabolic plasticity. Admiralty Bay is the largest bay on King George Island (South Shetland Islands, Antarctic Peninsula) and a combination of hydro-oceanographic characteristics (bathymetry, sea ice and glacier melting, seasonal entrance of water masses, turbidity, vertical fluxes) create conditions favoring organic carbon deposition on the seafloor and microbial activities. We sampled surface sediments from 15 sites across Admiralty Bay (100–502 m total depth) and the adjacent North Bransfield Basin (693–1147 m), and used the amplicon 454-sequencing of 16S rRNA gene tags to compare the bacterial composition, diversity, and microbial community structure across environmental parameters (sediment grain size, pigments and organic nutrients) between the two areas. Marine sediments had a high abundance of heterotrophic Gammaproteobacteria (92.4% and 83.8% inside and outside the bay, respectively), followed by Alphaproteobacteria (2.5 and 5.5%), Firmicutes (1.5 and 1.6%), Bacteroidetes (1.1 and 1.7%), Deltaproteobacteria (0.8 and 2.5%) and Actinobacteria (0.7 and 1.3%). Differences in alpha-diversity and bacterial community structure were found between the two areas, reflecting the physical and chemical differences in the sediments, and the organic matter input.
机译:就生物量和生物分类多样性而言,微生物在大多数南极海洋生态系统中占主导地位,并因其高代谢可塑性而在生态系统功能中发挥关键作用。金钟湾是乔治国王岛(南设得兰群岛,南极半岛)上最大的海湾,水文海洋学特征(测深法,海冰和冰川融化,水团的季节性入口,浊度,垂直通量)共同创造了有利于有机物的条件碳沉积在海底和微生物活动上。我们从金钟湾(总深度为100–502 m)和相邻的北布朗斯菲尔德盆地(693–1147 m)的15个地点采样了表面沉积物,并使用16S rRNA基因标签的454扩增子序列比较了细菌组成,多样性,以及两个区域之间跨环境参数(沉积物粒度,色素和有机营养物)的微生物群落结构。海洋沉积物具有丰富的异养型γ-变形杆菌(分别在海湾​​内外分别为92.4%和83.8%),其次是α-变形细菌(2.5和5.5%),Firmicutes(1.5和1.6%),拟杆菌(1.1和1.7%), Deltaproteobacteria(0.8和2.5%)和放线菌(0.7和1.3%)。在这两个区域之间发现了阿尔法多样性和细菌群落结构的差异,这反映了沉积物的物理和化学差异以及有机物的输入。

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