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Polar front associated variation in prokaryotic community structure in Arctic shelf seafloor

Permanent link
https://hdl.handle.net/10037/8764
DOI
https://doi.org/10.3389/fmicb.2015.00017
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Date
2015-01-23
Type
Journal article
Tidsskriftartikkel
Peer reviewed

Author
Nguyen, Tan Thi; Landfald, Bjarne
Abstract
Spatial variations in composition of marine microbial communities and its causes have largely been disclosed in studies comprising rather large environmental and spatial differences. In the present study, we explored if a moderate but temporally permanent climatic division within a contiguous arctic shelf seafloor was traceable in the diversity patterns of its bacterial and archaeal communities. Soft bottom sediment samples were collected at 10 geographical locations, spanning spatial distances of up to 640 km, transecting the oceanic polar front in the Barents Sea. The northern sampling sites were generally colder, less saline, shallower, and showed higher concentrations of freshly sedimented phytopigments compared to the southern study locations. Sampling sites depicted low variation in relative abundances of taxa at class level, with persistent numerical dominance by lineages of Gamma- and Deltaproteobacteria (57–66% of bacterial sequence reads). The Archaea, which constituted 0.7–1.8% of 16S rRNA gene copy numbers in the sediment, were overwhelmingly (85.8%) affiliated with the Thaumarchaeota. Beta-diversity analyses showed the environmental variations throughout the sampling range to have a stronger impact on the structuring of both the bacterial and archaeal communities than spatial effects. While bacterial communities were significantly influenced by the combined effect of several weakly selective environmental differences, including temperature, archaeal communities appeared to be more uniquely structured by the level of freshly sedimented phytopigments.
Description
Published version. Also available at http://dx.doi.org/10.3389/fmicb.2015.00017
Publisher
Frontiers
Citation
Frontiers in Microbiology 2015, 6:17
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