In Arctic marine bacterial communities, members of the phylum Verrucomicrobia are consistently detected, although not typically abundant, in 16S rRNA gene clone libraries and pyrotag surveys of the marine water column and in sediments. In an Arctic fjord (Smeerenburgfjord) of Svalbard, members of the Verrucomicrobia, together with Flavobacteria and smaller proportions of Alpha-and Gammaproteobacteria, constituted the most frequently detected bacterioplankton community members in 16S rRNA gene-based clone library analyses of the water column. Parallel measurements in the water column of the activities of six endo-acting polysaccharide hydrolases showed that chondroitin sulfate, laminarin, and xylan hydrolysis accounted for most of the activity. Several Verrucomicrobia water column phylotypes were affiliated with previously sequenced, glycoside hydrolaserich genomes of individual Verrucomicrobia cells that bound fluorescently labeled laminarin and xylan and therefore constituted candidates for laminarin and xylan hydrolysis. In sediments, the bacterial community was dominated by different lineages of Verrucomicrobia, Bacteroidetes, and Proteobacteria but also included members of multiple phylum-level lineages not observed in the water column. This community hydrolyzed laminarin, xylan, chondroitin sulfate, and three additional polysaccharide substrates at high rates. Comparisons with data from the same fjord in the previous summer showed that the bacterial community in Smeerenburgfjord changed in composition, most conspicuously in the changing detection frequency of Verrucomicrobia in the water column. Nonetheless, in both years the community hydrolyzed the same polysaccharide substrates.A major fraction of heterotrophic activity in the ocean is carried out by marine microbial communities (1). These communities use substrates such as high-molecular-weight carbohydrates (polysaccharides), which constitute a large percentage of phytoplankton biomass, particulate organic matter, and dissolved organic matter (DOM) in the ocean (2-5) and therefore fuel a considerable proportion of heterotrophic activity. To initiate the degradation of complex organic matter, bacteria must initially hydrolyze high-molecular-weight substrates by using extracellular enzymes in order to yield substrates sufficiently small to be taken into the microbial cell for further processing (6).The substrate spectrum and the rates of polysaccharide-hydrolyzing extracellular enzymes produced by microbial communities vary by location and depth in the ocean (7-9, 83) and can change through processes such as aggregate formation (10). Bacterial groups differ in their enzymatic spectra, as shown through field studies (11, 12), as well as genomic and microbiological investigation (13-16). Microbial communities involved in polysaccharide degradation in the water column include heterotrophic Gammaproteobacteria, fast-growing opportunists that can adapt quickly to changing substrate availability (17) and that include isolates that grow on rich standard media (...