Abstract

Microbial communities mediate the biogeochemical cycles that drive ecosystems, and it is important to understand how these communities are affected by changing environmental conditions, especially in complex coastal zones. As fresh and marine waters mix in estuaries and river plumes, the salinity, temperature, and nutrient gradients that are generated strongly influence bacterioplankton community structure, yet, a parallel change in functional diversity has not been described. Metagenomic and metatranscriptomic analyses were conducted on five water samples spanning the salinity gradient of the Columbia River coastal margin, including river, estuary, plume, and ocean, in August 2010. Samples were pre-filtered through 3 μm filters and collected on 0.2 μm filters, thus results were focused on changes among free-living microbial communities. Results from metagenomic 16S rRNA sequences showed taxonomically distinct bacterial communities in river, estuary, and coastal ocean. Despite the strong salinity gradient observed over sampling locations (0 to 33), the functional gene profiles in the metagenomes were very similar from river to ocean with an average similarity of 82%. The metatranscriptomes, however, had an average similarity of 31%. Although differences were few among the metagenomes, we observed a change from river to ocean in the abundance of genes encoding for catabolic pathways, osmoregulators, and metal transporters. Additionally, genes specifying both bacterial oxygenic and anoxygenic photosynthesis were abundant and expressed in the estuary and plume. Denitrification genes were found throughout the Columbia River coastal margin, and most highly expressed in the estuary. Across a river to ocean gradient, the free-living microbial community followed three different patterns of diversity: 1) the taxonomy of the community changed strongly with salinity, 2) metabolic potential was highly similar across samples, with few differences in functional gene abundance from river to ocean, and 3) gene expression was highly variable and generally was independent of changes in salinity.

Highlights

  • As fresh and marine waters mix in estuaries and river plumes, salinity, temperature, and nutrient gradients develop spatially from river to ocean

  • For the two plume samples, new plume refers to the lower salinity sample (15.4), while old plume refers to the higher salinity sample (25.4), where more mixing with ocean water occurred

  • We detected a few of the same functional differences among metagenomic samples, our results suggest that free-living microbial communities of this river-dominated coastal margin environment were functionally very similar from river to ocean based on genomic potential (Fig 3a, Bray Curtis similarity of 74–91% based on normalized abundance of Clusters of Orthologous Groups (COG) functions)

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Summary

Introduction

As fresh and marine waters mix in estuaries and river plumes, salinity, temperature, and nutrient gradients develop spatially from river to ocean. In a marine oxygen minimum zone, Stewart et al [10] compared metagenomic and metatranscriptomic data among samples collected across an oxygen gradient and observed differences in gene abundance and expression, as nitrogen cycling processes changed from oxidative to reductive and the community changed from nitrifying taxa to taxa associated with anammox and denitrification. These studies demonstrated the metabolic responsiveness of microbial communities to environmental gradients, and revealed potentially important ecological process and microbial community dynamics in biogeochemically active environments

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