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Osmotolerance is a driver of microbial carbon processes in the Elbe estuary.
Tobias-Hünefeldt SP, Woodhouse JN, Ruscheweyh H-J,
Sunagawa S, Russnak V, Streit WR, Grossart H-P
Estuaries are blue carbon loci, storing and exchanging carbon between aquatic, atmospheric, and terrestrial environments. Estuarine particles facilitate the transformation and transport of organic matter. The fate of particulate organic matter in estuaries is driven by structural changes in polymers that modify buoyancy, determining the proportions of sinking and suspended particles. In the open ocean and coastal ecosystems, the microbial composition and function of sinking and suspended particles differ, impacting carbon remineralization and sedimentation rates. We leverage 190 metagenomes and 73 metatranscriptomes to assess free-living, sinking, and suspended particle-associated microbial composition and function across the Elbe estuary. The salinity gradient in the Elbe estuary is the primary driver of microbiome composition and function. Transparent exopolymer particles (TEP) production was localized to freshwater, with seemingly no TEP-associated organisms detected above 20 practical salinity units (PSU). We observed differences in the function of free-living and particle-associated microbial communities, with diazotrophs enriched on particles. We observed that sinking particles may better support methanogenesis, and suspended particles showed signs of continued primary and secondary production. From this, we conclude that activities such as dredging, which resuspend sediment, will exacerbate carbon turnover and greenhouse gas emissions, and reduced dredging may lower greenhouse gas (GHG) emissions in the Elbe estuary. Many of these GHG linking processes are inhibited by salinity due to the osmosensitivity of methanogens and methanotrophs along the estuary. Changes in sea level and precipitation rates will likely directly interact with activities such as dredging, with as yet uncertain impacts on microbial carbon processing and storage.