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Grueterich, L.

Publications and source records attributed to Grueterich, L..

2 recordsLinked to original sources

Partitioning biota along the Elbe River estuary: where are the community transitions?

Estuarine zonation and community assemblages are frequently correlated with salinity, although the extent or nature of this correlation varies considerably among the published studies. While a smooth transition in biological communities is often conceptualized in association with estuarine fresh, brackish, and marine conditions, many studies have shown more distinct communities and the altogether absence of a brackish community. We explore these viewpoints in light of plant observations and soil and aquatic microbial analyses from permanent plots established on the Elbe River Estuary of northern Germany. Generally, two distinct communities were observed, a polyhaline assemblage towards the mouth of the system, and another that was associated with both the fresh and brackish mesohaline regimes further upriver. This was most pronounced among plant and soil bacteria communities, while aquatic 16S assemblages reflected little distinction at all. The proportion of marine classified taxa declined from the mouth to upriver and suggests that while the transition from marine to brackish or fresh vegetation falls within the sampled area, the same transition for microbial taxa could not be observed and may be further upriver. Thus, although we were able to identify two distinct communities, the "limit" of marine taxa was only evident for vegetation. While tidal and weather-related hydrology, as well as soil properties were also influential in distinguishing the communities, much of the variance remains unexplained. Further sampling, classification, and partitioning is necessary to determine the origin and/or autochthonous habitat, if any, for the Elbe River estuarine taxa. Geographic boundsbottom left: 53.556216{degrees}N, 8.824398{degrees}E top right: 53.917760 {degrees}N, 10.155669 {degrees}E

ecology↗

Environmental controls of dark CO2 fixation in wetland microbiomes

Rising atmospheric concentration of CO2 is a major concern to society due to its global warming potential. In soils, CO2 fixing microorganisms are preventing a part of the CO2 from entering the atmosphere. Yet, the pathways behind dark CO2 fixation are rarely studied in situ. Here we examined the environmental controls on the abundance and expression of key genes involved in microbial CO2 fixation in estuarine wetlands. A combined multi-omics approach incorporating metabarcoding, deep metagenomic and metatranscriptomic analyses confirmed that wetland microbiota harbor all six known CO2 fixation pathways and that these pathways are transcribed at high frequencies along several environmental gradients, albeit at different levels depending on the environmental niche. Notably, the transcription of the key genes for the reductive tricarboxylic acid cycle (rTCA) and the Calvin cycle were favored by low salinity and O2 rich niches high in organic matter, while the transcription of the key genes for the Wood-Ljungdahl pathway (WLP) and dicarboxylate/4-hydroxybutyrate cycle (DC/4-HB cycle) were favored by low O2 niches poor in organic matter. Taxonomic assignment of transcripts implied that dark CO2 fixation was mainly linked to few bacterial phyla, namely, Desulfobacterota, Gemmatimonadota, Methylomirabilota, Nitrospirota and Pseudomonadota.

microbiology↗