Jürgens, Klaus

Abstract Sandy sediments of the coastal ocean are generally not considered a habitat for highly active sulfate-reducing microorganisms (SRM) due to fluctuations in oxygen concentrations and carbon availability. This study investigated the taxonomic composition and gene expression patterns of sulfate-reducing communities in both sandy, organic-poor sediments and muddy, organic-rich sediments in the mesohaline southern Baltic Sea. Our results revealed that a novel order-level lineage within the class Thermodesulfovibrionia (phylum Nitrospirota), named Arenidesulfomonadales, contributed significantly to sulfate reduction in the sandy sediments and supported sulfate reduction rates similar to those in the organic-rich, muddy sediments. In the sands, Thermodesulfovibrionia effectively competed with Desulfobacterales, which strongly dominated the sulfate-reducing communities in the organic-rich sediments. Metatranscriptomic data revealed that Desulfobacterales functioned as typical secondary fermenters in both sediment types and expressed nearly complete sets of genes for the catabolism of fermentation products such as lactate, propionate, and butyrate. In contrast, the gene expression profile of Thermodesulfovibrionia suggests that hydrogenotrophic sulfate reduction, coupled with carbon fixation via the Wood–Ljungdahl pathway and a reduced capacity to oxidize organic compounds, was a competitive metabolic strategy enabling sulfate reduction to proceed independently of fermentation-derived carbon. Overall, our results suggest that overlooked lineages of SRM may contribute to higher levels of sulfate reduction than previously assumed in the extensive areas of permeable sediments of coastal and shelf seas.

Abstract Marine pelagic redoxclines are areas of enhanced biogeochemical cycling inhabited by distinct functional groups of prokaryotes. In this study, the diversity and abundance of archaeal and bacterial nitrifying populations throughout a pelagic redoxcline in the central Baltic Sea were examined using a suite of molecular methods. 16S rRNA/rRNA gene as well as bacterial and archaeal amoA mRNA/amoA gene fingerprints and clone libraries revealed that the putative nitrifying assemblages consisted solely of one crenarchaeotal subcluster, named GD2, which was closely related to Candidatus Nitrosopumilus maritimus. Neither distinct differences between transcript- and gene-based fingerprints nor pronounced differences in the crenarchaeotal composition throughout the whole redoxcline were detected. The abundance of this GD2 subgroup, as determined by the oligonucleotide probe Cren537 and the newly developed and more specific probe Cren679 showed that GD2 and total crenarchaeotal cell numbers were nearly identical throughout the redoxcline. The highest GD2 abundance (2.3 × 105 cells ml−1) occurred in the suboxic zone, accounting for around 26% of total prokaryotic cells. Below the chemocline, GD2 abundance was relatively stable (1.5–1.9 × 105 cells ml−1). Archaeal amoA expression was detected only in the putative nitrification zone and formed a narrow band in the suboxic layer, where ammonium, oxygen, nitrate, nitrite and phosphate concentrations were below 5 μmol l−1. To our knowledge this is the first study to show the dominance of only one crenarchaeotal nitrifying key cluster in a natural habitat. The metabolic properties and survival mechanisms present in this cluster inside and outside the nitrification zone remain to be determined.