A highly pure biomethane stream (≈97% CH₄) was produced continuously under halo-alkaline conditions (pH > 9, 0.6 M Na⁺) from complex alkaline organic waste residue originating from biopolymer extraction from sewage sludge. During the proof-of-concept operation, the substrate was degraded with similar efficiency (40% of the volatile solids, VS) compared to neutral conditions (36% of the VS). Operational data was utilised in a technical evaluation to identify bottlenecks for full-scale implementation at an early stage of process development and for comparison to conventional biogas upgrading using pressure swing and membranes. Initially identified bottlenecks for alkaline fermentation were related to overcautious assumptions, while others could be technically solved. Alkaline fermentation offers an attractive method for supplying increasingly needed high-purity biomethane using various recalcitrant substrates that have undergone alkaline pre-treatment. This is more feasible than the conventional ex-situ biogas upgrading. Next, upscaling steps for alkaline fermentation should be pursued. Strategies for integrated CO₂ sequestration and nutrient recovery are outlined, which will offer additional benefits in the future.

The draft genome of a chemolithoautotrophic ammonia-oxidizing bacterium of the genus Nitrosomonas is reported. Nitrosomonas sp. strain ANs5, previously classified as a strain of N. halophila, is an alkali-tolerant ammonia-oxidizing bacterium isolated from the soda lakes of northeast Mongolia.

Intensive microbiology studies of the past several decades of soda lakes, uncovered a rich functional diversity of haloalkaliphilic microbes driving carbon, nitrogen and sulfur cycles in these unique double-extreme habitats. One of the unexpected finding was a discovery there of aerobic extremely halophilic cellulotrophic natronoarchaea. Yet, little is still known about the identity of the soda lake bacteria able to use native cellulose as growth substrate, except for a single case of an anaerobic clostridium. In this work we present results of phenotypic and functional genomic analysis of an anaerobic bacterium, strain ANBcel5^T, enriched from hypersaline Siberian soda lakes with amorphous cellulose as growth substrate. Phylogenetic analysis placed the isolate into the family Chitinispirillaceae in the phylum Fibrobacterota as a new genus and species lineage with the 16S rRNA gene identity and Relative Evolutionary Divergence (RED) to its only known species Chitinispirillum alkaliphilum ACht6–1^T of 95.2 % and 0.847, respectively. In contrast, despite obvious morphological resemblance to ACht6–1^T, strain ANBcel5^T is a narrow cellulose-utilizing fermentative anaerobe fermenting cellulose and cellobiose to acetate, H₂ and succinate. It is a moderately salt-tolerant obligate alkaliphile growing optimally at 0.6 M total Na⁺ as carbonates and pH 9.5. Functional genome analysis of the isolate revealed the presence of multiple genes encoding extracellular endocellulases from the GH families 5 and 9, three sodium-translocating membrane complexes and osmolytes Nε-acetyl-β-lysine and glycine betaine biosynthesis. The bacterium is proposed to be classified as Cellulosispirillum alkaliphilum gen. nov., sp. nov. (DSM 113825 = UQM 41584).

A variety of lakes located in the dry steppe area of southwestern Siberia are exposed to rapid climatic changes, including intra-century cycles with alternating dry and wet phases driven by solar activity. As a result, the salt lakes of that region experience significant fluctuations in water level and salinity, which have an essential impact on the indigenous microbial communities. But there are few microbiological studies that have analyzed this impact, despite its importance for understanding the functioning of regional water ecosystems. This work is a retrospective study aimed at analyzing how solar activity-related changes in hydrological regime affect phototrophic microbial communities using the example of the shallow soda lake Tanatar VI, located in the Kulunda steppe (Altai Region, Russia, southwestern Siberia). The main approach used in this study was the comparison of hydrochemical and microscopic data obtained during annual field work with satellite and solar activity data for the 12-year observation period (2011–2022). The occurrence of 33 morphotypes of cyanobacteria, two key morphotypes of chlorophytes, and four morphotypes of anoxygenic phototrophic bacteria was analyzed due to their easily recognizable morphology. During the study period, the lake surface changed threefold and the salinity changed by more than an order of magnitude, which strongly correlated with the phases of the solar activity cycles. The periods of high (2011–2014; 100–250 g/L), medium (2015–2016; 60 g/L), extremely low (2017–2020; 13–16 g/L), and low (2021–2022; 23–34 g/L) salinity with unique biodiversity of phototrophic communities were distinguished. This study shows that solar activity cycles determine the dynamics of the total salinity of a southwestern Siberian soda lake, which in turn determines the communities and microorganisms that will occur in the lake, ultimately leading to cyclical changes in alternative states of the ecosystem (dynamic stability).