Biology subjects

Aalto, S. L.

Publications and source records attributed to Aalto, S. L..

3 recordsLinked to original sources

bioRxiv2024

Non-sulfate-based hydrogen sulfide production in engineered systems

Unwanted microbiological production of hydrogen sulfide (H2S) is a major challenge in engineered systems, such as sewage treatment plants, landfills, and aquaculture systems. While sulfur-rich amino acids and other substrates for non-sulfate-based H2S production are commonly present, the ability and potential of different microorganisms to perform sulfate-free H2S production has not yet been resolved. Here, we reveal the identity, activity, and genomic characteristics of bacteria that degrade cysteine to produce H2S in anaerobic enrichment bioreactors seeded with material from aquaculture systems. We compared them with canonical sulfate reducing bacteria and found that both sulfur sources led to microbial H2S production, yet with the process being more rapid with cysteine than with sulfate. 16S rRNA amplicon sequencing and metagenomic analysis showed four bacterial families, Dethiosulfatibacteraceae, Fusobacteriaceae, Vibrionaceae, and Desulfovibrionaceae to be centrally involved in non-sulfate H2S production. Metagenome/metatranscriptome assembled genomes uncovered the main cysteine-degradation pathway mediated by cysteine desulfidase cyuA and revealed that some bacteria potentially also use cysteine as a carbon source in sulfate-based H2S production.

microbiology↗

bioRxiv2021

Nitrate enhances anaerobic oxidation of methane in boreal lake sediments

The identity of electron acceptors in promoting anaerobic oxidation of methane (AOM) in the sediments of boreal lakes is currently unknown. Here, we studied the AOM rate of sediment slurries collected from three profundal stations of a nitrate-rich, oligo-mesotrophic, boreal lake (Lake Paajarvi, Finland), under varying nitrate concentrations using 13C-labelling. Furthermore, vertical profiles of the sediment and porewater geochemistry, and the microbial communities (16S rRNA gene and shotgun metagenomic sequencing) were analyzed. Despite geochemical data indicating that simultaneous consumption of nitrate and methane took place at the sediment layers chosen for incubations, AOM rate was not enhanced by nitrate amendments at either of the stations. AOM rate was much higher at the shallow Station 1 (0.9-6.8 nmol C cm-3 d-1) with high contents of labile phytoplankton-derived organic matter, than at the deeper stations, Station 2 (0-0.3 nmol C cm-3 d-1) and 3 (0-0.2 nmol C cm-3 d-1). Accordingly, a higher relative abundance of methanotrophic archaea (Candidatus Methanoperedens) and bacteria (Methylococcales) were observed in the layers chosen for incubations at Station 1 than at the other stations. Besides nitrate, the geochemical profiles indicated that AOM was potentially coupled with iron or sulfate reduction at all stations. Furthermore, putative nitrite-reducing methanotrophs (Ca. Methylomirabilis) were the most abundant methanotrophs above the incubation layer at Station 2 and 3, which suggests that nitrite reduction also plays a role in driving AOM in the study lake. We conclude that AOM is not uniquely coupled to nitrate reduction in sediments of nitrate-rich, oligo-mesotrophic, boreal lakes.

ecology↗

bioRxiv2018

Novel autotrophic organisms contribute significantly to the internal carbon cycling potential of a boreal lake

The authors declare no conflict of interest\n\nFunding sources: the Academy of Finland, Science for Life Laboratories, Tryggers Foundation, the Swedish Research Council VR and the Swedish Foundation for strategic research\n\nAbstractOxygen stratified lakes are typical for the boreal zone, and also a major source of greenhouse gas emissions in the region. Due to shallow light penetration, restricting the growth of phototrophic organisms, and large allochthonous organic carbon inputs from the catchment area, the lake metabolism is expected to be dominated by heterotrophic organisms. In this study we test this assumption and show that the potential for autotrophic carbon fixation and internal carbon cycling is high throughout the water column. Further, we show that during the summer stratification carbon fixation can exceed respiration in a boreal lake even below the euphotic zone. Metagenome assembled genomes and 16S profiling of a vertical transect of the lake revealed multiple organisms in oxygen depleted compartment belonging to novel or poorly characterized phyla. Many of these organisms were chemolithotrophic, deriving their energy from reactions related to sulfur, iron and nitrogen transformations. The community as well as the functions were stratified following the redox potentials. The autotrophic potential in the lake metagenome below the oxygenic zone was high, pointing towards a need for revising our concepts of internal carbon cycling in boreal lakes. Further, the importance of chemolithoautotrophy for the internal carbon cycling suggests that many predicted climate change associated changes in the physical properties of the lake, such as altered mixing patterns, likely have consequences for the whole lake metabolism even beyond the impact to the phototrophic community.\n\nImportanceAutotrophic organisms at the base of the food web are the only life form capable of turning inorganic carbon into organic form, facilitating the survival of all other organisms. In certain environments the autotrophic production is limited by environmental conditions and the food web is supported by carbon coming from outside the ecosystem. One such environment is stratified boreal lakes, which are one of the biggest sources of greenhouse gas emissions in the boreal region. Thus, carbon cycling in these habitats is of outmost importance for the future climate. Here we demonstrate a high potential for internal carbon cycling via phototrophic and novel chemolithotrophic organisms in the dark and anoxic layers of a boreal lake. Our results significantly increase our knowledge on the microbial communities and their metabolic potential in oxygen depleted freshwaters and help to understand and predict how climate change induced alterations could impact the lake carbon dynamics.

ecology↗