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Tuomela, N.

Publications and source records attributed to Tuomela, N..

3 recordsLinked to original sources

Ultra-small bacteria and their phages discovered through metagenomics in a sub-arctic degrading permafrost ecosystem

Patescibacteriota is a diverse bacterial phylum characterized by ultra-small cell size, streamlined genome, incomplete metabolism and episymbiotic lifestyle. While Patescibacteriota have been detected across a wide range of ecosystem types, their phages are not widely described. We utilized metagenomics to explore these less characterized parts of the microbiome in a sporadic permafrost ecosystem, with samples from palsa and peat soils, small ponds and streams. We retrieved 33 high-quality metagenome assembled genomes (MAGs) of Patescibacteriota, mainly from the classes Minisyncoccia and Saccharimonadia. Minisyncoccia was a dominant class in the thawing soils and thaw ponds, whereas the Saccharimonadia was more abundant in the frozen palsa soil layers. The distribution of the Patescibacteria classes was also reflected in their metabolic potential. For example, gluconeogenesis pathway was complete only in MAGs from the class Minisyncoccia, whereas cytochrome o ubiquinol oxidase was mainly found from the MAGs of the class Saccharimondia. The viral community analysis yielded 16 354 viral operational taxonomic units (vOTUs), which represented mainly tailed dsDNA viruses from the class Caudoviricetes. Based on genome size, 16 vOTUs were qualified as jumbophages and one as a megaphage. Similar to the bacterial community, the viral community composition differed across sample types. The most common hosts for bacterial viruses were phyla Pseudomonadota, Acidobacteriota and Actinomycetota. A further 196 vOTUs were in silico linked to Patescibacteriota hosts. The Patescibacteriota phages were diverse, with only two vOTUs representing the same genus. The relative abundance of Patescibacteriota-associated phages was especially high in frozen palsa soils, largely following the same pattern of abundance as Patescibacteriota.

microbiology↗

Northern palsa and peat ecosystem microbiomes are potentially supported by hydrogen and carbon monoxide metabolism

Northern peatland and permafrost ecosystems are facing rapid changes, with increasing temperatures, permafrost thaw and shifts in hydrology. Characterizing microbial communities and metabolic potential from the soils and associated water bodies is crucial to understanding the changes in biogeochemical cycling in these ecosystems. For this, samples were collected and sequenced from subarctic palsa and peat soils, along with samples from associated thaw ponds and streams. Metagenomics was utilized in describing the microbiome and its metabolic potential in these environments. Palsa soils hosted microbial communities that were distinct from the peatland soils, ponds and stream waters. Soils and their adjacent ponds shared taxa, and peat soils and ponds also shared taxa with the streams, unlike palsa soils which were likely more hydrologically isolated. Based on metabolic marker gene ratio for denitrification [(nirS+nirK)/nosZ], palsa soils had the strongest potential to be a source of nitrous oxide (N2O) out of all the sample types. Marker genes for hydrogen gas (H2) and carbon monoxide (CO) utilization were abundant across soil environments and metagenome assembled genomes, suggesting that trace gas oxidation is likely one of the key energy sources for microbiomes. In the palsa ponds and peat soils pmoA, marker gene for methanotrophy, was the most abundant compared to the other sample types.

microbiology↗

Carbon and microbes from thawing palsas and peats do not reach a wider fluvial system

Climate change is altering the biogeochemical cycling of carbon and nutrients in the northern peatland and permafrost regions, which provide one of the largest terrestrial carbon storages. Lateral transfer of carbon needs to be more widely studied, especially in smaller streams and catchments, as they receive high loading of organic matter and are hotspots of carbon degradation. In this study we combined measurements of dissolved organic matter (DOM) quality and quantity with microbial community data from a small Arctic catchment. Our aim was to understand how the catchment is affected by two sub-catchments, degrading palsa permafrost mire and peatland thawing in spring. The small thaw ponds in the palsa mire were clearly distinct from the rest of the catchment and ponds in the peatland: Palsa ponds had higher DOM concentration, more aromatic DOM and distinctive microbial communities compared to the peatland ponds and the rest of the catchment. DOC export rates from the palsa and peat sites were comparable at the time of sampling, but local DOM processing was higher in the palsa site. We also detected high abundances of ultra-small Patescibacteria. Patescibacteria dominated the microbial community composition in all the sampled waters.

microbiology↗