Biology subjects

Tveit, A. T.

Publications and source records attributed to Tveit, A. T..

4 recordsLinked to original sources

bioRxiv2026

A national baseline for methane sink habitats and methanotroph diversity

Methane emissions account for nearly a third of the Earths effective radiative forcing, with methanotrophs playing a critical role in mitigating emissions by oxidising methane in diverse environments1. Despite their ecological importance, methanotrophic diversity and environmental distribution remain incompletely characterised due to cultivation challenges, incomplete or low-quality metagenome-assembled genomes, and limited taxonomic resolution in marker gene surveys. Here, we present a national study of the biogeography of novel and known methanotrophs across Denmarks major natural, urban and agricultural habitats, using genome-resolved classification of 10,683 metagenomes2 and 102 new methanotrophic species3. By linking metabolic potential to habitat-specific distributions, we reveal uncharacterised methanotrophs as dominant in natural ecosystems. These findings provide a comprehensive baseline of methanotroph diversity, reveal clear contrasts between natural and disturbed habitats, and highlight candidate species and habitats for future methane-mitigation strategies.

microbiology↗

bioRxiv2025

Soil trace gas oxidizers divergently respond to short- and long-term warming

The upland soil microbiome is dominated by aerobic bacteria that oxidize atmospheric trace gases, including CO, H2, and CH4. As a result, soils are the largest biological sink for these climate-active gases. Whether global warming will enhance or suppress these processes remains unclear. Here, we studied the warming responses of soil trace gas oxidizers by profiling natural geothermal gradients in a subarctic grassland with over 60 years of field warming at +6{degrees}C. We integrate field flux measurements, ex situ biogeochemical assays, metagenomics, and metatranscriptomics to determine ecosystem and cellular-level responses. Our results show that the oxidation of atmospheric CO and H2, but not CH4, increased with long-term warming due to higher cell numbers. However, at the cellular level, trace gas oxidizers, especially methanotrophs, tended to reduce gas consumption and transcription of gas-metabolizing enzymes in response to long-term warming. Our findings suggest that soils may remain a robust sink for trace gases despite lower per-cell activity. This work establishes a framework for interpreting the relationships between temperature and microbial trace gas oxidation on timescales relevant to Earths climate system.

microbiology↗

bioRxiv2022

Abrupt permafrost thaw triggers microbial bloom and increased activity of microbial predators

Permafrost soils store a substantial part of the global soil carbon and nitrogen. However global warming causes abrupt erosion and gradual thaw, which make these stocks vulnerable to microbial decomposition into greenhouse gases. Here, we investigated the microbial response to abrupt in situ permafrost thaw. We sequenced the total RNA of a 1 m deep soil core consisting of up to 26500-year-old permafrost material from an active abrupt erosion site. We analysed the microbial community in the active layer soil, the recently thawed, and the intact permafrost and found maximum RNA:DNA ratios indicating a microbial bloom in recently thawed permafrost. Several fast-growing prokaryotic taxa dominated thawed permafrost, including Sphingobacteriales, Burkholderiales, and Nitrosomonadales. Overall, the thaw state and soil moisture consistently explained changes in community composition, with especially the permafrost community being significantly distinct from thawed soils. Predation correlated with changes in prokaryotic composition. Bacterial grazers were dominated by Myxococcales and abundant in the active layer. In contrast, protozoa, especially Cercozoa and Ciliophora, doubled in relative abundance in thawed layers. Our findings highlight the ecological importance of a rapid development of microbial blooms as well as the successive predation as biological control mechanism in abruptly thawing permafrost. One sentence summaryUsing total RNA from an up to 26500-year-old abruptly eroding permafrost site in Greenland, we described a microbial bloom and its controls, including bacterial and microeukaryotic predators. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=146 SRC="FIGDIR/small/499897v2_ufig1.gif" ALT="Figure 1"> View larger version (51K): org.highwire.dtl.DTLVardef@10ab79eorg.highwire.dtl.DTLVardef@9d0146org.highwire.dtl.DTLVardef@1bec509org.highwire.dtl.DTLVardef@179f397_HPS_FORMAT_FIGEXP M_FIG C_FIG

microbiology↗

bioRxiv2018

Inter- and intra-domain functional redundancy in the rumen microbiome during plant biomass degradation

BackgroundRuminant livestock is a major source of the potent greenhouse gas methane (CH4), produced by the complex rumen microbiome. Using an integrated approach, combining quantitative metatranscriptomics with gas- and volatile fatty acid (VFA) profiling, we gained fundamental insights into temporal dynamics of the cow rumen microbiome during feed degradation.\n\nResultsThe microbiome composition was highly individual and remarkably stable within each cow, despite similar gas emission and VFA profiles between cows. Gene expression profiles revealed a fast microbial growth response to feeding, reflected by drastic increases in microbial biomass, CH4 emissions and VFA concentrations. Microbiome individuality was accompanied by high inter- and intra-domain functional redundancy among pro- and eukaryotic microbiome members in the key steps of anaerobic feed degradation. Methyl-reducing but not CO2-reducing methanogens were correlated with increased CH4 emissions during plant biomass degradation.\n\nConclusionsThe major response of the rumen microbiome to feed intake was a general growth of the whole community. The high functional redundancy of the cow-individual microbiomes was possibly linked to the robust performance of the anaerobic degradation process. Furthermore, the strong response of methylotrophic methanogens is suggesting that they might play a more important role in ruminant CH4 emissions than previously assumed, making them potential targets for CH4 mitigation strategies.

microbiology↗