ArticleFrontiers in microbiology2021
Permafrost Active Layer Microbes From Ny Ålesund, Svalbard (79°N) Show Autotrophic and Heterotrophic Metabolisms With Diverse Carbon-Degrading Enzymes.
Article in Frontiers in microbiology, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
8 citing papers in PubMed, 16 citations in OpenAlex.
- Article
- Active layer and permafrost microbial community coalescence increases soil activity and diversity in mixed communities compared to permafrost alone.Frontiers in microbiology · 2025Article
- PRA Melting-ICE Project: Svalbard 2022 Expeditions Report.Open research Europe · 2024Article
- Exploring microbial diversity in Greenland Ice Sheet supraglacial habitats through culturing-dependent and -independent approaches.FEMS microbiology ecology · 2023Article
- Distinct taxonomic and functional profiles of high Arctic and alpine permafrost-affected soil microbiomes.Environmental microbiome · 2023Article
- Complex organic matter degradation by secondary consumers in chemolithoautotrophy-based subsurface geothermal ecosystems.PloS one · 2023Article
- Ruegeria alba sp. nov., Isolated from a Tidal Flat Sediment.Current microbiology · 2022Article
- Draft Genome Sequences of 10 Pseudomonas sp. Isolates from the Active Layer of Permafrost in Ny Ålesund, Svalbard, Norway.Microbiology resource announcements · 2022Article
Corrections and comments
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Authors and funding
10 authors at 3 institutions in 2 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The active layer of permafrost in Ny Ålesund, Svalbard (79°N) around the Bayelva River in the Leirhaugen glacier moraine is measured as a small net carbon sink at the brink of becoming a carbon source. In many permafrost-dominating ecosystems, microbes in the active layers have been shown to drive organic matter degradation and greenhouse gas production, creating positive feedback on climate change. However, the microbial metabolisms linking the environmental geochemical processes and the populations that perform them have not been fully characterized. In this paper, we present geochemical, enzymatic, and isotopic data paired with 10
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Registered trials
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