ArticleNature communications2023
Stabilization of mineral-associated organic carbon in Pleistocene permafrost.
Article in Nature communications, 2023. 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.
The trial behind it
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Who cites it
8 citing papers in PubMed, 47 citations in OpenAlex.
- Saline Permafrost and Cryopegs as Potentially Important Sources of COGlobal change biology · 2026Article
- Hump-Shaped Relationship Between Microbial Carbon Use-Efficiency and Soil Organic Carbon in Alpine Grasslands.Advanced science (Weinheim, Baden-Wurttemberg, Germany) · 2026Article
- Model substrate particles uncover dynamics of microbial communities associated with particulate organic matter decomposition in soil.ISME communications · 2026Article
- Geospatial patterns in terrestrial organic matter reactivity across four shelf seas spanning the Eurasian Arctic.Science advances · 2025Article
- Permafrost carbon cycle and its dynamics on the Tibetan Plateau.Science China. Life sciences · 2024Review
- Carbon Fate, Iron Dissolution, and Molecular Characterization of Dissolved Organic Matter in Thawed Yedoma Permafrost under Varying Redox Conditions.Environmental science & technology · 2024Article
- Mineral-mediated stability of organic carbon in soil and relevant interaction mechanisms.Eco-Environment & Health · 2024Review
- Article
Corrections and comments
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Authors and funding
10 authors at 6 institutions in 5 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Ice-rich Pleistocene-age permafrost is particularly vulnerable to rapid thaw, which may quickly expose a large pool of sedimentary organic matter (OM) to microbial degradation and lead to emissions of climate-sensitive greenhouse gases. Protective physico-chemical mechanisms may, however, restrict microbial accessibility and reduce OM decomposition; mechanisms that may be influenced by changing environmental conditions during sediment deposition. Here we study different OM fractions in Siberian permafrost deposited during colder and warmer periods of the past 55,000 years. Among known stabilization mechanisms, the occlusion of OM in aggregates is of minor importance, while 33-74% of the organic carbon is associated with small, <6.3 µm mineral particles. Preservation of carbon in mineral-associated OM is enhanced by reactive iron minerals particularly during cold and dry climate, reflected by low microbial CO
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Registered trials
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