ArticleThe ISME journal2023
Rapid growth rate responses of terrestrial bacteria to field warming on the Antarctic Peninsula.
Article in The ISME journal, 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
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
8 citing papers in PubMed, 17 citations in OpenAlex.
- Soil microbial growth rate, trophic strategy, and the oligotroph-copiotroph continuum.Applied and environmental microbiology · 2026Article
- Seasonal thawing of high Arctic soils triggers selective microbial growth and predation.mSystems · 2026Article
- A Large Fraction of Soil Microbial Taxa Is Sensitive to Experimental Warming.Global change biology · 2025Article
- Comparing field and lab quantitative stable isotope probing for nitrogen assimilation in soil microbes.Applied and environmental microbiology · 2025Article
- Bacterial community composition and function in different habitats in Antarctic Fildes region revealed by high-throughput sequencing.Frontiers in microbiology · 2025Article
- The biogeography of soil microbiome potential growth rates.Nature communications · 2024Article
- Asymmetric winter warming reduces microbial carbon use efficiency and growth more than symmetric year-round warming in alpine soils.Proceedings of the National Academy of Sciences of the United States of America · 2024Article
- Soil warming increases the number of growing bacterial taxa but not their growth rates.Science advances · 2024Article
Corrections and comments
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Authors and funding
6 authors at 2 institutions in 1 country.
Funding
Abstract
Ice-free terrestrial environments of the western Antarctic Peninsula are expanding and subject to colonization by new microorganisms and plants, which control biogeochemical cycling. Measuring growth rates of microbial populations and ecosystem carbon flux is critical for understanding how terrestrial ecosystems in Antarctica will respond to future warming. We implemented a field warming experiment in early (bare soil; +2 °C) and late (peat moss-dominated; +1.2 °C) successional glacier forefield sites on the western Antarctica Peninsula. We used quantitative stable isotope probing with H
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Registered trials
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