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Biogenic volatile release from permafrost thaw is determined by the soil microbial sink
Warming in the Arctic accelerates thawing of permafrost-affected soils, which leads to a release of greenhouse gases to the atmosphere. We do not know whether permafrost thaw also releases non-methane volatile organic compounds that can contribute to both negative and positive radiative forcing on c...
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| Udgivet i: | Nat Commun |
|---|---|
| Main Authors: | , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Nature Publishing Group UK
2018
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6109083/ https://ncbi.nlm.nih.gov/pubmed/30143640 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05824-y |
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