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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Detalles Bibliográficos
Autores principales: Kramshøj, Magnus, Albers, Christian N., Holst, Thomas, Holzinger, Rupert, Elberling, Bo, Rinnan, Riikka
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6109083/
https://www.ncbi.nlm.nih.gov/pubmed/30143640
http://dx.doi.org/10.1038/s41467-018-05824-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6109083/
https://www.ncbi.nlm.nih.gov/pubmed/30143640
http://dx.doi.org/10.1038/s41467-018-05824-y

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