Strong geologic methane emissions from discontinuous terrestrial permafrost in the Mackenzie Delta, Canada

Arctic permafrost caps vast amounts of old, geologic methane (CH(4)) in subsurface reservoirs. Thawing permafrost opens pathways for this CH(4) to migrate to the surface. However, the occurrence of geologic emissions and their contribution to the CH(4) budget in addition to recent, biogenic CH(4) is...

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Detalles Bibliográficos
Autores principales: Kohnert, Katrin, Serafimovich, Andrei, Metzger, Stefan, Hartmann, Jörg, Sachs, Torsten
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5517603/
https://www.ncbi.nlm.nih.gov/pubmed/28725016
http://dx.doi.org/10.1038/s41598-017-05783-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5517603/
https://www.ncbi.nlm.nih.gov/pubmed/28725016
http://dx.doi.org/10.1038/s41598-017-05783-2

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