Direct isotopic evidence of biogenic methane production and efflux from beneath a temperate glacier

The base of glaciers and ice sheets provide environments suitable for the production of methane. High pressure conditions beneath the impermeable ‘cap’ of overlying ice promote entrapment of methane reserves that can be released to the atmosphere during ice thinning and meltwater evacuation. However...

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Detalles Bibliográficos
Autores principales: Burns, R., Wynn, P. M., Barker, P., McNamara, N., Oakley, S., Ostle, N., Stott, A. W., Tuffen, H., Zhou, Zheng, Tweed, F. S., Chesler, A., Stuart, M.
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/PMC6244297/
https://www.ncbi.nlm.nih.gov/pubmed/30459433
http://dx.doi.org/10.1038/s41598-018-35253-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6244297/
https://www.ncbi.nlm.nih.gov/pubmed/30459433
http://dx.doi.org/10.1038/s41598-018-35253-2

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