Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming

Methane seepage from the upper continental slopes of Western Svalbard has previously been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient bottom waters. Here we show that sediment cores drilled off Prins Karls Foreland contain freshwater from dissociating hydrates....

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Detalles Bibliográficos
Autores principales: Wallmann, Klaus, Riedel, M., Hong, W. L., Patton, H., Hubbard, A., Pape, T., Hsu, C. W., Schmidt, C., Johnson, J. E., Torres, M. E., Andreassen, K., Berndt, C., Bohrmann, G.
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/PMC5758787/
https://www.ncbi.nlm.nih.gov/pubmed/29311564
http://dx.doi.org/10.1038/s41467-017-02550-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5758787/
https://www.ncbi.nlm.nih.gov/pubmed/29311564
http://dx.doi.org/10.1038/s41467-017-02550-9

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