Gas hydrate dissociation linked to contemporary ocean warming in the southern hemisphere

Ocean warming related to climate change has been proposed to cause the dissociation of gas hydrate deposits and methane leakage on the seafloor. This process occurs in places where the edge of the gas hydrate stability zone in sediments meets the overlying warmer oceans in upper slope settings. Here...

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Detalles Bibliográficos
Autores principales: Ketzer, Marcelo, Praeg, Daniel, Rodrigues, Luiz F., Augustin, Adolpho, Pivel, Maria A. G., Rahmati-Abkenar, Mahboubeh, Miller, Dennis J., Viana, Adriano R., Cupertino, José A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7391661/
https://www.ncbi.nlm.nih.gov/pubmed/32728027
http://dx.doi.org/10.1038/s41467-020-17289-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7391661/
https://www.ncbi.nlm.nih.gov/pubmed/32728027
http://dx.doi.org/10.1038/s41467-020-17289-z

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