Rapid Sediment Accumulation Results in High Methane Effluxes from Coastal Sediments

Globally, the methane (CH(4)) efflux from the ocean to the atmosphere is small, despite high rates of CH(4) production in continental shelf and slope environments. This low efflux results from the biological removal of CH(4) through anaerobic oxidation with sulfate in marine sediments. In some setti...

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Detalles Bibliográficos
Autores principales: Egger, Matthias, Lenstra, Wytze, Jong, Dirk, Meysman, Filip J. R., Sapart, Célia J., van der Veen, Carina, Röckmann, Thomas, Gonzalez, Santiago, Slomp, Caroline P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2016
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4999275/
https://www.ncbi.nlm.nih.gov/pubmed/27560511
http://dx.doi.org/10.1371/journal.pone.0161609

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4999275/
https://www.ncbi.nlm.nih.gov/pubmed/27560511
http://dx.doi.org/10.1371/journal.pone.0161609

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