Extreme (13)C depletion of carbonates formed during oxidation of biogenic methane in fractured granite

Precipitation of exceptionally (13)C-depleted authigenic carbonate is a result of, and thus a tracer for, sulphate-dependent anaerobic methane oxidation, particularly in marine sediments. Although these carbonates typically are less depleted in (13)C than in the source methane, because of incorporat...

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Detalles Bibliográficos
Autores principales: Drake, Henrik, Åström, Mats E., Heim, Christine, Broman, Curt, Åström, Jan, Whitehouse, Martin, Ivarsson, Magnus, Siljeström, Sandra, Sjövall, Peter
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4432592/
https://www.ncbi.nlm.nih.gov/pubmed/25948095
http://dx.doi.org/10.1038/ncomms8020

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4432592/
https://www.ncbi.nlm.nih.gov/pubmed/25948095
http://dx.doi.org/10.1038/ncomms8020

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