The effect of temperature on organic carbon degradation in marine sediments

The degradation of sedimentary particulate organic carbon (POC) is a key carbon cycle process that fuels the deep subseafloor biosphere. The reactivity of POC is expected to decrease with increasing sediment age, severely restricting the energy available to microorganisms. Conversely, increasing tem...

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Detalles Bibliográficos
Autores principales: Malinverno, Alberto, Martinez, Ernesto A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4671099/
https://www.ncbi.nlm.nih.gov/pubmed/26640172
http://dx.doi.org/10.1038/srep17861

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4671099/
https://www.ncbi.nlm.nih.gov/pubmed/26640172
http://dx.doi.org/10.1038/srep17861

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