Spatial variation of sediment mineralization supports differential CO(2) emissions from a tropical hydroelectric reservoir

Substantial amounts of organic matter (OM) from terrestrial ecosystems are buried as sediments in inland waters. It is still unclear to what extent this OM constitutes a sink of carbon, and how much of it is returned to the atmosphere upon mineralization to carbon dioxide (CO(2)). The construction o...

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Detalles Bibliográficos
Autores principales: Cardoso, Simone J., Vidal, Luciana O., Mendonça, Raquel F., Tranvik, Lars J., Sobek, Sebastian, Fábio, Roland
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2013
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3639384/
https://www.ncbi.nlm.nih.gov/pubmed/23641239
http://dx.doi.org/10.3389/fmicb.2013.00101

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3639384/
https://www.ncbi.nlm.nih.gov/pubmed/23641239
http://dx.doi.org/10.3389/fmicb.2013.00101

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