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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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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Frontiers Media S.A.
2013
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3639384/ https://ncbi.nlm.nih.gov/pubmed/23641239 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2013.00101 |
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