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CH(4) oxidation in a boreal lake during the development of hypolimnetic hypoxia
Freshwater ecosystems represent a significant natural source of methane (CH(4)). CH(4) produced through anaerobic decomposition of organic matter (OM) in lake sediment and water column can be either oxidized to carbon dioxide (CO(2)) by methanotrophic microbes or emitted to the atmosphere. While the...
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| Publicado no: | Aquat Sci |
|---|---|
| Main Authors: | , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Springer International Publishing
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7181431/ https://ncbi.nlm.nih.gov/pubmed/32362734 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1007/s00027-019-0690-8 |
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