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The transformation of macrophyte‐derived organic matter to methane relates to plant water and nutrient contents
Macrophyte detritus is one of the main sources of organic carbon (OC) in inland waters, and it is potentially available for methane (CH(4)) production in anoxic bottom waters and sediments. However, the transformation of macrophyte‐derived OC into CH(4) has not been studied systematically, thus its...
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| Pubblicato in: | Limnol Oceanogr |
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| Autori principali: | , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
John Wiley & Sons, Inc.
2019
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6774319/ https://ncbi.nlm.nih.gov/pubmed/31598008 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/lno.11148 |
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