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Time-scales of hydrological forcing on the geochemistry and bacterial community structure of temperate peat soils
Peatlands are an important global carbon reservoir. The continued accumulation of carbon in peatlands depends on the persistence of anoxic conditions, in part induced by water saturation, which prevents oxidation of organic matter, and slows down decomposition. Here we investigate how and over what...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2015
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4594127/ https://www.ncbi.nlm.nih.gov/pubmed/26440376 http://dx.doi.org/10.1038/srep14612 |