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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...

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Detalles Bibliográficos
Publicado en:Sci Rep
Main Authors: Nunes, Flavia L. D., Aquilina, Luc, de Ridder, Jo, Francez, André-Jean, Quaiser, Achim, Caudal, Jean-Pierre, Vandenkoornhuyse, Philippe, Dufresne, Alexis
Formato: Artigo
Idioma:Inglês
Publicado: Nature Publishing Group 2015
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Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC4594127/
https://ncbi.nlm.nih.gov/pubmed/26440376
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep14612
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