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
Autores principales: Nunes, Flavia L. D., Aquilina, Luc, de Ridder, Jo, Francez, André-Jean, Quaiser, Achim, Caudal, Jean-Pierre, Vandenkoornhuyse, Philippe, Dufresne, Alexis
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
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

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4594127/
https://www.ncbi.nlm.nih.gov/pubmed/26440376
http://dx.doi.org/10.1038/srep14612

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