Topsoil organic matter build‐up in glacier forelands around the world

Since the last glacial maximum, soil formation related to ice‐cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that...

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Detalles Bibliográficos
Autores principales: Khedim, Norine, Cécillon, Lauric, Poulenard, Jérôme, Barré, Pierre, Baudin, François, Marta, Silvio, Rabatel, Antoine, Dentant, Cédric, Cauvy‐Fraunié, Sophie, Anthelme, Fabien, Gielly, Ludovic, Ambrosini, Roberto, Franzetti, Andrea, Azzoni, Roberto Sergio, Caccianiga, Marco Stefano, Compostella, Chiara, Clague, John, Tielidze, Levan, Messager, Erwan, Choler, Philippe, Ficetola, Gentile Francesco
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Primary Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8048894/
https://www.ncbi.nlm.nih.gov/pubmed/33342032
http://dx.doi.org/10.1111/gcb.15496

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8048894/
https://www.ncbi.nlm.nih.gov/pubmed/33342032
http://dx.doi.org/10.1111/gcb.15496

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