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...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Global change biology 2021-04, Vol.27 (8), p.1662-1677
Hauptverfasser:	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
Format:	Artikel
Sprache:	eng
Schlagworte:	Accumulation Aromatic compounds Biodiversity Biodiversity and Ecology Biogeochemistry Botanics Carbon Carbon 13 carbon stability chronosequence Climate Climate change climate sensitivity Climatic conditions Construction Control stability Durability Ecology, environment Ecosystems Environmental Sciences Functional groups Glaciers Global warming Ice Cover Ice formation Life Sciences Nitrogen Nitrogen enrichment Nitrogen isotopes Organic matter Organic soils Oxygen enrichment Pools Primary Primary s Soil Soil formation Soil organic matter Soil shrinkage Soil stability Soils Stocks Storage Systematics, Phylogenetics and taxonomy Temperature Thermal stability Topsoil topsoil development Vegetal Biology Vulnerability
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!