Increased belowground carbon inputs and warming promote loss of soil organic carbon through complementary microbial responses

Current carbon cycle-climate models predict that future soil carbon storage will be determined by the balance between CO2 fertilization and warming. However, it is uncertain whether greater carbon inputs to soils with elevated CO2 will be sequestered, particularly since warming hastens soil carbon d...

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Veröffentlicht in:	Soil biology & biochemistry 2014-09, Vol.76, p.57-69
Hauptverfasser:	Hopkins, Francesca M., Filley, Timothy R., Gleixner, Gerd, Lange, Markus, Top, Sara M., Trumbore, Susan E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Agronomy. Soil science and plant productions Biochemistry and biology Biological and medical sciences Carbon isotopes Chemical, physicochemical, biochemical and biological properties Elevated CO2 Fundamental and applied biological sciences. Psychology Microbiology Organic matter Physics, chemistry, biochemistry and biology of agricultural and forest soils PLFA Priming effect Soil organic matter decomposition Soil science Temperature response
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