Bioavailability of soil organic matter and microbial community dynamics upon permafrost thaw
Amplified Arctic warming could thaw 25% of the permafrost area by 2100, exposing vast amounts of currently fixed organic carbon to microbially mediated decomposition and release of greenhouse gasses through soil organic matter (SOM) respiration. We performed time-series incubation experiments with H...
Main Authors: | Coolen, Marco, van de Giessen, J., Zhu, E., Wuchter, C. |
---|---|
Format: | Journal Article |
Published: |
2011
|
Online Access: | http://hdl.handle.net/20.500.11937/11127 |
Similar Items
-
The transcriptional response of microbial communities in thawing Alaskan permafrost soils
by: Coolen, Marco, et al.
Published: (2015) -
The transcriptional response of microbial communities in thawing Alaskan permafrost soils
by: Coolen, Marco J. L., et al.
Published: (2015) -
Biogenic volatile release from permafrost thaw is determined by the soil microbial sink
by: Magnus Kramshøj, et al.
Published: (2018-08-01) -
Input of easily available organic C and N stimulates microbial decomposition of soil organic matter in arctic permafrost soil
by: Wild, Birgit, et al.
Published: (2014) -
Environmental selection of planktonic methanogens in permafrost thaw ponds
by: Crevecoeur, Sophie, et al.
Published: (2016)