Despite their low primary production, ombrotrophic peatlands have a considerable potential to store atmospheric carbon as a result of their extremely low litter decomposition rates. Projected changes in temperature and nitrogen (N) deposition may increase decomposition rates by their positive effects on microbial activity and litter quality, which can be expected to result in enhanced mass loss and N release from Sphagnum and vascular plant litter. This is the first study that examines the combined effects of increased temperature and N deposition on decomposition in bogs. We investigated mass loss and N release at four bog sites along a gradient from north Sweden to northeast Germany in which both temperature and N deposition increased fro...
• Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holoc...
Peatland ecosystems only cover 2-3 % of the Earth‟s surface but they represent significant carbon st...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
High-latitude peatlands are important soil carbon sinks. In these ecosystems, the mineralization of ...
Peatlands provide multiple ecosystem services, including extensive carbon sequestration and storage,...
Peat bogs have historically represented exceptional carbon (C) sinks because of their extremely low ...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
S phagnum bogs harbour a wealth of rare vascular plant and bryophyte species, preserve an amazing po...
Decomposition rates and changes of carbon and nitrogen contents of Sphagnum litter in mire vegetatio...
Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low t...
Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low t...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
To predict the role of ombrotrophic bogs as carbon sinks in the future, it is crucial to understand ...
• Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holoc...
Peatland ecosystems only cover 2-3 % of the Earth‟s surface but they represent significant carbon st...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
High-latitude peatlands are important soil carbon sinks. In these ecosystems, the mineralization of ...
Peatlands provide multiple ecosystem services, including extensive carbon sequestration and storage,...
Peat bogs have historically represented exceptional carbon (C) sinks because of their extremely low ...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
S phagnum bogs harbour a wealth of rare vascular plant and bryophyte species, preserve an amazing po...
Decomposition rates and changes of carbon and nitrogen contents of Sphagnum litter in mire vegetatio...
Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low t...
Litter decomposition and nutrient mineralization in high-latitude peatlands are constrained by low t...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
To predict the role of ombrotrophic bogs as carbon sinks in the future, it is crucial to understand ...
• Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holoc...
Peatland ecosystems only cover 2-3 % of the Earth‟s surface but they represent significant carbon st...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...