Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio between net primary production and decomposition, both of which can change under projected increases of atmospheric CO2 and N deposition. The decomposition of litter is influenced by 1) the quality of the litter, and 2) the microenvironmental conditions in which the litter decomposes. This study aims at experimentally testing the effects of these two drivers in the context of global change. We studied the in situ litter decomposition from three common peatland species (Eriophorum vaginatum, Polytrichum strictum and Sphagnum fallax) collected after one year of litter production under pre-treatment conditions (elevated CO2: 560 ppm or enhanced N: 3 ...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...
Despite their low primary production, ombrotrophic peatlands have a considerable potential to store ...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
International audiencePurpose: The carbon sink function of peatlands is primarily driven by a higher...
Atmospheric CO2-C sequestration is directly related to the formation of peat which in turn is depend...
Peat bogs have historically represented exceptional carbon (C) sinks because of their extremely low ...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...
Despite their low primary production, ombrotrophic peatlands have a considerable potential to store ...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
International audiencePurpose: The carbon sink function of peatlands is primarily driven by a higher...
Atmospheric CO2-C sequestration is directly related to the formation of peat which in turn is depend...
Peat bogs have historically represented exceptional carbon (C) sinks because of their extremely low ...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...
Despite their low primary production, ombrotrophic peatlands have a considerable potential to store ...
Permafrost thaw is a major potential feedback source to climate change as it can drive the increased...