International audiencePurpose: The carbon sink function of peatlands is primarily driven by a higher production than decomposition of the litter Sphagnum mosses. The observed increase of vascular plants in peatlands could alter the decomposition rate and the carbon (C) cycle through a litter mixing effect, which is still poorly studied. Here, we examine the litter mixing effect of a peat moss (Sphagnum fallax) and two vascular plants (Pinus uncinata and Eriophorum vaginatum) in the field and laboratory-based experiment.Materials and methods: During the laboratory incubation, mass loss, CO2 production, and dissolved organic carbon concentration were periodically monitored during 51 days. The collected data were then processed in a C dynamics...
The discussion paper published in Biogeosciences Discuss.: Straková, P., Niemi, R. M., Freeman, C., ...
Pristine peatlands are carbon (C) accumulating wetland ecosystems sustained by a high water level (W...
A small imbalance in plant productivity and decomposition accounts for the carbon (C) accumulation c...
International audiencePurpose: The carbon sink function of peatlands is primarily driven by a higher...
International audiencePurposeThe accumulation of carbon in peatlands originates from the slow rate o...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
Northern peatlands are important stores of carbon. Following mechanical harvesting, peatlands are of...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
In peatlands the reduced decomposition rate of plant litter is the fundamental mechanism making thes...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
Peatlands can be classified into fens and bogs based on their hydrology. Development of fens to bogs...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
© 2017 Elsevier Ltd Peatland decomposition may be altered by hydrology and plant functional groups (...
The discussion paper published in Biogeosciences Discuss.: Straková, P., Niemi, R. M., Freeman, C., ...
Pristine peatlands are carbon (C) accumulating wetland ecosystems sustained by a high water level (W...
A small imbalance in plant productivity and decomposition accounts for the carbon (C) accumulation c...
International audiencePurpose: The carbon sink function of peatlands is primarily driven by a higher...
International audiencePurposeThe accumulation of carbon in peatlands originates from the slow rate o...
Peatlands represent massive global C pools and sinks. Carbon accumulation depends on the ratio betwe...
There is concern that changes in climate and land use could increase rates of decomposition in peatl...
Northern peatlands are important stores of carbon. Following mechanical harvesting, peatlands are of...
Historically, slow decomposition rates have resulted in the accumulation of large amounts of carbon ...
In peatlands the reduced decomposition rate of plant litter is the fundamental mechanism making thes...
Nitrogen (N) deposition may affect litter decomposition and may thus have an impact on the rate of c...
Peatlands can be classified into fens and bogs based on their hydrology. Development of fens to bogs...
Bogs are globally important sinks of atmospheric carbon (C) due to the accumulation of partially dec...
© 2017 Elsevier Ltd Peatland decomposition may be altered by hydrology and plant functional groups (...
The discussion paper published in Biogeosciences Discuss.: Straková, P., Niemi, R. M., Freeman, C., ...
Pristine peatlands are carbon (C) accumulating wetland ecosystems sustained by a high water level (W...
A small imbalance in plant productivity and decomposition accounts for the carbon (C) accumulation c...