Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respond to the changing climate is still relatively unknown. A global picture of the variations in peat organic matter chemistry will aid our ability to gauge peatland soil response to climate. The goal of this research is to test the hypotheses that (a) peat carbohydrate content, an indicator of soil organic matter reactivity, will increase with latitude and decrease with mean annual temperatures, (b) while peat aromatic content, an indicator of recalcitrance, will vary inversely, and (c) elevation will have a similar effect to latitude. We used Fourier Transform Infrared Spectroscopy to examine variations in the organic matter functional groups o...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
The humification process is one of the least understood and most intriguing aspects of humus chemist...
Peatlands store carbon in the form of dead organic residues. Climate change and human impact impose ...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands represent large terrestrial carbon banks. Given that most peat accumulates in boreal regio...
Peatlands are climate critical carbon (C) reservoirs that could become a C source under continued wa...
Peatlands are climate critical carbon (C) reservoirs that could become a C source under continued wa...
This is the final version. Available from the European Association of Geoscientists & Engineers via ...
Large tracts of arctic and subarctic peatlands are underlain by permafrost. These peatlands store la...
Studies conducted across northern Europe and North America have shown increases in dissolved organic...
International audienceDue to the wet and anoxic specific environmental conditions, which reduce the ...
Understanding the effects of elevated temperatures on soil organic matter (SOM) decomposition pathwa...
More than one third of global soil organic matter (SOM) is stored in peatlands, despite them occupyi...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
The humification process is one of the least understood and most intriguing aspects of humus chemist...
Peatlands store carbon in the form of dead organic residues. Climate change and human impact impose ...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands contain a significant fraction of global soil carbon, but how these reservoirs will respon...
Peatlands represent large terrestrial carbon banks. Given that most peat accumulates in boreal regio...
Peatlands are climate critical carbon (C) reservoirs that could become a C source under continued wa...
Peatlands are climate critical carbon (C) reservoirs that could become a C source under continued wa...
This is the final version. Available from the European Association of Geoscientists & Engineers via ...
Large tracts of arctic and subarctic peatlands are underlain by permafrost. These peatlands store la...
Studies conducted across northern Europe and North America have shown increases in dissolved organic...
International audienceDue to the wet and anoxic specific environmental conditions, which reduce the ...
Understanding the effects of elevated temperatures on soil organic matter (SOM) decomposition pathwa...
More than one third of global soil organic matter (SOM) is stored in peatlands, despite them occupyi...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
The humification process is one of the least understood and most intriguing aspects of humus chemist...
Peatlands store carbon in the form of dead organic residues. Climate change and human impact impose ...