[1] Northern peatlands are significant stocks of terrestrial soil carbon, and it has been predicted that warmer temperatures and lower water tables resulting from climate change will convert these ecosystems into sources for atmospheric carbon dioxide (CO2). However, these predictions do not consider the potential for hydrologically induced ecological succession or the spatial variability of carbon accumulation rates between different microforms in peatlands. To address these issues, the vegetation community was described, and the rates of gross ecosystem photosynthesis (GEP), ecosystem respiration (Rtot) and net ecosystem CO2 exchange were determined along poor fen microtopographic gradients at a control site and at a site which experience...
<div><p>Raised bogs have accumulated more atmospheric carbon than any other terrestrial ecosystem on...
Globally, peatlands store a large quantity of soil carbon that can be subsequently modified by hydro...
International audienceThe C-sink function of peatlands is mainly controlled by soil waterlogging and...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
A small imbalance in plant productivity and decomposition accounts for the carbon (C) accumulation c...
Northern peatlands are globally important long-term sinks of carbon due to their predominantly satur...
Globally, peatlands play an important role in the carbon (C) cycle. High water level is a key factor...
Drier conditions caused by drainage for infrastructure development, or associated with global climat...
The surface of bogs is commonly patterned and composed of different vegetation communities, defined ...
Peatland disturbance through drainage threatens to liberate large amounts of C stocks by increasing ...
International audienceThe function of peatlands as a large carbon (C) reservoir results from the net...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
Over the last millennium peatlands have accumulated significant carbon stores. Drainage for agricult...
We quantified the role of spatially varying vegetation composition in seasonal and interannual chang...
Sherpa Romeo green journal. Permission to archive final published versionNorthern peatlands are a di...
<div><p>Raised bogs have accumulated more atmospheric carbon than any other terrestrial ecosystem on...
Globally, peatlands store a large quantity of soil carbon that can be subsequently modified by hydro...
International audienceThe C-sink function of peatlands is mainly controlled by soil waterlogging and...
Boreal peatlands are important ecosystems from a carbon balance perspective because they are natural...
A small imbalance in plant productivity and decomposition accounts for the carbon (C) accumulation c...
Northern peatlands are globally important long-term sinks of carbon due to their predominantly satur...
Globally, peatlands play an important role in the carbon (C) cycle. High water level is a key factor...
Drier conditions caused by drainage for infrastructure development, or associated with global climat...
The surface of bogs is commonly patterned and composed of different vegetation communities, defined ...
Peatland disturbance through drainage threatens to liberate large amounts of C stocks by increasing ...
International audienceThe function of peatlands as a large carbon (C) reservoir results from the net...
Peatland ecosystems store between 200 and 450 Gt C (1015 gC). It is estimated that peatlands constit...
Over the last millennium peatlands have accumulated significant carbon stores. Drainage for agricult...
We quantified the role of spatially varying vegetation composition in seasonal and interannual chang...
Sherpa Romeo green journal. Permission to archive final published versionNorthern peatlands are a di...
<div><p>Raised bogs have accumulated more atmospheric carbon than any other terrestrial ecosystem on...
Globally, peatlands store a large quantity of soil carbon that can be subsequently modified by hydro...
International audienceThe C-sink function of peatlands is mainly controlled by soil waterlogging and...