Peatlands are ecosystems for which carbon budget relies strongly on the meteorological and hydrological conditions. Here, using a manipulative field experiment, we measured ecosystem respiration (RECO) over two years (2013–2014) in a poor fen in Poland to estimate the carbon emission in a changing climate. The experiment consisted of warming (open-top chambers - OTC) and water table manipulation. The application of OTC increased the mean values of daily maximum air temperature by approx. 1.1–1.8 °C. Warming or the increased water table depth separately resulted in an increase in ecosystem respiration by approx. 0.1 μmol CO2 m−2 s−1 and 0.3 μmol CO2 m−2 s−1, respectively. However, our results show also the additive nature of warming and wate...
The carbon cycle modulates climate change, via the regulation of atmospheric CO2. and it represents ...
Upland peat is the world's largest store of soil carbon and one of the most climatically sensitive. ...
Since the last deglaciation, 300-500 Pg carbon have accumulated in northern peatlands (346 mill. ha)...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
International audienceThe function of peatlands as a large carbon (C) reservoir results from the net...
Among the largest uncertainties in current projections of future climate is the feedback between the...
Ecosystem respiration (ER) is an important but poorly understood part of the carbon (C) budget of pe...
Ecosystem respiration (ER) is an important but poorly understood part of the carbon (C) budget of pe...
Midlatitude treed bogs represent significant carbon (C) stocks and are highly sensitive to global cl...
Abstract Northern peatlands form a major soil carbon (C) stock. With climate change, peatland C mine...
[1] Northern peatlands are significant stocks of terrestrial soil carbon, and it has been predicted ...
There is an urgent need to understand the effect of climate warming on the carbon dynamics of lakes ...
The peat soils found in blanket bogs are significant stores of carbon. The degree to which these eco...
The carbon (C) balance of boreal peatlands is mainly the sum of three different C fluxes: carbon dio...
Drainage of peatlands is expected to turn these ecosystems into carbon sources to the atmosphere. We...
The carbon cycle modulates climate change, via the regulation of atmospheric CO2. and it represents ...
Upland peat is the world's largest store of soil carbon and one of the most climatically sensitive. ...
Since the last deglaciation, 300-500 Pg carbon have accumulated in northern peatlands (346 mill. ha)...
Climate warming is expected to accelerate peatland degradation and release rates of carbon dioxide (...
International audienceThe function of peatlands as a large carbon (C) reservoir results from the net...
Among the largest uncertainties in current projections of future climate is the feedback between the...
Ecosystem respiration (ER) is an important but poorly understood part of the carbon (C) budget of pe...
Ecosystem respiration (ER) is an important but poorly understood part of the carbon (C) budget of pe...
Midlatitude treed bogs represent significant carbon (C) stocks and are highly sensitive to global cl...
Abstract Northern peatlands form a major soil carbon (C) stock. With climate change, peatland C mine...
[1] Northern peatlands are significant stocks of terrestrial soil carbon, and it has been predicted ...
There is an urgent need to understand the effect of climate warming on the carbon dynamics of lakes ...
The peat soils found in blanket bogs are significant stores of carbon. The degree to which these eco...
The carbon (C) balance of boreal peatlands is mainly the sum of three different C fluxes: carbon dio...
Drainage of peatlands is expected to turn these ecosystems into carbon sources to the atmosphere. We...
The carbon cycle modulates climate change, via the regulation of atmospheric CO2. and it represents ...
Upland peat is the world's largest store of soil carbon and one of the most climatically sensitive. ...
Since the last deglaciation, 300-500 Pg carbon have accumulated in northern peatlands (346 mill. ha)...