Greenhouse gas balance of forestry-drained boreal peatlands: Sinks or sources?

[1]  Timo Penttilä,et al.  Greenhouse gas flux measurements in a forestry-drained peatland indicate a large carbon sink , 2011 .

[2]  T. Laurila,et al.  Comparison of greenhouse gas fluxes and nitrogen budgets from an ombotrophic bog in Scotland and a minerotrophic sedge fen in Finland , 2010 .

[3]  M. Pihlatie,et al.  Responses of N2O fluxes to temperature, water table and N deposition in a northern boreal fen , 2010 .

[4]  Timo Penttilä,et al.  Soil–atmosphere CO2, CH4 and N2O fluxes in boreal forestry-drained peatlands , 2010 .

[5]  P. Martikainen,et al.  Greenhouse gas emissions from cultivated and abandoned organic croplands , 2008 .

[6]  Jani V Anttila,et al.  Dynamics of Litterfall and Decomposition in Peatland Forests: Towards Reliable Carbon Balance Estimation? , 2008 .

[7]  Steve Frolking,et al.  Holocene radiative forcing impact of northern peatland carbon accumulation and methane emissions , 2006 .

[8]  K. Minkkinen,et al.  Post-drainage changes in vegetation composition and carbon balance in Lakkasuo mire, Central Finland , 1999, Plant and Soil.

[9]  Timo Penttilä,et al.  Dynamics of plant‐mediated organic matter and nutrient cycling following water‐level drawdown in boreal peatlands , 2003 .

[10]  M. Cannell,et al.  Carbon balance of afforested peatland in Scotland , 2003 .

[11]  Jukka Turunen,et al.  Estimating carbon accumulation rates of undrained mires in Finland–application to boreal and subarctic regions , 2002 .

[12]  Hannu Hökkä,et al.  Tree stand development and carbon sequestration in drained peatland stands in Finland : a simulation study , 2001 .

[13]  N. Roulet,et al.  Carbon balance of a boreal patterned peatland , 2000 .

[14]  K. Minkkinen,et al.  Long-term effect of forest drainage on the peat carbon stores of pine mires in Finland , 1998 .

[15]  Hannu Nykänen,et al.  Fluxes of nitrous oxide from boreal peatlands as affected by peatland type, water table level and nitrification capacity , 1996 .