To quantify potential nitrogen (N) deposition impacts on peatland carbon (C) uptake, we explored temporal and spatial trends in N deposition and climate impacts on the production of the key peat forming functional group (Sphagnum mosses) across European peatlands for the period 1900–2050. Using a modelling approach we estimated that between 1900 and 1950 N deposition impacts remained limited irrespective of geographical position. Between 1950 and 2000 N deposition depressed production between 0 and 25% relative to 1900, particularly in temperate regions. Future scenarios indicate this trend will continue and become more pronounced with climate warming. At the European scale, the consequences for Sphagnum net C-uptake remained small relative...
The response of peatlands to changes in the climatic water budget is crucial to predicting potential...
The majority of northern peatlands were initiated during the Holocene. Owing to their mass imbalance...
Peatlands are a major terrestrial carbon store and a persistent natural carbon sink during the Holoc...
To quantify potential nitrogen (N) deposition impacts on peatland carbon (C) uptake, we explored tem...
Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holocen...
• Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holoc...
Peatlands in the northern hemisphere have accumulated more atmospheric C during the Holocene than an...
Bogs are important sinks of atmospheric carbon (C) due to their unique ability to accumulate vast a...
The relative importance of global versus local environmental factors for growth and thus carbon upta...
Peatland ecosystems only cover 2-3 % of the Earth‟s surface but they represent significant carbon st...
The response of peatlands to changes in the climatic water budget is crucial to predicting potential...
The majority of northern peatlands were initiated during the Holocene. Owing to their mass imbalance...
Peatlands are a major terrestrial carbon store and a persistent natural carbon sink during the Holoc...
To quantify potential nitrogen (N) deposition impacts on peatland carbon (C) uptake, we explored tem...
Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holocen...
• Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holoc...
Peatlands in the northern hemisphere have accumulated more atmospheric C during the Holocene than an...
Bogs are important sinks of atmospheric carbon (C) due to their unique ability to accumulate vast a...
The relative importance of global versus local environmental factors for growth and thus carbon upta...
Peatland ecosystems only cover 2-3 % of the Earth‟s surface but they represent significant carbon st...
The response of peatlands to changes in the climatic water budget is crucial to predicting potential...
The majority of northern peatlands were initiated during the Holocene. Owing to their mass imbalance...
Peatlands are a major terrestrial carbon store and a persistent natural carbon sink during the Holoc...