Climatic modifiers of the response to nitrogen deposition in peat-forming Sphagnum mosses: a meta-analysis
Peatlands in the northern hemisphere have accumulated more atmospheric carbon (C) during the Holocene than any other terrestrial ecosystem, making peatlands long-term C sinks of global importance. Projected increases in nitrogen (N) deposition and temperature make future accumulation rates uncertain.
Keywords: carbon ; climate ; global change ; meta-regression ; nitrogen ; peatlands ; productivity ; Sphagnum ; Global Change ; Nutritional Constraints ; Terrestrial Ecosystems ; Carbon Accumulation ; Species Richness ; Ombrotrophic Bog ; Vascular Plants ; N Deposition ; Water-Table ; Growth
Record created on 2011-07-21, modified on 2016-08-09