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  4. Climatic modifiers of the response to nitrogen deposition in peat-forming Sphagnum mosses: a meta-analysis
 
research article

Climatic modifiers of the response to nitrogen deposition in peat-forming Sphagnum mosses: a meta-analysis

Limpens, J.
•
Granath, G.
•
Gunnarsson, U.
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2011
New Phytologist

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.

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Type
research article
DOI
10.1111/j.1469-8137.2011.03680.x
Web of Science ID

WOS:000292211800018

Author(s)
Limpens, J.
Granath, G.
Gunnarsson, U.
Aerts, R.
Bayley, S.
Bragazza, L.  
Bubier, J.
Buttler, A.  
van den Berg, L. J. L.
Francez, A.-J.
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Date Issued

2011

Publisher

Wiley-Blackwell

Published in
New Phytologist
Volume

191

Start page

496

End page

507

Subjects

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

Editorial or Peer reviewed

REVIEWED

Written at

EPFL

EPFL units
ECOS  
Available on Infoscience
July 21, 2011
Use this identifier to reference this record
https://infoscience.epfl.ch/handle/20.500.14299/69681
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