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000010926 0247_ $$2DOI$$a10.1111/j.1365-3040.2010.02201.x
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000010926 041__ $$aeng
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000010926 084__ $$2WoS$$aPlant Sciences
000010926 1001_ $$0P:(DE-HGF)0$$aDieleman, W.I.J.$$b0
000010926 245__ $$aSoil [N] modulates soil C cycling in CO2-fumigated tree stands: a meta-analysis
000010926 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2010
000010926 300__ $$a2001 - 2011
000010926 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
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000010926 440_0 $$04976$$aPlant, Cell and Environment$$v33$$x0140-7791$$y12
000010926 500__ $$aWe thank L. E. Henry and K. Pregitzer for providing data, as well as C. Korner for useful information about their experimental sites. Special thanks go to the researchers of the ECOCRAFT [Framework programmes of the EC (EC contracts within 5FP and 6FP, Environment and Research)] and the EUROFACE projects, who provided the large number of data that formed the foundation for this paper. M. L. is a postdoctoral research associate of the Flemish Science Foundation FWO (Fonds Wetenschappelijk onderzoek, FWO Vlaanderen). I.J. holds an FWO research grant, and S. L. holds a European Research Council (ERC) grant. Part of this research has been funded through the UA-Research Centre of Excellence ECO.
000010926 520__ $$aUnder elevated atmospheric CO(2) concentrations, soil carbon (C) inputs are typically enhanced, suggesting larger soil C sequestration potential. However, soil C losses also increase and progressive nitrogen (N) limitation to plant growth may reduce the CO(2) effect on soil C inputs with time. We compiled a data set from 131 manipulation experiments, and used meta-analysis to test the hypotheses that: (1) elevated atmospheric CO(2) stimulates soil C inputs more than C losses, resulting in increasing soil C stocks; and (2) that these responses are modulated by N. Our results confirm that elevated CO(2) induces a C allocation shift towards below-ground biomass compartments. However, the increased soil C inputs were offset by increased heterotrophic respiration (Rh), such that soil C content was not affected by elevated CO(2). Soil N concentration strongly interacted with CO(2) fumigation: the effect of elevated CO(2) on fine root biomass and -production and on microbial activity increased with increasing soil N concentration, while the effect on soil C content decreased with increasing soil N concentration. These results suggest that both plant growth and microbial activity responses to elevated CO(2) are modulated by N availability, and that it is essential to account for soil N concentration in C cycling analyses.
000010926 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000010926 588__ $$aDataset connected to Web of Science, Pubmed
000010926 650_2 $$2MeSH$$aAtmosphere
000010926 650_2 $$2MeSH$$aBiomass
000010926 650_2 $$2MeSH$$aCarbon Cycle
000010926 650_2 $$2MeSH$$aCarbon Dioxide
000010926 650_2 $$2MeSH$$aFertilizers
000010926 650_2 $$2MeSH$$aNitrogen Cycle
000010926 650_2 $$2MeSH$$aSoil: analysis
000010926 650_2 $$2MeSH$$aTrees: growth & development
000010926 650_7 $$00$$2NLM Chemicals$$aFertilizers
000010926 650_7 $$00$$2NLM Chemicals$$aSoil
000010926 650_7 $$0124-38-9$$2NLM Chemicals$$aCarbon Dioxide
000010926 650_7 $$2WoSType$$aJ
000010926 65320 $$2Author$$a[CO2] enrichment
000010926 65320 $$2Author$$aC sequestration
000010926 65320 $$2Author$$afine root production
000010926 65320 $$2Author$$amicrobial respiration
000010926 65320 $$2Author$$aN fertilization
000010926 65320 $$2Author$$aroot biomass
000010926 7001_ $$0P:(DE-HGF)0$$aLuyssaert, S.$$b1
000010926 7001_ $$0P:(DE-HGF)0$$aRey, A.$$b2
000010926 7001_ $$0P:(DE-HGF)0$$aDe Angelis, P.$$b3
000010926 7001_ $$0P:(DE-HGF)0$$aBarton, C.V.M.$$b4
000010926 7001_ $$0P:(DE-HGF)0$$aBroadmeadow, M.S.J.$$b5
000010926 7001_ $$0P:(DE-HGF)0$$aBroadmeadow, S.B.$$b6
000010926 7001_ $$0P:(DE-HGF)0$$aChigwerewe, K.S.$$b7
000010926 7001_ $$0P:(DE-HGF)0$$aCrookshanks, M.$$b8
000010926 7001_ $$0P:(DE-HGF)0$$aDufrene, E.$$b9
000010926 7001_ $$0P:(DE-HGF)0$$aJarvis, P.G.$$b10
000010926 7001_ $$0P:(DE-HGF)0$$aKasurinen, A.$$b11
000010926 7001_ $$0P:(DE-HGF)0$$aKellomäki, S.$$b12
000010926 7001_ $$0P:(DE-HGF)0$$aLe Dantec, V.$$b13
000010926 7001_ $$0P:(DE-HGF)0$$aLiberloo, M.$$b14
000010926 7001_ $$0P:(DE-HGF)0$$aMarek, M.$$b15
000010926 7001_ $$0P:(DE-HGF)0$$aMedlyn, B.$$b16
000010926 7001_ $$0P:(DE-HGF)0$$aPokorny, R.$$b17
000010926 7001_ $$0P:(DE-HGF)0$$aScarascia-Mugnozza, G.$$b18
000010926 7001_ $$0P:(DE-Juel1)129409$$aTemperton, V. M.$$b19$$uFZJ
000010926 7001_ $$0P:(DE-HGF)0$$aTingey, D.$$b20
000010926 7001_ $$0P:(DE-HGF)0$$aUrban, O.$$b21
000010926 7001_ $$0P:(DE-HGF)0$$aCeulemans, R.$$b22
000010926 7001_ $$0P:(DE-HGF)0$$aJanssens, I.A.$$b23
000010926 773__ $$0PERI:(DE-600)2020843-1$$a10.1111/j.1365-3040.2010.02201.x$$gVol. 33, p. 2001 - 2011$$p2001 - 2011$$q33<2001 - 2011$$tPlant, cell & environment$$v33$$x0140-7791$$y2010
000010926 8567_ $$uhttp://dx.doi.org/10.1111/j.1365-3040.2010.02201.x
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000010926 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
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