Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales

Through increases in net primary production (NPP), elevated CO<sub>2</sub> is hypothesized to increase the amount of plant litter entering the soil. The fate of this extra carbon on the forest floor or in mineral soil is currently not clear. Moreover, increased rates of NPP can be mainta...

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Main Authors: A. R. Smith, D. L. Godbold, E. Velthorst, M. Lukac, M. R. Hoosbeek
Format: Article
Language:English
Published: Copernicus Publications 2011-02-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/8/353/2011/bg-8-353-2011.pdf
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spelling doaj-0f0a96690a3a443e9c2e8f7d428d05872020-11-25T00:13:29ZengCopernicus PublicationsBiogeosciences1726-41701726-41892011-02-018235336410.5194/bg-8-353-2011Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in WalesA. R. SmithD. L. GodboldE. VelthorstM. LukacM. R. HoosbeekThrough increases in net primary production (NPP), elevated CO<sub>2</sub> is hypothesized to increase the amount of plant litter entering the soil. The fate of this extra carbon on the forest floor or in mineral soil is currently not clear. Moreover, increased rates of NPP can be maintained only if forests can escape nitrogen limitation. In a Free atmospheric CO<sub>2</sub> Enrichment (FACE) experiment near Bangor, Wales, 4 ambient and 4 elevated [CO<sub>2</sub>] plots were planted with patches of <i>Betula pendula</i>, <i>Alnus glutinosa</i> and <i>Fagus sylvatica</i> on a former arable field. After 4 years, biomass averaged for the 3 species was 5497 (se 270) g m<sup>−2</sup> in ambient and 6450 (se 130) g m<sup>−2</sup> in elevated [CO<sub>2</sub>] plots, a significant increase of 17% (<i>P</i> = 0.018). During that time, only a shallow L forest floor litter layer had formed due to intensive bioturbation. Total soil C and N contents increased irrespective of treatment and species as a result of afforestation. We could not detect an additional C sink in the soil, nor were soil C stabilization processes affected by elevated [CO<sub>2</sub>]. We observed a decrease of leaf N content in <i>Betula</i> and <i>Alnus</i> under elevated [CO<sub>2</sub>], while the soil C/N ratio decreased regardless of CO<sub>2</sub> treatment. The ratio of N taken up from the soil and by N<sub>2</sub>-fixation in <i>Alnus</i> was not affected by elevated [CO<sub>2</sub>]. We infer that increased nitrogen use efficiency is the mechanism by which increased NPP is sustained under elevated [CO<sub>2</sub>] at this site. http://www.biogeosciences.net/8/353/2011/bg-8-353-2011.pdf
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language English
format Article
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author A. R. Smith
D. L. Godbold
E. Velthorst
M. Lukac
M. R. Hoosbeek
spellingShingle A. R. Smith
D. L. Godbold
E. Velthorst
M. Lukac
M. R. Hoosbeek
Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
Biogeosciences
author_facet A. R. Smith
D. L. Godbold
E. Velthorst
M. Lukac
M. R. Hoosbeek
author_sort A. R. Smith
title Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
title_short Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
title_full Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
title_fullStr Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
title_full_unstemmed Free atmospheric CO<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic N<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in Wales
title_sort free atmospheric co<sub>2</sub> enrichment increased above ground biomass but did not affect symbiotic n<sub>2</sub>-fixation and soil carbon dynamics in a mixed deciduous stand in wales
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2011-02-01
description Through increases in net primary production (NPP), elevated CO<sub>2</sub> is hypothesized to increase the amount of plant litter entering the soil. The fate of this extra carbon on the forest floor or in mineral soil is currently not clear. Moreover, increased rates of NPP can be maintained only if forests can escape nitrogen limitation. In a Free atmospheric CO<sub>2</sub> Enrichment (FACE) experiment near Bangor, Wales, 4 ambient and 4 elevated [CO<sub>2</sub>] plots were planted with patches of <i>Betula pendula</i>, <i>Alnus glutinosa</i> and <i>Fagus sylvatica</i> on a former arable field. After 4 years, biomass averaged for the 3 species was 5497 (se 270) g m<sup>−2</sup> in ambient and 6450 (se 130) g m<sup>−2</sup> in elevated [CO<sub>2</sub>] plots, a significant increase of 17% (<i>P</i> = 0.018). During that time, only a shallow L forest floor litter layer had formed due to intensive bioturbation. Total soil C and N contents increased irrespective of treatment and species as a result of afforestation. We could not detect an additional C sink in the soil, nor were soil C stabilization processes affected by elevated [CO<sub>2</sub>]. We observed a decrease of leaf N content in <i>Betula</i> and <i>Alnus</i> under elevated [CO<sub>2</sub>], while the soil C/N ratio decreased regardless of CO<sub>2</sub> treatment. The ratio of N taken up from the soil and by N<sub>2</sub>-fixation in <i>Alnus</i> was not affected by elevated [CO<sub>2</sub>]. We infer that increased nitrogen use efficiency is the mechanism by which increased NPP is sustained under elevated [CO<sub>2</sub>] at this site.
url http://www.biogeosciences.net/8/353/2011/bg-8-353-2011.pdf
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