Shrubland primary production and soil respiration diverge along European climate gradient

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Shrubland primary production and soil respiration diverge along European climate gradient. / Reinsch, Sabine; Koller, Eva; Sowerby, Alwyn et al.
In: Scientific Reports, Vol. 7, 43952, 03.2017.

Research output: Contribution to journalArticlepeer-review

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Reinsch, S, Koller, E, Sowerby, A, de Dato, G, Estiarte, M, Guidolotti, G, Kovács-Láng, E, Kröel-Dulay, G, Lellei-Kovács, E, Larsen, KS, Liberati, D, Peñuelas, J, Ransijn, J, Robinson, D, Schmidt, IK, Smith, A, Tietema, A, Dukes, JS, Beier, C & Emmett, B 2017, 'Shrubland primary production and soil respiration diverge along European climate gradient', Scientific Reports, vol. 7, 43952. https://doi.org/10.1038/srep43952

APA

Reinsch, S., Koller, E., Sowerby, A., de Dato, G., Estiarte, M., Guidolotti, G., Kovács-Láng, E., Kröel-Dulay, G., Lellei-Kovács, E., Larsen, K. S., Liberati, D., Peñuelas, J., Ransijn, J., Robinson, D., Schmidt, I. K., Smith, A., Tietema, A., Dukes, J. S., Beier, C., & Emmett, B. (2017). Shrubland primary production and soil respiration diverge along European climate gradient. Scientific Reports, 7, Article 43952. https://doi.org/10.1038/srep43952

CBE

Reinsch S, Koller E, Sowerby A, de Dato G, Estiarte M, Guidolotti G, Kovács-Láng E, Kröel-Dulay G, Lellei-Kovács E, Larsen KS, et al. 2017. Shrubland primary production and soil respiration diverge along European climate gradient. Scientific Reports. 7:Article 43952. https://doi.org/10.1038/srep43952

MLA

VancouverVancouver

Reinsch S, Koller E, Sowerby A, de Dato G, Estiarte M, Guidolotti G et al. Shrubland primary production and soil respiration diverge along European climate gradient. Scientific Reports. 2017 Mar;7:43952. Epub 2017 Mar 3. doi: 10.1038/srep43952

Author

Reinsch, Sabine ; Koller, Eva ; Sowerby, Alwyn et al. / Shrubland primary production and soil respiration diverge along European climate gradient. In: Scientific Reports. 2017 ; Vol. 7.

RIS

TY - JOUR

T1 - Shrubland primary production and soil respiration diverge along European climate gradient

AU - Reinsch, Sabine

AU - Koller, Eva

AU - Sowerby, Alwyn

AU - de Dato, Giovanbattista

AU - Estiarte, Marc

AU - Guidolotti, Gabriele

AU - Kovács-Láng, Edit

AU - Kröel-Dulay, György

AU - Lellei-Kovács, Eszter

AU - Larsen, Klaus S.

AU - Liberati, Dario

AU - Peñuelas, Josep

AU - Ransijn, Johannes

AU - Robinson, David

AU - Schmidt, Inger K.

AU - Smith, Andrew

AU - Tietema, Albert

AU - Dukes, Jeffrey S.

AU - Beier, Claus

AU - Emmett, Bridget

PY - 2017/3

Y1 - 2017/3

N2 - Above- and belowground carbon (C) stores of terrestrial ecosystems are vulnerable to environmental change. Ecosystem C balances in response to environmental changes have been quantified at individual sites, but the magnitudes and directions of these responses along environmental gradients remain uncertain. Here we show the responses of ecosystem C to 8-12 years of experimental drought and night-time warming across an aridity gradient spanning seven European shrublands using indices of C a ssimilation(aboveground net primary production: aNPP) and soil C efflux (soil respiration: Rs). The changes of aNPP and Rs in response to drought indicated that wet systems had an overall risk of increased loss of C but drier systems did not. Warming had no consistent effect on aNPP across the climate gradient and Rs increased from drier to wetter sites. Our findings suggest that the above- and belowground C fluxes become decoupled, with no evidence of acclimation at a decadal timescale. aNPP and Rs especially differed in 3 their sensitivity to drought and warming, with belowground processes being more sensitive to environmental change.

AB - Above- and belowground carbon (C) stores of terrestrial ecosystems are vulnerable to environmental change. Ecosystem C balances in response to environmental changes have been quantified at individual sites, but the magnitudes and directions of these responses along environmental gradients remain uncertain. Here we show the responses of ecosystem C to 8-12 years of experimental drought and night-time warming across an aridity gradient spanning seven European shrublands using indices of C a ssimilation(aboveground net primary production: aNPP) and soil C efflux (soil respiration: Rs). The changes of aNPP and Rs in response to drought indicated that wet systems had an overall risk of increased loss of C but drier systems did not. Warming had no consistent effect on aNPP across the climate gradient and Rs increased from drier to wetter sites. Our findings suggest that the above- and belowground C fluxes become decoupled, with no evidence of acclimation at a decadal timescale. aNPP and Rs especially differed in 3 their sensitivity to drought and warming, with belowground processes being more sensitive to environmental change.

UR - https://static-content.springer.com/esm/art%3A10.1038%2Fsrep43952/MediaObjects/41598_2017_BFsrep43952_MOESM21_ESM.pdf

U2 - 10.1038/srep43952

DO - 10.1038/srep43952

M3 - Article

VL - 7

JO - Scientific Reports

JF - Scientific Reports

SN - 2045-2322

M1 - 43952

ER -