Data from: Isotopic methods for non-destructive assessment of carbon dynamics in shrublands under long-term climate change manipulation

Andresen LC, Dominguez MT, Reinsch S, Smith AR, Schmidt IK, Ambus P, Beier C, Boeckx P, Bol R, de Dato G, Emmett BA, Estiarte M, Garnett MH, Kröel-Dulay G, Mason SL, Nielsen CS, Penuelas J, Tietema A

Date Published: January 12, 2018

DOI: https://doi.org/10.5061/dryad.mc460

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Title PLANT_ISOTOPES
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Description Isotopic signal (13C and 15N) of plant responses to precipitation across the INCREASE experimental network (Data in Box 1A from Andresen et al., 2018).
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Title 14C_RESPIRATION
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Description Values of the 14C signature (natural abundance) of CO2 in soil efflux samples, collected at the Peaknaze site (UK) (Data in Box 2B from Andresen et al., 2018).
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Title 13CPLFA_DK
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Description Results of a 13C-CO2 pulse experiment conducted at the Brandbjerg site (Denmark). Values of recovery of 13C (% from added 13C) in PLFA of soil Gram-negative bacteria, at different times since 13C pulse (Data in Box 3C from Andresen et al., 2018).
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Title 14C_kinetics
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Description Results of an experiment on microbial mineralisation of carbon compounds, using low-molecular weight carbon substrates labelled with 14C. Values in this file show the exponential decay kinetics for 14C-CO2 evolution during microbial 14C substrate mineralisation (Data in Box 4A from Andresen et al., 2018).
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Title 14C_halflife
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Description Results of an experiment on microbial mineralisation of carbon compounds, using low-molecular weight carbon substrates labelled with 14C. Values correspond to half-life of added 14C-sugars in the soil solution of samples collected across the INCREASE network. Mean annual temperature of each site indicated (Data in Box 4B from Andresen et al., 2018).
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Title CALLUNA_ISOTOPES
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Description Values of δ13C in Calluna vulgaris leaves and annual precipitation of year before sample collection (Data in Box 1B from Andresen et al., 2018).
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Title 13CPLFA_UK
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Description Results of a 13C-CO2 pulse experiment conducted along a gradient of soil moisture at the Clocaenog site (UK). Values correspond to 13C content in different phospholipid-derived fatty-acid methyl esters (FAMEs) extracted from soils after the 13C-pulse (Data in Box 3B from Andresen et al., 2018).
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When using this data, please cite the original publication:

Andresen LC, Dominguez MT, Reinsch S, Smith AR, Schmidt IK, Ambus P, Beier C, Boeckx P, Bol R, de Dato G, Emmett BA, Estiarte M, Garnett MH, Kröel-Dulay G, Mason SL, Nielsen CS, Penuelas J, Tietema A (2018) Isotopic methods for non-destructive assessment of carbon dynamics in shrublands under long-term climate change manipulation. Methods in Ecology and Evolution, online in advance of print. https://doi.org/10.1111/2041-210x.12963

Additionally, please cite the Dryad data package:

Andresen LC, Dominguez MT, Reinsch S, Smith AR, Schmidt IK, Ambus P, Beier C, Boeckx P, Bol R, de Dato G, Emmett BA, Estiarte M, Garnett MH, Kröel-Dulay G, Mason SL, Nielsen CS, Penuelas J, Tietema A (2018) Data from: Isotopic methods for non-destructive assessment of carbon dynamics in shrublands under long-term climate change manipulation. Dryad Digital Repository. https://doi.org/10.5061/dryad.mc460
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