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Soil properties as key predictors of global grassland production: have we overlooked micronutrients?
Radujković, D., Verbruggen, E., Seabloom, E. W., Bahn, M., Biederman, L. A., Borer, E. T., … Vicca, S. (2021). Soil properties as key predictors of global grassland production: have we overlooked micronutrients? Ecology Letters, 24(12), 2713-2725. https://doi.org/10.1111/ele.13894
Negative effects of nitrogen override positive effects of phosphorus on grassland legumes worldwide
Tognetti, P. M., Prober, S. M., Báez, S., Chaneton, E. J., Firn, J., Risch, A. C., … Sankaran, M. (2021). Negative effects of nitrogen override positive effects of phosphorus on grassland legumes worldwide. Proceedings of the National Academy of Sciences of the United States of America PNAS, 118(28), e2023718118 (8 pp.). https://doi.org/10.1073/pnas.2023718118
Herbivory and eutrophication mediate grassland plant nutrient responses across a global climatic gradient
Anderson, T. M., Griffith, D. M., Grace, J. B., Lind, E. M., Adler, P. B., Biederman, L. A., … Borer, E. T. (2018). Herbivory and eutrophication mediate grassland plant nutrient responses across a global climatic gradient. Ecology, 99(4), 822-831. https://doi.org/10.1002/ecy.2175
Long-term tracing of whole catchment <sup>15</sup>N additions in a mountain spruce forest: measurements and simulations with the TRACE model
Krause, K., Providoli, I., Currie, W. S., Bugmann, H., & Schleppi, P. (2012). Long-term tracing of whole catchment 15N additions in a mountain spruce forest: measurements and simulations with the TRACE model. Trees: Structure and Function, 26(6), 1683-1702. https://doi.org/10.1007/s00468-012-0737-0
Impact of different nitrogen emission sources on tree physiology as assessed by a triple stable isotope approach
Guerrieri, M. R., Siegwolf, R. T. W., Saurer, M., Jäggi, M., Cherubini, P., Ripullone, F., & Borghetti, M. (2009). Impact of different nitrogen emission sources on tree physiology as assessed by a triple stable isotope approach. Atmospheric Environment, 43(2), 410-418. https://doi.org/10.1016/j.atmosenv.2008.08.042
Immobilization, stabilization and remobilization of nitrogen in forest soils at elevated CO&lt;sub&gt;2&lt;/sub&gt;: a &lt;sup&gt;15&lt;/sup&gt;N and &lt;sup&gt;13&lt;/sup&gt;C tracer study
Hagedorn, F., Maurer, S., Bucher, J. B., & Siegwolf, R. T. W. (2005). Immobilization, stabilization and remobilization of nitrogen in forest soils at elevated CO2: a 15N and 13C tracer study. Global Change Biology, 11(10), 1816-1827. https://doi.org/10.1111/j.1365-2486.2005.01041.x
Increased N deposition retards mineralization of old soil organic matter
Hagedorn, F., Spinnler, D., & Siegwolf, R. (2003). Increased N deposition retards mineralization of old soil organic matter. Soil Biology and Biochemistry, 35(12), 1683-1692. https://doi.org/10.1016/j.soilbio.2003.08.015
Biomass and nutrient concentrations in the foliage of beech (Fagus sylvatica L.) and Norway spruce (Picea abies) plants of a model ecosystem in response to a 4-year exposure to atmospheric CO<sub>2</sub> enrichment and increased N deposition
Landolt, W., Egli, P., Pezzotta, D., & Bucher, J. B. (2003). Biomass and nutrient concentrations in the foliage of beech (Fagus sylvatica L.) and Norway spruce (Picea abies) plants of a model ecosystem in response to a 4-year exposure to atmospheric CO2 enrichment and increased N deposition. Ekologia Bratislava, 22(1), 176-188.
Elevated CO<SUB>2</SUB> influences nutrient availability in young beech-spruce communities on two soil types
Hagedorn, F., Landolt, W., Tarjan, D., Egli, P., & Bucher, J. B. (2002). Elevated CO2 influences nutrient availability in young beech-spruce communities on two soil types. Oecologia, 132(1), 109-117. https://doi.org/10.1007/s00442-002-0937-1
Elevated atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and increased N deposition effects on dissolved organic carbon—clues from &lt;em&gt;δ&lt;/em&gt;&lt;sup&gt;13&lt;/sup&gt;C signature&lt;br /&gt;  
Hagedorn, F., Blaser, P., & Siegwolf, R. (2002). Elevated atmospheric CO2 and increased N deposition effects on dissolved organic carbon—clues from δ13C signature
 . Soil Biology and Biochemistry, 34(3), 355-366. https://doi.org/10.1016/S0038-0717(01)00191-2
Effects of elevated atmospheric CO<sub>2</sub> and increased N deposition on dissolved organic carbon - clues from δ<sup>13</sup>C signature
Hagedorn, F., Blaser, P., & Siegwolf, R. (2001). Effects of elevated atmospheric CO2 and increased N deposition on dissolved organic carbon - clues from δ13C signature. In O. K. Broggaard, J. A. Jørgensen, & L. H. Rasmussen (Eds.), 8th Nordic IHSS symposium on humic substances - characterisation, dynamics, transport and effects (pp. 76-79). International Humic Substances Society.
Responses of N fluxes and pools to elevated atmospheric CO<SUB>2</SUB> in model forest ecosystems with acidic and calcareous soils
Hagedorn, F., Bucher, J. B., Tarjan, D., Rusert, P., & Bucher-Wallin, I. (2000). Responses of N fluxes and pools to elevated atmospheric CO2 in model forest ecosystems with acidic and calcareous soils. Plant and Soil, 224(2), 273-286. https://doi.org/10.1023/A:1004831401190