Carbon–nitrogen interactions in European forests and semi-natural vegetation – Part 2: Untangling climatic, edaphic, management and nitrogen deposition effects on carbon sequestration potentials. Flechard, C., R., van Oijen, M., Cameron, D., R., de Vries, W., Ibrom, A., Buchmann, N., Dise, N., B., Janssens, I., A., Neirynck, J., Montagnani, L., Varlagin, A., Loustau, D., Legout, A., Ziemblińska, K., Aubinet, M., Aurela, M., Chojnicki, B., H., Drewer, J., Eugster, W., Francez, A., Juszczak, R., Kitzler, B., Kutsch, W., L., Lohila, A., Longdoz, B., Matteucci, G., Moreaux, V., Neftel, A., Olejnik, J., Sanz, M., J., Siemens, J., Vesala, T., Vincke, C., Nemitz, E., Zechmeister-Boltenstern, S., Butterbach-Bahl, K., Skiba, U., M., & Sutton, M., A. Biogeosciences, 17(6):1621-1654, 3, 2020.
Carbon–nitrogen interactions in European forests and semi-natural vegetation – Part 2: Untangling climatic, edaphic, management and nitrogen deposition effects on carbon sequestration potentials [link]Website  doi  abstract   bibtex   
2.5–3 g N m−2 yr−1) but accompanied by increasingly large ecosystem N losses by leaching and gaseous emissions. The reduced increase in productivity per unit N deposited at high Ndep levels implies that the forecast increased Nr emissions and increased Ndep levels in large areas of Asia may not positively impact the continent's forest CO2 sink. The large level of unexplained variability in observed carbon sequestration efficiency (CSE) across sites further adds to the uncertainty in the dC∕dN response.]]>
@article{
 title = {Carbon–nitrogen interactions in European forests and semi-natural vegetation – Part 2: Untangling climatic, edaphic, management and nitrogen deposition effects on carbon sequestration potentials},
 type = {article},
 year = {2020},
 pages = {1621-1654},
 volume = {17},
 websites = {https://bg.copernicus.org/articles/17/1621/2020/},
 month = {3},
 day = {26},
 id = {fc2c3f17-c623-3881-a69d-3153b9984699},
 created = {2021-02-11T10:41:48.920Z},
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 profile_id = {5c1040db-25e3-36ea-a919-0994a44709e7},
 group_id = {c4af41cc-7e3c-3fd3-9982-bdb923596eee},
 last_modified = {2021-03-02T15:39:02.125Z},
 read = {false},
 starred = {false},
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 confirmed = {true},
 hidden = {false},
 citation_key = {Flechard2020a},
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 abstract = {2.5–3 g N m−2 yr−1) but accompanied by increasingly large ecosystem N losses by leaching and gaseous emissions. The reduced increase in productivity per unit N deposited at high Ndep levels implies that the forecast increased Nr emissions and increased Ndep levels in large areas of Asia may not positively impact the continent's forest CO2 sink. The large level of unexplained variability in observed carbon sequestration efficiency (CSE) across sites further adds to the uncertainty in the dC∕dN response.]]>},
 bibtype = {article},
 author = {Flechard, Chris R. and van Oijen, Marcel and Cameron, David R. and de Vries, Wim and Ibrom, Andreas and Buchmann, Nina and Dise, Nancy B. and Janssens, Ivan A. and Neirynck, Johan and Montagnani, Leonardo and Varlagin, Andrej and Loustau, Denis and Legout, Arnaud and Ziemblińska, Klaudia and Aubinet, Marc and Aurela, Mika and Chojnicki, Bogdan H. and Drewer, Julia and Eugster, Werner and Francez, André-Jean and Juszczak, Radosław and Kitzler, Barbara and Kutsch, Werner L. and Lohila, Annalea and Longdoz, Bernard and Matteucci, Giorgio and Moreaux, Virginie and Neftel, Albrecht and Olejnik, Janusz and Sanz, Maria J. and Siemens, Jan and Vesala, Timo and Vincke, Caroline and Nemitz, Eiko and Zechmeister-Boltenstern, Sophie and Butterbach-Bahl, Klaus and Skiba, Ute M. and Sutton, Mark A.},
 doi = {10.5194/bg-17-1621-2020},
 journal = {Biogeosciences},
 number = {6}
}

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