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dc.creatorDirnboeck, Thomas
dc.creatorProell, Gisela
dc.creatorAustnes, Kari
dc.creatorBeloica, Jelena
dc.creatorBeudert, Burkhard
dc.creatorCanullo, Roberto
dc.creatorDe Marco, Alessandra
dc.creatorFornasier, Maria Francesca
dc.creatorFutter, Martyn
dc.creatorGoergen, Klaus
dc.creatorGrandin, Ulf
dc.creatorHolmberg, Maria
dc.creatorLindroos, Antti-Jussi
dc.creatorMirtl, Michael
dc.creatorNeirynck, Johan
dc.creatorPecka, Tomasz
dc.creatorNieminen, Tiina Maileena
dc.creatorNordbakken, Jorn-Frode
dc.creatorPosch, Maximilian
dc.creatorReinds, Gert-Jan
dc.creatorRowe, Edwin C.
dc.creatorSalemaa, Maija
dc.creatorScheuschner, Thomas
dc.creatorStarlinger, Franz
dc.creatorUzieblo, Aldona Katarzyna
dc.creatorValinia, Salar
dc.creatorWeldon, James
dc.creatorWamelink, Wieger G. W.
dc.creatorForsius, Martin
dc.date.accessioned2024-12-20T13:30:49Z
dc.date.available2024-12-20T13:30:49Z
dc.date.issued2018
dc.identifier.issn1748-9326
dc.identifier.urihttps://omorika.sfb.bg.ac.rs/handle/123456789/964
dc.description.abstractAtmospheric nitrogen (N) pollution is considered responsible for a substantial decline in plant species richness and for altered community structures in terrestrial habitats worldwide. Nitrogen affects habitats through direct toxicity, soil acidification, and in particular by favoring fast-growing species. Pressure from N pollution is decreasing in some areas. In Europe (EU28), overall emissions ofNO(x) declined by more than 50% while NH3 declined by less than 30% between the years 1990 and 2015, and further decreases may be achieved. The timescale over which these improvements will affect ecosystems is uncertain. Here we use 23 European forest research sites with high quality long-term data on deposition, climate, soil recovery, and understory vegetation to assess benefits of currently legislated N deposition reductions in forest understory vegetation. A dynamic soil model coupled to a statistical plant species niche model was applied with site-based climate and deposition. We use indicators of N deposition and climate warming effects such as the change in the occurrence of oligophilic, acidophilic, and cold-tolerant plant species to compare the present with projections for 2030 and 2050. The decrease in N deposition under current legislation emission (CLE) reduction targets until 2030 is not expected to result in a release from eutrophication. Albeit the model predictions show considerable uncertainty when compared with observations, they indicate that oligophilic forest understory plant species will further decrease. This result is partially due to confounding processes related to climate effects and to major decreases in sulphur deposition and consequent recovery from soil acidification, but shows that decreases in N deposition under CLE will most likely be insufficient to allow recovery from eutrophication.en
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/654359/EU//
dc.relationInternational Cooperative Programs Integrated Monitoring and Forests under the LRTAP Convention
dc.relationNERC [ceh020015] Funding Source: UKRI
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceEnvironmental Research Letters
dc.subjectmodellingen
dc.subjectLTERen
dc.subjectLRTAP Conventionen
dc.subjectforest ecosystemen
dc.subjectclimate changeen
dc.subjectair pollutionen
dc.titleCurrently legislated decreases in nitrogen deposition will yield only limited plant species recovery in European forestsen
dc.typearticle
dc.rights.licenseBY
dc.citation.issue12
dc.citation.other13(12): -
dc.citation.rankaM21
dc.citation.volume13
dc.identifier.doi10.1088/1748-9326/aaf26b
dc.identifier.fulltextomorika.sfb.bg.ac.rs/bitstream/id/1069/961.pdf
dc.identifier.rcubconv_1386
dc.identifier.scopus2-s2.0-85060126024
dc.identifier.wos000453617600003
dc.type.versionpublishedVersion


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