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hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorAUGUSTO, Laurent
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorACHAT, David L.
hal.structure.identifierEarth and Life Institute [Louvain-La-Neuve] [ELI]
dc.contributor.authorJONARD, Mathieu
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorVIDAL, David
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorRINGEVAL, Bruno
dc.date.accessioned2024-04-08T12:09:26Z
dc.date.available2024-04-08T12:09:26Z
dc.date.issued2017
dc.identifier.issn1354-1013
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/196575
dc.description.abstractEnBecause the capability of terrestrial ecosystems to fix carbon is constrained by nutrient availability, understanding how nutrients limit plant growth is a key contemporary question. However, what drives nutrient limitations at global scale remains to be clarified. Using global data on plant growth, plant nutritive status, and soil fertility, we investigated to which extent soil parent materials explain nutrient limitations. We found that N limitation was not linked to soil parent materials, but was best explained by climate: ecosystems under harsh (i.e., cold and or dry) climates were more N-limited than ecosystems under more favourable climates. Contrary to N limitation, P limitation was not driven by climate, but by soil parent materials. The influence of soil parent materials was the result of the tight link between actual P pools of soils and physical–chemical properties (acidity, P richness) of soil parent materials. Some other ground-related factors (i.e., soil weathering stage, landform) had a noticeable influence on P limitation, but their role appeared to be relatively smaller than that of geology. The relative importance of N limitation versus P limitation was explained by a combination of climate and soil parent material: at global scale, N limitation became prominent with increasing climatic constraints, but this global trend was modulated at lower scales by the effect of parent materials on P limitation, particularly under climates favourable to biological activity. As compared with soil parent materials, atmospheric deposition had only a weak influence on the global distribution of actual nutrient limitation. Our work advances our understanding of the distribution of nutrient limitation at global scale. In particular, it stresses the need to take soil parent materials into account when investigating plant growth response to environment changes.
dc.language.isoen
dc.publisherWiley
dc.rights.urihttp://creativecommons.org/licenses/by-sa/
dc.subjectdépôt atmosphérique
dc.subjectsubstrat solide
dc.subjectbiodisponibilité
dc.subjectcroissance des plantes
dc.subjectécosystème terrestre
dc.subject.enatmospheric deposition
dc.subject.enbedrock
dc.subject.enbioavailability
dc.subject.ennitrogen limitation
dc.subject.enphosphorus limitation
dc.subject.enplant growth
dc.subject.enterrestrial ecosystems
dc.title.enSoil parent material-A major driver of plant nutrient limitations in terrestrial ecosystems
dc.typeArticle de revue
dc.identifier.doi10.1111/gcb.13691
dc.subject.halSciences du Vivant [q-bio]
bordeaux.journalGlobal Change Biology
bordeaux.page3808–3824
bordeaux.volume23
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue9
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-01608410
hal.version1
hal.popularnon
hal.audienceNon spécifiée
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-01608410v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Global%20Change%20Biology&rft.date=2017&rft.volume=23&rft.issue=9&rft.spage=3808%E2%80%933824&rft.epage=3808%E2%80%933824&rft.eissn=1354-1013&rft.issn=1354-1013&rft.au=AUGUSTO,%20Laurent&ACHAT,%20David%20L.&JONARD,%20Mathieu&VIDAL,%20David&RINGEVAL,%20Bruno&rft.genre=article


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