Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/24836
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dc.contributor.authorMatías, Luisen_UK
dc.contributor.authorLinares, Juan Cen_UK
dc.contributor.authorSánchez-Miranda, Ángelaen_UK
dc.contributor.authorJump, Alistair Sen_UK
dc.date.accessioned2017-10-02T23:35:11Z-
dc.date.available2017-10-02T23:35:11Z-
dc.date.issued2017-10en_UK
dc.identifier.urihttp://hdl.handle.net/1893/24836-
dc.description.abstractOngoing changes in global climate are altering ecological conditions for many species. The consequences of such changes are typically most evident at the edge of a species’ geographical distribution, where differences in growth or population dynamics may result in range expansions or contractions. Understanding population responses to different climatic drivers along wide latitudinal and altitudinal gradients is necessary in order to gain a better understanding of plant responses to ongoing increases in global temperature and drought severity. We selected Scots pine (Pinus sylvestrisL.) as a model species to explore growth responses to climatic variability (seasonal temperature and precipitation) over the last century through dendrochronological methods. We developed linear models based on age, climate and previous growth to forecast growth trends up to year 2100 using climatic predictions. Populations were located at the treeline across a latitudinal gradient covering the northern, central and southernmost populations and across an altitudinal gradient at the southern edge of the distribution (treeline, medium and lower elevations). Radial growth was maximal at medium altitude and treeline of the southernmost populations. Temperature was the main factor controlling growth variability along the gradients, although the timing and strength of climatic variables affecting growth shifted with latitude and altitude. Predictive models forecast a general increase in Scots pine growth at treeline across the latitudinal distribution, with southern populations increasing growth up to year 2050, when it stabilises. The highest responsiveness appeared at central latitude, and moderate growth increase is projected at the northern limit. Contrastingly, the model forecasted growth decline at lowland-southern populations, suggesting an upslope range displacement over the coming decades. Our results give insight into the geographical responses of tree species to climate change and demonstrate the importance of incorporating biogeographical variability into predictive models for an accurate prediction of species dynamics as climate changes.en_UK
dc.language.isoenen_UK
dc.publisherWiley-Blackwellen_UK
dc.relationMatías L, Linares JC, Sánchez-Miranda Á & Jump AS (2017) Contrasting growth forecasts across the geographical range of Scots pine due to altitudinal and latitudinal differences in climatic sensitivity. Global Change Biology, 23 (10), pp. 4106-4116. https://doi.org/10.1111/gcb.13627en_UK
dc.rightsThis item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. This is the peer reviewed version of the following article: Matías, L., Linares, J. C., Sánchez-Miranda, Á. and Jump, A. S. (2017), Contrasting growth forecasts across the geographical range of Scots pine due to altitudinal and latitudinal differences in climatic sensitivity. Glob Change Biol, 23: 4106–4116, which has been published in final form at https://doi.org/10.1111/gcb.13627. This article may be used for non-commercial purposes in accordance With Wiley Terms and Conditions for self-archiving.en_UK
dc.subjectClimateen_UK
dc.subjectDendrochronologyen_UK
dc.subjectDistributionen_UK
dc.subjectGrowthen_UK
dc.subjectModellingen_UK
dc.subjectPinus sylvestrisen_UK
dc.titleContrasting growth forecasts across the geographical range of Scots pine due to altitudinal and latitudinal differences in climatic sensitivityen_UK
dc.typeJournal Articleen_UK
dc.rights.embargoreason[Matias_et_al_Growth_forecast_Resubmission_Final.pdf] Publisher requires embargo of 12 months after formal online publication.en_UK
dc.identifier.doi10.1111/gcb.13627en_UK
dc.identifier.pmid28100041en_UK
dc.citation.jtitleGlobal Change Biologyen_UK
dc.citation.issn1365-2486en_UK
dc.citation.issn1354-1013en_UK
dc.citation.volume23en_UK
dc.citation.issue10en_UK
dc.citation.spage4106en_UK
dc.citation.epage4116en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusAM - Accepted Manuscripten_UK
dc.contributor.funderEuropean Commissionen_UK
dc.author.emaila.s.jump@stir.ac.uken_UK
dc.citation.date15/02/2017en_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.contributor.affiliationUniversidad Pablo de Olavideen_UK
dc.contributor.affiliationUniversity of Stirlingen_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.identifier.isiWOS:000410642100013en_UK
dc.identifier.scopusid2-s2.0-85013662079en_UK
dc.identifier.wtid539233en_UK
dc.contributor.orcid0000-0002-2167-6451en_UK
dc.date.accepted2017-01-09en_UK
dcterms.dateAccepted2017-01-09en_UK
dc.date.filedepositdate2017-01-26en_UK
dc.relation.funderprojectCan altitudinal data predict latitudinal responses of plants to climate change?en_UK
dc.relation.funderrefFP7-PEOPLE-2001-IEFen_UK
rioxxterms.apcnot requireden_UK
rioxxterms.typeJournal Article/Reviewen_UK
rioxxterms.versionAMen_UK
local.rioxx.authorMatías, Luis|en_UK
local.rioxx.authorLinares, Juan C|en_UK
local.rioxx.authorSánchez-Miranda, Ángela|en_UK
local.rioxx.authorJump, Alistair S|0000-0002-2167-6451en_UK
local.rioxx.projectFP7-PEOPLE-2001-IEF|European Commission (Horizon 2020)|en_UK
local.rioxx.freetoreaddate2018-02-16en_UK
local.rioxx.licencehttp://www.rioxx.net/licenses/under-embargo-all-rights-reserved||2018-02-15en_UK
local.rioxx.licencehttp://www.rioxx.net/licenses/all-rights-reserved|2018-02-16|en_UK
local.rioxx.filenameMatias_et_al_Growth_forecast_Resubmission_Final.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source1354-1013en_UK
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