Vis enkel innførsel

dc.contributor.authorDox, Inge
dc.contributor.authorGričar, Jožica
dc.contributor.authorMarchand, Lorène Julia
dc.contributor.authorLeys, Sebastien
dc.contributor.authorZuccarini, Paolo
dc.contributor.authorGeron, Charly
dc.contributor.authorPrislan, Peter
dc.contributor.authorMariën, Bertold
dc.contributor.authorFonti, Patrick
dc.contributor.authorLange, Holger
dc.contributor.authorPeñuelas, Josep
dc.contributor.authorVan den Bulcke, Jan
dc.contributor.authorCampioli, Matteo
dc.date.accessioned2020-10-02T11:21:49Z
dc.date.available2020-10-02T11:21:49Z
dc.date.created2020-07-15T11:29:28Z
dc.date.issued2020-04-27
dc.identifier.citationTree Physiology, Volume 40, Issue 8, August 2020, Pages 1001–1013en_US
dc.identifier.issn0829-318X
dc.identifier.urihttps://hdl.handle.net/11250/2680905
dc.description.abstractCessation of xylem formation or wood growth (CWG) and onset of foliar senescence (OFS) are key autumn phenological events in temperate deciduous trees. Their timing is fundamental for the development and survival of trees, ecosystem nutrient cycling and the seasonal exchange of matter and energy between the biosphere and atmosphere, and affects the impact and feedback of forests to global change. A large-scale experimental effort and improved observational methods have allowed us to compare the timing of CWG and OFS for different deciduous tree species in Western Europe, particularly in silver birch, a pioneer species, and European beech, a late-succession species, at stands of different latitudes, of different levels of site fertility, for 2 years with contrasting meteorological and drought conditions, i.e., the low moderately dry 2017 and the extremely dry 2018. Specifically, we tested whether foliar senescence started before, after or concurrently with CWG. Onset of foliar senescence and CWG occurred generally between late September and early November, with larger differences across species and sites for OFS. Foliar senescence started concurrently with CWG in most cases, except for the drier 2018 and, for beech, at the coldest site, where OFS occurred significantly later than CWG. The behavior of beech in Spain, the southern edge of its European distribution, was unclear, with no CWG, but very low wood growth at the time of OFS. Our study suggests that OFS is generally triggered by the same drivers of CWG or when wood growth decreases in late summer, indicating an overarching mechanism of sink limitation as a possible regulator of the timing of foliar senescence.en_US
dc.language.isoengen_US
dc.publisherOxford University Pressen_US
dc.rightsNavngivelse-Ikkekommersiell 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/deed.no*
dc.titleTimeline of autumn phenology in temperate deciduous treesen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© The Author(s) 2020en_US
dc.source.pagenumber1001–1013en_US
dc.source.volume40en_US
dc.source.journalTree Physiologyen_US
dc.source.issue8en_US
dc.identifier.doi10.1093/treephys/tpaa058
dc.identifier.cristin1819458
dc.relation.projectEC/H2020/714916en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel

Navngivelse-Ikkekommersiell 4.0 Internasjonal
Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse-Ikkekommersiell 4.0 Internasjonal