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Beyond width and density: stable carbon and oxygen isotopes in cork-rings provide insights of physiological responses to water stress in Quercus suber L

dc.contributor.authorCosta, Augusta
dc.contributor.authorCherubini, Paolo
dc.contributor.authorGraça, José
dc.contributor.authorSpiecker, Heinrich
dc.contributor.authorBarbosa, Inês
dc.contributor.authorMáguas, C.
dc.date.accessioned2022-12-02T15:09:06Z
dc.date.available2022-12-02T15:09:06Z
dc.date.issued2022-11
dc.description.abstractAs climate change increasingly affects forest ecosystems, detailed understanding of major effects is important to anticipate their consequences under future climate scenarios. The Mediterranean region is a prominent climate change hotspot, and evergreen cork oak (Quercus suber L.) woodlands are particularly climatically sensitive due to cork (bark) harvesting. Cork oak’s drought avoidance strategy is well-known and includes structural and physiological adaptations that maximise soil water uptake and transport and limit water use, potentially leading to reduced stem and cork growth. Trees’ responses to cope with water-limited conditions have been extensively described based on cork-rings width and, more recently, on cork-rings density, in dendroecological studies. However, so far, tree functional attributes and physiological strategies, namely photosynthetic metabolism adjustments affecting cork formation, have never been addressed and/or integrated on these previous cork-rings-based studies. In this study, we address the relation between carbon and oxygen stable isotopes of cork rings and precipitation and temperature, in two distinct locations of southwestern Portugal–the (wetter) Tagus basin peneplain and the (drier) Grândola mountains. We aimed at assessing whether the two climatic factors affect cork-ring isotopic composition under contrasting conditions of water availability, and, therefore, if carbon and oxygen signatures in cork can reflect tree functional (physiological and structural) responses to stressful conditions, which might be aggravated by climate change. Our results indicate differences between the study areas. At the drier site, the stronger statistically significant negative cork δ13C correlations were found with mean temperature, whereas strong positive cork δ18O correlations were fewer and found only with precipitation. Moreover, at the wetter site, cork rings are enriched in 18O and depleted in 13C, indicating, respectively, shallow groundwater as the water source for physiological processes related with biosynthesis of non-photosynthetic secondary tissues, such as suberin, and a weak stomatal regulation under high water availability, consistent with non-existent water availability constrains. In contrast, at the drier site, trees use water from deeper ground layers, depleted in 18O, and strongly regulate stomatal conductance under water stress, thus reducing photosynthetic carbon uptake and probably relying on stored carbon reserves for cork ring formation. These results suggest that although stable isotopes signatures in cork rings are not proxies for net growth, they may be (fairly) robust indicators of trees’ physiological and structural adjustments to climate and environmental changes in Mediterranean environments.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationCosta A, Cherubini P, Graça J, Spiecker H, Barbosa I, Máguas C. 2022. Beyond width and density: stable carbon and oxygen isotopes in cork-rings provide insights of physiological responses to water stress in Quercus suber L. PeerJ 10:e14270 https://doi.org/10.7717/peerj.14270pt_PT
dc.identifier.doi10.7717/peerj.14270pt_PT
dc.identifier.urihttp://hdl.handle.net/10451/55325
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherPeerJpt_PT
dc.relationFCT EXPL/AGR-FOR/1220/2012pt_PT
dc.relationFCT UID/AMB/04085/2013pt_PT
dc.relationFCT UIDB/00239/2020pt_PT
dc.relationFCT PTDC/BIA-FBT/29704-2017pt_PT
dc.relationFCT SFRH/BPD/97166/2013; CEEINST/00012/2018—ENGFLpt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.titleBeyond width and density: stable carbon and oxygen isotopes in cork-rings provide insights of physiological responses to water stress in Quercus suber Lpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.startPagee14270pt_PT
oaire.citation.titlePeerJpt_PT
oaire.citation.volume10pt_PT
person.familyNameMaria Filipe Máguas da Silva Hanson
person.givenNameCristina
person.identifier.ciencia-idAC15-C40D-D0A2
person.identifier.orcid0000-0002-4396-7073
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication55a08da9-2d04-420e-944a-417db0467301
relation.isAuthorOfPublication.latestForDiscovery55a08da9-2d04-420e-944a-417db0467301

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