1. Decoupling of Tree‐Ring Cellulose δ18O and δ2H Highlighted by Their Contrasting Relationships to Climate and Tree Intrinsic Variables.
- Author
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Charlet de Sauvage, Justine, Saurer, Matthias, Treydte, Kerstin, and Lévesque, Mathieu
- Subjects
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SILVER fir , *TREE age , *CROWNS (Botany) , *SPRING , *STABLE isotopes - Abstract
ABSTRACT Oxygen (
δ 18O) and hydrogen (δ 2H) stable isotope ratios are tightly coupled in precipitation and, albeit damped, in leaf water, but are often decoupled in tree‐ring cellulose. The environmental and physiological conditions in which this decoupling occurs are not yet well understood. We investigated the relationships betweenδ 18O andδ 2H and tree‐ring width (TRW), tree crown volume, tree age and climate in silver fir and Douglas‐fir and found substantial differences betweenδ 18O andδ 2H. Overall,δ 18O–δ 2H correlations were weak to absent but became significantly negative under high summer vapour pressure deficit (VPD).δ 18O andδ 2H had positive and negative nonlinear relationships with TRW, respectively, with clear relationships at the site and tree levels for silver fir and, to a lesser extent, for Douglas‐fir. Age trends for silver fir were weakly negative inδ 18O but positive inδ 2H. Tree crown volume andδ 18O orδ 2H had no significant relationships. Most strikingly,δ 18O strongly depended on spring climate (precipitation and VPD), whereasδ 2H depended on summer climate (temperature and VPD) for both species. Our study shows that theδ 18O–δ 2H decoupling in tree‐ring cellulose in two temperate conifer species could be highlighted by their contrasting relationships to climate and tree intrinsic variables (TRW, age). [ABSTRACT FROM AUTHOR]- Published
- 2024
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