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稳定同位素标记揭示了温带树苗在芽萌动前的水分和碳通量。

Stable Isotope Labelling Reveals Water and Carbon Fluxes in Temperate Tree Saplings Before Budbreak.

作者信息

Walde Manuel G, Lehmann Marco M, Gessler Arthur, Vitasse Yann, Diao Haoyu

机构信息

Ecosystem Ecology, Forest Dynamics, Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, Switzerland.

Institute of Terrestrial Ecosystems, ETH Zurich (Swiss Federal Institute of Technology), Zurich, Switzerland.

出版信息

Plant Cell Environ. 2025 Jan;48(1):805-817. doi: 10.1111/pce.15173. Epub 2024 Oct 1.

Abstract

Despite considerable experimental effort, the physiological mechanisms governing temperate tree species' water and carbon dynamics before the onset of the growing period remain poorly understood. We applied H-enriched water during winter dormancy to the soil of four potted European tree species. After 8 weeks of chilling, hydrogen isotopes in stem, twig and bud water were measured six times during 2 consecutive weeks of forcing conditions (Experiment 1). Additionally, we pulse-labelled above-ground plant tissues using H-enriched water vapour and C-enriched CO 7 days after exposure to forcing conditions to trace atmospheric water and carbon uptake (Experiment 2). Experiment 1 revealed soil water incorporation into the above-ground organs of all species during the chilling phase and significant species-specific differences in water allocation during the forcing conditions, which we attributed to differences in structural traits. Experiment 2 illustrated water vapour incorporation into all above-ground tissue of all species. However, the incorporation of carbon was found for evergreen saplings only. Our results suggest that temperate trees take up and reallocate soil water and absorb atmospheric water to maintain sufficient above-ground tissue hydration during winter. Therefore, our findings provide new insights into the water allocation dynamics of temperate trees during early spring.

摘要

尽管进行了大量实验研究,但对于温带树种在生长季开始前的水分和碳动态的生理机制仍知之甚少。我们在冬季休眠期向四种盆栽欧洲树种的土壤中施加了富含氢的水。经过8周的低温处理后,在连续2周的催芽条件下对茎、小枝和芽中的氢同位素进行了6次测量(实验1)。此外,在暴露于催芽条件7天后,我们使用富含氢的水蒸气和富含碳的二氧化碳对地上植物组织进行脉冲标记,以追踪大气水分和碳的吸收情况(实验2)。实验1表明,在低温阶段所有树种的地上器官都吸收了土壤水分,并且在催芽条件下水分分配存在显著的物种特异性差异,我们将其归因于结构特征的差异。实验2表明所有树种的地上组织都吸收了水蒸气。然而,仅在常绿幼树中发现了碳的吸收。我们的研究结果表明,温带树木在冬季吸收并重新分配土壤水分,吸收大气水分以维持地上组织的充分水合作用。因此,我们的研究结果为早春温带树木的水分分配动态提供了新的见解。

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