Forestry and Forest Products Research Institute, Wood Anatomy and Quality Laboratory, Tsukuba 305-8687, Japan.
Tree Physiol. 2022 Nov 8;42(11):2153-2173. doi: 10.1093/treephys/tpac055.
Introductory biology lessons around the world typically teach that plants absorb water through their roots, but, unfortunately, absorption of water through leaves and subsequent transport and use of this water for biomass formation remains a field limited mostly to specialists. Recent studies have identified foliar water uptake as a significant net water source for terrestrial plants. The growing interest in the development of a new model that includes both foliar water uptake (in liquid form) and root water uptake to explain hydrogen and oxygen isotope ratios in leaf water and tree rings demands a method for distinguishing between these two water sources. Therefore, in this study, I have devised a new labelling method that utilizes two different water sources, one enriched in deuterium (HDO + D2O; δD = 7.0 × 10 4‰, δ18O = 4.1‰) and one enriched in oxygen-18 (H218O; δD = -85‰, δ18O = 1.1 × 104‰), to simultaneously label both foliar-absorbed and root-absorbed water and quantify their relative contributions to plant biomass. Using this new method, I here present evidence that, in the case of well-watered Cryptomeria japonica D. Don, hydrogen and oxygen incorporated into new leaf cellulose in the rainy season derives mostly from foliar-absorbed water (69% from foliar-absorbed water and 31% from root-absorbed water), while that of new root cellulose derives mostly from root-absorbed water (20% from foliar-absorbed water and 80% from root-absorbed water), and new branch xylem is somewhere in between (55% from foliar-absorbed water and 45% from root-absorbed water). The dual-labelling method first implemented in this study enables separate and simultaneous labelling of foliar-absorbed and root-absorbed water and offers a new tool to study the uptake, transport and assimilation processes of these waters in terrestrial plants.
全世界的基础生物学课程通常都教授说植物通过根部吸收水分,但遗憾的是,通过叶片吸收水分以及随后将水分运输并用于生物量形成仍然主要局限于专家领域。最近的研究已经确定,叶片吸水是陆地植物的一个重要净水源。由于人们越来越关注开发一种新模型,该模型既包括叶片吸水(以液态形式),也包括根部吸水,以解释叶片水分和树木年轮中的氢和氧同位素比值,因此需要一种方法来区分这两种水源。因此,在这项研究中,我设计了一种新的标记方法,利用两种不同的水源,一种富含氘(HDO+D2O;δD=7.0×10-4‰,δ18O=4.1‰),另一种富含氧-18(H218O;δD=-85‰,δ18O=1.1×10-4‰),同时标记叶片吸收和根部吸收的水分,并量化它们对植物生物量的相对贡献。使用这种新方法,我在这里提供的证据表明,在水分充足的日本柳杉情况下,雨季新叶纤维素中纳入的氢和氧主要来自叶片吸收的水分(叶片吸收的水分占 69%,根部吸收的水分占 31%),而新根纤维素的水分主要来自根部吸收的水分(叶片吸收的水分占 20%,根部吸收的水分占 80%),新树枝木质部则介于两者之间(叶片吸收的水分占 55%,根部吸收的水分占 45%)。本研究首次实施的双标记方法能够分别和同时标记叶片吸收和根部吸收的水分,为研究陆地植物对这些水分的吸收、运输和同化过程提供了一种新工具。