Karst fissures mitigate the negative effects of drought on plant growth and photosynthetic physiology

IF 2.3 2区 环境科学与生态学 Q2 ECOLOGY Oecologia Pub Date : 2024-04-29 DOI:10.1007/s00442-024-05556-5
Jie Luo, Wei-xue Luo, Jun-ting Liu, Yong-jian Wang, Zong-feng Li, Jian-ping Tao, Jin-chun Liu
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Abstract

Hard limestone substrates, which are extensively distributed, are believed to exacerbate drought and increase the difficulty of restoration in vulnerable karst regions. Fissures in such substrates may alleviate the negative effect of drought on plants, but the underlying mechanisms remain poorly understood. In a two-way factorial block design, the growth and photosynthesis of 2-year-old Phoebe zhennan seedlings were investigated in two water availabilities (high versus low) and three stimulated fissure habitat groups (soil, soil-filled fissure and non-soil-filled fissure). Moreover, the fissure treatments included both small and big fissures. Compared to the soil group, the non-soil-filled fissure group had decreased the total biomass, root biomass, total root length, and the root length of fine roots in the soil layer at both water availabilities, but increased net photosynthetic rate (Pn) and retained stable water use efficiency (WUE) at low water availability. However, there were no significant differences between the soil-filled fissure group and soil group in the biomass accumulation and allocation as well as Pn. Nevertheless, the SF group decreased the root distribution in total and in the soil layer, and also increased WUE at low water availability. Across all treatments, fissure size had no effect on plant growth or photosynthesis. Karst fissures filled with soil can alleviate drought impacts on plant root growth, which involves adjusting root distribution strategies and increasing water use efficiency. These results suggest that rock fissures can be involved in long-term plant responses to drought stress and vegetation restoration in rocky mountain environments under global climate change.

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喀斯特裂缝减轻了干旱对植物生长和光合生理的负面影响
分布广泛的坚硬石灰岩基质被认为会加剧干旱,增加脆弱岩溶地区的恢复难度。此类基质中的裂隙可能会减轻干旱对植物的负面影响,但其潜在机制仍鲜为人知。在一个双向因子区组设计中,研究了在两种水分利用率(高与低)和三种受刺激的裂隙生境组(土壤、充满土壤的裂隙和非充满土壤的裂隙)中,2 年生浙贝母幼苗的生长和光合作用。此外,裂缝处理包括小裂缝和大裂缝。与土壤组相比,非充满土壤的裂缝组在两种供水条件下土壤层的总生物量、根生物量、总根长和细根根长都有所下降,但在低供水条件下净光合速率(Pn)有所提高,水分利用效率(WUE)保持稳定。然而,土壤填充裂缝组与土壤组在生物量积累和分配以及 Pn 方面没有显著差异。然而,SF 组减少了根系在整个土壤层和土壤层中的分布,也增加了低水分供应时的 WUE。在所有处理中,裂缝大小对植物生长和光合作用没有影响。岩溶裂隙填充土壤可以减轻干旱对植物根系生长的影响,这包括调整根系分布策略和提高水分利用效率。这些结果表明,在全球气候变化的情况下,岩石裂缝可参与植物对干旱胁迫的长期响应和岩石山地环境的植被恢复。
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来源期刊
Oecologia
Oecologia 环境科学-生态学
CiteScore
5.10
自引率
0.00%
发文量
192
审稿时长
5.3 months
期刊介绍: Oecologia publishes innovative ecological research of international interest. We seek reviews, advances in methodology, and original contributions, emphasizing the following areas: Population ecology, Plant-microbe-animal interactions, Ecosystem ecology, Community ecology, Global change ecology, Conservation ecology, Behavioral ecology and Physiological Ecology. In general, studies that are purely descriptive, mathematical, documentary, and/or natural history will not be considered.
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