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在新热带草原中,不同生长型对水分的获取存在分区:草本植物是否开拓了第三个水分获取小生境?

The partitioning of water uptake between growth forms in a Neotropical savanna: do herbs exploit a third water source niche?

机构信息

Pós Graduação em Ecologia, Departamento de Ecologia, Instituto de Ciências Biológicas, Universidade de Brasília, Brasília, Brazil.

出版信息

Plant Biol (Stuttg). 2013 Jan;15(1):84-92. doi: 10.1111/j.1438-8677.2012.00618.x. Epub 2012 Jun 5.

Abstract

In addition to trees and grasses, the savannas of central Brazil are characterised by a diverse herbaceous dicot flora. Here we tested whether the coexistence of a highly diversified assemblage of species resulted in stratification or strong overlap in the use of soil water resources. We measured oxygen and hydrogen isotope ratios of stem water from herbs, grasses and trees growing side by side, as well as the isotopic composition of water in soil profile, groundwater and rainfall, and predawn (Ψ(pd)) and midday (Ψ(md)) leaf water potentials. We used a stable isotope mixing model to estimate vertical partitioning of soil water by the three growth forms. Grasses relied on shallow soil water (5-50 cm) and were strongly anisohydric. Ψ(pd) and Ψ(md) decreased significantly from the wet to the dry season. Trees extracted water from deeper regions of the soil profile (60-120 cm) and were isohydric. Ψ(pd) and Ψ(md) did not change from the wet to the dry season. Herbs overlapped with grasses in patterns of water extraction in the dry season (between 10 and 40 cm), but they took up water at soil depths intermediate (70-100 cm) to those of trees and grasses during the wet season. They showed seasonal changes in Ψ(pd) but not in Ψ(md). We conclude that vertical partitioning of soil water may have contributed to coexistence of these three growth forms and resulted in a more complex pattern of soil water extraction than the two-compartment model of soil water uptake currently used to explain the structure and function of tropical savanna ecosystems.

摘要

除了树木和草类,巴西中部稀树草原的特征还在于其多样化的草本双子叶植物群。在这里,我们检验了高度多样化的物种组合共存是否会导致对土壤水资源的分层或强烈重叠利用。我们测量了与树木和草类生长在一起的草本植物的茎水的氧和氢同位素比值,以及土壤剖面、地下水和降雨中的水的同位素组成,以及预日(Ψ(pd))和日中(Ψ(md))叶片水势。我们使用稳定同位素混合模型来估计三种生长形式对土壤水分的垂直分配。草类依赖于浅层土壤水(5-50 厘米),并且强烈的非等水。从湿到干季,Ψ(pd)和 Ψ(md)显著降低。树木从土壤剖面较深的区域(60-120 厘米)提取水分,是等水的。从湿到干季,Ψ(pd)和 Ψ(md)没有变化。草本植物在旱季与草类的水分提取模式重叠(在 10 到 40 厘米之间),但在雨季,它们吸收的水分在深度上介于树木和草类之间(70-100 厘米)。它们表现出预日(pd)的季节性变化,但日中(md)没有变化。我们得出结论,土壤水分的垂直分配可能有助于这三种生长形式的共存,并导致比目前用于解释热带稀树草原生态系统结构和功能的土壤水分吸收两室模型更复杂的土壤水分提取模式。

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