Yu Kailiang, Foster Adrianna
Department of Environmental Sciences, University of Virginia, Charlottesville, VA, 22904, USA.
Oecologia. 2016 Apr;180(4):1113-25. doi: 10.1007/s00442-015-3518-9. Epub 2015 Dec 28.
Past studies have largely focused on hydraulic redistribution (HR) in trees, shrubs, and grasses, and recognized its role in interspecies interactions. HR in plants that conduct crassulacean acid metabolism (CAM), however, remains poorly investigated, as does the effect of HR on transpiration in different vegetation associations (i.e., tree-grass, CAM-grass, and tree-CAM associations). We have developed a mechanistic model to investigate the net direction and magnitude of HR at the patch scale for tree-grass, CAM-grass, and tree-CAM associations at the growing season to yearly timescale. The modeling results show that deep-rooted CAM plants in CAM-grass associations could perform hydraulic lift at a higher rate than trees in tree-grass associations in a relatively wet environment, as explained by a significant increase in grass transpiration rate in the shallow soil layer, balancing a lower transpiration rate by CAM plants. By comparison, trees in tree-CAM associations may perform hydraulic descent at a higher rate than those in tree-grass associations in a dry environment. Model simulations also show that hydraulic lift increases the transpiration of shallow-rooted plants, while hydraulic descent increases that of deep-rooted plants. CAM plants transpire during the night and thus perform HR during the day. Based on these model simulations, we suggest that the ability of CAM plants to perform HR at a higher rate may have different effects on the surrounding plant community than those of plants with C3 or C4 photosynthetic pathways (i.e., diurnal transpiration).
过去的研究主要集中在树木、灌木和草本植物中的水分再分配(HR),并认识到其在种间相互作用中的作用。然而,进行景天酸代谢(CAM)的植物中的HR研究仍然很少,HR对不同植被组合(即树-草、CAM-草和树-CAM组合)蒸腾作用的影响也是如此。我们开发了一个机理模型,以研究生长季节到年度时间尺度上,树-草、CAM-草和树-CAM组合在斑块尺度上HR的净方向和大小。模拟结果表明,在相对湿润的环境中,CAM-草组合中的深根CAM植物比树-草组合中的树木能以更高的速率进行水分提升,这可以通过浅层土壤中草本植物蒸腾速率的显著增加来解释,从而平衡了CAM植物较低的蒸腾速率。相比之下,在干旱环境中,树-CAM组合中的树木可能比树-草组合中的树木以更高的速率进行水分下降。模型模拟还表明,水分提升增加了浅根植物的蒸腾作用,而水分下降则增加了深根植物的蒸腾作用。CAM植物在夜间进行蒸腾作用,因此在白天进行水分再分配。基于这些模型模拟,我们认为CAM植物以更高速率进行水分再分配的能力,可能对周围植物群落产生与具有C3或C4光合途径的植物(即昼夜蒸腾作用)不同的影响。