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Prolonged experimental drought reduces plant hydraulic conductance and transpiration and increases mortality in a piñon–juniper woodland

机译:长时间的实验干旱会降低松树-松树林的植物水力传导和蒸腾作用,并增加死亡率。

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AbstractPlant hydraulic conductance (ks) is a critical control on whole-plant water use and carbon uptake and, during drought, influences whether plants survive or die. To assess long-term physiological and hydraulic responses of mature trees to water availability, we manipulated ecosystem-scale water availability from 2007 to 2013 in a piñon pine (Pinus edulis) and juniper (Juniperus monosperma) woodland. We examined the relationship between ks and subsequent mortality using more than 5 years of physiological observations, and the subsequent impact of reduced hydraulic function and mortality on total woody canopy transpiration (EC) and conductance (GC). For both species, we observed significant reductions in plant transpiration (E) and ks under experimentally imposed drought. Conversely, supplemental water additions increased E and ks in both species. Interestingly, both species exhibited similar declines in ks under the imposed drought conditions, despite their differing stomatal responses and mortality patterns during drought. Reduced whole-plant ks also reduced carbon assimilation in both species, as leaf-level stomatal conductance (gs) and net photosynthesis (An) declined strongly with decreasing ks. Finally, we observed that chronically low whole-plant ks was associated with greater canopy dieback and mortality for both piñon and juniper and that subsequent reductions in woody canopy biomass due to mortality had a significant impact on both daily and annual canopy EC and GC. Our data indicate that significant reductions in ks precede drought-related tree mortality events in this system, and the consequence is a significant reduction in canopy gas exchange and carbon fixation. Our results suggest that reductions in productivity and woody plant cover in piñon–juniper woodlands can be expected due to reduced plant hydraulic conductance and increased mortality of both piñon pine and juniper under anticipated future conditions of more frequent and persistent regional drought in the southwestern United States.
机译:摘要植物水力传导率(k s )是控制整个植物水分利用和碳吸收的关键控制,在干旱期间会影响植物存活或死亡。为了评估成熟树木对水供应的长期生理和水力响应,我们在2007年至2013年间对松树松(Pinus edulis)和杜松(Juniperus monosperma)林地进行了生态系统规模的水利用。我们使用超过5年的生理观察研究了k s 与后续死亡率之间的关系,以及水力功能和死亡率降低对木质冠层蒸腾总量(E C )和电导(G C )。对于这两种物种,我们都观察到在干旱条件下植物的蒸腾作用(E)和k s 明显减少。相反,补充水增加了两个物种的E和k s 。有趣的是,尽管在干旱条件下它们的气孔反应和死亡率模式不同,但两种物种在强加的干旱条件下均表现出相似的k s 下降。减少的全株k s 还减少了两个物种的碳同化,如叶片水平气孔导度(g s )和净光合作用(A n )随着k s 的减少而强烈下降。最后,我们观察到,长期低全株k s 与松树和杜松的较高冠层枯萎率和死亡率相关,并且由于死亡率造成的木质冠层生物量随后减少对每日两者都有显着影响和年度冠层E C 和G C 。我们的数据表明,在该系统中,k s 的显着降低先于干旱相关的树木死亡事件,其结果是冠层气体交换和固碳的显着降低。我们的结果表明,在美国西南部地区更频繁和持续的干旱地区,预计未来条件下,由于松木和杜松的水力传导率降低,并且松木和杜松的死亡率增加,因此可以预期松木-杜松林地生产力和木本植物覆盖率下降。 。

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