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首页> 外文期刊>Ecology and Evolution >Plant‐soil feedbacks from 30‐year family‐specific soil cultures: phylogeny, soil chemistry and plant life stage
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Plant‐soil feedbacks from 30‐year family‐specific soil cultures: phylogeny, soil chemistry and plant life stage

机译:30年家庭特定土壤文化对植物土壤的反馈:系统发育,土壤化学和植物生命阶段

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AbstractIntraspecific negative feedback effects, where performance is reduced on soils conditioned by conspecifics, are widely documented in plant communities. However, interspecific feedbacks are less well studied, and their direction, strength, causes, and consequences are poorly understood. If more closely related species share pathogens, or have similar soil resource requirements, plants may perform better on soils conditioned by more distant phylogenetic relatives. There have been few empirical tests of this prediction across plant life stages, and none of which attempt to account for soil chemistry. Here, we test the utility of phylogeny for predicting soil feedback effects on plant survival and performance (germination, seedling survival, growth rate, biomass). We implement a full factorial experiment growing species representing five families on five plant family-specific soil sources. Our experiments exploit soils that have been cultured for over 30 years in plant family-specific beds at Oxford University Botanic Gardens. Plant responses to soil source were idiosyncratic, and species did not perform better on soils cultured by phylogenetically more distant relatives. The magnitude and sign of feedback effects could, however, be explained by differences in the chemical properties of “home” and “away” soils. Furthermore, the direction of soil chemistry-related plant-soil feedbacks was dependent on plant life stage, with the effects of soil chemistry on germination success and accumulation of biomass inversely related. Our results (1) suggest that the phylogenetic distance between plant families cannot predict plant–soil feedbacks across multiple life stages, and (2) highlight the need to consider changes in soil chemistry as an important driver of population responses. The contrasting responses at plant life stages suggest that studies focusing on brief phases in plant demography (e.g., germination success) may not give a full picture of plant–soil feedback effects.
机译:摘要种内负反馈效应在植物群落中被广泛记录,在种内负反馈效应下,因种而异。但是,种间反馈的研究较少,并且对它们的方向,强度,原因和后果了解甚少。如果更密切相关的物种共有病原体,或具有相似的土壤资源需求,则植物可能在距离较近的系统发生亲戚条件下的土壤上表现更好。几乎没有关于植物整个生命阶段的这一预测的实证检验,也没有一个尝试说明土壤化学性质。在这里,我们测试系统发育的效用,以预测土壤反馈对植物存活和表现(发芽,幼苗存活,生长速率,生物量)的影响。我们实施了一个完整的阶乘实验,在五个特定于植物科的土壤源上代表五个科的生长物种。我们的实验利用在牛津大学植物园的植物家族专用床中培养了30多年的土壤。植物对土壤来源的反应是特异的,在系统发育较远的近缘种培养的土壤上,物种的表现也不佳。但是,可以通过“家”和“外”土壤的化学性质差异来解释反馈效应的大小和迹象。此外,土壤化学相关的植物-土壤反馈的方向取决于植物的生命阶段,而土壤化学对发芽成功和生物量积累的影响则成反比。我们的结果(1)表明植物科之间的系统发育距离无法预测多个生命阶段的植物-土壤反馈,并且(2)强调需要将土壤化学变化视为种群响应的重要驱动因素。在植物生命阶段不同的响应表明,研究集中在植物人口统计学的短暂阶段(例如,发芽成功)可能无法全面反映植物-土壤反馈效应。

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