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Relationship between soil nutrient availability and plant species richness in a tropical semi-arid environment.

机译:在热带半干旱环境中土壤养分利用率与植物物种丰富度之间的关系。

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Question: What is the relationship between soil fertility and plant species richness in the 'fertile islands' occurring beneath two species of legume (Cercidium praecox and Prosopis laevigata)? Location: Tehuacan-Cuicatlan region, central Mexico. Methods: Plant richness was measured in three micro-environments (below canopies of C. praecox, below canopies of P. laevigata and in areas without canopies). The concentration of soil nutrients (C, N and P), C and N in the microbiota, and processes of ecosystem functioning (net C mineralization rate and N mineralization) were measured. The relationship between soil variables and plant richness were assessed with ANCOVAs. Results: Soil nutrients and species richness increases markedly under fertility islands. There were higher concentrations of C and N in the soil, faster rates of C mineralization, and higher species richness under P. laevigata canopies. The relationship between soil fertility and species richness was always positive except for total N, ammonium and net C mineralization rate under C. praecox, and for available P under P. laevigata. Conclusions: The sign of the relationship between soil fertility and species richness varies according to the nutrient and the micro-environment. Positive relationships could result from between species complementarity and facilitation. Negative relationships could be explained by a specific limitation threshold for some soil resources (P and N for plants and C for the soil microbiota) which eliminate the possibilities of between species complementarity and facilitation above that threshold. As in all observational studies, these relationships should be considered only correlational..
机译:问题:在两个豆科植物(Cercidium praecox和Prosopis laevigata)下面的“肥沃的岛屿”中,土壤肥力和植物物种丰富度之间有什么关系?地点:墨西哥中部的特瓦坎-屈卡特兰地区。方法:在三个微环境(C. praecox冠层以下,P。laevigata冠层以下和无冠层区域)中测量植物的丰富度。测量了土壤养分(C,N和P),微生物区系中的C和N的浓度以及生态系统功能的过程(净C矿化率和N矿化)。土壤变量与植物丰富度之间的关系用ANCOVA进行了评估。结果:在肥育岛下,土壤养分和物种丰富度显着增加。在P. laevigata冠层下,土壤中的C和N浓度较高,C矿化速率较高,物种丰富度较高。土壤肥力与物种丰富度之间的关系一直是正的,除了总氮,总铵和净碳矿化率(在雷竹下)和可利用磷(在P. laevigata下)之外。结论:土壤肥力与物种丰富度之间关系的迹象因养分和微环境而异。物种互补和促进之间可能产生积极关系。负关系可以通过某些土壤资源(植物的P和N以及土壤微生物群的C)的特定限制阈值来解释,该阈值消除了物种补充和促进之间在该阈值之上的可能性。与所有观察性研究一样,这些关系应仅视为相关关系。

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