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Root and Rhizosphere Bacterial Phosphatase Activity Varies with Tree Species and Soil Phosphorus Availability in Puerto Rico Tropical Forest

机译:波多黎各热带森林的根和根际细菌磷酸酶活性随树种和土壤磷有效性而变化

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Tropical forests generally occur on highly weathered soils that, in combination with the immobility of phosphorus (P), often result in soils lacking orthophosphate, the form of P most easily metabolized by plants and microbes. In these soils, mineralization of organic P can be the major source for orthophosphate. Both plants and microbes encode for phosphatases capable of mineralizing a range of organic P compounds. However, the activity of these enzymes depends on several edaphic factors including P availability, tree species, and microbial communities. Thus, phosphatase activity in both roots and the root microbial community constitute an important role in P mineralization and P nutrient dynamics that are not well studied in tropical forests. To relate phosphatase activity of roots and bacteria in tropical forests, we measured phosphatase activity in roots and bacterial isolates as well as bacterial community composition from the rhizosphere. Three forests in the Luquillo Mountains of Puerto Rico were selected to represent a range of soil P availability as measured using the resin P method. Within each site, a minimum of three tree species were chosen to sample. Root and bacterial phosphatase activity were both measured using a colorimetric assay with para-nitrophenyl phosphate as a substrate for the phosphomonoesterase enzyme. Both root and bacterial phosphatase were chiefly influenced by tree species. Though tree species was the only significant factor in root phosphatase activity, there was a negative trend between soil P availability and phosphatase activity in linear regressions of average root phosphatase and resin P. Permutational multivariate analysis of variance of bacterial community composition based on 16S amplicon sequencing indicated that bacterial composition was strongly controlled by soil P availability ( p -value < 0.05). These results indicate that although root and bacterial phosphatase activity were influenced by tree species; bacterial community composition was chiefly influenced by P availability. Although the sample size is limited given the tremendous diversity of tropical forests, our study indicates the importance of roots and bacterial function to understanding phosphatase activity. Future work will broaden the diversity of tree species and microbial members sampled to provide insight into P mineralization and model representation of tropical forests.
机译:热带森林通常发生在高风化的土壤上,再加上磷(P)的固定化,通常会导致土壤缺乏正磷酸盐,正磷酸盐最容易被植物和微生物代谢。在这些土壤中,有机磷的矿化可能是正磷酸盐的主要来源。植物和微生物均编码能够使一系列有机P化合物矿化的磷酸酶。但是,这些酶的活性取决于几种营养因素,包括磷的利用率,树木种类和微生物群落。因此,在热带森林中尚未充分研究的根和根微生物群落中的磷酸酶活性在磷矿化和磷养分动态中起着重要作用。为了关联热带森林中的根和细菌的磷酸酶活性,我们测量了根和细菌分离物中的磷酸酶活性以及根际中的细菌群落组成。选择了波多黎各卢奎洛山脉的三片森林来代表使用树脂P方法测得的土壤P的有效利用范围。在每个地点内,至少要选择三种树种进行采样。根和细菌磷酸酶活性均使用比色测定法以对硝基苯基磷酸酯为磷酸单酯酶的底物进行测定。根和细菌的磷酸酶都主要受树种的影响。虽然树种是影响根磷酸酶活性的唯一重要因素,但在平均根磷酸酶和树脂P的线性回归中,土壤磷的利用率与磷酸酶活性之间呈负趋势。基于16S扩增子序列的细菌群落组成变异的排列多变量分析指出细菌组成受到土壤磷有效性的强烈控制(p值<0.05)。这些结果表明,尽管根和细菌的磷酸酶活性受树种的影响;细菌群落组成主要受磷有效性的影响。尽管鉴于热带森林的巨大多样性,样本数量有限,但我们的研究表明了根源和细菌功能对于理解磷酸酶活性的重要性。未来的工作将扩大树木物种和采样的微生物成员的多样性,以提供对磷矿化和热带森林模型表示的见解。

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