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Role of soil microorganisms in improving P nutrition of plants

机译:土壤微生物在改善植物磷素营养中的作用

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摘要

Phosphorus (P) is one of the major plant growth-limiting nutrients although it is abundant in soils in both inorganic and organic forms. Phosphate solubilizing micro-organisms (PSMs) are ubiquitous in soils and could play an important role in supplying P to plants in a more environmentally friendly and sustainable manner. Although solubilization of P compounds by microbes is very common under laboratory conditions, results in the field have been highly variable. This variability has hampered the large-scale use of PSMs in agriculture. Many reasons have been suggested for this variability, but none of them have been extensively investigated. In spite of the importance of PSMs in agriculture, the detailed biochemical and molecular mechanisms of P solubilization are not known. Recent work in our laboratory has shown that the conditions employed to isolate PSMs do not reflect soil conditions and that PSMs capable of effectively releasing P from soil are not so highly abundant as was suggested in earlier studies. These studies have also indicated that the mineral phosphate solubilizing (mps) ability of microbes could be linked to specific genes, and that these genes are present even in non P solubilizing bacteria. Understanding the genetic basis of P solubilization could help in transforming more rhizosphere-competent bacteria into PSMs. Further research should also focus on the microbial solubilization of iron (Fe) and aluminum (Al) phosphates, as well as mobilization of the organic phosphate reserves present in the soils.
机译:磷(P)是限制植物生长的主要养分之一,尽管它以无机和有机形式大量存在于土壤中。磷酸盐增溶微生物(PSM)在土壤中无处不在,并且在以更环保和可持续的方式向植物供应磷方面可能发挥重要作用。尽管在实验室条件下微生物对P化合物的溶解非常普遍,但该领域的结果却变化很大。这种可变性阻碍了PSM在农业中的大规模使用。对于这种可变性,已经提出了许多原因,但是没有一个被广泛研究。尽管PSM在农业中很重要,但尚不了解P增溶的详细生化和分子机理。我们实验室的最新工作表明,用于分离PSM的条件不能反映土壤条件,并且能够有效地从土壤中释放P的PSM并不像以前的研究那样高度丰富。这些研究还表明,微生物对矿物磷酸盐的增溶(mps)能力可能与特定基因有关,并且这些基因甚至存在于非P增溶细菌中。了解P溶解的遗传基础可以帮助将更多具有根际适应能力的细菌转化为PSM。进一步的研究还应集中于微生物溶解铁(Fe)和铝(Al)磷酸盐,以及动员土壤中存在的有机磷酸盐储备。

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