Tian Jiang, Ge Fei, Zhang Dayi, Deng Songqiang, Liu Xingwang
Department of Chemical Engineering, Xiangtan University, Xiangtan 411105, China.
Department of Environmental Science and Engineering, College of Environment and Resources, Xiangtan University, Xiangtan 411105, China.
Biology (Basel). 2021 Feb 17;10(2):158. doi: 10.3390/biology10020158.
Phosphorus (P) is a vital element in biological molecules, and one of the main limiting elements for biomass production as plant-available P represents only a small fraction of total soil P. Increasing global food demand and modern agricultural consumption of P fertilizers could lead to excessive inputs of inorganic P in intensively managed croplands, consequently rising P losses and ongoing eutrophication of surface waters. Despite phosphate solubilizing microorganisms (PSMs) are widely accepted as eco-friendly P fertilizers for increasing agricultural productivity, a comprehensive and deeper understanding of the role of PSMs in P geochemical processes for managing P deficiency has received inadequate attention. In this review, we summarize the basic P forms and their geochemical and biological cycles in soil systems, how PSMs mediate soil P biogeochemical cycles, and the metabolic and enzymatic mechanisms behind these processes. We also highlight the important roles of PSMs in the biogeochemical P cycle and provide perspectives on several environmental issues to prioritize in future PSM applications.
磷(P)是生物分子中的一种重要元素,也是生物量生产的主要限制元素之一,因为植物可利用的磷仅占土壤总磷的一小部分。全球粮食需求的增加以及现代农业对磷肥的消耗,可能导致集约化管理农田中无机磷的过量投入,从而增加磷的流失,并导致地表水持续富营养化。尽管解磷微生物(PSMs)作为提高农业生产力的生态友好型磷肥已被广泛接受,但对于解磷微生物在管理磷缺乏的磷地球化学过程中的作用,仍缺乏全面而深入的理解。在这篇综述中,我们总结了土壤系统中磷的基本形态及其地球化学和生物循环,解磷微生物如何介导土壤磷的生物地球化学循环,以及这些过程背后的代谢和酶促机制。我们还强调了解磷微生物在生物地球化学磷循环中的重要作用,并就未来解磷微生物应用中需要优先考虑的几个环境问题提供了观点。