Manzoor Aamir, Dippold Michaela A, Loeppmann Sebastian, Blagodatskaya Evgenia
Biogeochemistry of Agroecosystems, University of Goettingen, Goettingen, Germany.
Geo-Biosphere Interactions, Department of Geosciences, University of Tuebingen, Tuebingen, Germany.
Front Plant Sci. 2022 Jul 19;13:935829. doi: 10.3389/fpls.2022.935829. eCollection 2022.
The activity of extracellular phosphatases is a dynamic process controlled by both plant roots and microorganisms, which is responsible for the mineralization of soil phosphorus (P). Plants regulate the availability of soil P through the release of root mucilage and the exudation of low-molecular weight organic acids (LMWOAs). Mucilage increases soil hydraulic conductivity as well as pore connectivity, both of which are associated with increased phosphatase activity. The LMWOAs, in turn, stimulate the mineralization of soil P through their synergistic effects of acidification, chelation, and exchange reactions. This article reviews the catalytic properties of extracellular phosphatases and their interactions with the rhizosphere interfaces. We observed a biphasic effect of root metabolic products on extracellular phosphatases, which notably altered their catalytic mechanism. In accordance with the proposed conceptual framework, soil P is acquired by both plants and microorganisms in a coupled manner that is characterized by the exudation of their metabolic products. Due to inactive or reduced root exudation, plants recycle P through adsorption on the soil matrix, thereby reducing the rhizosphere phosphatase activity. The two-phase conceptual framework might assist in understanding P-acquisition (substrate turnover) and P-restoration (phosphatase adsorption by soil) in various terrestrial ecosystems.
细胞外磷酸酶的活性是一个由植物根系和微生物共同控制的动态过程,它负责土壤磷(P)的矿化。植物通过释放根黏液和分泌低分子量有机酸(LMWOAs)来调节土壤磷的有效性。黏液增加了土壤的水力传导率以及孔隙连通性,这两者都与磷酸酶活性的增加有关。反过来,低分子量有机酸通过其酸化、螯合和交换反应的协同作用刺激土壤磷的矿化。本文综述了细胞外磷酸酶催化特性及其与根际界面的相互作用。我们观察到根系代谢产物对细胞外磷酸酶有双相效应,这显著改变了它们的催化机制。根据提出的概念框架,植物和微生物以一种以其代谢产物分泌为特征的耦合方式获取土壤磷。由于根系分泌物不活跃或减少,植物通过吸附在土壤基质上来循环利用磷,从而降低根际磷酸酶活性。这个两阶段概念框架可能有助于理解各种陆地生态系统中的磷获取(底物周转)和磷恢复(土壤对磷酸酶的吸附)。