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矿质元素的生物地球化学循环直接影响生态系统的生产力和稳定性。磷(P)作为碳、氮之外陆地生态系统最关键的营养元素,在植物体内的分配和代谢决定了植物的生长过程及生产力水平[1]。低磷环境在生态系统内普遍存在,土壤总磷库80%以上的磷不可移动[2],植物难以吸收利用。同时,土壤有效磷(Pi)易被铝离子、铁离子、钙离子吸附固定,与氢氧化合物构成螯合物[3−5],因此有效磷浓度随土壤发育而下降,导致世界范围内有效磷浓度低于10 µmol·L−1的土壤广泛存在[6]。
为满足农林业生产需求,集约施用磷肥成为生产经营的主要措施。然而,一般磷肥当季利用率仅为10%~25%,75%~90%的磷被转化固定成植物难以吸收的形态[7],导致磷肥利用率低下。同时,随着经济增长和人口剧增,过度开采和不合理的磷肥经营管理造成磷矿资源储备耗竭、水体磷素增加,对生态环境造成严重威胁[8−10]。近年来,关于土壤磷素循环研究的不断深入,揭示了植物进化形成的一系列复杂适应性策略[11−12],并发现土壤功能微生物对土壤磷库活化和植物营养健康有重要影响[13−14]。丛枝菌根真菌(arbuscular mycorrhizal fungi,AMF)和溶磷细菌(phosphate-solubilizing bacteria,PSB)在自然界土壤中普遍存在。研究发现,丛枝菌根真菌和溶磷细菌可以溶解难溶性无机磷、矿化有机磷,两者直接参与土壤磷素活化与植物磷素获取过程,与土壤、植物之间联系密切[15−16],在维持土壤磷养分有效性和生态系统功能中发挥重要作用[16−18]。鉴于此,为开发可持续土壤磷素高效利用途径,围绕植物-丛枝菌根真菌-溶磷细菌共生关系,详述了丛枝菌根真菌与溶磷细菌在植物磷养分吸收中的作用,强调了植物-丛枝菌根真菌-溶磷细菌互作增效对土壤磷素调动的途径和机制。
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