Hirano Yu, Kitayama Kanehiro, Imai Nobuo
Department of Forest Science Tokyo University of Agriculture Setagaya Japan.
Graduate School of Agriculture Kyoto University Kyoto Japan.
Ecol Evol. 2022 Mar 7;12(3):e8669. doi: 10.1002/ece3.8669. eCollection 2022 Feb.
Soil organic phosphorus (P) compounds can be the main P source for plants in P-limited tropical rainforests. Phosphorus occurs in diverse chemical forms, including monoester P, diester P, and phytate, which require enzymatic hydrolysis by phosphatase into inorganic P before assimilation by plants. The interactions between plant interspecific differences in organic P acquisition strategies via phosphatase activities with root morphological traits would lead to P resource partitioning, but they have not been rigorously evaluated. We measured the activities of three classes of phosphatases (phosphomonoesterase, PME; phosphodiesterase, PDE; and phytase, PhT), specific root length (SRL), root diameter, and root tissue density in mature tree species with different mycorrhizal associations (ectomycorrhizal [ECM] or arbuscular mycorrhizal [AM]) and different successional status (climax or pioneer species) in Sabah, Malaysia. We studied nitrogen (N)- and P-fertilized plots to evaluate the acquisition strategies for organic P under P-limited conditions 7 years after fertilization was initiated. P fertilization reduced the PME activity in all studied species and reduced PhT and PDE activities more in climax species than in the two pioneer species, irrespective of the mycorrhizal type. PDE activity increased in some climax species after N fertilization, suggesting that these species allocate excess N to the synthesis of PDE. Moreover, PME and PhT activities, but not PDE activity, correlated positively with SRL. We suggest that climax species tend to be more strongly dependent on recalcitrant organic P (i.e., phytate and/or diester P) than pioneer species, regardless of the mycorrhizal type. We also suggest that trees in which root PME or PhT activity is enhanced can increase their SRL to acquire P efficiently. Resource partitioning of soil organic P would occur among species through differences in their phosphatase activities, which plays potentially ecologically important role in reducing the competition among coexisting tree species in lowland tropical rainforests.
在磷受限的热带雨林中,土壤有机磷化合物可能是植物的主要磷源。磷以多种化学形式存在,包括单酯磷、二酯磷和植酸盐,植物在吸收之前需要磷酸酶将其酶解为无机磷。植物通过磷酸酶活性获取有机磷的种间差异与根系形态特征之间的相互作用会导致磷资源的分配,但尚未得到严格评估。我们测量了马来西亚沙巴州具有不同菌根关联(外生菌根[ECM]或丛枝菌根[AM])和不同演替状态(顶极或先锋物种)的成熟树种中三类磷酸酶(磷酸单酯酶,PME;磷酸二酯酶,PDE;和植酸酶,PhT)的活性、比根长(SRL)、根直径和根组织密度。我们研究了氮(N)和磷施肥地块,以评估施肥开始7年后在磷受限条件下有机磷的获取策略。无论菌根类型如何,施磷降低了所有研究物种的PME活性,并且顶极物种中PhT和PDE活性的降低幅度比两个先锋物种更大。施氮后,一些顶极物种的PDE活性增加,表明这些物种将过量的氮分配到PDE的合成中。此外,PME和PhT活性与SRL呈正相关,但PDE活性与SRL无相关性。我们认为,无论菌根类型如何,顶极物种往往比先锋物种更强烈地依赖难降解有机磷(即植酸盐和/或二酯磷)。我们还认为,根系PME或PhT活性增强的树木可以增加其SRL以有效获取磷。土壤有机磷的资源分配将通过物种间磷酸酶活性的差异而发生,这在减少低地热带雨林中共存树种之间的竞争方面可能发挥潜在的重要生态作用。