Institute of Agricultural Sciences in the Tropics (Hans-Ruthenberg-Institute), University of Hohenheim, Stuttgart, Germany.
Department of Tropical Forages Program, The Alliance of Bioversity International and the International Center for Tropical Agriculture (CIAT), Cali, Colombia.
Physiol Plant. 2021 May;172(1):116-123. doi: 10.1111/ppl.13300. Epub 2021 Jan 15.
Biological nitrification inhibition (BNI) of Brachiaria humidicola has been attributed to nitrification-inhibiting fusicoccanes, most prominently 3-epi-brachialactone. However, its release mechanism from B. humidicola roots remains elusive. Two hydroponic experiments were performed to investigate the role of rhizosphere pH and nutritional N form in regulating 3-epi-brachialactone release by B. humidicola and verify the underlying release pathway. Low rhizosphere pH and NH nutrition promoted 3-epi-brachialactone exudation. However, the substitution of NH by K revealed that the NH effect was not founded in a direct physiological response to the N form but was related to the cation-anion balance during nutrient uptake. Release of 3-epi-brachialactone correlated with the transmembrane proton gradient ΔpH and NH uptake (R = 0.92 for high ~6.8 and R = 0.84 for low ~4.2 trap solution pH). This corroborated the release of 3-epi-brachialactone through secondary transport, with the proton motive force (ΔP) defining transport rates across the plasma membrane. It was concluded that 3-epi-brachialactone release cannot be conceptualized as a regulated response to soil pH or NH availability, but merely as the result of associated changes in ΔP.
生物硝化抑制(BNI)已归因于湿润臂形草中的硝化抑制 Fusicoccan ,最突出的是 3-epi-brachialactone。然而,其从湿润臂形草根释放的机制仍然难以捉摸。进行了两项水培实验,以研究根际 pH 值和营养 N 形式在调节湿润臂形草中 3-epi-brachialactone 释放中的作用,并验证潜在的释放途径。低根际 pH 值和 NH 营养促进了 3-epi-brachialactone 的分泌。然而,用 K 取代 NH 表明,NH 的影响不是基于对 N 形式的直接生理反应,而是与养分吸收过程中的阴阳离子平衡有关。3-epi-brachialactone 的释放与跨膜质子梯度 ΔpH 和 NH 吸收相关(高 ~6.8 的 R = 0.92,低 ~4.2 的 R = 0.84)。这证实了 3-epi-brachialactone 通过次级转运释放,质子动势(ΔP)定义了跨质膜的转运速率。结论是,3-epi-brachialactone 的释放不能被概念化为对土壤 pH 或 NH 可用性的调节反应,而仅仅是由于 ΔP 的相关变化的结果。