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青霉中存在两个不同的细胞内无机硫酸盐池的证据。

Evidence for two distinct intracellular pools of inorganic sulfate in Penicillium notatum.

作者信息

Hunter D R, Segel I H

出版信息

J Bacteriol. 1985 Jun;162(3):881-7. doi: 10.1128/jb.162.3.881-887.1985.

Abstract

A strain of Penicillium notatum unable to metabolize inorganic sulfate can accumulate sulfate internally to an apparent equilibrium concentration 10(5) greater than that remaining in the medium. The apparent Keq is near constant at all initial external sulfate concentrations below that which would eventually exceed the internal capacity of the cells. Under equilibrium conditions of zero net flux, external 35SO42- exchanges with internal, unlabeled SO42- at a rate consistent with the kinetic constants with the sulfate transport system. Efflux experiments demonstrated that sulfate occupies two distinct intracellular pools. Pool 1 is characterized by the rapid release of 35SO42- when the suspension of preloaded cells is adjusted to 10 mM azide at pH 8.4 (t 1/2, 0.38 min). 35SO42- in pool 1 also rapidly exchanges with unlabeled medium sulfate. Pool 2 is characterized by the slow release of 35SO42- induced by azide at pH 8.4 or unlabeled sulfate (t 1/2, 32 to 49 min). Early in the 35SO42- accumulation process, up to 78% of the total transported substrate is found in pool 1. At equilibrium, pool 1 accounts for only about 2% of the total accumulated 35SO42-. The kinetics of 35SO42- accumulation is consistent with the following sequential process: medium----pool 1----pool 2. Monensin (33 microns) accelerates the transfer of 35SO42- from pool 1 to pool 2. Valinomycin (0.2 microM) and tetraphenylboron- (1 mM) retard the transfer of 35SO42- from pool 1 to pool 2. At the concentrations used, neither of the ionophores nor tetraphenylboron- affect total 35SO42- uptake. Pool 2 may reside in a vacuole or other intracellular organelle. A model for the transfer of sulfate from pool 1 to pool 2 is presented.

摘要

一种无法代谢无机硫酸盐的青霉菌株能够在其内部积累硫酸盐,使其表观平衡浓度比培养基中剩余的浓度高10^5倍。在所有初始外部硫酸盐浓度低于最终会超过细胞内部容量的浓度时,表观平衡常数(Keq)几乎保持恒定。在净通量为零的平衡条件下,外部的35SO42-与内部未标记的SO42-以与硫酸盐转运系统动力学常数一致的速率进行交换。流出实验表明,硫酸盐占据两个不同的细胞内池。池1的特征是,当预加载细胞的悬浮液在pH 8.4下调整到10 mM叠氮化物时,35SO42-会快速释放(半衰期为0.38分钟)。池1中的35SO42-也会与未标记的培养基硫酸盐快速交换。池2的特征是,在pH 8.4下由叠氮化物或未标记的硫酸盐诱导的35SO42-缓慢释放(半衰期为32至49分钟)。在35SO42-积累过程的早期,高达78%的总转运底物存在于池1中。在平衡时,池1仅占总积累的35SO42-的约2%。35SO42-积累的动力学与以下顺序过程一致:培养基→池1→池2。莫能菌素(33微摩尔)加速35SO42-从池1向池2的转移。缬氨霉素(0.2微摩尔)和四苯硼酸盐(1毫摩尔)延缓35SO42-从池1向池2的转移。在所使用的浓度下,离子载体和四苯硼酸盐均不影响35SO42-的总摄取量。池2可能存在于液泡或其他细胞内细胞器中。本文提出了一个硫酸盐从池1向池2转移的模型。

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