Higgins John A, Ramos Danielle Santiago, Gili Stefania, Spetea Cornelia, Kanoski Scott, Ha Darren, McDonough Alicia A, Youn Jang H
Department of Geosciences, Princeton University, Princeton, NJ, United States.
Department of Marine and Coastal Science, Rutgers University, New Brunswick, NJ, United States.
Front Physiol. 2022 Oct 26;13:1016242. doi: 10.3389/fphys.2022.1016242. eCollection 2022.
As the most abundant cation in archaeal, bacterial, and eukaryotic cells, potassium (K) is an essential element for life. While much is known about the machinery of transcellular and paracellular K transport-channels, pumps, co-transporters, and tight-junction proteins-many quantitative aspects of K homeostasis in biological systems remain poorly constrained. Here we present measurements of the stable isotope ratios of potassium (K/K) in three biological systems (algae, fish, and mammals). When considered in the context of our current understanding of plausible mechanisms of K isotope fractionation and K transport in these biological systems, our results provide evidence that the fractionation of K isotopes depends on transport pathway and transmembrane transport machinery. Specifically, we find that passive transport of K down its electrochemical potential through channels and pores in tight-junctions at favors K, a result which we attribute to a kinetic isotope effect associated with dehydration and/or size selectivity at the channel/pore entrance. In contrast, we find that transport of K against its electrochemical gradient pumps and co-transporters is associated with less/no isotopic fractionation, a result that we attribute to small equilibrium isotope effects that are expressed in pumps/co-transporters due to their slower turnover rate and the relatively long residence time of K in the ion pocket. These results indicate that stable K isotopes may be able to provide quantitative constraints on transporter-specific K fluxes (e.g., the fraction of K efflux from a tissue by channels vs. co-transporters) and how these fluxes change in different physiological states. In addition, precise determination of K isotope effects associated with K transport channels, pumps, and co-transporters may provide unique constraints on the mechanisms of K transport that could be tested with steered molecular dynamic simulations.
作为古菌、细菌和真核细胞中含量最丰富的阳离子,钾(K)是生命的必需元素。虽然人们对跨细胞和细胞旁钾转运机制——通道、泵、协同转运蛋白和紧密连接蛋白——了解很多,但生物系统中钾稳态的许多定量方面仍知之甚少。在此,我们展示了在三个生物系统(藻类、鱼类和哺乳动物)中钾(K/K)稳定同位素比率的测量结果。结合我们目前对这些生物系统中钾同位素分馏和钾转运可能机制的理解来看,我们的结果表明钾同位素的分馏取决于转运途径和跨膜转运机制。具体而言,我们发现钾通过紧密连接中的通道和孔隙沿其电化学势被动转运有利于K,我们将此结果归因于与通道/孔隙入口处脱水和/或尺寸选择性相关的动力学同位素效应。相比之下,我们发现钾逆其电化学梯度通过泵和协同转运蛋白转运与较少/无同位素分馏相关,我们将此结果归因于由于泵/协同转运蛋白周转速率较慢以及钾在离子口袋中的停留时间相对较长而在其中表现出的小平衡同位素效应。这些结果表明,稳定的钾同位素或许能够对转运蛋白特异性的钾通量(例如,通过通道与协同转运蛋白从组织中流出的钾的比例)以及这些通量在不同生理状态下如何变化提供定量限制。此外,精确测定与钾转运通道、泵和协同转运蛋白相关的钾同位素效应,可能为钾转运机制提供独特的限制条件,这些条件可用引导分子动力学模拟进行测试。