Division of Cardiology, Department of Medicine, Department of Biomedical Engineering, Johns Hopkins University, Baltimore, MD 21205, USA.
J Gen Physiol. 2012 Jun;139(6):465-78. doi: 10.1085/jgp.201210784.
Mitochondrial Ca(2+) uptake is thought to provide an important signal to increase energy production to meet demand but, in excess, can also trigger cell death. The mechanisms defining the relationship between total Ca(2+) uptake, changes in mitochondrial matrix free Ca(2+), and the activation of the mitochondrial permeability transition pore (PTP) are not well understood. We quantitatively measure changes in Ca(2+) and Ca(2+) during Ca(2+) uptake in isolated cardiac mitochondria and identify two components of Ca(2+) influx. Ca(2+) recordings revealed that the first, MCU(mode1), required at least 1 µM Ru360 to be completely inhibited, and responded to small Ca(2+) additions in the range of 0.1 to 2 µM with rapid and large changes in Ca(2+). The second component, MCU(mode2), was blocked by 100 nM Ru360 and was responsible for the bulk of total Ca(2+) uptake for large Ca(2+) additions in the range of 2 to 10 µM; however, it had little effect on steady-state Ca(2+). MCU(mode1) mediates changes in Ca(2+) of 10s of μM, even in the presence of 100 nM Ru360, indicating that there is a finite degree of Ca(2+) buffering in the matrix associated with this pathway. In contrast, the much higher Ca(2+) loads evoked by MCU(mode2) activate a secondary dynamic Ca(2+) buffering system consistent with calcium-phosphate complex formation. Increasing P(i) potentiated Ca(2+) increases via MCU(mode1) but suppressed Ca(2+) changes via MCU(mode2). The results suggest that the role of MCU(mode1) might be to modulate oxidative phosphorylation in response to intracellular Ca(2+) signaling, whereas MCU(mode2) and the dynamic high-capacity Ca(2+) buffering system constitute a Ca(2+) sink function. Interestingly, the trigger for PTP activation is unlikely to be Ca(2+) itself but rather a downstream byproduct of total mitochondrial Ca(2+) loading.
线粒体 Ca(2+)摄取被认为提供了一个重要的信号,以增加能量产生来满足需求,但过量也会引发细胞死亡。定义总 Ca(2+)摄取、线粒体基质游离 Ca(2+)变化和线粒体通透性转换孔 (PTP) 激活之间关系的机制尚不清楚。我们定量测量了分离的心肌线粒体中 Ca(2+)摄取过程中 Ca(2+) 和 Ca(2+) 的变化,并确定了 Ca(2+)内流的两个组成部分。Ca(2+)记录显示,第一个组成部分 MCU(模式 1)至少需要 1 µM Ru360 才能完全被抑制,并对 0.1 至 2 µM 范围内的小 Ca(2+)添加做出快速且大幅度的 Ca(2+)变化。第二个组成部分 MCU(模式 2)被 100 nM Ru360 阻断,负责 2 至 10 µM 范围内大 Ca(2+)添加的大部分总 Ca(2+)摄取;然而,它对稳态 Ca(2+)几乎没有影响。即使存在 100 nM Ru360,MCU(模式 1)也介导 10s 数量级的 Ca(2+)变化,表明与该途径相关的基质中存在有限程度的 Ca(2+)缓冲。相比之下,MCU(模式 2)引起的 Ca(2+)负荷要高得多,激活了与钙-磷复合物形成一致的二次动态 Ca(2+)缓冲系统。增加 P(i)增强了 MCU(模式 1)引起的 Ca(2+)增加,但抑制了 MCU(模式 2)引起的 Ca(2+)变化。结果表明,MCU(模式 1)的作用可能是响应细胞内 Ca(2+)信号来调节氧化磷酸化,而 MCU(模式 2)和动态大容量 Ca(2+)缓冲系统构成了 Ca(2+)吸收功能。有趣的是,PTP 激活的触发因素不太可能是 Ca(2+)本身,而是总线粒体 Ca(2+)负载的下游副产物。