Abstract

Cytotoxicity associated with pathophysiological Ca(2+) overload (e.g. in stroke) appears mediated by an event termed the mitochondrial permeability transition (mPT). We built and solved a kinetic model of the mPT in populations of isolated rat liver mitochondria that quantitatively describes Ca(2+)-induced mPT as a two-step sequence of pre-swelling induction followed by Ca(2+)-driven, positive feedback, autocatalytic propagation. The model was formulated as two differential equations, each directly related to experimental parameters (Ca(2+) flux/mitochondrial swelling). These parameters were simultaneously assessed using a spectroscopic approach to monitor multiple mitochondrial properties. The derived kinetic model correctly identifies a correlation between initial Ca(2+) concentration and delay interval prior to mPT induction. Within the model's framework, Ru-360 (a ruthenium complex) and Mg(2+) were shown to compete with the Ca(2+)-stimulated initiation phase of mPT induction, consistent with known inhibition at the phenomenological level of the Ca(2+) uniporter. The model further reveals that Mg(2+), but not Ru-360, inhibits Ca(2+)-induced effects on a downstream stage of mPT induction at a site distinct from the uniporter. The analytical approach was then applied to promethazine, an FDA-approved drug previously shown to inhibit both mPT and ischemia-reperfusion injury. Kinetic analysis revealed that promethazine delayed mPT induction in a manner qualitatively distinct from that of lower concentrations of Mg(2+). In summary, we have developed a kinetic model to aid in the quantitative characterization of mPT induction. This model is consistent with/informative about the biochemistry of several mPT inhibitors, and its success suggests that this kinetic approach can aid in the classification of agents or targets that modulate mPT induction.

Highlights

  • Cellular Ca2ϩ concentration and a mitochondria-associated process

  • From a kinetic point of view, at least three conceptually distinct phases must be resolved during the mitochondrial permeability transition (mPT) induction: (i) the initiation phase, which includes the initial intake of excess Ca2ϩ via the Ca2ϩ uniporter; (ii) the “lag” phase, during which Ca2ϩ cycling induces or accompanies a series of reactions in mitochondria; and (iii) the propagation or termination phase

  • In the analysis that follows, only the kinetic data for Ca2ϩ concentration and mitochondria swelling were used to formulate the kinetic model of the mPT process

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Summary

Introduction

Cellular Ca2ϩ concentration and a mitochondria-associated process. These events have been hypothesized to be linked biochemically, because mitochondria are a major site for Ca2ϩ sequestration, normally absorbing excess cytosolic Ca2ϩ through the Ca2ϩ uniporter (which is driven by the membrane potential ⌬␸m) and releasing it via the Naϩ/Ca2ϩ and Ca2ϩ/Hϩ exchangers, resulting in a slow, continuous cycling of Ca2ϩ across the inner mitochondrial membrane. From a kinetic point of view, at least three conceptually distinct phases must be resolved during the mPT induction: (i) the initiation phase, which includes the initial intake of excess Ca2ϩ via the Ca2ϩ uniporter; (ii) the “lag” phase, during which Ca2ϩ cycling induces or accompanies a series of reactions in mitochondria (e.g. the pore constituents are recruited and possibly assembled); and (iii) the propagation or termination phase This final phase is associated with a decrease in membrane potential observable at the population level, release of mitochondrially sequestered Ca2ϩ (and a resultant increase in the steady-state Ca2ϩ concentration in the medium, which fuels subsequent Ca2ϩ uptake by the remaining intact mitochondria, creating a positive feedback loop for damage propagation), final pore assembly, and pore opening. The first order kinetic models developed by Massari [13] and used by Krasnikov et al [14] are only applicable at saturating concentrations of Ca2ϩ and fail to account for the lag phase often observed at lower, more (patho)physiologically relevant Ca2ϩ concentrations

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