Calcium and regulation of the mitochondrial permeability transition

[Display omitted] •Permeability transition pore (PTP) is a Ca2+-activated channel whose prolonged openings can lead to depolarization, Ca2+ release and cell death.•Our working hypothesis is that the channel forms from F-ATP synthase dimers following Ca2+-binding to the catalytic site.•Ca2+ competes...

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Published inCell calcium (Edinburgh) Vol. 70; pp. 56 - 63
Main Authors Giorgio, Valentina, Guo, Lishu, Bassot, Claudio, Petronilli, Valeria, Bernardi, Paolo
Format Journal Article
LanguageEnglish
Published Netherlands Elsevier Ltd 01.03.2018
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Summary:[Display omitted] •Permeability transition pore (PTP) is a Ca2+-activated channel whose prolonged openings can lead to depolarization, Ca2+ release and cell death.•Our working hypothesis is that the channel forms from F-ATP synthase dimers following Ca2+-binding to the catalytic site.•Ca2+ competes with PTP-inhibitory Mg2+, and is an essential permissive factor for PTP opening.•Ca2+ binding could cause a conformational change transmitted via OSCP to the peripheral stalk and the the inner membrane. Recent years have seen renewed interest in the permeability transition pore, a high conductance channel responsible for permeabilization of the inner mitochondrial membrane, a process that leads to depolarization and Ca2+ release. Transient openings may be involved in physiological Ca2+ homeostasis while long-lasting openings may trigger and/or execute cell death. In this review we specifically focus (i) on the hypothesis that the PTP forms from the F-ATP synthase and (ii) on the mechanisms through which Ca2+ can reversibly switch this energy-conserving nanomachine into an energy-dissipating device.
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ISSN:0143-4160
1532-1991
DOI:10.1016/j.ceca.2017.05.004