Chemiosmotic systems in bioenergetics: H⁺-cycles and Na⁺-cycles

Abstract

The development of membrane bioenergetic studies during the last 25 years has clearly demonstrated the validity of the Mitchellian chemiosmotic H⁺ cycle concept. The circulation of H⁺ ions was shown to couple respiration-dependent or light-dependent energy-releasing reactions to ATP formation and performance of other types of membrane-linked work in mitochondria, chloroplasts, some bacteria, tonoplasts, secretory granules and plant and fungal outer cell membranes. A concrete version of the direct chemiosmotic mechanism, in which H⁺ potential formation is a simple consequence of the chemistry of the energy-releasing reaction, is already proved for the photosynthetic reaction centre complexes.

Recent progress in the studies on chemiosmotic systems has made it possible to extend the coupling-ion principle to an ion other than H⁺. It was found that, in ceertain bacteria, as well as in the outer membrane of the animal cell, Na⁺ effectively substitutes for H⁺ as the coupling ion (the chemiosmotic Na⁺ cycle). A precedent is set when the Na⁺ cycle appears to be the only mechanism of energy production in the bacterial cell. In the more typical case, however, the H⁺ and Na⁺ cycles coexist in one and the same membrane (bacteria) or in two diffeerent membranes of one and the same cell (animals). The sets of$\Delta \bar \mu H^ +$ and$\Delta \bar \mu Na^ +$ generators as well as$\Delta \bar \mu H^ +$ and$\Delta \bar \mu Na^ +$ consumers found in different types of biomembranes, are listed and discussed.