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

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 and generators as well as and consumers found in different types of biomembranes, are listed and discussed.