The earliest known H+-PPase (proton-pumping inorganic pyrophosphatase), the integrally membrane-bound H+-PPi synthase (proton-pumping inorganic pyrophosphate synthase) from Rhodospirillum rubrum, is still the only alternative to H+-ATP synthase in biological electron transport phosphorylation. Cloning of several higher plant vacuolar H+-PPase genes has led to the recognition that the corresponding proteins form a family of extremely similar proton-pumping enzymes. The bacterial H+-PPi synthase and two algal vacuolar H+-PPases are homologous with this family, as deduced from their cloned genes. The prokaryotic and algal homologues differ more than the H+-PPases from higher plants, facilitating recognition of functionally significant entities. Primary structures of H+-PPases are reviewed and compared with H+-ATPases and soluble PPases.

SummarySuggestions by Calvin about a role of inorganic pyrophosphate (PPi) in early photosynthesis and by Lipmann that PPi may have been the original energy-rich phosphate donor in biological energy conversion, were followed in the mid-1960s by experimental results with isolated chromatophore membranes from the purple photosynthetic bacterium Rhodospirillum rubrum. PPi was shown to be hydrolysed in an uncoupler stimulated reaction by a membranebound inorganic pyrophosphatase (PPase), to be formed at the expense of light energy in photophosphorylation and to be utilized as an energy donor for various energy-requiring reactions, as a first known alternative to ATP. This direct link between PPi and photosynthesis led to increasing attention concerning the role of PPi in both early and present biological energy transfer. In the 1970s, the PPase was shown to be a proton pump and to be present also in higher plants. In the 1990s, sequences of H þ -PPase genes were obtained from plants, protists, bacteria and archaea and two classes of H þ -PPases differing in K þ sensitivity were established. Over 200 H þ -PPase sequences have now been determined. Recent biochemical and biophysical results have led to new progress and questions regarding the H þ -PPase family, as well as the families of soluble PPases and the inorganic polyphosphatases, which hydrolyse inorganic linear high-molecular-weight polyphosphates (HMWpolyP). Here we will focus attention on the H þ -PPases, their evolution and putative active site motifs, response to monovalent cations, genetic regulation and some very recent results, based on new methods for obtaining large quantities of purified protein, about their tertiary and quaternary structures. IUBMB Life, 59: 76-83, 2007

Inorganic pyrophosphate is identified as the major product of photophosphorylation by isolated chromatophores from Rhodospirillum rubrum in the absence of added nucleotides.

The discovery that photosynthetic bacterial membrane-bound inorganic pyrophosphatase (PPase) catalyzed light-induced phosphorylation of orthophosphate (Pi) to pyrophosphate (PPi) and the capability of PPi to drive energy requiring dark reactions supported PPi as a possible early alternative to ATP. Like the proton-pumping ATPase, the corresponding membrane-bound PPase also is a H+-pump, and like the Na+-pumping ATPase, it can be a Na+-pump, both in archaeal and bacterial membranes. We suggest that PPi and Na+ transport preceded ATP and H+ transport in association with geochemistry of the Earth at the time of the origin and early evolution of life. Life may have started in connection with early plate tectonic processes coupled to alkaline hydrothermal activity. A hydrothermal environment in which Na+ is abundant exists in sediment-starved subduction zones, like the Mariana forearc in the W Pacific Ocean. It is considered to mimic the Archean Earth. The forearc pore fluids have a pH up to 12.6, a Na+-concentration of 0.7 mol/kg seawater. PPi could have been formed during early subduction of oceanic lithosphere by dehydration of protonated orthophosphates. A key to PPi formation in these geological environments is a low local activity of water.

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