Respiratory chains from aerobic thermophilic prokaryotes.

Thermophiles are organisms that grow optimally above 50 degrees C and up to approximately 120 degrees C. These extreme conditions must have led to specific characteristics of the cellular components. In this paper we extensively analyze the types of respiratory complexes from thermophilic aerobic prokaryotes. The different membrane-bound complexes so far characterized are described, and the genomic data available for thermophilic archaea and bacteria are analyzed. It is observed that no specific characteristics can be associated to thermophilicity as the different types of complexes I-IV are present randomly in thermophilic aerobic organisms, as well as in mesophiles. Rather, the extensive genomic analyses indicate that the differences concerning the several complexes are related to the organism phylogeny, i.e., to evolution and lateral gene transfer events.

The quinol:fumarate oxidoreductase from the sulphate reducing bacterium Desulfovibrio gigas: spectroscopic and redox studies.

The membrane bound fumarate reductase (FRD) from the sulphate-reducer Desulfovibrio gigas was purified from cells grown on a fumarate/sulphate medium and extensively characterized. The FRD is isolated with three subunits of apparent molecular masses of 71, 31, and 22 kDa. The enzyme is capable of both fumarate reduction and succinate oxidation, exhibiting a higher specificity toward fumarate (Km for fumarate is 0.42 and for succinate 2 mM) and a reduction rate 30 times faster than that for oxidation. Studies by Visible and EPR spectroscopies allowed the identification of two B-type haems and the three iron-sulplur clusters usually found in FRDs and succinate dehydrogenases: [2Fe-2S]2+/1+ (S1), [4Fe-4S]2+/1+ (S2), and [3Fe-4S]1+/0 (S3). The apparent macroscopic reduction potentials for the metal centers, at pH 7.6, were determined by redox titrations: -45 and -175 mV for the two haems, and +20 and -140 mV for the S3 and SI clusters, respectively. The reduction potentials of the haem groups are pH dependent, supporting the proposal that fumarate reduction is associated with formation of the membrane proton gradient. Furthermore, co-reconstitution in liposomes of D. gigas FRD, duroquinone, and D. gigas cytochrome bd shows that this system is capable of coupling succinate oxidation with oxygen reduction to water.

Quinol:fumarate oxidoreductases and succinate:quinone oxidoreductases: phylogenetic relationships, metal centres and membrane attachment.

A comprehensive phylogenetic analysis of the core subunits of succinate:quinone oxidoreductases and quinol:fumarate oxidoreductases is performed, showing that the classification of the enzymes as type A to E based on the type of the membrane anchor fully correlates with the specific characteristics of the two core subunits. A special emphasis is given to the type E enzymes, which have an atypical association to the membrane, possibly involving anchor subunits with amphipathic helices. Furthermore, the redox properties of the SQR/QFR proteins are also reviewed, stressing out the recent observation of redox-Bohr effect upon haem reduction, observed for the Desulfovibrio gigas and Rhodothermus marinus enzymes, which indicates a direct protonation event at the haems or at a nearby residue. Finally, the possible contribution of these enzymes to the formation/dissipation of a transmembrane proton gradient is discussed, considering recent experimental and structural data.