Abstract Anaerobic microorganisms of the Geobacter genus are effective electron sources for the synthesis of nanoparticles, for bioremediation of polluted water, and for the production of electricity in fuel cells. In multistep reactions, electrons are transferred via iron/heme cofactors of c-type cytochromes from the inner cell membrane to extracellular metal ions, which are bound to outer membrane cytochromes. We measured electron production and electron flux rates to 5×105 e s−1 per G. sulfurreducens. Remarkably, these rates are independent of the oxidants, and follow zero order kinetics. It turned out that the microorganisms regulate electron flux rates by increasing their Fe2+/Fe3+ ratios in the multiheme cytochromes whenever the activity of the extracellular metal oxidants is diminished. By this mechanism the respiration remains constant even when oxidizing conditions are changing. This homeostasis is a vital condition for living systems, and makes G. sulfurreducens a versatile electron source.

Thermal perturbation of the dicluster ferredoxin from Acidianus ambivalens was investigated employing a toolbox of spectroscopic methods. FTIR and visible CD were used for assessing changes of the secondary structure and coarse alterations of the [3Fe4S] and [4Fe4S] cluster moieties, respectively. Fine details of the disassembly of the metal centers were revealed by paramagnetic NMR and resonance Raman spectroscopy. Overall, thermally induced unfolding of AaFd is initiated with the loss of α-helical content at relatively low temperatures (Tapp (m) ~ 44 °C), followed by the disruption of both iron−sulfur clusters (Tapp (m) ~ 53−60 °C). The degradation of the metal centers triggers major structural changes on the protein matrix, including the loss of tertiary contacts (Tapp (m) ~ 58 °C) and a change, rather than a significant net loss, of secondary structure (Tapp (m) ~ 60 °C). This latter process triggers a secondary structure reorganization that is consistent with the formation of a molten globule state. The combined spectroscopic approach here reported illustrates how changes in the metalloprotein organization are intertwined with disassembly of the iron−sulfur centers, denoting the conformational interplay of the protein backbone with cofactors.

The membranes of the thermoacidophilic archaeon Sulfolobus metallicus exhibit an oxygen consumption activity of 0.5 nmol O2 min−1 mg−1, which is insensitive to rotenone, suggesting the presence of a type-II NADH dehydrogenase. Following this observation, the enzyme was purified from solubilised membranes and characterised. The pure protein is a monomer with an apparent molecular mass of 49 kDa, having a high N-terminal amino acid sequence similarity towards other prokaryotic enzymes of the same type. It contains a covalently attached flavin, which was identified as being FMN by 31P-NMR spectroscopy, a novelty among type-II NADH dehydrogenases. Metal analysis showed the absence of iron, indicating that no FeS clusters are present in the protein. The average reduction potential of the FMN group was determined to be +160 mV, at 25 °C and pH 6.5, by redox titrations monitored by visible spectroscopy. Catalytically, the enzyme is a NADH:quinone oxidoreductase, as it is capable of transferring electrons from NADH to several quinones, including ubiquinone-1, ubiquinone-2 and caldariella quinone. Maximal turnover rates of 195 μmol NADH oxidized min−1 mg−1 at 60 °C were obtained using ubiquinone-2 as electron acceptor, after enzyme dilution and incubation with phospholipids.