scholarly journals The role of mitochondria in cellular iron–sulfur protein biogenesis and iron metabolism

2012 ◽  
Vol 1823 (9) ◽  
pp. 1491-1508 ◽  
Author(s):  
Roland Lill ◽  
Bastian Hoffmann ◽  
Sabine Molik ◽  
Antonio J. Pierik ◽  
Nicole Rietzschel ◽  
...  
2020 ◽  
Vol 401 (6-7) ◽  
pp. 855-876 ◽  
Author(s):  
Roland Lill

AbstractProtein cofactors often are the business ends of proteins, and are either synthesized inside cells or are taken up from the nutrition. A cofactor that strictly needs to be synthesized by cells is the iron-sulfur (Fe/S) cluster. This evolutionary ancient compound performs numerous biochemical functions including electron transfer, catalysis, sulfur mobilization, regulation and protein stabilization. Since the discovery of eukaryotic Fe/S protein biogenesis two decades ago, more than 30 biogenesis factors have been identified in mitochondria and cytosol. They support the synthesis, trafficking and target-specific insertion of Fe/S clusters. In this review, I first summarize what led to the initial discovery of Fe/S protein biogenesis in yeast. I then discuss the function and localization of Fe/S proteins in (non-green) eukaryotes. The major part of the review provides a detailed synopsis of the three major steps of mitochondrial Fe/S protein biogenesis, i.e. the de novo synthesis of a [2Fe-2S] cluster on a scaffold protein, the Hsp70 chaperone-mediated transfer of the cluster and integration into [2Fe-2S] recipient apoproteins, and the reductive fusion of [2Fe-2S] to [4Fe-4S] clusters and their subsequent assembly into target apoproteins. Finally, I summarize the current knowledge of the mechanisms underlying the maturation of cytosolic and nuclear Fe/S proteins.


2014 ◽  
Vol 111 (17) ◽  
pp. 6203-6208 ◽  
Author(s):  
L. Banci ◽  
D. Brancaccio ◽  
S. Ciofi-Baffoni ◽  
R. Del Conte ◽  
R. Gadepalli ◽  
...  

2020 ◽  
Vol 11 ◽  
Author(s):  
Jiri Kucera ◽  
Jan Lochman ◽  
Pavel Bouchal ◽  
Eva Pakostova ◽  
Kamil Mikulasek ◽  
...  

Hydrogen can serve as an electron donor for chemolithotrophic acidophiles, especially in the deep terrestrial subsurface and geothermal ecosystems. Nevertheless, the current knowledge of hydrogen utilization by mesophilic acidophiles is minimal. A multi-omics analysis was applied on Acidithiobacillus ferrooxidans growing on hydrogen, and a respiratory model was proposed. In the model, [NiFe] hydrogenases oxidize hydrogen to two protons and two electrons. The electrons are used to reduce membrane-soluble ubiquinone to ubiquinol. Genetically associated iron-sulfur proteins mediate electron relay from the hydrogenases to the ubiquinone pool. Under aerobic conditions, reduced ubiquinol transfers electrons to either cytochrome aa3 oxidase via cytochrome bc1 complex and cytochrome c4 or the alternate directly to cytochrome bd oxidase, resulting in proton efflux and reduction of oxygen. Under anaerobic conditions, reduced ubiquinol transfers electrons to outer membrane cytochrome c (ferrireductase) via cytochrome bc1 complex and a cascade of electron transporters (cytochrome c4, cytochrome c552, rusticyanin, and high potential iron-sulfur protein), resulting in proton efflux and reduction of ferric iron. The proton gradient generated by hydrogen oxidation maintains the membrane potential and allows the generation of ATP and NADH. These results further clarify the role of extremophiles in biogeochemical processes and their impact on the composition of the deep terrestrial subsurface.


2021 ◽  
Vol 1868 (1) ◽  
pp. 118863
Author(s):  
Joseph J. Braymer ◽  
Sven A. Freibert ◽  
Magdalena Rakwalska-Bange ◽  
Roland Lill

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