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Mitochondrial complex I is a 1MDa membrane protein complex with a central role in aerobic energy metabolism. The bioenergetic core functions are executed by 14 central subunits that are conserved from bacteria to man. Despite recent progress in structure determination, our understanding of the function of the ~30 accessory subunits associated with the mitochondrial complex is still limited. We have investigated the structure of complex I from the aerobic yeast Yarrowia lipolytica by cryo-electron microscopy. Our density map at 7.9Å resolution closely matches the 3.6-3.9Å X-ray structure of the Yarrowia lipolytica complex. However, the cryo-EM map indicated an additional subunit on the side of the matrix arm above the membrane surface, pointing away from the membrane arm. The density, which is not present in any previously described complex I structure and occurs in about 20 % of the particles, was identified as the accessory sulfur transferase subunit ST1. The Yarrowia lipolytica complex I preparation is active in generating H2S from the cysteine derivative 3-mercaptopyruvate, catalyzed by ST1. We thus provide evidence for a link between respiratory complex I and mitochondrial sulfur metabolism.
Anaerobic ammonium oxidation (anammox) is a major process in the biogeochemical nitrogen cycle in which nitrite and ammonium are converted to dinitrogen gas and water through the highly reactive intermediate hydrazine. So far, it is unknown how anammox organisms convert the toxic hydrazine into nitrogen and harvest the extremely low potential electrons (−750 mV) released in this process. We report the crystal structure and cryo electron microscopy structures of the responsible enzyme, hydrazine dehydrogenase, which is a 1.7 MDa multiprotein complex containing an extended electron transfer network of 192 heme groups spanning the entire complex. This unique molecular arrangement suggests a way in which the protein stores and releases the electrons obtained from hydrazine conversion, the final step in the globally important anammox process.
Nitrate is an abundant nutrient and electron acceptor throughout Earth’s biosphere. Virtually all nitrate in nature is produced by the oxidation of nitrite by the nitrite oxidoreductase (NXR) multiprotein complex. NXR is a crucial enzyme in the global biological nitrogen cycle, and is found in nitrite-oxidizing bacteria (including comammox organisms), which generate the bulk of the nitrate in the environment, and in anaerobic ammonium-oxidizing (anammox) bacteria which produce half of the dinitrogen gas in our atmosphere. However, despite its central role in biology and decades of intense study, no structural information on NXR is available. Here, we present a structural and biochemical analysis of the NXR from the anammox bacterium Kuenenia stuttgartiensis, integrating X-ray crystallography, cryo-electron tomography, helical reconstruction cryo-electron microscopy, interaction and reconstitution studies and enzyme kinetics. We find that NXR catalyses both nitrite oxidation and nitrate reduction, and show that in the cell, NXR is arranged in tubules several hundred nanometres long. We reveal the tubule architecture and show that tubule formation is induced by a previously unidentified, haem-containing subunit, NXR-T. The results also reveal unexpected features in the active site of the enzyme, an unusual cofactor coordination in the protein’s electron transport chain, and elucidate the electron transfer pathways within the complex.
High-resolution cryo-EM structures of respiratory complex I: Mechanism, assembly, and disease
(2019)
Respiratory complex I is a redox-driven proton pump, accounting for a large part of the electrochemical gradient that powers mitochondrial adenosine triphosphate synthesis. Complex I dysfunction is associated with severe human diseases. Assembly of the one-megadalton complex I in the inner mitochondrial membrane requires assembly factors and chaperones. We have determined the structure of complex I from the aerobic yeast Yarrowia lipolytica by electron cryo-microscopy at 3.2-Å resolution. A ubiquinone molecule was identified in the access path to the active site. The electron cryo-microscopy structure indicated an unusual lipid-protein arrangement at the junction of membrane and matrix arms that was confirmed by molecular simulations. The structure of a complex I mutant and an assembly intermediate provide detailed molecular insights into the cause of a hereditary complex I-linked disease and complex I assembly in the inner mitochondrial membrane.
Mitochondrial complex I has a key role in cellular energy metabolism, generating a major portion of the proton motive force that drives aerobic ATP synthesis. The hydrophilic arm of the L-shaped ~1 MDa membrane protein complex transfers electrons from NADH to ubiquinone, providing the energy to drive proton pumping at distant sites in the membrane arm. The critical steps of energy conversion are associated with the redox chemistry of ubiquinone. We report the cryo-EM structure of complete mitochondrial complex I from the aerobic yeast Yarrowia lipolytica both in the deactive form and after capturing the enzyme during steady-state activity. The site of ubiquinone binding observed during turnover supports a two-state stabilization change mechanism for complex I.
Highlights
• Cryo-EM structure of a yeast F1Fo-ATP synthase dimer
• Inhibitor-free X-ray structure of the F1 head and rotor complex
• Mechanism of ATP generation by rotary catalysis
• Structural basis of cristae formation in the inner mitochondrial membrane
Summary
We determined the structure of a complete, dimeric F1Fo-ATP synthase from yeast Yarrowia lipolytica mitochondria by a combination of cryo-EM and X-ray crystallography. The final structure resolves 58 of the 60 dimer subunits. Horizontal helices of subunit a in Fo wrap around the c-ring rotor, and a total of six vertical helices assigned to subunits a, b, f, i, and 8 span the membrane. Subunit 8 (A6L in human) is an evolutionary derivative of the bacterial b subunit. On the lumenal membrane surface, subunit f establishes direct contact between the two monomers. Comparison with a cryo-EM map of the F1Fo monomer identifies subunits e and g at the lateral dimer interface. They do not form dimer contacts but enable dimer formation by inducing.
In dieser Arbeit wurden zwei Schlüsselenzyme des Energiestoffwechsels in Archaeen im Hinblick auf ihre funktionellen, spektroskopischen und strukturellen Eigenschaften untersucht. Die Heterodisulfid-Reduktase (Hdr) katalysiert die Reduktion des terminalen Elektronenakzeptors CoM-S-S-CoB zu CoM-SH (Coenzym M) und CoB-SH (Coenzym B) und spielt eine Schlüsselrolle im zentralen Energie-konservierenden Prozess von methanogenen Archaeen. Hdr existiert in Form von zwei unterschiedlichen Enzymen: HdrDE und HdrABC. Beide weisen ein charakteristisches Cystein-reiches Sequenzmotiv (CCG-Domäne) auf, welches als Bindestelle für ein ungewöhliches [4Fe-4S]-Zentrum dient. Frühere Studien zeigten, dass das [4Fe-4S]-Zentrum in der Untereinheit HdrB lokalisiert ist und als zentraler Bestandteil des aktiven Zentrums die Fähigkeit besitzt, ein Thiyl-Radikal zu binden. Darauf aufbauend wurden genetische, spektroskopische und strukturelle Untersuchungen überwiegend am H2:Heterodisulfid-Oxidoreduktase-Komplex (Mvh:Hdr) aus Methanothermobacter marburgensis oder an der heterolog produzierten Untereinheit HdrB durchgeführt. Das Reinigungsprotokoll des Mvh:Hdr-Komplexes wurde für Kristallisationsexperimente und für ENDOR- und Mössbauer-spektroskopische Studien optimiert. Eine Kristallisation des Mvh:Hdr-Komplexes gelang nicht; doch konnten Kristalle der Heterodisulfid-Reduktase-assoziierten Hydrogenase (Mvh) bis zu einer Auflösung von 3.34 Å vermessen und mit Hilfe der anomalen Information der Elektronentransferweg zwischen den [Fe-S]-Clustern definiert werden. Ergänzende elektronenmikroskopische Studien zeigten einen unsymmetrischen Aufbau des Komplexes. DesWeiteren wurde die Untereinheit HdrB aus M. marburgensis in Methanosarcina acetivorans heterolog produziert und seine Funktionalität kinetisch und spektroskopisch nachgewiesen. Ferner wurde HdrB in Escherichia coli heterolog produziert und gereinigt, um Kristallisationsexperimente durchzuführen und es für ENDOR- und Mössbauer-Studien verfügbar zu machen. Um HdrB spektroskopisch zu vergleichen, wurde eine Untereinheit der Succinat:Chinon Oxidoreduktase (SdhE) aus Sulfolobus solfataricus ebenfalls heterolog in E. coli produziert und mittels ENDOR-Spektroskopie charakterisiert. Ein grundlegender Prozess des biogeochemischen Schwefelkreislaufes ist die dissimilatorische Sulfat-Reduktion, in der Sulfat (SO4 2􀀀) zu Schwefelwasserstoff (H2S) umgewandelt wird. Die dissimilatorische Sulfit-Reduktase (dSir), das Schlüsselenzym im Energiestoffwechsel der Sulfat-Reduzierer, besitzt einen einzigartigen Sirohäm-[4Fe-4S]-Cofaktor, der die Reduktion von Sulfit (SO3 2􀀀) zu H2S in einem 6-Elektronen-Schritt katalysiert. Um diesen Mechanismus zu untersuchen, wurden kinetische, spektroskopische und röntxi Zusammenfassung genkristallographische Methoden angewandt. Die Kristallstrukturen von dSir aus Archaeoglobus fulgidus wurden im Komplex mit Sulfit, Sulfid (S2􀀀), Kohlenmonoxid (CO), Cyanid (CN􀀀), Nitrit (NO2􀀀), Nitrat (NO3 􀀀) und Phosphat (PO4 3􀀀) gelöst. Aktivitätstest und analytische Studien zeigten, dass dSir von A. fulgidus neben Sulfit und Nitrit auch Thiosulfat und Trithionat reduziert und Letztere auch als Intermediate entstehen. Auf dieser Basis wurde ein 3-Stufen-Mechanismus postuliert, wobei jede Stufe aus einem 2-Elektronentransfer, einer Aufnahme von zwei Protonen und einer Dehydrationsreaktion besteht. Im Vergleich zur assimilatorischen Sulfit-Reduktase (aSir) aus E. coli zeigt die dSir-Struktur einen veränderten Substratkanal, eine Rotation des Sulfits um 60° und beträchtliche Konformationsänderungen der katalytischen Reste Arga170 und Lysa211. Aufgrund dieser Änderungen kann ausschließlich in dSir ein weiteres Sulfit-Molekül in van-der-Waals-Kontakt zum an das Sirohäm-gebundene Sulfit oder Schwefel-Sauerstoff-Zwischenprodukt platziert werden, das nötig ist, um Thiosulfat und Trithionat zu synthetisieren.
Mitochondrial NADH:ubiquinone oxidoreductase (complex I) is a 1 MDa membrane protein complex with a central role in energy metabolism. Redox-driven proton translocation by complex I contributes substantially to the proton motive force that drives ATP synthase. Several structures of complex I from bacteria and mitochondria have been determined but its catalytic mechanism has remained controversial. We here present the cryo-EM structure of complex I from Yarrowia lipolytica at 2.1 Å resolution, which reveals the positions of more than 1600 protein-bound water molecules, of which ∼100 are located in putative proton translocation pathways. Another structure of the same complex under steady-state activity conditions at 3.4 Å resolution indicates conformational transitions that we associate with proton injection into the central hydrophilic axis. By combining high-resolution structural data with site-directed mutagenesis and large-scale molecular dynamics simulations, we define details of the proton translocation pathways, and offer new insights into the redox-coupled proton pumping mechanism of complex I.
Mitochondrial NADH:ubiquinone oxidoreductase (complex I) is a 1-MDa membrane protein complex with a central role in energy metabolism. Redox-driven proton translocation by complex I contributes substantially to the proton motive force that drives ATP synthase. Several structures of complex I from bacteria and mitochondria have been determined, but its catalytic mechanism has remained controversial. We here present the cryo-EM structure of complex I from Yarrowia lipolytica at 2.1-Å resolution, which reveals the positions of more than 1600 protein-bound water molecules, of which ~100 are located in putative proton translocation pathways. Another structure of the same complex under steady-state activity conditions at 3.4-Å resolution indicates conformational transitions that we associate with proton injection into the central hydrophilic axis. By combining high-resolution structural data with site-directed mutagenesis and large-scale molecular dynamic simulations, we define details of the proton translocation pathways and offer insights into the redox-coupled proton pumping mechanism of complex I.