Metal limitation of cyanobacterial N2 fixation and implications for the Precambrian nitrogen cycle

Nitrogen fixation is a critical part of the global nitrogen cycle, replacing biologically available reduced nitrogen lost by denitrification. The redox‐sensitive trace metals Fe and Mo are key components of the primary nitrogenase enzyme used by cyanobacteria (and other prokaryotes) to fix atmospheric N₂ into bioessential compounds. Progressive oxygenation of the Earth's atmosphere has forced changes in the redox state of the oceans through geologic time, from anoxic Fe‐enriched waters in the Archean to partially sulfidic deep waters by the mid‐Proterozoic. This development of ocean redox chemistry during the Precambrian led to fluctuations in Fe and Mo availability that could have significantly impacted the ability of prokaryotes to fix nitrogen. It has been suggested that metal limitation of nitrogen fixation and nitrate assimilation, along with increased rates of denitrification, could have resulted in globally reduced rates of primary production and nitrogen‐starved oceans through much of the Proterozoic. To test the first part of this hypothesis, we grew N₂‐fixing cyanobacteria in cultures with metal concentrations reflecting an anoxic Archean ocean (high Fe, low Mo), a sulfidic Proterozoic ocean (low Fe, moderate Mo), and an oxic Phanerozoic ocean (low Fe, high Mo). We measured low rates of cellular N₂ fixation under [Fe] and [Mo] estimated for the Archean ocean. With decreased [Fe] and higher [Mo] representing sulfidic Proterozoic conditions, N₂ fixation, growth, and biomass C:N were similar to those observed with metal concentrations of the fully oxygenated oceans that likely developed in the Phanerozoic. Our results raise the possibility that an initial rise in atmospheric oxygen could actually have enhanced nitrogen fixation rates to near modern marine levels, providing that phosphate was available and rising O₂ levels did not markedly inhibit nitrogenase activity.     

Reconstructing the evolutionary history of nitrogenases: Evidence for ancestral molybdenum‐cofactor utilization

The nitrogenase metalloenzyme family, essential for supplying fixed nitrogen to the biosphere, is one of life's key biogeochemical innovations. The three forms of nitrogenase differ in their metal dependence, each binding either a FeMo‐, FeV‐, or FeFe‐cofactor where the reduction of dinitrogen takes place. The history of nitrogenase metal dependence has been of particular interest due to the possible implication that ancient marine metal availabilities have significantly constrained nitrogenase evolution over geologic time. Here, we reconstructed the evolutionary history of nitrogenases, and combined phylogenetic reconstruction, ancestral sequence inference, and structural homology modeling to evaluate the potential metal dependence of ancient nitrogenases. We find that active‐site sequence features can reliably distinguish extant Mo‐nitrogenases from V‐ and Fe‐nitrogenases and that inferred ancestral sequences at the deepest nodes of the phylogeny suggest these ancient proteins most resemble modern Mo‐nitrogenases. Taxa representing early‐branching nitrogenase lineages lack one or more biosynthetic nifE and nifN genes that both contribute to the assembly of the FeMo‐cofactor in studied organisms, suggesting that early Mo‐nitrogenases may have utilized an alternate and/or simplified pathway for cofactor biosynthesis. Our results underscore the profound impacts that protein‐level innovations likely had on shaping global biogeochemical cycles throughout the Precambrian, in contrast to organism‐level innovations that characterize the Phanerozoic Eon.     

Cell biology of molybdenum in plants and humans

The transition element molybdenum (Mo) needs to be complexed by a special cofactor in order to gain catalytic activity. With the exception of bacterial Mo-nitrogenase, where Mo is a constituent of the FeMo-cofactor, Mo is bound to a pterin, thus forming the molybdenum cofactor Moco, which in different variants is the active compound at the catalytic site of all other Mo-containing enzymes. In eukaryotes, the most prominent Mo-enzymes are nitrate reductase, sulfite oxidase, xanthine dehydrogenase, aldehyde oxidase, and the mitochondrial amidoxime reductase. The biosynthesis of Moco involves the complex interaction of six proteins and is a process of four steps, which also requires iron, ATP and copper. After its synthesis, Moco is distributed to the apoproteins of Mo-enzymes by Moco-carrier/binding proteins. A deficiency in the biosynthesis of Moco has lethal consequences for the respective organisms. In humans, Moco deficiency is a severe inherited inborn error in metabolism resulting in severe neurodegeneration in newborns and causing early childhood death. This article is part of a Special Issue entitled: Cell Biology of Metals.     

Insertion of heterometals into the NifEN-associated iron–molybdenum cofactor precursor

The cofactors of Mo-, V-, Fe-dependent nitrogenases are believed to be highly homologous in structure despite the different types of heterometals (Mo, V, and Fe) they contain. Previously, a precursor form of the FeMo cofactor (FeMoco) was captured on NifEN, a scaffold protein for FeMoco biosynthesis. This all-Fe precursor closely resembles the Fe/S core structure of the FeMoco and, therefore, could reasonably serve as a precursor for all nitrogenase cofactors. Here, we report the heterologous incorporation of V and Fe into the NifEN-associated FeMoco precursor. EPR and activity analyses indicate that V and Fe can be inserted at much reduced efficiencies compared with Mo, and incorporation of both V and Fe is enhanced in the presence of homocitrate. Further, native polyacrylamide gel electrophoresis experiments suggest that NifEN undergoes a significant conformational rearrangement upon metal insertion, which allows the subsequent NifEN–MoFe protein interactions and the transfer of the cofactor between the two proteins. The combined outcome of these in vitro studies leads to the proposal of a selective mechanism that is utilized in vivo to maintain the specificity of heterometals in nitrogenase cofactors, which is likely accomplished through the redox regulation of metal mobilization by different Fe proteins (encoded by nifH, vnfH, and anfH, respectively), as well as the differential interactions between these Fe proteins and their respective scaffold proteins (NifEN and VnfEN) in the Mo-, V-, and Fe-dependent nitrogenase systems.     

Molybdenum independence of nitrogenase component synthesis in the non-heterocystous cyanobacterium Plectonema.

The cyanobacterium Plectonema boryanum (IU 594-UTEX 594) fixes N2 only in the absence of combined N and of O2. We induced nitrogenase by transfer to anaerobic N-free medium and studied the effect of Mo starvation on nitrogenase activity and synthesis. Activity was first detected within 3 h after transfer by the acetylene reduction assay in controls, increasing for at least 25 h. Cells grown on nitrate and Mo and then transferred to N-free, Mo-free medium produced 8% of the control nitrogenase activity. Addition of W to the Mo-free medium reduced the activity to 0.5%. Under both Mo starvation conditions, nitrogenase protein components were synthesized. Component II of the cyanobacterial enzyme was detected by in vitro complementation with Mo-containing component I from Klebsiella pneumoniae or Azotobacter vinelandii but not Clostridium pasteurianum. Component I activity was restored by addition of Mo to cultures in which new enzyme synthesis was blocked by chloramphenicol. Acidified extracts of Plectonema induced in Mo-containing medium contained the Fe-Mo cofactor required to activate extracts of the Azotobacter mutant UW45 in vitro, but they did not activate extracts of Mo-starved Plectonema. Analysis of 35SO4(2-)-labeled proteins by polyacrylamide gel electrophoresis suggested that Mo is required for the conversion of a high-molecular-weight precursor to component I in Plectonema.     

Cell biology of molybdenum in plants

The transition element molybdenum (Mo) is of essential importance for (nearly) all biological systems as it is required by enzymes catalyzing important reactions within the cell. The metal itself is biologically inactive unless it is complexed by a special cofactor. With the exception of bacterial nitrogenase, where Mo is a constituent of the FeMo-cofactor, Mo is bound to a pterin, thus forming the molybdenum cofactor (Moco) which is the active compound at the catalytic site of all other Mo-enzymes. In plants, the most prominent Mo-enzymes are nitrate reductase, sulfite oxidase, xanthine dehydrogenase, aldehyde oxidase, and the mitochondrial amidoxime reductase. The biosynthesis of Moco involves the complex interaction of six proteins and is a process of four steps, which also includes iron as well as copper in an indispensable way. After its synthesis, Moco is distributed to the apoproteins of Mo-enzymes by Moco-carrier/binding proteins that also participate in Moco-insertion into the cognate apoproteins. Xanthine dehydrogenase and aldehyde oxidase, but not the other Mo-enzymes, require a final step of posttranslational activation of their catalytic Mo-center for becoming active.     

The vanadium-containing nitrogenase of Azotobacter

Fifty years after a role of vanadium in biological fixation was proposed, it was shown that in addition to their well-characterized molybdendum nitrogenases, Azotobacter chroococcum and Azotobacter vinelandii both have a genetically distinct nitrogenase system in which the conventional molybdoprotein is replaced by a vanadoprotein. Both Mo-nitrogenases and V-nitrogenases have similar requirements for activity: MgATP, a low potential reductant and the absence of oxygen. The genes encoding the V-nitrogenase are expressed only under conditions of Mo-deficiency. V-Nitrogenase of A.chroococcum is made up of a tetrameric VFe protein (Mr 210,000) with an alpha 2 beta 2 structure containing two V atoms, 23 Fe atoms and 20 acid-labile sulphide atoms per tetramer, and a dimeric Fe protein (Mr 64,000) with a gamma 2 structure containing four Fe atoms and four acid-labile sulphide atoms per dimer. Vanadium K-edge X-ray absorption spectroscopy indicates that V in the VFe protein, like Mo in MoFe protein, has S, Fe and possibly O as nearest neighbours. A vanadium- and iron-containing cofactor (FeVaco) can be extracted from the VFe protein and will restore C2H2 reductase, but no nitrogenase activity, to the inactive MoFe protein accumulated by mutants unable to synthesize the molybdenum- and iron-containing co-factor of Mo-nitrogenase. The products of C2H2 reduction by the hybrid protein (C2H6 as well as C2H4) are a characteristic of the VFe protein and provide evidence that FeVaco is, or forms part of the active site of V-nitrogenase.     

Transport of molybdate in the cyanobacterium Anabaena variabilis ATCC 29413

Heterocyst-forming filamentous cyanobacteria, such as Anabaena variabilis ATCC 29413, require molybdenum as a component of two essential cofactors for the enzymes nitrate reductase and nitrogenase. A. variabilis efficiently transported (99)Mo (molybdate) at concentrations less than 10(-9) M. Competition experiments with other oxyanions suggested that the molybdate-transport system of A. variabilis also transported tungstate but not vanadate or sulfate. Although tungstate was probably transported, tungsten did not function in place of molybdenum in the Mo-nitrogenase. Transport of (99)Mo required prior starvation of the cells for molybdate, suggesting that the Mo-transport system was repressed by molybdate. Starvation, which required several generations of growth for depletion of molybdate, was enhanced by growth under conditions that required synthesis of nitrate reductase or nitrogenase. These data provide evidence for a molybdate storage system in A. variabilis. NtcA, a regulatory protein that is essential for synthesis of nitrate reductase and nitrogenase, was not required for transport of molybdate. The closely related strain Anabaena sp. PCC 7120 transported (99)Mo in a very similar way to A. variabilis.     

An atomic level model for the interactions of molybdenum nitrogenase with carbon monoxide, acetylene, and ethylene

A combination of density functional theory and molecular mechanics calculations has been used to study the possible interactions of CO, C(2)H(2), and C(2)H(4) with the central Fe and terminal Mo sites of the iron-molybdenum cofactor of nitrogenase. The most favorable binding mode for CO on the central section of the FeMoco appears to be end-on to a single Fe and results in a change from high to low spin for the ligating Fe atom. If a coordination site for CO is available on the Mo, this becomes the preferred CO binding site. Calculated nu(CO) infrared frequencies are compared with the experimental values given in the literature. C(2)H(2) binds weakly in a side-on orientation to a single Fe site; addition of a single H(+)/e(-) couple to the substrate results in spontaneous migration of the resulting -CH=CH(2) group from Fe to a central S atom of the cofactor. Further reduction liberates C(2)H(4) or alternatively can give an S=CHCH(3) intermediate, which then goes on to produce C(2)H(6). A model for C(2)H(2) reduction by nitrogenase is proposed, based on the results of the calculations and the extensive literature on this process.     

Immunological evidence for the capability of free-living Rhizobium japonicum to synthesize a portion of a nitrogenase component

Immunodiffusion tests conducted under aerobic conditions demonstrated that cross-reactive material to antiserum prepared against the MoFe protein component of nitrogenase from soybean nodule bacteroids was detectable in extracts of free-living Rhizobium japonicum cells cultured in a standard medium under: aerobic conditions; aerobic conditions with nitrate; aerobic conditions with ammonia; anaerobic conditions with nitrate; and anaerobic conditions with nitrate and ammonia. The most intense precipitin bands resulted from cross-section of the antiserum with extracts of cells cultured anaerobically with nitrate or anaerobically with ammonia and nitrate. Immunodiffusion experiments with crude bacteroid extract and purified MoFe protein revealed a greater number of precipitin bands in tests conducted under aerobic conditions than those conducted under anaerobic conditions. These results indicate that some of the cross-reactive material observed under aerobic conditions resulted from breakdown of the MoFe protein. Bacteroid extracts of nodules from plants supplied with ammonia exhibited only a trace of nitrogenase activity. The addition of an excess of the Fe protein component of nitrogenase, however, resulted in a 270-fold enhancement of activity indicating the presence of active MoFe protein in these extracts.Our experiments together with results published elsewhere provide evidence that the genetic information for synthesis of a part of the MoFe component of nitrogenase is carried by Rhizobium.     

Carbon substrate re-orders relative growth of a bacterium using Mo-, V-, or Fe-nitrogenase for nitrogen fixation

Biological nitrogen fixation is catalyzed by the molybdenum (Mo), vanadium (V) and iron (Fe)-only nitrogenase metalloenzymes. Studies with purified enzymes have found that the ‘alternative’ V- and Fe-nitrogenases generally reduce N₂ more slowly and produce more byproduct H₂ than the Mo-nitrogenase, leading to an assumption that their usage results in slower growth. Here we show that, in the metabolically versatile photoheterotroph Rhodopseudomonas palustris, the type of carbon substrate influences the relative rates of diazotrophic growth based on different nitrogenase isoforms. The V-nitrogenase supports growth as fast as the Mo-nitrogenase on acetate but not on the more oxidized substrate succinate. Our data suggest that this is due to insufficient electron flux to the V-nitrogenase isoform on succinate compared with acetate. Despite slightly faster growth based on the V-nitrogenase on acetate, the wild-type strain uses exclusively the Mo-nitrogenase on both carbon substrates. Notably, the differences in H₂:N₂ stoichiometry by alternative nitrogenases (~1.5 for V-nitrogenase, ~4–7 for Fe-nitrogenase) and Mo-nitrogenase (~1) measured here are lower than prior in vitro estimates. These results indicate that the metabolic costs of V-based nitrogen fixation could be less significant for growth than previously assumed, helping explain why alternative nitrogenase genes persist in diverse diazotroph lineages and are broadly distributed in the environment.     

A new method for extraction of iron-molybdenum cofactor (FeMoco) from nitrogenase adsorbed to DEAE-cellulose. 1. Effects of anions, cations, and preextraction treatments

A convenient and rapid method of obtaining the cofactor of nitrogenase (FeMoco) with a low and apparently limiting Fe/Mo ratio has been developed. FeMoco can be extracted from the MoFe protein bound to DEAE-cellulose. The cofactor is eluted in either N-methylformamide (NMF), N,N-dimethylformamide (DMF), or mixtures of these solvents by use of salts such as Et4NBr,Bu4NBr,Ph4PCl, and Ph4AsCl. The method is simple, is rapid (45 min), yields concentrated cofactor, and, unlike the original method [Shah, V. K., & Brill, W. J. (1977) Proc. Natl. Acad. Sci. U.S.A. 74, 3249-3253] which requires anaerobic centrifugation, is easily scaled up. Furthermore, it gives yields of cofactor in excess of 70%. Its disadvantages are a high Fe:Mo ratio when DMF is the extracting solvent and a high salt concentration in the resultant FeMoco solution. These disadvantages are easily overcome by removing excess Fe by pretreating the cofactor with bipyridyl while still on the column. This gives Fe:Mo ratios of (6 +/- 1):1 (11 trials) with specific activities ranging from 170 to 220 nmol of C2H4/[min.(nmol of Mo)]. Chromatography on Sephadex LH-20 removes ca. 99% of the excess salt. The adsorption of MoFe protein to DEAE-cellulose seems to facilitate denaturation by organic solvents so that pretreatment of the protein with acid, used in earlier methods, is unnecessary. There is an apparent dependence on the charge density of the anion employed for elution of FeMoco bound to DEAE-cellulose, such that Cl- greater than Br- much greater than I-, PF6- is the order of effectiveness of the Bu4N+ salts of these anions.(ABSTRACT TRUNCATED AT 250 WORDS)     

An atomic-level mechanism for molybdenum nitrogenase. Part 1. Reduction of dinitrogen

The properties of the Fe and Mo sites of the iron-molybdenum cofactor of nitrogenase with respect to binding and activation of N(2) have been studied by molecular mechanics calculations on the local protein environment and by density functional theory (DFT) calculations on subsections of the cofactor. The DFT calculations indicate that the homocitrate ligand of the cofactor can become monodentate on reduction, allowing N(2) to bind at Mo. In addition, the neighboring Fe atom plays a crucial role in N(2) reduction by stabilizing the initial reduced N(2) species and by facilitating cleavage of the N-N bond. The various possible isomers for partially reduced N(2) intermediates have been compared by DFT, and a detailed model for the reduction of N(2) is developed based on these results, together with chemical precedents and the available biochemical data for nitrogenase.     

Role of ammona in regulation of nitrogenase synthesis and activity in Anabaena cylindrica

The regulation of nitrogenase biosynthesis and activity by ammonia was studied in the heterocystous cyanobacterium Anabaena cylindrica. Nitrogenase synthesis was measured by in vivo acetylene reduction assays and in vitro by an activity-independent, immunoelectrophoretic measurement of the Fe-Mo protein (Component I). When ammonia was added to differentiating cultures after a point when heterocyst differentiation became irreversible, FeMo protein synthesis was also insensitive to ammonia. Treating log-phase batch cultures with 100% O₂ for 30 min resulted in a loss of 90% of nitrogenase activity and a 50% loss of the FeMo protein. Recovery was inhibited by chloramphenicol but not by ammonia or urea. The addition of ammonia to log-phase cultures resulted in a decrease in specific levels of nitrogenase activity and FeMo protein that occurred at the same rate as algal growth and was independent of O₂ tension of the culture media. However, in light-limited linear-phase cultures, ammonia effected a dramatic inhibition of nitrogenase activity. These results indicate that nitrogenase biosynthesis becomes insensitive to repression by ammonia as heterocysts mature and that ammonia or its metabolites act to regulate nitrogen fixation by inhibiting heterocyst differentiation and by inhibiting nitrogenase activity through competition with nitrogenase for reductant and/or ATP, but not by directly regulating nitrogenase biosynthesis in heterocysts.     

Identification of an Fe protein residue (Glu146) of Azotobacter vinelandii nitrogenase that is specifically involved in FeMo cofactor insertion

The Fe protein of nitrogenase has three separate functions. Much is known about the regions of the protein that are critical to its function as an electron donor to the MoFe protein, but almost nothing is known about the regions of the protein that are critical to its functions in either FeMo cofactor biosynthesis or FeMo cofactor insertion. Using computer modeling and information obtained from Fe protein mutants that were made decades ago by chemical mutagenesis, we targeted a surface residue Glu(146) as potentially being involved in FeMo cofactor biosynthesis and/or insertion. The Azotobacter vinelandii strain expressing an E146D Fe protein variant grows at approximately 50% of the wild type rate. The purified E146D Fe protein is fully functional as an electron donor to the MoFe protein, but the MoFe protein synthesized by that strain is partially ( approximately 50%) FeMo cofactor-deficient. The E146D Fe protein is fully functional in an in vitro FeMo cofactor biosynthesis assay, and the strain expressing this protein accumulates "free" FeMo cofactor. Assays that compared the ability of wild type and E146D Fe proteins to participate in FeMo cofactor insertion demonstrate, however, that the mutant is severely altered in this last reaction. This is the first known mutation that only influences the insertion reaction.     

A facile method of isolation for the iron molybdenum cofactor of nitrogenase and bacterial ferritin from extracts of azotobacter vinelandii

An alternative method has been developed for the isolation of both the iron molybdenum cofactor of nitrogenase (FeMoco), a small molecular weight FeMoS cluster which is the putative nitrogen- reducing site of the enzyme, and bacterioferritin, an iron storage protein similar to other ferritins, but containing heme prosthetic groups. Previously the isolation of these two species, the characterization of which is of significant current interest, has been dependent on the purification of the nitrogenase enzyme from Azotobacter vinelandii. Out new procedure eliminates the use of the anaerobic column chromatography necessary to obtain pure nitrogenase components, involving instead the heat and RNAase/ DNAase treatment of crude extracts of ruptured cells followed by sedimentation (150000 × g for 18 h) of both the 'nitrogenase complex' and bacterioferritin. The redissolved pellet from this centrifugation yields the pure crystalline bacterioferritin on addition of Mg²⁺. and cooling, the iron content of the protein being higher by this method than in previous reports. Likewise, denaturation by acid/base treatment of this protein mixture yields a precipitate which can be extracted with either N-methylformamide or N,N-dimethylformamide containing dithionite ion to yield solutions of FeMoco, as evidenced by UW 45 reconstitution and EPR spectral criteria. Unfortunately, preparations of FeMoco obtained by this method have a variable, but consistently low, Fe/Mo ratio and additional visible spectral features, indicating that they are significantly less pure than that those generated from purified nitrogenase. The aqueous supernatant from the denaturation also yields bacterioferritin, but with a lower iron content than that from the direct crystallization method.     

Accumulation of 99Mo-containing iron-molybdenum cofactor precursors of nitrogenase on NifNE,NifH, and NifX of Azotobacter vinelandii

The biosynthesis of the iron-molybdenum cofactor (FeMo-co) of nitrogenase was investigated using the purified in vitro FeMo-co synthesis system and 99Mo. The purified system involves the addition of all components that are known to be required for FeMo-co synthesis in their purified forms. Here, we report the accumulation of a 99Mo-containing FeMo-co precursor on NifNE. Apart from NifNE, NifH and NifX also accumulate 99Mo label. We present evidence that suggests NifH may serve as the entry point for molybdenum incorporation into the FeMo-co biosynthetic pathway. We also present evidence suggesting a role for NifX in specifying the organic acid moiety of FeMo-co.     

Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry

Recent years have witnessed major upheavals in views about early eukaryotic evolution. One very significant finding was that mitochondria, including hydrogenosomes and the newly discovered mitosomes, are just as ubiquitous and defining among eukaryotes as the nucleus itself. A second important advance concerns the readjustment, still in progress, about phylogenetic relationships among eukaryotic groups and the roughly six new eukaryotic supergroups that are currently at the focus of much attention. From the standpoint of energy metabolism (the biochemical means through which eukaryotes gain their ATP, thereby enabling any and all evolution of other traits), understanding of mitochondria among eukaryotic anaerobes has improved. The mainstream formulations of endosymbiotic theory did not predict the ubiquity of mitochondria among anaerobic eukaryotes, while an alternative hypothesis that specifically addressed the evolutionary origin of energy metabolism among eukaryotic anaerobes did. Those developments in biology have been paralleled by a similar upheaval in the Earth sciences regarding views about the prevalence of oxygen in the oceans during the Proterozoic (the time from ca 2.5 to 0.6 Ga ago). The new model of Proterozoic ocean chemistry indicates that the oceans were anoxic and sulphidic during most of the Proterozoic. Its proponents suggest the underlying geochemical mechanism to entail the weathering of continental sulphides by atmospheric oxygen to sulphate, which was carried into the oceans as sulphate, fueling marine sulphate reducers (anaerobic, hydrogen sulphide-producing prokaryotes) on a global scale. Taken together, these two mutually compatible developments in biology and geology underscore the evolutionary significance of oxygen-independent ATP-generating pathways in mitochondria, including those of various metazoan groups, as a watermark of the environments within which eukaryotes arose and diversified into their major lineages.     

Cell biology of molybdenum

The transition element molybdenum (Mo) is of essential importance for (nearly) all biological systems as it is required by enzymes catalyzing diverse key reactions in the global carbon, sulfur and nitrogen metabolism. The metal itself is biologically inactive unless it is complexed by a special cofactor. With the exception of bacterial nitrogenase, where Mo is a constituent of the FeMo-cofactor, Mo is bound to a pterin, thus forming the molybdenum cofactor (Moco) which is the active compound at the catalytic site of all other Mo-enzymes. In eukaryotes, the most prominent Mo-enzymes are (1) sulfite oxidase, which catalyzes the final step in the degradation of sulfur-containing amino acids and is involved in detoxifying excess sulfite, (2) xanthine dehydrogenase, which is involved in purine catabolism and reactive oxygen production, (3) aldehyde oxidase, which oxidizes a variety of aldehydes and is essential for the biosynthesis of the phytohormone abscisic acid, and in autotrophic organisms also (4) nitrate reductase, which catalyzes the key step in inorganic nitrogen assimilation. All Mo-enzymes, except plant sulfite oxidase, need at least one more redox active center, many of them involving iron in electron transfer. The biosynthesis of Moco involves the complex interaction of six proteins and is a process of four steps, which also includes iron as well as copper in an indispensable way. Moco as released after synthesis is likely to be distributed to the apoproteins of Mo-enzymes by putative Moco-carrier proteins. Xanthine dehydrogenase and aldehyde oxidase, but not sulfite oxidase and nitrate reductase, require the post-translational sulfuration of their Mo-site for becoming active. This final maturation step is catalyzed by a Moco-sulfurase enzyme, which mobilizes sulfur from l-cysteine in a pyridoxal phosphate-dependent manner as typical for cysteine desulfurases.