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Methane (CH 4 ), the most abundant hydrocarbon in the atmosphere, originates largely from biogenic sources 1 linked to an increasing number of organisms occurring in oxic and anoxic environments. Traditionally, biogenic CH 4 has been regarded as the final product of anoxic decomposition of organic matter by methanogenic archaea. However, plants 2 , 3 , fungi 4 , algae 5 and cyanobacteria 6 can produce CH 4 in the presence of oxygen. Although methanogens are known to produce CH 4 enzymatically during anaerobic energy metabolism 7 , the requirements and pathways for CH 4 production by non-methanogenic cells are poorly understood. Here, we demonstrate that CH 4 formation by Bacillus subtilis and Escherichia coli is triggered by free iron and reactive oxygen species (ROS), which are generated by metabolic activity and enhanced by oxidative stress. ROS-induced methyl radicals, which are derived from organic compounds containing sulfur- or nitrogen-bonded methyl groups, are key intermediates that ultimately lead to CH 4 production. We further show CH 4 production by many other model organisms from the Bacteria, Archaea and Eukarya domains, including in several human cell lines. All these organisms respond to inducers of oxidative stress by enhanced CH 4 formation. Our results imply that all living cells probably possess a common mechanism of CH 4 formation that is based on interactions among ROS, iron and methyl donors, opening new perspectives for understanding biochemical CH 4 formation and cycling. Methane formation by a ROS-mediated process is linked to metabolic activity and is identified as a conserved feature across living systems.

Methane is a potent greenhouse gas, which likely enabled the evolution of life by keeping the early Earth warm. Here, we demonstrate routes towards abiotic methane and ethane formation under early-earth conditions from methylated sulfur and nitrogen compounds with prebiotic origin. These compounds are demethylated in Fenton reactions governed by ferrous iron and reactive oxygen species (ROS) produced by light and heat in aqueous environments. After the emergence of life, this phenomenon would have greatly intensified in the anoxic Archean by providing methylated sulfur and nitrogen substrates. This ROS-driven Fenton chemistry can occur delocalized from serpentinization across Earth’s humid realm and thereby substantially differs from previously suggested methane formation routes that are spatially restricted. Here, we report that Fenton reactions driven by light and heat release methane and ethane and might have shaped the chemical evolution of the atmosphere prior to the origin of life and beyond. Abiotic methane and ethane formation routes in aqueous environments driven by light and heat are identified. The released hydrocarbons may have contributed to the chemical evolution of the atmosphere from prior to the origin of life until today.

Ethylene glycol is a monomer of the plastic polyethylene terephthalate (PET) and an environmental pollutant of increasing concern. Although it is generally accepted that bacteria use ethylene glycol as growth substrate, not all involved enzymes are well understood. Here, we show that Paracoccus denitrificans assimilates ethylene glycol solely via NAD-dependent alcohol and aldehyde dehydrogenases. Using comparative proteomics, we identify a gene cluster that is strongly expressed in the presence of ethylene glycol. We report the functional and structural characterization of EtgB and EtgA, key enzymes encoded by this etg gene cluster. We furthermore show that the transcriptional activator EtgR controls expression of the gene cluster. Adaptive laboratory evolution on ethylene glycol results in faster growth, enabled by increased production of EtgB and EtgA. Bioinformatic analysis reveals that the etg gene cluster is widely distributed among bacteria, suggesting a common role of NAD-dependent dehydrogenases in microbial ethylene glycol assimilation. Ethylene glycol is a monomer of the ubiquitous plastic polyethylene terephthalate (PET). Here, the authors report the discovery of NAD-dependent alcohol and aldehyde dehydrogenases in the soil bacterium Paracoccus denitrificans for ethylene glycol catabolism.

The iron protein components of bacterial nitrogenases are capable of reducing carbon dioxide (CO 2 ) to carbon monoxide (CO) in the absence of their catalytic partners, mimicking the activity of CO dehydrogenase. The iron (Fe) proteins of molybdenum (Mo) and vanadium (V) nitrogenases mimic carbon monoxide (CO) dehydrogenase in catalyzing the interconversion between CO 2 and CO under ambient conditions. Catalytic reduction of CO 2 to CO is achieved in vitro and in vivo upon redox changes of the Fe-protein-associated [Fe 4 S 4 ] clusters. These observations establish the Fe protein as a model for investigation of CO 2 activation while suggesting its biotechnological adaptability for recycling the greenhouse gas into useful products.

The vanadium (V)-nitrogenase of Azotobacter vinelandii catalyses the in vitro conversion of carbon monoxide (CO) to hydrocarbons. Here we show that an A. vinelandii strain expressing the V-nitrogenase is capable of in vivo reduction of CO to ethylene (C 2 H 4 ), ethane (C 2 H 6 ) and propane (C 3 H 8 ). Moreover, we demonstrate that CO is not used as a carbon source for cell growth, being instead reduced to hydrocarbons in a secondary metabolic pathway. These findings suggest a possible role of the ancient nitrogenase as an evolutionary link between the carbon and nitrogen cycles on Earth and establish a solid foundation for biotechnological adaptation of a whole-cell approach to recycling carbon wastes into hydrocarbon products. Thus, this study has several repercussions for evolution-, environment- and energy-related areas. Nitrogenases reduce inorganic nitrogen to organic ammonia in a crucial step of the nitrogen cycle. Here the authors show that the vanadium-nitrogenase of Azotobacter vinelandii can also catalyse the in vivo conversion of carbon monoxide to hydrocarbons in a secondary non-biosynthetic pathway.

Nitrogenases are essential for biological nitrogen fixation, converting atmospheric nitrogen gas to bioavailable ammonia. The production of ammonia by diazotrophic organisms, harboring nitrogenases, is essential for sustaining plant growth. Hence, there is a large scientific interest in understanding the cellular mechanisms for nitrogen fixation via nitrogenases. Nitrogenases rely on highly reduced electrons to power catalysis, although we lack knowledge as to which proteins shuttle the electrons to nitrogenases within cells. Here, we characterized the electron transport to the iron (Fe)-nitrogenase in the model diazotroph Rhodobacter capsulatus , showing that two distinct ferredoxins are very important for nitrogen fixation despite having different redox centers. In addition, our research expands upon the debate on whether ferredoxins have functional redundancy or perform distinct roles within cells. Here, we observe that both essential ferredoxins likely have distinct roles based on differential proteome shifts of deletion strains and different complementation behaviors.

NifEN is a biosynthetic scaffold for the cofactor of Mo-nitrogenase (designated the M-cluster). Previous studies have revealed the sequence and structural homology between NifEN and NifDK, the catalytic component of nitrogenase. However, direct proof for the functional homology between the two proteins has remained elusive. Here we show that, upon maturation of a cofactor precursor (designated the L-cluster) on NifEN, the cluster species extracted from NifEN is spectroscopically equivalent and functionally interchangeable with the native M-cluster extracted from NifDK. Both extracted clusters display nearly indistinguishable EPR features, X-ray absorption spectroscopy/extended X-ray absorption fine structure (XAS/EXAFS) spectra and reconstitution activities, firmly establishing the M-cluster–bound NifEN (designated NifENM) as the only protein other than NifDK to house the unique nitrogenase cofactor. Iron chelation experiments demonstrate a relocation of the cluster from the surface to its binding site within NifENM upon maturation, which parallels the insertion of M-cluster into an analogous binding site in NifDK, whereas metal analyses suggest an asymmetric conformation of NifENM with an M-cluster in one αβ-half and an empty cluster-binding site in the other αβ-half, which led to the proposal of a stepwise assembly mechanism of the M-cluster in the two αβ-dimers of NifEN. Perhaps most importantly, NifENM displays comparable ATP-independent substrate-reducing profiles to those of NifDK, which establishes the M-cluster–bound αβ-dimer of NifENM as a structural and functional mimic of one catalytic αβ-half of NifDK while suggesting the potential of this protein as a useful tool for further investigations of the mechanistic details of nitrogenase.

The Mo- and V-nitrogenases are two homologous members of the nitrogenase family that are distinguished mainly by the presence of different heterometals (Mo or V) at their respective cofactor sites (M- or V-cluster). However, the V-nitrogenase is ~600-fold more active than its Mo counterpart in reducing CO to hydrocarbons at ambient conditions. Here, we expressed an M-cluster-containing, hybrid V-nitrogenase in Azotobacter vinelandii and compared it to its native, V-cluster-containing counterpart in order to assess the impact of protein scaffold and cofactor species on the differential reactivities of Mo- and V-nitrogenases toward CO. Housed in the VFe protein component of V-nitrogenase, the M-cluster displayed electron paramagnetic resonance (EPR) features similar to those of the V-cluster and demonstrated an ~100-fold increase in hydrocarbon formation activity from CO reduction, suggesting a significant impact of protein environment on the overall CO-reducing activity of nitrogenase. On the other hand, the M-cluster was still ~6-fold less active than the V-cluster in the same protein scaffold, and it retained its inability to form detectable amounts of methane from CO reduction, illustrating a fine-tuning effect of the cofactor properties on this nitrogenase-catalyzed reaction. Together, these results provided important insights into the two major determinants for the enzymatic activity of CO reduction while establishing a useful framework for further elucidation of the essential catalytic elements for the CO reactivity of nitrogenase. IMPORTANCE This is the first report on the in vivo generation and in vitro characterization of an M-cluster-containing V-nitrogenase hybrid. The “normalization” of the protein scaffold to that of the V-nitrogenase permits a direct comparison between the cofactor species of the Mo- and V-nitrogenases (M- and V-clusters) in CO reduction, whereas the discrepancy between the protein scaffolds of the Mo- and V-nitrogenases (MoFe and VFe proteins) housing the same cofactor (M-cluster) allows for an effective assessment of the impact of the protein environment on the CO reactivity of nitrogenase. The results of this study provide a first look into the “weighted” contributions of protein environment and cofactor properties to the overall activity of CO reduction; more importantly, they establish a useful platform for further investigation of the structural elements attributing to the CO-reducing activity of nitrogenase. This is the first report on the in vivo generation and in vitro characterization of an M-cluster-containing V-nitrogenase hybrid. The “normalization” of the protein scaffold to that of the V-nitrogenase permits a direct comparison between the cofactor species of the Mo- and V-nitrogenases (M- and V-clusters) in CO reduction, whereas the discrepancy between the protein scaffolds of the Mo- and V-nitrogenases (MoFe and VFe proteins) housing the same cofactor (M-cluster) allows for an effective assessment of the impact of the protein environment on the CO reactivity of nitrogenase. The results of this study provide a first look into the “weighted” contributions of protein environment and cofactor properties to the overall activity of CO reduction; more importantly, they establish a useful platform for further investigation of the structural elements attributing to the CO-reducing activity of nitrogenase.

NifB, a radical SAM enzyme, catalyzes the biosynthesis of the L cluster (Fe8S9C), a structural homolog and precursor to the nitrogenase active-site M cluster ([MoFe7S9C·R-homocitrate]). Sequence analysis shows that NifB contains the CxxCxxxC motif that is typically associated with the radical SAM cluster ([Fe4S4]SAM) involved in the binding of S-adenosylmethionine (SAM). In addition, NifB houses two transient [Fe4S4] clusters (K cluster) that can be fused into an 8Fe L cluster concomitant with the incorporation of an interstitial carbide ion, which is achieved through radical SAM chemistry initiated at the [Fe4S4]SAM cluster upon its interaction with SAM. Here, we report a VTVH MCD/EPR spectroscopic study of the L cluster biosynthesis on NifB, which focuses on the initial interaction of SAM with [Fe4S4]SAM in a variant NifB protein (MaNifBSAM) containing only the [Fe4S4]SAM cluster and no K cluster. Titration of MaNifBSAM with SAM reveals that [Fe4S4]SAM exists in two forms, labeled Fe4S4SAMA+ and Fe4S4SAMB2+ . It is proposed that these forms are involved in the synthesis of the L cluster. Of the two cluster types, only Fe4S4SAMB2+ initially interacts with SAM, resulting in the generation of Z, an S = ½ paramagnetic [Fe4S4]SAM/SAM complex.Graphic abstract

Nitrogenases are best known for catalyzing the reduction of dinitrogen to ammonia at a complex metallic cofactor. Recently, nitrogenases were shown to reduce carbon dioxide (CO 2 ) and carbon monoxide to hydrocarbons, offering a pathway to recycle carbon waste into hydrocarbon products. Among the three nitrogenase isozymes, the iron nitrogenase has the highest wild-type activity for the reduction of CO 2 , but the molecular architecture facilitating these activities has remained unknown. Here, we report a 2.35-Å cryogenic electron microscopy structure of the ADP·AlF 3 -stabilized iron nitrogenase complex from Rhodobacter capsulatus , revealing an [Fe 8 S 9 C - ( R )-homocitrate] cluster in the active site. The enzyme complex suggests that the iron nitrogenase G subunit is involved in cluster stabilization and substrate channeling and confers specificity between nitrogenase reductase and catalytic component proteins. Moreover, the structure highlights a different interface between the two catalytic halves of the iron and the molybdenum nitrogenase, potentially influencing the intrasubunit ‘communication’ and thus the nitrogenase mechanism. Using cryo-EM, Schmidt, Schulz, et al. solve the structure of the iron nitrogenase complex, which shows a unique architecture of alternative nitrogenases and suggests the G subunit to be involved in substrate channeling, stabilization of the cofactor and determining specificty among nitrogenase components.