The iron-sulphur proteins: Evolution of a ubiquitous protein from model systems to higher organisms

Iron: Life's primeval transition metal

Modern life requires many different metal ions, which enable diverse biochemical functions. It is commonly assumed that metal ions' environmental availabilities controlled the evolution of early life. We argue that evolution can only explore the chemistry that life encounters, and fortuitous chemical interactions between metal ions and biological compounds can only be selected for if they first occur sufficiently frequently. We calculated maximal transition metal ion concentrations in the ancient ocean, determining that the amounts of biologically important transition metal ions were orders of magnitude lower than ferrous iron. Under such conditions, primitive bioligands would predominantly interact with Fe(II). While interactions with other metals in certain environments may have provided evolutionary opportunities, the biochemical capacities of Fe(II), Fe-S clusters, or the plentiful magnesium and calcium could have satisfied all functions needed by early life. Primitive organisms could have used Fe(II) exclusively for their transition metal ion requirements.

Ferredoxins: Functions, Evolution, Potential Applications, and Challenges of Subtype Classification

Ferredoxins are proteins found in all biological kingdoms and are involved in essential biological processes including photosynthesis, lipid metabolism, and biogeochemical cycles. Ferredoxins are classified into different groups based on the iron-sulfur (Fe-S) clusters that they contain. A new subtype classification and nomenclature system, based on the spacing between amino acids in the Fe-S binding motif, has been proposed in order to better understand ferredoxins' biological diversity and evolutionary linkage across different organisms. This new classification system has revealed an unparalleled diversity between ferredoxins and has helped identify evolutionarily linked ferredoxins between species. The current review provides the latest insights into ferredoxin functions and evolution, and the new subtype classification, outlining their potential biotechnological applications and the future challenges in streamlining the process.

Structural insights into 3Fe-4S ferredoxins diversity in M. tuberculosis highlighted by a first redox complex with P450

Ferredoxins are small iron-sulfur proteins and key players in essential metabolic pathways. Among all types, 3Fe-4S ferredoxins are less studied mostly due to anaerobic requirements. Their complexes with cytochrome P450 redox partners have not been structurally characterized. In the present work, we solved the structures of both 3Fe-4S ferredoxins from M. tuberculosis-Fdx alone and the fusion FdxE-CYP143. Our SPR analysis demonstrated a high-affinity binding of FdxE to CYP143. According to SAXS data, the same complex is present in solution. The structure reveals extended multipoint interactions and the shape/charge complementarity of redox partners. Furthermore, FdxE binding induced conformational changes in CYP143 as evident from the solved CYP143 structure alone. The comparison of FdxE-CYP143 and modeled Fdx-CYP51 complexes further revealed the specificity of ferredoxins. Our results illuminate the diversity of electron transfer complexes for the production of different secondary metabolites.

Metalloproteins and the pyrite-based origin of life: a critical assessment

We critically examine the proposal by Wächtershäuser (Prokaryotes 1:275-283, 2006a, Philos Trans R Soc Lond B Biol Sci 361: 787-1808, 2006b) that putative transition metal binding sites in protein components of the translation machinery of hyperthermophiles provide evidence of a direct relationship with the FeS clusters of pyrite and thus indicate an autotrophic origin of life in volcanic environments. Analysis of completely sequenced cellular genomes of Bacteria, Archaea and Eucarya does not support the suggestion by Wächtershäuser (Prokaryotes 1:275-283, 2006a, Philos Trans R Soc Lond B Biol Sci 361: 787-1808, 2006b) that aminoacyl-tRNA synthetases and ribosomal proteins bear sequence signatures typical of strong covalent metal bonding whose absence in mesophilic species reveals a process of adaptation towards less extreme environments.

Serpentinization as a source of energy at the origin of life

For life to have emerged from CO₂, rocks, and water on the early Earth, a sustained source of chemically transducible energy was essential. The serpentinization process is emerging as an increasingly likely source of that energy. Serpentinization of ultramafic crust would have continuously supplied hydrogen, methane, minor formate, and ammonia, as well as calcium and traces of acetate, molybdenum and tungsten, to off-ridge alkaline hydrothermal springs that interfaced with the metal-rich carbonic Hadean Ocean. Silica and bisulfide were also delivered to these springs where cherts and sulfides were intersected by the alkaline solutions. The proton and redox gradients so generated represent a rich source of naturally produced chemiosmotic energy, stemming from geochemistry that merely had to be tapped, rather than induced, by the earliest biochemical systems. Hydrothermal mounds accumulating at similar sites in today's oceans offer conceptual and experimental models for the chemistry germane to the emergence of life, although the ubiquity of microbial communities at such sites in addition to our oxygenated atmosphere preclude an exact analogy.

Carbon Monoxide and Cyanide Ligands in the Active Site of [FeFe]-Hydrogenases

The [FeFe]-hydrogenases, although share common features when compared to other metal containing hydrogenases, clearly have independent evolutionary origins. Examples of [FeFe]-hydrogenases have been characterized in detail by biochemical and spectroscopic approaches and the high resolution structures of two examples have been determined. The active site H-cluster is a complex bridged metal assembly in which a [4Fe-4S] cubane is bridged to a 2Fe subcluster with unique non-protein ligands including carbon monoxide, cyanide, and a five carbon dithiolate. Carbon monoxide and cyanide ligands as a component of a native active metal center is a property unique to the metal containing hydrogenases and there has been considerable attention to the characterization of the H-cluster at the level of electronic structure and mechanism as well as to defining the biological means to synthesize such a unique metal cluster. The chapter describes the structural architecture of [FeFe]-hydrogenases and key spectroscopic observations that have afforded the field with a fundamental basis for understanding the relationship between structure and reactivity of the H-cluster. In addition, the results and ideas concerning the topic of H-cluster biosynthesis as an emerging and fascinating area of research, effectively reinforcing the potential linkage between iron-sulfur biochemistry to the role of iron-sulfur minerals in prebiotic chemistry and the origin of life.

From volcanic origins of chemoautotrophic life to Bacteria, Archaea and Eukarya

The theory of a chemoautotrophic origin of life in a volcanic iron-sulphur world postulates a pioneer organism at sites of reducing volcanic exhalations. The pioneer organism is characterized by a composite structure with an inorganic substructure and an organic superstructure. Within the surfaces of the inorganic substructure iron, cobalt, nickel and other transition metal centres with sulphido, carbonyl and other ligands were catalytically active and promoted the growth of the organic superstructure through carbon fixation, driven by the reducing potential of the volcanic exhalations. This pioneer metabolism was reproductive by an autocatalytic feedback mechanism. Some organic products served as ligands for activating catalytic metal centres whence they arose. The unitary structure-function relationship of the pioneer organism later gave rise to two major strands of evolution: cellularization and emergence of the genetic machinery. This early phase of evolution ended with segregation of the domains Bacteria, Archaea and Eukarya from a rapidly evolving population of pre-cells. Thus, life started with an initial, direct, deterministic chemical mechanism of evolution giving rise to a later, indirect, stochastic, genetic mechanism of evolution and the upward evolution of life by increase of complexity is grounded ultimately in the synthetic redox chemistry of the pioneer organism.

Did membrane electrochemistry precede translation?

The discovery of RNA-based enzymes, such as ribonuclease-P, has stimulated new interest in the idea that catalytic functions of RNA preceded the use of coded enzymes during an era loosely termed 'the RNA world'. This paper examines various lines of evidence which support the idea that electrochemical processes associated with the membrane may have preceded the development of coded protein enzymes and may have provided a basis for the phosphorylation energy of the RNA world.

Early assignments of the genetic code dependent upon protein structure

Orgel (1972) has suggested that polynucleotides with sequences of alternating purine/pyrimidine are likely to have predominated in prebiotic conditions. Therefore, in any early template-directed protein synthesis, the number of available codons would have been limited. However, for any self-organizing system to survive and propagate, some feedback must occur from the products of the synthesis to the control of the synthetic procedure itself; i.e. the protein synthesized should have catalysed some step in the initation of template-directed synthesis. A given protein structure with a characteristic conformation and function would be optimal for the product of such a synthesis, and this in turn would limit the number of nucleotide sequences of those available able to give rise to a functioning synthetic assembly. A possible candidate for such an early polypeptide is the ferredoxin group of proteins and it is shown that with the present-day code the corresponding nucleotides do have a high percentage of alternating purine/pyrimidine sequences. Hence these combined restraints on the primitive synthetic machinery would direct the possible assignments of the genetic code helping to explain its regularity and universality.

Early evolution of cellular electron transport: molecular models for the ferredoxin-rubredoxin-flavodoxin region

Using information from conformation-predicting algorithms and X-ray data, a possible mode of structural evolution from an ancestral molecule of about 28 residues to bacterial ferredoxins and rubredoxins is suggested. The possibility of a further evolutionary pathway leading to flavodoxin-like proteins is also indicated.

Biologically important thiol-disulfide reactions and the role of cyst(e)ine in proteins: an evolutionary perspective

Selected aspects of the reactions of thiols and disulfides are reviewed in an evolutionary context with special emphasis on the implications of the transition from a reducing to an oxidizing atmosphere on the earth. It is argued that thiols were important in prebiotic chemistry and in primitive metabolism but that disulfides, owing to their general instability in a reducing environment, came to be of importance as structural links in proteins only after the transition to an oxidizing atmosphere. The occurrence of glutathione is reviewed and discussed in terms of the role of glutathione in maintaining a reducing intracellular environment. The occurrence of cysteine and cystine in intracellular and extracellular proteins of bacteria and of animals is examined in terms of the redox state of the environment in which the protein functions. Thiol-disulfide changes associated with the dormant state are described and the role of cellular water content in dormancy is discussed. The potential significance of reactions between thiols and products of oxidative metabolism is discussed with special emphasis upon thiol additions to carbonyl and alpha, beta-unsaturated carbonyl groups and their possible role in steroid-receptor interaction.

Structure and function of chloroplast-type ferredoxins

Comparison of various chloroplast-type ferredoxin sequences, chemical and enzymic modifications, reconstitution experiments, and fluorescence measurement of chloroplast-type ferredoxins have led to the following conclusions. 1. Tyrosine, histidine, and tryptophan residues are not directly involved in the oxidation-reduction mechanism of ferredoxins. The four indispensible cysteine residues in spinach ferredoxin which constitutes a part of the iron-sulfur cluster are located at residues 39, 44. 47 and 77. Two out of six cysteine residues in Spirulina ferredoxin could be easily modified with vinylpyridine without the loss of reconstitutive ability i.e. the apoferredoxin could be converted to the holoform by the addition of iron and sulfide. 2. Spinach ferredoxin was digested with carboxypeptidase A and the terminal alanine could be removed without loss of the spectral properties of native ferredoxin. However, the removal of the terminal three residues gave rise to the loss of reconstitutive ability. 3. The amino groups of spinach ferredoxin were modified by acetic anhydride and four residues were acetylated. The acetylated preparation of ferredoxin had an unique spectrum. Upon the addition of high concentration of ions the spectrum of this derivative resembled the spectrum of native ferredoxin. Acetylferredoxin did not combine with ferredoxin-NADP reductase, but upon the addition of moderate concentrations of cations, it did bind to this enzyme.