Structural Analysis of Monomeric RNA-Dependent Polymerases Revisited.

In the past few years, our understanding of the RNA virosphere has changed dramatically due to the growth and spurt of metagenomics, exponentially increasing the number of RNA viral sequences, and providing a better understanding of their range of potential hosts. As of today, the only conserved protein among RNA viruses appears to be the monomeric RNA-dependent RNA polymerase. This enzyme belongs to the right-hand DNA-and RNA polymerases, which also includes reverse transcriptases and eukaryotic replicative DNA polymerases. The ubiquity of this protein in RNA viruses makes it a unique evolutionary marker and an appealing broad-spectrum antiviral target. In this work pairwise structural comparisons of viral RdRps and RTs were performed, including tertiary structures that have been obtained in the last few years. The resulting phylogenetic tree shows that the RdRps from (+)ss- and dsRNA viruses might have been recruited several times throughout the evolution of mobile genetic elements. RTs also display multiple evolutionary routes. We have identified a structural core comprising the entire palm, a large moiety of the fingers and the N-terminal helices of the thumb domain, comprising over 300 conserved residues, including two regions that we have named the "knuckles" and the "hypothenar eminence". The conservation of an helix bundle in the region preceding the polymerase domain confirms that (-)ss and dsRNA Reoviruses' polymerases share a recent ancestor. Finally, the inclusion of DNA polymerases into our structural analyses suggests that monomeric RNA-dependent polymerases might have diverged from B-family polymerases.

Alarmones as Vestiges of a Bygone RNA World.

All known alarmones are ribonucleotides or ribonucleotide derivatives that are synthesized when cells are under stress conditions, triggering a stringent response that affects major processes such as replication, gene expression, and metabolism. The ample phylogenetic distribution of alarmones (e.g., cAMP, Ap(n)A, cGMP, AICAR, and ZTP) suggests that they are very ancient molecules that may have already been present in cellular systems prior to the evolutionary divergence of the Archaea, Bacteria, and Eukarya domains. Their chemical structure, wide biological distribution, and functional role in highly conserved cellular processes support the possibility that these modified nucleotides are molecular fossils of an epoch in the evolution of chemical signaling and metabolite sensing during which RNA molecules played a much more conspicuous role in biological catalysis and genetic information.

On the Early Evolution of Catabolic Pathways: A Comparative Genomics Approach. I. The Cases of Glucose, Ribose, and the Nucleobases Catabolic Routes.

Compared with the large corpus of published work devoted to the study of the origin and early development of anabolism, little attention has been given to the discussion of the early evolution of catabolism in spite of its significance. In the present study, we have used comparative genomics to explore the evolution and phylogenetic distribution of the enzymes that catalyze the extant catabolic pathways of the monosaccharides glucose and ribose, as well as those of the nucleobases adenine, guanine, cytosine, uracil, and thymine. Based on the oxygen dependence of the enzymes, their conservation, and evolution, we speculate on the relative antiquity of the pathways. Our results allow us to suggest which catabolic pathways and enzymes may have already been present in the last common ancestor. We conclude that the enzymatic degradations of ribose, as well as those of purines adenine and guanine, are among the most ancient catabolic pathways which can be traced by protein-based methodologies.

Giardia lamblia: Identification of peroxisomal-like proteins.

The protozoan parasite Giardia lamblia has traditionally been reported as lacking peroxisomes, organelles involved in fatty acid metabolism and detoxification of reactive oxygen species. We here report the finding with transmission electron microscopy of an oxidase activity in cytoplasmic vesicles of trophozoites and cysts of G. lamblia. These vesicles were positive to 3,3'-diaminobenzidine and to cerium chloride staining. In addition, using bioinformatic tools, two peroxisomal proteins were identified in the G. lamblia proteome: acyl-CoA synthetase long chain family member 4 (ACSL-4) and peroxin-4 (PEX-4). With confocal and immunoelectron microscopy using polyclonal antibodies both proteins were identified in cytoplasmic vesicles of trophozoites. Altogether, our results suggest for the first time the presence of peroxisomal-like proteins in the cytoplasm of G. lamblia.

Methanogenesis on Early Stages of Life: Ancient but Not Primordial.

Of the six known autotrophic pathways, the Wood-Ljungdahl pathway (WL) is the only one present in both the acetate producing Bacteria (homoacetogens) and the methane producing Archaea (hydrogenotrophic methanogens), and it has been suggested that WL is one of the oldest metabolic pathways. However, only the so-called carbonyl branch is shared by Archaea and Bacteria, while the methyl branch is different, both in the number of reactions and enzymes, which are not homologous among them. In this work we show that some parts of the methyl branch of archaeal Wood-Ljungdahl pathway (MBWL) are present in bacteria as well as in non-methanogen archaea, although the tangled evolutionary history of MBWL cannot be traced back to the Last Common Ancestor. We have also analyzed the different variants of methanogenesis (hydrogenotrophic, acetoclastic and methylotrophic pathways), and concluded that each of these pathways, and every different enzyme or subunit (in the case of multimeric enzymes), has their own intricate evolutionary history. Our study supports the scenario of hydrogenotrophic methanogenesis being older than the other variants, albeit not old enough to be present in the last archaeal common ancestor.

On the origin of mitosing cells: A historical appraisal of Lynn Margulis endosymbiotic theory.

Although for a long-time symbiosis was considered to be quite rare and with no role in evolutionary processes, Lynn Margulis demonstrated that endosymbiotic events played a key role in the origin and evolution of eukaryotic cells. Starting with her seminal assay in the Journal of Theoretical Biology in 1967 (authored as Lynn Sagan), her lifelong work on eukaryogenesis and the role of symbiosis in evolution stands as a valid and authoritative contribution to science. As was quick to acknowledge, she was not the first to discuss the significance of symbiosis to explain the origin of mitochondria and chloroplasts, but no one else had done it to her extent and depth, nor had anyone provided a variety of testable hypotheses. While it is true that some of her proposals were incomplete or mistaken, morphological, biochemical and geochemical evidence together with phylogenomic analyses of mitochondria, chloroplasts and eukaryotic nuclear genomes have demonstrated the validity of her evolutionary scheme, as well that of her specific predictions on the chimeric nature of genomes and the mosaicism of metabolic pathways in eukaryotic cells.

Can an Imidazole Be Formed from an Alanyl-Seryl-Glycine Tripeptide under Possible Prebiotic Conditions?

The five-membered heterocyclic imidazole group, which is an essential component of purines, histidine and many cofactors, has been abiotically synthesized in different model experiments that attempt to simulate the prebiotic environment. The evolutionary significance of imidazoles is highlighted not only by its presence in nucleic acid components and in histidine, but also by experimental reports of its ability to restore the catalytic activity of ribozymes. However, as of today there are no reports of histidine in carbonaceous chondrites, and although the abiotic synthesis of His reported by Shen et al. (1987, 1990a) proceeds via an Amadori rearrangement, like in the biosynthesis of histidine, neither the reactants nor the conditions are truly prebiotic. Based on the autocatalytic biosynthesis of 4-methylidene-imidazole-one (MIO), a cofactor of some members of the amino acid aromatic ammonia-lyases and aminomutases, which occur via the self-condensation of a simple Ala-Ser-Gly motif within the sequence of the enzymes, we propose a possible prebiotic synthesis of an imidazolide.

Alexandr I. Oparin and the Origin of Life: A Historical Reassessment of the Heterotrophic Theory.

The heterotrophic origin of life proposed by A. I. Oparin in the 1920s was part of a Darwinian framework that assumed that living organisms were the historical outcome of a gradual transformation of lifeless matter. Eighty years ago, he presented a much more detailed scheme of the processes that may have led to life. As argued here, the development of the heterotrophic theory has been shaped by an entangled scenario in which a number of technical and scientific developments concur, as well as non-scientific issues including the Stalinist period and the tensions of the Cold War atmosphere. What has been largely ignored until now is the key role played by Haeckel's ideas in shaping Oparin's theory. The heterotrophic theory has been erroneously described as a metabolism-first hypothesis in which genetic material was not included due to ideological pressures of the Soviet government. As shown here, both characterizations are mistaken. The development of Oparin's views and the ensuing debates cannot be understood without considering the confrontation between Mendelism and Darwinism during the first three decades of the past century, combined with the doubts surrounding the existence of genes.

On the lack of evolutionary continuity between prebiotic peptides and extant enzymes.

The significance of experiments that claim to simulate the properties of prebiotic small peptides and polypeptides as models of the polymers that may have preceded proteins is critically addressed. As discussed here, most of these experiments are based only on a small number of a larger set of amino acids that may have been present in the prebiotic environment, supported by both experimental simulations and the repertoire of organic compounds reported in carbonaceous chondrites. Model experiments with small peptides may offer some insights into the processes that contributed to generate the chemical environment leading to the emergence of informational oligomers, but not to the origin of proteins. The large body of circumstantial evidence indicating that catalytic RNA played a key role in the origin of protein synthesis during the early stages of cellular evolution implies that the emergence of the genetic code and of protein biosynthesis are no longer synonymous with the origin of life. Hence, reports on the abiotic synthesis of small catalytic peptides under potential prebiotic conditions do not provide information on the origin of triplet encoded protein biosynthesis, but in some cases may serve as models to understand the properties of the earliest proteins.

Primordial synthesis of amines and amino acids in a 1958 Miller H2S-rich spark discharge experiment.

Archived samples from a previously unreported 1958 Stanley Miller electric discharge experiment containing hydrogen sulfide (H(2)S) were recently discovered and analyzed using high-performance liquid chromatography and time-of-flight mass spectrometry. We report here the detection and quantification of primary amine-containing compounds in the original sample residues, which were produced via spark discharge using a gaseous mixture of H(2)S, CH(4), NH(3), and CO(2). A total of 23 amino acids and 4 amines, including 7 organosulfur compounds, were detected in these samples. The major amino acids with chiral centers are racemic within the accuracy of the measurements, indicating that they are not contaminants introduced during sample storage. This experiment marks the first synthesis of sulfur amino acids from spark discharge experiments designed to imitate primordial environments. The relative yield of some amino acids, in particular the isomers of aminobutyric acid, are the highest ever found in a spark discharge experiment. The simulated primordial conditions used by Miller may serve as a model for early volcanic plume chemistry and provide insight to the possible roles such plumes may have played in abiotic organic synthesis. Additionally, the overall abundances of the synthesized amino acids in the presence of H(2)S are very similar to the abundances found in some carbonaceous meteorites, suggesting that H(2)S may have played an important role in prebiotic reactions in early solar system environments.

Low complexity regions (LCRs) contribute to the hypervariability of the HIV-1 gp120 protein.

Low complexity regions (LCRs) are sequences of nucleic acids or proteins defined by a compositional bias. Their occurrence has been confirmed in sequences of the three cellular lineages (Bacteria, Archaea and Eucarya), and has also been reported in viral genomes. We present here the results of a detailed computer analysis of the LCRs present in the HIV-1 glycoprotein 120 (gp120) encoded by the viral gene env. The analysis was performed using a sample of 3637 Env polyprotein sequences derived from 4117 completely sequenced and translated HIV-1 genomes available in public databases as of December 2012. We have identified 1229 LCRs located in four different regions of the gp120 protein that correspond to four of the five regions that have been identified as hypervariable (V1, V2, V4 and V5). The remaining 29 LCRs are found in the signal peptide and in the conserved regions C2, C3, C4 and C5. No LCR has been identified in the hypervariable region V3. The LCRs detected in the V1, V2, V4, and V5 hypervariable regions exhibit a high Asn content in their amino acid composition, which very likely correspond to glycosylation sites, which may contribute to the retroviral ability to avoid the immune system. In sharp contrast with what is observed in gp120 proteins lacking LCRs, the glycosylation sites present in LCRs tend to be clustered towards the center of the region forming well-defined islands. The results presented here suggest that LCRs represent a hitherto undescribed source of genomic variability in lentivirus, and that these repeats may represent an important source of antigenic variation in HIV-1 populations. The results reported here may exemplify the evolutionary processes that may have increased the size of primitive cellular RNA genomes and the role of LCRs as a source of raw material during the processes of evolutionary acquisition of new functions.

Norvaline and norleucine may have been more abundant protein components during early stages of cell evolution.

The absence of the hydrophobic norvaline and norleucine in the inventory of protein amino acids is readdressed. The well-documented intracellular accumulation of these two amino acids results from the low-substrate specificity of the branched-chain amino acid biosynthetic enzymes that act over a number of related α-ketoacids. The lack of absolute substrate specificity of leucyl-tRNA synthase leads to a mischarged norvalyl-tRNA(Leu) that evades the translational proofreading activities and produces norvaline-containing proteins, (cf. Apostol et al. J Biol Chem 272:28980-28988, 1997). A similar situation explains the presence of minute but detectable amounts of norleucine in place of methionine. Since with few exceptions both leucine and methionine are rarely found in the catalytic sites of most enzymes, their substitution by norvaline and norleucine, respectively, would have not been strongly hindered in small structurally simple catalytic polypeptides during the early stages of biological evolution. The report that down-shifts of free oxygen lead to high levels of intracellular accumulation of pyruvate and the subsequent biosynthesis of norvaline (Soini et al. Microb Cell Factories 7:30, 2008) demonstrates the biochemical and metabolic consequences of the development of a highly oxidizing environment. The results discussed here also suggest that a broader definition of biomarkers in the search for extraterrestrial life may be required.

Comparing the evolutionary dynamics of predominant SARS-CoV-2 virus lineages co-circulating in Mexico.

Over 200 different SARS-CoV-2 lineages have been observed in Mexico by November 2021. To investigate lineage replacement dynamics, we applied a phylodynamic approach and explored the evolutionary trajectories of five dominant lineages that circulated during the first year of local transmission. For most lineages, peaks in sampling frequencies coincided with different epidemiological waves of infection in Mexico. Lineages B.1.1.222 and B.1.1.519 exhibited similar dynamics, constituting clades that likely originated in Mexico and persisted for >12 months. Lineages B.1.1.7, P.1 and B.1.617.2 also displayed similar dynamics, characterized by multiple introduction events leading to a few successful extended local transmission chains that persisted for several months. For the largest B.1.617.2 clades, we further explored viral lineage movements across Mexico. Many clades were located within the south region of the country, suggesting that this area played a key role in the spread of SARS-CoV-2 in Mexico.

Subtle structural differences of nucleotide analogs may impact SARS-CoV-2 RNA-dependent RNA polymerase and exoribonuclease activity.

The rapid spread and public health impact of the novel SARS-CoV-2 variants that cause COVID-19 continue to produce major global impacts and social distress. Several vaccines were developed in record time to prevent and limit the spread of the infection, thus playing a pivotal role in controlling the pandemic. Although the repurposing of available drugs attempts to provide therapies of immediate access against COVID-19, there is still a need for developing specific treatments for this disease. Remdesivir, molnupiravir and Paxlovid remain the only evidence-supported antiviral drugs to treat COVID-19 patients, and only in severe cases. To contribute on the search of potential Covid-19 therapeutic agents, we targeted the viral RNA-dependent RNA polymerase (RdRp) and the exoribonuclease (ExoN) following two strategies. First, we modeled and analyzed nucleoside analogs sofosbuvir, remdesivir, favipiravir, ribavirin, and molnupiravir at three key binding sites on the RdRp-ExoN complex. Second, we curated and virtually screened a database containing 517 nucleotide analogs in the same binding sites. Finally, we characterized key interactions and pharmacophoric features presumably involved in viral replication halting at multiple sites. Our results highlight structural modifications that might lead to more potent SARS-CoV-2 inhibitors against an expansive range of variants and provide a collection of nucleotide analogs useful for screening campaigns.

Two short low complexity regions (LCRs) are hallmark sequences of the Delta SARS-CoV-2 variant spike protein.

Low complexity regions (LCRs) are protein sequences formed by a set of compositionally biased residues. LCRs are extremely abundant in cellular proteins and have also been reported in viruses, where they may partake in evasion of the host immune system. Analyses of 28,231 SARS-CoV-2 whole proteomes and of 261,051 spike protein sequences revealed the presence of four extremely conserved LCRs in the spike protein of several SARS-CoV-2 variants. With the exception of Iota, where it is absent, the Spike LCR-1 is present in the signal peptide of 80.57% of the Delta variant sequences, and in other variants of concern and interest. The Spike LCR-2 is highly prevalent (79.87%) in Iota. Two distinctive LCRs are present in the Delta spike protein. The Delta Spike LCR-3 is present in 99.19% of the analyzed sequences, and the Delta Spike LCR-4 in 98.3% of the same set of proteins. These two LCRs are located in the furin cleavage site and HR1 domain, respectively, and may be considered hallmark traits of the Delta variant. The presence of the medically-important point mutations P681R and D950N in these LCRs, combined with the ubiquity of these regions in the highly contagious Delta variant opens the possibility that they may play a role in its rapid spread.

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.

Enhanced synthesis of alkyl amino acids in Miller's 1958 H2S experiment.

Stanley Miller's 1958 H(2)S-containing experiment, which included a simulated prebiotic atmosphere of methane (CH(4)), ammonia (NH(3)), carbon dioxide (CO(2)), and hydrogen sulfide (H(2)S) produced several alkyl amino acids, including the α-, ß-, and γ-isomers of aminobutyric acid (ABA) in greater relative yields than had previously been reported from his spark discharge experiments. In the presence of H(2)S, aspartic and glutamic acids could yield alkyl amino acids via the formation of thioimide intermediates. Radical chemistry initiated by passing H(2)S through a spark discharge could have also enhanced alkyl amino acid synthesis by generating alkyl radicals that can help form the aldehyde and ketone precursors to these amino acids. We propose mechanisms that may have influenced the synthesis of certain amino acids in localized environments rich in H(2)S and lightning discharges, similar to conditions near volcanic systems on the early Earth, thus contributing to the prebiotic chemical inventory of the primordial Earth.

Prebiotic synthesis of methionine and other sulfur-containing organic compounds on the primitive Earth: a contemporary reassessment based on an unpublished 1958 Stanley Miller experiment.

Original extracts from an unpublished 1958 experiment conducted by the late Stanley L. Miller were recently found and analyzed using modern state-of-the-art analytical methods. The extracts were produced by the action of an electric discharge on a mixture of methane (CH(4)), hydrogen sulfide (H(2)S), ammonia (NH(3)), and carbon dioxide (CO(2)). Racemic methionine was formed in significant yields, together with other sulfur-bearing organic compounds. The formation of methionine and other compounds from a model prebiotic atmosphere that contained H(2)S suggests that this type of synthesis is robust under reducing conditions, which may have existed either in the global primitive atmosphere or in localized volcanic environments on the early Earth. The presence of a wide array of sulfur-containing organic compounds produced by the decomposition of methionine and cysteine indicates that in addition to abiotic synthetic processes, degradation of organic compounds on the primordial Earth could have been important in diversifying the inventory of molecules of biochemical significance not readily formed from other abiotic reactions, or derived from extraterrestrial delivery.