Primitive purine biosynthesis connects ancient geochemistry to modern metabolism.

An unresolved question in the origin and evolution of life is whether a continuous path from geochemical precursors to the majority of molecules in the biosphere can be reconstructed from modern-day biochemistry. Here we identified a feasible path by simulating the evolution of biosphere-scale metabolism, using only known biochemical reactions and models of primitive coenzymes. We find that purine synthesis constitutes a bottleneck for metabolic expansion, which can be alleviated by non-autocatalytic phosphoryl coupling agents. Early phases of the expansion are enriched with enzymes that are metal dependent and structurally symmetric, supporting models of early biochemical evolution. This expansion trajectory suggests distinct hypotheses regarding the tempo, mode and timing of metabolic pathway evolution, including a late appearance of methane metabolisms and oxygenic photosynthesis consistent with the geochemical record. The concordance between biological and geological analyses suggests that this trajectory provides a plausible evolutionary history for the vast majority of core biochemistry.

The methanogen core and pangenome: conservation and variability across biology's growth temperature extremes.

Temperature is a key variable in biological processes. However, a complete understanding of biological temperature adaptation is lacking, in part because of the unique constraints among different evolutionary lineages and physiological groups. Here we compared the genomes of cultivated psychrotolerant and thermotolerant methanogens, which are physiologically related and span growth temperatures from -2.5°C to 122°C. Despite being phylogenetically distributed amongst three phyla in the archaea, the genomic core of cultivated methanogens comprises about one-third of a given genome, while the genome fraction shared by any two organisms decreases with increasing phylogenetic distance between them. Increased methanogenic growth temperature is associated with reduced genome size, and thermotolerant organisms-which are distributed across the archaeal tree-have larger core genome fractions, suggesting that genome size is governed by temperature rather than phylogeny. Thermotolerant methanogens are enriched in metal and other transporters, and psychrotolerant methanogens are enriched in proteins related to structure and motility. Observed amino acid compositional differences between temperature groups include proteome charge, polarity and unfolding entropy. Our results suggest that in the methanogens, shared physiology maintains a large, conserved genomic core even across large phylogenetic distances and biology's temperature extremes.

Scaling of Protein Function across the Tree of Life.

Scaling laws are a powerful way to compare genomes because they put all organisms onto a single curve and reveal nontrivial generalities as genomes change in size. The abundance of functional categories across genomes has previously been found to show power law scaling with respect to the total number of functional categories, suggesting that universal constraints shape genomic category abundance. Here, we look across the tree of life to understand how genome evolution may be related to functional scaling. We revisit previous observations of functional genome scaling with an expanded taxonomy by analyzing 3,726 bacterial, 220 archaeal, and 79 unicellular eukaryotic genomes. We find that for some functional classes, scaling is best described by multiple exponents, revealing previously unobserved shifts in scaling as genome-encoded protein annotations increase or decrease. Furthermore, we find that scaling varies between phyletic groups at both the domain and phyla levels and is less universal than previously thought. This variability in functional scaling is not related to taxonomic phylogeny resolved at the phyla level, suggesting that differences in cell plan or physiology outweigh broad patterns of taxonomic evolution. Since genomes are maintained and replicated by the functional proteins encoded by them, these results point to functional degeneracy between taxonomic groups and unique evolutionary trajectories toward these. We also find that individual phyla frequently span scaling exponents of functional classes, revealing that individual clades can move across scaling exponents. Together, our results reveal unique shifts in functions across the tree of life and highlight that as genomes grow or shrink, proteins of various functions may be added or lost.

One-Pot De Novo Synthesis of [4Fe-4S] Proteins Using a Recombinant SUF System under Aerobic Conditions.

Fe-S clusters are essential cofactors mediating electron transfer in respiratory and metabolic networks. However, obtaining active [4Fe-4S] proteins with heterologous expression is challenging due to (i) the requirements for [4Fe-4S] cluster assembly, (ii) the O2 lability of [4Fe-4S] clusters, and (iii) copurification of undesired proteins (e.g., ferredoxins). Here, we established a facile and efficient protocol to express mature [4Fe-4S] proteins in the PURE system under aerobic conditions. An enzyme aconitase and thermophilic ferredoxin were selected as model [4Fe-4S] proteins for functional verification. We first reconstituted the SUF system in vitro via a stepwise manner using the recombinant SUF subunits (SufABCDSE) individually purified from E. coli. Later, the incorporation of recombinant SUF helper proteins into the PURE system enabled mRNA translation-coupled [4Fe-4S] cluster assembly under the O2-depleted conditions. To overcome the O2 lability of [4Fe-4S] Fe-S clusters, an O2-scavenging enzyme cascade was incorporated, which begins with formate oxidation by formate dehydrogenase for NADH regeneration. Later, NADH is consumed by flavin reductase for FADH2 regeneration. Finally, bifunctional flavin reductase, along with catalase, removes O2 from the reaction while supplying FADH2 to the SufBC2D complex. These amendments enabled a one-pot, two-step synthesis of mature [4Fe-4S] proteins under aerobic conditions, yielding holo-aconitase with a maximum concentration of ∼0.15 mg/mL. This renovated system greatly expands the potential of the PURE system, paving the way for the future reconstruction of redox-active synthetic cells and enhanced cell-free biocatalysis.

Alternating co-synthesis of glycol nucleic acid (GNA) monomers with dicarboxylic acids via drying.

We report the co-polymerization of glycol nucleic acid (GNA) monomers with unsubstituted and substituted dicarboxylic acid linkers under plausible early Earth aqueous dry-down conditions. Both linear and branched co-polymers are produced. Mechanistic aspects of the reaction and potential roles of these polymers in prebiotic chemistry are discussed.

An evolutionary history of the CoA-binding protein Nat/Ivy.

Nat/Ivy is a diverse and ubiquitous CoA-binding evolutionary lineage that catalyzes acyltransferase reactions, primarily converting thioesters into amides. At the heart of the Nat/Ivy fold is a phosphate-binding loop that bears a striking resemblance to that of P-loop NTPases-both are extended, glycine-rich loops situated between a ß-strand and an α-helix. Nat/Ivy, therefore, represents an intriguing intersection between thioester chemistry, a putative primitive energy currency, and an ancient mode of phospho-ligand binding. Current evidence suggests that Nat/Ivy emerged independently of other cofactor-utilizing enzymes, and that the observed structural similarity-particularly of the cofactor binding site-is the product of shared constraints instead of shared ancestry. The reliance of Nat/Ivy on a ß-α-ß motif for CoA-binding highlights the extent to which this simple structural motif may have been a fundamental evolutionary "nucleus" around which modern cofactor-binding domains condensed, as has been suggested for HUP domains, Rossmanns, and P-loop NTPases. Finally, by dissecting the patterns of conserved interactions between Nat/Ivy families and CoA, the coevolution of the enzyme and the cofactor was analyzed. As with the Rossmann, it appears that the pyrophosphate moiety at the center of the cofactor predates the enzyme, suggesting that Nat/Ivy emerged sometime after the metabolite dephospho-CoA.

A Cristae-Like Microcompartment in Desulfobacterota.

Some Alphaproteobacteria contain intracytoplasmic membranes (ICMs) and proteins homologous to those responsible for the mitochondrial cristae, an observation which has given rise to the hypothesis that the Alphaproteobacteria endosymbiont had already evolved cristae-like structures and functions. However, our knowledge of microbial fine structure is still limited, leaving open the possibility of structurally homologous ICMs outside the Alphaproteobacteria. Here, we report on the detailed characterization of lamellar cristae-like ICMs in environmental sulfate-reducing Desulfobacterota that form syntrophic partnerships with anaerobic methane-oxidizing (ANME) archaea. These structures are junction-bound to the cytoplasmic membrane and resemble the form seen in the lamellar cristae of opisthokont mitochondria. Extending these observations, we also characterized similar structures in Desulfovibrio carbinolicus, a close relative of the magnetotactic D. magneticus, which does not contain magnetosomes. Despite a remarkable structural similarity, the key proteins involved in cristae formation have not yet been identified in Desulfobacterota, suggesting that an analogous, but not a homologous, protein organization system developed during the evolution of some members of Desulfobacterota. IMPORTANCE Working with anaerobic consortia of methane oxidizing ANME archaea and their sulfate-reducing bacterial partners recovered from deep sea sediments and with the related sulfate-reducing bacterial isolate D. carbinolicus, we discovered that their intracytoplasmic membranes (ICMs) appear remarkably similar to lamellar cristae. Three-dimensional electron microscopy allowed for the novel analysis of the nanoscale attachment of ICMs to the cytoplasmic membrane, and these ICMs are structurally nearly identical to the crista junction architecture seen in metazoan mitochondria. However, the core junction-forming proteins must be different. The outer membrane vesicles were observed to bud from syntrophic Desulfobacterota, and darkly stained granules were prominent in both Desulfobacterota and D. carbinolicus. These findings expand the taxonomic breadth of ICM-producing microorganisms and add to our understanding of three-dimensional microbial fine structure in environmental microorganisms.