Enhancement of peptide bond formation by polyribonucleotides on clay surfaces in fluctuating environments

Origins and emergent evolution of life: the colloid microsphere hypothesis revisited

Self-replicating molecules, in particular RNA, have long been assumed as key to origins of life on Earth. This notion, however, is not very secure since the reduction of life's complexity to self-replication alone relies on thermodynamically untenable assumptions. Alternative, earlier hypotheses about peptide-dominated colloid self-assembly should be revived. Such macromolecular conglomerates presumably existed in a dynamic equilibrium between confluent growth in sessile films and microspheres detached in turbulent suspension. The first organic syntheses may have been driven by mineral-assisted photoactivation at terrestrial geothermal fields, allowing photo-dependent heterotrophic origins of life. Inherently endowed with rudimentary catalyst activities, mineral-associated organic microstructures can have evolved adaptively toward cooperative 'protolife' communities, in which 'protoplasmic continuity' was maintained throughout a graded series of 'proto-biofilms', 'protoorganisms' and 'protocells' toward modern life. The proneness of organic microspheres to merge back into the bulk of sessile films by spontaneous fusion can have made large populations promiscuous from the beginning, which was important for the speed of collective evolution early on. In this protein-centered scenario, the emergent coevolution of uncoded peptides, metabolic cofactors and oligoribonucleotides was primarily optimized for system-supporting catalytic capabilities arising from nonribosomal peptide synthesis and nonreplicative ribonucleotide polymerization, which in turn incorporated other reactive micromolecular organics as vitamins and cofactors into composite macromolecular colloid films and microspheres. Template-dependent replication and gene-encoded protein synthesis emerged as secondary means for further optimization of overall efficieny later on. Eventually, Darwinian speciation of cell-like lineages commenced after minimal gene sets had been bundled in transmissible genomes from multigenomic protoorganisms.

Steps towards the formation of a protocell: the possible role of short peptides

The paper deals with molecular self-organization leading to formation of a protocell. Plausible steps towards a protocell include: polymerization of peptides and oligonucleotides on mineral surfaces; coevolution of peptides and oligonucleotides with formation of collectively autocatalytic sets; self-organization of short peptides into vesicles; entrapment of the peptide/oligonucleotide systems in mixed peptide and simple amphiphile membranes; and formation of functioning protocells with metabolism and cell division. The established propensity of short peptides to self-ordering and to formation of vesicles makes this sequence plausible. We further suggest that evolution of a protocell produced cellular ancestors of viruses as well as ancestors of cellular organisms.

Thermosynthesis as energy source for the RNA World: A model for the bioenergetics of the origin of life

The thermosynthesis concept, biological free energy gain from thermal cycling, is combined with the concept of the RNA World. The resulting overall origin of life model suggests new explanations for the emergence of the genetic code and the ribosome. It is proposed that the first protein named pF(1) obtained the energy to support the RNA World by a thermal variation of F(1) ATP synthase's binding change mechanism. It is further proposed that this pF(1) was the single translation product during the emergence of the genetic machinery. During thermal cycling pF(1) condensed many substrates with broad specificity, yielding NTPs and randomly constituted protein and RNA libraries that contained self-replicating RNA. The smallness of pF(1) permitted the emergence of the genetic machinery by selection of RNA that increased the fraction of pF(1)s in the protein library: (1) an amino acids concatenating progenitor of rRNA bound to (2) a chain of 'positional tRNAs' linked by mutual recognition, and yielded a pF(1) (or its main motif); this positional tRNA set gradually evolved to a set of regular tRNAs functioning according to the genetic code, with concomitant emergence of (3) an mRNA coding for pF(1).

Preferential amino acid sequences in alumina-catalyzed peptide bond formation

The catalytic effect of activated alumina on amino acid condensation was investigated. The readiness of amino acids to form peptide sequences was estimated on the basis of the yield of dipeptides and was found to decrease in the order glycine (Gly), alanine (Ala), leucine (Leu), valine (Val), proline (Pro). For example, approximately 15% Gly was converted to the dipeptide (Gly(2)), 5% to cyclic anhydride (cyc(Gly(2))) and small amounts of tri- (Gly(3)) and tetrapeptide (Gly(4)) were formed after 28 days. On the other hand, only trace amounts of Pro(2) were formed from proline under the same conditions. Preferential formation of certain sequences was observed in the mixed reaction systems containing two amino acids. For example, almost ten times more Gly-Val than Val-Gly was formed in the Gly+Val reaction system. The preferred sequences can be explained on the basis of an inductive effect that side groups have on the nucleophilicity and electrophilicity, respectively, of the amino and carboxyl groups. A comparison with published data of amino acid reactions in other reaction systems revealed that the main trends of preferential sequence formation were the same as those described for the salt-induced peptide formation (SIPF) reaction. The results of this work and other previously published papers show that alumina and related mineral surfaces might have played a crucial role in the prebiotic formation of the first peptides on the primitive earth.

The effect of smectite composition on the catalysis of peptide bond formation

Clay-catalyzed glycine and diglycine oligomerizations were performed as drying/wetting cycles at 80 degrees C. Two trioctahedral smectites (hectorite and saponite), three pure montmorillonites, a ferruginous smectite, an Fe(II)-rich smectite, and three smectites containing goethite admixture were used as catalysts. Highest peptide bond formation was found with trioctahedral smectites. About 7% of glycine was converted to diglycine and diketopiperazine on hectorite after 7 days. In the case of dioctahedral smectites, highest yields were achieved using clays with a negative-layer charge localized in the octahedral sheets (up to 2% of converted glycine after 7 days). The presence of Fe(II) in clay is reflected in a higher efficiency in catalyzing amino acid dimerization (about 3.5% of converted glycine after 7 days). The possible significance of the results for prebiotic chemistry is discussed.

Investigation on the mechanism of peptide chain prolongation on montmorillonite

Experiments with reduced-charge montmorillonites with gradually collapsed interlayer space prove that peptide formation processes occur mainly at the edges of the clay mineral. Activation of peptides and amino acids and the intermediate formation of cyclic anhydrides are found to be the two dominant processes determining the formation of higher peptides on the mineral surface.

Peptide chain elongation: a possible role of montmorillonite in prebiotic synthesis of protein precursors

Several studies have proven the ability of montmorillonite to catalyse amino acid condensation under assumed prebiotic conditions, simulating wetting-drying cycles. In this work, the oligomerization of short peptides gly2, gly3, gly4 and ala2 on Ca- and Cu-montmorillonite in drying-wetting cycles at 80 degrees C was studied. The catalytic effect of montmorillonite was found to be much higher than in the case of glycine oligomerization. From gly2 after 3 weeks, 10% oligomers (up to gly6, with gly3 as main products) are formed. Gly3 and gly4 give higher oligomers even after 1 cycle. Ala2 produces both ala3 and ala4, whereas ala does not produce any oligomers under these conditions. Heteroologomerization was observed: ala-gly-gly is formed from ala and gly2. Much higher yields are obtained using Ca-montmorillonite, because copper (II) oxidizes organic molecules. The influence of the reaction mechanism on the preferential oligomerization of oligopeptides is discussed.

The evolutionary transition from RNA to DNA in early cells

The evolution of genetic material can be divided into at least three major phases: first, genomes of "nucleic acid-like" molecules; secondly, genomes of RNA; and finally, double-stranded DNA genomes such as those present in all contemporary cells. Using properties of nucleic acid molecules, we attempt to explain the evolutionary transition from RNA alone as a cellular informational macromolecule prior to the evolution of cell systems based on double-stranded DNA. The idea that ribonucleic acid-based cellular genomes preceded DNA is based on the following: (1) protein synthesis can occur in the absence of DNA but not of RNA; (2) RNA molecules have some catalytic properties; (3) the ubiquity of purine and pyridine nucleotide coenzymes as well as other similar ribonucleotide cofactors in metabolic pathways; and (4) the fact that the biosynthesis of deoxyribonucleotides always proceeds via the enzymatic reduction of ribonucleotides. The "RNA prior to DNA" hypothesis can be further developed by understanding the selective pressures that led to the biosynthesis of deoxyribose, thymine, and proofreading DNA polymerases. Taken together these observations suggest to us that DNA was selected as an informational molecule in cells to stabilize earlier RNA-protein replicating systems.(ABSTRACT TRUNCATED AT 250 WORDS)

Stereoselective aminoacylation of a dinucleoside monophosphate by the imidazolides of DL-alanine and N-(tert-butoxycarbonyl)-DL-alanine

The aminoacylation of diinosine monophosphate (IpI) was studied. When the acylating agent was the imidazolide of N-(tert-butoxycarbonyl)-DL-alanine, a 40% enantiomeric excess of the L isomer was incorporated at the internal 2' site and the positions of equilibrium for the 2' in equilibrium with 3' migration reaction differed for the D and L enantiomers. The reactivity of the nucleoside hydroxyl groups decreased in the order 2'(3') greater than internal 2' greater than 5', and the extent of reaction was affected by the concentration of the imidazole buffer (pH 7.1). In contrast, reaction of IpI with the imidazolide of unprotected DL-alanine led to an excess of the D isomer at the internal 2' site, while reaction with the N-carboxy anhydride of DL-alanine proceeded without detectable stereoselection. The relevance of these results to the evolution of optical activity and the origin of genetically directed protein synthesis is discussed.

Acyl silicates and acyl aluminates as activated intermediates in peptide formation on clays

Glycine reacts with heating on dried clays and other minerals to give peptides in much better yield than in the absence of mineral. This reaction was proposed to occur by way of an activated intermediate such as an acyl silicate or acyl aluminate (i.e., the anhydride of a carboxylic acid with Si-OH or Al-OH), analogous to acyl phosphates involved in several biochemical reactions including peptide bond synthesis. We confirmed the proposed mechanism by trapping the intermediate, as well as by direct spectroscopic observation of a related intermediate. The reaction of amino acids on periodically dried mineral surfaces represents a widespread, geologically realistic setting for prebiotic peptide formation via in situ activation.

Theoretical investigation of the role of clay edges in prebiotic peptide bond formation. I. Structures of acetic acid, glycine, H2SO4, H3PO4, Si(OH)4, Al(OH)4-

Activation of amino acids appears to have played a crucial role in prebiotic peptide bond formation. As a model of this process in living systems, phosphates have been used as amino acid activators. The possible role of clay and other minerals has also been investigated. We are presently using ab initio methods to investigate the activation of amino acids by these agents, as an initial step in peptide bond formation. A model of this activation process is described by the reaction: ZCH2COOH + XO4Hn+1 --> ZCH2COOXO3Hn + H2O. The first step in such an investigation, reported here, was to determine the lowest energy structures of a suitable set of reactions. As initial models of amino acids, Z was chosen to be H and NH2, corresponding to acetic acid and glycine, respectively, XO4Hn+1 = H3PO4 represents a phosphate group, while Si(OH)4 describes an edge tetrahedral site of a clay mineral. Al(OH)4- was also included to represent tetrahedral edge site where the silicon is replaced by an aluminum. Finally, to complete the series XO4Hn+1, H2SO4 was added to the set of reactants. All species were optimized using the STO-3G and STO-3G* basis sets. For H3PO4 and Al(OH)4-, STO-3G* full optimizations were not possible. In these cases, certain torsional angles were optimized separately, then held at the optimized value, while the rest of the bond lengths and angles were optimized. All structures were compared to other calculations and to experimental geometries when available.

Protein replication by amino acid pairing

Biological problems concerning the origin of life and the mode of prion replication (Prusiner, 1982) may require protein replication (the synthesis of one protein sequence from another) as part of their solution. It is suggested that complementarity between protein sequences may be determined by amino acid pairing (Root-Bernstein, 1982a). Two mechanisms using the complementarity afforded by amino acid pairing are proposed. Experimental tests of the mechanisms are suggested.

A theory for the origin of a self-replicating chemical system. II. Computer simulation of the autogen

In order to better understand the feasibility and limitations of the autogen (White 1980), a computer simulation based on the fluctuating clay environment was used to test whether autocatalytic growth would occur under various conditions. The results suggest that overall accuracies of replication and translation in the range of 90% and 10%, and protoenzyme turnover numbers of 10--120 monomers/protoenzyme/day are adequate for exponential growth. Nucleation of the components of the autogen from random background oligomers would be extremely rapid if oligomers lengths 2--6 were adequately functional, whereas oligomer lengths much greater than 10 are prohibited. The autogen would most likely nucleate and grow to dominance either rapidly (10--100 cycles of roughly 1 day each) or not at all.

A theory for the origin of a self-replicating chemical system. I: Natural selection of the autogen from short, random oligomers

A theory is described for the origin of a simple chemical system named an autogen, consisting of two short oligonucleotide sequences coding for two simple catalytic peptides. If the theory is valid, under appropriate conditions the autogen would be capable of self-reproduction in a truly genetic process involving both replication and translation. Limited catalytic ability, short oligomer sequences, and low selectivities leading to sloppy information transfer processes are shown to be adequate for the origin of the autogen from random background oligomers. A series of discrete steps, each highly probable if certain minimum requirements and boundary conditions are satisfied, lead to exponential increase in population of all components in the system due to autocatalysis and hypercyclic organization. Nucleation of the components and exponential increase to macroscopic amounts could occur in times on the order of weeks. The feasibility of the theory depends on a number of factors, including the capability of simple protoenzymes to provide moderate enhancements of the accuracies of replication and translation and the likelihood of finding an environment where all of the required processes can occur simultaneously. Regardless of whether or not the specific form proposed for the autogen proves to be feasible, the theory suggests that the first self-replicating chemical systems may have been extremely simple, and that the period of time required for chemical evolution prior to Darwinian natural selection may have been far shorter than generally assumed. Due to the short time required, this theory, unlike others on the origin of genetic processes, is potentially capable of direct experimental verification. A number of prerequisites leading up to such an experiment are suggested, and some have been fulfilled. If successful, such an experiment would be the first laboratory demonstration of the spontaneous emergence by natural selection of a genetic, self-replicating, and evolving molecular system, and might represent the first step in the prebiotic environment of true Darwinian evolution toward a living cell.

A possible role of fluctuating clay-water systems in the production of ordered prebiotic oligomers

A model is proposed for the intermediate stages of prebiotic evolution, based on the characteristics of the adsorption and condensation of amino acids and nucleotides on the surface area of clay minerals in a fluctuating environment. Template replication and translation of adsorbed oligonucleotides and catalytic effects by peptide products on further condensation are proposed, due to specific properties of hypohydrous clay surfaces as well as the biomolecules themselves. Experimental evidence supports some of the proposed interactions, and all of them can be tested experimentally.