Cyanamide mediated syntheses under plausible primitive earth conditions

When an aqueous solution (pH 7.0) of 3H deoxythymidine 5'-triphosphate, deoxythymidine 5'-phosphate, 4-amino-5-imidazolecarboxamide, cyanamide and ammonium chloride was dried and heated at 60 degrees C for 18 h, oligomers were obtained in a yield of approximately 80%. After the chemical degradation of any pyrophosphate bonds present in these oligomers, linear polynucleotides of up to 7-8 units in length were isolated by DEAE cellulose column chromatography and identified by enzymatic digestion procedures. The di- and trinucleotide fractions were degraded 87% and 100% by snake venom phosphodiesterase and 39% and 9% by spleen phosphodiesterase. This synthesis of deoxythymidine oligonucleotides was conducted under potentially prebiotic conditions and may offer a possible method for the synthesis of deoxyoligonucleotides on the primitive Earth.     

Cyanamide mediated syntheses under plausible primitive earth conditions

Summary When an aqueous solution (pH 7.0) of deoxythymidine 5-phosphate, 4-amino-5-imidazolecarboxamide and cyanamide was dried and heated for 18 h at 60°C, P¹, P²-dideoxythymidine 5-pyrophosphate (I) was formed in a 58% yield. Oligonucleotides were not detected in the reaction product. Under conditions employed in the above reaction, (I) was shown to be stable. In prebiotic polymerization reactions employing deoxythymidine 5-triphosphate as the polymerizing species, (I) could therefore function as a primer and minimize the formation of cyclic nucleotides.Abbreviations dT deoxythymidine - dTMP deoxythymidine 5-phosphate - dTppT P¹, P²-dideoxythymidine 5-pyrophosphate - dTTP deoxythymidine 5-triphosphate - AICA 4-amino-5-imidazolecarboxamide     

Cyanamide mediated syntheses under plausible primitive earth conditions

Peptides were formed in yields of 5%, 17% and 66%, respectively, when aqueous solutions of glycine, isoleucine or phenylalanine were dried and heated for 24 h at 90 degrees C with adenosine 5'-triphosphate, 4-amino-5-imidazolecarboxamide and cyanamide. Glycine and L-phenylalanine produced mixtures of di-, tri- and tetrapeptides, while L-isoleucine gave only the dipeptide in detectable quantities. The dipeptides of L-isoleucine and L-phenylalanine were identified by mass spectrometry and enzymatic and enzymatic degradation.     

Cyanamide mediated syntheses under plausible primitive earth conditions

Summary A mixture of ammonium palmitate,¹⁴C-sn-glycero-1(3)-phosphate, cyanimide and imidazole when heated for several hours formed significant quantities of phospholipids. These reaction products were shown by chromatographic, chemical and enzymatic procedures to be monopalmitoylglycerophosphate (MPGP), dipalmitoylglycerophosphate (DPGP) and monopalmitoyl cyclic glycerophosphate (cMPGP). A portion of the MPGP and DPGP possessed the same steric configuration as naturally occurring lysophosphatidic acid and phosphatidic acid. The yield of total phospholipid was maximal at temperatures between 60° and 90° after 8 h. When ratios of reactants were varied, up to 45% of radioactive glycerophosphate was converted into phospholipids. The average proportions of individual phosphatidic acids were: 60% MPGP, 27% DPGP and 13% cMPGP. Evidence was obtained for a synergistic relationship between cyanamide and imidazole in promoting the formation of phosphatidic acids. These results suggest that phosphatidic acids, which are essential precursors for the biochemical synthesis of more complex membrane phospholipids, could have been produced on the primitive Earth.The following abbreviations are employed: for phospholipid standards with designated steric configuration LPA lysophosphatidic acid (1-acyl-sn-glycero-3-phosphate) - PA phosphatidic acid (1, 2-di-acyl-sn-glycero-3-phosphate) - MPGP monopalmitoylglycerophosphate - cMPGP monopalmitoyl cyclic glycerophosphate (1(3)-acyl-sn-glycero-2,3 (1,2)-cyclic phosphate) - DPGP dipalmitoylglycerophosphate - GP glycerophosphate - cGP cyclic glycerophosphate (sn-glycero-2,3 (1,2)-cyclic phosphate) - TLC thin layer chromatographyTo whom reprint requests should be addressed.     

Cyanamide mediated synthesis under plausible primitive earth conditions

Summary The formation of glycerol occurs when a solution of DL-glyceraldehyde is heated in the presence of hydrogen sulfide at room temperature. DL-glyceraldehyde and dihydroxyacetone treated with hydrazine, as well as DL-glyceraldehyde incubated with formaldehyde are also partially converted to glycerol. The yields of the above reactions are from approximately 1% to about 3%. The formation of glycerophosphates occurs when glycerol is heated with ammonium dihydrogen phosphate and either urea or cyanamide. The yield of glycerophosphates is about 30%, most of which issn-glycero-1 (3)-phosphate. These findings indicate that glycerol andsn-glycero-3-phosphate, which are moieties of glycerolipids, could have been formed under conditions which may have prevailed on the primitive Earth.     

Synthesis of putrescine under possible primitive earth conditions

The synthesis of putrescine was accomplished by decarboxylation of L-orithine when this amino acid was heated in aqueous solution and in the absence of oxygen. Chromatographic, radioisotopic, and enzymatic techniques were used to demonstrate that one mole of non-radioactive putrescine and one mole of¹⁴CO₂ was formed during the heating of L-(1-¹⁴C)-ornithine. This work indicates that the synthesis of putrescine can occur starting with ornithine and in conditions that are presumed could have existed on the primitive Earth. The possible significance of these results in the prebiotic molecular evolution is briefly discussed.     

Synthesis of phosphatidylethanolamine under possible primitive earth conditions

Summary The synthesis of phosphatidylethanolamine was accomplished when a mixture of phosphatidic acid, ethanolamine, and cyanamide at pH 7.3 was taken to dryness and heated at temperatures ranging from 25 to 60°C for 6 h. Chromatographic, enzymatic, and chemical techniques were used to identify and confirm that phosphatidylethanolamine had been formed. This work indicates that the synthesis of this compound can occur starting with precursors and conditions that are presumed to have existed on the primitive Earth.     

Polymerization of amino acids under primitive earth conditions

Summary Chemical evolution on the primitive earth must have involved the condensation of-amino acids to peptides under a variety of conditions. Subjecting a mixture of methane, ammonia, and water to an electric discharge in the presence of free amino acids yields small peptides. The dehydration-condensation may have taken place via ammonium cyanide, the hydrogen cyanide tetramer, or aminonitriles. The experiments may be considered genuinely prebiotic and significant in the context of chemical evolution.     

Construction of protocellular structures under simulated primitive earth conditions

We have developed experimental approaches for the construction of protocellular structures under simulated primitive earth conditions and studied their formation and characteristics. Three types of envelopes; protein envelopes, lipid envelopes, and lipid-protein envelopes are considered as candidates for protocellular structures. Simple protein envelopes and lipid envelopes are presumed to have originated at an early stage of chemical evolution, interaction mutually and then evolved into more complex envelopes composed of both lipids and proteins.Three kinds of protein envelopes were constructedin situ from amino acids under simulated primitive earth conditions such as a fresh water tide pool, a warm sea, and a submarine hydrothermal vent. One protein envelope was formed from a mixture of amino acid amides at 80 °C using multiple hydration-dehydration cycles. Marigranules, protein envelope structures, were produced from mixtures of glycine and acidic, basic and aromatic amino acids at 105 °C in a modified sea medium enriched with essential transition elements. Thermostable microspheres were also formed from a mixture of glycine, alanine, valine, and aspartic acid at 250 °C and above. The microspheres did not form at lower temperatures and consist of silicates and peptide-like polymers containing imide bonds and amino acid residues enriched in valine. Amphiphilic proteins with molecular weights of 2000 were necessary for the formation of the protein envelopes.Stable lipid envelopes were formed from different dialkyl phospholipids and fatty acids.Large, stable, lipid-protein envelopes were formed from egg lecithin and the solubilized marigranules. Polycations such as polylysine and polyhistidine, or basic proteins such as lysozyme and cytochromec also stabilized lipid-protein envelopes.     

Cyanamide mediated syntheses of peptides containing histidine and hydrophobic amino acids

Summary Using the model of a primitive earth evaporation pond, the synthesis of three histidyl peptides in yields of up to 11% was demonstrated when aqueous solutions of histidine, leucine, ATP, cyanamide, and MgCl₂ were evaporated and heated for 24 h at 80°C. In addition, peptides were formed in yields of up to 56%, 35%, and 21%, respectively for phenylalanine, leucine, and alanine when aqueous solutions of the appropriate amino acid were evaporated and heated with cyanamide and one or more of the following components: ATP, AMP, 4-amino-5-imidazole carboxamide, or MgCl₂. The greatest peptide yield occurred at pH 3. But peptide formation was demonstrated for a system of Leu, cyanamide, and MgCl₂ adjusted to pH 7 with NH₄OH.Peptide synthesis was also studied in the presence of CaCl₂, ZnCl₂, different adenosine nucleotides, and UTP to compare their effects on peptide synthesis. The optimum conditions for cyanamide mediated peptide synthesis were also studied in terms of pH, reaction time, reaction temperature, and cyanamide concentration. The major side product in nearly all reactions studied appears to be an amino acid-cyanamide adduct. Peptides were analyzed and identified by thin layer chromatography, acid hydrolysis, and enzymatic degradation.     

Drawbacks of the ancient RNA-based life-like system under primitive earth conditions

Following the discovery of ribozymes, the “RNA world” hypothesis has become the most accepted hypothesis concerning the origin of life and genetic information. However, this hypothesis has several drawbacks. Verification of the hypothesis from different viewpoints led us to proposals from the viewpoint of the hydrothermal origin of life, solubility of RNA and related biopolymers, and the possibility of creating an evolutionary system comparable to the in vitro selection technique for functional RNA molecules based on molecular biology.     

HCN: A plausible source of purines,pyrimidines and amino acids on the primitive earth

Dilute (0.1 M) solutions of HCN condense to oligomers at pH 9.2. Hydrolysis of these oligomers yields 4,5-dihydroxypyrimidine, orotic acid, 5-hydroxyuracil, adenine, 4-aminoimidazole-5-carboxamide and amino acids. These results, together with the earlier data, demonstrate that the three main classes of nitrogen-containing biomolecules, purines, pyrimidines and amino acids may have originated from HCN on the primitive earth. The observation of orotic acid and 4-aminoimidazole-5-carboxyamide suggests that the contemporary biosynthetic pathways for nucleotides may have evolved from the compounds released on hydrolysis of HCN oligomers.     

Non-enzymatic transfer of sequence information under plausible prebiotic conditions

We simulated in our laboratory a prebiotic environment where dry and wet periods were cycled. Under anhydrous conditions, lipid molecules present in the medium could form fluid lamellar matrices and work as organizing agents for the condensation of nucleic acid monomers into polymers. We exposed a mixture of 2′-deoxyribonucleoside 5′-monophosphates and a ssDNA oligomer template to this dry environment at 90 °C under a continuous gentle stream of CO₂ and we followed it with rehydration periods. After five dry/wet cycles we were able to detect the presence of a product that was complementary to the template. The reaction had a 0.5% yield with respect to the template, as measured by staining with the Pico Green^® fluorescent probe. Absent initial template, the product of the reaction remained below the detection limit. In order to characterize the fidelity of replication, the synthesized strand was ligated to adapters, amplified by PCR, and sequenced. The alignment of the sequenced DNA to the expected complementary sequence revealed that the misincorporation rate was 9.9%. We present these results as a proof of concept for the possibility of having non-enzymatic transfer of sequence information in a prebiotically plausible environment.     

Survival of blue-green algae under primitive atmospheric conditions

Conditions on the primordial Earth are reviewed and information on pertinent microfossils and primitive microorganisms presented. A series of simulated pre-Cambrian environments are set up and 8 strains of blue-green algae are tested under 7 different anaerobic, mildly reducing atmospheres. Of 61 cultures tested, 12 showed growth, 32 survived and 17 died. Growth was measured spectrophotometrically. Microscopic examination failed to show any gross morphological changes in the experimental cultures. It is concluded that certain strains of blue-green algae have retained their ability to survive or grow under a primordial atmosphere.This study supported by the Graduate Department of Marine Science, Long Island University. The author wishes to thank Dr George Claus for his kind assistance.     

Synthesis of protein,nucleosides and other organic compounds from cyanamide and potassium nitrite under possible primitive earth conditions

The mixing of cyanamide and KNO₂ produced changes from white solids to yellow liquid and then to orange solid. The gases cyanogen and ammonia were formed. No external energy was used. The reactions were carried out with a small amount of O₂. The presence of proteins in the reaction product formed 13 months after the mixing was indicated by the positive reactions of the cyanamide-KNO₂ reaction product with ninhydrin, microbiuret, and Folin reagent; the ultraviolet absorption at about 280 nm; the yield of 24% of 15 amino acids; and molecular weight measurements of more than 160 000. The presence of nucleosides, nucleic acid bases, hydrocarbons, and organic esters in the reaction product formed 2 months after the mixing was indicated by ultraviolet absorption at about 260 nm, and the results of ligand-exchange chromatography, paper chromatography, infrared analysis, mass spectral analysis, and NMR spectroscopy. Possible cyanamide-mediated dehydration reactions and mechanisms are discussed.     

Synthesis of the coenzymes adenosine diphosphate glucose,guanosine diphosphate glucose,and cytidine diphosphoethanolamine under primitive earth conditions

The nonenzymatic synthesis of the coenzymes adenosine diphosphate glucose (ADPG), guanosine diphosphate glucose (GDPG), and cytidine diphosphoethanolamine (CDP-ethanolamine) has been carried out under conditions considered to have been prevalent on the early Earth. The production of these compounds was performed by allowing simple precursor molecules to react under aqueous solutions, at moderate temperatures and short periods of time, with mediation by cyanamide or urea. These two condensing agents are considered to have been present in significant amounts on the primitive Earth and have been previously used in the nonenzymatic synthesis of several other important biochemical compounds. In our experiments, ADPG was obtained by heating glucose-1-phosphate (G1P) and ATP in the presence of cyanamide for 24 h at 70 degrees C. The reaction of G1P and GTP under the same conditions yielded GDPG. The cyanamide-mediated production of CDP-ethanolamine was carried out by reacting a mixture of ethanolamine phosphate and CTP for 24 h at 70 degrees C. The separation and identification of the reaction products was carried out by paper chromatography, thin-layer chromatography, high performance thin-layer chromatography, high performance liquid chromatography, both normal and reverse-phase, UV spectroscopy, enzymatic assays, and acid hydrolysis. Due to the mild conditions employed, and to the relative ease of these reactions, these studies offer a simple attractive system for the nonenzymatic synthesis of phosphorylated high-energy metabolic intermediates under conditions considered to have been prevalent on the ancient Earth.     

Synthesis of protein, nucleosides and other organic compounds from cyanamide and potassium nitrite under possible primitive earth conditions.

The mixing of cyanamide and KNO2 produced changes from white solids to yellow liquid and then to orange solid. The gases cyanogen and ammonia were formed. No external energy was used. The reactions were carried out with a small amount of O2. The presence of proteins in the reaction product formed 13 months after the mixing was indicated by the positive reactions of the cyanamide-KNO2 reaction product with ninhydrin, microbiuret, and Folin reagent; the ultraviolet absorption at about 280 nm; the yield of 24% of 15 amino acids; and molecular weight measurements of more than 160,000. The presence of nucleosides, nucleic acid bases, hydrocarbons, and organic esters in the reaction product formed 2 months after the mixing was indicated by ultraviolet absorption at about 260 nm, and the results of ligand-exchange chromatography, paper chromatography, infrared analysis, mass spectral analysis, and NMR spectroscopy. Possible cyanamide-mediated dehydration reactions and mechanisms are discussed.