A possible prebiotic function of cytosine as amino acid synthesizer

HJ369

The biochemical role of purine and pyrimidine bases may have been very different at the beginning of life. Their possible direct involvement in amino acid synthesis was examined via development of an in vitro reaction system, which simulated the chemical constituency of early life microenvironments. Reductive amination of pyruvate to alanine and possible alanine products by free cytosine was detected in this system. Crucial to the success of the reaction was an imine formation step, carried out under anhydrous conditions. A similar role for the adenine/hypoxanthine couple could not be verified. The possible evolutionary precedence of such an imine-involving mechanism for direct amino acid synthesis to the appearance of nucleic acids as ‘genetic information conveyors’ is proposed.

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Introduction
It is generally believed that life first appeared in a very hot, acidic, reducing, anaerobic, aqueous environment rich in hydrogen gas and sulfur and iron compounds of very negative oxidoreduction potential (1-3). Free nucleic acid bases can be synthesized from aqueous ammonium cyanide or from a mixture of methane, ammonia and water (4), but also from formamide (5,6). The free bases are of low solubility, not only to water but also to organic solvents (7), while ribonucleosides are water soluble. Under the harsh prebiotic conditions of early life, free bases probably existed initially rather than ribonucleosides, as indicated by the ease of nucleic acid deprivation (8) and the cleavage of N-glycosidic bonds (9) under hot acidic conditions, and ribonucleosides and nucleic acids evolved later. It is difficult to envisage how nucleic acids could ‘code’ for protein synthesis in their very early evolutionary stages when they are expected to have been small, perhaps only triads of bases, and devoid of regulatory promoter-like and ribosome-binding sites.

It is believed that RNA is the earliest form of nucleic acid and DNA appeared later, as a more stable depository format of the genetic material (10,11). Therefore, to relate the base structure to any probable catalytic role in amino acid synthesis, we could consider the four RNA bases. Thymine is 5´-methylated uracil and cytosine is uracil aminated at carbon 4. Uracil and cytosine may be considered two alternative states of the same base, with cytosine donating its 4-amino group for reductive amination of an α-keto acid to the corresponding amino acid, and being converted into uracil in the process. A similar role can be envisaged for hypoxanthine and its 6-aminated state, adenine.

This article attempts to experimentally prove such a directly biosynthetic role of pyrimidines in specific prebiotic microenvironments, at the very early stage of small, perhaps even trinucleotide-size, RNAs or even at a free base stage. The functional role of the exocyclic amino group of cytosine in aminating pyruvate to alanine was examined. Pyruvate may be an early prebiotic organic molecule, formed in hydrothermal vents from alkyl thiols and carbon monoxide, under the catalytic action of iron-sulfur centers (12).

According to a prebiotic evolution hypothesis (3,13,14), amino acids were formed first and polypeptides followed by random polymerization. The ‘RNA world’ theory (15) proposes that RNA was formed first by random polymerization of ribonucleotides. Selection for peptidyl transferase activity, arising from the need for better catalysis in ribonucleoprotein complexes, resulted in the first ribosomes and polypeptide synthesis. This work supports the view that at some evolutionary point amino acids may have started to be synthesized in a way dependent on the bases, which could be the origin of the contemporary interdependence of polypeptide-nucleic acid synthesis. This eliminates a significant degree of randomness, since it creates spatial proximity of amino acids to bases, facilitating a subsequent polymerization into polypeptides and RNA, respectively. The various successive ‘sections’ of the polypeptide-RNA complex could then catalyze different reactions, the product of one being a substrate for the next, or could bind to neighboring chemical groups of a substrate molecule.

Results
A reaction scheme for the use of cytosine in the amination of pyruvate to alanine was designed, as described in the Methods, and is shown in Figure 1.

Figure 1: Reaction scheme used in the present work and the expected final products.
An imine is first formed between the cytosine exocyclic amino group and the pyruvate α-keto group, under anhydrous conditions. The imine is then reduced to secondary amine by hydrogen synthesized in situ from zinc powder and 2 M HCl. The alanine-cytosine conjugate is subsequently sulfonated by sodium acid sulfite (added as sodium bisulfite). Liberation of alanine from its conjugate occurs by overnight incubation at low temperature.

HJ369_fig1

A purple spot of retention factor (Rf) the same as that of alanine was produced using the ninhydrin reaction on paper chromatograms of the cytosine-pyruvate reaction (Figure 2). Purple color is produced with amino acids that have a primary amine group, whereas proline and imino acids give yellow products (16,17). The method is very sensitive, being able to detect picogram quantities of amino acids. The purple spot was produced with greater efficiency when a combination of Zn and HCl were used as the in situ hydrogen-generating system. A minimum of 1 h of hydrogenation and overnight incubation at 4°C, after sulfonation, were required for the amino acid spot to be detected. Only the cytosine-pyruvate reaction produced the purple spot.

Figure 2:  Paper chromatography analysis of pyrimidine-pyruvate reactions.
Amino acids were detected by the ninhydrin method. A) Paper dot blots of the cytosine (C) and the uracil (U) reactions carried out in the presence (+Pyr) or absence (-Pyr) of pyruvate. Only the cytosine-pyruvate reaction stained positive for amino acids. B) Cytosine-pyruvate reaction products under various modifications of the conditions described in Figure 1. The developing solution was butanol/acetic acid/water, 4/4/1, v/v/v. Ala: 10 μg of standard alanine. 1: NaHSO3 was added first for 1 h, followed by HCl + Zn. Only traces of amino acid spot were detected at Rf the same as that of the standard alanine. 2-4: reactions were performed as described in Figure 1, but in water and under 20, 60 and 90°C respectively. No amino acid spots were detected. 5: Reduction of the imine double bond was performed with LiAlH4 instead of HCl + Zn. Traces of alanine were detected. 6: Normal anhydrous Schiff base reaction conditions, as described in Figure 1. Reduction with Zn + HCl, before sulfonation. A significant amount of alanine was obtained. C) Comparison of cytosine and uracil reactions with pyruvate, under conditions expected to generate alanine. Developing solution was butanol/acetic acid/water, 12/1/5, v/v/v. Only the cytosine-pyruvate reaction (C) produced alanine. Ala: 10 μg of standard alanine.

HJ369_fig2

The proton nuclear resonance (H-NMR) spectra (Figure 3) of the supernatants of the two reactions show a broad peak at 5.5 ppm, characteristic of the alanine amino group (NH3+) (18) present only in the cytosine-pyruvate reaction. It cannot be attributed to the cytosine exocyclic 4-amino group, which resonates at >7 ppm (19).

Figure 3: Hydrogen NMR spectra, in deuterated DMSO, of the water-soluble products from the cytosine- and uracil-pyruvate reactions.
The charged amino group (-NH3+) of alanine resonates at around 5.5 ppm as a broad peak only in the cytosine-containing reaction.

HJ369_fig3

The two-dimensional homonuclear correlated nuclear magnetic resonance (H,H-COSY NMR) spectra (Figure 4) both show coupling (solid line rectangle) of a methyl group at 1.22 ppm to a 3.6 ppm peak. These values can be attributed to the lactate salt methyl-methine moiety (CH3-CH<) resonance (18,20). Lactate is an expected product in both reactions, resulting from hydrogen-mediated reduction of pyruvate. In addition, coupling between a doublet at 1.38 ppm and a 3.4 ppm peak (dotted line square) is evident in the cytosine-pyruvate reaction and fits the alanine cation CH3-CH< resonance values as referred to in the RIO-DB Spectral Database for Organic compounds (RIO-DB-SDBS), in the Human Metabolome Database (HMDB) and especially for dimethyl sulfoxide (DMSO)-water mixtures by Zhou et al. (21).

Figure 4: Two-dimensional homonuclear correlated NMR spectra (H,H-COSY) of the water-soluble products of the cytosine-pyruvate (‘C’) and the uracil-pyruvate (‘U’) reactions for alanine synthesis. The region detecting resonance couplings in the methylmethine (CH3-CH<) group is shown (0.8-4.2 ppm). A methyl group at 1.22 ppm is coupled (solid line square) to a peak at 3.8 ppm, in both samples. This fits the lactate salt resonance values. A second coupling (dotted line square) between a doublet at 1.38 ppm and a peak at 3.4 ppm is present only in the cytosine-pyruvate reaction products. This is in agreement with reported alanine resonances.

HJ369_fig4

Liquid chromatography-mass spectrometry (LC-MS) analysis (Figure 5) detected the positive ion of alanine (alanine + H+) at m/z = 90, in the cytosine-pyruvate reaction (‘C’), but not in the uracil-pyruvate reaction (‘U’), at retention time 4.18 min, the same as that of standard alanine. Only small peaks, of noise level intensity, are detected at the same retention time of the uracil-pyruvate reaction chromatogram.

Other peaks, unique to the cytosine-pyruvate reaction, appear in the spectra as shown in Figure 6. Both reactions show large amounts of m/z = 91 peaks at retention time 3.5-4.7 min, which can be attributed to lactate-H+ positive ion. The alanine-cytosine conjugate is expected to occur only in the cytosine-pyruvate reaction and could account for the strong positive ion peak of m/z = 186 (cytosine-alanine-H+) with retention time 4.72 min. Small amounts of an m/z = 112 peak at 4.6 min, attributed to the alanine-Na+ positive ion, were also detected only in the cytosine-pyruvate reaction. Similarly, an m/z = 132 ion at 5.4 min, which could represent N-acetyl-alanine-H+ ions formed by reaction of alanine with pyruvate degradation products (22-24), showed only in the cytosine-pyruvate reaction. A prominent peak of m/z = 325, at 5.75 min of the cytosine-pyruvate chromatogram, fits the mass of a tetra-alanine-Na+ positive ion.

Figure 5: Comparison of the pyrimidine-pyruvate reaction products, using liquid chromatography/electron spray ionization mass spectrometry (LC-ESI/MS).
The cytosine-pyruvate reaction (C) contains an ion peak of m/z = 90, the same as standard alanine N+1 positive ion (alanine+H+) and with the same retention time with it (4.18 min). No such ion was detected in the uracil-pyruvate reaction (U) at that retention time, only small ‘noise level peaks’.

HJ369_fig5

As further supporting evidence for the proposed putative identity of these additional products, unique to the cytosine-pyruvate reaction, the UV absorption spectra of their chromatogram peaks are shown in Figure 7. Despite the possible presence of other co-migrating ions, the absorption maxima of alanine and alanine derivatives, at 202-204 nm, were detected in all, but were missing from the equivalent retention times of the uracil-pyruvate reaction chromatograms.

Product yields were calculated by comparison of the peak areas of the compounds (three independent experiments) to that of standard alanine and correcting for molecular weight differences. The yields, as percentages of the original pyruvate transformed into other products, are shown in Figure 8.

Discussion

Synthesis of amino acids by reductive amination of α-keto acids by ammonia in an aqueous environment is possible (25,26), but the amino acids are N-acylated by a second molecule of the α-keto acid and hydrolysis at pH 3-4 is required to liberate them. This work shows that amino acid synthesis can occur in a hydrophobic, reducing microenvironment. The imine synthesis step requires an anhydrous environment, achieved by carrying out the reaction in xylene. An anhydrous microenvironment around an α-keto acid could exist if several purine or pyrimidine molecules, forced by the repulsive forces of the surrounding water, could associate to form a hydrophobic cavity containing the α-keto acid, as happens in the interior of the nucleic acid double helices. As has been proposed (27), the formation of ribonucleosides and then oligonucleotides would facilitate the bases staying together and the formation of such a hydrophobic cavity, establishing the three-base codon as the minimum required size for the enclosure of α-keto acids and their amination to amino acids.

Figure 6: Various positive ion peaks in the LC-MS analysis of the cytosine-pyruvate (C) and the uracil-pyruvate (U) reactions.
The upper line in the spectra shows the total ion spectrum of the entire chromatogram. The lower train of peaks shows ions of the indicated mass/charge ratio, scattered along the entire chromatogram. Both reactions contain the N+1 positive ion at m/z = 91, with retention time 3.4-4.7 min, attributed to lactate. The cytosine-pyruvate reaction has also small quantities of unique ion peaks at 112, 132, 186 and 325 m/z. The 186 m/z peak, at retention time 4.72 min, fits the size of the N+1 ion of a cytosine-alanine conjugate. The other unique ion peaks fit various alanine derivatives, including the N+23 positive ion with sodium (m/z = 112), the N-acetyl-alanine N+1 ion (m/z = 132) and a tetra-alanine N+1 ion (m/z = 325).

HJ369_fig6

Amination of α-keto acids using free ammonium ions and reductive power from sulfur compounds, such as FeS and H2S, without the need for the existence of any nucleic acids or even bases, has been experimentally proved by Hafenbradl et al. (28). Similarly, Huber and Wächtershäuser (29) have reductively aminated a variety of α-keto acids into amino acids, using ammonium ions and FeS. In their reactions, aqueous media were used and the pH was 8.8-12.7, which is close to the pKa of the ammonium ion source. Their proposed primordial amino acid synthesis scheme fits well with an alkaline aqueous early life environment. In contrast, the model we propose in this paper requires hot, mildly acidic, sulfurous, hydrophobic microenvironments, such as those in the interior of a nucleic acid double helix or in the interior of cytosine-hydrophobic compound aggregates, positioned close to undersea hydrothermal vents. The presence of H2 and ammonia, as well as the low pH and high temperature in hydrothermal vents, are well documented (30-32). The reaction conditions used in this work are similar to the conditions encountered in hydrothermal vents. The only disputable point could perhaps be the use of bisulfite ion HSO3- used for sulfonation. In water, the bisulfite ion is in chemical equilibrium with SO2. Although (bi)sulfite and SO2 are present in magma and volcano emissions (33,34), they have not been reported for submarine hydrothermal vents (31). This is expected because SO2 is rapidly converted into bisulfite ions upon contact with water. Bisulfite itself readily reacts with dissolved oxygen to give sulfate ions. Its existence in hydrothermal microenvironments under oxygen-free prebiotic conditions is a reasonable expectation.

Figure 7: Ultraviolet (UV) absorption spectra of the ion LC-MS ion peaks, unique to the cytosine-pyruvate reaction (Figure 6).
Their absorption maxima in the 202-204 nm region are in agreement with the presence of an alanine moiety. The differences in the absorption curve shape in other parts of the UV spectrum could be related either to the rest of the molecule or to the co-migrating ions in the chromatogram. The alanine maximum was absent from the equivalent retention times of the uracil-pyruvate reaction LC-MS.

A previous hypothesis on the involvement of the exocyclic groups of cytosine, adenine and guanine in amino acid synthesis (35) required the presence of entire codons or at least dinucleotides, carrying the corresponding α-keto acid esterified at carbon 2´ of the riboses. In the current work, we show that amino acid synthesis is possible even by free cytosine, provided that a relatively hydrophobic microenvironment is created. Therefore, on an evolutionary time scale, amino acid and perhaps also oligopeptide synthesis could have preceded the appearance of nucleic acids and even that of nucleosides.

Explanations of the origin of tetra-alanine can be based on known amide group chemistry (9,36,37). The formation of an amide bond by direct nucleophilic attack of amino groups on carboxyl carbon is unfavorable because the hydroxyl is a very poor leaving group. Contemporary ribosomes have solved this problem by esterifying the COOH of amino acids to the 3’-OH of the last ribose of their tRNA. Carbonyl carbons of esters are easily susceptible to nucleophilic attack by the amino group of a second amino acid, forming a peptide bond. However, there are no alcohols in our reactions for such ester formation, except the lactate hydroxyl group, after the reduction step (Figure 1) and the possibility must be examined that lactate could be involved in peptide formation.

Alternatively, under the dehydrating conditions of the reaction, before the sulfonation step, anhydrides could form between the carboxyl groups of two alanines still conjugated to the cytosines. Such anhydrides can be attacked under anhydrous conditions by the secondary amino group of a third alanine, still bound to cytosine. The resulting dipeptide will have both its amino groups still attached to cytosines, from which it can detach itself after sulfonation. Also, two such dipeptide-cytosine conjugates can further react similarly to produce tetra-peptides. No longer peptides have been detected. This route of amino acid polymerization into peptides has previously been found to be successful (13) and is shown in Figure 8.

Figure 8: Percentages of the original pyruvate transformed into other products.
Putative pathways for tetra-alanine formation via an ester to lactate and via an anhydride are also shown.

HJ369_fig8

Adenine was shown to be unable to aminate keto acids under the experimental conditions we used. In adenine, the positive charge of the initial carbocation, formed during the sulfonation reaction, spreads to the neighboring imidazole ring, making attack by the nucleophile HSO3- more difficult. The same, of course, holds for the case of guanine. The development of special conditions, resembling those of ancestral life, will have to be designed for proving a similar function of purines in amino acid synthesis or a different primeval role may have to be proposed for them. Uracil and hypoxanthine (the precursors of adenine and guanine) possess no exocyclic amino group to donate to pyruvate and can be considered deaminated forms of cytosine and adenine, respectively. Accordingly, uracil could be seen as an initial acceptor of amino and other nitrogen-containing groups, being converted into cytosine in the process. A possibility presently examined by our team is that purines evolved later than pyrimidines and were used as the initial harvesters of inorganic nitrogen species, other than ammonia, subsequently passing these groups to uracil.

Conclusion

The amino acid alanine can be synthesized by reductive amination of the corresponding α-keto acid pyruvate by cytosine, in a hydrophobic, reducing microenvironment, without the need for extreme pH. This is proposed as a possible primeval route to amino acid synthesis and as a potential first function of nucleic acids or free pyrimidines, before their role as ‘genetic information’ molecules was evolved.

Methods
Formation of the Schiff base
A combination and adaptation of the methods of Kundu et al. (38) and Khrushcheva et al. (39) were used for the formation of imines between pyruvic acid and pyrimidines. Two to 100 mg of pyrimidine base (cytosine or uracil) were separately put into a 1.7 mL microfuge tube, together with an equal weight of sodium pyruvate and anhydrous sodium sulfate. The mixture was suspended in 500 μL xylene and heated in a microwave oven (Deawoo model KOR-6135) three times, for 3 min each time, at maximum power. The reactions were then left at 90°C for 24 h. Imine synthesis requires anhydrous conditions and is known to proceed also in solid phase reactions. Xylene was used to facilitate the heat transfer processes in the reaction mixture and the reaction ingredients are insoluble to it. Sodium sulfate was included to help remove traces of water present in the reactants or generated during the Schiff base formation. At the end of the reaction period, the mixtures had the appearance of a white paste, with most of the xylene and water having evaporated.

Reduction of the imine N=C bonds into amine and liberation of the amino acid
After completion of the imine formation reactions of the previous section, 10 mg solid zinc powder and 250 μL of xylene were added to each of them. Then, 10 μl 2M HCl were added under the xylene layer and mixed gently with the zinc-pyruvate-base solid mixture. The reaction was allowed to proceed at 60°C for 3 h, with the lids of the microfuge tubes open. Evolution of hydrogen gas bubbles trapped under the xylene layer among the solid constituents was visible after 15 min. In separate reactions, reduction with 10 μL 1 M LiAlH4 in 2 M HCl was also attempted. After 3 h, all of the water and the xylene had evaporated, leaving a dry, white solid, which was light yellowish in the case of the cytosine reaction.

To split the base-amino acid conjugate into free base and amino acid, the bisulfite reaction (40-43) was adapted. To the solids of each pyrimidine reaction, 300 μL freshly made 2 M NaHSO3 (as sodium bisulfite) were added, and the mixture was briefly vortexed and allowed to stand at 4°C overnight. The sulfonate of the secondary amine (base-alanine complex) is slowly hydrolyzed during this time, producing the uracil sulfonate and alanine. After a 10-minute heating at 90°C to help dissolve the products, any remaining insoluble matter was pelleted at 10,000 x g for 15 min. The supernatant, containing any produced alanine and other solubles, was transferred to a clean microfuge tube.

Detection and identification of soluble products
Five μL of each reaction were analyzed by ascending paper chromatography with butanol/acetic acid/water 12/3/5 (v/v/v) (alanine Rf = 0.37) or butanol/acetic acid/water 4/1/1 (v/v/v) (alanine Rf = 0.21) as the developing phase, for a distance of 20 cm. The chromatogram was then briefly dipped into a solution of 0.1 w/v ninhydrin in acetone and heated to 100°C for 5-10 min. Purple (mauve) spots, characteristic of amino acid reaction with ninhydrin, were developed at an Rf the same as that for the alanine standard. The rest of the water soluble reaction products were allowed to dry under reduced pressure, re-dissolved in 500 μL of water and 20 μL of the mixture were subjected to LC-MS using a LCMS-2010EV Shimadzu instrument, equipped with a 4.6 x 150 mm Pathfinder silica 100, 3.5 UM reverse phase HPLC column. The liquid phase consisted of 50% v/v methanol, 50% v/v water, 0.05% v/v formic acid, at a flow rate of 0.4 mL min-1. Detection of the eluted compounds was via a SPD-M20A diode array detector, scanning at all wavelengths from 190 to 800 nm, and by a MS detector using an electrospray interface (ESI) in positive ionization mode at full scan acquisition between m/z 50-500. The detector voltage was set at 1.4 kV and the nebulizing gas (N2) flow rate was 1.5 L min-1. These conditions preserve most of N+1 molecular positive ion (with proton addition) and the N+23 positive ion (with sodium ion addition). For interpretation of the mass and UV spectra, the information provided by Williams and Fleming (44), McLafferty and Turècek (45) and Siuzdak (46) was used. The H-NMR spectra were recorded in DMSO-d6 at 500 MHz, using a Bruker Avance DRX 500 MHz (11.4 Tesla) instrument. After removal of the insolubles by centrifugation, the supernatant was dried and the residue was taken in deuterated DMSO. For the interpretation of the NMR spectra, standard texts and books were consulted, including Friebolin (47) and Williams and Fleming (44). After the first delineation of the molecular features of the compounds, more specific information on their structure was derived from specific published articles and spectra databases, as cited in the text.H

Acknowledgements
The authors would like to thank Dr. Constantine Petrotos of the Technological and Educational Institute of Larisa, Greece, for the initial, although unsuccessful, efforts to identify alanine by GC-MS.

Authors declare no conflicts of interest.

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About the authors
Yannis Gounaris is a Professor of Molecular Biology with over 30 years of research experience in plant and microorganism molecular biology. The mechanism of molecular evolution is his most recent interest.

Constantinos Litinas is a Professor of Organic Chemistry with over 30 years of experience in the identification of molecular structures of organic molecules by spectroscopic means, primarily NMR and MS.

Eleni Evgenidou is a postdoctoral research associate, experienced in LC-MS and general chemistry techniques for the isolation and identification of organics.

References

  1. Miller SL, Cleaves HJ. Prebiotic chemistry on the primitive earth. In: Rigoutsos I, Stephanopoulos G, editors. Systems biology, Volume I: Genomics. Oxford: Oxford University Press; 2006. p. 3-56.
  2. Miller S, Orgel L. The origins of life on the earth. Englewood Cliffs (NJ): Prentice-Hall; 1974.
  3. Oparin A. The origin of life. New York: Macmillan; 1938.
  4. Schopf J, editor. Earth’s earliest biosphere: Its origin and evolution. Princeton (NJ): Princeton University Press; 1983.
  5. Basile B, Lazcano A, Oró J. Prebiotic syntheses of purines and pyrimidines. Adv Space Res. 1984;4:125-31.
    http://dx.doi.org/10.1016/0273-1177(84)90554-4
  6. Saladino R, Crestini C, Costanzo G, Negri R, diMauro E. A possible prebiotic synthesis of purine, adenosine, cytosine and 4(3H)-pyrimidinone from formamide. Implications for the origin of life. Bioorgan Med Chem. 2001;9:1249-53.
    http://dx.doi.org/10.1016/S0968-0896(00)00340-0
  7. O’Neil MJ, editor. The Merck Index. Whitehouse Station (NJ): RSC Publishing; 2013.
  8. Lindahl T, Nyberg B. Rate of depurination of native deoxyribonucleic acid. Biochemistry. 1972;11:3610-8.
    http://dx.doi.org/10.1021/bi00769a018
  9. March J. Advanced organic chemistry. New York, Chichester, Brisbane, Toronto, Singapore: John Wiley & Sons; 1985.
  10. Gilbert W. The RNA world. Nature. 1986;319:618.
    http://dx.doi.org/10.1038/319618a0
  11. Orgel LE. Prebiotic chemistry and the origin of the RNA world. Crit Rev Biochem Mol. 2004;39:99-123.
    http://dx.doi.org/10.1080/10409230490460765
  12. Cody GD, Boctor NZ, Filley TR, Hazen RM, Scott JH, Sharma A, et al. Primordial carbonylated iron-sulfur compounds and the synthesis of pyruvate. Science. 2004;289:1337-40.
    http://dx.doi.org/10.1126/science.289.5483.1337
  13. Fox SW. Self-ordered polymers and propagative cell-like systems. Naturwissenschaften. 1969;69:1-9.
    http://dx.doi.org/10.1007/BF00599584
  14. Miller SL. A production of amino acids under possible primitive earth conditions. Science. 117:528-9.
    http://dx.doi.org/10.1126/science.117.3046.528
  15. Gesteland, RF, Cech, T, Atkins, JF. The RNA world: The nature of modern RNA suggests a prebiotic RNA world. Plainview (N.Y): Cold Spring Harbor Laboratory Press; 2006.
  16. Moore S, Stein WH. Photometric ninhydrin method for use in the chromatography of amino acids. J Biol Chem. 1948;176:367-88.
  17. Troll W, Cannan RK. A modified photometric ninhydrin method for the analysis of amino and imino acids. J Biol Chem. 1953;200:803-11.
  18. Wang J, Greaves TL, Kennedy DF, Weerawardena A, Song G, Drummond CG. Lyotropic liquid crystals in amino acid derived protic ionic liquids: Physicochemical properties and behaviour as amphiphile self-assembly media. Aust J Chem. 2011;64:180-9.
    http://dx.doi.org/10.1071/CH10314
  19. Marzilli LG, Chang C-H, Caradonna JP, Kistenmacher TJ. Solution and solid state studies on the interaction of protonated cytosine salts. I. Influence of anions on 1H NMR spectra and degree of protonation in mixtures of protonated and unprotonated cytosine and derivatives. Adv Mol Relax Int Pr. 1979;15:85-101.
    http://dx.doi.org/10.1016/0378-4487(79)80025-4
  20. Cervantes-Cuevas H, Joseph-Nathan P. Preparation of (R)-(+)-lithium lactate. Monatsh Chem. 1997;128:201-6.
    http://dx.doi.org/10.1007/BF00807309
  21. Zhou Y, Won J, Lee JY, Yoon J. Studies leading to the development of a highly selective colorimetric and fluorescent chemosensor for lysine. Chem Commun. 2011;47:1997-9.
    http://dx.doi.org/10.1039/c0cc04942e
  22. Hardebeck HG. Decarboxylation of pyruvic acid in aqueous solution by thermal protenoids. Arch Biochem Biophys. 1968;123:72-81.
    http://dx.doi.org/10.1016/0003-9861(68)90105-7
  23. Leermakers PA, Ross ME, Vesley GF, Warren PC. Thermal and photochemical decomposition of ethyl and isopropyl pyruvate in the vapor phase. J Org Chem. 1965;30:914-6.
    http://dx.doi.org/10.1021/jo01014a062
  24. Margolis SA, Coxon B. Identification and quantitation of the impurities in sodium pyruvate. Anal Chem. 1986;58:2404-10.
    http://dx.doi.org/10.1021/ac00125a033
  25. Yanagawa H, Makino Y, Sato K, Nishizawa M, Egami F. A novel way for the formation of alpha-amino acids and their derivatives in an aqueous medium. Adv Space Res. 1983;3:69-74.
    http://dx.doi.org/10.1016/0273-1177(83)90043-1
  26. Yanagawa H, Makino Y, Sato K, Nishizawa M, Egami F. Novel formation of alpha-amino acids from alpha-oxo acids and ammonia in an aqueous medium. Orig Life. 1984;14:163-9.
    http://dx.doi.org/10.1007/BF00933654
  27. Gounaris Y. An evolutionary theory based on a protein-mRNA co-synthesis hypothesis. J Biol Res-Thessalon. 2011;15:3-16.
  28. Hafenbradl D, Keller M, Wächtershäuser G, Stetter KO. Primordial amino acids by reductive amination of ∝-oxo acids in conjunction with the oxidative formation of pyrite. Tetrahedron Lett. 1995;29:5179-82.
    http://dx.doi.org/10.1016/0040-4039(95)01008-6
  29. Huber C, Wächtershäuser G. Primordial reductive amination revisited. Tetrahedron Lett. 2003;44:1695-7.
    http://dx.doi.org/10.1016/S0040-4039(02)02863-0
  30. Baross JA, Hoffman SE. Submarine hydrothermal vents and associated gradient environments as sites for the origin and evolution of life. Orig Life Evol Biosph. 1985;15:327-45.
    http://dx.doi.org/10.1007/BF01808177
  31. Kingston-Tivey M. Generation of seafloor hydrothermal vent fluids and associated mineral deposits. Oceanography. 2007;20:52-67.
  32. Martin W, Baross J, Kelley D, Russell MJ. Hydrothermal vents and the origin of life. Nat Rev Microbiol. 2008;6:805-14.
  33. Carroll MR, Holloway JR. Volatiles in magmas. Washington (DC): Amer Mineral Soc; 1994.
  34. Métrich N, Bonnin-Mosbah M, Susini J, Menez B, Galoisy L. Presence of sulfite (SIV) in arc magmas: Implications for volcanic sulfur emissions. Geophys Res Lett. 2002; 29: 33-1-33-4.
  35. Copley SD, Smith E, Morowitz HJ. A mechanism for the association of amino acids with their codons and the origin of the genetic code. Proc Natl Acad Sci. 2005;102:4442-7.
    http://dx.doi.org/10.1073/pnas.0501049102
  36. Albertson NF. Synthesis of peptides with mixed anhydrides. Org React 1962;12:157-355.
  37. Bruckner R. Organic mechanisms. Reactions, stereochemistry and synthesis. Berlin, Heidelberg: Springer-Verlag; 2010.
  38. Kundu A, Shakil NA, Saxena DB, Pankaj KJ, Walia S. Microwave assisted solvent-free synthesis and biological activities of novel imines (Schiff bases). J Environ Sci Heal B. 2009;44:428-34.
    http://dx.doi.org/10.1080/03601230902934645
  39. Khrushcheva NS, Loin NM, Sokolov VI. Solid-state synthesis of Schiff bases. Russ Chem B+. 1997;46:1952-5.
    http://dx.doi.org/10.1007/BF02503793
  40. Hayatsu H, Wataya Y, Kai K. The addition of sodium bisulfate to uracil and to cytosine. J Am Chem Soc. 1969;92:724-6.
    http://dx.doi.org/10.1021/ja00706a062
  41. Hayatsu H. Co-operative mutagenic actions of bisulfate and nitrogen nucleophiles. J Mol Biol. 1977;115:19-31.
    http://dx.doi.org/10.1016/0022-2836(77)90243-1
  42. Shapiro R, Servis RE, Welcher M. Reaction of uracil and cytosine derivatives with sodium bisulfate. A specific deamination method. J Am Chem Soc. 1969;92:422-4.
    http://dx.doi.org/10.1021/ja00705a626
  43. Shapiro R, Weingras JM. Bisulfite-catalyzed transamination of cytosine and cytidine. Biochem Bioph Res Co. 1970;40:839-43.
    http://dx.doi.org/10.1016/0006-291X(70)90979-4
  44. Williams DH, Fleming I. Spectroscopic methods in organic chemistry. London: McGraw-Hill; 1995.
  45. McLafferty FW, Turècek F. Interpretation of mass spectra. Sausalito (CA): University Science Books; 1993.
  46. Siuzdak G. Mass spectrometry for biotechnology. San Diego, New York, Boston, London, Sydney, Tokyo, Toronto: Academic Press; 1996.
  47. Friebolin H. Basic one- and two-dimensional NMR spectroscopy. Weinheim (NY): VCH Publishers; 1993.

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