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. 2018 May 8;9(1):1821.
doi: 10.1038/s41467-018-04147-2.

Mimicking the surface and prebiotic chemistry of early Earth using flow chemistry

Affiliations

Mimicking the surface and prebiotic chemistry of early Earth using flow chemistry

Dougal J Ritson et al. Nat Commun. .

Abstract

When considering life's aetiology, the first questions that must be addressed are "how?" and "where?" were ostensibly complex molecules, considered necessary for life's beginning, constructed from simpler, more abundant feedstock molecules on primitive Earth. Previously, we have used multiple clues from the prebiotic synthetic requirements of (proto)biomolecules to pinpoint a set of closely related geochemical scenarios that are suggestive of flow and semi-batch chemistries. We now wish to report a multistep, uninterrupted synthesis of a key heterocycle (2-aminooxazole) en route to activated nucleotides starting from highly plausible, prebiotic feedstock molecules under conditions which mimic this scenario. Further consideration of the scenario has uncovered additional pertinent and novel aspects of prebiotic chemistry, which greatly enhance the efficiency and plausibility of the synthesis.

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Conflict of interest statement

The authors declare no competing interests.

Figures

Fig. 1
Fig. 1
Photochemical reduction of cyanohydrins. Solvated electrons and/or H can efficiently reduce cyanohydrins. These reactions are promoted by Cu+ or Fe2+ ions and a sulfurous stoichiometric reductant under UV irradiation
Fig. 2
Fig. 2
Thermal metamorphosis of ferrocyanide salts. The products formed by heating ferrocyanide can be altered simply by exchanging the counter-ion of ferrocyanide and/or varying the temperature to which the salt is heated
Fig. 3
Fig. 3
Photochemical reduction of 4 using the Fe2+/NaHSO3 system. Typical conditions: glycolonitrile 4 (30 mM), Na2SO3 (50 mM), NaH2PO4 (100 mM) and K4[Fe(CN)6] (5 mM) in H2O:D2O (9:1), pH adjusted to 6.5 with degassed HCl/NaOH and the solution was irradiated. Glyceronitrile 6 was presumed to be formed due to the liberation of cyanide in the work-up procedure, whereby paramagnetic Fex(CN)yLz species were removed by the addition of NaSH to allow NMR spectra to be acquired
Fig. 4
Fig. 4
Protection and concentration of aldehydes. 1H NMR Spectra showing how aldehydes can be protected and concentrated under prebiotically plausible conditions via the intermediacy of their bisulfite adducts. a aldehyde = formaldehyde 2; b aldehyde = glycolaldehyde 5; c aldehyde = glyceraldehyde 10. Upper spectra—solution of aldehyde, NaH2PO4 and HSO3; centre upper spectra—as upper spectra after heating to dryness for 40 h then redissolving in D2O; centre lower spectra—as upper spectra without the addition of HSO3; lower spectra—as centre lower spectra after heating to dryness for 40 h then redissolving in D2O (in a, the singlet observed at 3.3 ppm, upper and centre lower spectra, is MeOH, included in commercial formaldehyde as a stabiliser)
Fig. 5
Fig. 5
Protection of 5 at high pH and modified Strecker synthesis. 1H NMR Spectra showing the protection of glycolaldehyde 5 by bisulfite in the presence of NH3 and the Knoevenagel–Bucherer modified Strecker synthesis of serine aminonitrile. a Upper spectrum—5 in H2O/D2O with NH3 at pH 9.2 after 10 min; lower spectrum—as upper spectrum after 7 days at room temperature. b Upper spectrum—5 and Na2SO3 in H2O/D2O with NH3 at pH 9.2 after 10 min; centre spectrum—as upper spectrum after 7 days; lower—as centre spectrum with KCN added after 2 h, pH 9.2
Fig. 6
Fig. 6
Reactions of 7 with NH2CN and CaNCN. The use of cyanamide, when attempting to form 2-AO 13 from 7 (pathway A), results in the undesirable reaction of displaced bisulfite with 18, but using calcium cyanamide circumvents this problem by precipitating calcium sulfite (pathway B)
Fig. 7
Fig. 7
Flow chemistry set-up starting with glycolonitrile 4. This arrangement was designed to simulate a possible geochemical environment on early Earth (see main text). Initial concentrations: glycolonitrile 4 (60 mM), Na2SO3 (200 mM), NaH2PO4 (50 mM) and K4[Fe(CN)6] (10 mM)
Fig. 8
Fig. 8
Flow chemistry set-up starting with HMSA 9. This arrangement was designed to mimic the second variant of our geochemical scenario (see main text)
Fig. 9
Fig. 9
The two viable routes to ribo-aminooxazoline 12 starting from 4. All steps have been demonstrated under batch conditions, but those steps depicted in magenta have been performed in flow conditions in a “continuous”, uninterrupted manner starting from glycolonitrile 4 or HMSA 9. a Route to 12 via the addition of 2-AO 13 to glyceraldehyde 10. b Route to 12 via aldol reaction of 5 and 10 after their liberation from 7 and 14, respectively

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