| Literature DB >> 29116184 |
Raffaele Saladino1, Bruno M Bizzarri2, Lorenzo Botta2, Jiří Šponer3,4, Judit E Šponer3, Thomas Georgelin5,6, Maguy Jaber7, Baptiste Rigaud8, Mikhail Kapralov9, Gennady N Timoshenko9, Alexei Rozanov9, Eugene Krasavin9, Anna Maria Timperio2, Ernesto Di Mauro10.
Abstract
The formation of nucleosides in abiotic conditions is a major hurdle in origin-of-life studies. We have determined the pathway of a general reaction leading to the one-pot synthesis of ribo- and 2'-deoxy-ribonucleosides from sugars and purine nucleobases under proton irradiation in the presence of a chondrite meteorite. These conditions simulate the presumptive conditions in space or on an early Earth fluxed by slow protons from the solar wind, potentially mimicking a plausible prebiotic scenario. The reaction (i) requires neither pre-activated precursors nor intermediate purification/concentration steps, (ii) is based on a defined radical mechanism, and (iii) is characterized by stereoselectivity, regioselectivity and (poly)glycosylation. The yield is enhanced by formamide and meteorite relative to the control reaction.Entities:
Year: 2017 PMID: 29116184 PMCID: PMC5677017 DOI: 10.1038/s41598-017-15392-8
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Reaction of adenine (1) with 2-deoxyribose (2).
| Entry | Conditions | Adeninea (%) | Product (%)d | |||||
|---|---|---|---|---|---|---|---|---|
| α-dfA(3) | β-dfA (4) | α-dpA (5) | β-dpA (6) | df(p)A 7a | poly-df(p)A 7b | |||
| 1 | Dry stateb | 51 | 9.2 | 3.1 | 19.5 | 5.4 | 6.3 | 0.6 |
| 2 | FA | 20 | 16.3 | 8.1 | 32.8 | 9.9 | 9.8 | 1.4 |
| 3 | FA + meteorite | ≤1 | 21.3 (21.3)c | 30.2 (30.1) | 25.1 (25.2) | 6.8 (6.8) | 15.2 (15.1) | 1.4 (1.4) |
FA = NH2CHO. Meteorite = NWA 1465. The reaction provides furanosides (f) and pyranosides (p) as α- and β-isomers. α-dfA = α-D-2′-deoxy-ribofuranosyl adenine; β-dfA = β-D-2′-deoxy-ribofuranosyl adenine; α-dpA = α-D-2′-deoxy-ribopyranosyl adenine; β-dpA = β-D-2′-deoxy-ribopiranosyl adenine; df(p)A = N6-glycosyl-2′-deoxyadenosine isomers; poly-df(p)A = N6,6-bis-glycosylated-2′-deoxyadenosine isomers. aUnreacted adenine. bObtained after dissolution of 2-deoxyribose in distilled water and successive drying under nitrogen. cData obtained in the reaction with untreated NWA 1465. dThe yield was calculated as percentage (%) of nucleoside (mmol) with respect to starting adenine. The data are the mean values of three experiments with standard deviation equal to or less than 0.1%.
Figure 1Formation of adenosine nucleosides by irradiation of adenine (1) and carbohydrates (2) and (9) (2: 2-deoxy-D-ribose. 9: D-ribose).
Figure 2HPLC chromatographic profile for the irradiation of adenine (1) and 2-deoxyribose (2) in NH2CHO and NWA 1465. Peak A (21.026 min): α-dpA (5). Peak B (23.944 min): β-dpA (6). Peak C (26.176 min): α-dfA (3). Peak D (26.684 min) β-dfA (4). Peak E (31.347-34.388 min): df(p)A (7a–b). The magnification reports the same reaction mixture co-injected with a standard sample of α-dpA (5).
Figure 3MALDI TOF/TOF analysis of the reaction between adenine (1) and 2-D-deoxyribose (2) in NH2CHO in the presence of NWA 1465. M/z = 252, 2′-deoxy adenosine. M/z = 368 df(p)A (7a–b). M/z = 484, 600, 716 and 832 products corresponding to addition of three, four, five and six sugar moieties, respectively.
Reaction of adenine (1) with ribose (9).
| Entry | Conditions | Adeninea (%) | Product yield (%)c | ||
|---|---|---|---|---|---|
| α-pA (12) | β-fA (11) | α-fA (10) + β-pA (13) | |||
| 1 | Dry stateb | 75 | 7.3 | 2.9 | 14.8 |
| 2 | FA | 63 | 10.4 | 5.6 | 21.2 |
| 3 | FA/NWA 1465 | 52 | 6.1 | 20.1 | 16.9 |
FA = NH2CHO. Meteorite = NWA 1465. The reaction provides furanosides (f) and pyranosides (p) as α- and β-isomers. α-fA = α-D-ribofuranosyl adenine; β-fA = β-D-ribofuranosyl adenine; α-pA = α-D-ribopyranosyl adenine; β-pA = β-D-ribopiranosyl adenine. aUnreacted adenine. bObtained after dissolution of ribose in distilled water and successive drying under nitrogen. cThe yield was calculated as percentage (%) of nucleoside (mmol) with respect to starting adenine. The data are the mean values of three experiments with standard deviation equal to or less than 0.1%.
13C-NMR determination of pyranoside and furanoside isomers of 2-deoxyribose (2) and ribose (9) in formamidea.
| Entry | Sugar | Glycoside isomers | Solvent | Amount (%) |
|---|---|---|---|---|
| 1 | 2-D-deoxyribose ( | β-pyranose | NH2CHO (H2O) | 40.6 (40.0) |
| 2 | 2-D-deoxyribose ( | α-pyranose | NH2CHO (H2O) | 42.7 (39.0) |
| 3 | 2-D-deoxyribose ( | β-furanose | NH2CHO (H2O) | 8.0 (9.9) |
| 4 | 2-D-deoxyribose ( | α-furanose | NH2CHO (H2O) | 9.7 (10.9) |
| 5 | D-ribose ( | β-pyranose | NH2CHO (H2O) | 64.9 (62.3) |
| 6 | D-ribose ( | α-pyranose | NH2CHO (H2O) | 16.9 (20.5) |
| 7 | D-ribose ( | β-furanose | NH2CHO (H2O) | 10.7 (12.1) |
| 8 | D-ribose ( | α-furanose | NH2CHO (H2O) | 7.5 (6.7) |
aAnomeric ratios in formamide and in water calculated on the basis of the intensity of the C1 peaks. Adding to this selectivity, the amount of β-isomers increased in the presence of NWA 1465. β-Isomers usually prevailed in mineral catalysis conditions, presumably due to the preferred attack of the nucleobases from the less hindered side of the carbohydrate adsorbed on the mineral surface[42].
Figure 4Proposed reaction mechanism for the nucleoside formation assuming adenine base and 2-deoxy ribose in its pyranose forms. R = OH, H for ribose and deoxyribose, respectively. For a more detailed mechanistic model see Fig. SI #8-A.
Figure 5N6-glycosidation of nucleobases by a C1-centered ribose radical is made possible by the presence of an H-atom bound to N6. The same mechanism is not possible at N7 because of the lack of covalently bound H.