Abstract
Reduced oxidation state phosphorus compounds may have been brought to the early Earth via meteorites or could have formed through geologic processes. These compounds could have played a role in the origin of biological phosphorus (P, hereafter) compounds. Reduced oxidation state P compounds are generally more soluble in water and are more reactive than orthophosphate and its associated minerals. However, to date no facile routes to generate C–O–P type compounds using reduced oxidation state P compounds have been reported under prebiotic conditions. In this study, we investigate the reactions between reduced oxidation state P compounds—and their oxidized products generated via Fenton reactions—with the nucleosides uridine and adenosine. The inorganic P compounds generated via Fenton chemistry readily react with nucleosides to produce organophosphites and organophosphates, including phosphate diesters via one-pot syntheses. The reactions were facilitated by NH4+ ions and urea as a condensation agent. We also present the results of the plausible stability of the organic compounds such as adenosine in an environment containing an abundance of H2O2. Such results have direct implications on finding organic compounds in Martian environments and other rocky planets (including early Earth) that were richer in H2O2 than O2. Finally, we also suggest a route for the sink of these inorganic P compounds, as a part of a plausible natural P cycle and show the possible formation of secondary phosphate minerals such as struvite and brushite on the early Earth.
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Abbreviations
- P:
-
Phosphorus
- MS:
-
Mass spectrometry
- LCMS:
-
Liquid chromatography-mass spectrometry
- PAA:
-
Phosphonoacetic acid
- U-P-U and Ad-P-Ad:
-
Phosphate diester of uridine and adenosine
- 5′-UMP:
-
Uridine-5-monophosphate
- 2′-UMP:
-
Uridine-2-monophosphate
- 3′-UMP:
-
Uridine-3-monophosphate
- 5′-AMP:
-
Adenosine-5-monophosphate
- 2′-AMP:
-
Adenosine-2-monophosphate
- 3′-AMP:
-
Adenosine-3-monophosphate
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Acknowledgements
This work was supported by NASA Exobiology program (80NSSCC18K1288). This work has also been supported in part by University of South Florida Interdisciplinary NMR Facility, The Department of Chemistry and the College of Arts and Sciences, Tampa, Florida. The Chemical Purification Analysis and Screening Core Facility (CPAS) at University of South Florida have supported the mass spectrometry data analysis. This manuscript was greatly benefited from the useful discussions with Prof. Dr. Ram Krishnamurthy (Scripps Research Institute). Authors also acknowledge the help of Prof. Bill Baker, Prof. Laurent Calcul from USF Chemistry department, and Danny Lindsay with the various instrumental set-ups during the project. Maheen Gull is extremely grateful to her husband Ryan for help with the figures and graphical abstract of the paper and watching the kids so that the experiments could be finished on time. Thanks are also due to Andrew Stella-Vega for the helpful discussions about the manuscript. The authors also thank the anonymous reviewers for the helpful suggestions. Maheen Gull would also like to thank her mother in Pakistan for all the support and to her father and finally to her daughters Luna Faye and Nova Joy for the inspiration to do better.
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Gull, M., Feng, T., Bracegirdle, J. et al. Organophosphorus Compound Formation Through the Oxidation of Reduced Oxidation State Phosphorus Compounds on the Hadean Earth. J Mol Evol 91, 60–75 (2023). https://doi.org/10.1007/s00239-022-10086-w
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DOI: https://doi.org/10.1007/s00239-022-10086-w