Dissipative Photochemical Abiogenesis of the Purines

We have proposed that the abiogenesis of life around the beginning of the Archean may have been an example of “spontaneous” microscopic dissipative structuring of UV-C pigments under the prevailing surface ultraviolet solar spectrum. The thermodynamic function of these Archean pigments (the “fundame...

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Main Authors: Claudeth Hernández, Karo Michaelian
Format: Article
Language:English
Published: MDPI AG 2022-07-01
Series:Entropy
Subjects:
Online Access:https://www.mdpi.com/1099-4300/24/8/1027
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author Claudeth Hernández
Karo Michaelian
author_facet Claudeth Hernández
Karo Michaelian
author_sort Claudeth Hernández
collection DOAJ
description We have proposed that the abiogenesis of life around the beginning of the Archean may have been an example of “spontaneous” microscopic dissipative structuring of UV-C pigments under the prevailing surface ultraviolet solar spectrum. The thermodynamic function of these Archean pigments (the “fundamental molecules of life”), as for the visible pigments of today, was to dissipate the incident solar light into heat. We have previously described the non-equilibrium thermodynamics and the photochemical mechanisms which may have been involved in the dissipative structuring of the purines adenine and hypoxanthine from the common precursor molecules of hydrogen cyanide and water under this UV light. In this article, we extend our analysis to include the production of the other two important purines, guanine and xanthine. The photochemical reactions are presumed to occur within a fatty acid vesicle floating on a hot (∼80 °C) neutral pH ocean surface exposed to the prevailing UV-C light. Reaction–diffusion equations are resolved under different environmental conditions. Significant amounts of adenine (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>5</mn></mrow></msup></semantics></math></inline-formula> M) and guanine (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></semantics></math></inline-formula> M) are obtained within 60 Archean days, starting from realistic concentrations of the precursors hydrogen cyanide and cyanogen (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>5</mn></mrow></msup></semantics></math></inline-formula> M).
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spelling doaj.art-952dbafc86bb43e683a4d0e09401bfb62023-12-01T23:38:49ZengMDPI AGEntropy1099-43002022-07-01248102710.3390/e24081027Dissipative Photochemical Abiogenesis of the PurinesClaudeth Hernández0Karo Michaelian1Department of Physics, Division of Exact and Natural Sciences, Campus Hermosillo, Universidad de Sonora, Hermosillo C.P. 83067, MexicoDepartment of Nuclear Physics and Application of Radiation, Instituto de Física, Universidad Nacional Autónoma de México, Circuito Interior de la Investigación Científica, Cuidad Universitaria, Cuidad de México C.P. 04510, MexicoWe have proposed that the abiogenesis of life around the beginning of the Archean may have been an example of “spontaneous” microscopic dissipative structuring of UV-C pigments under the prevailing surface ultraviolet solar spectrum. The thermodynamic function of these Archean pigments (the “fundamental molecules of life”), as for the visible pigments of today, was to dissipate the incident solar light into heat. We have previously described the non-equilibrium thermodynamics and the photochemical mechanisms which may have been involved in the dissipative structuring of the purines adenine and hypoxanthine from the common precursor molecules of hydrogen cyanide and water under this UV light. In this article, we extend our analysis to include the production of the other two important purines, guanine and xanthine. The photochemical reactions are presumed to occur within a fatty acid vesicle floating on a hot (∼80 °C) neutral pH ocean surface exposed to the prevailing UV-C light. Reaction–diffusion equations are resolved under different environmental conditions. Significant amounts of adenine (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>5</mn></mrow></msup></semantics></math></inline-formula> M) and guanine (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>6</mn></mrow></msup></semantics></math></inline-formula> M) are obtained within 60 Archean days, starting from realistic concentrations of the precursors hydrogen cyanide and cyanogen (∼<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><msup><mn>10</mn><mrow><mo>−</mo><mn>5</mn></mrow></msup></semantics></math></inline-formula> M).https://www.mdpi.com/1099-4300/24/8/1027origin of lifedissipative structuringnon-equilibrium thermodynamicsprebiotic chemistryabiogenesisadenine
spellingShingle Claudeth Hernández
Karo Michaelian
Dissipative Photochemical Abiogenesis of the Purines
Entropy
origin of life
dissipative structuring
non-equilibrium thermodynamics
prebiotic chemistry
abiogenesis
adenine
title Dissipative Photochemical Abiogenesis of the Purines
title_full Dissipative Photochemical Abiogenesis of the Purines
title_fullStr Dissipative Photochemical Abiogenesis of the Purines
title_full_unstemmed Dissipative Photochemical Abiogenesis of the Purines
title_short Dissipative Photochemical Abiogenesis of the Purines
title_sort dissipative photochemical abiogenesis of the purines
topic origin of life
dissipative structuring
non-equilibrium thermodynamics
prebiotic chemistry
abiogenesis
adenine
url https://www.mdpi.com/1099-4300/24/8/1027
work_keys_str_mv AT claudethhernandez dissipativephotochemicalabiogenesisofthepurines
AT karomichaelian dissipativephotochemicalabiogenesisofthepurines