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Impact-induced amino acid formation on Hadean Earth and Noachian Mars
Abiotic synthesis of biomolecules is an essential step for the chemical origin of life. Many attempts have succeeded in synthesizing biomolecules, including amino acids and nucleobases (e.g., via spark discharge, impact shock, and hydrothermal heating), from reduced compounds that may have been limi...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7280214/ https://www.ncbi.nlm.nih.gov/pubmed/32513990 http://dx.doi.org/10.1038/s41598-020-66112-8 |
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author | Takeuchi, Yuto Furukawa, Yoshihiro Kobayashi, Takamichi Sekine, Toshimori Terada, Naoki Kakegawa, Takeshi |
author_facet | Takeuchi, Yuto Furukawa, Yoshihiro Kobayashi, Takamichi Sekine, Toshimori Terada, Naoki Kakegawa, Takeshi |
author_sort | Takeuchi, Yuto |
collection | PubMed |
description | Abiotic synthesis of biomolecules is an essential step for the chemical origin of life. Many attempts have succeeded in synthesizing biomolecules, including amino acids and nucleobases (e.g., via spark discharge, impact shock, and hydrothermal heating), from reduced compounds that may have been limited in their availabilities on Hadean Earth and Noachian Mars. On the other hand, formation of amino-acids and nucleobases from CO(2) and N(2) (i.e., the most abundant C and N sources on Earth during the Hadean) has been limited via spark discharge. Here, we demonstrate the synthesis of amino acids by laboratory impact-induced reactions among simple inorganic mixtures: Fe, Ni, Mg(2)SiO(4), H(2)O, CO(2), and N(2), by coupling the reduction of CO(2), N(2), and H(2)O with the oxidation of metallic Fe and Ni. These chemical processes simulated the possible reactions at impacts of Fe-bearing meteorites/asteroids on oceans with a CO(2) and N(2) atmosphere. The results indicate that hypervelocity impact was a source of amino acids on the Earth during the Hadean and potentially on Mars during the Noachian. Amino acids formed during such events could more readily polymerize in the next step of the chemical evolution, as impact events locally form amino acids at the impact sites. |
format | Online Article Text |
id | pubmed-7280214 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-72802142020-06-15 Impact-induced amino acid formation on Hadean Earth and Noachian Mars Takeuchi, Yuto Furukawa, Yoshihiro Kobayashi, Takamichi Sekine, Toshimori Terada, Naoki Kakegawa, Takeshi Sci Rep Article Abiotic synthesis of biomolecules is an essential step for the chemical origin of life. Many attempts have succeeded in synthesizing biomolecules, including amino acids and nucleobases (e.g., via spark discharge, impact shock, and hydrothermal heating), from reduced compounds that may have been limited in their availabilities on Hadean Earth and Noachian Mars. On the other hand, formation of amino-acids and nucleobases from CO(2) and N(2) (i.e., the most abundant C and N sources on Earth during the Hadean) has been limited via spark discharge. Here, we demonstrate the synthesis of amino acids by laboratory impact-induced reactions among simple inorganic mixtures: Fe, Ni, Mg(2)SiO(4), H(2)O, CO(2), and N(2), by coupling the reduction of CO(2), N(2), and H(2)O with the oxidation of metallic Fe and Ni. These chemical processes simulated the possible reactions at impacts of Fe-bearing meteorites/asteroids on oceans with a CO(2) and N(2) atmosphere. The results indicate that hypervelocity impact was a source of amino acids on the Earth during the Hadean and potentially on Mars during the Noachian. Amino acids formed during such events could more readily polymerize in the next step of the chemical evolution, as impact events locally form amino acids at the impact sites. Nature Publishing Group UK 2020-06-08 /pmc/articles/PMC7280214/ /pubmed/32513990 http://dx.doi.org/10.1038/s41598-020-66112-8 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Takeuchi, Yuto Furukawa, Yoshihiro Kobayashi, Takamichi Sekine, Toshimori Terada, Naoki Kakegawa, Takeshi Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title | Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title_full | Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title_fullStr | Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title_full_unstemmed | Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title_short | Impact-induced amino acid formation on Hadean Earth and Noachian Mars |
title_sort | impact-induced amino acid formation on hadean earth and noachian mars |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7280214/ https://www.ncbi.nlm.nih.gov/pubmed/32513990 http://dx.doi.org/10.1038/s41598-020-66112-8 |
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