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      Deoxyribose and deoxysugar derivatives from photoprocessed astrophysical ice analogues and comparison to meteorites

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      1 , 2 , , 3 , 1
      Nature Communications
      Nature Publishing Group UK

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          Abstract

          Sugars and their derivatives are essential to all terrestrial life. Their presence in meteorites, together with amino acids, nucleobases, amphiphiles, and other compounds of biological importance, may have contributed to the inventory of organics that played a role in the emergence of life on Earth. Sugars, including ribose (the sugar of RNA), and other sugar derivatives have been identified in laboratory experiments simulating photoprocessing of ices under astrophysical conditions. In this work, we report the detection of 2-deoxyribose (the sugar of DNA) and several deoxysugar derivatives in residues produced from the ultraviolet irradiation of ice mixtures consisting of H 2O and CH 3OH. The detection of deoxysugar derivatives adds to the inventory of compounds of biological interest that can form under astrophysical conditions and puts constraints on their abiotic formation pathway. Finally, we report that some of the deoxysugar derivatives found in our residues are also newly identified in carbonaceous meteorites.

          Abstract

          Sugars are known to form from the UV photoprocessing of ices under astrophysical conditions. Here, the authors report the detection of deoxyribose, the sugar of DNA, and other deoxysugars from the UV photoprocessing of H 2O:CH 3OH ice mixtures, which are compared with materials from carbonaceous meteorites.

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          Endogenous production, exogenous delivery and impact-shock synthesis of organic molecules: an inventory for the origins of life.

          Sources of organic molecules on the early Earth divide into three categories: delivery by extraterrestrial objects; organic synthesis driven by impact shocks; and organic synthesis by other energy sources (such as ultraviolet light or electrical discharges). Estimates of these sources for plausible end-member oxidation states of the early terrestrial atmosphere suggest that the heavy bombardment before 3.5 Gyr ago either produced or delivered quantities of organics comparable to those produced by other energy sources. Which sources of prebiotic organics were quantitatively dominant depends strongly on the composition of the early terrestrial atmosphere. In the event of an early strongly reducing atmosphere, production by atmospheric shocks seems to have dominated that due to electrical discharges. Organic synthesis by ultraviolet light may, in turn, have dominated shock production, but only if a long-wavelength absorber such as H2S were supplied to the atmosphere at a rate sufficient for synthesis to have been limited by ultraviolet flux, rather than by reactant abundance. In the apparently more likely case of an early terrestrial atmosphere of intermediate oxidation state, atmospheric shocks were probably of little importance for direct organic production. For [H2]/[CO2] ratios of approximately 0.1, net organic production was some three orders of magnitude lower than for reducing atmospheres, with delivery of intact exogenous organics in interplanetary dust particles (IDPs) and ultraviolet production being the most important sources. At still lower [H2]/[CO2] ratios, IDPs may have been the dominant source of prebiotic organics on the early Earth. Endogenous, exogenous and impact-shock sources of organics could each have made a significant contribution to the origins of life.
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            Evidence for early life in Earth’s oldest hydrothermal vent precipitates

            Although it is not known when or where life on Earth began, some of the earliest habitable environments may have been submarine-hydrothermal vents. Here we describe putative fossilized microorganisms that are at least 3,770 million and possibly 4,280 million years old in ferruginous sedimentary rocks,
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              UV radiation field inside dense clouds - Its possible existence and chemical implications

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                Author and article information

                Contributors
                michel.nuevo-1@nasa.gov
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                18 December 2018
                18 December 2018
                2018
                : 9
                : 5276
                Affiliations
                [1 ]ISNI 0000 0001 1955 7990, GRID grid.419075.e, NASA Ames Research Center, ; MS 245-6, Moffett Field, CA 94035 USA
                [2 ]GRID grid.471367.0, BAER Institute, , NASA Research Park, ; MS 18-4, Moffett Field, CA 94035 USA
                [3 ]ISNI 0000 0001 1955 7990, GRID grid.419075.e, NASA Ames Research Center, ; MS 239-4, Moffett Field, CA 94035 USA
                Author information
                http://orcid.org/0000-0003-1527-2669
                http://orcid.org/0000-0002-6034-9816
                Article
                7693
                10.1038/s41467-018-07693-x
                6299135
                30563961
                cd187f19-ed28-40c9-8959-30386705694d
                © This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply 2018

                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/.

                History
                : 30 May 2018
                : 14 November 2018
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