26 research outputs found

    From interstellar chemistry to prebiotic chemistry: organic matter evolution toward the life

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    WOS:000305043300007International audienceFrom interstellar chemistry to prebiotic chemistry: organic matter evolution toward the life The formation and evolution of organic matter starts mostly in dense molecular clouds. These clouds are mainly composed of interstellar grains, including most of the organic matter of 1:he interstellar medium embedded in molecular ices. During the evolution of these grains, this organic matter will undergo many chemical changes (ion bombardment, UV irradiations, and thermal effects) to achieve a true complexity of the organic matrix. In some areas, the cloud will collapse gravitationally on itself to form a "solar nebula" that will evolve into a protostar and potentially to a planetary system like our own. During this evolution, the interstellar grains will agglomerate to form small objects including the original organic matter, which from their evolution around the star can be described as comets or asteroids. These small objects can serve as a reservoir of organic matter for the development of prebiotic chemistry on the surface of terrestrial planets like the Earth, a prelude to the emergence of biosystems as it has indeed been the case on the Earth

    From interstellar chemistry to prebiotic chemistry: organic matter evolution toward the life

    No full text
    WOS:000305043300007International audienceFrom interstellar chemistry to prebiotic chemistry: organic matter evolution toward the life The formation and evolution of organic matter starts mostly in dense molecular clouds. These clouds are mainly composed of interstellar grains, including most of the organic matter of 1:he interstellar medium embedded in molecular ices. During the evolution of these grains, this organic matter will undergo many chemical changes (ion bombardment, UV irradiations, and thermal effects) to achieve a true complexity of the organic matrix. In some areas, the cloud will collapse gravitationally on itself to form a "solar nebula" that will evolve into a protostar and potentially to a planetary system like our own. During this evolution, the interstellar grains will agglomerate to form small objects including the original organic matter, which from their evolution around the star can be described as comets or asteroids. These small objects can serve as a reservoir of organic matter for the development of prebiotic chemistry on the surface of terrestrial planets like the Earth, a prelude to the emergence of biosystems as it has indeed been the case on the Earth

    On the conditions for mimicking natural selection in chemical systems

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    International audienc

    Data-Driven UPLC-Orbitrap MS Analysis in Astrochemistry

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    International audienceMeteorites have been found to be rich and highly diverse in organic compounds. Next to previous direct infusion high resolution mass spectrometry experiments (DI-HR-MS), we present here data-driven strategies to evaluate UPLC-Orbitrap MS analyses. This allows a comprehensive mining of structural isomers extending the level of information on the molecular diversity in astrochemical materials. As a proof-of-concept study, Murchison and Allende meteorites were analyzed. Both, global organic fingerprint and specific isomer analyses are discussed. Up to 31 different isomers per molecular composition are present in Murchison suggesting the presence of ≈ 440,000 different compounds detected therein. By means of this time-resolving high resolution mass spectrometric method, we go one step further toward the characterization of chemical structures within complex extraterrestrial mixtures, enabling a better understanding of organic chemical evolution, from interstellar ices toward small bodies in the Solar System

    Data-Driven UPLC-Orbitrap MS Analysis in Astrochemistry

    No full text
    Meteorites have been found to be rich and highly diverse in organic compounds. Next to previous direct infusion high resolution mass spectrometry experiments (DI-HR-MS), we present here data-driven strategies to evaluate UPLC-Orbitrap MS analyses. This allows a comprehensive mining of structural isomers extending the level of information on the molecular diversity in astrochemical materials. As a proof-of-concept study, Murchison and Allende meteorites were analyzed. Both, global organic fingerprint and specific isomer analyses are discussed. Up to 31 different isomers per molecular composition are present in Murchison suggesting the presence of ≈440,000 different compounds detected therein. By means of this time-resolving high resolution mass spectrometric method, we go one step further toward the characterization of chemical structures within complex extraterrestrial mixtures, enabling a better understanding of organic chemical evolution, from interstellar ices toward small bodies in the Solar System

    Data-Driven UPLC-Orbitrap MS Analysis in Astrochemistry

    No full text
    International audienceMeteorites have been found to be rich and highly diverse in organic compounds. Next to previous direct infusion high resolution mass spectrometry experiments (DI-HR-MS), we present here data-driven strategies to evaluate UPLC-Orbitrap MS analyses. This allows a comprehensive mining of structural isomers extending the level of information on the molecular diversity in astrochemical materials. As a proof-of-concept study, Murchison and Allende meteorites were analyzed. Both, global organic fingerprint and specific isomer analyses are discussed. Up to 31 different isomers per molecular composition are present in Murchison suggesting the presence of ≈ 440,000 different compounds detected therein. By means of this time-resolving high resolution mass spectrometric method, we go one step further toward the characterization of chemical structures within complex extraterrestrial mixtures, enabling a better understanding of organic chemical evolution, from interstellar ices toward small bodies in the Solar System

    Data-Driven UPLC-Orbitrap MS Analysis in Astrochemistry

    No full text
    International audienceMeteorites have been found to be rich and highly diverse in organic compounds. Next to previous direct infusion high resolution mass spectrometry experiments (DI-HR-MS), we present here data-driven strategies to evaluate UPLC-Orbitrap MS analyses. This allows a comprehensive mining of structural isomers extending the level of information on the molecular diversity in astrochemical materials. As a proof-of-concept study, Murchison and Allende meteorites were analyzed. Both, global organic fingerprint and specific isomer analyses are discussed. Up to 31 different isomers per molecular composition are present in Murchison suggesting the presence of ≈ 440,000 different compounds detected therein. By means of this time-resolving high resolution mass spectrometric method, we go one step further toward the characterization of chemical structures within complex extraterrestrial mixtures, enabling a better understanding of organic chemical evolution, from interstellar ices toward small bodies in the Solar System

    Rosetta et ExoMars sur les traces des origines moléculaires de la vie

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    National audienceLa plus rĂ©cente mission spatiale comĂ©taire, Rosetta, Ă©tait Ă©quipĂ©e d'instruments capables de caractĂ©riser les molĂ©cules organiques de la comĂšte 67P/Tchourioumov-GuĂ©rassimenko avec une prĂ©cision sans prĂ©cĂ©dent. Les spectromĂštres de masse ont rĂ©vĂ©lĂ© une grande diversitĂ© de molĂ©cules organiques et indiquent que 67P contient Ă  la fois des entitĂ©s molĂ©culaires primitives, probablement issues du nuage molĂ©culaire parent du Soleil, et d'autres, transformĂ©es dans l'environnement du disque protoplanĂ©taire lors de sa formation. La prĂ©sence de glycine et d'autres molĂ©cules organiques Ă  intĂ©rĂȘt « prĂ©biotique » renforce l'idĂ©e selon laquelle comĂštes et astĂ©roĂŻdes auraient pu apporter les briques molĂ©culaires de la vie sur Terre. La mission ExoMars, quant Ă  elle, va analyser la surface martienne pour chercher de potentielles traces de vie passĂ©e (ou prĂ©sente) sur la planĂšte rouge, Ă  travers les rapports Ă©nantiomĂ©riques des principales molĂ©cules prĂ©biotiques chirales, essentiellement des acides aminĂ©s et/ou des sucres. Cet article donne une vue d'ensemble de la chimie interstellaire, des grands nuages sombres aux petits corps de notre systĂšme solaire qui sont les tĂ©moins directs de la chimie de ces origines. Le but est de retracer les possibles origines molĂ©culaires de la vie sur Terre, dans un cadre dĂ©fini par l'astrochimie et l'astrophysique. Un paragraphe est consacrĂ© au dĂ©roulement de la mission Rosetta, ses rĂ©sultats les plus importants et leurs implications pour l'apport extraterrestre de molĂ©cules organiques sur la Terre primitive. Enfin, un intĂ©rĂȘt particulier est portĂ© au chromatographe en phase gazeuse de l'instrument MOMA Ă  bord de l'astromobile Rosalind Franklin du programme ExoMars, qui devrait arriver Ă  destination dĂ©but 2023. Mots-clĂ©s: Rosetta, ExoMars, nuage molĂ©culaire, comĂšte, chiralitĂ©, origine de la vie

    Prebiotic significance of extraterrestrial ice photochemistry: detection of hydantoin in organic residues.

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    International audienceThe delivery of extraterrestrial organic materials to primitive Earth from meteorites or micrometeorites has long been postulated to be one of the origins of the prebiotic molecules involved in the subsequent apparition of life. Here, we report on experiments in which vacuum UV photo-irradiation of interstellar/circumstellar ice analogues containing H(2)O, CH(3)OH, and NH(3) led to the production of several molecules of prebiotic interest. These were recovered at room temperature in the semi-refractory, water-soluble residues after evaporation of the ice. In particular, we detected small quantities of hydantoin (2,4-imidazolidinedione), a species suspected to play an important role in the formation of poly- and oligopeptides. In addition, hydantoin is known to form under extraterrestrial, abiotic conditions, since it has been detected, along with various other derivatives, in the soluble part of organic matter of primitive carbonaceous meteorites. This result, together with other related experiments reported recently, points to the potential importance of the photochemistry of interstellar "dirty" ices in the formation of organics in Solar System materials. Such molecules could then have been delivered to the surface of primitive Earth, as well as other telluric (exo-) planets, to help trigger first prebiotic reactions with the capacity to lead to some form of primitive biomolecular activity

    L'asymétrie de la vie: une origine extraterrestre?

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    National audienceHow did life begin? How did the single handedness of the molecular building blocks of the complex trinity – DNA, RNA, and proteins come about? Among all the theories regarding the origin of biomolecular asymmetry, those focusing on asymmetric photochemical processes using circularly polarized light (CPL) in interstellar environments appear to be the most promising. Here, insights from recent analyses of meteorites and interstellar ice analogs will be discussed along with the influence of CPL on the organic precursor molecules of life.Comment la vie est-t-elle apparue sur Terre ? Pourquoi les molĂ©cules du vivant sont-elles asymĂ©triques ? Dans cet article sont rĂ©sumĂ©es les rĂ©centes analyses des Ă©chantillons de mĂ©tĂ©orites et d'analogues de matiĂšre organique issus de glaces interstellaires simulĂ©es en laboratoire, une matiĂšre supposĂ©e ĂȘtre, au moins en partie, la matiĂšre organique originelle de notre systĂšme solaire. L'origine de l'asymĂ©trie biochimique est discutĂ©e Ă  travers l'influence de la lumiĂšre circulairement polarisĂ©e (LCP), observĂ©e dans de nombreuses rĂ©gions de formation d'Ă©toiles. Un intĂ©rĂȘt particulier est portĂ© aux rĂ©centes avancĂ©es des travaux de notre groupement de recherche, basĂ©s essentiellement sur une approche expĂ©rimentale de simulation de ces glaces en laboratoire. Mots-clĂ©s ChiralitĂ©, acides aminĂ©s, sucres, comĂšte, mĂ©tĂ©orite, origine de la vie
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