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      Prebiotic chemicals—amino acid and phosphorus—in the coma of comet 67P/Churyumov-Gerasimenko

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      1 , 2 , * , 1 , 3 , 4 , 1 , 5 , 1 , 6 , 1 , 5 , 7 , 8 , 8 , 9 , 10 , 1 , 5 , 5 , 1 , 10 , 1 , 1 , 11 , 2 , 11 , 12 , 13 , 14 , 15 , 16 , 1 , 1 , 1 , 10 , 1
      Science Advances
      American Association for the Advancement of Science
      Origins of life, chemistry, astronomy, comets, prebiotic molecules, amino acid, 67P/Churyumov-Gerasimenko

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          Abstract

          The detection of glycine and phosphorus in the coma of 67P shows that comets contain all ingredients to help spark life on Earth.

          Abstract

          The importance of comets for the origin of life on Earth has been advocated for many decades. Amino acids are key ingredients in chemistry, leading to life as we know it. Many primitive meteorites contain amino acids, and it is generally believed that these are formed by aqueous alterations. In the collector aerogel and foil samples of the Stardust mission after the flyby at comet Wild 2, the simplest form of amino acids, glycine, has been found together with precursor molecules methylamine and ethylamine. Because of contamination issues of the samples, a cometary origin was deduced from the 13C isotopic signature. We report the presence of volatile glycine accompanied by methylamine and ethylamine in the coma of 67P/Churyumov-Gerasimenko measured by the ROSINA (Rosetta Orbiter Spectrometer for Ion and Neutral Analysis) mass spectrometer, confirming the Stardust results. Together with the detection of phosphorus and a multitude of organic molecules, this result demonstrates that comets could have played a crucial role in the emergence of life on Earth.

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          COMETARY SCIENCE. Organic compounds on comet 67P/Churyumov-Gerasimenko revealed by COSAC mass spectrometry.

          Comets harbor the most pristine material in our solar system in the form of ice, dust, silicates, and refractory organic material with some interstellar heritage. The evolved gas analyzer Cometary Sampling and Composition (COSAC) experiment aboard Rosetta's Philae lander was designed for in situ analysis of organic molecules on comet 67P/Churyumov-Gerasimenko. Twenty-five minutes after Philae's initial comet touchdown, the COSAC mass spectrometer took a spectrum in sniffing mode, which displayed a suite of 16 organic compounds, including many nitrogen-bearing species but no sulfur-bearing species, and four compounds—methyl isocyanate, acetone, propionaldehyde, and acetamide—that had not previously been reported in comets.
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            Understanding prebiotic chemistry through the analysis of extraterrestrial amino acids and nucleobases in meteorites.

            The discoveries of amino acids of extraterrestrial origin in many meteorites over the last 50 years have revolutionized the Astrobiology field. A variety of non-terrestrial amino acids similar to those found in life on Earth have been detected in meteorites. A few amino acids have even been found with chiral excesses, suggesting that meteorites could have contributed to the origin of homochirality in life on Earth. In addition to amino acids, which have been productively studied for years, sugar-like molecules, activated phosphates, and nucleobases have also been determined to be indigenous to numerous meteorites. Because these molecules are essential for life as we know it, and meteorites have been delivering them to the Earth since accretion, it is plausible that the origin(s) of life on Earth were aided by extraterrestrially-synthesized molecules. Understanding the origins of life on Earth guides our search for life elsewhere, helping to answer the question of whether biology is unique to Earth. This tutorial review focuses on meteoritic amino acids and nucleobases, exploring modern analytical methods and possible formation mechanisms. We will also discuss the unique window that meteorites provide into the chemistry that preceded life on Earth, a chemical record we do not have access to on Earth due to geologic recycling of rocks and the pervasiveness of biology across the planet. Finally, we will address the future of meteorite research, including asteroid sample return missions.
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              Organic synthesis via irradiation and warming of ice grains in the solar nebula.

              Complex organic compounds, including many important to life on Earth, are commonly found in meteoritic and cometary samples, though their origins remain a mystery. We examined whether such molecules could be produced within the solar nebula by tracking the dynamical evolution of ice grains in the nebula and recording the environments to which they were exposed. We found that icy grains originating in the outer disk, where temperatures were less than 30 kelvin, experienced ultraviolet irradiation exposures and thermal warming similar to that which has been shown to produce complex organics in laboratory experiments. These results imply that organic compounds are natural by-products of protoplanetary disk evolution and should be important ingredients in the formation of all planetary systems, including our own.
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                Author and article information

                Journal
                Sci Adv
                Sci Adv
                SciAdv
                advances
                Science Advances
                American Association for the Advancement of Science
                2375-2548
                May 2016
                27 May 2016
                : 2
                : 5
                : e1600285
                Affiliations
                [1 ]Physikalisches Institut, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
                [2 ]Center for Space and Habitability, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
                [3 ]Department of Geoscience, Tel Aviv University, Ramat Aviv 6997801, Tel Aviv, Israel.
                [4 ]LATMOS/IPSL-CNRS-UPMC-UVSQ (Laboratoire Atmosphères, Milieux, Observations Spatiales/ Institut Pierre Simon Laplace–CNRS–Universite Pierre et Marie Curie–Universite de Versailles Saint-Quentin-en-Yvelines), 4 Avenue de Neptune, F-94100 Saint-Maur, France.
                [5 ]Department of Climate and Space Sciences and Engineering, University of Michigan, 2455 Hayward, Ann Arbor, MI 48109, USA.
                [6 ]Laboratoire de Physique et Chimie de l’Environnement et de l’Espace (LPC2E), UMR CNRS 7328–Université d’Orléans, 45100 Orléans, France.
                [7 ]LISA (Laboratoire Interuniversitaire des Systèmes Atmosphériques), UMR CNRS 7583, Université Paris Est Créteil et Université Paris Diderot, IPSL, 94010 Créteil, France.
                [8 ]Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Ringlaan 3, B-1180 Brussels, Belgium.
                [9 ]Institute of Computer and Network Engineering (IDA), Technische Universität Braunschweig, Hans-Sommer-Straße 66, D-38106 Braunschweig, Germany.
                [10 ]Department of Space Science, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78228, USA.
                [11 ]Max-Planck-Institut für Sonnensystemforschung, Justus-von-Liebig-Weg 3, 37077 Göttingen, Germany.
                [12 ]Centre de Recherches Pétrographiques et Géochimiques (CRPG-CNRS), Université de Lorraine, 15 rue Notre Dame des Pauvres, BP 20, 54501 Vandoeuvre lès Nancy, France.
                [13 ]Aix Marseille Université, CNRS, LAM (Laboratoire d’Astrophysique de Marseille) UMR 7326, 13388 Marseille, France.
                [14 ]Institute for Astronomy, University of Hawaii, Honolulu, HI 96822, USA.
                [15 ]Université de Toulouse, UPS-OMP (Université Toulouse III Paul Sabatier–Observatoire Midi-Pyrénées), IRAP, F-31028 Toulouse, France.
                [16 ]CNRS, IRAP, 9 Avenue du Colonel Roche, BP 44346, F-31028 Toulouse Cedex 4, France.
                Author notes
                [* ]Corresponding author. Email: kathrin.altwegg@ 123456space.unibe.ch
                Author information
                http://orcid.org/0000-0002-2677-8238
                http://orcid.org/0000-0003-2315-5526
                http://orcid.org/0000-0001-5158-5940
                http://orcid.org/0000-0002-4261-2772
                http://orcid.org/0000-0001-5956-4722
                http://orcid.org/0000-0001-9170-5265
                http://orcid.org/0000-0003-4805-5695
                http://orcid.org/0000-0003-4101-7901
                http://orcid.org/0000-0001-5956-4722
                http://orcid.org/0000-0001-9360-4951
                http://orcid.org/0000-0002-8502-1980
                http://orcid.org/0000-0002-7988-1191
                http://orcid.org/0000-0002-5984-6153
                http://orcid.org/0000-0001-6549-3318
                http://orcid.org/0000-0003-2588-7659
                http://orcid.org/0000-0002-1812-1201
                http://orcid.org/0000-0002-1978-1025
                Article
                1600285
                10.1126/sciadv.1600285
                4928965
                27386550
                2ea64842-3359-47f7-b47a-657cc4442f05
                Copyright © 2016, The Authors

                This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial license, which permits use, distribution, and reproduction in any medium, so long as the resultant use is not for commercial advantage and provided the original work is properly cited.

                History
                : 10 February 2016
                : 03 May 2016
                Funding
                Funded by: FundRef http://dx.doi.org/10.13039/501100001711, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung;
                Award ID: ID0EXMBM7734
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100003497, Bundesbehörden der Schweizerischen Eidgenossenschaft;
                Award ID: ID0EPRBM7735
                Award ID: Prodex
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100004189, Max-Planck-Gesellschaft;
                Award ID: ID0EJWBM7736
                Award ID: 50QP1302
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/100006196, Jet Propulsion Laboratory;
                Award ID: ID0EF3BM7737
                Award ID: 1496541
                Award Recipient :
                Funded by: Belgian Science Policy Office;
                Award ID: ID0EFCCM7738
                Award ID: PRODEX/ROSINA PEA 90020
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100001665, Agence Nationale de la Recherche;
                Award ID: ID0EKJCM7739
                Award ID: ANR-11-IDEX-0001-02
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100002830, Centre National d’Etudes Spatiales;
                Award ID: ID0EZPCM7740
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100002830, Centre National d’Etudes Spatiales;
                Award ID: ID0ECXCM7741
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100000781, european research council;
                Award ID: ID0EL5CM7742
                Award ID: 267255
                Award Recipient :
                Funded by: FundRef http://dx.doi.org/10.13039/501100006245, Ministry of Science and Technology, Israel;
                Award ID: ID0EVCDM7743
                Award Recipient :
                Funded by: Israel Space Agency;
                Award ID: ID0ECIDM7744
                Award Recipient :
                Funded by: NASA;
                Award ID: ID0ENNDM7745
                Award ID: JPL-1266313
                Award Recipient :
                Funded by: NASA;
                Award ID: ID0ERUDM7746
                Award ID: NAS703001TONMO710889
                Award Recipient :
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                Ma. Florcloven Cruz

                origins of life,chemistry,astronomy,comets,prebiotic molecules,amino acid,67p/churyumov-gerasimenko

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