Glyceraldehyde and Glycolaldehyde in Interstellar Ice Analogues and the Role of Aldehydes in Cosmochemical Evolution
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Modelling Panspermia in the TRAPPIST-1 System
October 13, 2017 Modelling panspermia in the TRAPPIST-1 system James A. Blake1,2*, David J. Armstrong1,2, Dimitri Veras1,2 Abstract The recent ground-breaking discovery of seven temperate planets within the TRAPPIST-1 system has been hailed as a milestone in the development of exoplanetary science. Centred on an ultra-cool dwarf star, the planets all orbit within a sixth of the distance from Mercury to the Sun. This remarkably compact nature makes the system an ideal testbed for the modelling of rapid lithopanspermia, the idea that micro-organisms can be distributed throughout the Universe via fragments of rock ejected during a meteoric impact event. We perform N-body simulations to investigate the timescale and success-rate of lithopanspermia within TRAPPIST-1. In each simulation, test particles are ejected from one of the three planets thought to lie within the so-called ‘habitable zone’ of the star into a range of allowed orbits, constrained by the ejection velocity and coplanarity of the case in question. The irradiance received by the test particles is tracked throughout the simulation, allowing the overall radiant exposure to be calculated for each one at the close of its journey. A simultaneous in-depth review of space microbiological literature has enabled inferences to be made regarding the potential survivability of lithopanspermia in compact exoplanetary systems. 1Department of Physics, University of Warwick, Coventry, CV4 7AL 2Centre for Exoplanets and Habitability, University of Warwick, Coventry, CV4 7AL *Corresponding author: [email protected] Contents Universe, and can propagate from one location to another. This interpretation owes itself predominantly to the works of William 1 Introduction1 Thompson (Lord Kelvin) and Hermann von Helmholtz in the 1.1 Mechanisms for panspermia...............2 latter half of the 19th Century. -
Prebiological Evolution and the Metabolic Origins of Life
Prebiological Evolution and the Andrew J. Pratt* Metabolic Origins of Life University of Canterbury Keywords Abiogenesis, origin of life, metabolism, hydrothermal, iron Abstract The chemoton model of cells posits three subsystems: metabolism, compartmentalization, and information. A specific model for the prebiological evolution of a reproducing system with rudimentary versions of these three interdependent subsystems is presented. This is based on the initial emergence and reproduction of autocatalytic networks in hydrothermal microcompartments containing iron sulfide. The driving force for life was catalysis of the dissipation of the intrinsic redox gradient of the planet. The codependence of life on iron and phosphate provides chemical constraints on the ordering of prebiological evolution. The initial protometabolism was based on positive feedback loops associated with in situ carbon fixation in which the initial protometabolites modified the catalytic capacity and mobility of metal-based catalysts, especially iron-sulfur centers. A number of selection mechanisms, including catalytic efficiency and specificity, hydrolytic stability, and selective solubilization, are proposed as key determinants for autocatalytic reproduction exploited in protometabolic evolution. This evolutionary process led from autocatalytic networks within preexisting compartments to discrete, reproducing, mobile vesicular protocells with the capacity to use soluble sugar phosphates and hence the opportunity to develop nucleic acids. Fidelity of information transfer in the reproduction of these increasingly complex autocatalytic networks is a key selection pressure in prebiological evolution that eventually leads to the selection of nucleic acids as a digital information subsystem and hence the emergence of fully functional chemotons capable of Darwinian evolution. 1 Introduction: Chemoton Subsystems and Evolutionary Pathways Living cells are autocatalytic entities that harness redox energy via the selective catalysis of biochemical transformations. -
Laboratory Studies for Planetary Sciences
Laboratory Studies for Planetary Sciences A Planetary Decadal Survey White Paper Prepared by the American Astronomical Society (AAS) Working Group on Laboratory Astrophysics (WGLA) http://www.aas.org/labastro Targeted Panels: Terrestrial Planets; Outer Solar System Satellites; Small Bodies Lead Author: Murthy S. Gudipati Ice Spectroscopy Lab, Science Division, Mail Stop 183-301, Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109. [email protected], 818-354-2637 Co-Authors: Michael A'Hearn - University of Maryland [email protected], 301-405-6076 Nancy Brickhouse - Harvard-Smithsonian Center for Astrophysics [email protected], 617-495-7438 John Cowan - University of Oklahoma [email protected], 405-325-3961 Paul Drake - University of Michigan [email protected], 734-763-4072 Steven Federman - University of Toledo [email protected], 419-530-2652 Gary Ferland - University of Kentucky [email protected], 859-257-879 Adam Frank - University of Rochester [email protected], 585-275-1717 Wick Haxton - University of Washington [email protected], 206-685-2397 Eric Herbst - Ohio State University [email protected], 614-292-6951 Michael Mumma - NASA/GSFC [email protected], 301-286-6994 Farid Salama - NASA/Ames Research Center [email protected], 650-604-3384 Daniel Wolf Savin - Columbia University [email protected], 212-854-4124, Lucy Ziurys – University of Arizona [email protected], 520-621-6525 1 Brief Description: The WGLA of the AAS promotes collaboration and exchange of knowledge between astronomy and planetary sciences and the laboratory sciences (physics, chemistry, and biology). -
Chemical Evolution Theory of Life's Origins the Lattimer, AST 248, Lecture 13 – P.2/20 Organics
Chemical Evolution Theory of Life's Origins 1. the synthesis and accumulation of small organic molecules, or monomers, such as amino acids and nucleotides. • Production of glycine (an amino acid) energy 3HCN+2H2O −→ C2H5O2N+CN2H2. • Production of adenine (a base): 5 HCN → C5H5N5, • Production of ribose (a sugar): 5H2CO → C5H10O5. 2. the joining of these monomers into polymers, including proteins and nucleic acids. Bernal showed that clay-like materials could serve as sites for polymerization. 3. the concentration of these molecules into droplets, called protobionts, that had chemical characteristics different from their surroundings. This relies heavily on the formation of a semi-permeable membrane, one that allows only certain materials to flow one way or the other through it. Droplet formation requires a liquid with a large surface tension, such as water. Membrane formation naturally occurs if phospholipids are present. 4. The origin of heredity, or a means of relatively error-free reproduction. It is widely, but not universally, believed that RNA-like molecules were the first self-replicators — the RNA world hypothesis. They may have been preceded by inorganic self-replicators. Lattimer, AST 248, Lecture 13 – p.1/20 Acquisition of Organic Material and Water • In the standard model of the formatio of the solar system, volatile materials are concentrated in the outer solar system. Although there is as much carbon as nearly all other heavy elements combined in the Sun and the bulk of the solar nebula, the high temperatures in the inner solar system have lead to fractional amounts of C of 10−3 of the average. -
Nomination Background: Dihydroxyacetone (CASRN: 96-26-4)
SUMMARY OF DATA FOR CHEMICAL SELECTION Dihydroxyacetone 96-26-4 BASIS OF NOMINATION TO THE CSWG As consumers have become more mindful of the hazards ofa "healthy tan," more individuals have turned to sunless tanning. Sunless tanning products represent about 10% of the $400 million market for suntan preparations, and these products are the fastest growing segment of the suntanning preparation market. All sunless tanners contain dihydroxyacetone. Information on the toxicity of dihydroxyacetone appears contradictory. A mutagen that induces DNA strand breaks, dihydroxyacetone is also an intermediate in carbohydrate metabolism in higher plants and animals. Such contradictions are not unprecedented, and it has been suggested that autooxidation of cx-hydroxycarbonyl compounds including reducing sugars may play a role in diseases associated with age and diabetes (Morita, 1991 ). When dihydroxyacetone was applied to the skin of mice, no carcinogenic effect was observed. It is unclear whether this negative response was caused by a failure ofthe compound to penetrate the skin. If so, extrapolating the dermal results to other routes of exposure would not be appropriate. NCI is nominating dihydroxyacetone to the NTP for dermal penetration studies in rats and mice to determine whether dihydroxyacetone can penetrate the skin. This information will clarify whether additional testing of dihydroxyacetone is warranted. Dihydroxyacetone 96-26-4 CHEMICAL IDENTIFICATION CAS Registry Number: 96-26-4 Chemical Abstracts Service Name: 1,3-Dihydroxy-2-propanone (9CI; 8CI) Synonyms and Tradenames: 1,3-Dihydroxydimethyl ketone; Chromelin; CTF A 00816; Dihyxal; Otan; Oxantin; Oxatone; Soleal; Triulose; Viticolor Structural Class: Ketone, ketotriose compound Structure. Molecular Formula. and Molecular Weight: 0 II /c"-. -
Biochemistry Entry of Fructose and Galactose
Paper : 04 Metabolism of carbohydrates Module : 06 Entry of Fructose and Galactose Dr. Vijaya Khader Dr. MC Varadaraj Principal Investigator Dr.S.K.Khare,Professor IIT Delhi. Paper Coordinator Dr. Ramesh Kothari,Professor UGC-CAS Department of Biosciences Saurashtra University, Rajkot-5, Gujarat-INDIA Dr. S. P. Singh, Professor Content Reviewer UGC-CAS Department of Biosciences Saurashtra University, Rajkot-5, Gujarat-INDIA Dr. Charmy Kothari, Assistant Professor Content Writer Department of Biotechnology Christ College, Affiliated to Saurashtra University, Rajkot-5, Gujarat-INDIA 1 Metabolism of Carbohydrates Biochemistry Entry of Fructose and Galactose Description of Module Subject Name Biochemistry Paper Name 04 Metabolism of Carbohydrates Module Name/Title 06 Entry of Fructose and Galactose 2 Metabolism of Carbohydrates Biochemistry Entry of Fructose and Galactose METABOLISM OF FRUCTOSE Objectives 1. To study the major pathway of fructose metabolism 2. To study specialized pathways of fructose metabolism 3. To study metabolism of galactose 4. To study disorders of galactose metabolism 3 Metabolism of Carbohydrates Biochemistry Entry of Fructose and Galactose Introduction Sucrose disaccharide contains glucose and fructose as monomers. Sucrose can be utilized as a major source of energy. Sucrose includes sugar beets, sugar cane, sorghum, maple sugar pineapple, ripe fruits and honey Corn syrup is recognized as high fructose corn syrup which gives the impression that it is very rich in fructose content but the difference between the fructose content in sucrose and high fructose corn syrup is only 5-10%. HFCS is rich in fructose because the sucrose extracted from the corn syrup is treated with the enzyme that converts some glucose in fructose which makes it more sweet. -
Computational Surface Modelling of Ices and Minerals of Interstellar Interest—Insights and Perspectives
minerals Review Computational Surface Modelling of Ices and Minerals of Interstellar Interest—Insights and Perspectives Albert Rimola 1,* , Stefano Ferrero 1, Aurèle Germain 2 , Marta Corno 2 and Piero Ugliengo 2,3 1 Departament de Química, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain; [email protected] 2 Dipartimento di Chimica, Università degli Studi di Torino, 10125 Torino, Italy; [email protected] (A.G.); [email protected] (M.C.); [email protected] (P.U.) 3 Nanostructured Interfaces and Surfaces (NIS) Centre, Università degli Studi di Torino, 10125 Torino, Italy * Correspondence: [email protected]; Tel.: +34-93-581-3723 Abstract: The universe is molecularly rich, comprising from the simplest molecule (H2) to complex organic molecules (e.g., CH3CHO and NH2CHO), some of which of biological relevance (e.g., amino acids). This chemical richness is intimately linked to the different physical phases forming Solar-like planetary systems, in which at each phase, molecules of increasing complexity form. Interestingly, synthesis of some of these compounds only takes place in the presence of interstellar (IS) grains, i.e., solid-state sub-micron sized particles consisting of naked dust of silicates or carbonaceous materials that can be covered by water-dominated ice mantles. Surfaces of IS grains exhibit particular characteristics that allow the occurrence of pivotal chemical reactions, such as the presence of binding/catalytic sites and the capability to dissipate energy excesses through the grain phonons. The present know-how on the physicochemical features of IS grains has been obtained by the fruitful synergy of astronomical observational with astrochemical modelling and laboratory experiments. -
Interstellar Dust Within the Life Cycle of the Interstellar Medium K
EPJ Web of Conferences 18, 03001 (2011) DOI: 10.1051/epjconf/20111803001 C Owned by the authors, published by EDP Sciences, 2011 Interstellar dust within the life cycle of the interstellar medium K. Demyk1,2,a 1Université de Toulouse, UPS-OMP, IRAP, Toulouse, France 2CNRS, IRAP, 9 Av. colonel Roche, BP. 44346, 31028 Toulouse Cedex 4, France Abstract. Cosmic dust is omnipresent in the Universe. Its presence influences the evolution of the astronomical objects which in turn modify its physical and chemical properties. The nature of cosmic dust, its intimate coupling with its environment, constitute a rich field of research based on observations, modelling and experimental work. This review presents the observations of the different components of interstellar dust and discusses their evolution during the life cycle of the interstellar medium. 1. INTRODUCTION Interstellar dust grains are found everywhere in the Universe: in the Solar System, around stars at all evolutionary stages, in interstellar clouds of all kind, in galaxies and in the intergalactic medium. Cosmic dust is intimately mixed with the gas-phase and represents about 1% of the gas (in mass) in our Galaxy. The interstellar extinction and the emission of diffuse interstellar clouds is reproduced by three dust components: a population of large grains, the BGs (Big Grains, ∼10–500 nm) made of silicate and a refractory mantle, a population of carbonaceous nanograins, the VSGs (Very Small Grains, 1–10 nm) and a population of macro-molecules the PAHs (Polycyclic Aromatic Hydrocarbons) [1]. These three components are more or less abundant in the diverse astrophysical environments reflecting the coupling of dust with the environment and its evolution according to the physical and dynamical conditions. -
Amino Acids and the Asymmetry of Life; Springer, 2008.Pdf
Amino Acids and the Asymmetry of Life Advances in Astrobiology and Biogeophysics springer.com This series aims to report new developments in research and teaching in the inter- disciplinary fields of astrobiology and biogeophysics. This encompasses all aspects of research into the origins of life – from the creation of matter to the emergence of complex life forms – and the study of both structure and evolution of planetary ecosystems under a given set of astro- and geophysical parameters. The methods con- sidered can be of theoretical, computational, experimental and observational nature. Preference will be given to proposals where the manuscript puts particular emphasis on the overall readability in view of the broad spectrum of scientific backgrounds involved in astrobiology and biogeophysics. The type of material considered for publication includes: • Topical monographs • Lectures on a new field, or presenting a new angle on a classical field • Suitably edited research reports • Compilations of selected papers from meetings that are devoted to specific topics The timeliness of a manuscript is more important than its form which may be un- finished or tentative. Publication in this new series is thus intended as a service to the international scientific community in that the publisher, Springer-Verlag, offers global promotion and distribution of documents which otherwise have a restricted readership. Once published and copyrighted, they can be documented in the scientific literature. Series Editors: Dr. André Brack Dr. Christopher P. McKay Centre de Biophysique Moléculaire NASA Ames Research Center CNRS, Rue Charles Sadron Moffet Field 45071 Orléans, Cedex 2, France CA 94035,USA [email protected] Dr. -
28Edc458904fb754f74e03e12f8
life Review The Astrophysical Formation of Asymmetric Molecules and the Emergence of a Chiral Bias † Adrien D. Garcia 1, Cornelia Meinert 1 , Haruna Sugahara 1,2, Nykola C. Jones 3 , Søren V. Hoffmann 3 and Uwe J. Meierhenrich 1,* 1 Institut de Chimie de Nice, Université Côte d’Azur, CNRS, UMR 7272, 06108 Nice, France; [email protected] (A.D.G.); [email protected] (C.M.); [email protected] (H.S.) 2 Japan Aerospace Exploration Agency–Institute of Space and Astronautical Science, 3-1-1 Yoshinodai, Chuo Sagamihara, Kanagawa 252-5210, Japan 3 ISA, Department of Physics and Astronomy, Aarhus University, 8000 Aarhus C, Denmark; [email protected] (N.C.J.); [email protected] (S.V.H.) * Correspondence: [email protected]; Tel.: +33-492-076-177 † This manuscript is dedicated to the 80th anniversary of Prof. Dr. Wolfram H.-P. Thiemann. Received: 22 February 2019; Accepted: 11 March 2019; Published: 16 March 2019 Abstract: The biomolecular homochirality in living organisms has been investigated for decades, but its origin remains poorly understood. It has been shown that circular polarized light (CPL) and other energy sources are capable of inducing small enantiomeric excesses (ees) in some primary biomolecules, such as amino acids or sugars. Since the first findings of amino acids in carbonaceous meteorites, a scenario in which essential chiral biomolecules originate in space and are delivered by celestial bodies has arisen. Numerous studies have thus focused on their detection, identification, and enantiomeric excess calculations in extraterrestrial matrices. In this review we summarize the discoveries in amino acids, sugars, and organophosphorus compounds in meteorites, comets, and laboratory-simulated interstellar ices. -
Interstellar Ice Photochemistry and the Deuterium Enrichment and Chemical Properties of Meteoritic Polycyclic Aromatic Hydrocarbons S
63rd Annual Meteoritical Society Meeting 5003.pdf INTERSTELLAR ICE PHOTOCHEMISTRY AND THE DEUTERIUM ENRICHMENT AND CHEMICAL PROPERTIES OF METEORITIC POLYCYCLIC AROMATIC HYDROCARBONS S. A. Sandford1, M. P. Bernstein1,2, L. J. Allamandola1, J. S. Gillette3, and R. N. Zare3, 1NASA-Ames Research Center, MS 245-6, Moffett Field CA 94035 ([email protected]), 2SETI Institute, 2035 Landings Drive, Mountain View CA 94043, USA, 3Department of Chemistry, Stanford University, Stanford CA 94305, USA. Introduction: Polycyclic aromatic hydrocarbons surroundings over time. However, exchanged D atoms (PAHs) are known to be abundant and ubiquitous in at the other sites are labile only under UV irradiation; the interstellar medium (ISM) [1]. At the temperatures once irradiation ceases these atoms will not exchange typical of dense interstellar molecular clouds (T = 10–- with the environment. 50 K), the birth sites of stars and planetary systems, Because the aromatic fractions of meteoritic PAHs will be frozen out of the gas phase into icy grain organics are known to be enriched in deuterium [6], mantles. These mantles contain a number of molecular this raises the possibility that interstellar species, the most abundant being H2O, CH3OH, CO, photoprocessing of PAHs in D-enriched interstellar CO2, NH3, CH 4, and possibly N2 and O2 [2]. Many of ices has occurred [7]. The measured D/H ratios of these molecules are expected to be enriched in interstellar ices [8] and the observed exchange rates for deuterium via a number of interstellar chemical coronene (C 24H12)-D2O and d12-coronene (C24D12)-H2O processes [2]. While frozen in these D-enriched ices, isotopic substitution experiments show that PAHs in the PAHs will be exposed to ultraviolet photons from interstellar ices could easily attain the D/H levels nearby stars, the attenuated diffuse ISM radiation field, observed in meteorites [7]. -
Rosetta/COSAC
C4PO research themes 10.1 ESA’s Cometary Mission Rosetta-Philae A. Context and state of the art Uwe Meierhenrich, member of the Institut Convergence, is involved as Co-Investigator (Co-I) in the COSAC experiment of the Rosetta-Philae mission. He is in particular in charge of the chirality-part of COSAC: ESA’s Rosetta mission [1], successfully launched in March 2004, reached its target comet 67P/Churyumov- Gerasimenko (67P/C-G) in 2014. Contrary to its predecessor missions Giotto and Vega to comet 1P/Halley [2,3], Deep-Space 1 to comet 19P/Borrelly [4], Stardust to comet 81P/Wild 2 [5], and Deep Impact to comet 9P/Tempel 1 [6], Rosetta is the first space mission designed and constructed to follow a cometary nucleus through perihelion passage and to deposit a landing unit on the cometary nucleus. In November 2014 the Philae lander detached from the Rosetta spacecraft and landed on the surface of the cometary nucleus that was of unknown morphology and chemical composition. Philae contains the cometary sampling and composition (COSAC) instrument that is equipped with a chirality module for the in situ identification, separation, and quantification of organic molecules including enantiomers expected to be present in cometary ices. The COSAC analysis was assumed to provide essential information on the Solar System formation and possibly on the origin of organic molecules and molecular asymmetry in biological systems [7]. COSAC is equipped with a multi-column gas chromatograph (GC), a time-of-flight mass spectrometer (TOFMS), and connected to an electronic system that allows remote operation of the suite.