Sustainability and the Astrobiological Perspective: Framing Human Futures in a Planetary Context
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The Great Oxidation Event: an Expert Discussion on the Causes, the Processes, and the Still Unknowns
ASTROBIOLOGY Volume 12, Number 12, 2012 The Astrobiology Society Roundtable ª Mary Ann Liebert, Inc. DOI: 10.1089/ast.2012.1110 The Great Oxidation Event: An Expert Discussion on the Causes, the Processes, and the Still Unknowns Moderator: Frances Westall1 Participants: Ariel Anbar,2 Woody Fischer,3 and Lee Kump4 Dr. Frances Westall (FW): Let’s begin with each of you seeming to get honed in on the Archean-Proterozoic tran- giving an overview as to the importance of biogenic pro- sition, I have always looked for a change in the solid cesses in the rise of oxygen—oxygenic photosynthesis. Lee, Earth dynamics that is linked to that, because the Archean- would you like to begin? Proterozoic boundary was defined based on geological evi- Dr. Lee Kump (LK): What is really interesting about the dence for the stabilization of continental cratons. history of atmospheric oxygenation is that there is this event That is what ultimately led Mark Barley and me to look at or interval of change from an anoxic Archean atmosphere to that issue of changes in style of tectonics at the Archean- an oxygenated post-Archean atmosphere (Holland, 1994). Proterozoic boundary, and ultimately focus on the style of When we think about the causes of the rise of oxygen and we volcanism (Kump and Barley, 2007). This was, again, the think about the Great Oxidation Event, it is really a funda- result of Holland pointing out that in modern volcanic sys- mental change in the way the Earth system functioned. It is a tems, the oxygen demand from the release of fluids, gases of new state; it is the oxygenated state that is distinct from the subaerial volcanoes was significantly less than that from the anoxic state, and it is nonreversible. -
40Th Annual Meeting of the AAS Division for Planetary Sciences
40th Annual Meeting of the AAS Division for Planetary Sciences 10-15 October 2008 - Ithaca, New York, Statler Hotel, 130 Statler Drive, Ithaca, NY 14853 Friday, Saturday, Sunday, Monday, Tuesday, Wednesday, 10 October 11 October 12 October 13 October 14 October 15 October 8:00 Registration Park Atrium, Statler Hotel 8 am-4 pm Registration 8 am-noon 8:30- 1 Exoplanets I 20 Titan: Upper Atmosphere 50 Outer Planets II 59 Galilean Satellites 10:00 Statler Auditorium Statler Auditorium Statler Auditorium Statler Auditorium 2 Comets I 21 Planetary Rings: Theory 51 Mercury 60 Asteroid Composition DPS Members Meeting Statler Ballroom Statler Ballroom Statler Ballroom Statler Ballroom Statler Auditorium 3 Mars: Surface 22 MB Asteroids & Trojans 52 Asteroid Discovery & Orbits Uris Hall Uris Hall Uris Hall 10:00- Coffee Break Coffee Break Coffee Break Coffee Break Coffee Break 10:30 10:30- 4 Exoplanets II 23 Titan: Lower Atmosphere 34 Titan: Subsurface 53 Outer Planets III 61 Saturnian Satellites 12:00 Statler Auditorium Statler Auditorium Statler Auditorium Statler Auditorium Statler Auditorium 5 Comets II 24 Planetary Rings: Physical 35 Outer Planets I 54 Laboratory Research 62 Venus Statler Ballroom Statler Ballroom Statler Ballroom Statler Ballroom Statler Ballroom 6 Mars: Atmosphere 25 Near Earth Asteroids 36 Icy Dwarf Planets 55 Asteroid Evolution Uris Hall Uris Hall Uris Hall Uris Hall 12:00- Lunch Lunch Lunch Lunch 1:30 Meet the IAU NSF Town Hall DPS Women Green Conferencing Yale/Princeton Rooms Yale/Princeton Rooms Yale/Princeton Rooms Yale/Princeton Rooms 1:30- 7 Special Session 37 Special Session 56 Special Session 2:30 Dynamical Classification 26 Prize Lectures Exoplanets Mission Highlights of Planetary Bodies Kuiper Prize: Statler Auditorium Statler Auditorium All talks in any given session Statler Auditorium Michael F. -
Prebiotic Chemistry, Origin, and Early Evolution of Life
Say what you are going to say, say it, say what you said Guiding theory Richard Feynman Polyelectrolytes with uniform structure are universal for Darwinism A specific hypothesis to provide context The polyelectrolyte that supported Earth’s first Darwinism was RNA Focus on paradoxes to constrain human self-deception "Settled science" says that RNA is impossible to form prebiotically Strategies for paradox resolution Mineral-guided processes allow RNA to form nonetheless Natural history context The needed chemistry-mineral combination was transient on Earth Your reward A relatively simple path to form RNA prebiotically A relatively narrow date when life on Earth originated prebiotically A clear statement of the next round of paradoxes Elisa Biondi, Hyo-Joong Kim, Daniel Hutter, Clemens Richert, Stephen Mojzsis, Ramon Brasser, Dustin Trail, Kevin Zahnle, David Catling, Rob Lavinsky Say what you are going to say, say it, say what you said Guiding theory Richard Feynman Polyelectrolytes with uniform structure are universal for Darwinism A specific hypothesis to provide context The polyelectrolyte that supported Earth’s first Darwinism was RNA Focus on paradoxes to constrain human self-deception "Settled science" says that RNA is impossible to form prebiotically Strategies for paradox resolution Mineral-guided processes allow RNA to form nonetheless Natural history context The needed chemistry-mineral combination was transient on Earth Your reward A relatively simple path to form RNA prebiotically A relatively narrow date when life on Earth originated prebiotically A clear statement of the next round of paradoxes Elisa Biondi, Hyo-Joong Kim, Daniel Hutter, Clemens Richert, Stephen Mojzsis, Ramon Brasser, Dustin Trail, Kevin Zahnle, David Catling, Rob Lavinsky What does a repeating backbone charge do for informational molecule? O 1. -
Snowball Earth: a Thin-Ice Solution with Flowing Sea Glaciers’’ by David Pollard and James F
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, C09016, doi:10.1029/2005JC003411, 2006 Click Here for Full Article Comment on ‘‘Snowball Earth: A thin-ice solution with flowing sea glaciers’’ by David Pollard and James F. Kasting Stephen G. Warren1,2 and Richard E. Brandt1 Received 22 November 2005; revised 22 May 2006; accepted 9 June 2006; published 14 September 2006. Citation: Warren, S. G., and R. E. Brandt (2006), Comment on ‘‘Snowball Earth: A thin-ice solution with flowing sea glaciers’’ by David Pollard and James F. Kasting, J. Geophys. Res., 111, C09016, doi:10.1029/2005JC003411. 1. Introduction 2. Choices of Model Variables That Favor [1] Pollard and Kasting [2005] (hereinafter referred to as Thin Ice PK) have coupled an energy-balance climate model to an 2.1. Albedo of Cold Glacier Ice ice-shelf flow model, to investigate the Snowball Earth [2] As sea glaciers flowed equatorward into the tropical episodes of the Neoproterozoic, 600–800 million years region of net sublimation, their surface snow and subsurface ago, when the ocean apparently froze all the way to the firn would sublimate away, exposing bare glacier ice to equator [Hoffman and Schrag, 2002]. PK’s particular con- the atmosphere and solar radiation. This ice would be cern was to investigate the possibility that over a wide freshwater (meteoric) ice, which originated from compres- equatorial band where sublimation exceeded snowfall, the sion of snow, so it would contain numerous bubbles, giving bare ice may have been thin enough to permit transmission a high albedo. The albedo of cold (nonmelting) glacier ice of sunlight to the water below, providing an extensive exposed by sublimation (Antarctic ‘‘blue ice’’) has been refugium for the photosynthetic eukaryotes that survived measured as 0.55–0.65 in four experiments in the Atlantic the Snowball events. -
Enceladus Life Finder: the Search for Life in a Habitable Moon
Geophysical Research Abstracts Vol. 17, EGU2015-14923, 2015 EGU General Assembly 2015 © Author(s) 2015. CC Attribution 3.0 License. Enceladus life finder: the search for life in a habitable moon. Jonathan Lunine (1), Hunter Waite (2), Frank Postberg (3), Linda Spilker (4), and Karla Clark (4) (1) Center for Radiophysics and Space Research, Cornell University, Ithaca ([email protected]), (2) Southwest Research Institute,San Antonio, ( [email protected]), (3) U. Stuttgart, Stuttgart, ([email protected]), (4) Jet Propulsion Laboratory, Pasadena CA 91125, ( [email protected]) Is there life elsewhere in the solar system? Guided by the principle that we can most easily recognize life as we know it—life that requires liquid water—Enceladus is particularly attractive because liquid water from its deep interior is actively erupting into space, making sampling of the interior straightforward. The Cassini Saturn Orbiter has provided the motivation. In particular, at high resolution, spatial coincidences between individual geysers and small-scale hot spots revealed the liquid reservoir supplying the eruptions to be not in the near-surface but deeper within the moon [1], putting on a firm foundation the principle that sampling the plume allows us to know the composition of the ocean. Sensitive gravity and topography measurements established the location and dimensions of that reservoir: ∼ 35 km beneath the SPT ice shell and extending out to at least 50 degrees latitude, implying an interior ocean large enough to have been stable over geologic time [2]. The Cassini ion neutral mass spectrometer (INMS) discovered organic and nitrogen-bearing molecules in the plume vapour, and the Cosmic Dust Analyser (CDA) detected salts in the plume icy grains, arguing strongly for ocean water being in con-tact with a rocky core [3], [4]. -
Emanuele Serrelli Nathalie Gontier Editors Explanation, Interpretation
Interdisciplinary Evolution Research 2 Emanuele Serrelli Nathalie Gontier Editors Macroevolution Explanation, Interpretation and Evidence Interdisciplinary Evolution Research Volume 2 Series editors Nathalie Gontier, Lisbon, Portugal Olga Pombo, Lisbon, Portugal [email protected] About the Series The time when only biologists studied evolution has long since passed. Accepting evolution requires us to come to terms with the fact that everything that exists must be the outcome of evolutionary processes. Today, a wide variety of academic disciplines are therefore confronted with evolutionary problems, ranging from physics and medicine, to linguistics, anthropology and sociology. Solving evolutionary problems also necessitates an inter- and transdisciplinary approach, which is why the Modern Synthesis is currently extended to include drift theory, symbiogenesis, lateral gene transfer, hybridization, epigenetics and punctuated equilibria theory. The series Interdisciplinary Evolution Research aims to provide a scholarly platform for the growing demand to examine specific evolutionary problems from the perspectives of multiple disciplines. It does not adhere to one specific academic field, one specific school of thought, or one specific evolutionary theory. Rather, books in the series thematically analyze how a variety of evolutionary fields and evolutionary theories provide insights into specific, well-defined evolutionary problems of life and the socio-cultural domain. Editors-in-chief of the series are Nathalie Gontier and Olga Pombo. The -
Mr. Brent Sherwood Caltech/JPL, United States, [email protected]
Paper ID: 32273 67th International Astronautical Congress 2016 oral IAA/IAF SPACE LIFE SCIENCES SYMPOSIUM (A1) Astrobiology and Exploration (5) Author: Mr. Brent Sherwood Caltech/JPL, United States, [email protected] Prof. Jonathan Lunine Cornell University, United States, [email protected] Mr. John Elliott National Aeronautics and Space Administration (NASA), Jet Propulsion Laboratory, United States, [email protected] Prof. Sascha Kempf University of Colorado Boulder, United States, [email protected] Mr. Travis Imken Jet Propulsion Laboratory, United States, [email protected] Dr. Peter Kahn Jet Propulsion Laboratory, United States, [email protected] Mr. Andreas Frick (country is not specified), (email is not specified) Mr. Daniel Belter Jet Propulsion Laboratory, United States, [email protected] Ms. Kelli McCoy Jet Propulsion Laboratory, United States, [email protected] Dr. David Oh Jet Propulsion Laboratory - California Institute of Technology, United States, [email protected] Dr. J. Hunter Waite Southwest Research Institute, United States, [email protected] Mr. Michael Dinicola Jet Propulsion Laboratory, United States, [email protected] SYLPH: LIFE DETECTION IN A EUROPA PLUME Abstract An investigation and system concept is described, that would equip NASA's ocean-worlds flagship mission (aka Clipper, in development now) to directly sample the chemistry of an ocean plume at Europa. Cassini discoveries at Enceladus indicate that space-flight instruments available today can exquisitely measure the composition of ice grains, dust grains, and gas in an ocean plume, revealing the ocean's hab- itability and even detecting chemical signatures of extant life with multiple, independent tests. -
Download Vol. 3 No. 2. Full Issue
ISSN 2398-5496 Vol 3, No 2. 2019 the journal of population and sustainability Information ISSN 2398-5496 The Journal of Population and Sustainability (JP&S) is an open access interdisciplinary journal exploring all aspects of the relationship between human numbers and environmental issues. The journal publishes both peer reviewed and invited material. It is intended that the JP&S act as an interdisciplinary hub facilitating collaboration and furthering the development of the field. While published by environmental charity Population Matters, the JP&S is editorially independent and welcomes contributions from scholars with a variety of perspectives on the role of population in environmental problems. The views and opinions expressed by authors are their own and do not necessarily reflect those of the editor, the editorial board or publisher. www.jpopsus.org Editor: David Samways Editorial Board: Jeroen van den Bergh (Universitat Autònoma de Barcelona) John Cleland (London School of Hygiene and Tropical Medicine) Diana Coole (Birkbeck, University of London) Herman Daly (University of Maryland) Kerryn Higgs (University of Tasmania) Graeme Maxton (Club of Rome) Fred Naggs (Natural History Museum) Jane O’Sullivan (University of Queensland) Niki Rust (Newcastle University) Bill Ryerson (Population Media Centre) Submissions We invite contributions from the social sciences, humanities, environmental and natural sciences including those concerned with family planning and reproductive health. We also invite contributions from those working for NGOs with interests in population and environmental issues. We are interested in publishing original research papers, reviews of already published research, opinion pieces and book reviews. For submission details please see our website: www.jpopsus.org The editor would like to thank Bill Anderson-Samways, Harry Cripps, and Peter Slater for their help in producing this issue. -
Methanogenic Burst in the End-Permian Carbon Cycle
Methanogenic burst in the end-Permian carbon cycle Daniel H. Rothmana,b,1, Gregory P. Fournierc, Katherine L. Frenchb, Eric J. Almc, Edward A. Boyleb, Changqun Caod, and Roger E. Summonsb aLorenz Center, bDepartment of Earth, Atmospheric, and Planetary Sciences, and cDepartment of Biological Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139; and dState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China Edited by John M. Hayes, Woods Hole Oceanographic Institution, Woods Hole, MA, and approved February 4, 2014 (received for review September 27, 2013) The end-Permian extinction is associated with a mysterious disrup- and its perturbation to the carbon cycle but also to amplify the tion to Earth’s carbon cycle. Here we identify causal mechanisms via development of marine anoxia. Taken as a whole, these results three observations. First, we show that geochemical signals indicate reconcile an array of apparently disparate observations about the superexponential growth of the marine inorganic carbon reservoir, end-Permian event. coincident with the extinction and consistent with the expansion of a new microbial metabolic pathway. Second, we show that the effi- Growth of the Marine Carbon Reservoir cient acetoclastic pathway in Methanosarcina emerged at a time sta- Fig. 1A displays the carbon-isotopic record in Meishan, China tistically indistinguishable from the extinction. Finally, we show that (5). Immediately preceding the extinction event, the isotopic com- nickel concentrations in South China sediments increased sharply at position δ1 of carbonate carbon declines by about 7‰ during the extinction, probably as a consequence of massive Siberian volca- a period of about 100 thousand years (Kyr), first slowly, and sub- nism, enabling a methanogenic expansion by removal of nickel lim- sequently rapidly. -
The First Billion Years: Warm and Wet Or Cold and Icy? Robert M
The First Billion Years: Warm and Wet or Cold and Icy? Robert M. Haberle Space Science and Astrobiology Division NASA/Ames Research Center July 15, 2014 Mars 8 Meeting Acknowledgements: Mike Carr, David Catling, and Kevin Zahnle Haberle, 8th Mars Conference Evidence for a Different Valley Networks Climate Isotopic Heavy Isotopes Aqueous Minerals 14N/15N 170±15 (Viking) 20Ne/22Ne ~10 (Meteorites) 36Ar/38Ar 4.2±0.2 (MSL) δ13C 46±4‰ (MSL) Elmann and Edwards (2014) 129Xe/132Xe ~ 2.5 (Viking) Haberle, 8th Mars Conference The First Billion Years Haberle, 8th Mars Conference Faint Young Sun Problem Noachian Haberle, 8th Mars Conference Atmospheric Redox and Outgassing The oxidation state of volcanic gases (principally H2/H2O) is governed by the oxidation state (fO2) of the upper mantle. During core(a) formation After core(b) formation Since core formation was fast (< 10 My), the mantle was likely weakly reducing and Outgassing products were mostly CO2, H2O, and N2 Haberle, 8th Mars Conference 1-D Calculations of Pollack et al. (1987) Main Conclusion: Early Mars was Continuously Warm and Wet - 5 bars of CO2 maintained against carbonate loss by impact recycling Haberle, 8th Mars Conference Problems With This Model Haberle, 8th Mars Conference 1. CO2 condenses in the atmosphere reducing the greenhouse effect. Latent heat release warms the upper atmosphere Kasting (1991) Haberle, 8th Mars Conference 2. Collision Induced Absorption Overestimated We now have more accurate absorption data based on theoretical and experimental data Old parameterizations overestimated induced-dipole absorption -1 in the 250-500 cm region Haberle, 8th Mars Conference Wordsworth et al. -
Habitable Zone
How to Find a Habitable Planet James Kasting Department of Geosciences Penn State University The search for other habitable worlds is ancient “There are infinite worlds both like and unlike this world of ours...”--- Epicurus (c. 300 BCE) (died painfully 269 BCE) “… false and "There are countless suns and damnable ...” countless earths …” G. Galilei (b. 1564) Giordano Bruno (b. 1584) in De L'infinito Universo E Mondi From Mike Devirian, (life imprisonment JPL (burned at the stake in Campo 1633) dei Fiore, Rome, 1600) • Even today, opinions differ widely as to whether other Earth-like planets exist… The Gaia hypothesis First presented in the 1970s by James Lovelock 1979 1988 http://www.ecolo.org/lovelock Gaia—The Greek goddess • According to this hypothesis, life creates and maintains conditions for its own existence by stabilizing Earth’s climate and other aspects of the Earth system • If this idea is correct, then only planets that are already inhabited would be habitable http://www.paleothea.com/Majors.html The Medea and Rare Earth hypotheses Peter Ward 2009 2000 Medea hypothesis: Life is harmful to the Earth! Rare Earth hypothesis: Complex life (animals, including humans) is rare in the universe The latest addition to this literature Me My new book (Princeton University Press, 2010) • As you will see, I am more optimistic than either Peter Ward or Jim Lovelock Talk outline • Introduction (which you heard already) • Part 1: What makes Earth unique, and what is life? • Part 2: Can we find Earth-like planets around other stars, and can -
NASA Astrobiology Institute 2018 Annual Science Report
A National Aeronautics and Space Administration 2018 Annual Science Report Table of Contents 2018 at the NAI 1 NAI 2018 Teams 2 2018 Team Reports The Evolution of Prebiotic Chemical Complexity and the Organic Inventory 6 of Protoplanetary Disk and Primordial Planets Lead Institution: NASA Ames Research Center Reliving the Past: Experimental Evolution of Major Transitions 18 Lead Institution: Georgia Institute of Technology Origin and Evolution of Organics and Water in Planetary Systems 34 Lead Institution: NASA Goddard Space Flight Center Icy Worlds: Astrobiology at the Water-Rock Interface and Beyond 46 Lead Institution: NASA Jet Propulsion Laboratory Habitability of Hydrocarbon Worlds: Titan and Beyond 60 Lead Institution: NASA Jet Propulsion Laboratory The Origins of Molecules in Diverse Space and Planetary Environments 72 and Their Intramolecular Isotope Signatures Lead Institution: Pennsylvania State University ENIGMA: Evolution of Nanomachines in Geospheres and Microbial Ancestors 80 Lead Institution: Rutgers University Changing Planetary Environments and the Fingerprints of Life 88 Lead Institution: SETI Institute Alternative Earths 100 Lead Institution: University of California, Riverside Rock Powered Life 120 Lead Institution: University of Colorado Boulder NASA Astrobiology Institute iii Annual Report 2018 2018 at the NAI In 2018, the NASA Astrobiology Program announced a plan to transition to a new structure of Research Coordination Networks, RCNs, and simultaneously planned the termination of the NASA Astrobiology Institute