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Mars, the Nearest Habitable World – a Comprehensive Program for Future Mars Exploration
Mars, the Nearest Habitable World – A Comprehensive Program for Future Mars Exploration Report by the NASA Mars Architecture Strategy Working Group (MASWG) November 2020 Front Cover: Artist Concepts Top (Artist concepts, left to right): Early Mars1; Molecules in Space2; Astronaut and Rover on Mars1; Exo-Planet System1. Bottom: Pillinger Point, Endeavour Crater, as imaged by the Opportunity rover1. Credits: 1NASA; 2Discovery Magazine Citation: Mars Architecture Strategy Working Group (MASWG), Jakosky, B. M., et al. (2020). Mars, the Nearest Habitable World—A Comprehensive Program for Future Mars Exploration. MASWG Members • Bruce Jakosky, University of Colorado (chair) • Richard Zurek, Mars Program Office, JPL (co-chair) • Shane Byrne, University of Arizona • Wendy Calvin, University of Nevada, Reno • Shannon Curry, University of California, Berkeley • Bethany Ehlmann, California Institute of Technology • Jennifer Eigenbrode, NASA/Goddard Space Flight Center • Tori Hoehler, NASA/Ames Research Center • Briony Horgan, Purdue University • Scott Hubbard, Stanford University • Tom McCollom, University of Colorado • John Mustard, Brown University • Nathaniel Putzig, Planetary Science Institute • Michelle Rucker, NASA/JSC • Michael Wolff, Space Science Institute • Robin Wordsworth, Harvard University Ex Officio • Michael Meyer, NASA Headquarters ii Mars, the Nearest Habitable World October 2020 MASWG Table of Contents Mars, the Nearest Habitable World – A Comprehensive Program for Future Mars Exploration Table of Contents EXECUTIVE SUMMARY .......................................................................................................................... -
Mid-Latitude Ice on Mars: a Science Target for Planetary Climate Histories and an Exploration Target for in Situ Resources
Mid-Latitude Ice on Mars: A Science Target for Planetary Climate Histories and an Exploration Target for In Situ Resources A White Paper submitted to the Planetary Sciences Decadal Survey 2023–2032 Primary Contact: Ali M. Bramson, Purdue University ([email protected]) Authors: Ali M. Bramson1,2 John (Jack) W. Holt2 Eric I. Petersen2,12 Chimira Andres3 Suniti Karunatillake8 Nathaniel E. Putzig6 Jonathan Bapst4 Aditya Khuller9 Hanna G. Sizemore6 Patricio Becerra5 Michael T. Mellon10 Isaac B. Smith6,13 Samuel W. Courville6 Gareth A. Morgan6 David E. Stillman14 Colin M. Dundas7 Rachel W. Obbard11 Paul Wooster15 Shannon M. Hibbard3 Matthew R. Perry6 1Purdue University, 2University of Arizona, 3University of Western Ontario CA, 4Jet Propulsion Laboratory, California Institute of Technology, 5University of Bern CH, 6Planetary Science Institute, 7U.S. Geological Survey, 8Louisiana State University, 9Arizona State University, 10Cornell University, 11SETI Institute, 12University of Alaska Fairbanks, 13York University, 14Southwest Research Institute, 15SpaceX Signatories: Ken Herkenhoff, U.S. Geological Survey Alfred McEwen, U. of Arizona David M. Hollibaugh Baker, NASA GSFC Wendy Calvin, U. of Nevada Reno Stefano Nerozzi, U. of Arizona Nicolas Thomas, U. of Bern, CH Serina Diniega, NASA JPL Paul Hayne, U. of Colorado Boulder Jeffrey Plaut, NASA JPL/Caltech Kim Seelos, JHU/APL Charity Phillips-Lander, SwRI Shane Byrne, U. of Arizona Cynthia Dinwiddie, SwRI Devanshu Jha, MVJ College of Eng., IN Aymeric Spiga, LMD/Sorbonne Université, FR Michael S. Veto, Ball Aerospace Andreas Johnsson, U. of Gothenburg, SE Matthew Chojnacki, PSI Michael Mischna, NASA JPL/Caltech Jacob Widmer, Representing Self Adrian J. Brown, Plancius Research, LLC Carol Stoker, NASA Ames Noora Alsaeed, CU Boulder, LASP Alberto G. -
Quantitative High-Resolution Reexamination of a Hypothesized
RESEARCH ARTICLE Quantitative High‐Resolution Reexamination of a 10.1029/2018JE005837 Hypothesized Ocean Shoreline in Cydonia Key Points: • We apply a proposed Mensae on Mars ‐ fi paleoshoreline identi cation toolkit Steven F. Sholes1,2 , David R. Montgomery1, and David C. Catling1,2 to newer high‐resolution data of an exemplar site for paleoshorelines on 1Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA, 2Astrobiology Program, Mars • Any wave‐generated University of Washington, Seattle, WA, USA paleoshorelines should exhibit expressions identifiable in the residual topography from an Abstract Primary support for ancient Martian oceans has relied on qualitative interpretations of idealized slope hypothesized shorelines on relatively low‐resolution images and data. We present a toolkit for • Our analysis of these curvilinear features does not support a quantitatively identifying paleoshorelines using topographic, morphological, and spectroscopic paleoshoreline interpretation and is evaluations. In particular, we apply the validated topographic expression analysis of Hare et al. (2001, more consistent with eroded https://doi.org/10.1029/2001JB000344) for the first time beyond Earth, focusing on a test case of putative lithologies shoreline features along the Arabia level in northeast Cydonia Mensae, as first described by Clifford and Supporting Information: Parker (2001, https://doi.org/10.1006/icar.2001.6671). Our results show these curvilinear features are • Supporting Information S1 inconsistent with a wave‐generated shoreline interpretation. The topographic expression analysis identifies a few potential shoreline terraces along the historically proposed contacts, but these tilt in different directions, do not follow an equipotential surface (even accounting for regional tilting), and are Correspondence to: not laterally continuous. -
Hawaiian Volcanoes: from Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012
AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012 Conveners Michael Poland, USGS – Hawaiian Volcano Observatory, USA Paul Okubo, USGS – Hawaiian Volcano Observatory, USA Ken Hon, University of Hawai'i at Hilo, USA Program Committee Rebecca Carey, University of California, Berkeley, USA Simon Carn, Michigan Technological University, USA Valerie Cayol, Obs. de Physique du Globe de Clermont-Ferrand Helge Gonnermann, Rice University, USA Scott Rowland, SOEST, University of Hawai'i at M noa, USA Financial Support 2 AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Meeting At A Glance Sunday, 19 August 2012 1600h – 1700h Welcome Reception 1700h – 1800h Introduction and Highlights of Kilauea’s Recent Eruption Activity Monday, 20 August 2012 0830h – 0900h Welcome and Logistics 0900h – 0945h Introduction – Hawaiian Volcano Observatory: Its First 100 Years of Advancing Volcanism 0945h – 1215h Magma Origin and Ascent I 1030h – 1045h Coffee Break 1215h – 1330h Lunch on Your Own 1330h – 1430h Magma Origin and Ascent II 1430h – 1445h Coffee Break 1445h – 1600h Magma Origin and Ascent Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Origin and Ascent III 1645h – 1900h Poster Session Tuesday, 21 August 2012 0900h – 1215h Magma Storage and Island Evolution I 1215h – 1330h Lunch on Your Own 1330h – 1445h Magma Storage and Island Evolution II 1445h – 1600h Magma Storage and Island Evolution Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Storage -
Is It the First Use of the Word Astrobiology ? Author
Title : Is it the first use of the word Astrobiology ? Author : Danielle Briot Adress : Observatoire de Paris 61 avenue de l’Observatoire 75014 Paris France tel : 33(0)1 40 51 22 39 and 33(0)1 45 07 78 57 [email protected] running title : First use of the word Astrobiology ? 1 Abstract The research of life in Universe is a ancient quest that has taken different forms over the centuries. It has given rise to a new science, which is normally referred as Astrobiology. It is interesting to research when this word was used for the first time and when this science developed to represent the search for life in Universe as is done today. There are records of the usage of the word "Astrobiology" as early as 1935, in an article published in a French popular science magazine. Moreover this article is quite remarkable because its portrayal of the concept of the subject is very similar to that considered today. The author of this paper was Ary J. Sternfeld (1905 - 1980), who was ortherwise known as a poorly respected great pioneer of astronautics. We provide a brief description of his life, which was heavily influenced by the tragic events of the 20th century history, from Poland and France to Russia. He was a prolific scientific writer who wrote a number of very successful scientific books and papers. Keywords : History – Pioneers 2 1. Introduction The question of the life in the Universe, in relation with the question of the multiplicity of worlds, is very ancient and probably dates back to Greek philosophers. -
Seasonal and Interannual Variability of Solar Radiation at Spirit, Opportunity and Curiosity Landing Sites
Seasonal and interannual variability of solar radiation at Spirit, Opportunity and Curiosity landing sites Álvaro VICENTE-RETORTILLO1, Mark T. LEMMON2, Germán M. MARTÍNEZ3, Francisco VALERO4, Luis VÁZQUEZ5, Mª Luisa MARTÍN6 1Departamento de Física de la Tierra, Astronomía y Astrofísica II, Universidad Complutense de Madrid, Madrid, Spain, [email protected]. 2Department of Atmospheric Sciences, Texas A&M University, College Station, TX, USA, [email protected]. 3Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA, [email protected]. 4Departamento de Física de la Tierra, Astronomía y Astrofísica II, Universidad Complutense de Madrid, Madrid, Spain, [email protected]. 5Departamento de Matemática Aplicada, Universidad Complutense de Madrid, Madrid, Spain, [email protected]. 6Departamento de Matemática Aplicada, Universidad de Valladolid, Segovia, Spain, [email protected]. Received: 14/04/2016 Accepted: 22/09/2016 Abstract In this article we characterize the radiative environment at the landing sites of NASA's Mars Exploration Rover (MER) and Mars Science Laboratory (MSL) missions. We use opacity values obtained at the surface from direct imaging of the Sun and our radiative transfer model COMIMART to analyze the seasonal and interannual variability of the daily irradiation at the MER and MSL landing sites. In addition, we analyze the behavior of the direct and diffuse components of the solar radiation at these landing sites. Key words: Solar radiation; Mars Exploration Rovers; Mars Science Laboratory; opacity, dust; radiative transfer model; Mars exploration. Variabilidad estacional e interanual de la radiación solar en las coordenadas de aterrizaje de Spirit, Opportunity y Curiosity Resumen El presente artículo está dedicado a la caracterización del entorno radiativo en los lugares de aterrizaje de las misiones de la NASA de Mars Exploration Rover (MER) y de Mars Science Laboratory (MSL). -
CYDONIA PYRAMID COMPLEX the SCARED PLANET Martian Motifs by Luis B
CYDONIA PYRAMID COMPLEX THE SCARED PLANET Martian Motifs by Luis B. Vega [email protected] www.PostScripts.org ‘…and with every wicked deception directed against those who are perishing, because they refused the love of the truth that would have saved them. For this reason, GOD will send them a powerful delusion so that they will believe The Lie, in order that judgment will come upon all who have disbelieved the truth and delighted in wickedness..’ -2 Thessalonians 2:10-12 The purpose of this study is to depict the various coordinates, approximate angles and measurements of the Cydonia pyramid complex anomaly on Mars. The depiction will be generated using Google Earth’s Mars coordinates, GPS calculations and figures. The illustration will show the entirety of the ‘Red Planet’, Mars from a frontal view that has the Valles Marineris featured very prominently. Although the rendition of the imagery is very low resolution, there is a general sense of where the Cydonia pyramid complex is situated on the planet. Although many in the past have composed a mathematical and Sacred Geometry association with the Cydonia ‘Pyramids’, this study will keep it simple and just touch on some elementary correlations. The study will only seek to highlight what is already known about the Cydonia, Mars pyramid anomaly but introduced new inferences and possible Biblical implications as to the Last Days coming deception. This study will delineate the Red Planet based on the concepts of Sacred Geometry. Depicted are 2 intersecting triangles that span the circle of the planet. These 2 triangles produce a hexagram centered on the Equator that is marked by Google and NASA. -
Ancient Fluid Escape and Related Features in Equatorial Arabia Terra (Mars)
EPSC Abstracts Vol. 7 EPSC2012-132-3 2012 European Planetary Science Congress 2012 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2012 Ancient fluid escape and related features in equatorial Arabia Terra (Mars) F. Franchi(1), A. P. Rossi(2), M. Pondrelli(3), B. Cavalazzi(1), R. Barbieri(1), Dipartimento di Scienze della Terra e Geologico Ambientali, Università di Bologna, via Zamboni 67, 40129 Bologna, Italy ([email protected]). 2Jacobs University, Bremen, Germany. 3IRSPS, Università D’Annunzio, Pescara, Italy. Abstract Noachian [1]. The ELDs are composed by light rocks showing a polygonal pattern, described elsewhere on Arabia Terra, in the equatorial region of Mars, is Mars [4], and is characterized by a high sinuosity of long-time studied area especially for the abundance the strata that locally follows a concentric trend of fluid related features. Detailed stratigraphic and informally called “pool and rim” structures (Fig. morphological study of the succession exposed in the 1A). Crommelin and Firsoff craters evidenced the occurrences of flow structures and spring deposits that endorse the presence of fluids circulation in the Late Noachian. All the morphologies in these two proto-basins occur within the Equatorial Layered Deposits (ELDs). 1. Introduction Martian layered spring deposits are of considerable interest for their supposed relationship with water and high potential of microbial signatures preservation. Their supposed fluid-related origin [1] makes the Equatorial Layered Deposits attractive targets for future missions with astrobiological purposes. In this study we report the occurrence of mounds fields and flow structures in Firsoff and Crommelin craters and summarize the result of a detailed study of the remote-sensing data sets available in this region. -
FROM WET PLANET to RED PLANET Current and Future Exploration Is Shaping Our Understanding of How the Climate of Mars Changed
FROM WET PLANET TO RED PLANET Current and future exploration is shaping our understanding of how the climate of Mars changed. Joel Davis deciphers the planet’s ancient, drying climate 14 DECEMBER 2020 | WWW.GEOLSOC.ORG.UK/GEOSCIENTIST WWW.GEOLSOC.ORG.UK/GEOSCIENTIST | DECEMBER 2020 | 15 FEATURE GEOSCIENTIST t has been an exciting year for Mars exploration. 2020 saw three spacecraft launches to the Red Planet, each by diff erent space agencies—NASA, the Chinese INational Space Administration, and the United Arab Emirates (UAE) Space Agency. NASA’s latest rover, Perseverance, is the fi rst step in a decade-long campaign for the eventual return of samples from Mars, which has the potential to truly transform our understanding of the still scientifi cally elusive Red Planet. On this side of the Atlantic, UK, European and Russian scientists are also getting ready for the launch of the European Space Agency (ESA) and Roscosmos Rosalind Franklin rover mission in 2022. The last 20 years have been a golden era for Mars exploration, with ever increasing amounts of data being returned from a variety of landed and orbital spacecraft. Such data help planetary geologists like me to unravel the complicated yet fascinating history of our celestial neighbour. As planetary geologists, we can apply our understanding of Earth to decipher the geological history of Mars, which is key to guiding future exploration. But why is planetary exploration so focused on Mars in particular? Until recently, the mantra of Mars exploration has been to follow the water, which has played an important role in shaping the surface of Mars. -
Appendix I Lunar and Martian Nomenclature
APPENDIX I LUNAR AND MARTIAN NOMENCLATURE LUNAR AND MARTIAN NOMENCLATURE A large number of names of craters and other features on the Moon and Mars, were accepted by the IAU General Assemblies X (Moscow, 1958), XI (Berkeley, 1961), XII (Hamburg, 1964), XIV (Brighton, 1970), and XV (Sydney, 1973). The names were suggested by the appropriate IAU Commissions (16 and 17). In particular the Lunar names accepted at the XIVth and XVth General Assemblies were recommended by the 'Working Group on Lunar Nomenclature' under the Chairmanship of Dr D. H. Menzel. The Martian names were suggested by the 'Working Group on Martian Nomenclature' under the Chairmanship of Dr G. de Vaucouleurs. At the XVth General Assembly a new 'Working Group on Planetary System Nomenclature' was formed (Chairman: Dr P. M. Millman) comprising various Task Groups, one for each particular subject. For further references see: [AU Trans. X, 259-263, 1960; XIB, 236-238, 1962; Xlffi, 203-204, 1966; xnffi, 99-105, 1968; XIVB, 63, 129, 139, 1971; Space Sci. Rev. 12, 136-186, 1971. Because at the recent General Assemblies some small changes, or corrections, were made, the complete list of Lunar and Martian Topographic Features is published here. Table 1 Lunar Craters Abbe 58S,174E Balboa 19N,83W Abbot 6N,55E Baldet 54S, 151W Abel 34S,85E Balmer 20S,70E Abul Wafa 2N,ll7E Banachiewicz 5N,80E Adams 32S,69E Banting 26N,16E Aitken 17S,173E Barbier 248, 158E AI-Biruni 18N,93E Barnard 30S,86E Alden 24S, lllE Barringer 29S,151W Aldrin I.4N,22.1E Bartels 24N,90W Alekhin 68S,131W Becquerei -
Meyer, Michael Mars Exploration and Mars Sample Return
Michael Meyer Lead Scientist Planetary Science Decadal Survey Mars Exploration & Mars Sample Return Panel on Mars, Nov 2, 2020 1 Why Mars? Mars is a habitable planet and has the potential to answer fundamental questions about our Solar System • The potential for life • A geological record of the first billion years of planetary evolution • A drastically changing climate through time • A compelling target for Human Exploration Mars Exploration Program Analysis Group Goals Human Life Climate Geology Exploration I. Determine if Mars ever supported life III. Understand II. Understand the origin and I. Determine if IV. Prepare for the processes evolution of Mars ever human and history of Mars as a supported, or exploration climate on Mars geological still supports life system Life I. Determine if Mars A. Search for evidence of life in environments that have a high potential for habitability and preservation of biosignatures. ever supported, or B. Assess the extent of abiotic organic chemical evolution. still supports, life. Climate II. Understand the A. Characterize the state and controlling processes of the present-day climate of Mars under the current orbital configuration. processes and B. Characterize the history and controlling processes of Mars’ climate in the recent past, history of climate under different orbital configurations. on Mars. C. Characterize Mars’ ancient climate and underlying processes. Geology III. Understand the A. Document the geologic record preserved in the crust and investigate the processes that have created and modified that record. origin and evolution B. Determine the structure, composition, and dynamics of the interior and how it has of Mars as a evolved. -
Post-Early Mars Fluvial Landforms on Mid-Latitude Impact Ejecta
42nd Lunar and Planetary Science Conference (2011) 1378.pdf POST-EARLY MARS FLUVIAL LANDFORMS ON MID-LATITUDE IMPACT EJECTA. N. Mangold, LPGN/CNRS, Université Nantes, 44322 Nantes, France. [email protected] Introduction: Early in Mars’ history (<3.7 Gy), the restrial rivers shows that these discharge rates are very climate may have been warmer than at present leading high given their length. to valley networks [1], but more recent valleys formed All examples studied were observed in regions be- on volcanoes [2,3,4], Valles Marineris [5,6], and glacial tween 25° and 42° of latitude in both hemispheres. No landforms [7,8] in conditions probably colder than in example of fluvial landforms on ejecta was found over the primitive period. Rare examples of fluvial valleys 117 craters >16 km in diameter in equatorial regions over ejecta blankets have been reported for impact (<25°N). The high proportion of craters with fresh craters [9,10,11]. In the present study, tens of craters ejecta eroded by fluvial landforms at mid-latitudes sug- (12 to 110 km in diameter) with fluvial landforms on gests that this process was common at these latitudes, ejecta were found in the mid-latitude band (25-45°) in and not limited to oldest periods. both hemisphere. Fluvial landforms on well-preserved Interpretation: Mid-latitudes (>25°) contain land- craters ejecta offer a new perspective in the under- forms such as pitted terrains or lineated fills that are standing of fluvial valleys. interpreted as being due to shallow ice deposited by Observations: A survey of hundreds of large im- atmospheric processes [12,13].