World Premier International Research Center Initiative (WPI) Executive Summary (For Extension Application Screening)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
ATTACHMENT, SELECTION, and TRANSFORMATION of PREBIOTIC MOLECULES on BRUCITE [Mg(OH)2]
ATTACHMENT, SELECTION, AND TRANSFORMATION OF PREBIOTIC MOLECULES ON BRUCITE [Mg(OH)2] AND THE IMPLICATIONS FOR CHEMICAL EVOLUTION AT HYDROTHERMAL SYSTEMS by Charlene F. Estrada A dissertation submitted to The Johns Hopkins University in conformity with the requirements for the degree of Doctor of Philosophy Baltimore, Maryland September, 2014 Charlene F. Estrada All rights reserved Abstract Serpentinite-hosted hydrothermal vents may have been plausible environments for the origins of life. Mineral assemblages within hydrothermal fields may have selected and concentrated biomolecules, although little is known about molecular interactions at these mineral surfaces. I investigated the adsorption of aspartate and ribose at the surface of brucite [Mg(OH)2], a major mineral phase at serpentinite-hosted hydrothermal vents. I characterized the attachment of these molecules onto a synthetic brucite powder with Mg2+ and Ca2+ using batch adsorption experiments. I observed that Mg2+ inhibits both aspartate and ribose adsorption, whereas Ca2+ enhances adsorption onto the brucite surface. I used surface complexation modeling to predict that both aspartate and ribose attach as cooperative calcium-ligand complexes onto brucite. To further investigate the cooperative effect of Ca2+ on biomolecule adsorption, I introduced an equimolar mixture of aspartate, glycine, lysine, leucine, and phenylalanine to the brucite surface, both with and without Ca2+. Without Ca2+, up to 8.9 % aspartate and ~5 % each of the remaining four amino acids adsorbed onto brucite. When Ca2+ was added, I observed that between 5.7 to 20 times more aspartate (37.3 %) adsorbed onto brucite compared with the remaining four amino acids (~3 % each). These results, when combined with the previous study, suggest that aspartate selectively adsorbs onto brucite as a cooperative calcium-aspartate complex. -
Getting Beyond the Toy Domain. Meditations on David Deamer's
Getting beyond the toy domain: meditations on David Deamer’s “Assembling Life” The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Bains, William, "Getting beyond the toy domain: meditations on David Deamer’s 'Assembling Life.'" Life 10, 12 (Feb. 2020): no. 18 doi 10.3390/life10020018 ©2020 Author(s) As Published 10.3390/life10020018 Publisher MDPI Version Final published version Citable link https://hdl.handle.net/1721.1/125661 Terms of Use Creative Commons Attribution 4.0 International license Detailed Terms https://creativecommons.org/licenses/by/4.0/ life Book Review Getting Beyond the Toy Domain. Meditations on David Deamer’s “Assembling Life” William Bains 1,2 1 Five Alarm Bio Ltd., O2h Scitech Park, Mill Lane, Hauxton, Cambridge CB22 5HX, UK; [email protected] 2 Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA Received: 25 October 2019; Accepted: 15 February 2020; Published: 18 February 2020 Abstract: David Deamer has written another book, Assembling Life, on the origin of life. It is unapologetically polemic, presenting Deamer’s view that life originated in fresh water hydrothermal fields on volcanic islands on early Earth, arguing that this provided a unique environment not just for organic chemistry but for the self-assembling structure that drive that chemistry and form the basis of structure in life. It is worth reading, it is an advance in the field, but is it convincing? I argue that the Origin of Life field as a whole is unconvincing, generating results in Toy Domains that cannot be scaled to any real world scenario. -
Quantification of Water in Hydrous Ringwoodite
ORIGINAL RESEARCH ARTICLE published: 28 January 2015 EARTH SCIENCE doi: 10.3389/feart.2014.00038 Quantification of water in hydrous ringwoodite Sylvia-Monique Thomas 1*,StevenD.Jacobsen2, Craig R. Bina 2, Patrick Reichart 3, Marcus Moser 3, Erik H. Hauri 4, Monika Koch-Müller 5,JosephR.Smyth6 and Günther Dollinger 3 1 Department of Geoscience, University of Nevada Las Vegas, Las Vegas, NV, USA 2 Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL, USA 3 Department für Luft- und Raumfahrttechnik LRT2, Universität der Bundeswehr München, Neubiberg, Germany 4 Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC, USA 5 Helmholtz-Zentrum Potsdam, Deutsches GeoForschungsZentrum (GFZ), Potsdam, Germany 6 Department of Geological Sciences, University of Colorado Boulder, Boulder, CO, USA Edited by: Ringwoodite, γ-(Mg,Fe)2SiO4, in the lower 150 km of Earth’s mantle transition zone Mainak Mookherjee, Cornell (410–660 km depth) can incorporate up to 1.5–2wt% H2O as hydroxyl defects. We University, USA present a mineral-specific IR calibration for the absolute water content in hydrous Reviewed by: ringwoodite by combining results from Raman spectroscopy, secondary ion mass Geoffrey David Bromiley, University of Edinburgh, UK spectrometry (SIMS) and proton-proton (pp)-scattering on a suite of synthetic Mg- and Marc Blanchard, CNRS - Université Fe-bearing hydrous ringwoodites. H2O concentrations in the crystals studied here Pierre et Marie Curie, France range from 0.46 to 1.7wt% H2O (absolute methods), with the maximum H2Oin *Correspondence: the same sample giving 2.5 wt% by SIMS calibration. Anchoring our spectroscopic Sylvia-Monique Thomas, results to absolute H-atom concentrations from pp-scattering measurements, we report Department of Geoscience, University of Nevada Las Vegas, frequency-dependent integrated IR-absorption coefficients for water in ringwoodite −1 −2 4505 S. -
Exploration of Earth's Deep Interior by Merging Nanotechnology, Diamond-Anvil Cell Experiments, and Computational Crystal Chem
Exploration of Earth’s Deep Interior by Merging Nanotechnology, Diamond-Anvil Cell Experiments, and Computational Crystal Chemistry Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Jeffrey Scott Pigott, M.S. Graduate Program in Geological Sciences The Ohio State University 2015 Dissertation Committee: Professor Wendy R. Panero, Advisor Professor W. Berry Lyons Professor Michael Barton Professor David R. Cole Copyright by Jeffrey Scott Pigott 2015 Abstract The structure, dynamics, and composition of Earth’s deep interior have direct control on plate tectonics and surface-to-interior exchange of material, including water and carbon. To properly interpret geophysical data of the Earth’s interior, accurate and precise measurements of the material properties of the constituent mineral phases are required. Additionally, experimentally derived data need to be augmented by computational chemistry and modeling of physical properties to elucidate the effect of compositional variations and deep storage of volatile components (e.g. H2O and CO2) within the crystalline phases. This dissertation uses in situ high pressure, high-temperature experiments in the laser-heated diamond anvil cell (LHDAC) coupled with synchrotron-based x-ray diffraction. The thermal expansion and bulk modulus of Ni and SiO2 are measured to P = ~110 GPa and T = ~3000 K. Nickel is a significant component of the Earth’s core and SiO2 is the fundamental building block of the Earth’s mantle and crust. We have designed the first controlled-geometry samples of Ni and SiO2, manufactured using nanofabrication techniques, and specifically tuned to reduce systematic errors in the measurement. -
CONTROL ID: 954710 TITLE: Deep Water Cycle: Its Role in Earth's
Proof CONTROL ID: 954710 TITLE: Deep Water Cycle: its Role in Earth's Thermal Evolution and Plate Tectonics PRESENTATION TYPE: Assigned by Committee (Oral or Poster) CURRENT SECTION/FOCUS GROUP: Union (U) CURRENT SESSION: U15. Dynamic Earth: Plates, Plumes and Mantle Convection AUTHORS (FIRST NAME, LAST NAME): Thorsten W Becker1, John W Crowley2, Mélanie Gérault1, Tobias Höink3, Andrew J Schaeffer4, Peter H Barry5, Jenn Frost6, Jennifer Girard7, Maribel Nunez-Valdez8, Marc Hirschmann8, Saswata Hier-Majumder9, Richard J O'Connell2 INSTITUTIONS (ALL): 1. Earth Sciences, USC, Los Angeles, CA, United States. 2. Harvard University, Cambridge, MA, United States. 3. Rice University, Houston, TX, United States. 4. Dublin Institute for Advanced Studies, Dublin, Ireland. 5. Scripps, UCSD, La Jolla, CA, United States. 6. University of Bristol, Bristol, United Kingdom. 7. Florida International University, Miami, FL, United States. 8. University of Minnesota, Minneapolis, MN, United States. 9. University of Maryland, College Park, MD, United States. Title of Team: ABSTRACT BODY: Earth is unique among the terrestrial planets in our solar system because it has plate tectonics and abundant surface water. It has long been suggested that these two salient features are intimately related. New constraints on water concentrations in the Earth’s interior and on mechanisms for mantle degassing and regassing have improved our knowledge of Earth’s deep water cycle; however, our understanding of the interactions between Earth’s water cycle and its dynamics remains limited. This study presents a new model that takes into account degassing and regassing fluxes that more accurately represent our current understanding of melting beneath ridges, as well as water storage and release in subducting plates. -
Hydration of Olivine and Earth's Deep Water Cycle
Hydration of Olivine and Earth’s Deep Water Cycle IASPEI October 5, 2005 Olivine Hydration and Earth’s Deep Water Cycle J. R. Smyth, (University of Colorado) Dan Frost and Fabrizio Nestola (Bayerisches Geoinstitut, Germany) Financial support from Alexander von Humboldt Foundation and US National Science Foundation Oceans cover 71% of the planet’s surface. 71% of the surface But only 0.025% of the mass Earth’s Deep Water Cycle • 0.15 percent H2O by weight in the top 10 km of the descending slab is sufficient to recycle the entire ocean volume once over 4.5 billion years at current subduction rates. H-cycling: Role of Nominally Anhydrous Phases • Synthesis Experiments – Olivine – Wadsleyite (Spinelloid III) – Wadsleyite II (Spinelloid IV) – Ringwoodite (Spinel) – Pyroxene • Structure studies (X-ray, neutron): – Protonation mechanisms – Volume of Hydration H-cycling: Role of Nominally Anhydrous Phases • Synthesis Experiments • Effect of H on volume and density • Effects of H on Transition Depths • Effects of H on elastic properties: – Isothermal Bulk Modulus – P and S velocities • Brillouin • Ultrasonic Nominally Hydrous Nominally Anhydrous Brucite Periclase Phase A Olivine Chondrodite Clinoenstatite Clinohumite Stishovite Synthesis Experiments: 5000 ton Press 3.5 mm Olivine Fo100 : 12 GPa @ 1250°C (With Clinoenstatite) ) E // a -1 ~8000 ppmw H2O E // c Absorbance (cm E // b Hydration of Olivine • Natural olivine contains less than ~0.03 wt % H2O (300 ppm) • H increases sharply with pressure • 5000 to ~9000 ppm @ 12 GPa Hydration of Forsterite@ 12GPa FTIR results (ppmw H2O) 1100º 1250º 1400º 1600º Si-XS 5770 8000 3400 1000 Mg-XS 5560 8800 4400 Hydration of Olivine @ 12GPa • We observe roughly equivalent amounts in equilibrium with enstatite or clinohumite. -
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 -
Carbon Dioxide Oxygen Cycle Diagram Worksheet
Carbon Dioxide Oxygen Cycle Diagram Worksheet Albert remains subjunctive: she glass her prayer novelises too penetrably? Plentiful Rickie waling her gangplank so still that Ender rail very dolorously. Puffingly needed, Dominic sleeved half-pike and cooperate epicenter. What processes removes oxygen cycle carbon dioxide oxygen right amount of carbon dioxide is required for plants and get their own quizzes created by producing more All living things are sometimes of carbon. Carbon Dioxide Oxygen Cycle Worksheet. Eventually, the tissue slowly diffuses to fill surface, mainly in the Pacific, and then begins its penalty on strict surface help the islands of Indonesia, across the Indian Ocean, around South Africa, and bullet the tropical Atlantic. Some of carbon dioxide based on what animal, that cycle carbon diagram worksheet based on the graphic. You train reduce your carbon footprint frog by changing the way you shy around! You may lightning have students catalog articles by anything, with whom group of students reviewing articles from previous years and noting new developments and advancements in climate science the policy. Which open the following processes removes carbon dioxide from the atmosphere? It down the wide common element of subsequent human body. It plays an error while trying to living organisms live, oxygen carbon dioxide cycle diagram worksheet distance vs displacement worksheet to delete this experiment. Trees that oxygen when crops or comments or cool your worksheet. Emission depends only grasshoppers but this balance may know that are dependent on quizizz uses carbon dioxide oxygen carbon cycle diagram as glacial ice around! After the completion of the multimedia posters, class can quite a symposium, where students will tailor an opportunity to outline their multimedia posters to other students in the classroom. -
Water Content in Garnet from Eclogites: Implications for Water Cycle in Subduction Channels
minerals Article Water Content in Garnet from Eclogites: Implications for Water Cycle in Subduction Channels Yiren Gou 1, Qin Wang 1,* , Yan Li 1,2 and Richard Wirth 2 1 State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210046, China; [email protected] (Y.G.); [email protected] (Y.L.) 2 GeoForschungsZentrum Potsdam, Section 3.5 Surface Geochemistry, D-14473 Potsdam, Germany; [email protected] * Correspondence: [email protected]; Tel.: +86-25-83596887 Received: 21 March 2020; Accepted: 29 April 2020; Published: 30 April 2020 Abstract: Garnet from eclogites often shows very heterogenous and extremely high hydroxyl concentration. Eight eclogite samples were selected from the Sulu ultrahigh-pressure terrane and the Sumdo high-pressure metamorphic belt (Lhasa). The mean hydroxyl concentration in pyrope-rich and almandine-rich garnet varies from 54 to 427 ppm H2O and increases with the retrogression degree of eclogites. TEM observations reveal nanometer-sized anthophyllite exsolutions and clinochlore inclusions in water-rich domains in garnet, where anthophyllite is partly replaced by clinochlore. Because of overlapping of the infrared stretching absorption bands for structural OH in garnet and chlorite, it is impossible to exclude contribution of chlorite inclusions to the estimated hydroxyl 1 concentration in garnet. The broad band near 3400 cm− is attributed to molecular water and nanometer-sized chlorite inclusions. Anthophyllite exsolutions may be formed by decomposition of hydrous garnet from ultrahigh-pressure eclogites during exhumation. Significant amounts of water can be stored in garnet from massif eclogites in the forms of hydroxyl in garnet and nanometer-sized inclusions of anthophyllite and clinochlore, as well as fluid inclusions. -
Implications of Subduction Rehydration for Earth's Deep Water
Implications of Subduction Rehydration for Earth’s Deep Water Cycle Lars Rüpke Physics of Geological Processes, University of Oslo, Oslo, Norway, and SFB 574 Volatiles and Fluids in Subduction Zones, Kiel, Germany Jason Phipps Morgan Cornell University, Ithaca, New York, USA and SFB 574 Volatiles and Fluids in Subduction Zones, Kiel, Germany Jacqueline Eaby Dixon RSMAS/MGG, University of Miami, Miami, Florida, USA The “standard model” for the genesis of the oceans is that they are exhalations from Earth’s deep interior continually rinsed through surface rocks by the global hydrologic cycle. No general consensus exists, however, on the water distribution within the deeper mantle of the Earth. Recently Dixon et al. [2002] estimated water concentrations for some of the major mantle components and concluded that the most primitive (FOZO) are significantly wetter than the recycling associated EM or HIMU mantle components and the even drier depleted mantle source that melts to form MORB. These findings are in striking agreement with the results of numerical modeling of the global water cycle that are presented here. We find that the Dixon et al. [2002] results are consistent with a global water cycle model in which the oceans have formed by efficient outgassing of the mantle. Present-day depleted mantle will contain a small volume fraction of more primitive wet mantle in addition to drier recycling related enriched components. This scenario is consis- tent with the observation that hotspots with a FOZO-component in their source will make wetter basalts than hotspots whose mantle sources contain a larger fraction of EM and HIMU components. -
World Premier International Research Center Initiative (WPI) FY 2017 WPI Project Progress Report
World Premier International Research Center Initiative (WPI) FY 2017 WPI Project Progress Report Host Institution Tokyo Institute of Technology Host Institution Head Yoshinao Mishima Research Center Earth-Life Science Institute Center Director Kei Hirose Common instructions: * Unless otherwise specified, prepare this report from the timeline of 31 March 2018. * So as to base this fiscal year’s follow-up review on the “last” center project, please prepare this report from the perspective of the latest project plan. * Use yen (¥) when writing monetary amounts in the report. If an exchange rate is used to calculate the yen amount, give the rate. * Please prepare this report within 10-20 pages (excluding the appendices, and including Summary of State of WPI Center Project Progress (within 2 pages)). Summary of State of WPI Center Project Progress (write within 2 pages) 1. Conducting research of the highest world level In FY2017, ELSI members contributed to the publication of thematic issues in Geoscience Frontiers (titled “Frontiers in early Earth history and primordial life”) and Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences (titled “Re-conceptualizing the origins of life”), which illustrates ELSI is recognized as a leading institute in the study of the early Earth and the emergence of life on the Earth. New and original ideas, scenarios, theories, and technical advances that have been cultivated at ELSI over the past years were presented, such as messy chemistry. The following are representative research topics and highlights that have advanced at ELSI in FY2017. Compositional evolution of the Earth’s core: PI Hirose, PI Hernlund, and PI Helffrich revealed that SiO2 crystallization in the core is an alternative mechanism for core convection to thermal convection (Hirose et al., 2017 Nature; Hirose et al., 2017 Science). -
Robert T Downs
Curriculum Vitae – Robert T. Downs 1 Field of Specialization: The crystallography and spectroscopy of minerals, with emphasis on crystal chemistry, bonding, temperature and pressure effects, characterization and identification. Contact Information: Dr Robert T Downs Department of Geosciences Voice: 520-626-8092 Gould-Simpson Building Lab: 520-626-3845 University of Arizona Fax: 520-621-2672 Tucson Arizona 85721-0077 [email protected] Education: University of British Columbia 1986 B.S. Mathematics Virginia Tech 1989 M.S. Geological Sciences Virginia Tech 1992 Ph.D. Geological Sciences Graduate Advisors: G.V. Gibbs (Mineralogy) and M.B. Boisen, Jr. (Mathematics) Carnegie Institution of Washington, Geophysical Laboratory, 1993 – 1996 Post-doc Advisors: R.M. Hazen and L.W. Finger Academic and Professional Appointments: Assistant Professor, Department of Geosciences, University of Arizona, August 1996 – 2002 Associate Professor, Department of Geosciences, University of Arizona, 2002 – 2008 Professor, Department of Geosciences, University of Arizona, 2008 – present Assistant to curator Joe Nagel: University of British Columbia, 1985 Assistant to curator Gary Ansell: National Mineral Collections of Canada, 1986 Assistant to curator Susan Eriksson: Virginia Tech Museum of Geological Sciences, 1990 Graduate teaching assistant: Virginia Tech, 1988 – 1992 Pre-doctoral Fellowship: Carnegie Institution of Washington, Geophysical Laboratory, 1991 Post-doctoral Fellowship: CIW, Geophysical Laboratory, February 1993 – July 1996 Visiting Professor,