Abstracts from the Fifth European Workshop on Astrobiology EANA
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(2016), Volume 4, Issue 2, 77-90
ISSN 2320-5407 International Journal of Advanced Research (2016), Volume 4, Issue 2, 77-90 Journal homepage: http://www.journalijar.com INTERNATIONAL JOURNAL OF ADVANCED RESEARCH RESEARCH ARTICLE LICHENOMETRIC DATING CURVE AS APPLIED TO GLACIER RETREAT STUDIES IN THE HIMALAYAS. Gaurav K. Mishra, Santosh Joshi and Dalip K. Upreti. Lichenology Laboratory, CSIR-National Botanical Research Institute, Rana Pratap Marg, Lucknow- 226001. Manuscript Info Abstract Manuscript History: The study critically favours the importance of lichens in estimating palaeoclimatic events and its use in depicting the future discretion regarding Received: 14 December 2015 Final Accepted: 19 January 2016 glacier retreat. Besides the various lichenometric studies carried out in Indian Published Online: February 2016 Himalayan region, the world-wide classical work of different glaciologist and geologist on different applications of lichenometry is also well focused. Key words: The study also highlights the benefits, restrains, and drawbacks associated Lichens, lichenometry,glacier with the lichenometry. Being a globally accepted biological technique retreat,India. particular emphasis is given on the need of innovative approach in implementation of lichenometry in Indian Himalayan region. *Corresponding Author Gaurav K. Mishra. Copy Right, IJAR, 2016,. All rights reserved. Introduction:- Lichens are slow growing organisms and take several years to get established in nature. Lichens are a unique group of plants, comprising of two micro-organisms, fungus (mycobiont), an organism capable of producing food via photosynthesis and alga (photobiont). These photobionts are predominantly members of the chlorophyta (green algae) or cynophyta (blue-green algae or cynobacteria). The peculiar nature of lichens enables them to colonize variety of substrate like rock, boulders, bark, soil, leaf and man-made buildings. -
Can Parietin Transfer Energy Radiatively to Photosynthetic Pigments?
molecules Communication Can Parietin Transfer Energy Radiatively to Photosynthetic Pigments? Beatriz Fernández-Marín 1, Unai Artetxe 1, José María Becerril 1, Javier Martínez-Abaigar 2, Encarnación Núñez-Olivera 2 and José Ignacio García-Plazaola 1,* ID 1 Department Plant Biology and Ecology, University of the Basque Country (UPV/EHU), 48940 Leioa, Spain; [email protected] (B.F.-M.); [email protected] (U.A.); [email protected] (J.M.B.) 2 Faculty of Science and Technology, University of La Rioja (UR), 26006 Logroño (La Rioja), Spain; [email protected] (J.M.-A.); [email protected] (E.N.-O.) * Correspondence: [email protected]; Tel.: +34-94-6015319 Received: 22 June 2018; Accepted: 16 July 2018; Published: 17 July 2018 Abstract: The main role of lichen anthraquinones is in protection against biotic and abiotic stresses, such as UV radiation. These compounds are frequently deposited as crystals outside the fungal hyphae and most of them emit visible fluorescence when excited by UV. We wondered whether the conversion of UV into visible fluorescence might be photosynthetically used by the photobiont, thereby converting UV into useful energy. To address this question, thalli of Xanthoria parietina were used as a model system. In this species the anthraquinone parietin accumulates in the outer upper cortex, conferring the species its characteristic yellow-orange colouration. In ethanol, parietin absorbed strongly in the blue and UV-B and emitted fluorescence in the range 480–540 nm, which partially matches with the absorption spectra of photosynthetic pigments. In intact thalli, it was determined by confocal microscopy that fluorescence emission spectra shifted 90 nm towards longer wavelengths. -
Viability of the Lichen Xanthoria Elegans and Its Symbionts After 18 Months of Space Exposure and Simulated Mars Conditions on the ISS
International Journal of Astrobiology 14 (3): 411–425 (2015) doi:10.1017/S1473550414000214 © Cambridge University Press 2014 Viability of the lichen Xanthoria elegans and its symbionts after 18 months of space exposure and simulated Mars conditions on the ISS Annette Brandt1, Jean-Pierre de Vera2, Silvano Onofri3 and Sieglinde Ott1 1Institute of Botany, Heinrich-Heine-University, Universitätsstr. 1, 40225 Düsseldorf, Germany 2Institute of Planetary Research, German Aerospace Center (DLR), Rutherfordstr. 2, 12489 Berlin, Germany 3Department of Ecological and Biological Sciences (DEB), Tuscia University, Largo dell’Università, 01100 Viterbo, Italy e-mail: [email protected] Abstract: The lichen Xanthoria elegans has been exposed to space conditions and simulated Mars-analogue conditions in the lichen and fungi experiment (LIFE) on the International Space Station (ISS). After several simulations and short space exposure experiments such as BIOPAN, this was the first long-term exposure of eukaryotic organisms to the hostile space conditions of the low Earth orbit (LEO). The biological samples were integrated in the EXPOSE-E facility and exposed for 1.5 years outside the ISS to the combined impact of insolation, ultraviolet (UV)-irradiation, cosmic radiation, temperatures and vacuum conditions of LEO space. Additionally, a subset of X. elegans samples was exposed to simulated Martian environmental conditions by applying Mars-analogue atmosphere and suitable solar radiation filters. After their return to Earth the viability of the lichen samples was ascertained by viability analysis of LIVE/DEAD staining and confocal laser-scanning microscopy, but also by analyses of chlorophyll a fluorescence. According to the LIVE/DEAD staining results, the lichen photobiont showed an average viability rate of 71%, whereas the even more resistant lichen mycobiont showed a rate of 84%. -
Esa Publications
number 172 | 4th quarter 2017 bulletin → united space in europe European Space Agency The European Space Agency was formed out of, and took over the rights and The ESA headquarters are in Paris. obligations of, the two earlier European space organisations – the European Space Research Organisation (ESRO) and the European Launcher Development The major establishments of ESA are: Organisation (ELDO). The Member States are Austria, Belgium, Czech Republic, Denmark, Estonia, Finland, France, Germany, Greece, Hungary, Ireland, Italy, ESTEC, Noordwijk, Netherlands. Luxembourg, the Netherlands, Norway, Poland, Portugal, Romania, Spain, Sweden, Switzerland and the United Kingdom. Slovenia is an Associate Member. Canada ESOC, Darmstadt, Germany. takes part in some projects under a cooperation agreement. Bulgaria, Cyprus, Malta, Latvia, Lithuania and Slovakia have cooperation agreements with ESA. ESRIN, Frascati, Italy. ESAC, Madrid, Spain. In the words of its Convention: the purpose of the Agency shall be to provide for and to promote, for exclusively peaceful purposes, cooperation among European EAC, Cologne, Germany. States in space research and technology and their space applications, with a view to their being used for scientific purposes and for operational space applications ECSAT, Harwell, United Kingdom. systems: ESEC, Redu, Belgium. → by elaborating and implementing a long-term European space policy, by recommending space objectives to the Member States, and by concerting the policies of the Member States with respect to other national -
Molecular Phylogenetic Study at the Generic Boundary Between the Lichen-Forming Fungi Caloplaca and Xanthoria (Ascomycota, Teloschistaceae)
Mycol. Res. 107 (11): 1266–1276 (November 2003). f The British Mycological Society 1266 DOI: 10.1017/S0953756203008529 Printed in the United Kingdom. Molecular phylogenetic study at the generic boundary between the lichen-forming fungi Caloplaca and Xanthoria (Ascomycota, Teloschistaceae) Ulrik SØCHTING1 and Franc¸ ois LUTZONI2 1 Department of Mycology, Botanical Institute, University of Copenhagen, O. Farimagsgade 2D, DK-1353 Copenhagen K, Denmark. 2 Department of Biology, Duke University, Durham, NC 27708-0338, USA. E-mail : [email protected] Received 5 December 2001; accepted 5 August 2003. A molecular phylogenetic analysis of rDNA was performed for seven Caloplaca, seven Xanthoria, one Fulgensia and five outgroup species. Phylogenetic hypotheses are constructed based on nuclear small and large subunit rDNA, separately and in combination. Three strongly supported major monophyletic groups were revealed within the Teloschistaceae. One group represents the Xanthoria fallax-group. The second group includes three subgroups: (1) X. parietina and X. elegans; (2) basal placodioid Caloplaca species followed by speciations leading to X. polycarpa and X. candelaria; and (3) a mixture of placodioid and endolithic Caloplaca species. The third main monophyletic group represents a heterogeneous assemblage of Caloplaca and Fulgensia species with a drastically different metabolite content. We report here that the two genera Caloplaca and Xanthoria, as well as the subgenus Gasparrinia, are all polyphyletic. The taxonomic significance of thallus morphology in Teloschistaceae and the current delimitation of the genus Xanthoria is discussed in light of these results. INTRODUCTION Taxonomy of Teloschistaceae and its genera The Teloschistaceae is a well-delimited family of Hawksworth & Eriksson (1986) assigned the Teloschis- lichenized fungi. -
A Critique of Phanerozoic Climatic Models Involving Changes in The
Earth-Science Reviews 56Ž. 2001 1–159 www.elsevier.comrlocaterearscirev A critique of Phanerozoic climatic models involving changes in the CO2 content of the atmosphere A.J. Boucot a,), Jane Gray b,1 a Department of Zoology, Oregon State UniÕersity, CorÕallis, OR 97331, USA b Department of Biology, UniÕersity of Oregon, Eugene, OR 97403, USA Received 28 April 1998; accepted 19 April 2001 Abstract Critical consideration of varied Phanerozoic climatic models, and comparison of them against Phanerozoic global climatic gradients revealed by a compilation of Cambrian through Miocene climatically sensitive sedimentsŽ evaporites, coals, tillites, lateritic soils, bauxites, calcretes, etc.. suggests that the previously postulated climatic models do not satisfactorily account for the geological information. Nor do many climatic conclusions based on botanical data stand up very well when examined critically. Although this account does not deal directly with global biogeographic information, another powerful source of climatic information, we have tried to incorporate such data into our thinking wherever possible, particularly in the earlier Paleozoic. In view of the excellent correlation between CO2 present in Antarctic ice cores, going back some hundreds of thousands of years, and global climatic gradient, one wonders whether or not the commonly postulated Phanerozoic connection between atmospheric CO2 and global climatic gradient is more coincidence than cause and effect. Many models have been proposed that attempt to determine atmospheric composition and global temperature through geological time, particularly for the Phanerozoic or significant portions of it. Many models assume a positive correlation between atmospheric CO2 and surface temperature, thus viewing changes in atmospheric CO2 as playing the critical role in r regulating climate temperature, but none agree on the levels of atmospheric CO2 through time. -
Lichen Life in Antarctica a Review on Growth and Environmental Adaptations of Lichens in Antarctica
Lichen Life in Antarctica A review on growth and environmental adaptations of lichens in Antarctica Individual Project for ANTA 504 for GCAS 08/09 Lorna Little Contents Antarctic Vegetation ...............................................................................................................................3 The Basics of Lichen Life .........................................................................................................................4 Environmental Influences .......................................................................................................................7 Nutrients .............................................................................................................................................7 Water Relations and Temperature .....................................................................................................7 UV‐B Radiation and Climate Change Effects.......................................................................................8 Variations in Lichen Growth and Colonisation......................................................................................10 Growth rate.......................................................................................................................................10 Case Studies of Antarctic Lichens .....................................................................................................13 Colonisation ......................................................................................................................................15 -
18Th EANA Conference European Astrobiology Network Association
18th EANA Conference European Astrobiology Network Association Abstract book 24-28 September 2018 Freie Universität Berlin, Germany Sponsors: Detectability of biosignatures in martian sedimentary systems A. H. Stevens1, A. McDonald2, and C. S. Cockell1 (1) UK Centre for Astrobiology, University of Edinburgh, UK ([email protected]) (2) Bioimaging Facility, School of Engineering, University of Edinburgh, UK Presentation: Tuesday 12:45-13:00 Session: Traces of life, biosignatures, life detection Abstract: Some of the most promising potential sampling sites for astrobiology are the numerous sedimentary areas on Mars such as those explored by MSL. As sedimentary systems have a high relative likelihood to have been habitable in the past and are known on Earth to preserve biosignatures well, the remains of martian sedimentary systems are an attractive target for exploration, for example by sample return caching rovers [1]. To learn how best to look for evidence of life in these environments, we must carefully understand their context. While recent measurements have raised the upper limit for organic carbon measured in martian sediments [2], our exploration to date shows no evidence for a terrestrial-like biosphere on Mars. We used an analogue of a martian mudstone (Y-Mars[3]) to investigate how best to look for biosignatures in martian sedimentary environments. The mudstone was inoculated with a relevant microbial community and cultured over several months under martian conditions to select for the most Mars-relevant microbes. We sequenced the microbial community over a number of transfers to try and understand what types microbes might be expected to exist in these environments and assess whether they might leave behind any specific biosignatures. -
Lichens of Alaska's South Coast
Lichens of Alaska’s South Coast United States Forest Service R10-RG-190 Department of Alaska Region July 2011 Agriculture WHAT IS A LICHEN? Lichens are specialized fungi that “farm” algae as a food source. Unlike molds, mildews, and mushrooms that parasi ze or scavenge food from other organisms, the fungus of a lichen cul vates ny algae and / or blue-green bacteria (called cyanobacteria) within the fabric of interwoven fungal threads that form the body of the lichen (or thallus). The algae and cyanobacteria produce food for themselves and for the fungus by conver ng carbon dioxide and water into sugars using the sun’s energy (photosynthesis). Thus, a lichen is a combina on of two or some mes three organisms living together. Perhaps the most important contribu on of the fungus is to provide a protec ve habitat for the algae or cyanobacteria. The green or blue-green photosynthe c layer is o en visible between two white fungal layers if a piece of lichen thallus is torn off . Most lichen-forming fungi cannot exist without the photosynthe c partner because they have become dependent on them for survival. But in all cases, a fungus looks quite diff erent in the lichenized form compared to its free-living form. HOW DO LICHENS REPRODUCE? Lichens sexually reproduce with frui ng bodies of various shapes and colors that can o en look like miniature mushrooms. These are called apothecia (Fig. 1) and contain spores that germinate and Figure 1. Apothecia, fruiting grow into the fungus. Each bodies fungus must fi nd the right photosynthe c partner in order to become a lichen. -
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 -
Further Investigations on Rhizocarpon of North-Eastern Iran: R
Hindawi Publishing Corporation Journal of Mycology Volume 2014, Article ID 528041, 5 pages http://dx.doi.org/10.1155/2014/528041 Research Article Further Investigations on Rhizocarpon of North-Eastern Iran: R. geographicum Mahroo Haji Moniri Department of Biology, Faculty of Sciences, Islamic Azad University, Mashhad Branch, Mashhad 917 56 89 119, Iran Correspondence should be addressed to Mahroo Haji Moniri; h [email protected] Received 15 January 2014; Accepted 7 April 2014; Published 29 April 2014 Academic Editor: Simona Nardoni Copyright © 2014 Mahroo Haji Moniri. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Morphology, anatomy, secondary chemistry, ecology, and distribution of Rhizocarpon geographicum (Rhizocarpaceae, lichenized Ascomycota) in north-eastern Iran are investigated and discussed. 1. Introduction the elevation of the sites ranges from 1340 to 1880 m. Over 537 Rhizocarpon thalli were investigated of which 311 (58%) Iran has an exceptional variety of biomes which has resulted belong to R. geographicum. As a result much new information in an extensive diversity in many organism groups including became available on the species of Rhizocarpon [11–13]. Mor- lichens. The history of lichenological exploration in north- phological and anatomical characteristics of the thalli and eastern Iran is fairly extensive, dating back to the middle fruiting bodies were examined with a stereomicroscope and a of the twentieth century [1, 2]. Since 2004, however, the light microscope. Preparations were made in distilled water, investigations in the present Khorasan provinces have much 10% KOH and KI. -
Apollo 17 Index: 70 Mm, 35 Mm, and 16 Mm Photographs
General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Center for Aerospace Information (CASI) Preparation, Scanning, Editing, and Conversion to Adobe Portable Document Format (PDF) by: Ronald A. Wells University of California Berkeley, CA 94720 May 2000 A P O L L O 1 7 I N D E X 7 0 m m, 3 5 m m, A N D 1 6 m m P H O T O G R A P H S M a p p i n g S c i e n c e s B r a n c h N a t i o n a l A e r o n a u t i c s a n d S p a c e A d m i n i s t r a t i o n J o h n s o n S p a c e C e n t e r H o u s t o n, T e x a s APPROVED: Michael C .