The Resolved Mystery of Tardigrades
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Diversity of Bacteria and Archaea in the Deep-Sea Low-Temperature Hydrothermal Sulfide Chimney of the Northeastern Pacific Ocean
African Journal of Biotechnology Vol. 11(2), pp. 337-345, 5 January, 2012 Available online at http://www.academicjournals.org/AJB DOI: 10.5897/AJB11.2692 ISSN 1684–5315 © 2012 Academic Journals Full Length Research Paper Diversity of bacteria and archaea in the deep-sea low-temperature hydrothermal sulfide chimney of the Northeastern Pacific Ocean Xia Ding1*, Xiao-Jue Peng1#, Xiao-Tong Peng2 and Huai-Yang Zhou3 1College of Life Sciences and Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, Nanchang University, Nanchang 330031, China. 2Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China. 3National Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China. Accepted 4 November, 2011 Our knowledge of the diversity and role of hydrothermal vents microorganisms has considerably expanded over the past decade, while little is known about the diversity of microorganisms in low-temperature hydrothermal sulfide chimney. In this study, denaturing gradient gel electrophoresis (DGGE) and 16S rDNA sequencing were used to examine the abundance and diversity of microorganisms from the exterior to the interior of the deep sea low-temperature hydrothermal sulfide chimney of the Northeastern Pacific Ocean. DGGE profiles revealed that both bacteria and archaea could be examined in all three zones of the chimney wall and the compositions of microbial communities within different zones were vastly different. Overall, for archaea, cell abundance was greatest in the outermost zone of the chimney wall. For bacteria, there was no significant difference in cell abundance among three zones. In addition, phylogenetic analysis revealed that Verrucomicrobia and Deltaproteobacteria were the predominant bacterial members in exterior zone, beta Proteobacteria were the dominant members in middle zone, and Bacillus were the abundant microorganisms in interior zone. -
Where Less May Be More: How the Rare Biosphere Pulls Ecosystems Strings
The ISME Journal (2017) 11, 853–862 OPEN © 2017 International Society for Microbial Ecology All rights reserved 1751-7362/17 www.nature.com/ismej MINI REVIEW Where less may be more: how the rare biosphere pulls ecosystems strings Alexandre Jousset1, Christina Bienhold2,3, Antonis Chatzinotas4,5, Laure Gallien6,7, Angélique Gobet8, Viola Kurm9, Kirsten Küsel10,5, Matthias C Rillig11,12, Damian W Rivett13, Joana F Salles14, Marcel GA van der Heijden15,16,17, Noha H Youssef18, Xiaowei Zhang19, Zhong Wei20 and WH Gera Hol9 1Utrecht University, Department of Biology, Institute of Environmental Biology, Ecology and Biodiversity Group, Utrecht, The Netherlands; 2Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; 3Max Planck Institute for Marine Microbiology, Bremen, Germany; 4Helmholtz Centre for Environmental Research – UFZ, Leipzig, Germany; 5German Centre for Integrative Biodiversity Research (iDiv), Halle-Jena-Leipzig, Leipzig, Germany; 6Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, Switzerland; 7Center for Invasion Biology, Department of Botany & Zoology, Stellenbosch University, Matieland, South Africa; 8Sorbonne Universités, UPMC Université Paris 06, CNRS, UMR 8227, Integrative Biology of Marine Models, Station Biologique de Roscoff, F-29688, Roscoff Cedex, France; 9Netherlands Institute of Ecology, Department of Terrestrial Ecology, Wageningen, The Netherlands; 10Friedrich Schiller University Jena, Institute of Ecology, Jena, Germany; 11Freie Universtät Berlin, -
Experimental and Statistical Analysis of Nutritional Requirements for the Growth of the Extremophile Deinococcus Geothermalis DSM 11300
Experimental and statistical analysis of nutritional requirements for the growth of the extremophile Deinococcus geothermalis DSM 11300 Julie Bornot, Cesar Arturo Aceves-Lara, Carole Molina-Jouve, Jean-Louis Uribelarrea, Nathalie Gorret To cite this version: Julie Bornot, Cesar Arturo Aceves-Lara, Carole Molina-Jouve, Jean-Louis Uribelarrea, Nathalie Gor- ret. Experimental and statistical analysis of nutritional requirements for the growth of the ex- tremophile Deinococcus geothermalis DSM 11300. Extremophiles, Springer Verlag, 2014, 18 (6), pp.1009-1021. 10.1007/s00792-014-0671-8. hal-01268947 HAL Id: hal-01268947 https://hal.archives-ouvertes.fr/hal-01268947 Submitted on 11 Mar 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. OATAO is an open access repository that collects the work of Toulouse researchers and makes it freely available over the web where possible This is an author’s version published in: http://oatao.univ-toulouse.fr/22999 Official URL: https://doi.org/10.1007/s00792-014-0671-8 To cite this version: Bornot, Julie and Aceves-Lara, César-Arturo and Molina-Jouve, Carole and Uribelarrea, Jean-Louis and Gorret, Nathalie Experimental and statistical analysis of nutritional requirements for the growth of the extremophile Deinococcus geothermalis DSM 11300. -
FORMATION of HABITABLE WORLDS and FATE of HABITABLE ENVIRONMENTS 6:00 P.M
45th Lunar and Planetary Science Conference (2014) sess726.pdf Thursday, March 20, 2014 [R726] POSTER SESSION: FORMATION OF HABITABLE WORLDS AND FATE OF HABITABLE ENVIRONMENTS 6:00 p.m. Town Center Exhibit Area Johnson T. A. Park A. Hand K. P. POSTER LOCATION #473 The Workman-Reynolds Effect: An Investigation of the Ice-Water Interface of Dilute Salt Solutions [#1672] We report on experiments on the voltage potential that results from rapidly freezing dilute aqueous solutions. These results have application to icy satellites. Taylor A. R. Olsen A. A. Hausrath E. M. POSTER LOCATION #474 Serpentinite Dissolution: An Analog to Mantle-Ocean Interaction on Europa [#1903] Laboratory-based dissolution experiments between serpentinite rock and a variety of acids represent mantle-ocean interaction on the jovian moon, Europa. Hausrath E. M. Adcock C. T. Elwood Madden M. E. Gainey S. R. Olsen A. A. et al. POSTER LOCATION #475 Using Geochemical Kinetics to Interpret Potential Habitability [#2376] Geochemical kinetics can help shed light on factors affecting habitability, including water, release of nutrients, redox, pH, temperature, and ionic strength. Som S. M. Fristad K. E. Hoehler T. M. POSTER LOCATION #476 An Integrative Approach to Assessing Habitability of H2 Metabolisms in Hydrothermal Springs [#2828] We present an ongoing project that surveys H2 from springs sourced in rocks of varying silica content and in parallel investigate habitability numerically. Djordjevic S. Mickol R. L. Kral T. A. POSTER LOCATION #477 Simulating Martian Conditions: Methanogen Survivability During Freeze-Thaw Cycles [#2539] Methanogens are obligate anaerobes that tolerate a wide range of conditions. It is proposed that these Archaea are able to persist in a martian environment. -
Science and Innovation: the Under-Fueled Engine of Prosperity
Science and Innovation: The Under-Fueled Engine of Prosperity JULY 14, 2021 AUTHOR Benjamin F. Jones* ABSTRACT Science and innovation are central to human progress and national economic success. Currently, the United States invests 2.8% of GDP in research and development, which is supported by a range of public policies. This paper asks whether the United States invests enough. To answer that question, the conceptual case for government intervention and skepticism about that case are reviewed. The paper then turns to systematic evidence, including the very latest evidence, regarding the operation of the science and innovation system and its social returns. This evidence suggests a clear answer: We massively underinvest in science and innovation, with implications for our standards of living, health, national competitiveness, and capacity to respond to crisis. * Kellogg School of Management and National Bureau of Economic Research. Email: [email protected]. 1. Introduction Scientific and technological advances have long been recognized as engines of economic growth and rising prosperity. The fruits of these advances—instantaneous global communications, vaccines, airplanes, heart surgery, computers, skyscrapers, industrial robots, on-demand entertainment, to name a few—might seem almost magical to our ancestors from not-too-many generations ago. The power of this progress has been broadly evident since the Industrial Revolution and was recognized at the time, including by political leaders. As the British Prime Minister Benjamin Disraeli noted in 1873, “How much has happened in these fifty years … I am thinking of those revolutions of science which … have changed the position and prospects of mankind more than all the conquests and all the codes and all the legislators that ever lived.” Disraeli was talking of things like the steam engine, the telegraph, and textile manufacturing. -
Arxiv.Org | Cornell University Library, July, 2019. 1
arXiv.org | Cornell University Library, July, 2019. Extremophiles: a special or general case in the search for extra-terrestrial life? Ian von Hegner Aarhus University Abstract Since time immemorial life has been viewed as fragile, yet over the past few decades it has been found that many extreme environments are inhabited by organisms known as extremophiles. Knowledge of their emergence, adaptability, and limitations seems to provide a guideline for the search of extra-terrestrial life, since some extremophiles presumably can survive in extreme environments such as Mars, Europa, and Enceladus. Due to physico-chemical constraints, the first life necessarily came into existence at the lower limit of it‟s conceivable complexity. Thus, the first life could not have been an extremophile, furthermore, since biological evolution occurs over time, then the dual knowledge regarding what specific extremophiles are capable of, and to the analogue environment on extreme worlds, will not be sufficient as a search criterion. This is because, even though an extremophile can live in an extreme environment here-and-now, its ancestor however could not live in that very same environment in the past, which means that no contemporary extremophiles exist in that environment. Furthermore, a theoretical framework should be able to predict whether extremophiles can be considered a special or general case in the galaxy. Thus, a question is raised: does Earth‟s continuous habitability represent an extreme or average value for planets? Thus, dependent on whether it is difficult or easy for worlds to maintain the habitability, the search for extra- terrestrial life with a focus on extremophiles will either represent a search for dying worlds, or a search for special life on living worlds, focusing too narrowly on extreme values. -
Susceptibility of Archaea to Antimicrobial Agents: Applications to Clinical Microbiology
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector REVIEW 10.1111/j.1469-0691.2012.03913.x Susceptibility of archaea to antimicrobial agents: applications to clinical microbiology S. Khelaifia and M. Drancourt Unite´ de Recherche sur les Maladies Infectieuses et Tropicales Emergentes, UMR CNRS 6236 IRD 3R198, Me´diterrane´e Infection, Faculte´ de Me´decine, Aix-marseille-Universite´, Marseille, France Abstract We herein review the state of knowledge regarding the in vitro and in vivo susceptibility of archaea to antimicrobial agents, including some new molecules. Indeed, some archaea colonizing the human microbiota have been implicated in diseases such as periodontopathy. Archaea are characterized by their broad-spectrum resistance to antimicrobial agents. In particular, their cell wall lacks peptidoglycan, making them resistant to antimicrobial agents interfering with peptidoglycan biosynthesis. Archaea are, however, susceptible to the pro- tein synthesis inhibitor fusidic acid and imidazole derivatives. Also, squalamine, an antimicrobial agent acting on the cell wall, proved effective against human methanogenic archaea. In vitro susceptibility data could be used to design protocols for the decontamination of complex microbiota and the selective isolation of archaea in anaerobic culture. Keywords: Antimicrobial agent, archaea, methanogenic archaea, microbiota, susceptibility testing Article published online: 23 May 2012 Clin Microbiol Infect 2012; 18: 841–848 Corresponding author: M. Drancourt, Unite´ des Rickettsies, Fa- culte´ de Me´decine, 27, Boulevard Jean Moulin-Cedex 5, France E-mail: [email protected] Methanogenic archaea (herein referred to as methano- Introduction gens) are the sole organisms producing methane from H2 +CO2 [6]. -
Extremely Thermophilic Microorganisms As Metabolic Engineering Platforms for Production of Fuels and Industrial Chemicals
REVIEW published: 05 November 2015 doi: 10.3389/fmicb.2015.01209 Extremely thermophilic microorganisms as metabolic engineering platforms for production of fuels and industrial chemicals Benjamin M. Zeldes 1, Matthew W. Keller 2, Andrew J. Loder 1, Christopher T. Straub 1, Michael W. W. Adams 2 and Robert M. Kelly 1* 1 Department of Chemical and Biomolecular Engineering, North Carolina State University, Raleigh, NC, USA, 2 Department of Biochemistry and Molecular Biology, University of Georgia, Athens, GA, USA Enzymes from extremely thermophilic microorganisms have been of technological interest for some time because of their ability to catalyze reactions of industrial significance at elevated temperatures. Thermophilic enzymes are now routinely produced in recombinant mesophilic hosts for use as discrete biocatalysts. Genome and metagenome sequence data for extreme thermophiles provide useful information for putative biocatalysts for a wide range of biotransformations, albeit involving at most a few enzymatic steps. However, in the past several years, unprecedented progress has been made in establishing molecular genetics tools for extreme thermophiles to the point Edited by: that the use of these microorganisms as metabolic engineering platforms has become Bettina Siebers, University of Duisburg-Essen, possible. While in its early days, complex metabolic pathways have been altered or Germany engineered into recombinant extreme thermophiles, such that the production of fuels and Reviewed by: chemicals at elevated temperatures has become possible. Not only does this expand the Haruyuki Atomi, thermal range for industrial biotechnology, it also potentially provides biodiverse options Kyoto University, Japan Phillip Craig Wright, for specific biotransformations unique to these microorganisms. The list of extreme University of Sheffield, UK thermophiles growing optimally between 70 and 100◦C with genetic toolkits currently *Correspondence: available includes archaea and bacteria, aerobes and anaerobes, coming from genera Robert M. -
Extreme Organisms on Earth Show Us Just How Weird Life Elsewhere Could Be. by Chris Impey Astrobiology
Astrobiology Extreme organisms on Earth show us just how weird life elsewhere could be. by Chris Impey How life could thrive on hostile worlds Humans have left their mark all over Earth. We’re proud of our role as nature’s generalists — perhaps not as swift as the gazelle or as strong as the gorilla, but still pretty good at most things. Alone among all species, technology has given us dominion over the planet. Humans are endlessly plucky and adaptable; it seems we can do anything. Strain 121 Yet in truth, we’re frail. From our safe living rooms, we may admire the people who conquer Everest or cross deserts. But without technology, we couldn’t live beyond Earth’s temperate zones. We cannot survive for long in temperatures below freezing or above 104° Fahrenheit (40° Celsius). We can stay underwater only as long as we can hold our breath. Without water to drink we’d die in 3 days. Microbes, on the other hand, are hardy. And within the microbial world lies a band of extremists, organisms that thrive in conditions that would cook, crush, smother, and dissolve most other forms of life. Collectively, they are known as extremophiles, which means, literally, “lovers of extremes.” Extremophiles are found at temperatures above the boiling point and below the freezing point of water, in high salinity, and in strongly acidic conditions. Some can live deep inside rock, and others can go into a freeze-dried “wait state” for tens of thousands of years. Some of these microbes harvest energy from meth- ane, sulfur, and even iron. -
DOGAMI Open-File Report O-86-06, the State of Scientific
"ABLE OF CONTENTS Page INTRODUCTION ..~**********..~...~*~~.~...~~~~1 GORDA RIDGE LEASE AREA ....................... 2 RELATED STUDIES IN THE NORTH PACIFIC .+,...,. 5 BYDROTHERMAL TEXTS ........................... 9 34T.4 GAPS ................................... r6 ACKNOWLEDGEMENT ............................. I8 APPENDIX 1. Species found on the Gorda Ridge or within the lease area . .. .. .. .. .. 36 RPPENDiX 2. Species found outside the lease area that may occur in the Gorda Ridge Lease area, including hydrothermal vent organisms .................................55 BENTHOS THE STATE OF SCIENTIFIC INFORMATION RELATING TO THE BIOLOGY AND ECOLOGY 3F THE GOUDA RIDGE STUDY AREA, NORTZEAST PACIFIC OCEAN: INTRODUCTION Presently, only two published studies discuss the ecology of benthic animals on the Gorda Sidge. Fowler and Kulm (19701, in a predominantly geolgg isal study, used the presence of sublittor31 and planktsnic foraminiferans as an indication of uplift of tfie deep-sea fioor. Their resuits showed tiac sedinenta ana foraminiferans are depositea in the Zscanaba Trough, in the southern part of the Corda Ridge, by turbidity currents with a continental origin. They list 22 species of fararniniferans from the Gorda Rise (See Appendix 13. A more recent study collected geophysical, geological, and biological data from the Gorda Ridge, with particular emphasis on the northern part of the Ridge (Clague et al. 19843. Geological data suggest the presence of widespread low-temperature hydrothermal activity along the axf s of the northern two-thirds of the Corda 3idge. However, the relative age of these vents, their present activity and presence of sulfide deposits are currently unknown. The biological data, again with an emphasis on foraminiferans, indicate relatively high species diversity and high density , perhaps assoc iated with widespread hydrotheraal activity. -
Marine Extremophiles: a Source of Hydrolases for Biotechnological Applications
Mar. Drugs 2015, 13, 1925-1965; doi:10.3390/md13041925 OPEN ACCESS marine drugs ISSN 1660-3397 www.mdpi.com/journal/marinedrugs Article Marine Extremophiles: A Source of Hydrolases for Biotechnological Applications Gabriel Zamith Leal Dalmaso 1,2, Davis Ferreira 3 and Alane Beatriz Vermelho 1,* 1 BIOINOVAR—Biotechnology laboratories: Biocatalysis, Bioproducts and Bioenergy, Institute of Microbiology Paulo de Góes, Federal University of Rio de Janeiro, Av. Carlos Chagas Filho, 373, 21941-902 Rio de Janeiro, Brazil; E-Mail: [email protected] 2 Graduate Program in Plant Biotechnology, Health and Science Centre, Federal University of Rio de Janeiro, Av. Carlos Chagas Filho, 373, 21941-902 Rio de Janeiro, Brazil 3 BIOINOVAR—Biotechnology Laboratories: Virus-Cell Interaction, Institute of Microbiology Paulo de Góes, Federal University of Rio de Janeiro, Av. Carlos Chagas Filho, 373, 21941-902 Rio de Janeiro, Brazil; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +55-(21)-3936-6743; Fax: +55-(21)-2560-8344. Academic Editor: Kirk Gustafson Received: 1 December 2014 / Accepted: 25 March 2015 / Published: 3 April 2015 Abstract: The marine environment covers almost three quarters of the planet and is where evolution took its first steps. Extremophile microorganisms are found in several extreme marine environments, such as hydrothermal vents, hot springs, salty lakes and deep-sea floors. The ability of these microorganisms to support extremes of temperature, salinity and pressure demonstrates their great potential for biotechnological processes. Hydrolases including amylases, cellulases, peptidases and lipases from hyperthermophiles, psychrophiles, halophiles and piezophiles have been investigated for these reasons. -
METHANOGENS AS MODELS for LIFE on MARS. R. L. Mickol1, W. H. Waddell2, and T
Eighth International Conference on Mars (2014) 1005.pdf METHANOGENS AS MODELS FOR LIFE ON MARS. R. L. Mickol1, W. H. Waddell2, and T. A. Kral1,3, 1Arkansas Center for Space and Planetary Sciences, 202 Old Museum Building, University of Arkansas, Fayetteville, Arkansas, 72701, USA, [[email protected]], 2Dept. of Health, Human Performance, and Recreation, HPER 308, University of Arkansas, Fayetteville, Arkansas, 72701, USA, 3Dept. of Biological Sciences, SCEN 632, University of Arkansas, Fayetteville, Arkansas, 72701, USA. Introduction: The discovery of methane in the Sciences, University of Arkansas, Fayetteville, Arkan- martian atmosphere [1-4] has fueled the study of meth- sas. All four methanogen species were tested in these anogens as ideal candidates for life on Mars. Methano- experiments. Methanogens were grown in their respec- gens are chemoautotrophs from the domain Archaea. tive anaerobic growth media and placed into the cham- These microorganisms utilize hydrogen as an energy ber with a palladium catalyst box to remove residual source and carbon dioxide as a carbon source to pro- oxygen. The chamber was evacuated to a pre- duce methane. Methanogens can be considered ideal determined pressure and filled with 80:20 H2:CO2 gas. candidates for life on Mars because they are anaerobic, This procedure was repeated three times to ensure re- they do not require organic nutrients and are non- moval of the atmosphere. The chamber was then main- photosynthetic, indicating they could exist in sub- tained at the desired pressure (133-143 mbar, 67-72 surface environments. mbar, 33-38 mbar, 6-10 mbar, 7-20 mbar) for the dura- Our lab has studied methanogens as models for life tion of the experiments.