DOCSLIB.ORG

Academic Voices.Indd

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Academic Voices.Indd Academic Voices A Multidisciplinary Journal Volume 1, N0. 1, 2011 POSITION OF CYANOBACTERIA AND ALGAE IN ORIGIN OF LIFE Vishwanath Prasad Department of Botany Abstract Our beautiful planet, the earth was originated 4.5 billion years ago in our solar system. Between 3.5 – 4.0 billion years ago, after several events of chemical evolution and modifi cation in the earth's atmosphere, the fi rst life, amino acid and nucleic acid, called ecobiont or protobiont, was originated in abiogenesis phase and started protobiology phase. The life has evolved into three domains: age of Eobacteria, Cyanobacteria and Eukaryotes which ultimately evolve into land plants. The purpose of the this article is to add some recent information about origin of life and position of cyanobacteria in the evolution of higher plants. Keywords Origin, life, Ecobiont, Cyanobacteria, algae. Introduction from each other by immense large empty space. Spiral galaxy, our closest neighbour Life is very mysterious gift of nature on called the Andromeda Nebula, located at this beautiful planet, earth. The origin of about 28 million light years from the earth is life and even earth in the universe is still the cluster of galaxies. Average galaxy consists mysterious and complex. The earth is a tiny of some 100 billion stars. Our sun is one of the part of the Universe. The theoretical rough middle size star and our earth is a middle size estimate reveals that the universe consists planet of the solar system (Carl Zeiss, 2005). about 50 billion galaxies. Astrophysics study The earth was probably formed about 4.5x109 of the universe from the earth using the art years ago, however, the oldest terrestrial rocks technology observation reveals the presence found to date are about 3.5x109 years old or so. of two galaxies, elliptical and spiral, separated ( Margulis et al, 1976). 94 Cyanobacteria and Algae in origin of life Origin of Life : primitive prokaryote chlorobacteria, the fi rst negibacteria with cell bounded by two acyl Life probably originated when the earth's ester phospholipid membranes. They have atmosphere was anoxic and consist of methane, anoxygenic photosynthesis, chaemosynthesis ammonia, nitrogen and water vapour with using hydrogen or H s as hydrogen donor preponderance of hydrogen (Oparin, 1964). 2 Many events of chemical evolution are likely to to fi x carbon. Then, transition occurred in have occurred in the prebiontic atmosphere, negibacteria, eurybacteria, posibacteria, probably between 3500-4000 million years glycobacteria and then into chlorobacteria ago and simpler organic compounds like with origination of fl agella in cells. This is amino acids were formed under the infl uence also called Chlorobacterial age. Archaea a of ultraviolet radiations and electric discharge third dormain of life, in addition to bacteria as sources of energy. Later, the earth cooled and eukaryote, on the basis of molecular, down suffi ciently to provide pools of liquid genomics and phylogenetic data is diversifi ed water. In the early period of earth, there were into two major phyla, the Crenarchaeota production of complex organic compounds and the Euryarchaeota. (Woese et. al., 1990; without life. It was called phase of abiogenesis. Gribaldo and Brochier, 2006) Nature have made several trials in creating Age of Cyanobacteria the fi rst biological entity. The droplet After the Chlorobacterial or Eobacterial age, called coacervates, may absorb water, swell the cellular innovation and microbial radiation and under go the processes of selectivity, dramatically transformed the earth's surface recognition, interaction etc. It could have and the glycobacterial revolution initiated led to replicating molecules which gradually an oxygenic age called age of Cyanobacteria. evolved into biological entities. This phage During this age, between 2.8 – 0.9 billion was the origin of amino acid which on heating years ago, cyanobacterial photosynthesis originated nucleic acid. This phage is called predominantly fed ecosystem and the eobiology (dawn of life ) or protobiology (fi rst biosphere was diff erentiated into aerobic and life). Thus, the organisms are accordingly anaerobic zones. Therefore, cyanobacteria are called eobionts or protobionts. The eobionts also called fi rst oxygen producing organism and coacervates are the origin of biological and architects of atmosphere. organisms . Presently, the geological and biological evidences suggest that the fi rst The Eobacteria and Cyanobacteria both have living forms on this planet were probably always two distinct lipid surface membranes some heterotrophic anaerobic bacteria. where as posibacteria consists only one surface membrane, therefore, the Precambrian Three – phases history of life period could be properly termed as Age of Under two revolutionary periods, Prokaryotes and the later half of this Eon, was Glycobacterial revolution and Neomuran the Age of cyanobacteria (Schopf, 2006) revolution (Cavalier – Smith, 2006), life has Unlike most other groups of bacteria, the evolved into following three ages of life: age cyanobacteria have a greater diversity of of Eobacteria , age of Cyanobacteria and age 1, N0. 2011 Vol. morphological phenotype with few exceptions. of Eukaryotes. Many cyanobacteria have exteremely Age of Eobacteria long generation times as compared to the popular heterotrophic bacteria. They have This fi rst phase began before 2.9 -2.8 effi cient DNA-repair systems. The genome Gyrs ago when the origin of cells and size is apparently larger in most complex anoxic photosynthesis generated the most cyanobacteria than Ecoli, Bacillus and smaller Voices, Academic 95 V. Prasad unicellular cyanobacteria. The genome size of was highly reducing and hence hydrogenase, about 128 strains of cyanobacteria ranges from nitrogenase enzymes acetylene, cyanide, ca 1.6 billion daltons in unicellular type to 8.6 cyanogens, nitrites etc have high probability billion daltons in more complex fi lamentous in cyanobacteria. They have a novel device, type (Castenholz, 1992). heterocysts, to protect the oxygen – labile nitrogenase. The cyanophycin granule in Proteins and nucleic acids are dividing cyanobacteria contains equimolar proportions fossils because they have been dynamically of arginine and aspartic acid. (Kumar, et. al., conserved by the evolutionary process over 1980) millions of years. The prebiontic atmosphere Present 0.065 Gyr dinosaurs diatoms dinoflagellates 0.253 Gyr mass extinction PHANEROZOIC Age of eukaryotes 0.543 Gyr Land Plants NEOPROTEROZOIC Snow ball earth Methanogenesis Eukaryotes, archaebacteria NEOMURAN REVOLUTION 0.9 Gyr 1000 Myr Actinobacteria MID-PROTEROZOIC 1.5 Gyr Oxygen-rich atmosphere Age of Cyanobacteria 2000 Myr. 2.1 Gyr 2.3 Gyr atmospheric oxygenation PALAEOPROTEROZOIC 2.4 Gyr snowball earth Cyanobacteria GLYCOBACTERIAL REVOLUTION Oxygenic 2.8 Gyr anoxic Photosynthesis atmosphere 3000 Myr. Age of Eobacteria 3.1 Gyr ARCHAEN Possible cellular fossils Origin of life 3.5 Gyr Vol. 1, N0. 2011 Vol. HADEAN 3.8 Gyr Oldest rocks No evidence for life 4000 Myr. ago Fig 1. Origin of Life (Source : Cavalier – Smith, 2006) Academic Voices, Voices, Academic (Gyr: Billion years; Myr: Million years ) 96 Cyanobacteria and Algae in origin of life Age of Eukaryote Chlorophyta, Rhodophyta, Glaucophyta, Euglenophyta, Chlorarachniophyta, The cyanobacterial oxygen liberation grew Haptophyta, Cryptophyta and Dinophyta. the ozone layer and later o.9 Gyr ago after rise Now, the algae may be classifi ed into 2 empires of planktons, during Neomuran revolution and 15 divisions (Prasad, 2010). another age started called age of Eukaryotes and Archaebacteria. During 720 Myr ago, due The eukaryotic phyla that exist today, to ultraviolet, the Arachean organic carbon have a fan–shaped phylogenetic evolution attributed methanogenesis and triggered (Hoek et. al., 2009). From the green lineage snow ball Earth episode by slight global diversifi cation the Charophytes have warming. originated. They have several similarities with land plants and initiated the evolution The evolution of green algal plastid is of and development of terrestrial ecosystems cyanobacterial origin due to endosymbiosis including Bryophytes, Pteridophytes, and which is supported by the discovery of the higher land plants (Kenrick and Crane, 1997; Prochlorophyta (Lewin, 1976). Cyanobacteria Bhattacharya and Medlin, 1998., Yin-lorg and are the source of Glaucophyte simple plastids. Jaff ery, 1999). The major lineages of the algae are the Eukaryotes 0.9 Gyr ago Archaebacteria Neomur Methanogenesis hyperthermophily unimembrana Neomuran revolution 0.9 Gyr ago 1.Surfacemembrane Colonize soil. 2.surfacemembranes Outer membrane Glycobacteria Eubacteria eg. Cyanobacteria Glycobacterial revolution Oxygen 1, N0. 2011 Vol. Negibacteria 2.8 Gyr ago Eobacteria eg. Chloroflexus 3.5 Gyr ago Fig 2. Tree of Life emphasizing major revolution (Source : Cavalier – Smith, 2006) Academic Voices, Voices, Academic 97 V. Prasad Fig 3. Tree of Life (Bhatacharya and Medlin, 1998; Hoek et. al., 2009) Conclusion References First of all, life between 3.5-4.0 billion years Bhattacharya, D. & Medlin, L. (1998). Algal ago, originated in in abiogenesis phase in Phylogeny and origin of Land Plants. Plant the form of amino acid and nucleic acid. The Physiol. 116, 9-15. life has evolved into three domains: age of Carl Zeiss, A.G. (2005). Black Hole in Ecobacteria, cyanobacteria and Eukaryotes. the Holmberg II Galaxy. Innovation, Cyanobacteria, fi rst phototrophs, during 16,10-11. glycobacterial revolution between
Load more

Recommended publications
  • Changes in the Human Skin Microbiome Over One Year's Time
    American Journal of Microbiology 3 (2): 18-30, 2012 ISSN 1948-982x © 2012 Science Publications doi:10.3844/ajmsp.2012.18.30 Published Online 3 (2) 2012 (http://www.thescipub.com/ajm.toc) Changes in the Human Skin Microbiome Over One Year’s Time 1,2 Richard W. Hyman, 1Farbod Babrzadeh, 1Curtis Palm, 1Chunlin Wang, 1Marilyn Fukushima and 1,2,3 Ronald W. Davis 1Stanford Genome Technology Center, 855 S California Avenue, Palo Alto, CA 94304, USA 2Department of Biochemistry, 3Department of Genetics, Stanford University College of Medicine, Stanford, CA 94305, USA ABSTRACT Human skin comprises a large number of distinguishable ecological niches. To describe fully the human skin microbiome, it will be necessary to identify the bacteria in each niche and to distinguish the commensal bacteria from the temporary residents. To contribute to the description of the human skin microbiome and employing a gene-based technology, we have identified the bacteria in two niches: the front and back of the base of the neck and over the course of one year. There were 50 volunteers and a total of 232 neck skin swabs. Roche 454 Tag pyrosequencing was employed to sequence a short hypervariable sequence region (V6) of the 16S ribosomal RNA gene. To identify the bacteria corresponding to the front and back of the neck for each volunteer, the “Classifier” software in the “Pyrosequencing” section of the Ribosomal Database Project was employed. The bacteria on virtually all 232 neck skin swabs were classified into bacterial Class. The skin microbiome of these two niches was composed principally of a mixture of five Classes of bacteria: Actinobacteria , Alphaproteobacteria , Bacilli , Betaproteobacteria and Gammaproteobacteria .
    [Show full text]
  • An Abstract of the Thesis Of
    AN ABSTRACT OF THE THESIS OF Kaitlin Mae McConnell, for the degree of Master of Science in Microbiology presented on September 6, 2019. Title: Reef Microbiomes of Mo’orea, French Polynesia, a Socio-Ecological Island System Abstract approved: ______________________________________________________ Andrew R. Thurber At a time of rapid global change, a socio-ecological system (SES) approach can provide a framework through which to quantify and communicate the risks and uncertainties of coupled human-natural systems. Islands, and tropical coral reef islands in particular, can be excellent models for SES research since they may be considered as both closed and open systems, where agents-- both human and non- human-- and their interactions, may be considered at a variety of spatial and temporal scales and with diverse levels of complexity. Bacteria and Archaea communities are the executants of biochemical cycling in systems, and alterations in the structure of microbial communities can provide indications of system-wide metabolic shifts driven by natural and human forces. In this thesis, I first present patterns of spatial and temporal variability in microbial communities across a tropical coral island reefscape, where I hypothesized: Microbiome host, habitat and sampling location will house distinct microbiomes (beta diversity) that differ between seasons. Microbiomes were primarily host specific, and host specificity varied with structural scale: microbiomes of reef sediment, seawater and corals were different from each other. Zooming in, the three species of corals examined also had distinct microbial communities associated with them. These host- specific microbiomes varied differentially across spatial scale, such as island side, reef habitat (fore, back and fringing reefs) and sampling locations.
    [Show full text]
  • The Phagotrophic Origin of Eukaryotes and Phylogenetic Classification Of
    International Journal of Systematic and Evolutionary Microbiology (2002), 52, 297–354 DOI: 10.1099/ijs.0.02058-0 The phagotrophic origin of eukaryotes and phylogenetic classification of Protozoa Department of Zoology, T. Cavalier-Smith University of Oxford, South Parks Road, Oxford OX1 3PS, UK Tel: j44 1865 281065. Fax: j44 1865 281310. e-mail: tom.cavalier-smith!zoo.ox.ac.uk Eukaryotes and archaebacteria form the clade neomura and are sisters, as shown decisively by genes fragmented only in archaebacteria and by many sequence trees. This sisterhood refutes all theories that eukaryotes originated by merging an archaebacterium and an α-proteobacterium, which also fail to account for numerous features shared specifically by eukaryotes and actinobacteria. I revise the phagotrophy theory of eukaryote origins by arguing that the essentially autogenous origins of most eukaryotic cell properties (phagotrophy, endomembrane system including peroxisomes, cytoskeleton, nucleus, mitosis and sex) partially overlapped and were synergistic with the symbiogenetic origin of mitochondria from an α-proteobacterium. These radical innovations occurred in a derivative of the neomuran common ancestor, which itself had evolved immediately prior to the divergence of eukaryotes and archaebacteria by drastic alterations to its eubacterial ancestor, an actinobacterial posibacterium able to make sterols, by replacing murein peptidoglycan by N-linked glycoproteins and a multitude of other shared neomuran novelties. The conversion of the rigid neomuran wall into a flexible surface coat and the associated origin of phagotrophy were instrumental in the evolution of the endomembrane system, cytoskeleton, nuclear organization and division and sexual life-cycles. Cilia evolved not by symbiogenesis but by autogenous specialization of the cytoskeleton.
    [Show full text]
  • Biology 1015 General Biology Lab Taxonomy Handout
    Biology 1015 General Biology Lab Taxonomy Handout Section 1: Introduction Taxonomy is the branch of science concerned with classification of organisms. This involves defining groups of biological organisms on the basis of shared characteristics and giving names to those groups. Something that you will learn quickly is there is a lot of uncertainty and debate when it comes to taxonomy. It is important to remember that the system of classification is binomial. This means that the species name is made up of two names: one is the genus name and the other the specific epithet. These names are preferably italicized, or underlined. The scientific name for the human species is Homo sapiens. Homo is the genus name and sapiens is the trivial name meaning wise. For green beans or pinto beans, the scientific name is Phaseolus vulgaris where Phaseolus is the genus for beans and vulgaris means common. Sugar maple is Acer saccharum (saccharum means sugar or sweet), and bread or brewer's yeast is Saccharomyces cerevisiae (the fungus myces that uses sugar saccharum for making beer cerevisio). In taxonomy, we frequently use dichotomous keys. A dichotomous key is a tool for identifying organisms based on a series of choices between alternative characters. Taxonomy has been called "the world's oldest profession", and has likely been taking place as long as mankind has been able to communicate (Adam and Eve?). Over the years, taxonomy has changed. For example, Carl Linnaeus the most renowned taxonomist ever, established three kingdoms, namely Regnum Animale, Regnum Vegetabile and Regnum Lapideum (the Animal, Vegetable and Mineral Kingdoms, respectively).
    [Show full text]
  • Deep Phylogeny, Ancestral Groups and the Four Ages of Life
    Downloaded from rstb.royalsocietypublishing.org on July 31, 2010 Deep phylogeny, ancestral groups and the four ages of life Thomas Cavalier-Smith Phil. Trans. R. Soc. B 2010 365, 111-132 doi: 10.1098/rstb.2009.0161 References This article cites 73 articles, 28 of which can be accessed free http://rstb.royalsocietypublishing.org/content/365/1537/111.full.html#ref-list-1 Article cited in: http://rstb.royalsocietypublishing.org/content/365/1537/111.full.html#related-urls This article is free to access Rapid response Respond to this article http://rstb.royalsocietypublishing.org/letters/submit/royptb;365/1537/111 Subject collections Articles on similar topics can be found in the following collections evolution (1878 articles) Receive free email alerts when new articles cite this article - sign up in the box at the top Email alerting service right-hand corner of the article or click here To subscribe to Phil. Trans. R. Soc. B go to: http://rstb.royalsocietypublishing.org/subscriptions This journal is © 2010 The Royal Society Downloaded from rstb.royalsocietypublishing.org on July 31, 2010 Phil. Trans. R. Soc. B (2010) 365, 111–132 doi:10.1098/rstb.2009.0161 Review Deep phylogeny, ancestral groups and the four ages of life Thomas Cavalier-Smith* Department of Zoology, University of Oxford, South Parks Road, Oxford OX1 3PS, UK Organismal phylogeny depends on cell division, stasis, mutational divergence, cell mergers (by sex or symbiogenesis), lateral gene transfer and death. The tree of life is a useful metaphor for organis- mal genealogical history provided we recognize that branches sometimes fuse. Hennigian cladistics emphasizes only lineage splitting, ignoring most other major phylogenetic processes.
    [Show full text]
  • DNA Repair: Lessons from the Evolution of Ionizing-Radiation-Resistant Prokaryotes – Fact and Theory
    7 DNA Repair: Lessons from the Evolution of Ionizing-Radiation-Resistant Prokaryotes – Fact and Theory Haïtham Sghaier Research Unit UR04CNSTN01 "Medical and Agricultural Applications of Nuclear Techniques", National Center for Nuclear Sciences and Technology (CNSTN), Sidi Thabet Technopark, Sidi Thabet, Tunisia 1. Introduction At the outset, I believe that the concept of ionizing-radiation (IR) resistance needs to be clarified in a tangible manner for readers of this chapter. I propose the following general definition adopted in a previous paper (Sghaier et al., 2008): An ionizing-radiation-resistant prokaryotes (IRRP) is any vegetative prokaryote that can thrive after exposure to high, acute IR (generally, with a D10 value - the dose necessary to effect a 90% reduction in Colony Forming Units - greater than 1 kGy) using efficient physiological, genetic and proteic protection and repair mechanisms to fully amend its DNA DSBs. IR resistance has been observed in a broad range of prokaryotic groups (Kopylov et al., 1993), including hyperthermophilic Archaea (P. abyssi, P. furiosus, Thermococcus marinus, Thermococcus radiotolerans and Thermococcus gammatolerans) (DiRuggiero et al., 1997; Jolivet et al., 2003a; Jolivet et al., 2003b; Jolivet et al., 2004), halophilic Archaea (Halobacterium sp.) (Kottemann et al., 2005), the Deinococcus-Thermus group (many Deinococcus sp. and Truepera radiovictrix) (Albuquerque et al., 2005), Actinobacteria (Rubrobacter radiotolerans, Rubrobacter xylanophilus and Kineococcus radiotolerans) (Yoshinaka et al., 1973; Ferreira et al., 1999; Phillips et al., 2002; Chen et al., 2004), Proteobacteria (Methylobacterium radiotolerans and Acinetobacter radioresistens) (Ito and Iizuka, 1971; Nishimura et al., 1994), Cyanobacteria (Chroococcidiopsis sp.) (Billi et al., 2000), and Sphingobacteria (Hymenobacter actinosclerus) (Collins et al., 2000).
    [Show full text]
  • Association Between Algal Productivity and Phycosphere Composition in an Outdoor Chlorella Sorokiniana Reactor Based on Multiple Longitudinal Analyses
    Association between algal productivity and phycosphere composition in an outdoor Chlorella sorokiniana reactor based on multiple longitudinal analyses Seth Steichen University of Arizona https://orcid.org/0000-0002-2267-7026 Song Gao Pacic Northwest National Laboratory Peter Waller University of Arizona Judith Brown ( [email protected] ) https://orcid.org/0000-0003-4669-8443 Research Keywords: 16S rRNA gene, benzalkonium chloride, biocide, Health Index, Melainabacteria, microalgal cultivation, microbiome, Vampirovibrionales Posted Date: January 24th, 2020 DOI: https://doi.org/10.21203/rs.2.21781/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published at Microbial Biotechnology on May 25th, 2020. See the published version at https://doi.org/10.1111/1751-7915.13591. Page 1/25 Abstract Background Microalgae as a biofuel source are of great interest. The outdoor Regional Algal Feedstock Testbed (RAFT) was established to optimize algal biomass production in the U.S. sunbelt states. The phycosphere inhabitants, consisting in part of the bacterial community within algal cultures, are hypothesized to contribute to algal productivity. However, little is known about their identity or specic contributions. In this study the bacterial composition of the Chlorella sorokiniana phycosphere was determined over several production cycles in different growing seasons by 16S rRNA gene sequencing and identication using the SILVA database. Results The C. sorokiniana bacterial phycosphere was sampled during 41 RAFT testbed cycles in two consecutive growing seasons. Eight reactors were sampled twice daily to establish baseline community composition, determined by high-throughput sequencing of 16S ribosomal RNA amplicons.
    [Show full text]
  • Chapter 1 Chapter 1: the Gospel According to LUCA
    UNIVERSITY OF CALIFORNIA, SAN DIEGO The gospel according to LUCA (the last universal common ancestor) A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Philosophy in Bioinformatics by Ruben Eliezer Meyer Valas Committee in charge: Professor Philip E. Bourne, Chair Professor William F. Loomis, Co-Chair Professor Russell F. Doolittle Professor Richard D. Norris Professor Milton H. Saier Jr. 2010 The Dissertation of Ruben Eliezer Meyer Valas is approved, and it is acceptable in quality and form for publication on microfilm and electronically: ______________________________________________________________________ ______________________________________________________________________ ______________________________________________________________________ ______________________________________________________________________ Co-chair ______________________________________________________________________ Chair University of California, San Diego 2010 iii DEDICATION I dedicate this work to Alexander “Sasha” Shulgin. Sasha is probably the wisest person I’ve met. He refuses to allow anything other than his own imagination dictates the rules of what is possible. Many of us are just living inside his dreams. This thesis is my attempt at answering the great question of “why are we here?”, and Sasha is one of the few people I’d really listen to if he tried to answer it. iv EPIGRAPH "First they ignore you, then they ridicule you, then they fight you, then you win." Mahatma Gandhi v TABLE OF CONTENTS Signature
    [Show full text]
  • Origin of the Cell Nucleus, Mitosis and Sex: Roles of Intracellular Coevolution Thomas Cavalier-Smith*
    Cavalier-Smith Biology Direct 2010, 5:7 http://www.biology-direct.com/content/5/1/7 RESEARCH Open Access Origin of the cell nucleus, mitosis and sex: roles of intracellular coevolution Thomas Cavalier-Smith* Abstract Background: The transition from prokaryotes to eukaryotes was the most radical change in cell organisation since life began, with the largest ever burst of gene duplication and novelty. According to the coevolutionary theory of eukaryote origins, the fundamental innovations were the concerted origins of the endomembrane system and cytoskeleton, subsequently recruited to form the cell nucleus and coevolving mitotic apparatus, with numerous genetic eukaryotic novelties inevitable consequences of this compartmentation and novel DNA segregation mechanism. Physical and mutational mechanisms of origin of the nucleus are seldom considered beyond the long- standing assumption that it involved wrapping pre-existing endomembranes around chromatin. Discussions on the origin of sex typically overlook its association with protozoan entry into dormant walled cysts and the likely simultaneous coevolutionary, not sequential, origin of mitosis and meiosis. Results: I elucidate nuclear and mitotic coevolution, explaining the origins of dicer and small centromeric RNAs for positionally controlling centromeric heterochromatin, and how 27 major features of the cell nucleus evolved in four logical stages, making both mechanisms and selective advantages explicit: two initial stages (origin of 30 nm chromatin fibres, enabling DNA compaction; and firmer attachment of endomembranes to heterochromatin) protected DNA and nascent RNA from shearing by novel molecular motors mediating vesicle transport, division, and cytoplasmic motility. Then octagonal nuclear pore complexes (NPCs) arguably evolved from COPII coated vesicle proteins trapped in clumps by Ran GTPase-mediated cisternal fusion that generated the fenestrated nuclear envelope, preventing lethal complete cisternal fusion, and allowing passive protein and RNA exchange.
    [Show full text]
  • An Insert in EF-2 Excludes the Root from Eukaryotes and Archaea
    Structural Analysis of Polarizing Indels Argues the Root of the Tree of Life is Near the Chloroflexi Ruben Valas, Philip Bourne Contact: [email protected] Bioinformatics Program, University of California, San Diego Abstract An insert in EF-2 excludes the root from The HisA HisF indel does not exclude the Eukaryotes and Archaea root from the Eobacteria Determining which branches of the tree of life have derived features narrows down the possible location of the root. Currently the polarization of indels done by Lake et al.[1-5] and the polarizing transitions of Cavalier-Smith[6] arrive at contradictory positions for EF-2 is the Archaeal and Eukaryotic homolog of EF-G. EF-2 contains an insert that is not the root of the tree. We have analyzed the sequence based indel arguments using pro- present in EF-G or EF-Tu which implies the Archaea and Eukaryotes are derived. How- tein structure wherever possible. Structure strongly supports some of the polarizations, ever, the authors’ sequence alignment has been called into question. We performed a but in other indels it argues for a different conclusion. We conclude that there is no con- structural alignment EF-G (2BV3 colored blue), EF-Tu (1EFC colored cyan), EF-2 (1N0U tradiction between Lake et al. and Cavalier-Smith; the root of the tree of life must be colored red) to investigate whether their conclusion is valid. Our analysis is compli- near the Chloroflexi. cated by a disordered region in the structures that precedes the region of interest. The well conserved RGIT motif does align correctly when using structure alone.
    [Show full text]
  • GM Maize Crops and Plant Growth-Promoting Characterization of the Isolated Strains
    Analysis of Bacterial Diversity in the Rhizosphere of GM and Non- GM Maize Crops and Plant Growth-Promoting Characterization of the Isolated Strains By NASEER AHMAD Department of Plant Sciences Faculty of Biological Sciences Quaid-i-Azam University Islamabad-Pakistan 2013 Analysis of Bacterial Diversity in the Rhizosphere of GM and Non-GM Maize Crops and Plant Growth-Promoting Characterization of the Isolated Strains A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy By NASEER AHMAD Department of Plant Sciences Faculty of Biological Sciences Quaid-i-Azam University Islamabad-Pakistan 2013 i DECLARATION OF ORIGINALITY I hereby declare that the work accomplished in this thesis is the result of my own research carried out in the Molecular Systematics and Applied Ethnobotany Lab, Department of Biotechnology, Quaid-i-Azam University Islamabad. This thesis has not been published previously nor does it contain any material from the published resources that can be considered as the violation of international copyright law. Furthermore I also declare that I am aware of the terms ‘copyright’ and ‘plagiarism’ and if any copyright violation was found out in this work I will be responsible of the consequences of any such violation. Signature: _________ Name: Naseer Ahmad Date: / /2013 ii CERTIFICATE This thesis submitted by Mr. Naseer Ahmad, is accepted in its present form by the Department of Plant Sciences, Faculty of Biological Sciences, Quaid-i-Azam University, Islamabad as satisfying the thesis requirements for the degree of Doctor of Philosophy (Plant Sciences). Supervisor Prof. Dr. Zabta Khan Shinwari Chairman Department of Biotechnology External examiner External examiner Chairperson Prof.
    [Show full text]
  • Notification List
    International Journal of Systematic and Evolutionary Microbiology (2002), 52, 293–295 DOI: 10.1099/ijs.0.02318-0 NOTIFICATION LIST Notification that new names and new combinations have appeared in volume 52, part 1, of the IJSEM This listing of names published in a previous issue of the IJSEM is provided as a service to bacteriology to assist in the recognition of new names and new combinations. This procedure was proposed by the Judicial Commission [Minute II(ii), Int J Syst Bacteriol 41 (1991), p. 185]. The names given herein have priority according to the page number of the IJSEM on which they were proposed. Name Proposed as: Author(s) Page no. Negibacteria subregnum nov.*† Cavalier-Smith 10 Eobacteria infraregnum nov.*† Cavalier-Smith 10 Eobacteria divisio nov.*† Cavalier-Smith 10 Chlorobacteria class. nov.† Cavalier-Smith 10 Hadobacteria class. nov.† Cavalier-Smith 10 Glycobacteria infraregnum nov.*† Cavalier-Smith 10 Cyanobacteria nom. rev.*‡ Cavalier-Smith 10 Gloeobacteria subdivisio nov.* Cavalier-Smith 10 Gloeobacteria class. nov. Cavalier-Smith 10 Gloeobacterales ord. nov.§ Cavalier-Smith 10 Phycobacteria subdivisio nov.* Cavalier-Smith 10 Chroobacteria class. nov. Cavalier-Smith 10 Chroococcales ord. nov.§ Cavalier-Smith 10 Pleurocapsales ord. nov.§ Cavalier-Smith 11 Oscillatoriales ord. nov.§ Cavalier-Smith 11 Hormogoneae class. nov. Cavalier-Smith 11 Nostocales ord. nov.§ Cavalier-Smith 11 Stigonematales ord. nov.§ Cavalier-Smith 11 Spirochaetae divisio nov.* Cavalier-Smith 11 Spirochaetes class. nov. Cavalier-Smith 11 Sphingobacteria divisio nov.* Cavalier-Smith 11 Flavobacteria class. nov. Cavalier-Smith 11 Chlorobea class. nov. Cavalier-Smith 11 Exoflagellata superdivisio nov.*† Cavalier-Smith 11 Planctobacteria divisio nov.* Cavalier-Smith 11 Planctomycea class.
    [Show full text]