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Chapter 10: Classification of Microorganisms
Chapter 10: Classification of Microorganisms 1. The Taxonomic Hierarchy 2. Methods of Identification 1. The Taxonomic Hierarchy Phylogenetic Tree of the 3 Domains Taxonomic Hierarchy • 8 successive taxa are used to classify each species: Domain Kingdom Phylum Class Order Family Genus **species can also contain different strains** Species Scientific Nomenclature To avoid confusion, every type of organism must be referred to in a consistent way. The current system of nomenclature (naming) has been in use since the 18th century: • every type of organism is referred by its genus name followed by its specific epithet (i.e., species name) Homo sapiens (H. sapiens) Escherichia coli (E. coli) • name should be in italics and only the genus is capitalized which can also be abbreviated • names are Latin (or “Latinized” Greek) with the genus being a noun and the specific epithet an adjective **strain info can be listed after the specific epithet (e.g., E. coli DH5α)** 2. Methods of Identification Biochemical Testing In addition to morphological (i.e., appearance under the microscope) and differential staining characteristics, microorganisms can also be identified by their biochemical “signatures”: • the nutrient requirements and metabolic “by-products” of of a particular microorganism • different growth media can be used to test the physiological characteristics of a microorganism • e.g., medium with lactose only as energy source • e.g., medium that reveals H2S production **appearance on test medium reveals + or – result!** Commercial devices for rapid Identification Perform multiple tests simultaneously Enterotube II Such devices involve the simultaneous inoculation of various test media: • ~24 hrs later the panel of results reveals ID of organism! Use of Dichotomous Keys Series of “yes/no” biochemical tests to ID organism. -
Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide
antioxidants Review Anoxygenic Photosynthesis in Photolithotrophic Sulfur Bacteria and Their Role in Detoxication of Hydrogen Sulfide Ivan Kushkevych 1,* , Veronika Bosáková 1,2 , Monika Vítˇezová 1 and Simon K.-M. R. Rittmann 3,* 1 Department of Experimental Biology, Faculty of Science, Masaryk University, 62500 Brno, Czech Republic; [email protected] (V.B.); [email protected] (M.V.) 2 Department of Biology, Faculty of Medicine, Masaryk University, 62500 Brno, Czech Republic 3 Archaea Physiology & Biotechnology Group, Department of Functional and Evolutionary Ecology, Universität Wien, 1090 Vienna, Austria * Correspondence: [email protected] (I.K.); [email protected] (S.K.-M.R.R.); Tel.: +420-549-495-315 (I.K.); +431-427-776-513 (S.K.-M.R.R.) Abstract: Hydrogen sulfide is a toxic compound that can affect various groups of water microorgan- isms. Photolithotrophic sulfur bacteria including Chromatiaceae and Chlorobiaceae are able to convert inorganic substrate (hydrogen sulfide and carbon dioxide) into organic matter deriving energy from photosynthesis. This process takes place in the absence of molecular oxygen and is referred to as anoxygenic photosynthesis, in which exogenous electron donors are needed. These donors may be reduced sulfur compounds such as hydrogen sulfide. This paper deals with the description of this metabolic process, representatives of the above-mentioned families, and discusses the possibility using anoxygenic phototrophic microorganisms for the detoxification of toxic hydrogen sulfide. Moreover, their general characteristics, morphology, metabolism, and taxonomy are described as Citation: Kushkevych, I.; Bosáková, well as the conditions for isolation and cultivation of these microorganisms will be presented. V.; Vítˇezová,M.; Rittmann, S.K.-M.R. -
Revised Glossary for AQA GCSE Biology Student Book
Biology Glossary amino acids small molecules from which proteins are A built abiotic factor physical or non-living conditions amylase a digestive enzyme (carbohydrase) that that affect the distribution of a population in an breaks down starch ecosystem, such as light, temperature, soil pH anaerobic respiration respiration without using absorption the process by which soluble products oxygen of digestion move into the blood from the small intestine antibacterial chemicals chemicals produced by plants as a defence mechanism; the amount abstinence method of contraception whereby the produced will increase if the plant is under attack couple refrains from intercourse, particularly when an egg might be in the oviduct antibiotic e.g. penicillin; medicines that work inside the body to kill bacterial pathogens accommodation ability of the eyes to change focus antibody protein normally present in the body acid rain rain water which is made more acidic by or produced in response to an antigen, which it pollutant gases neutralises, thus producing an immune response active site the place on an enzyme where the antimicrobial resistance (AMR) an increasing substrate molecule binds problem in the twenty-first century whereby active transport in active transport, cells use energy bacteria have evolved to develop resistance against to transport substances through cell membranes antibiotics due to their overuse against a concentration gradient antiretroviral drugs drugs used to treat HIV adaptation features that organisms have to help infections; they -
Limits of Life on Earth Some Archaea and Bacteria
Limits of life on Earth Thermophiles Temperatures up to ~55C are common, but T > 55C is Some archaea and bacteria (extremophiles) can live in associated usually with geothermal features (hot springs, environments that we would consider inhospitable to volcanic activity etc) life (heat, cold, acidity, high pressure etc) Thermophiles are organisms that can successfully live Distinguish between growth and survival: many organisms can survive intervals of harsh conditions but could not at high temperatures live permanently in such conditions (e.g. seeds, spores) Best studied extremophiles: may be relevant to the Interest: origin of life. Very hot environments tolerable for life do not seem to exist elsewhere in the Solar System • analogs for extraterrestrial environments • `extreme’ conditions may have been more common on the early Earth - origin of life? • some unusual environments (e.g. subterranean) are very widespread Extraterrestrial Life: Spring 2008 Extraterrestrial Life: Spring 2008 Grand Prismatic Spring, Yellowstone National Park Hydrothermal vents: high pressure in the deep ocean allows liquid water Colors on the edge of the at T >> 100C spring are caused by different colonies of thermophilic Vents emit superheated water (300C or cyanobacteria and algae more) that is rich in minerals Hottest water is lifeless, but `cooler’ ~50 species of such thermophiles - mostly archae with some margins support array of thermophiles: cyanobacteria and anaerobic photosynthetic bacteria oxidize sulphur, manganese, grow on methane + carbon monoxide etc… Sulfolobus: optimum T ~ 80C, minimum 60C, maximum 90C, also prefer a moderately acidic pH. Live by oxidizing sulfur Known examples can grow (i.e. multiply) at temperatures which is abundant near hot springs. -
Marine Microorganisms: Evolution and Solution to Pollution Fu L Li1, Wang B1,2
COMMENTARY Marine microorganisms: Evolution and solution to pollution Fu L Li1, Wang B1,2 Li FL, Wang B. Marine microorganisms: Evolution and solution to pollution. J Mar Microbiol. 2018;2(1):4-5. nce ocean nurtured life, now she needs our care. Marine microorganism will be an opportunity to further understand ourselves and to seek for new Ois the host of ocean in all ages. We should learn from them humbly. methods of fighting old infections. Marine microorganism is tightly bond with human during the history of evolution and nowadays’ environment pollution. Along with industrial revolution, our marine ecosystem suffered serious pollutions. Microplastics are tiny plastic particles (<5 mm) (Figure 1B), Although the topic is still in debate, life is probably originated from which poison marine lives. Because these microplastics are very hard to be submarine in hydrothermal vent systems (1). In the journey of evolution, our degraded, it is predicted that there will be more microplastics than fish in biosphere was completely dominated by microbes for a very long time (Figure ocean by the year 2050 (7). Since marine sediments are considered as the sink 1A). Human being evolves with those microorganisms. Consequently, of microplastics and marine microbes are key dwellers of marine sediments, the influences of microorganisms can be found in all aspects of human more attention should be paid on the interactions between microplastics biology. More than 65% of our genes originated with bacteria, archaea, and and marine microbes. Actually, a call for this has been published in 2011 unicellular eukaryotes, including those genes responsible for host-microbe (8). -
Lokiarchaeota: Biologists Discover 'Missing Link' Microorganism
Home About Us News Archive Copyright Privacy Policy Contact Us Newsletter RSS HOME ASTRONOMY SPACE EXPLORATION ARCHAEOLOGY PALEONTOLOGY BIOLOGY PHYSICS Lokiarchaeota: Biologists Discover ‘Missing Link’ Microorganism May 7, 2015 by Sci-News.com « PREVIOUS Published in A team of biologists, co-led by Dr Lionel Guy and Dr Thijs J. G. Ettema from Biology Uppsala University in Sweden, has discovered a new group of Tagged as microorganisms that represents an intermediate form in-between the Archaea simple cells of bacteria and the complex cell types of eukaryotes. Bacteria Eukaryote Lokiarchaeota Follow Like 16k Share Tweet 12 Like 58 41 You Might Like Bottlenose Dolphins Form Highly Complex Networks of Friends Rorqual Whales This false-color image shows a cell of thermophilic methanogenic archaea. Image credit: University of Have Unique California Museum of Paleontology. Stretchy Nerves In 1977, biochemist Dr Carl Woese and his colleagues at the University of Illinois described an entirely new group of organisms, the Archaea (originally found in extreme environments, such as hydrothermal vents and terrestrial hot springs). The scientists were studying relationships among the prokaryotes using DNA Extinction of sequences, and found that Archaea have distinct molecular characteristics World’s Largest separating them from bacteria as well as from eukaryotes. They proposed that Herbivores May Lead to Empty life can be divided into three domains: Eukaryota, Eubacteria, and Landscapes, Say Archaebacteria. Researchers Despite that archaeal cells were simple and small like bacteria, scientists found that Archaea were more closely related to organisms with complex cell types, a group collectively known as ‘eukaryotes.’ This observation has puzzled Sichuan Bush biologists for years. -
Laboratory Exercises in Microbiology: Discovering the Unseen World Through Hands-On Investigation
City University of New York (CUNY) CUNY Academic Works Open Educational Resources Queensborough Community College 2016 Laboratory Exercises in Microbiology: Discovering the Unseen World Through Hands-On Investigation Joan Petersen CUNY Queensborough Community College Susan McLaughlin CUNY Queensborough Community College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/qb_oers/16 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Laboratory Exercises in Microbiology: Discovering the Unseen World through Hands-On Investigation By Dr. Susan McLaughlin & Dr. Joan Petersen Queensborough Community College Laboratory Exercises in Microbiology: Discovering the Unseen World through Hands-On Investigation Table of Contents Preface………………………………………………………………………………………i Acknowledgments…………………………………………………………………………..ii Microbiology Lab Safety Instructions…………………………………………………...... iii Lab 1. Introduction to Microscopy and Diversity of Cell Types……………………......... 1 Lab 2. Introduction to Aseptic Techniques and Growth Media………………………...... 19 Lab 3. Preparation of Bacterial Smears and Introduction to Staining…………………...... 37 Lab 4. Acid fast and Endospore Staining……………………………………………......... 49 Lab 5. Metabolic Activities of Bacteria…………………………………………….…....... 59 Lab 6. Dichotomous Keys……………………………………………………………......... 77 Lab 7. The Effect of Physical Factors on Microbial Growth……………………………... 85 Lab 8. Chemical Control of Microbial Growth—Disinfectants and Antibiotics…………. 99 Lab 9. The Microbiology of Milk and Food………………………………………………. 111 Lab 10. The Eukaryotes………………………………………………………………........ 123 Lab 11. Clinical Microbiology I; Anaerobic pathogens; Vectors of Infectious Disease….. 141 Lab 12. Clinical Microbiology II—Immunology and the Biolog System………………… 153 Lab 13. Putting it all Together: Case Studies in Microbiology…………………………… 163 Appendix I. -
PROTISTS Shore and the Waves Are Large, Often the Largest of a Storm Event, and with a Long Period
(seas), and these waves can mobilize boulders. During this phase of the storm the rapid changes in current direction caused by these large, short-period waves generate high accelerative forces, and it is these forces that ultimately can move even large boulders. Traditionally, most rocky-intertidal ecological stud- ies have been conducted on rocky platforms where the substrate is composed of stable basement rock. Projec- tiles tend to be uncommon in these types of habitats, and damage from projectiles is usually light. Perhaps for this reason the role of projectiles in intertidal ecology has received little attention. Boulder-fi eld intertidal zones are as common as, if not more common than, rock plat- forms. In boulder fi elds, projectiles are abundant, and the evidence of damage due to projectiles is obvious. Here projectiles may be one of the most important defi ning physical forces in the habitat. SEE ALSO THE FOLLOWING ARTICLES Geology, Coastal / Habitat Alteration / Hydrodynamic Forces / Wave Exposure FURTHER READING Carstens. T. 1968. Wave forces on boundaries and submerged bodies. Sarsia FIGURE 6 The intertidal zone on the north side of Cape Blanco, 34: 37–60. Oregon. The large, smooth boulders are made of serpentine, while Dayton, P. K. 1971. Competition, disturbance, and community organi- the surrounding rock from which the intertidal platform is formed zation: the provision and subsequent utilization of space in a rocky is sandstone. The smooth boulders are from a source outside the intertidal community. Ecological Monographs 45: 137–159. intertidal zone and were carried into the intertidal zone by waves. Levin, S. A., and R. -
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. -
Algae and Cyanobacteria in Coastal and Estuarine Waters
CHAPTER 7 Algae and cyanobacteria in coastal and estuarine waters n coastal and estuarine waters, algae range from single-celled forms to the seaweeds. ICyanobacteria are organisms with some characteristics of bacteria and some of algae. They are similar in size to the unicellular algae and, unlike other bacteria, contain blue-green or green pigments and are able to perform photosynthesis; thus, they are also termed blue-green algae. Algal blooms in the sea have occurred throughout recorded history but have been increasing during recent decades (Anderson, 1989; Smayda, 1989a; Hallegraeff, 1993). In several areas (e.g., the Baltic and North seas, the Adriatic Sea, Japanese coastal waters and the Gulf of Mexico), algal blooms are a recurring phe- nomenon. The increased frequency of occurrence has accompanied nutrient enrich- ment of coastal waters on a global scale (Smayda, 1989b). Blooms of non-toxic phytoplankton species and mass occurrences of macro-algae can affect the amenity value of recreational waters due to reduced transparency, dis- coloured water and scum formation. Furthermore, bloom degradation can be accom- panied by unpleasant odours, resulting in aesthetic problems (see chapter 9). Several human diseases have been reported to be associated with many toxic species of dinoflagellates, diatoms, nanoflagellates and cyanobacteria that occur in the marine environment (CDC, 1997). The effects of these algae on humans are due to some of their constituents, principally algal toxins. Marine algal toxins become a problem primarily because they may concentrate in shellfish and fish that are subsequently eaten by humans (CDR, 1991; Lehane, 2000), causing syndromes known as para- lytic shellfish poisoning (PSP), diarrhetic shellfish poisoning (DSP), amnesic shellfish poisoning (ASP), neurotoxic shellfish poisoning (NSP) and ciguatera fish poisoning (CFP). -
L Deposits of Microorganisms and Other Biological Material L
PCT Applicant’s Guide – International Phase – Annex L Page 1 L Deposits of Microorganisms L and Other Biological Material Requirements of designated and elected Offices Only Offices whose applicable national law contains provisions concerning the deposits of microorganisms and other biological material are listed in this table. Unless otherwise indicated in the table, deposits may be made for the purposes of patent procedure before these Offices with any depositary institution having acquired the status of international depositary authority under the Budapest Treaty on the International Recognition of the Deposit of Microorganisms for the Purposes of Patent Procedure (these institutions are indicated further in this Annex and notifications related thereto may be consulted under www.wipo.int/treaties/en/registration/budapest/). Further information concerning the requirements of international depository authorities under the Budapest Treaty is available at www.wipo.int/treaties/en/registration/budapest/guide/ Time (if any) earlier than Additional indications (if any) 16 months from priority date by which must be given besides which applicant must furnish: those prescribed in Rule 13bis.3(a)(i) to (iii) Designated the indications any additional pursuant to notifications from (or elected) Office prescribed in matter specified the Offices concerned Rule 13bis.3(a)(i) in the adjacent to (iii) right-hand column AL – Albania General Directorate of None At the time of To the extent available to the Industrial Property (GDIP) filing (as part of applicant, relevant information (Albania) the application) on the characteristics of the microorganism Deposits may also be made for the purposes of patent procedure before the General Directorate of Industrial Property (GDIP) (Albania) with any depositary institution specialized for that purpose. -
The Unicellular and Colonial Organisms Prokaryotic And
The Unicellular and Colonial Organisms Prokaryotic and Eukaryotic Cells As you know, the building blocks of life are cells. Prokaryotic cells are those cells that do NOT have a nucleus. They mostly include bacteria and archaea. These cells do not have membrane-bound organelles. Eukaryotic cells are those that have a true nucleus. That would include plant, animal, algae, and fungal cells. As you can see, to the left, eukaryotic cells are typically larger than prokaryotic cells. Today in lab, we will look at examples of both prokaryotic and eukaryotic unicellular organisms that are commonly found in pond water. When examining pond water under a microscope… The unpigmented, moving microbes will usually be protozoans. Greenish or golden-brown organisms will typically be algae. Microorganisms that are blue-green will be cyanobacteria. As you can see below, living things are divided into 3 domains based upon shared characteristics. Domain Eukarya is further divided into 4 Kingdoms. Domain Kingdom Cell type Organization Nutrition Organisms Absorb, Unicellular-small; Prokaryotic Photsyn., Archaeacteria Archaea Archaebacteria Lacking peptidoglycan Chemosyn. Unicellular-small; Absorb, Bacteria, Prokaryotic Peptidoglycan in cell Photsyn., Bacteria Eubacteria Cyanobacteria wall Chemosyn. Ingestion, Eukaryotic Unicellular or colonial Protozoa, Algae Protista Photosynthesis Fungi, yeast, Fungi Eukaryotic Multicellular Absorption Eukarya molds Plantae Eukaryotic Multicellular Photosynthesis Plants Animalia Eukaryotic Multicellular Ingestion Animals Prokaryotic Organisms – the archaea, non-photosynthetic bacteria, and cyanobacteria Archaea - Microorganisms that resemble bacteria, but are different from them in certain aspects. Archaea cell walls do not include the macromolecule peptidoglycan, which is always found in the cell walls of bacteria. Archaea usually live in extreme, often very hot or salty environments, such as hot mineral springs or deep-sea hydrothermal vents.