Composition of Prokaryotic and Eukaryotic Microbial Communities in Waters Around the Florida Reef Tract
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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. -
Norway and Its Marine Areas - a Brief Description of the Sea Floor
No.3 2003 IN FOCUS Norway and its marine areas - a brief description of the sea floor From the deep sea to the fjord floor Norwegian waters comprise widely differing environments - from the Bjørnøyrenna deep sea via the continental slope and continental shelf to the coastal zone with its strandflat, archipelagos and fjords.This constitutes a geologi- cal diversity that is unique in a European context. An exciting geological history lies Trænadjupet behind this diversity - a development that has taken place over more than 400 million years.The continents con- Vøringplatået sist of plates of solidified rock that float on partially molten rock, and these plates move relative to one another.Where they collide, the Earth's crust is folded and mountain chains are created.Where they drift apart, deep oceans form and new sea Storegga floor is created along rifts because molten rock (magma) streams up from below. A good example is the Mid-Atlantic Ridge, including Iceland, a which is a result of Greenland and n n e Europe drifting from each other at a r e rate of about 2 cm a year. k s r o The plates on which Norway and N Greenland rest collided more than 400 million years ago and formed mountain chains on either side of a Skagerrak shallow sea. Both Greenland and Norway are remnants of worn down mountain chains. Between these mountain chains, the shallow sea Figure 1.Norway and its neighbouring seas. gradually filled with sediments derived from the erosion of the chains.These sedi- ments became transformed into sandstones, shales and limestones and it is in these rocks we now find oil and gas on the Norwegian continental shelf. -
THE CASE AGAINST Marine Mammals in Captivity Authors: Naomi A
s l a m m a y t T i M S N v I i A e G t A n i p E S r a A C a C E H n T M i THE CASE AGAINST Marine Mammals in Captivity The Humane Society of the United State s/ World Society for the Protection of Animals 2009 1 1 1 2 0 A M , n o t s o g B r o . 1 a 0 s 2 u - e a t i p s u S w , t e e r t S h t u o S 9 8 THE CASE AGAINST Marine Mammals in Captivity Authors: Naomi A. Rose, E.C.M. Parsons, and Richard Farinato, 4th edition Editors: Naomi A. Rose and Debra Firmani, 4th edition ©2009 The Humane Society of the United States and the World Society for the Protection of Animals. All rights reserved. ©2008 The HSUS. All rights reserved. Printed on recycled paper, acid free and elemental chlorine free, with soy-based ink. Cover: ©iStockphoto.com/Ying Ying Wong Overview n the debate over marine mammals in captivity, the of the natural environment. The truth is that marine mammals have evolved physically and behaviorally to survive these rigors. public display industry maintains that marine mammal For example, nearly every kind of marine mammal, from sea lion Iexhibits serve a valuable conservation function, people to dolphin, travels large distances daily in a search for food. In learn important information from seeing live animals, and captivity, natural feeding and foraging patterns are completely lost. -
Marine Microplankton Ecology Reading
Marine Microplankton Ecology Reading Microbes dominate our planet, especially the Earth’s oceans. The distinguishing feature of microorganisms is their small size, usually defined as less than 200 micrometers (µm); they are all invisible to the naked eye. As a group, sea microbes are extremely diverse, and extremely versatile with respect to their abilities to make and eat food. All marine microbes are too small to swim against the current and are therefore classified as plankton. First we will discuss several ways to classify marine microbes. 1. Size Planktonic marine organisms can be divided into the following size categories: Category Size femtoplankton <0.2 µm picoplankton 0.2-2 µm nanoplankton 2-20 µm microplankton 20-200 µm mesoplankton 200-2000 µm In this laboratory we are concerned with the microscopic portion of the plankton, less than 200 µm. These organisms are not visible to the naked eye (Figure 1). Figure 1. Size classes of marine plankton 2. Type A. Viruses Viruses are the smallest and simplest microplankton. They range from 0.01 to 0.3 um in diameter. Externally, viruses have a capsid, or protein coat. Viruses can also have simple or complex external morphologies with tail fibers and structures that are used to inject DNA or RNA into their host. Viruses have little internal morphology. They do not have a nucleus or organelles. They do not have chlorophyll. Inside a virus there is only nucleic acid, either DNA or RNA. Viruses do not grow and have no metabolism. Marine viruses are highly abundant. There are up to 10 billion in one liter of seawater! B. -
Human Microbiome: Your Body Is an Ecosystem
Human Microbiome: Your Body Is an Ecosystem This StepRead is based on an article provided by the American Museum of Natural History. What Is an Ecosystem? An ecosystem is a community of living things. The living things in an ecosystem interact with each other and with the non-living things around them. One example of an ecosystem is a forest. Every forest has a mix of living things, like plants and animals, and non-living things, like air, sunlight, rocks, and water. The mix of living and non-living things in each forest is unique. It is different from the mix of living and non-living things in any other ecosystem. You Are an Ecosystem The human body is also an ecosystem. There are trillions tiny organisms living in and on it. These organisms are known as microbes and include bacteria, viruses, and fungi. There are more of them living on just your skin right now than there are people on Earth. And there are a thousand times more than that in your gut! All the microbes in and on the human body form communities. The human body is an ecosystem. It is home to trillions of microbes. These communities are part of the ecosystem of the human Photo Credit: Gaby D’Alessandro/AMNH body. Together, all of these communities are known as the human microbiome. No two human microbiomes are the same. Because of this, you are a unique ecosystem. There is no other ecosystem like your body. Humans & Microbes Microbes have been around for more than 3.5 billion years. -
Archaeal Distribution and Abundance in Water Masses of the Arctic Ocean, Pacific Sector
Vol. 69: 101–112, 2013 AQUATIC MICROBIAL ECOLOGY Published online April 30 doi: 10.3354/ame01624 Aquat Microb Ecol FREEREE ACCESSCCESS Archaeal distribution and abundance in water masses of the Arctic Ocean, Pacific sector Chie Amano-Sato1, Shohei Akiyama1, Masao Uchida2, Koji Shimada3, Motoo Utsumi1,* 1University of Tsukuba, Tennodai, Tsukuba, Ibaraki 305-8572, Japan 2National Institute for Environmental Studies, Onogawa, Tsukuba, Ibaraki 305-8506, Japan 3Tokyo University of Marine Science and Technology, Konan, Minato-ku, Tokyo 108-8477, Japan ABSTRACT: Marine planktonic Archaea have been recently recognized as an ecologically impor- tant component of marine prokaryotic biomass in the world’s oceans. Their abundance and meta- bolism are closely connected with marine geochemical cycling. We evaluated the distribution of planktonic Archaea in the Pacific sector of the Arctic Ocean using fluorescence in situ hybridiza- tion (FISH) with catalyzed reporter deposition (CARD-FISH) and performed statistical analyses using data for archaeal abundance and geochemical variables. The relative abundance of Thaum - archaeota generally increased with depth, and euryarchaeal abundance was the lowest of all planktonic prokaryotes. Multiple regression analysis showed that the thaumarchaeal relative abundance was negatively correlated with ammonium and dissolved oxygen concentrations and chlorophyll fluorescence. Canonical correspondence analysis showed that archaeal distributions differed with oceanographic water masses; in particular, Thaumarchaeota were abundant from the halocline layer to deep water, where salinity was higher and most nutrients were depleted. However, at several stations on the East Siberian Sea side of the study area and along the North- wind Ridge, Thaumarchaeota and Bacteria were proportionally very abundant at the bottom in association with higher nutrient conditions. -
About Cyanobacteria BACKGROUND Cyanobacteria Are Single-Celled Organisms That Live in Fresh, Brackish, and Marine Water
About Cyanobacteria BACKGROUND Cyanobacteria are single-celled organisms that live in fresh, brackish, and marine water. They use sunlight to make their own food. In warm, nutrient-rich environments, microscopic cyanobacteria can grow quickly, creating blooms that spread across the water’s surface and may become visible. Because of the color, texture, and location of these blooms, the common name for cyanobacteria is blue-green algae. However, cyanobacteria are related more closely to bacteria than to algae. Cyanobacteria are found worldwide, from Brazil to China, Australia to the United States. In warmer climates, these organisms can grow year-round. Scientists have called cyanobacteria the origin of plants, and have credited cyanobacteria with providing nitrogen fertilizer for rice and beans. But blooms of cyanobacteria are not always helpful. When these blooms become harmful to the environment, animals, and humans, scientists call them cyanobacterial harmful algal blooms (CyanoHABs). Freshwater CyanoHABs can use up the oxygen and block the sunlight that other organisms need to live. They also can produce powerful toxins that affect the brain and liver of animals and humans. Because of concerns about CyanoHABs, which can grow in drinking water and recreational water, the U.S. Environmental Protection Agency (EPA) has added cyanobacteria to its Drinking Water Contaminant Candidate List. This list identifies organisms and toxins that EPA considers to be priorities for investigation. ASSESSING THE IMPACT ON PUBLIC HEALTH Reports of poisonings associated with CyanoHABs date back to the late 1800s. Anecdotal evidence and data from laboratory animal research suggest that cyanobacterial toxins can cause a range of adverse human health effects, yet few studies have explored the links between CyanoHABs and human health. -
THE LIBERATION of OSLO and COPENHAGEN: a MIDSHIPMAN's MEMOIR C.B. Koester
THE LIBERATION OF OSLO AND COPENHAGEN: A MIDSHIPMAN'S MEMOIR C.B. Koester Introduction I joined HMS Devonshire, a County-class cruiser in the Home Fleet, on 16 September 1944. For the next nine months we operated out of Scapa Flow, the naval base in the Orkneys north of Scotland which had been home to Jellicoe's Grand Fleet during World War I and harboured the main units of the Home Fleet throughout the second conflict. It was a bleak, uninviting collection of seventy-three islands—at low water—twenty-nine of them inhabited, mainly by fishermen and shepherds. Winters were generally miserable and the opportunities for recreation ashore limited. There was boat-pulling and sailing, weather permitting; an occasional game of field hockey on the naval sports ground; and perhaps a Saturday afternoon concert in the fleet canteen or a "tea dance" at the Wrennery. Otherwise, we entertained ourselves aboard: singsongs in the Gunroom; a Sunday night film in the Wardroom; deck hockey in the Dog Watches; and endless games of "liar's dice." Our operations at sea were more harrowing, but only marginally more exciting, consisting mainly of attacks on German shore installations on the Norwegian coast. We rarely saw the coastline, however, for the strikes were carried out by aircraft flying from the escort carriers in the task force. At the same time, we had to be prepared for whatever counterattack the Germans might mount, and until Tirpitz was finally disabled on 12 November 1944, such a riposte might have been severe. That and the ever-present threat of submarines notwithstanding, for most of us these operations involved a large measure of boredom and discomfort. -
Antibiotics from Deep-Sea Microorganisms: Current Discoveries and Perspectives
marine drugs Review Antibiotics from Deep-Sea Microorganisms: Current Discoveries and Perspectives Emiliana Tortorella 1,†, Pietro Tedesco 1,2,†, Fortunato Palma Esposito 1,3,†, Grant Garren January 1,†, Renato Fani 4, Marcel Jaspars 5 and Donatella de Pascale 1,3,* 1 Institute of Protein Biochemistry, National Research Council, I-80131 Naples, Italy; [email protected] (E.T.); [email protected] (P.T.); [email protected] (F.P.E.); [email protected] (G.G.J.) 2 Laboratoire d’Ingénierie des Systèmes Biologiques et des Procédés, INSA, 31400 Toulouse, France 3 Stazione Zoologica “Anthon Dorn”, Villa Comunale, I-80121 Naples, Italy 4 Department of Biology, University of Florence, Sesto Fiorentino, I-50019 Florence, Italy; renato.fani@unifi.it 5 Marine Biodiscovery Centre, Department of Chemistry, University of Aberdeen, Aberdeen, Scotland AB24 3UE, UK; [email protected] * Correspondence: [email protected]; Tel.: +39-0816-132-314; Fax: +39-0816-132-277 † These authors equally contributed to the work. Received: 23 July 2018; Accepted: 27 September 2018; Published: 29 September 2018 Abstract: The increasing emergence of new forms of multidrug resistance among human pathogenic bacteria, coupled with the consequent increase of infectious diseases, urgently requires the discovery and development of novel antimicrobial drugs with new modes of action. Most of the antibiotics currently available on the market were obtained from terrestrial organisms or derived semisynthetically from fermentation products. The isolation of microorganisms from previously unexplored habitats may lead to the discovery of lead structures with antibiotic activity. The deep-sea environment is a unique habitat, and deep-sea microorganisms, because of their adaptation to this extreme environment, have the potential to produce novel secondary metabolites with potent biological activities. -
The Tautra Cold-Water Coral Reef
The Tautra Cold-Water Coral Reef Mapping and describing the biodiversity of a cold-water coral reef ecosystem in the Trondheimsfjord by use of multi-beam echo sounding and video mounted on a remotely operated vehicle June Jakobsen Marine Coastal Development Submission date: May 2016 Supervisor: Geir Johnsen, IBI Co-supervisor: Svein Karlsen, Fylkesmannen i Nord-Trøndelag Martin Ludvigsen, IMT Torkild Bakken, NTNU, Vitenskapsmuseet Norwegian University of Science and Technology Department of Biology i Contents Acknowledgements ................................................................................................................................. iii List of Abbreviations: .............................................................................................................................. iv Abstract: ................................................................................................................................................... v Sammendrag ............................................................................................................................................ vi Introduction: ............................................................................................................................................ 1 Theory ..................................................................................................................................................... 2 The geology of the fjord ..................................................................................................................... -
Local Controls on Sediment Accumulation and Distribution in a Fjord in the West Antarctic Peninsula: Implications for Palaeoenvironmental Interpretations Yuribia P
RESEARCH/REVIEW ARTICLE Local controls on sediment accumulation and distribution in a fjord in the West Antarctic Peninsula: implications for palaeoenvironmental interpretations Yuribia P. Munoz & Julia S. Wellner Department of Earth and Atmospheric Sciences, University of Houston, 4800 Calhoun Road, Houston, TX 77204, USA Keywords Abstract Flandres Bay; Antarctic Peninsula; sediment We analyse surface sediment and its distribution in Flandres Bay, West Antarctic distribution; grain size. Peninsula, in order to understand modern day sediment dispersal patterns in Correspondence a fjord with retreating, tidewater glaciers. The surface sediment descriptions Yuribia P. Munoz, Department of Earth and of 41 cores are included in this study. The sediment facies described include Atmospheric Sciences, University of muddy diatomaceous ooze, diatomaceous mud, pebbly mud, sandy mud and Houston, 4800 Calhoun Road, Houston, mud, with scattered pebbles present in most samples. In contrast to a traditional TX 77204, USA. E-mail: [email protected] conceptual model of glacial sediment distribution in fjords, grain size in Flandres Bay generally coarsens from the inner to outer bay. The smallest grain size sediments were found in the bay head and are interpreted as fine-grained deposits resulting from meltwater plumes and sediment gravity flows occurring close to the glacier front. The middle of the bay is characterized by a high silt percentage, which correlates to diatom-rich sediments. Sediments in the outer bay have a high component of coarse material, which is interpreted as being the result of winnowing from currents moving from the Bellingshausen Sea into the Gerlache Strait. Palaeoenvironmental reconstructions of glacial environ- ments often use grain size as an indicator of proximity to the ice margin. -
California State University, Northridge an Ecological
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE AN ECOLOGICAL AND PHYSIOLOGICAL ASSESSMENT OF TROPICAL CORAL REEF RESPONSES TO PAST AND PROJECTED DISTURBANCES A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Biology By Elizabeth Ann Lenz May 2014 The thesis of Elizabeth A. Lenz is approved by: Robert C. Carpenter, Ph.D. Date: Eric D. Sanford, Ph.D. Date: Mark A. Steele, Ph.D. Date: Peter J. Edmunds, Ph.D., Chair Date: California State University, Northridge ii ACKNOWLEDGEMENTS I would like to thank Dr. Peter J. Edmunds first and foremost for being my fearless leader and advisor - for the incredible opportunities and invaluable mentorship he has provided to me as a graduate student in the Polyp Lab. I am ever so grateful for his guidance, endless caffeinated energy, constructive critiques, and dry British humor. I would also like to thank my loyal committee members Drs. Robert Carpenter and Mark Steele at CSUN for their availability and expert advise during this process. Their suggestions have greatly contributed to my thesis. I would not only like to acknowledge Dr. Eric Sanford from UC Davis for serving on my committee, but thank him for his incessant support throughout my career over the last 7 years. I will always admire his contagious enthusiasm for invertebrates, passion for scientific research, and unlimited knowledge about marine ecology. My research would not have been possible without the technical support and assistance from my colleagues in Moorea, French Polynesia and St. John, USVI. I am grateful to Dr. Lorenzo Bramanti, Dr. Steeve Comeau, Vince Moriarty, Nate Spindel, Emily Rivest, Christopher Wall, Darren Brown, Alexandre Yarid, Nicolas Evensen, Craig Didden, the VIERS staff, and undergraduate assistants: Kristin Privitera-Johnson and Amanda Arnold.