Microbial Mat Ecosystems: Structure Types, Functional Diversity, and Biotechnological Application
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A Study on the Phototrophic Microbial Mat Communities of Sulphur Mountain Thermal Springs and Their Association with the Endangered, Endemic Snail Physella Johnsoni
A Study on the Phototrophic Microbial Mat Communities of Sulphur Mountain Thermal Springs and their Association with the Endangered, Endemic Snail Physella johnsoni By Michael Bilyj A thesis submitted to the Faculty of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science Department of Microbiology Faculty of Science University of Manitoba Winnipeg, Manitoba October 2011 © Copyright 2011, Michael A. Bilyj 1 Abstract The seasonal population fluctuation of anoxygenic phototrophs and the diversity of cyanobacteria at the Sulphur Mountain thermal springs of Banff, Canada were investigated and compared to the drastic population changes of the endangered snail Physella johnsoni. A new species and two strains of Rhodomicrobium were taxonomically characterized in addition to new species of Rhodobacter and Erythromicrobium. Major mat-forming organisms included Thiothrix-like species, oxygenic phototrophs of genera Spirulina, Oscillatoria, and Phormidium and purple nonsulfur bacteria Rhodobacter, Rhodopseudomonas and Rhodomicrobium. Aerobic anoxygenic phototrophs comprised upwards of 9.6 x 104 CFU/cm2 of mat or 18.9% of total aerobic heterotrophic bacterial isolates at certain sites, while maximal purple nonsulfur and purple sulfur bacteria were quantified at 3.2 x 105 and 2.0 x 106 CFU/cm2 of mat, respectively. Photosynthetic activity measurements revealed incredibly productive carbon fixation rates averaging 40.5 mg C/cm2/24 h. A temporal mismatch was observed for mat area and prokaryote-based organics to P. johnsoni population flux in a ―tracking inertia‖ manner. 2 Acknowledgements It is difficult to express sufficient gratitude to my supervisor Dr. Vladimir Yurkov for his unfaltering patience, generosity and motivation throughout this entire degree. -
7.014 Handout PRODUCTIVITY: the “METABOLISM” of ECOSYSTEMS
7.014 Handout PRODUCTIVITY: THE “METABOLISM” OF ECOSYSTEMS Ecologists use the term “productivity” to refer to the process through which an assemblage of organisms (e.g. a trophic level or ecosystem assimilates carbon. Primary producers (autotrophs) do this through photosynthesis; Secondary producers (heterotrophs) do it through the assimilation of the organic carbon in their food. Remember that all organic carbon in the food web is ultimately derived from primary production. DEFINITIONS Primary Productivity: Rate of conversion of CO2 to organic carbon (photosynthesis) per unit surface area of the earth, expressed either in terns of weight of carbon, or the equivalent calories e.g., g C m-2 year-1 Kcal m-2 year-1 Primary Production: Same as primary productivity, but usually expressed for a whole ecosystem e.g., tons year-1 for a lake, cornfield, forest, etc. NET vs. GROSS: For plants: Some of the organic carbon generated in plants through photosynthesis (using solar energy) is oxidized back to CO2 (releasing energy) through the respiration of the plants – RA. Gross Primary Production: (GPP) = Total amount of CO2 reduced to organic carbon by the plants per unit time Autotrophic Respiration: (RA) = Total amount of organic carbon that is respired (oxidized to CO2) by plants per unit time Net Primary Production (NPP) = GPP – RA The amount of organic carbon produced by plants that is not consumed by their own respiration. It is the increase in the plant biomass in the absence of herbivores. For an entire ecosystem: Some of the NPP of the plants is consumed (and respired) by herbivores and decomposers and oxidized back to CO2 (RH). -
Is It Essential to Sequence the Entire 16S Rrna Gene for Bacterial
» INSTRUMENTATION » Is it Essential to Sequence Introduction Bacterial Identification in the biopharmaceutical industry, especially in the Entire 16S rRNA Gene manufacturing facilities, is very important because an occurrence of a problematic microorganism in the final product could be harmful for the end user and detrimental to a company’s finances and reputation. for Bacterial Identification? Environmental Monitoring (EM) programs are the cornerstone of understanding the microbial ecology in a manufacturing facility and have become a regulatory requirement for most manufacturers. The EM program is a biological surveillance system which enables companies to quickly identify organisms which are transient or resident in their facilities before these organisms have an opportunity to contaminate a product. A properly executed EM program provides an early warning of potential contamination problems due to Sunhee Hong, PhD and equipment failure, inadequate cleaning, or deficiencies in staff hygiene Christine E. Farrance, PhD training, for example, so that problems can be corrected to prevent Charles River adulteration of the end product. The Food and Drug Administration (FDA) has published guidelines for the production of sterile drugs by aseptic processing which includes a section on EM programs, and the USP general information chapter “Microbiological Control and Monitoring of Aseptic Processing Environments” also contains detailed information regarding EM programs1. The EM program is only effective if the organisms recovered from the facility are accurately identified, so the information gathered can be used to understand the microbial control through tracking and trending and dictate appropriate remediation activities. There are several different options available for bacterial identification; however, the use of 16S rRNA gene sequences has been considered the most powerful and accurate tool, while conventional phenotypic methods often show major weaknesses2-5. -
Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-Rich, Geothermal Spring 2 3 Lewis M
bioRxiv preprint doi: https://doi.org/10.1101/428698; this version posted September 27, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-rich, Geothermal Spring 2 3 Lewis M. Ward1,2,3*, Airi Idei4, Mayuko Nakagawa2,5, Yuichiro Ueno2,5,6, Woodward W. 4 Fischer3, Shawn E. McGlynn2* 5 6 1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA 7 2. Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, 152-8550, Japan 8 3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 9 91125 USA 10 4. Department of Biological Sciences, Tokyo Metropolitan University, Hachioji, Tokyo 192-0397, 11 Japan 12 5. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 13 152-8551, Japan 14 6. Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth 15 Science and Technology, Natsushima-cho, Yokosuka 237-0061, Japan 16 Correspondence: [email protected] or [email protected] 17 18 Abstract 19 Hydrothermal systems, including terrestrial hot springs, contain diverse and systematic 20 arrays of geochemical conditions that vary over short spatial scales due to progressive interaction 21 between the reducing hydrothermal fluids, the oxygenated atmosphere, and in some cases 22 seawater. At Jinata Onsen, on Shikinejima Island, Japan, an intertidal, anoxic, iron- and 23 hydrogen-rich hot spring mixes with the oxygenated atmosphere and sulfate-rich seawater over 24 short spatial scales, creating an enormous range of redox environments over a distance ~10 m. -
The Vulnerability of Microbial Ecosystems in a Changing Climate: Potential Impact in Shark Bay
life Review The Vulnerability of Microbial Ecosystems in a Changing Climate: Potential Impact in Shark Bay Max Reinold 1,2, Hon Lun Wong 1,2, Fraser I. MacLeod 1,2, Julia Meltzer 1,2, April Thompson 1,2 and Brendan P. Burns 1,2,* 1 School of Biotechnology and Biomolecular Sciences, The University of New South Wales, Sydney 2052, Australia 2 Australian Centre for Astrobiology, The University of New South Wales, Sydney 2052, Australia * Correspondence: [email protected]; Tel.: +612-9385-3659; Fax: +612-9385-1591 Received: 30 July 2019; Accepted: 28 August 2019; Published: 2 September 2019 Abstract: The potential impact of climate change on eukaryotes, including humans, has been relatively well described. In contrast, the contribution and susceptibility of microorganisms to a changing climate have, until recently, received relatively less attention. In this review, the importance of microorganisms in the climate change discourse is highlighted. Microorganisms are responsible for approximately half of all primary production on earth, support all forms of macroscopic life whether directly or indirectly, and often persist in “extreme” environments where most other life are excluded. In short, microorganisms are the life support system of the biosphere and therefore must be included in decision making regarding climate change. Any effects climate change will have on microorganisms will inevitably impact higher eukaryotes and the activity of microbial communities in turn can contribute to or alleviate the severity of the changing climate. It is of vital importance that unique, fragile, microbial ecosystems are a focus of research efforts so that their resilience to extreme weather events and climate change are thoroughly understood and that conservation efforts can be implemented as a response. -
Interactions Between Photosynthesis and Respiration in an Aquatic Ecosystem
Interactions between Photosynthesis and Respiration in an Aquatic Ecosystem Jane E. Caldwell and Kristi Teagarden 53 Campus Drive, P.O. Box 6057 Dept. of Biology West Virginia University Morgantown, WV 26506 [email protected] (304)293-5201 extension 31459 [email protected] (304)293-5201 extension 31542 Abstract: Students measure the results of respiration and photosynthesis separately, combined, and in comparison to a non-living control “ecosystem”. The living ecosystem uses only snails and water plants. Oxygen, carbon dioxide, and ammonia nitrogen concentrations are measured with simple colorimetric and titration water tests using commercially available kits. The exercise is designed for large enrollment non-majors labs, but modifications for large and small classrooms are described. Introduction This lab exercise was developed for a freshman course for non-science majors at West Virginia University. The exercise asks students to apply their knowledge of basic metabolic processes to a series of simple aquatic ecosystems, which students monitor through water testing. These ecosystems consist of aquaria containing plants and/or snails with or without light exposure, and are compared against a non-living control system (an aquarium with water, light, and gravel). As they analyze their results, students observe the interplay of respiration, photosynthesis, protein digestion (or waste excretion), and decomposition through their effects on dissolved oxygen, carbon dioxide, and ammonia. Students synthesize these observations into written explanations of their results. During the course of the lab, students: • predict the relative levels of oxygen, carbon dioxide, and ammonia for various aquaria compared to a control aquarium. • observe and conduct titrimetric and colorimetric tests for dissolved compounds in water. -
The Mysterious Microbial Mats
Submarine Ring of Fire 2012: NE Lau Basin Expedition The Mysterious Microbial Mats Focus Ecological role of microbial mats in hydrothermal vent ecosystems Grade Level 5-6 (Life Science) Focus Question What is the role of microbial mats in hydrothermal vent ecosystems? Learning Objectives n Students will plan an investigation using a model ecosystem to explain some of the components of an anaerobic ecosystem. n Students will construct explanations for the potential role of microbial mats in hydrothermal vent ecosystems. Materials For each student group: q Directions for setting up Winogradsky columns from http:// quest.arc.nasa.gov/projects/astrobiology/fieldwork/lessons/ Winogradsky_5_8.pdf q Two 2-liter plastic soda bottles q Black mud from a local river, lake, or estuary, approximately 2.5 l q 2.5 l of water from each mud/sand location used q 1 small bucket q 250 ml graduated cylinder or 1 cup measure q 1 paint stirrer or large spoon q 1 sheet of newspaper q 1 tablespoon powdered chalk q One hard boiled egg yolk or one tablespoon calcium sulfate q 1 set measuring spoons q Aluminum foil or plastic wrap and rubber band q Masking tape and markers for labeling columns q (Optional) Pencil sharpener for crushing chalk q (Optional) Mortar and pestle for making egg yolk powder q (Optional) 1 lamp with 40- to 60-watt light bulb q (Optional) Microscopes and materials for making wet mounts Image captions/credits on Page 2. Audio-Visual Materials q (Optional) Interactive whiteboard 1 www.oceanexplorer.noaa.gov Submarine Ring of Fire 2012: NE Lau -
Hyphal Proteobacteria, Hirschia Baltica Gen. Nov. , Sp. Nov
INTERNATIONALJOURNAL OF SYSTEMATICBACTERIOLOGY, Oct. 1990, p. 443451 Vol. 40. No. 4 0020-7713/9O/040443-O9$02.00/0 Copyright 0 1990, International Union of Microbiological Societies Taxonomic and Phylogenetic Studies on a New Taxon of Budding, Hyphal Proteobacteria, Hirschia baltica gen. nov. , sp. nov. HEINZ SCHLESNER," CHRISTINA BARTELS, MANUEL SITTIG, MATTHIAS DORSCH, AND ERKO STACKEBRANDTT Institut fur Allgemeine Mikrobiologie, Christian-Albrecht-Universitat, 2300 Kiel, Federal Republic of Germany Four strains of budding, hyphal bacteria, which had very similar chemotaxonomic properties, were isolated from the Baltic Sea. The results of DNA-DNA hybridization experiments, indicated that three of the new isolates were closely related, while the fourth was only moderately related to the other three. Sequence signature and higher-order structural detail analyses of the 16s rRNA of strain IFAM 141gT (T = type strain) indicated that this isolate is related to the alpha subclass of the class Proteobacteriu. Although our isolates resemble members of the genera Hyphomicrobium and Hyphomonas in morphology, assignment to either of these genera was excluded on the basis of their markedly lower DNA guanine-plus-cytosine contents. We propose that these organisms should be placed in a new genus, Hirschiu baltica is the type species of this genus, and the type strain of H. bdtica is strain IFAM 1418 (= DSM 5838). Since the first description of a hyphal, budding bacterium, no1 and formamide were tested at concentrations of 0.02 and Hyphomicrobium vulgare (53), only the following additional 0.1% (vol/vol). Utilization of nitrogen sources was tested in genera having this morphological type have been formally M9 medium containing glucose as the carbon source. -
Photosynthesis and Respiration
HIGH SCHOOL LIFE SCIENCE: PHOTOSYNTHESIS AND RESPIRATION Standards Bundle Standards are listed within the bundle. Bundles are created with potential instructional use in mind, based upon potential for related phenomena that can be used throughout a unit. HS-LS1-5 Use a model to illustrate how photosynthesis transforms light energy into stored chemical energy. (SEP: 2; DCI: LS1.C; CCC: Systems, Energy/Matter) [Clarification Statement: Emphasis is on illustrating inputs and outputs of matter and the transfer and transformation of energy in photosynthesis by plants and other photosynthesizing organisms. Examples of models could include diagrams, chemical equations, and conceptual models.] [Assessment Boundary: Assessment does not include specific biochemical steps.] HS-LS1-7 Use a model of the major inputs and outputs of cellular respiration (aerobic and anaerobic) to exemplify the chemical process in which the bonds of food molecules are broken, the bonds of new compounds are formed, and a net transfer of energy results. (SEP: 2; DCI: LS1.C; CCC: Energy/Matter)[Clarification Statement: Emphasis is on the conceptual understanding of the inputs and outputs of the process of cellular respiration.] [Assessment Boundary: Assessment should not include identification of the steps or specific processes involved in cellular respiration.] HS-LS2-5 Develop a model to illustrate the role of photosynthesis and cellular respiration in the cycling of carbon among the biosphere, atmosphere, hydrosphere, and geosphere. (SEP: 2; DCI: LS2.B, PS3.D; CCC: Systems) [Clarification Statement: Examples of models could include simulations and mathematical models.] [Assessment Boundary: Assessment does not include the specific chemical steps of photosynthesis and respiration.] Content Overview This section provides a generic overview of the content or disciplinary core ideas as an entry point to the standards. -
“How to Make a Microbial Mat”
Science Lesson Plan: How to Make a Microbial Mat Brad Bebout, Allison Pfeifer, Erich Fleming, Adrienne Frisbee, Jan Winter NASA Ames Research Center Background Microbes have shaped the atmosphere and climate of Earth over geologic time. Microbes may be important in the search for life both within our solar system and on extrasolar planets. Some of the earliest and most widespread evidence of life on Earth were in the form of microbial mats. Microbial mats are complex, usually layered collections of microorganisms that can be observed in a number of aquatic ecosystems. They are complete ecosystems in miniature. In this activity, students create living versions of the microbial mats that have existed on earth for 3.5 billion years. Living microbial mats constructed in plastic boxes. Main Concepts Photosynthetic microbial mats are complex ecosystems that generally exhibit vertical gradients in light, and chemical compounds. These gradients are established by photosynthesis at the top of the mat and control the functioning of the intact ecosystem. Scientific Question What factors contribute to the vertical structure of microbial mats in the field? Objectives 1. The students will create their own microbial mat. 2. The microbial mat will be available for later experimentation and/or observation. Abstract of Lesson Microbial mats are defined as layered communities of microorganisms that are only a few millimeters thick. Many biogeochemical processes are conducted by the organisms in the mat to sustain life. For example, the mats perform photosynthesis, and respiration, and can acquire nitrogen through the process of nitrogen fixation. The mat community is a fully functioning ecosystem containing both producers and consumers or organic carbon. -
Forest Production Ecology • Objectives – Overview of Forest Production Ecology • C Cycling – Primary Productivity of Trees and Forest Ecosystems
Forest Production Ecology • Objectives – Overview of forest production ecology • C cycling – Primary productivity of trees and forest ecosystems … ecologists and ecosystem managers are unlikely to achieve desired management objectives unless they are familiar with the distribution and movements of energy that are responsible for the character and productivity of ecosystems under their management. (Kimmins 2004) – First: questions, take-home points, things you learned, etc. from reading assignment 1 Forest Production Ecology • Why should you care about C cycling? – C is the energy currency of all ecosystems • Plant (autotrophic) production is the base of almost all food/energy pyramids • Underlies all ecosystem goods & services – Plant C cycling, to a large extent, controls atmospheric CO2 concentrations (i.e., climate) • 3-4x as much C in terrestrial ecosystems as the atmosphere • Forests account for ~80% of global plant biomass and ~50% of global terrestrial productivity – C is fundamental to soil processes (i.e., SOM) • Belowground resources are a primary control over all ecosystem processes 2 Forest Production Ecology •Global Carbon Cycle ≈ “Breathing” of Earth 3 Forest Production Ecology • C enters via photosynthesis The C Bank Account 1. Gross Primary Production (GPP) •Total C input via photosynthesis 2. Accumulates in ecosystems (C pools/storage) as: (a) plant biomass; (b) SOM & microbial biomass; or (c) animal biomass 3. Returned to the atmosphere via: (a) respiration (R; auto- or hetero-trophic); (b) VOC emissions; or (c) disturbance Chapin et al. (2011) 4. Leached from or transferred laterally to another ecosystem Forest Production Ecology • Keys to understanding biological C cycling 1. Pools (storage) vs. fluxes (flows) of C • Live and dead (detrital) biomass • Above- and belowground 2. -
Microbial Lithification in Marine Stromatolites and Hypersaline Mats
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Published in Trends in Microbiology 13,9 : 429-438, 2005, 1 which should be used for any reference to this work Microbial lithification in marine stromatolites and hypersaline mats Christophe Dupraz1 and Pieter T. Visscher2 1Institut de Ge´ ologie, Universite´ de Neuchaˆ tel, Rue Emile-Argand 11, CP 2, CH-2007 Neuchaˆ tel, Switzerland 2Center for Integrative Geosciences, Department of Marine Sciences, University of Connecticut, 1080 Shennecossett Road, Groton, Connecticut, 06340, USA Lithification in microbial ecosystems occurs when pre- crucial role in regulating sedimentation and global bio- cipitation of minerals outweighs dissolution. Although geochemical cycles. the formation of various minerals can result from After the decline of stromatolites in the late Proterozoic microbial metabolism, carbonate precipitation is pos- (ca. 543 million years before present), microbially induced sibly the most important process that impacts global and/or controlled precipitation continued throughout the carbon cycling. Recent investigations have produced geological record as an active and essential player in most models for stromatolite formation in open marine aquatic ecosystems [9,10]. Although less abundant than in environments and lithification in shallow hypersaline the Precambrian, microbial precipitation is observed in a lakes, which could be highly relevant for interpreting the multitude of semi-confined (physically or chemically)