Studies on Microbial Diversity of a Soda Lake in India by Winogradsky Column Technique
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Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: a Critical Review of Current Knowledge
Utah State University DigitalCommons@USU All Graduate Plan B and other Reports Graduate Studies 12-2013 Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge Danielle Barandiaran Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/gradreports Part of the Soil Science Commons Recommended Citation Barandiaran, Danielle, "Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge" (2013). All Graduate Plan B and other Reports. 332. https://digitalcommons.usu.edu/gradreports/332 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Plan B and other Reports by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. METHYLMERCURY FATE IN THE HYPERSALINE ENVIRONMENT OF THE GREAT SALT LAKE: A CRITICAL REVIEW OF CURRENT KNOWLEDGE By Danielle Barandiaran A paper submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Soil Science Approved: Astrid Jacobson Jeanette Norton Major Professor Committee Member - Paul Grossl Teryl Roper Committee Member Department Head UTAH STATE UNIVERSITY Logan, Utah 2013 Copyright © Danielle Barandiaran 2013 All Rights Reserved iii ABSTRACT Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge by Danielle Barandiaran, Master of Science Utah State University, 2013 Major Professor: Dr. Astrid R. Jacobson Department: Plants, Soils & Climate Methylmercury (MeHg) is a highly potent neurotoxic form of the environmental pollutant Mercury (Hg). -
The Great Salt Lake Osmotic Power Potential
The Great Salt Lake Osmotic Power Potential Maher Kelada MIK Technology 2100 West Loop South, Suite 900 Houston, Texas, USA 77027 [email protected] Abstract: This is a proposal to develop a new source of renewable energy relying on hypersaline osmotic power generation technology that has been developed by MIK Technology, potentially for generating up to 400 megawatts of sustainable power from the Great Salt Lake, Utah, operating isothermally without generating any emissions. The proposed technology would reduce Utah State’s demand for coal by 10% or natural gas by 50%, using a clean and safe renewable source of energy. I. Osmotic Power Generation Concept Osmosis is nature’s gift to life. It is the vehicle that transports fluids in all living cells and without it, all biological functions and all forms of life cease to exist! Osmosis is the spontaneous movement of water, through a semi-permeable membrane that is permeable to water but impermeable to solute. Water moves from a solution in which solute is less concentrated to a solution in which solute is more concentrated. The driving force of the flow movement is the difference in the chemical potential on the two sides of the semi-permeable membrane, with the solvent moving from a region of higher potential (generally of a lower solute concentration) to the region of lower potential (generally of a higher solute concentration). The term “Chemical Potential” at times can be ambiguous and elusive. In fact, it is one of the most important partial molal quantities. It is the energy source associated with the activity of the ions of an ionizable substance. -
Altai Region, Russia)
Limnology and Freshwater Biology 2020 (4): 1019-1020 DOI:10.31951/2658-3518-2020-A-4-1019 SI: “The V-th Baikal Symposium on Microbiology” Short communication Salt-dependent succession of phototrophic communities in the soda lake Tanatar VI (Altai Region, Russia) Samylina O.S.1*, Namsaraev Z.B.2 1 Winogradsky Institute of Microbiology, Research Center of Biotechnology, Russian Academy of Sciences, 60 let Oktjabrja pr-t, 7-2, Moscow, 117312, Russia 2 NRC “Kurchatov Institute”, Akademika Kurchatova pl., 1, Moscow, 123182, Russia ABSTRACT. The paper describes the changes that occurred in the ecosystem of soda lake Tanatar VI during the 2011-2019 period when salinity decreased from 160-250 to 13-14 g/l Keywords: soda lake, Picocystis, cyanobacteria, biological soil crusts, succession, nitrogen fixation 1. Introduction salinity. Several types of phototrophic communities were detected in the Tanatar VI (Table): 1) Bottom, A great number and variety of saline lakes are floating and epiphytic cyanobacterial biofilms (CB); located in the Kulunda Steppe in the Altai Region. 2) floating and epiphytic Ctenocladus-communities These lakes are exposed to annual and long-standing with filamentous chlorophyte Ctenocladus circinnatus fluctuations of temperature, salinity, flooding and and cyanobacteria (CC); 3) Blooms of unicellular drying periods due to their locality in the zone of algae Picocystis salinarum (P-bloom); 4) Cyanobacterial cold arid climate. There are soda lakes among them, blooms (CB-bloom); 5) Biological soil crusts (BSC) which maintain stable alkaline pH due to a prevalence developed on the moist soil between thickets of of soluble carbonates in the brines. Thereby diversity Salicornia altaica near the lake. -
The Importance of the Salton Sea and Other Terminal Lakes in Supporting
The Importance of the Salton Sea and Other Terminal Lakes in Supporting Birds of the Pacific Flyway Terminal lakes, so called because they have no outlet, are characteristic water features of the Great Basin of the Intermountain West. Through the process of continued evaporation, minerals and salts that flow into these water bodies are retained and concentrated over time. The salinity of the water varies considerably among terminal lakes, depending on the quality of the source water and the length of time the lake has been in existence. Several of these, including the Great Salt Lake, Mono Lake, and the Salton Sea, have become more saline than the ocean. While all of these lakes support unique physical characteristics and aquatic ecosystems, one characteristic common to all is the importance they play in sustaining birds using the Pacific Flyway and portions of the Central Flyway. Physical and Biological Characteristics of Terminal Lakes in the West Terminal lakes along the Pacific Flyway (Exhibit 1) vary widely in their physical and biological characteristics. Elevations range from 6,381 feet at Mono Lake to -227 feet at the Salton Sea. They also vary greatly in depth and salinity, as shown in Exhibits 2 and 3. Most of these lakes are shallow with seasonal water input and high evaporation in the summer. Water quality is typically characterized by hard water and saline conditions, an artifact of dissolved constituents accumulating and increasing in concentration over time. While water quality in terminal lakes limits the diversity of the aquatic community to salt-tolerant organisms, these lakes often are very productive, and provide an ample food supply for waterbirds. -
Metagenomic Insights Into the Uncultured Diversity and Physiology of Microbes in Four Hypersaline Soda Lake Brines
Lawrence Berkeley National Laboratory Recent Work Title Metagenomic Insights into the Uncultured Diversity and Physiology of Microbes in Four Hypersaline Soda Lake Brines. Permalink https://escholarship.org/uc/item/9xc5s0v5 Journal Frontiers in microbiology, 7(FEB) ISSN 1664-302X Authors Vavourakis, Charlotte D Ghai, Rohit Rodriguez-Valera, Francisco et al. Publication Date 2016 DOI 10.3389/fmicb.2016.00211 Peer reviewed eScholarship.org Powered by the California Digital Library University of California ORIGINAL RESEARCH published: 25 February 2016 doi: 10.3389/fmicb.2016.00211 Metagenomic Insights into the Uncultured Diversity and Physiology of Microbes in Four Hypersaline Soda Lake Brines Charlotte D. Vavourakis 1, Rohit Ghai 2, 3, Francisco Rodriguez-Valera 2, Dimitry Y. Sorokin 4, 5, Susannah G. Tringe 6, Philip Hugenholtz 7 and Gerard Muyzer 1* 1 Microbial Systems Ecology, Department of Aquatic Microbiology, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Amsterdam, Netherlands, 2 Evolutionary Genomics Group, Departamento de Producción Vegetal y Microbiología, Universidad Miguel Hernández, San Juan de Alicante, Spain, 3 Department of Aquatic Microbial Ecology, Biology Centre of the Czech Academy of Sciences, Institute of Hydrobiology, Ceskéˇ Budejovice,ˇ Czech Republic, 4 Research Centre of Biotechnology, Winogradsky Institute of Microbiology, Russian Academy of Sciences, Moscow, Russia, 5 Department of Biotechnology, Delft University of Technology, Delft, Netherlands, 6 The Department of Energy Joint Genome Institute, Walnut Creek, CA, USA, 7 Australian Centre for Ecogenomics, School of Chemistry and Molecular Biosciences and Institute for Molecular Bioscience, The University of Queensland, Brisbane, QLD, Australia Soda lakes are salt lakes with a naturally alkaline pH due to evaporative concentration Edited by: of sodium carbonates in the absence of major divalent cations. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
Great Salt Lake Brine Chemistry Database, 1966–2011
GREAT SALT LAKE BRINE CHEMISTRY DATABASE, 1966–2011 by Andrew Rupke and Ammon McDonald OPEN-FILE REPORT 596 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 2012 GREAT SALT LAKE BRINE CHEMISTRY DATABASE, 1966–2011 by Andrew Rupke and Ammon McDonald Cover photo: The Southern Pacific Railroad rock causeway. The view is to the east, and the north arm of Great Salt Lake is on the left. OPEN-FILE REPORT 596 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 2012 STATE OF UTAH Gary R. Herbert, Governor DEPARTMENT OF NATURAL RESOURCES Michael Styler, Executive Director UTAH GEOLOGICAL SURVEY Richard G. Allis, Director PUBLICATIONS contact Natural Resources Map & Bookstore 1594 W. North Temple Salt Lake City, UT 84116 telephone: 801-537-3320 toll-free: 1-888-UTAH MAP website: mapstore.utah.gov email: [email protected] UTAH GEOLOGICAL SURVEY contact 1594 W. North Temple, Suite 3110 Salt Lake City, UT 84116 telephone: 801-537-3300 website: geology.utah.gov This open-file release makes information available to the public that may not conform to UGS technical, edito- rial, or policy standards; this should be considered by an individual or group planning to take action based on the contents of this report. Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. -
Great Salt Lake FAQ June 2013 Natural History Museum of Utah
Great Salt Lake FAQ June 2013 Natural History Museum of Utah What is the origin of the Great Salt Lake? o After the Lake Bonneville flood, the Great Basin gradually became warmer and drier. Lake Bonneville began to shrink due to increased evaporation. Today's Great Salt Lake is a large remnant of Lake Bonneville, and occupies the lowest depression in the Great Basin. Who discovered Great Salt Lake? o The Spanish missionary explorers Dominguez and Escalante learned of Great Salt Lake from the Native Americans in 1776, but they never actually saw it. The first white person known to have visited the lake was Jim Bridger in 1825. Other fur trappers, such as Etienne Provost, may have beaten Bridger to its shores, but there is no proof of this. The first scientific examination of the lake was undertaken in 1843 by John C. Fremont; this expedition included the legendary Kit Carson. A cross, carved into a rock near the summit of Fremont Island, reportedly by Carson, can still be seen today. Why is the Great Salt Lake salty? o Much of the salt now contained in the Great Salt Lake was originally in the water of Lake Bonneville. Even though Lake Bonneville was fairly fresh, it contained salt that concentrated as its water evaporated. A small amount of dissolved salts, leached from the soil and rocks, is deposited in Great Salt Lake every year by rivers that flow into the lake. About two million tons of dissolved salts enter the lake each year by this means. Where does the Great Salt Lake get its water, and where does the water go? o Great Salt Lake receives water from four main rivers and numerous small streams (66 percent), direct precipitation into the lake (31 percent), and from ground water (3 percent). -
Soda Springs, a Small San Bernardino County Desert Oasis, Eight Miles South of Interstate 15 and Baker, Between Barstow And
Volume XX, 1980 SODA SPRINGS, SAN BERNARDINO COUNTY: SEQUENTIAL LAND USE Stephen T. Glass* Soda Springs, a small San Bernardino County desert oasis, eight miles south of Interstate 15 and Baker, between Barstow and Las Vegas, goes unnoticed by the thousands of travelers that pass daily through the Mohave Desert by car, bus, or train. (Fig. 1) Little rem:ains to indicate Soda Spring's former importance to the region's development. Only faint remnants of the former Mojave Road and the Tonopah and Tidewater Railroad are noticeable to the perspicacious rock climber or air traveler. The historical succession of land uses in Soda Springs has recently been continued by the addition of the Desert Research Center, under the auspices of the California State University and Coliege System. Before European Settlement Soda Spring's strategic location in the eastern Mojave has had a major effect on the commerce and, as importantly, on human survival in the region. Before the advent of European explorers, ancient trade trails led some 283 miles from the Mojave Valley on the Colorado River to the Pacific Coast. The nomadic Mojave Indians maintained a large permanent village north of present day Needles. Acting as middle-men *Mr. Glass is Head, Office of Noise Control, Environmental Health Division, City of Long Beach. 10 T \ ..\ (�.�� Yt ";; t�.J� Ei9-:>-. /">�:��- K.'f!l�" .. ; .. - ·· . • �.t '•',, ,;:..:.\ .... .. � . (, .... ... • .. -�� ;f .. ,. .. , .":' ···' . : . ..(\ ' 0 . i k . .. -�,. r.·�·) . u_::?r��(�:}.. ts?�. } " :)�). ::/ ;"''\ . , · '*SoliS't ; ' \,_..""'••' • I /J� _,,,-.,- �--<>:>l . .' i •••••' •• • .. � .. \ ; . ( " ..·· • ..,,_ .,.,., ·-�v :. - .,«, TBI.OJIIIIOD .... ··. ' •J . �r(-·r: )·,' r'i;-·-!.{ ' , ., AND OTHER EARLY WAGON ROADS (y' (::./ OF THE ���� �;_...� ��: ,��r . -
Hidden Diversity of Plankton in the Soda Lake Nakuru, Kenya, During A
Hydrobiologia (2013) 702:95–103 DOI 10.1007/s10750-012-1310-y PRIMARY RESEARCH PAPER Hidden diversity of eukaryotic plankton in the soda lake Nakuru, Kenya, during a phase of low salinity revealed by a SSU rRNA gene clone library Wei Luo • Kiplagat Kotut • Lothar Krienitz Received: 12 July 2012 / Revised: 28 August 2012 / Accepted: 31 August 2012 / Published online: 16 September 2012 Ó Springer Science+Business Media B.V. 2012 Abstract A SSU rRNA gene clone library was Our findings reveal a hidden diversity, which would constructed to establish the diversity of eukaryotic not have been detected by traditional observations. plankton in the African soda lake Nakuru during a phase of low salinity (9.7 ppt = hyposaline). Nor- Keywords Chlorophyta Á Clone library Á Lake mally, the lake is mesosaline (up to 50 ppt) and its Nakuru Á Lesser Flamingo Á Phytoflagellates Á phytoplankton is dominated by few species of cyano- Soda lakes Á SSU rRNA bacteria, in particular Arthrospira fusiformis, which is the main food resource of Lesser Flamingos. Our study recovered a unique phytoplankton species composi- Introduction tion characterized by a high diversity of monadoid and coccoid green algae. Out of 77 clones detected, 52 The phytoplankton of saline-alkaline lakes in the Great belonged to Chlorophyta. Many of the chlorophytes African Rift Valley usually is dominated by cyano- were transported from the catchment area into the lake bacteria, mainly Arthrospira fusiformis (Voronichin) through small seasonal rivers and an outflow of the Koma´rek et Lund (often erroneously identified as Nakuru town sewage treatment plant. Other phyloge- ‘‘Spirulina platensis’’), which forms the food base for netic groups detected were Fungi, Cryptophyta, hundreds of thousands of Lesser Flamingos (Phoenic- Jakobida, Alveolata, Stramenopiles, and Metazoa. -
24-13 Robert
www.roavs.com EISSN: 2223-0343 Research Opinions in Animal & Veterinary Sciences Cyanobacterial toxins and bacterial infections are the possible causes of mass mortality of lesser flamingos in Soda lakes in northern Tanzania Robert D. Fyumagwa 1* , Zablon Bugwesa 1, Machoke Mwita 1, Emilian S. Kihwele 2, Athanas Nyaki 3, Robinson H. Mdegela 4 and Donald G. Mpanduji 4 1Tanzania Wildlife Research Institute (TAWIRI), P.O.Box 661, Arusha, Tanzania; 2Serengeti Nattional Park P. O. Box 3134, Arusha, Tanzania; 3Ngorongoro Conservation Area Authority (NCAA) P. O. Box 1, Ngorongoro, Aursha, Tanzania; 4Faculty of Veterinary Medicine, Sokoine University of Agriculture (SUA), P. O. Box 3022, Morogoro, Tanzania Abstract During the mass die-off of lesser flamingos in Soda lakes of Tanzania in 2000, 2002 and 2004, clinicopathological and toxicological investigations were made in order to elucidate the likely cause of mortality. Water and tissue samples were collected from the lakes and from dead flamingos respectively. While water samples were analyzed for pesticide residues, tissues were analyzed for pesticide residues and cyanotoxins. The significant pathological lesions observed in fresh carcasses included oedema in lungs, enlarged liver, haemorrhages in liver with multiple necrotic foci, haemorrhages in kidneys and haemorrhages in intestines with erosion of mucosa. Analysis of cyanotoxins revealed presence of neurotoxin (anatoxin-a) and hepatotoxins (microcystins LR, RR). Concentrations of microcystins LR were significantly higher (P = 0.0003) in liver than in other tissues. Based on clinicopathological findings and concentrations of the detected cyanotoxins, it is suspected that cyanobacterial toxins concurrent with secondary bacterial infection were the likely cause of the observed mortalities in flamingos. -
The Soda Lakes of Nhecolândia: a Conservation Opportunity for The
Perspectives in Ecology and Conservation 17 (2019) 9–18 ´ Supported by Boticario Group Foundation for Nature Protection www.perspectecolconserv.com Essays and Perspectives The soda lakes of Nhecolândia: A conservation opportunity for the Pantanal wetlands a b c,∗ d Renato L. Guerreiro , Ivan Bergier , Michael M. McGlue , Lucas V. Warren , b e d Urbano Gomes Pinto de Abreu , Jônatas Abrahão , Mario L. Assine a Instituto Federal de Educac¸ ão, Ciência e Tecnologia do Paraná, Av. Cívica, 475, 85935-000 Assis Chateaubriand, PR, Brazil b Embrapa Pantanal, Rua 21 de Setembro, 1880, 79302-090 Corumbá, MS, Brazil c Department of Earth and Environmental Sciences, University of Kentucky, 121 Washington Ave, Lexington, KY 40506, USA d Instituto de Geociências e Ciências Exatas, Unesp – Universidade Estadual Paulista, Avenida 24-A, Bela Vista, Rio Claro, SP CEP 13506-900, Brazil e Laboratório de Vírus, Instituto de Ciências Biológicas, Departamento de Microbiologia, Universidade Federal de Minas Gerais, Belo Horizonte 31270-901, Brazil a a b s t r a c t r t i c l e i n f o Article history: The Pantanal is the most conserved biome in Brazil and among the last wild refuges in South Amer- Received 2 July 2018 ica, but intensification of agriculture and other land use changes present challenges for protecting this Accepted 26 November 2018 exceptionally biodiverse wetland ecosystem. Recent studies have shed new light on the origins and bio- Available online 11 December 2018 geochemistry of a suite of >600 small saline-alkaline lakes in Nhecolândia, a floodplain setting located south of the Taquari River in south-central Pantanal.