The Prokaryotes
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Oceans of Archaea Abundant Oceanic Crenarchaeota Appear to Derive from Thermophilic Ancestors That Invaded Low-Temperature Marine Environments
Oceans of Archaea Abundant oceanic Crenarchaeota appear to derive from thermophilic ancestors that invaded low-temperature marine environments Edward F. DeLong arth’s microbiota is remarkably per- karyotes), Archaea, and Bacteria. Although al- vasive, thriving at extremely high ternative taxonomic schemes have been recently temperature, low and high pH, high proposed, whole-genome and other analyses E salinity, and low water availability. tend to support Woese’s three-domain concept. One lineage of microbial life in par- Well-known and cultivated archaea generally ticular, the Archaea, is especially adept at ex- fall into several major phenotypic groupings: ploiting environmental extremes. Despite their these include extreme halophiles, methanogens, success in these challenging habitats, the Ar- and extreme thermophiles and thermoacido- chaea may now also be viewed as a philes. Early on, extremely halo- cosmopolitan lot. These microbes philic archaea (haloarchaea) were exist in a wide variety of terres- first noticed as bright-red colonies trial, freshwater, and marine habi- Archaea exist in growing on salted fish or hides. tats, sometimes in very high abun- a wide variety For many years, halophilic isolates dance. The oceanic Marine Group of terrestrial, from salterns, salt deposits, and I Crenarchaeota, for example, ri- freshwater, and landlocked seas provided excellent val total bacterial biomass in wa- marine habitats, model systems for studying adap- ters below 100 m. These wide- tations to high salinity. It was only spread Archaea appear to derive sometimes in much later, however, that it was from thermophilic ancestors that very high realized that these salt-loving invaded diverse low-temperature abundance “bacteria” are actually members environments. -
Table S5. the Information of the Bacteria Annotated in the Soil Community at Species Level
Table S5. The information of the bacteria annotated in the soil community at species level No. Phylum Class Order Family Genus Species The number of contigs Abundance(%) 1 Firmicutes Bacilli Bacillales Bacillaceae Bacillus Bacillus cereus 1749 5.145782459 2 Bacteroidetes Cytophagia Cytophagales Hymenobacteraceae Hymenobacter Hymenobacter sedentarius 1538 4.52499338 3 Gemmatimonadetes Gemmatimonadetes Gemmatimonadales Gemmatimonadaceae Gemmatirosa Gemmatirosa kalamazoonesis 1020 3.000970902 4 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas indica 797 2.344876284 5 Firmicutes Bacilli Lactobacillales Streptococcaceae Lactococcus Lactococcus piscium 542 1.594633558 6 Actinobacteria Thermoleophilia Solirubrobacterales Conexibacteraceae Conexibacter Conexibacter woesei 471 1.385742446 7 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas taxi 430 1.265115184 8 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas wittichii 388 1.141545794 9 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas sp. FARSPH 298 0.876754244 10 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sorangium cellulosum 260 0.764953367 11 Proteobacteria Deltaproteobacteria Myxococcales Polyangiaceae Sorangium Sphingomonas sp. Cra20 260 0.764953367 12 Proteobacteria Alphaproteobacteria Sphingomonadales Sphingomonadaceae Sphingomonas Sphingomonas panacis 252 0.741416341 -
The Histology, Microbiology, and Molecular Ecology of Tissue-Loss Diseases Affecting Acropora Cervicornis in the Upper Florida Keys
THE HISTOLOGY, MICROBIOLOGY, AND MOLECULAR ECOLOGY OF TISSUE-LOSS DISEASES AFFECTING ACROPORA CERVICORNIS IN THE UPPER FLORIDA KEYS by Katheryn W. Patterson A Dissertation Submitted to the Graduate Faculty of George Mason University in Partial Fulfillment of The Requirements for the Degree of Doctor of Philosophy Environmental Science and Public Policy Committee: _________________________________________ Dr. Esther C. Peters, Dissertation Director _________________________________________ Dr. Cara Frankenfeld, Committee Member _________________________________________ Dr. Patrick Gillevet, Committee Member _________________________________________ Dr. Robert Jonas, Committee Member _________________________________________ Dr. E.C.M. Parsons, Committee Member _________________________________________ Dr. Albert Torzilli, Graduate Program Director _________________________________________ Dr. Robert Jonas, Department Chairperson _________________________________________ Dr. Donna M. Fox, Associate Dean, Office of Student Affairs & Special Programs, College of Science _________________________________________ Dr. Peggy Agouris, Dean, College of Science Date: __________________________________ Summer Semester 2015 George Mason University Fairfax, VA The Histology, MicrobiOlogy, and Molecular Ecology of Tissue-Loss Diseases Affecting Acropora cervicornis in the Upper Florida Keys A Dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at George Mason University by Katheryn W. Patterson Master of Science George Mason University, 2010 Director: Esther C. Peters, Professor Department of Environmental Science and Public Policy Summer Semester 2015 George Mason University Fairfax, VA This work is licensed under a creative commons attribution-noderivs 3.0 unported license. ii DEDICATION This dissertation is in memory of and dedicated to two professors, mentors, and friends that helped inspire and challenge me to be the person I am today. Thank you for encouraging me to stay on the path to become a marine biologist, Dr. -
Link to the Report
DISCLAIMER This report was prepared as an account of a workshop sponsored by the U.S. Department of Energy. Neither the United States Government nor any agency thereof, nor any of their employees or officers, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of document authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Copyrights to portions of this report (including graphics) are reserved by original copyright holders or their assignees, and are used by the Government’s license and by permission. Requests to use any images must be made to the provider identified in the image credits. On the cover: Argonne National Laboratory’s IBM Blue Gene/P supercomputer Inset visualization of ALG13 courtesy of David Baker, University of Washington AUTHORS AND CONTRIBUTORS Sponsors and representatives Susan Gregurick, DOE/Office of Biological and Environmental Science Daniel Drell, DOE/Office of Biological and Environmental Science Christine Chalk, DOE/Office of Advanced Scientific -
Bibliography
Bibliography Abella, C.A., X.P. Cristina, A. Martinez, I. Pibernat and X. Vila. 1998. on moderate concentrations of acetate: production of single cells. Two new motile phototrophic consortia: "Chlorochromatium lunatum" Appl. Microbiol. Biotechnol. 35: 686-689. and "Pelochromatium selenoides". Arch. Microbiol. 169: 452-459. Ahring, B.K, P. Westermann and RA. Mah. 1991b. Hydrogen inhibition Abella, C.A and LJ. Garcia-Gil. 1992. Microbial ecology of planktonic of acetate metabolism and kinetics of hydrogen consumption by Me filamentous phototrophic bacteria in holomictic freshwater lakes. Hy thanosarcina thermophila TM-I. Arch. Microbiol. 157: 38-42. drobiologia 243-244: 79-86. Ainsworth, G.C. and P.H.A Sheath. 1962. Microbial Classification: Ap Acca, M., M. Bocchetta, E. Ceccarelli, R Creti, KO. Stetter and P. Cam pendix I. Symp. Soc. Gen. Microbiol. 12: 456-463. marano. 1994. Updating mass and composition of archaeal and bac Alam, M. and D. Oesterhelt. 1984. Morphology, function and isolation terial ribosomes. Archaeal-like features of ribosomes from the deep of halobacterial flagella. ]. Mol. Biol. 176: 459-476. branching bacterium Aquifex pyrophilus. Syst. Appl. Microbiol. 16: 629- Albertano, P. and L. Kovacik. 1994. Is the genus LeptolynglYya (Cyano 637. phyte) a homogeneous taxon? Arch. Hydrobiol. Suppl. 105: 37-51. Achenbach-Richter, L., R Gupta, KO. Stetter and C.R Woese. 1987. Were Aldrich, H.C., D.B. Beimborn and P. Schönheit. 1987. Creation of arti the original eubacteria thermophiles? Syst. Appl. Microbiol. 9: 34- factual internal membranes during fixation of Methanobacterium ther 39. moautotrophicum. Can.]. Microbiol. 33: 844-849. Adams, D.G., D. Ashworth and B. -
Profile of Edward Delong Paul Gabrielsen Enzymes Among Four Genera of Marine Bac- Science Writer Teria and Infer Evolutionary Relationships
PROFILE PROFILE Profile of Edward DeLong Paul Gabrielsen enzymes among four genera of marine bac- Science Writer teria and infer evolutionary relationships. “That’s where the inkling started that I Every year, gray whales travel up and down Finding Himself could combine my interests in biology and my passion for the ocean,” DeLong says. “I the Pacific coast, migrating between the Born in 1958, the third of six children, hadn’t even realized up until that point that Bering Sea and Baja California. In the mid- DeLong grew up in Sonoma, California on an research was an option.” The findings were 1970s, Northern California amateur skin “overdose of Jacques Cousteau,” he says. As diver Edward DeLong tried to swim out to published in the Archives of Microbiology a teenager, he encountered sea lions and sea with DeLong as first author (1). meet them. With his sights set on some of otters on skin diving expeditions with friends, ’ the ocean s largest creatures, DeLong was and attempted to reach gray whales. “We Setting His Compass oblivious to the microecosystem swirling never actually met them face to face,” he says. DeLong arrived at the Scripps Institution of around him in the cool water. Instead, his DeLong’s father, a high school English Oceanography in 1982 to begin graduate fascination for the vast and mysterious ocean teacher, encouraged his children in academ- school. Under biophysicist Art Yayanos, impelled him to reach for the huge, shadowy ics, but 18-year-old DeLong did not feel DeLong studied pressure-adapted micro- whales in the distance. -
Identify the Core Bacterial Microbiome of Hydrocarbon Degradation and A
Identify the core bacterial microbiome of hydrocarbon degradation and a shift of dominant methanogenesis pathways in oil and aqueous phases of petroleum reservoirs with different temperatures from China Zhichao Zhou1, Bo Liang2, Li-Ying Wang2, Jin-Feng Liu2, Bo-Zhong Mu2, Hojae Shim3, and Ji-Dong Gu1,* 1 Laboratory of Environmental Microbiology and Toxicology, School of Biological Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, Hong Kong, People’s Republic of China 2 State Key Laboratory of Bioreactor Engineering and Institute of Applied Chemistry, East China University of Science and Technology, Shanghai 200237, People’s Republic of China 3 Faculty of Science and Technology, University of Macau, Macau, People’s Republic of China *Correspondence to: Ji-Dong Gu ([email protected]) 1 Supplementary Data 1.1 Characterization of geographic properties of sampling reservoirs Petroleum fluids samples were collected from eight sampling sites across China covering oilfields of different geological properties. The reservoir and crude oil properties together with the aqueous phase chemical concentration characteristics were listed in Table 1. P1 represents the sample collected from Zhan3-26 well located in Shengli Oilfield. Zhan3 block region in Shengli Oilfield is located in the coastal area from the Yellow River Estuary to the Bohai Sea. It is a medium-high temperature reservoir of fluvial face, made of a thin layer of crossed sand-mudstones, pebbled sandstones and fine sandstones. P2 represents the sample collected from Ba-51 well, which is located in Bayindulan reservoir layer of Erlian Basin, east Inner Mongolia Autonomous Region. It is a reservoir with highly heterogeneous layers, high crude oil viscosity and low formation fluid temperature. -
MMI Evaluation Summary Report June 2013
SUMMARY1 OF AAAS 2012 EVALUATION OF THE GORDON AND BETTY MOORE FOUNDATION’S MARINE MICROBIOLOGY INITIATIVE, PHASE 1 (2004–2010) BACKGROUND Oceans account for ~70% of Earth’s surface. Primary productivity, many chemical cycles, and food webs depend on the ocean’s microorganisms, which also convert carbon, nitrogen, sulfur, and trace minerals like iron from inorganic to biologically usable forms. We know that these important marine systems and processes Box 1. Marine microbial ecology defined have been experiencing unprecedented stress due to Marine microbial ecology is the study of increased nutrient run-off, overfishing, and pervasive and the single-celled organisms (bacteria, significant changes in ocean chemistry and temperature archaea, and eukaryotes) and viruses that live in the ocean and their interactions driven by increased emissions of greenhouse gases, yet our with each other and the environment specific knowledge is limited. Despite the fact that research around them. These microorganisms and in this field began more than 75 years ago, as recently as viruses are the ocean’s smallest and most the early 2000s, even the most basic ecological questions— abundant creatures, and they drive many Which organisms are present? What do they do? How do of the chemical reactions that comprise they interact?—remained unanswered due primarily to the Earth’s marine biogeochemical cycles. major obstacles such as: • An inability to grow most microbes in culture in tandem with limited morphological characteristics capable of differentiating species, creating a major taxonomic impediment resulting in treatment of broad groups of microbes as “black boxes” with little knowledge of the role of each species. -
Reviewer Biographies
Biosciences Area Review 2015 Lawrence Berkeley National Laboratory Reviewer Biographies Janet Braam, Ph.D., Rice University Janet Braam has a diverse scientific background, being involved in research that spans from translation medical research to basic plant cell biology. She received her PhD in Molecular Virology and Biology from the Sloan-Kettering Division of the Cornell Graduate School of Medical Sciences, elucidating the roles of influenza viral polymerase subunits. She then joined Stanford University School of Medicine as an NSF postdoctoral fellow in plant biology. Dr. Braam’s research at Stanford led to the discovery that plants turn on genes in response to touch and shed light on the importance of calcium signal transduction in mechanical perturbation responses in plants. In 1990, Dr. Braam joined the faculty at Rice University and rose through the ranks. She has had continual federal grant support and served on diverse grant and advisory panels Dr. Braam’s research contributions include uncovering roles of calcium-binding and cell wall proteins in plant responses to environmental stress, and elucidating aspects of nitric oxide signaling, autophagy regulation, and jasmonate dependent defense. Most recently, her research focus also includes the role of the circadian clock in plant defense, the complex regulation of chlorophyll biogenesis, phytohormone regulation, and autophagy control. Her discoveries in basic plant biology have potential translational application in drug discovery, crop nutrient enhancement, and nanomaterial toxicity analysis in plants. Charles Craik, Ph.D., University of California, San Francisco Charles S. Craik is a Professor in the Department of Pharmaceutical Chemistry at the University of California at San Francisco. -
Geobacteraceae Are Important Members of Mercury-Methylating Microbial Communities of Sediments Impacted by Waste Water Releases
The ISME Journal (2018) 12:802–812 https://doi.org/10.1038/s41396-017-0007-7 ARTICLE Geobacteraceae are important members of mercury-methylating microbial communities of sediments impacted by waste water releases 1 2 1 1 1 3 Andrea G. Bravo ● Jakob Zopfi ● Moritz Buck ● Jingying Xu ● Stefan Bertilsson ● Jeffra K. Schaefer ● 4 4,5 John Poté ● Claudia Cosio Received: 19 May 2017 / Revised: 29 September 2017 / Accepted: 18 October 2017 / Published online: 10 January 2018 © The Author(s) 2018. This article is published with open access Abstract Microbial mercury (Hg) methylation in sediments can result in bioaccumulation of the neurotoxin methylmercury (MMHg) in aquatic food webs. Recently, the discovery of the gene hgcA, required for Hg methylation, revealed that the diversity of Hg methylators is much broader than previously thought. However, little is known about the identity of Hg-methylating microbial organisms and the environmental factors controlling their activity and distribution in lakes. Here, we combined high-throughput sequencing of 16S rRNA and hgcA genes with the chemical characterization of sediments impacted by a 1234567890 waste water treatment plant that releases significant amounts of organic matter and iron. Our results highlight that the ferruginous geochemical conditions prevailing at 1–2 cm depth are conducive to MMHg formation and that the Hg- methylating guild is composed of iron and sulfur-transforming bacteria, syntrophs, and methanogens. Deltaproteobacteria, notably Geobacteraceae, dominated the hgcA carrying communities, while sulfate reducers constituted only a minor component, despite being considered the main Hg methylators in many anoxic aquatic environments. Because iron is widely applied in waste water treatment, the importance of Geobacteraceae for Hg methylation and the complexity of Hg- methylating communities reported here are likely to occur worldwide in sediments impacted by waste water treatment plant discharges and in iron-rich sediments in general. -
Supplement of Biogeosciences, 16, 4229–4241, 2019 © Author(S) 2019
Supplement of Biogeosciences, 16, 4229–4241, 2019 https://doi.org/10.5194/bg-16-4229-2019-supplement © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of Identifying the core bacterial microbiome of hydrocarbon degradation and a shift of dominant methanogenesis pathways in the oil and aqueous phases of petroleum reservoirs of different temperatures from China Zhichao Zhou et al. Correspondence to: Ji-Dong Gu ([email protected]) and Bo-Zhong Mu ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. 1 Supplementary Data 1.1 Characterization of geographic properties of sampling reservoirs Petroleum fluids samples were collected from eight sampling sites across China covering oilfields of different geological properties. The reservoir and crude oil properties together with the aqueous phase chemical concentration characteristics were listed in Table 1. P1 represents the sample collected from Zhan3-26 well located in Shengli Oilfield. Zhan3 block region in Shengli Oilfield is located in the coastal area from the Yellow River Estuary to the Bohai Sea. It is a medium-high temperature reservoir of fluvial face, made of a thin layer of crossed sand-mudstones, pebbled sandstones and fine sandstones. P2 represents the sample collected from Ba-51 well, which is located in Bayindulan reservoir layer of Erlian Basin, east Inner Mongolia Autonomous Region. It is a reservoir with highly heterogeneous layers, high crude oil viscosity and low formation fluid temperature. It was dedicated to water-flooding, however, due to low permeability and high viscosity of crude oil, displacement efficiency of water-flooding driving process was slowed down along the increase of water-cut rate. -
Supplementary Information
K-mer similarity, networks of microbial genomes and taxonomic rank Guillaume Bernard, Paul Greenfield, Mark A. Ragan, Cheong Xin Chan. Supplementary Figures Legends # Supplementary Figure S1: P- network of prokaryote phyla using !" with k=25, based on rRNAs. Edges represent connections between isolates of two phyla. The node size is proportional to the number of isolates in a phylum. Distance threshold = 6. Supplementary Figure S2: PCA analysis performed on the raw data of the COG categories profile for each genus. Each phylum is color-coded. Supplementary Figure S3: PCA analysis performed on the raw data of the COG categories profile for each genus. Each genus is color-coded according to the number of isolates. Supplementary Figure S4: PCA analysis performed on the normalised counts of center-scaled COG categories. Each phylum is color-coded. Supplementary Tables Legends Supplementary Table S1: List of the 2785 isolates used in this analysis. Supplementary Table S2: Network analysis of the I-network for 2705 complete genomes of bacteria and archaea. Supplementary Table S3: Network analysis of the I-network for 2616 genomes of bacteria and archaea, with rRNA genes removed. Supplementary Table S4: Network analysis of the rRNA gene sequences I-network of 2616 bacterial and archaeal isolates. Supplementary Table S5: Network analysis of the plasmid genomes I-network of 921 bacterial and plasmid genomes. Supplementary Table S6: Statistics of core k-mers for 151 genera. Supplementary Table S7: COG category profiles for 16 phyla. 1 Figure S1