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The Genome of Prasinoderma Coloniale Unveils the Existence of a Third Phylum Within Green Plants
SUPPLEMENTARY INFORMATIONARTICLES https://doi.org/10.1038/s41559-020-1221-7 In the format provided by the authors and unedited. The genome of Prasinoderma coloniale unveils the existence of a third phylum within green plants Linzhou Li1,2,13, Sibo Wang1,3,13, Hongli Wang1,4, Sunil Kumar Sahu 1, Birger Marin 5, Haoyuan Li1, Yan Xu1,4, Hongping Liang1,4, Zhen Li 6, Shifeng Cheng1, Tanja Reder5, Zehra Çebi5, Sebastian Wittek5, Morten Petersen3, Barbara Melkonian5,7, Hongli Du8, Huanming Yang1, Jian Wang1, Gane Ka-Shu Wong 1,9, Xun Xu 1,10, Xin Liu 1, Yves Van de Peer 6,11,12 ✉ , Michael Melkonian5,7 ✉ and Huan Liu 1,3 ✉ 1State Key Laboratory of Agricultural Genomics, BGI-Shenzhen, Shenzhen, China. 2Department of Biotechnology and Biomedicine, Technical University of Denmark, Lyngby, Denmark. 3Department of Biology, University of Copenhagen, Copenhagen, Denmark. 4BGI Education Center, University of Chinese Academy of Sciences, Shenzhen, China. 5Institute for Plant Sciences, Department of Biological Sciences, University of Cologne, Cologne, Germany. 6Department of Plant Biotechnology and Bioinformatics (Ghent University) and Center for Plant Systems Biology, Ghent, Belgium. 7Central Collection of Algal Cultures, Faculty of Biology, University of Duisburg-Essen, Essen, Germany. 8School of Biology and Biological Engineering, South China University of Technology, Guangzhou, China. 9Department of Biological Sciences and Department of Medicine, University of Alberta, Edmonton, Alberta, Canada. 10Guangdong Provincial Key Laboratory of Genome Read and Write, BGI-Shenzhen, Shenzhen, China. 11College of Horticulture, Nanjing Agricultural University, Nanjing, China. 12Centre for Microbial Ecology and Genomics, Department of Biochemistry, Genetics and Microbiology, University of Pretoria, Pretoria, South Africa. -
Basin Geochemical Evolution of the Eagle Ford and Effects On
BASIN GEOCHEMICAL EVOLUTION OF THE EAGLE FORD AND EFFECTS ON TRACE ELEMENT RELEASE A Thesis by IVAN MAULANA Submitted to the Office of Graduate and Professional Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Chair of Committee, Michael Tice Co-chair of Committee, Bruce Herbert Committee Members, Franco Marcantonio Terry Wade Head of Department, Michael Pope May 2016 Major Subject: Geology Copyright 2016 Ivan Maulana ABSTRACT The Ocean Anoxic Event 2 (OAE-2) at the Cenomanian-Turonian boundary is recognized from a carbon isotope excursion (CIE) in the Eagle Ford (EF) Group, and commonly attributed to global anoxic conditions in deeper marine settings. Whereas OAE are typically marked by widespread deposition of organic-rich shales, previous work shows diachroneity between the CIE and the organic-rich Lower EF, as well as anoxia- euxinia in the Western Interior Seaway of North America. We found evidence for periodic photic zone euxinia from an EF core, based on ratios of biomarkers and redox-sensitive trace elements. Sedimentary structures suggest depositional environments above storm wave base. Integration with a sequence-stratigraphic framework emphasizes the role of estuarine-style salinity stratification, subject to redox shifts caused by storm mixing in relatively shallow water depths. Independent zircon ages indicate that transition from the Lower to Upper EF occurs in the south before the north, consistent with a northward migration of this stratification mechanism as sea level rose. This implies that the redox states during deposition of the EF leading up to the CIE were influenced by regionally distinct mechanisms at relatively shallow water depths, instead of global anoxic conditions in deeper marine settings. -
Management Plan For
Measure 8 (2013) Annex Management Plan for Antarctic Specially Protected Area (ASPA) No.138 Linnaeus Terrace, Asgard Range, Victoria Land Introduction Linnaeus Terrace is an elevated bench of weathered Beacon Sandstone located at the western end of the Asgard Range, 1.5km north of Oliver Peak, at 161° 05.0' E 77° 35.8' S,. The terrace is ~ 1.5 km in length by ~1 km in width at an elevation of about 1600m. Linnaeus Terrace is one of the richest known localities for the cryptoendolithic communities that colonize the Beacon Sandstone. The sandstones also exhibit rare physical and biological weathering structures, as well as trace fossils. The excellent examples of cryptoendolithic communities are of outstanding scientific value, and are the subject of some of the most detailed Antarctic cryptoendolithic descriptions. The site is vulnerable to disturbance by trampling and sampling, and is sensitive to the importation of non-native plant, animal or microbial species and requires long-term special protection. Linnaeus Terrace was originally designated as Site of Special Scientific Interest (SSSI) No. 19 through Recommendation XIII-8 (1985) after a proposal by the United States of America. The SSSI expiry date was extended by Resolution 7 (1995), and the Management Plan was adopted in Annex V format through Measure 1 (1996). The site was renamed and renumbered as ASPA No 138 by Decision 1 (2002). The Management Plan was updated through Measure 10 (2008) to include additional provisions to reduce the risk of non-native species introductions into the Area. The Area is situated in Environment S – McMurdo – South Victoria Land Geologic based on the Environmental Domains Analysis for Antarctica and in Region 9 – South Victoria Land based on the Antarctic Conservation Biogeographic Regions. -
Molecular Biogeochemistry, Lecture 8
12.158 Lecture Pigment-derived Biomarkers (1) Colour, structure, distribution and function (2) Biosynthesis (3) Nomenclature (4) Aromatic carotenoids ● Biomarkers for phototrophic sulfur bacteria ● Alternative biological sources (5) Porphyrins and maleimides Many of the figures in this lecture were kindly provided by Jochen Brocks, RSES ANU 1 Carotenoid pigments ● Carotenoids are usually yellow, orange or red coloured pigments lutein β-carotene 17 18 19 2' 2 4 6 8 3 7 9 16 1 5 lycopenelycopene 2 Structural diversity ● More than 600 different natural structures are known, ● They are derived from the C40 carotenoid lycopene by varied hydrogenation, dehydrogenation, cyclization and oxidation reaction 17 18 19 2' 2 4 6 8 3 7 9 16 1 5 lycopene neurosporene α-carotene γ -carotene spirilloxanthin siphonaxanthin canthaxanthin spheroidenone 3 Structural diversity Purple non-sulfur bacteria peridinin 7,8-didehydroastaxanthin okenone fucoxanthin Biological distribution ● Carotenoids are biosynthesized de novo by all phototrophic bacteria, eukaryotes and halophilic archaea ● They are additionally synthesized by a large variety of non-phototrophs ● Vertebrates and invertebrates have to incorporate carotenoids through the diet, but have often the capacity to structurally modifiy them 4 Carotenoid function (1) Accessory pigments in Light Harvesting Complex (LHC) (annual production by marine phytoplancton alone: 4 million tons) e.g. LH-II Red and blue: protein complex Green: chlorophyll Yellow: lycopene (2) Photoprotection (3) photoreceptors for phototropism -
Phylogenetic and Evolutionary Patterns in Microbial Carotenoid Biosynthesis Are Revealed by Comparative Genomics
Phylogenetic and Evolutionary Patterns in Microbial Carotenoid Biosynthesis Are Revealed by Comparative Genomics Jonathan L. Klassen* Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada Abstract Background: Carotenoids are multifunctional, taxonomically widespread and biotechnologically important pigments. Their biosynthesis serves as a model system for understanding the evolution of secondary metabolism. Microbial carotenoid diversity and evolution has hitherto been analyzed primarily from structural and biosynthetic perspectives, with the few phylogenetic analyses of microbial carotenoid biosynthetic proteins using either used limited datasets or lacking methodological rigor. Given the recent accumulation of microbial genome sequences, a reappraisal of microbial carotenoid biosynthetic diversity and evolution from the perspective of comparative genomics is warranted to validate and complement models of microbial carotenoid diversity and evolution based upon structural and biosynthetic data. Methodology/Principal Findings: Comparative genomics were used to identify and analyze in silico microbial carotenoid biosynthetic pathways. Four major phylogenetic lineages of carotenoid biosynthesis are suggested composed of: (i) Proteobacteria; (ii) Firmicutes; (iii) Chlorobi, Cyanobacteria and photosynthetic eukaryotes; and (iv) Archaea, Bacteroidetes and two separate sub-lineages of Actinobacteria. Using this phylogenetic framework, specific evolutionary mechanisms are proposed for carotenoid desaturase CrtI-family -
Effect of Phenol on Β-Carotene Content in Total Carotenoids Production in Cultivation of Rhodotorula Glutinis
Korean J. Chem. Eng., 21(3), 689-692 (2004) Effect of Phenol on β-Carotene Content in Total Carotenoids Production in Cultivation of Rhodotorula glutinis Bong Kyun Kim*, Pyoung Kyu Park, Hee Jeong Chae** and Eui Yong Kim† Department of Chemical Engineering, University of Seoul, Seoul 130-743, Korea *R&D Center, SEMO Co. Ltd., Incheon 558-10, Korea **Department of Food and Biotechnology, and Department of Innovative Industrial Technology, Graduate School of Venture, Hoseo University, Asan 336-795, Korea (Received 28 November 2003 • accepted 18 December 2003) Abstract−The composition of carotenoids produced by R. glutinis was observed to be dependent upon the addition of phenol into medium. A stimulatory effect of phenol on β-carotene of Rhodotorula glutins K-501 grown on glucose was investigated. Carotenoids produced by Rhodotorula glutinis K-501 were identified to torularhodin, torulene and β-carotene, whose composition was 79.5%, 6.4% and 14.1%, respectively. The β-carotene content increased up to 35% when phenol was added to culture media at 500 ppm. The ratio of torularhodin decreased with increasing phenol con- centration, while torulene content was almost constant. Key words: Phenol, β-Carotene, Carotenogenic Ratio, Rhodotorula glutinis INTRODUCTION Sporobolomyces, produce a variety of carotenoids that have a broad region of light absorption of 450-550 nm so that the culture broth Carotenoids are liposoluble tetraterpenes, usually red or yellow, has a colored appearance [Girad et al., 1994; Walker et al., 1973]. and are one of the most important families of natural pigments. These The fermentation conditions, such as cultivation temperature [Nelis pigments have several conjugated double bonds that act as chro- and Deleenheer, 1991], lightening [Meyer et al., 1994], induced sub- mophores and thus absorb light in the visible region, which gives stances [Schroeder et al., 1993, 1995], and inhibitors [Girad et al., them their strong coloration properties. -
Classification of Three Airborne Bacteria and Proposal Of
International Journal of Systematic and Evolutionary Microbiology (2002), 52, 445–456 DOI: 10.1099/ijs.0.01682-0 Classification of three airborne bacteria and proposal of Hymenobacter aerophilus sp. nov. 1 Institut fu$ r Bakteriologie, Sandra Buczolits,1,2 Ewald B. M. Denner,2 Dietmar Vybiral,2 Mykologie und Hygiene, 1,2 3 1,2 Veterina$ rmedizinische Monika Wieser, Peter Ka$ mpfer and Hans-Ju$ rgen Busse Universita$ t, Veterina$ rplatz 1, A-1210 Wien, Austria 2 Author for correspondence: Hans-Ju$ rgen Busse. Tel: j43 1 25077 2128. Fax: j43 1 25077 2190. Institut fu$ r Mikrobiologie e-mail: Hans-Juergen.Busse!vu-wien.ac.at und Genetik, Universita$ t Wien, A-1030 Wien, Austria Three aerobic, Gram-negative, rod-shaped, non-spore-forming, red-pigmented, 3 Institut fu$ r Angewandte airborne bacteria (I/26-Cor1T, I/32A-Cor1 and I/74-Cor2) collected in the Museo Mikrobiologie, Justus- Liebig-Universita$ t Giessen, Correr (Venice, Italy) were investigated to determine their taxonomic status by D-35390 Giessen, Germany analysing their biochemical, physiological and chemotaxonomic features and the GMC content of genomic DNA and by comparing their genomic fingerprints. Additionally, the almost complete 16S rRNA gene sequence of strain I/26-Cor1T was analysed. The three strains were nearly identical in their morphological, physiological, biochemical and chemotaxonomic properties. The strains contained a menaquinone system with the predominant menaquinone MK-7 and a fatty acid profile with C15:0 anteiso, C15:0 iso and C16:1 predominant. Phosphatidylethanolamine and several unidentified lipids were detected in the polar lipid profiles. The polyamine pattern consisted of sym-homospermidine as the major compound. -
MYB72-Dependent Coumarin Exudation Shapes Root Microbiome Assembly to Promote Plant Health
MYB72-dependent coumarin exudation shapes root microbiome assembly to promote plant health Ioannis A. Stringlisa,1,KeYua,1, Kirstin Feussnerb,1, Ronnie de Jongea,c,d, Sietske Van Bentuma, Marcel C. Van Verka, Roeland L. Berendsena, Peter A. H. M. Bakkera, Ivo Feussnerb,e, and Corné M. J. Pietersea,2 aPlant–Microbe Interactions, Department of Biology, Science4Life, Utrecht University, 3508 TB Utrecht, The Netherlands; bDepartment of Plant Biochemistry, Albrecht-von-Haller-Institute for Plant Sciences, University of Göttingen, 37077 Göttingen, Germany; cDepartment of Plant Systems Biology, Vlaams Instituut voor Biotechnologie, 9052 Ghent, Belgium; dDepartment of Plant Biotechnology and Bioinformatics, Ghent University, 9052 Ghent, Belgium; and eDepartment of Plant Biochemistry, Göttingen Center for Molecular Biosciences, University of Göttingen, 37077 Göttingen, Germany Edited by Jeffery L. Dangl, University of North Carolina at Chapel Hill, Chapel Hill, NC, and approved April 3, 2018 (received for review December 22, 2017) Plant roots nurture a tremendous diversity of microbes via exudation of leaves do not display abundant transcriptional changes (9). photosynthetically fixed carbon sources. In turn, probiotic members of However, upon pathogen or insect attack, ISR-expressing leaves the root microbiome promote plant growth and protect the host plant develop an accelerated, primed defense response that is associated against pathogens and pests. In the Arabidopsis thaliana–Pseudomonas with enhanced resistance (9–11). In contrast to foliar tissues, simiae WCS417 model system the root-specific transcription factor WCS417-colonized roots show abundant transcriptional changes MYB72 and the MYB72-controlled β-glucosidase BGLU42 emerged as (9, 11–13). Among the WCS417-induced genes, the root-specific important regulators of beneficial rhizobacteria-induced systemic resis- R2R3-type MYB transcription factor gene MYB72 emerged as a tance (ISR) and iron-uptake responses. -
P^I"~ SUBMITTED to the DEPARTMENT of L \IL.~D EARTH, ATMOSPHERIC and PLANETARY SCIENCES in PARTIAL FULFILLMENT of the REQUIREMENTS for the DEGREE OF
Molecular studies of the sources and significance of archaeal lipids in the oceans by Sara Ann Lincoln MIA IsJ:S' iNSTITUTE B.S. Geosciences B.S. Geological Oceanography L T University of Rhode Island (2006) P^I"~ SUBMITTED TO THE DEPARTMENT OF L \IL.~d EARTH, ATMOSPHERIC AND PLANETARY SCIENCES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN GEOCHEMISTRY SEPTEMBER 2013 © Massachusetts Institute of Technology All rights reserved. Author:................. Department of Earth, Atmospheric and Planetary Sciences Certified by:........................... Roger E. Summons Professor of Geobiology Department of Earth, Atmospheric and Planetary Sciences Thesis supervisor ..................#......r....... ........................................................ Edward F. DeLong Morton and Claire Goulder amily P fessor in Environmental Systems Depar e Civil and Environmental Engineering 7) Thesis supervisor Accepted by: ...................................... Robert van der Hilst Schlumberger Professor of Earth Sciences Head, Department of Earth, Atmospheric and Planetary Sciences THIS PAGE INTENTIONALLY LEFT BLANK Molecular studies of the sources and significance of archaeal lipids in the oceans by Sara Ann Lincoln Submitted to the Department of Earth, Atmospheric and Planetary Sciences on July 29, 2013 in partial fulfillment of the requirements for the Degree of Doctor of Philosophy in Geochemistry ABSTRACT Marine archaea are ubiquitous and abundant in the modem oceans and have a geologic record extending >100 million years. However, factors influencing the populations of the major clades - chemolithoautotrophic Marine Group I Thaumarchaeota (MG-I) and heterotrophic Marine Group II Euryarchaeota (MG-II) - and their membrane lipid signatures are not well understood. Here, I paired techniques of organic geochemistry and molecular biology to explore the sources and significance of archaeal tetraether lipids in the marine water column. -
Ancestry and Adaptive Radiation of Bacteroidetes As Assessed by Comparative Genomics
1 Ancestry and adaptive radiation of Bacteroidetes as assessed by comparative genomics 2 3 Raul Munoza,b,*, Hanno Teelinga, Rudolf Amanna and Ramon Rosselló-Mórab,* 4 5 a Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, D-28359 6 Bremen, Germany. 7 b Marine Microbiology Group, Department of Ecology and Marine Resources, Institut Mediterrani 8 d’Estudis Avançats (CSIC-UIB), E-07190 Esporles, Balearic Islands, Spain. 9 10 * Corresponding authors: 11 Raul Munoz, Marine Microbiology Group, Carrer Miquel Marquès 21, 07190 Esporles, Illes 12 Balears, Spain. e-mail: [email protected] 13 Ramon Rosselló-Móra, Marine Microbiology Group, Carrer Miquel Marquès 21, 07190 Esporles, 14 Illes Balears, Spain. e-mail: [email protected] 15 16 17 18 Keywords + 19 Bacteroidetes, Na -NQR, alternative complex III, caa3 cytochrome oxidase, gliding, T9SS. 20 21 Abbreviations 22 m.s.i.: median sequence identity. 23 24 25 26 27 ABSTRACT 28 As of this writing, the phylum Bacteroidetes comprises more than 1,500 described species with 29 diverse ecological roles. However, there is little understanding of archetypal Bacteroidetes traits on 30 a genomic level. We compiled a representative set of 89 Bacteroidetes genomes and used pairwise 31 reciprocal best match gene comparisons and gene syntenies to identify common traits that allow to 32 trace Bacteroidetes’ evolution and adaptive radiation. Highly conserved among all studied 33 Bacteroidetes was the type IX secretion system (T9SS). Class-level comparisons furthermore 34 suggested that the ACIII-caa3COX super-complex evolved in the ancestral aerobic bacteroidetal 35 lineage, and was secondarily lost in extant anaerobic Bacteroidetes. -
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 -
Algal Toxic Compounds and Their Aeroterrestrial, Airborne and Other Extremophilic Producers with Attention to Soil and Plant Contamination: a Review
toxins Review Algal Toxic Compounds and Their Aeroterrestrial, Airborne and other Extremophilic Producers with Attention to Soil and Plant Contamination: A Review Georg G¨аrtner 1, Maya Stoyneva-G¨аrtner 2 and Blagoy Uzunov 2,* 1 Institut für Botanik der Universität Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria; [email protected] 2 Department of Botany, Faculty of Biology, Sofia University “St. Kliment Ohridski”, 8 blvd. Dragan Tsankov, 1164 Sofia, Bulgaria; mstoyneva@uni-sofia.bg * Correspondence: buzunov@uni-sofia.bg Abstract: The review summarizes the available knowledge on toxins and their producers from rather disparate algal assemblages of aeroterrestrial, airborne and other versatile extreme environments (hot springs, deserts, ice, snow, caves, etc.) and on phycotoxins as contaminants of emergent concern in soil and plants. There is a growing body of evidence that algal toxins and their producers occur in all general types of extreme habitats, and cyanobacteria/cyanoprokaryotes dominate in most of them. Altogether, 55 toxigenic algal genera (47 cyanoprokaryotes) were enlisted, and our analysis showed that besides the “standard” toxins, routinely known from different waterbodies (microcystins, nodularins, anatoxins, saxitoxins, cylindrospermopsins, BMAA, etc.), they can produce some specific toxic compounds. Whether the toxic biomolecules are related with the harsh conditions on which algae have to thrive and what is their functional role may be answered by future studies. Therefore, we outline the gaps in knowledge and provide ideas for further research, considering, from one side, Citation: G¨аrtner, G.; the health risk from phycotoxins on the background of the global warming and eutrophication and, ¨а Stoyneva-G rtner, M.; Uzunov, B.