The Role of Polyphosphate in Motility, Adhesion, and Biofilm Formation in Sulfolobales. Microorganisms 2021, 9
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Genome-Resolved Meta-Analysis of the Microbiome in Oil Reservoirs Worldwide
microorganisms Article Genome-Resolved Meta-Analysis of the Microbiome in Oil Reservoirs Worldwide Kelly J. Hidalgo 1,2,* , Isabel N. Sierra-Garcia 3 , German Zafra 4 and Valéria M. de Oliveira 1 1 Microbial Resources Division, Research Center for Chemistry, Biology and Agriculture (CPQBA), University of Campinas–UNICAMP, Av. Alexandre Cazellato 999, 13148-218 Paulínia, Brazil; [email protected] 2 Graduate Program in Genetics and Molecular Biology, Institute of Biology, University of Campinas (UNICAMP), Rua Monteiro Lobato 255, Cidade Universitária, 13083-862 Campinas, Brazil 3 Biology Department & CESAM, University of Aveiro, Aveiro, Portugal, Campus de Santiago, Avenida João Jacinto de Magalhães, 3810-193 Aveiro, Portugal; [email protected] 4 Grupo de Investigación en Bioquímica y Microbiología (GIBIM), Escuela de Microbiología, Universidad Industrial de Santander, Cra 27 calle 9, 680002 Bucaramanga, Colombia; [email protected] * Correspondence: [email protected]; Tel.: +55-19981721510 Abstract: Microorganisms inhabiting subsurface petroleum reservoirs are key players in biochemical transformations. The interactions of microbial communities in these environments are highly complex and still poorly understood. This work aimed to assess publicly available metagenomes from oil reservoirs and implement a robust pipeline of genome-resolved metagenomics to decipher metabolic and taxonomic profiles of petroleum reservoirs worldwide. Analysis of 301.2 Gb of metagenomic information derived from heavily flooded petroleum reservoirs in China and Alaska to non-flooded petroleum reservoirs in Brazil enabled us to reconstruct 148 metagenome-assembled genomes (MAGs) of high and medium quality. At the phylum level, 74% of MAGs belonged to bacteria and 26% to archaea. The profiles of these MAGs were related to the physicochemical parameters and recovery management applied. -
Marsarchaeota Are an Aerobic Archaeal Lineage Abundant in Geothermal Iron Oxide Microbial Mats
Marsarchaeota are an aerobic archaeal lineage abundant in geothermal iron oxide microbial mats Authors: Zackary J. Jay, Jacob P. Beam, Mansur Dlakic, Douglas B. Rusch, Mark A. Kozubal, and William P. Inskeep This is a postprint of an article that originally appeared in Nature Microbiology on May 14, 2018. The final version can be found at https://dx.doi.org/10.1038/s41564-018-0163-1. Jay, Zackary J. , Jacob P. Beam, Mensur Dlakic, Douglas B. Rusch, Mark A. Kozubal, and William P. Inskeep. "Marsarchaeota are an aerobic archaeal lineage abundant in geothermal iron oxide microbial mats." Nature Microbiology 3, no. 6 (May 2018): 732-740. DOI: 10.1038/ s41564-018-0163-1. Made available through Montana State University’s ScholarWorks scholarworks.montana.edu Marsarchaeota are an aerobic archaeal lineage abundant in geothermal iron oxide microbial mats Zackary J. Jay1,4,7, Jacob P. Beam1,5,7, Mensur Dlakić2, Douglas B. Rusch3, Mark A. Kozubal1,6 and William P. Inskeep 1* The discovery of archaeal lineages is critical to our understanding of the universal tree of life and evolutionary history of the Earth. Geochemically diverse thermal environments in Yellowstone National Park provide unprecedented opportunities for studying archaea in habitats that may represent analogues of early Earth. Here, we report the discovery and character- ization of a phylum-level archaeal lineage proposed and herein referred to as the ‘Marsarchaeota’, after the red planet. The Marsarchaeota contains at least two major subgroups prevalent in acidic, microaerobic geothermal Fe(III) oxide microbial mats across a temperature range from ~50–80 °C. Metagenomics, single-cell sequencing, enrichment culturing and in situ transcrip- tional analyses reveal their biogeochemical role as facultative aerobic chemoorganotrophs that may also mediate the reduction of Fe(III). -
Archaeology of Eukaryotic DNA Replication
Downloaded from http://cshperspectives.cshlp.org/ on September 25, 2021 - Published by Cold Spring Harbor Laboratory Press Archaeology of Eukaryotic DNA Replication Kira S. Makarova and Eugene V. Koonin National Center for Biotechnology Information, National Library of Medicine, National Institutes of Health, Bethesda, Maryland 20894 Correspondence: [email protected] Recent advances in the characterization of the archaeal DNA replication system together with comparative genomic analysis have led to the identification of several previously un- characterized archaeal proteins involved in replication and currently reveal a nearly com- plete correspondence between the components of the archaeal and eukaryotic replication machineries. It can be inferred that the archaeal ancestor of eukaryotes and even the last common ancestor of all extant archaea possessed replication machineries that were compa- rable in complexity to the eukaryotic replication system. The eukaryotic replication system encompasses multiple paralogs of ancestral components such that heteromeric complexes in eukaryotes replace archaeal homomeric complexes, apparently along with subfunctionali- zation of the eukaryotic complex subunits. In the archaea, parallel, lineage-specific dupli- cations of many genes encoding replication machinery components are detectable as well; most of these archaeal paralogs remain to be functionally characterized. The archaeal rep- lication system shows remarkable plasticity whereby even some essential components such as DNA polymerase and single-stranded DNA-binding protein are displaced by unrelated proteins with analogous activities in some lineages. ouble-stranded DNA is the molecule that Okazaki fragments (Kornberg and Baker 2005; Dcarries genetic information in all cellular Barry and Bell 2006; Hamdan and Richardson life-forms; thus, replication of this genetic ma- 2009; Hamdan and van Oijen 2010). -
Insights Into Archaeal Evolution and Symbiosis from the Genomes of a Nanoarchaeon and Its Inferred Crenarchaeal Host from Obsidian Pool, Yellowstone National Park
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Microbiology Publications and Other Works Microbiology 4-22-2013 Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar University of Tennessee - Knoxville, [email protected] Kira S. Makarova National Institutes of Health David E. Graham University of Tennessee - Knoxville, [email protected] Yuri I. Wolf National Institutes of Health Eugene V. Koonin National Institutes of Health See next page for additional authors Follow this and additional works at: https://trace.tennessee.edu/utk_micrpubs Part of the Microbiology Commons Recommended Citation Biology Direct 2013, 8:9 doi:10.1186/1745-6150-8-9 This Article is brought to you for free and open access by the Microbiology at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Microbiology Publications and Other Works by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. Authors Mircea Podar, Kira S. Makarova, David E. Graham, Yuri I. Wolf, Eugene V. Koonin, and Anna-Louise Reysenbach This article is available at TRACE: Tennessee Research and Creative Exchange: https://trace.tennessee.edu/ utk_micrpubs/44 Podar et al. Biology Direct 2013, 8:9 http://www.biology-direct.com/content/8/1/9 RESEARCH Open Access Insights into archaeal evolution and symbiosis from the genomes of a nanoarchaeon and its inferred crenarchaeal host from Obsidian Pool, Yellowstone National Park Mircea Podar1,2*, Kira S Makarova3, David E Graham1,2, Yuri I Wolf3, Eugene V Koonin3 and Anna-Louise Reysenbach4 Abstract Background: A single cultured marine organism, Nanoarchaeum equitans, represents the Nanoarchaeota branch of symbiotic Archaea, with a highly reduced genome and unusual features such as multiple split genes. -
A Survey of Carbon Fixation Pathways Through a Quantitative Lens
Journal of Experimental Botany, Vol. 63, No. 6, pp. 2325–2342, 2012 doi:10.1093/jxb/err417 Advance Access publication 26 December, 2011 REVIEW PAPER A survey of carbon fixation pathways through a quantitative lens Arren Bar-Even, Elad Noor and Ron Milo* Department of Plant Sciences, The Weizmann Institute of Science, Rehovot 76100, Israel * To whom correspondence should be addressed. E-mail: [email protected] Received 15 August 2011; Revised 4 November 2011; Accepted 8 November 2011 Downloaded from Abstract While the reductive pentose phosphate cycle is responsible for the fixation of most of the carbon in the biosphere, it http://jxb.oxfordjournals.org/ has several natural substitutes. In fact, due to the characterization of three new carbon fixation pathways in the last decade, the diversity of known metabolic solutions for autotrophic growth has doubled. In this review, the different pathways are analysed and compared according to various criteria, trying to connect each of the different metabolic alternatives to suitable environments or metabolic goals. The different roles of carbon fixation are discussed; in addition to sustaining autotrophic growth it can also be used for energy conservation and as an electron sink for the recycling of reduced electron carriers. Our main focus in this review is on thermodynamic and kinetic aspects, including thermodynamically challenging reactions, the ATP requirement of each pathway, energetic constraints on carbon fixation, and factors that are expected to limit the rate of the pathways. Finally, possible metabolic structures at Weizmann Institute of Science on July 3, 2016 of yet unknown carbon fixation pathways are suggested and discussed. -
Counts Metabolic Yr10.Pdf
Advanced Review Physiological, metabolic and biotechnological features of extremely thermophilic microorganisms James A. Counts,1 Benjamin M. Zeldes,1 Laura L. Lee,1 Christopher T. Straub,1 Michael W.W. Adams2 and Robert M. Kelly1* The current upper thermal limit for life as we know it is approximately 120C. Microorganisms that grow optimally at temperatures of 75C and above are usu- ally referred to as ‘extreme thermophiles’ and include both bacteria and archaea. For over a century, there has been great scientific curiosity in the basic tenets that support life in thermal biotopes on earth and potentially on other solar bodies. Extreme thermophiles can be aerobes, anaerobes, autotrophs, hetero- trophs, or chemolithotrophs, and are found in diverse environments including shallow marine fissures, deep sea hydrothermal vents, terrestrial hot springs— basically, anywhere there is hot water. Initial efforts to study extreme thermo- philes faced challenges with their isolation from difficult to access locales, pro- blems with their cultivation in laboratories, and lack of molecular tools. Fortunately, because of their relatively small genomes, many extreme thermo- philes were among the first organisms to be sequenced, thereby opening up the application of systems biology-based methods to probe their unique physiologi- cal, metabolic and biotechnological features. The bacterial genera Caldicellulosir- uptor, Thermotoga and Thermus, and the archaea belonging to the orders Thermococcales and Sulfolobales, are among the most studied extreme thermo- philes to date. The recent emergence of genetic tools for many of these organ- isms provides the opportunity to move beyond basic discovery and manipulation to biotechnologically relevant applications of metabolic engineering. -
The Archaeal Ced System Imports DNA
The archaeal Ced system imports DNA Marleen van Wolferena,1, Alexander Wagnera,1, Chris van der Doesa, and Sonja-Verena Albersa,2 aMolecular Biology of Archaea, Institute of Biology II – Microbiology, University of Freiburg, 79104 Freiburg, Germany Edited by Norman R. Pace, University of Colorado at Boulder, Boulder, CO, and approved January 12, 2016 (received for review July 13, 2015) The intercellular transfer of DNA is a phenomenon that occurs species exchange chromosomal DNA between cells connected by in all domains of life and is a major driving force of evolution. bridges (11). This transfer is thought to occur in a bidirectional Upon UV-light treatment, cells of the crenarchaeal genus Sulfo- manner via cell fusion leading to the formation of diploid cells with lobus express Ups pili, which initiate cell aggregate formation. mixed chromosomes (12). Interestingly, this type of DNA transfer Within these aggregates, chromosomal DNA, which is used for was shown to occur between different Haloferax species and in- the repair of DNA double-strand breaks, is exchanged. Because volved DNA fragments of up to 500 kbp DNA (13). Nevertheless, so far no clear homologs of bacterial DNA transporters have the mechanism of DNA transfer is so far not understood. Other been identified among the genomes of Archaea, the mechanisms described archaeal conjugative systems include self-transmissible of archaeal DNA transport have remained a puzzling and under- plasmids, which have so far only been studied for Sulfolobus spe- saci_0568 saci_0748, investigated topic. Here we identify and cies. These plasmids are grouped into the so-called pKEF and Sulfolobus acidocaldarius two genes from that are highly in- pARN plasmids (14, 15) and only a few of their genes encode duced upon UV treatment, encoding a transmembrane protein homologs of bacterial conjugation proteins, including the so-far- and a membrane-bound VirB4/HerA homolog, respectively. -
(Gid ) Genes Coding for Putative Trna:M5u-54 Methyltransferases in 355 Bacterial and Archaeal Complete Genomes
Table S1. Taxonomic distribution of the trmA and trmFO (gid ) genes coding for putative tRNA:m5U-54 methyltransferases in 355 bacterial and archaeal complete genomes. Asterisks indicate the presence and the number of putative genes found. Genomes Taxonomic position TrmA Gid Archaea Crenarchaea Aeropyrum pernix_K1 Crenarchaeota; Thermoprotei; Desulfurococcales; Desulfurococcaceae Cenarchaeum symbiosum Crenarchaeota; Thermoprotei; Cenarchaeales; Cenarchaeaceae Pyrobaculum aerophilum_str_IM2 Crenarchaeota; Thermoprotei; Thermoproteales; Thermoproteaceae Sulfolobus acidocaldarius_DSM_639 Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Sulfolobus solfataricus Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Sulfolobus tokodaii Crenarchaeota; Thermoprotei; Sulfolobales; Sulfolobaceae Euryarchaea Archaeoglobus fulgidus Euryarchaeota; Archaeoglobi; Archaeoglobales; Archaeoglobaceae Haloarcula marismortui_ATCC_43049 Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloarcula Halobacterium sp Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloarcula Haloquadratum walsbyi Euryarchaeota; Halobacteria; Halobacteriales; Halobacteriaceae; Haloquadra Methanobacterium thermoautotrophicum Euryarchaeota; Methanobacteria; Methanobacteriales; Methanobacteriaceae Methanococcoides burtonii_DSM_6242 Euryarchaeota; Methanomicrobia; Methanosarcinales; Methanosarcinaceae Methanococcus jannaschii Euryarchaeota; Methanococci; Methanococcales; Methanococcaceae Methanococcus maripaludis_S2 Euryarchaeota; Methanococci; -
Post-Genomic Characterization of Metabolic Pathways in Sulfolobus Solfataricus
Post-Genomic Characterization of Metabolic Pathways in Sulfolobus solfataricus Jasper Walther Thesis committee Thesis supervisors Prof. dr. J. van der Oost Personal chair at the laboratory of Microbiology Wageningen University Prof. dr. W. M. de Vos Professor of Microbiology Wageningen University Other members Prof. dr. W.J.H. van Berkel Wageningen University Prof. dr. V.A.F. Martins dos Santos Wageningen University Dr. T.J.G. Ettema Uppsala University, Sweden Dr. S.V. Albers Max Planck Institute for Terrestrial Microbiology, Marburg, Germany This research was conducted under the auspices of the Graduate School VLAG Post-Genomic Characterization of Metabolic Pathways in Sulfolobus solfataricus Jasper Walther Thesis Submitted in fulfilment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnificus Prof. dr. M.J. Kropff, in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Monday 23 January 2012 at 11 a.m. in the Aula. Jasper Walther Post-Genomic Characterization of Metabolic Pathways in Sulfolobus solfataricus, 164 pages. Thesis, Wageningen University, Wageningen, NL (2012) With references, with summaries in Dutch and English ISBN 978-94-6173-203-3 Table of contents Chapter 1 Introduction 1 Chapter 2 Hot Transcriptomics 17 Chapter 3 Reconstruction of central carbon metabolism in Sulfolobus solfataricus using a two-dimensional gel electrophoresis map, stable isotope labelling and DNA microarray analysis 45 Chapter 4 Identification of the Missing -
Ammonia-Oxidizing Archaea Use the Most Energy Efficient Aerobic Pathway for CO2 Fixation
Ammonia-oxidizing archaea use the most energy efficient aerobic pathway for CO2 fixation Martin Könneke, Daniel M. Schubert, Philip C. Brown, Michael Hügler, Sonja Standfest, Thomas Schwander, Lennart Schada von Borzyskowski, Tobias J. Erb, David A. Stahl, Ivan A. Berg Supporting Information: Supplementary Appendix SI Text Phylogenetic analysis of the proteins involved in the HP/HB cycle in N. maritimus. The enzymes of the HP/HB cycle with unequivocally identified genes consisting of more than 200 amino acids were used for the phylogenetic analysis (Table 1). The genes for biotin carrier protein (Nmar_0274, 140 amino acids), small subunit of methylmalonyl-CoA mutase (Nmar_0958, 140 amino acids) and methylmalonyl-CoA epimerase (Nmar_0953, 131 amino acids) were not analyzed, because their small size prevents reliable phylogenetic tree construction. The genes for acetyl-CoA/propionyl-CoA carboxylase and methylmalonyl-CoA carboxylase homologues can be found in autotrophic Thaumarchaeota and aerobic Crenarchaeota as well as in some heterotrophic Archaea (SI Appendix, Figs. S7-S9, Table S4). Although these enzymes are usually regarded as characteristic enzymes of the HP/HB cycle, they also participate in various heterotrophic pathways in Archaea, e.g. in the methylaspartate cycle of acetate assimilation in haloarchaea (1), propionate and leucine assimilation (2, 3), oxaloacetate or methylmalonyl-CoA decarboxylation (4, 5), anaplerotic pyruvate carboxylation (6). In all three trees (SI Appendix, Figs. S7-S9) the crenarchaeal enzymes tend to cluster with thaumarchaeal ones, but there appears to be no special connection between aerobic Crenarchaeota (Sulfolobales) and Thaumarchaeota sequences. Thaumarchaeal 4-hydroxybutyryl-CoA dehydratase genes form a separate cluster closely related to bacterial sequences; the bacterial enzymes are probably involved in aminobutyrate fermentation (Fig. -
Calditol-Linked Membrane Lipids Are Required for Acid Tolerance in Sulfolobus Acidocaldarius
Calditol-linked membrane lipids are required for acid tolerance in Sulfolobus acidocaldarius Zhirui Zenga,1, Xiao-Lei Liub,1, Jeremy H. Weia, Roger E. Summonsc, and Paula V. Welandera,2 aDepartment of Earth System Science, Stanford University, Stanford, CA 94305; bDepartment of Geology and Geophysics, University of Oklahoma, Norman, OK 73019; and cDepartment of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139 Edited by Katherine H. Freeman, Pennsylvania State University, University Park, PA, and approved November 7, 2018 (received for review August 14, 2018) Archaea have many unique physiological features of which the lipid and sea-surface temperatures in the Mesozoic and early Cenozoic, composition of their cellular membranes is the most striking. and the geologic history of archaea in ancient sediments (13, 14). Archaeal ether-linked isoprenoidal membranes can occur as bilayers However, deciphering the evolutionary implications of archaeal or monolayers, possess diverse polar head groups, and a multiplicity lipid biosynthesis, as well as being able to properly interpret ar- of ring structures in the isoprenoidal cores. These lipid structures chaeal lipid biomarkers, requires a full understanding of the are proposed to provide protection from the extreme temperature, biosynthetic pathways and the physiological roles of these various pH, salinity, and nutrient-starved conditions that many archaea structures in extant archaea. inhabit. However, many questions remain regarding the synthesis Studies of archaeal membrane lipid synthesis have revealed and physiological role of some of the more complex archaeal lipids. distinct proteins and biochemical reactions, but several open In this study, we identify a radical S-adenosylmethionine (SAM) questions remain (4, 15). -
Lipids of Sulfolobus Spp. | Encyclopedia
Lipids of Sulfolobus spp. Subjects: Biophysics | Biotechnology Contributors: Kerstin Rastaedter , David J. Wurm Submitted by: Kerstin Rastaedter Definition Archaea, and thereby, Sulfolobus spp. exhibit a unique lipid composition of ether lipids, which are altered in regard to the ratio of diether to tetraether lipids, number of cyclopentane rings and type of head groups, as a coping mechanism against environmental changes. Sulfolobales mainly consist of C40-40 tetraether lipids (caldarchaeol) and partly of C20-20 diether lipids (archaeol). A variant of caldarchaeol called glycerol dialkylnonitol tetraether (GDNT) has only been found in Sulfolobus and other members of the Creanarchaeota phylum so far. Altering the numbers of incorporated cyclopentane rings or the the diether to tetraether ratio results in more tightly packed membranes or vice versa. 1. The Cell Membrane and Lipids of Sulfolobus spp. The thermoacidophilic genus Sulfolobus belongs to the phylum Crenarchaeota and is a promising player for biotechnology [1], since it harbors a couple of valuable products, such as extremozymes[ 2], trehalose [3], archaeocins [4] and lipids for producing archaeosomes [5]. Genetic tools for this genus have rapidly advanced in recent years[ 6], generating new possibilities in basic science and for biotechnological applications alike. The cultivation conditions are preferably at around 80 °C and pH 3 [7]. Sulfolobus species are able to grow aerobically and can be readily cultivated on a laboratory scale. These organisms became a model organism for Crenarchaeota and for adaption processes to extreme environments [8][9][10][11][12][13]. Sulfolobus species were found in solfataric fields all over the world[ 14]. A major drawback of cultivating this organism was the lack of a defined cultivation medium.