A New View of the Tree of Life
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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). -
The Great Oxidation Event Expanded the Genetic Repertoire of Arsenic Metabolism and Cycling
The Great Oxidation Event expanded the genetic repertoire of arsenic metabolism and cycling Song-Can Chena,b,c,1, Guo-Xin Suna,1, Yu Yand, Konstantinos T. Konstantinidise,f, Si-Yu Zhange, Ye Denga, Xiao-Min Lia,c, Hui-Ling Cuia,c, Florin Musatb, Denny Poppg, Barry P. Rosenh,2, and Yong-Guan Zhua,i,2 aState Key Lab of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, 100085 Beijing, China; bDepartment of Isotope Biogeochemistry, Helmholtz Centre for Environmental Research – UFZ, 04318 Leipzig, Germany; cCollege of Resources and Environment, University of Chinese Academy of Sciences, 100049 Beijing, China; dDepartment of Environmental Science and Engineering, Huaqiao University, 361021 Xiamen, China; eSchool of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, GA 30332; fSchool of Biological Sciences, Georgia Institute of Technology, Atlanta, GA 30332; gDepartment of Environmental Microbiology, Helmholtz Centre for Environmental Research – UFZ, 04318 Leipzig, Germany; hDepartment of Cellular Biology and Pharmacology, Herbert Wertheim College of Medicine, Florida International University, Miami, FL 33199; and iKey Lab of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, 361021 Xiamen, China Edited by Donald E. Canfield, Institute of Biology and Nordic Center for Earth Evolution (NordCEE), University of Southern Denmark, Odense M., Denmark, and approved March 20, 2020 (received for review January 25, 2020) The rise of oxygen on the early Earth about 2.4 billion years ago under an atmosphere with very low oxygen levels (<<0.001% reorganized the redox cycle of harmful metal(loids), including that compared with present atmospheric level) (9). -
Global Metagenomic Survey Reveals a New Bacterial Candidate Phylum in Geothermal Springs
ARTICLE Received 13 Aug 2015 | Accepted 7 Dec 2015 | Published 27 Jan 2016 DOI: 10.1038/ncomms10476 OPEN Global metagenomic survey reveals a new bacterial candidate phylum in geothermal springs Emiley A. Eloe-Fadrosh1, David Paez-Espino1, Jessica Jarett1, Peter F. Dunfield2, Brian P. Hedlund3, Anne E. Dekas4, Stephen E. Grasby5, Allyson L. Brady6, Hailiang Dong7, Brandon R. Briggs8, Wen-Jun Li9, Danielle Goudeau1, Rex Malmstrom1, Amrita Pati1, Jennifer Pett-Ridge4, Edward M. Rubin1,10, Tanja Woyke1, Nikos C. Kyrpides1 & Natalia N. Ivanova1 Analysis of the increasing wealth of metagenomic data collected from diverse environments can lead to the discovery of novel branches on the tree of life. Here we analyse 5.2 Tb of metagenomic data collected globally to discover a novel bacterial phylum (‘Candidatus Kryptonia’) found exclusively in high-temperature pH-neutral geothermal springs. This lineage had remained hidden as a taxonomic ‘blind spot’ because of mismatches in the primers commonly used for ribosomal gene surveys. Genome reconstruction from metagenomic data combined with single-cell genomics results in several high-quality genomes representing four genera from the new phylum. Metabolic reconstruction indicates a heterotrophic lifestyle with conspicuous nutritional deficiencies, suggesting the need for metabolic complementarity with other microbes. Co-occurrence patterns identifies a number of putative partners, including an uncultured Armatimonadetes lineage. The discovery of Kryptonia within previously studied geothermal springs underscores the importance of globally sampled metagenomic data in detection of microbial novelty, and highlights the extraordinary diversity of microbial life still awaiting discovery. 1 Department of Energy Joint Genome Institute, Walnut Creek, California 94598, USA. 2 Department of Biological Sciences, University of Calgary, Calgary, Alberta T2N 1N4, Canada. -
Geomicrobiological Processes in Extreme Environments: a Review
202 Articles by Hailiang Dong1, 2 and Bingsong Yu1,3 Geomicrobiological processes in extreme environments: A review 1 Geomicrobiology Laboratory, China University of Geosciences, Beijing, 100083, China. 2 Department of Geology, Miami University, Oxford, OH, 45056, USA. Email: [email protected] 3 School of Earth Sciences, China University of Geosciences, Beijing, 100083, China. The last decade has seen an extraordinary growth of and Mancinelli, 2001). These unique conditions have selected Geomicrobiology. Microorganisms have been studied in unique microorganisms and novel metabolic functions. Readers are directed to recent review papers (Kieft and Phelps, 1997; Pedersen, numerous extreme environments on Earth, ranging from 1997; Krumholz, 2000; Pedersen, 2000; Rothschild and crystalline rocks from the deep subsurface, ancient Mancinelli, 2001; Amend and Teske, 2005; Fredrickson and Balk- sedimentary rocks and hypersaline lakes, to dry deserts will, 2006). A recent study suggests the importance of pressure in the origination of life and biomolecules (Sharma et al., 2002). In and deep-ocean hydrothermal vent systems. In light of this short review and in light of some most recent developments, this recent progress, we review several currently active we focus on two specific aspects: novel metabolic functions and research frontiers: deep continental subsurface micro- energy sources. biology, microbial ecology in saline lakes, microbial Some metabolic functions of continental subsurface formation of dolomite, geomicrobiology in dry deserts, microorganisms fossil DNA and its use in recovery of paleoenviron- Because of the unique geochemical, hydrological, and geological mental conditions, and geomicrobiology of oceans. conditions of the deep subsurface, microorganisms from these envi- Throughout this article we emphasize geomicrobiological ronments are different from surface organisms in their metabolic processes in these extreme environments. -
Intra-Field Variation of Prokaryotic Communities on and Below the Seafloor 24 in the Back-Arc Hydrothermal System of the Southern Mariana Trough
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector Intra-Field Variation of Prokaryotic Communities On and Below the Seafloor 24 in the Back-Arc Hydrothermal System of the Southern Mariana Trough Shingo Kato, Moriya Ohkuma, and Akihiko Yamagishi Abstract Deep-sea hydrothermal vents harbor diverse prokaryotes. There are a variety of habitat types in a deep-sea hydrothermal field, e.g., active and inactive chimneys, iron-rich mats, venting fluid and hydrothermal plume. Numerous studies have shown the diversity and composition of prokaryotic communities in individual habitats. However, it is still unclear whether and how the characteristics of prokaryotic communities in their respective habitats are different. Previously, we reported 16S rRNA genes in a variety of habitats, i.e., hydrothermally active and inactive chimneys, iron-rich mats, a vent fluid, crustal fluids from boreholes, as well as ambient seawater in a back-arc basin hydrothermal field of the Southern Mariana Trough. Here we summarize the prokaryotic communities in the col- lected samples at higher taxonomic resolution (up to family level) using the detected 16S rRNA gene sequences and compare them using recently developed bioinformatics tools. The comparative analysis clearly highlights differences in prokaryotic communities among the habitat types on and below the seafloor in the Southern Mariana Trough. Furthermore, descriptions of cultured species and environmental clones close to the detected sequences provide valuable information for understanding of their distribution and potential of ecological roles in deep-sea hydrothermal fields. Keywords 16S rRNA gene Archaea Back-arc basin Bacteria Chemosynthetic ecosystem Deep- sea hydrothermal vents Prokaryotic community 24.1 Introduction The online version of this chapter (doi:10.1007/978-4-431-54865-2_24) Deep-sea hydrothermal vents are oases for organisms on the contains supplementary material, which is available to authorized users. -
The Phylogenetic Composition and Structure of Soil Microbial Communities Shifts in Response to Elevated Carbon Dioxide
The ISME Journal (2012) 6, 259–272 & 2012 International Society for Microbial Ecology All rights reserved 1751-7362/12 www.nature.com/ismej ORIGINAL ARTICLE The phylogenetic composition and structure of soil microbial communities shifts in response to elevated carbon dioxide Zhili He1, Yvette Piceno2, Ye Deng1, Meiying Xu1,3, Zhenmei Lu1,4, Todd DeSantis2, Gary Andersen2, Sarah E Hobbie5, Peter B Reich6 and Jizhong Zhou1,2 1Institute for Environmental Genomics, Department of Botany and Microbiology, University of Oklahoma, Norman, OK, USA; 2Ecology Department, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, USA; 3Guangdong Provincial Key Laboratory of Microbial Culture Collection and Application, Guangdong Institute of Microbiology, Guangzhou, China; 4College of Life Sciences, Zhejiang University, Hangzhou, China; 5Department of Ecology, Evolution, and Behavior, St Paul, MN, USA and 6Department of Forest Resources, University of Minnesota, St Paul, MN, USA One of the major factors associated with global change is the ever-increasing concentration of atmospheric CO2. Although the stimulating effects of elevated CO2 (eCO2) on plant growth and primary productivity have been established, its impacts on the diversity and function of soil microbial communities are poorly understood. In this study, phylogenetic microarrays (PhyloChip) were used to comprehensively survey the richness, composition and structure of soil microbial communities in a grassland experiment subjected to two CO2 conditions (ambient, 368 p.p.m., versus elevated, 560 p.p.m.) for 10 years. The richness based on the detected number of operational taxonomic units (OTUs) significantly decreased under eCO2. PhyloChip detected 2269 OTUs derived from 45 phyla (including two from Archaea), 55 classes, 99 orders, 164 families and 190 subfamilies. -
Resilience of Microbial Communities After Hydrogen Peroxide Treatment of a Eutrophic Lake to Suppress Harmful Cyanobacterial Blooms
microorganisms Article Resilience of Microbial Communities after Hydrogen Peroxide Treatment of a Eutrophic Lake to Suppress Harmful Cyanobacterial Blooms Tim Piel 1,†, Giovanni Sandrini 1,†,‡, Gerard Muyzer 1 , Corina P. D. Brussaard 1,2 , Pieter C. Slot 1, Maria J. van Herk 1, Jef Huisman 1 and Petra M. Visser 1,* 1 Department of Freshwater and Marine Ecology, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, 1090 GE Amsterdam, The Netherlands; [email protected] (T.P.); [email protected] (G.S.); [email protected] (G.M.); [email protected] (C.P.D.B.); [email protected] (P.C.S.); [email protected] (M.J.v.H.); [email protected] (J.H.) 2 Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherland Institute for Sea Research, 1790 AB Den Burg, The Netherlands * Correspondence: [email protected]; Tel.: +31-20-5257073 † These authors have contributed equally to this work. ‡ Current address: Department of Technology & Sources, Evides Water Company, 3006 AL Rotterdam, The Netherlands. Abstract: Applying low concentrations of hydrogen peroxide (H2O2) to lakes is an emerging method to mitigate harmful cyanobacterial blooms. While cyanobacteria are very sensitive to H2O2, little Citation: Piel, T.; Sandrini, G.; is known about the impacts of these H2O2 treatments on other members of the microbial com- Muyzer, G.; Brussaard, C.P.D.; Slot, munity. In this study, we investigated changes in microbial community composition during two P.C.; van Herk, M.J.; Huisman, J.; −1 lake treatments with low H2O2 concentrations (target: 2.5 mg L ) and in two series of controlled Visser, P.M. -
Differential Depth Distribution of Microbial Function and Putative Symbionts Through Sediment-Hosted Aquifers in the Deep Terrestrial Subsurface
ARTICLES https://doi.org/10.1038/s41564-017-0098-y Differential depth distribution of microbial function and putative symbionts through sediment-hosted aquifers in the deep terrestrial subsurface Alexander J. Probst1,5,7, Bethany Ladd2,7, Jessica K. Jarett3, David E. Geller-McGrath1, Christian M. K. Sieber1,3, Joanne B. Emerson1,6, Karthik Anantharaman1, Brian C. Thomas1, Rex R. Malmstrom3, Michaela Stieglmeier4, Andreas Klingl4, Tanja Woyke 3, M. Cathryn Ryan 2* and Jillian F. Banfield 1* An enormous diversity of previously unknown bacteria and archaea has been discovered recently, yet their functional capacities and distributions in the terrestrial subsurface remain uncertain. Here, we continually sampled a CO2-driven geyser (Colorado Plateau, Utah, USA) over its 5-day eruption cycle to test the hypothesis that stratified, sandstone-hosted aquifers sampled over three phases of the eruption cycle have microbial communities that differ both in membership and function. Genome- resolved metagenomics, single-cell genomics and geochemical analyses confirmed this hypothesis and linked microorganisms to groundwater compositions from different depths. Autotrophic Candidatus “Altiarchaeum sp.” and phylogenetically deep- branching nanoarchaea dominate the deepest groundwater. A nanoarchaeon with limited metabolic capacity is inferred to be a potential symbiont of the Ca. “Altiarchaeum”. Candidate Phyla Radiation bacteria are also present in the deepest groundwater and they are relatively abundant in water from intermediate depths. During the recovery phase of the geyser, microaerophilic Fe- and S-oxidizers have high in situ genome replication rates. Autotrophic Sulfurimonas sustained by aerobic sulfide oxidation and with the capacity for N2 fixation dominate the shallow aquifer. Overall, 104 different phylum-level lineages are present in water from these subsurface environments, with uncultivated archaea and bacteria partitioned to the deeper subsurface. -
Dissertation Implementing Organic Amendments To
DISSERTATION IMPLEMENTING ORGANIC AMENDMENTS TO ENHANCE MAIZE YIELD, SOIL MOISTURE, AND MICROBIAL NUTRIENT CYCLING IN TEMPERATE AGRICULTURE Submitted by Erika J. Foster Graduate Degree Program in Ecology In partial fulfillment of the requirements For the Degree of Doctor of Philosophy Colorado State University Fort Collins, Colorado Summer 2018 Doctoral Committee: Advisor: M. Francesca Cotrufo Louise Comas Charles Rhoades Matthew D. Wallenstein Copyright by Erika J. Foster 2018 All Rights Reserved i ABSTRACT IMPLEMENTING ORGANIC AMENDMENTS TO ENHANCE MAIZE YIELD, SOIL MOISTURE, AND MICROBIAL NUTRIENT CYCLING IN TEMPERATE AGRICULTURE To sustain agricultural production into the future, management should enhance natural biogeochemical cycling within the soil. Strategies to increase yield while reducing chemical fertilizer inputs and irrigation require robust research and development before widespread implementation. Current innovations in crop production use amendments such as manure and biochar charcoal to increase soil organic matter and improve soil structure, water, and nutrient content. Organic amendments also provide substrate and habitat for soil microorganisms that can play a key role cycling nutrients, improving nutrient availability for crops. Additional plant growth promoting bacteria can be incorporated into the soil as inocula to enhance soil nutrient cycling through mechanisms like phosphorus solubilization. Since microbial inoculation is highly effective under drought conditions, this technique pairs well in agricultural systems using limited irrigation to save water, particularly in semi-arid regions where climate change and population growth exacerbate water scarcity. The research in this dissertation examines synergistic techniques to reduce irrigation inputs, while building soil organic matter, and promoting natural microbial function to increase crop available nutrients. The research was conducted on conventional irrigated maize systems at the Agricultural Research Development and Education Center north of Fort Collins, CO. -
Ultradeep Microbial Communities at 4.4 Km Within Crystalline Bedrock: Implications for Habitability in a Planetary Context
life Article Ultradeep Microbial Communities at 4.4 km within Crystalline Bedrock: Implications for Habitability in a Planetary Context Lotta Purkamo 1,2,* , Riikka Kietäväinen 2,3, Maija Nuppunen-Puputti 4, Malin Bomberg 4 and Claire Cousins 1 1 School of Earth and Environmental Sciences, University of St Andrews, St Andrews KY16 9AL, UK; [email protected] 2 Geological Survey of Finland, 02151 Espoo, Finland; riikka.kietavainen@gtk.fi 3 Department of Geosciences and Geography, University of Helsinki, 00014 Helsinki, Finland 4 VTT Technical Research Centre of Finland, 02044 VTT, Finland; maija.nuppunen-puputti@vtt.fi (M.N.-P.); malin.bomberg@vtt.fi (M.B.) * Correspondence: lotta.purkamo@gtk.fi; Tel.: +358-44-322-9432 Received: 1 November 2019; Accepted: 1 January 2020; Published: 4 January 2020 Abstract: The deep bedrock surroundings are an analog for extraterrestrial habitats for life. In this study, we investigated microbial life within anoxic ultradeep boreholes in Precambrian bedrock, including the adaptation to environmental conditions and lifestyle of these organisms. Samples were collected from Pyhäsalmi mine environment in central Finland and from geothermal drilling wells in Otaniemi, Espoo, in southern Finland. Microbial communities inhabiting the up to 4.4 km deep bedrock were characterized with phylogenetic marker gene (16S rRNA genes and fungal ITS region) amplicon and DNA and cDNA metagenomic sequencing. Functional marker genes (dsrB, mcrA, narG) were quantified with qPCR. Results showed that although crystalline bedrock provides very limited substrates for life, the microbial communities are diverse. Gammaproteobacterial phylotypes were most dominant in both studied sites. Alkanindiges -affiliating OTU was dominating in Pyhäsalmi fluids, while different depths of Otaniemi samples were dominated by Pseudomonas. -
Systema Naturae 2000 (Phylum, 6 Nov 2017)
The Taxonomicon Systema Naturae 2000 Classification of Domain Bacteria (prokaryotes) down to Phylum Compiled by Drs. S.J. Brands Universal Taxonomic Services 6 Nov 2017 Systema Naturae 2000 - Domain Bacteria - Domain Bacteria Woese et al. 1990 1 Genus †Eoleptonema Schopf 1983, incertae sedis 2 Genus †Primaevifilum Schopf 1983, incertae sedis 3 Genus †Archaeotrichion Schopf 1968, incertae sedis 4 Genus †Siphonophycus Schopf 1968, incertae sedis 5 Genus Bactoderma Tepper and Korshunova 1973 (Approved Lists 1980), incertae sedis 6 Genus Stibiobacter Lyalikova 1974 (Approved Lists 1980), incertae sedis 7.1.1.1.1.1 Superphylum "Proteobacteria" Craig et al. 2010 1.1 Phylum "Alphaproteobacteria" 1.2.1 Phylum "Acidithiobacillia" 1.2.2.1 Phylum "Gammaproteobacteria" 1.2.2.2.1 Candidate phylum Muproteobacteria (RIF23) Anantharaman et al. 2016 1.2.2.2.2 Phylum "Betaproteobacteria" 2 Phylum "Zetaproteobacteria" 7.1.1.1.1.2 Phylum "Deltaproteobacteria_1" 7.1.1.1.2.1.1.1 Phylum "Deltaproteobacteria" [polyphyletic] 7.1.1.1.2.1.1.2.1 Phylum "Deltaproteobacteria_2" 7.1.1.1.2.1.1.2.2 Phylum "Deltaproteobacteria_3" 7.1.1.1.2.1.2 Candidate phylum Dadabacteria (CSP1-2) Hug et al. 2015 7.1.1.1.2.2.1 Candidate phylum "MBNT15" 7.1.1.1.2.2.2 Candidate phylum "Uncultured Bacterial Phylum 10 (UBP10)" Parks et al. 2017 7.1.1.2.1 Phylum "Nitrospirae_1" 7.1.1.2.2 Phylum Chrysiogenetes Garrity and Holt 2001 7.1.2.1.1 Phylum "Nitrospirae" Garrity and Holt 2001 [polyphyletic] 7.1.2.1.2.1.1 Candidate phylum Rokubacteria (CSP1-6) Hug et al. -
Insights Into the Dynamics Between Viruses and Their Hosts in a Hot Spring Microbial Mat
The ISME Journal (2020) 14:2527–2541 https://doi.org/10.1038/s41396-020-0705-4 ARTICLE Insights into the dynamics between viruses and their hosts in a hot spring microbial mat 1,2,11 1,2 1,2 1,2 1,2 Jessica K. Jarett ● Mária Džunková ● Frederik Schulz ● Simon Roux ● David Paez-Espino ● 1,2 1,2 1,2 3 4 Emiley Eloe-Fadrosh ● Sean P. Jungbluth ● Natalia Ivanova ● John R. Spear ● Stephanie A. Carr ● 5 6 7 8,9 1,2 Christopher B. Trivedi ● Frank A. Corsetti ● Hope A. Johnson ● Eric Becraft ● Nikos Kyrpides ● 9 1,2,10 Ramunas Stepanauskas ● Tanja Woyke Received: 13 January 2020 / Revised: 3 June 2020 / Accepted: 11 June 2020 / Published online: 13 July 2020 © The Author(s) 2020. This article is published with open access Abstract Our current knowledge of host–virus interactions in biofilms is limited to computational predictions based on laboratory experiments with a small number of cultured bacteria. However, natural biofilms are diverse and chiefly composed of uncultured bacteria and archaea with no viral infection patterns and lifestyle predictions described to date. Herein, we predict the first DNA sequence-based host–virus interactions in a natural biofilm. Using single-cell genomics and metagenomics – 1234567890();,: 1234567890();,: applied to a hot spring mat of the Cone Pool in Mono County, California, we provide insights into virus host range, lifestyle and distribution across different mat layers. Thirty-four out of 130 single cells contained at least one viral contig (26%), which, together with the metagenome-assembled genomes, resulted in detection of 59 viruses linked to 34 host species.