Short-Term Effect of Simulated Salt Marsh Restoration by Sand- Amendment on Sediment Bacterial Communities
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Phylogenetic Diversity of NTT Nucleotide Transport Proteins in Free-Living and Parasitic Bacteria and Eukaryotes
Major, P., Embley, T. M., & Williams, T. (2017). Phylogenetic Diversity of NTT Nucleotide Transport Proteins in Free-Living and Parasitic Bacteria and Eukaryotes. Genome Biology and Evolution, 9(2), 480- 487. [evx015]. https://doi.org/10.1093/gbe/evx015 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1093/gbe/evx015 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Oxford University Press at https://academic.oup.com/gbe/article/2970297/Phylogenetic. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ GBE Phylogenetic Diversity of NTT Nucleotide Transport Proteins in Free-Living and Parasitic Bacteria and Eukaryotes Peter Major1,T.MartinEmbley1, and Tom A. Williams2,* 1Institute for Cell and Molecular Biosciences, University of Newcastle, Newcastle upon Tyne, United Kingdom 2School of Earth Sciences, University of Bristol, United Kingdom *Corresponding author: E-mail: [email protected]. Accepted: January 30, 2017 Abstract Plasma membrane-located nucleotide transport proteins (NTTs) underpin the lifestyle of important obligate intracellular bacterial and eukaryotic pathogens by importing energy and nucleotides from infected host cells that the pathogens can no longer make for themselves. As such their presence is often seen as a hallmark of an intracellular lifestyle associated with reductive genome evolution and loss of primary biosynthetic pathways. -
Table S4. Phylogenetic Distribution of Bacterial and Archaea Genomes in Groups A, B, C, D, and X
Table S4. Phylogenetic distribution of bacterial and archaea genomes in groups A, B, C, D, and X. Group A a: Total number of genomes in the taxon b: Number of group A genomes in the taxon c: Percentage of group A genomes in the taxon a b c cellular organisms 5007 2974 59.4 |__ Bacteria 4769 2935 61.5 | |__ Proteobacteria 1854 1570 84.7 | | |__ Gammaproteobacteria 711 631 88.7 | | | |__ Enterobacterales 112 97 86.6 | | | | |__ Enterobacteriaceae 41 32 78.0 | | | | | |__ unclassified Enterobacteriaceae 13 7 53.8 | | | | |__ Erwiniaceae 30 28 93.3 | | | | | |__ Erwinia 10 10 100.0 | | | | | |__ Buchnera 8 8 100.0 | | | | | | |__ Buchnera aphidicola 8 8 100.0 | | | | | |__ Pantoea 8 8 100.0 | | | | |__ Yersiniaceae 14 14 100.0 | | | | | |__ Serratia 8 8 100.0 | | | | |__ Morganellaceae 13 10 76.9 | | | | |__ Pectobacteriaceae 8 8 100.0 | | | |__ Alteromonadales 94 94 100.0 | | | | |__ Alteromonadaceae 34 34 100.0 | | | | | |__ Marinobacter 12 12 100.0 | | | | |__ Shewanellaceae 17 17 100.0 | | | | | |__ Shewanella 17 17 100.0 | | | | |__ Pseudoalteromonadaceae 16 16 100.0 | | | | | |__ Pseudoalteromonas 15 15 100.0 | | | | |__ Idiomarinaceae 9 9 100.0 | | | | | |__ Idiomarina 9 9 100.0 | | | | |__ Colwelliaceae 6 6 100.0 | | | |__ Pseudomonadales 81 81 100.0 | | | | |__ Moraxellaceae 41 41 100.0 | | | | | |__ Acinetobacter 25 25 100.0 | | | | | |__ Psychrobacter 8 8 100.0 | | | | | |__ Moraxella 6 6 100.0 | | | | |__ Pseudomonadaceae 40 40 100.0 | | | | | |__ Pseudomonas 38 38 100.0 | | | |__ Oceanospirillales 73 72 98.6 | | | | |__ Oceanospirillaceae -
Yu-Chen Ling and John W. Moreau
Microbial Distribution and Activity in a Coastal Acid Sulfate Soil System Introduction: Bioremediation in Yu-Chen Ling and John W. Moreau coastal acid sulfate soil systems Method A Coastal acid sulfate soil (CASS) systems were School of Earth Sciences, University of Melbourne, Melbourne, VIC 3010, Australia formed when people drained the coastal area Microbial distribution controlled by environmental parameters Microbial activity showed two patterns exposing the soil to the air. Drainage makes iron Microbial structures can be grouped into three zones based on the highest similarity between samples (Fig. 4). Abundant populations, such as Deltaproteobacteria, kept constant activity across tidal cycling, whereas rare sulfides oxidize and release acidity to the These three zones were consistent with their geological background (Fig. 5). Zone 1: Organic horizon, had the populations changed activity response to environmental variations. Activity = cDNA/DNA environment, low pH pore water further dissolved lowest pH value. Zone 2: surface tidal zone, was influenced the most by tidal activity. Zone 3: Sulfuric zone, Abundant populations: the heavy metals. The acidity and toxic metals then Method A Deltaproteobacteria Deltaproteobacteria this area got neutralized the most. contaminate coastal and nearby ecosystems and Method B 1.5 cause environmental problems, such as fish kills, 1.5 decreased rice yields, release of greenhouse gases, Chloroflexi and construction damage. In Australia, there is Gammaproteobacteria Gammaproteobacteria about a $10 billion “legacy” from acid sulfate soils, Chloroflexi even though Australia is only occupied by around 1.0 1.0 Cyanobacteria,@ Acidobacteria Acidobacteria Alphaproteobacteria 18% of the global acid sulfate soils. Chloroplast Zetaproteobacteria Rare populations: Alphaproteobacteria Method A log(RNA(%)+1) Zetaproteobacteria log(RNA(%)+1) Method C Method B 0.5 0.5 Cyanobacteria,@ Bacteroidetes Chloroplast Firmicutes Firmicutes Bacteroidetes Planctomycetes Planctomycetes Ac8nobacteria Fig. -
Effects of Different Straw Biochar Combined with Microbial Inoculants on Soil Environment of Ginseng
Effects of Different Straw Biochar Combined With Microbial Inoculants on Soil Environment of Ginseng Yuqi Qi Jilin Agricultural University Haolang Liu Jilin Agricultural University Jihong Wang ( [email protected] ) Jilin Agricultural University Yingping Wang Jilin Agricultural University Research Article Keywords: Microbial agent, Ginseng, Biochar, Soil remediation, Microbiota Posted Date: February 13th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-189319/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published at Scientic Reports on July 19th, 2021. See the published version at https://doi.org/10.1038/s41598-021-94209-1. Page 1/23 Abstract Ginseng is an important cash crop. The long-term continuous cropping of ginseng causes the imbalance of soil environment and the exacerbation of soil-borne diseases, which affects the healthy development of ginseng industry. In this study, ginseng continuous cropping soil was treated with microbial inocula using broad-spectrum biocontrol microbial strain Frankia F1. Wheat straw, rice straw and corn straw were the best carrier materials for microbial inoculum. After treatment with microbial inoculum prepared with corn stalk biochar, the soil pH value, organic matter, total nitrogen, available nitrogen, available phosphorus, and available potassium were increased by 11.18%, 55.43%, 33.07%, 26.70%, 16.40%, and 9.10%, the activities of soil urease, catalase and sucrase increased by 52.73%, 16.80% and 43.80%, respectively. A Metagenomic showed that after the application of microbial inoculum prepared fromwith corn stalk biochar, soil microbial OTUs, Chao1 index, Shannon index, and Simpson index increased by 19.86%, 16.05%, 28.83%, and 3.16%, respectively. -
Microbiology of Seamounts Is Still in Its Infancy
or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval portionthe ofwith any articlepermitted only photocopy by is of machine, reposting, this means or collective or other redistirbution This article has This been published in MOUNTAINS IN THE SEA Oceanography MICROBIOLOGY journal of The 23, Number 1, a quarterly , Volume OF SEAMOUNTS Common Patterns Observed in Community Structure O ceanography ceanography S BY DAVID EmERSON AND CRAIG L. MOYER ociety. © 2010 by The 2010 by O ceanography ceanography O ceanography ceanography ABSTRACT. Much interest has been generated by the discoveries of biodiversity InTRODUCTION S ociety. ociety. associated with seamounts. The volcanically active portion of these undersea Microbial life is remarkable for its resil- A mountains hosts a remarkably diverse range of unusual microbial habitats, from ience to extremes of temperature, pH, article for use and research. this copy in teaching to granted ll rights reserved. is Permission S ociety. ociety. black smokers rich in sulfur to cooler, diffuse, iron-rich hydrothermal vents. As and pressure, as well its ability to persist S such, seamounts potentially represent hotspots of microbial diversity, yet our and thrive using an amazing number or Th e [email protected] to: correspondence all end understanding of the microbiology of seamounts is still in its infancy. Here, we of organic or inorganic food sources. discuss recent work on the detection of seamount microbial communities and the Nowhere are these traits more evident observation that specific community groups may be indicative of specific geochemical than in the deep ocean. -
The Ecophysiology of Iron-Oxidizing Zetaproteobacteria: Microbe- Mineral Interactions, Transcriptomic Responses, and Biomineralization
The Ecophysiology of Iron-Oxidizing Zetaproteobacteria: Microbe- Mineral Interactions, Transcriptomic Responses, and Biomineralization The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Cohen, Jacob W. 2020. The Ecophysiology of Iron-Oxidizing Zetaproteobacteria: Microbe-Mineral Interactions, Transcriptomic Responses, and Biomineralization. Doctoral dissertation, Harvard University, Graduate School of Arts & Sciences. Citable link https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37365123 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The ecophysiology of iron-oxidizing Zetaproteobacteria: microbe-mineral interactions, transcriptomic responses, and biomineralization A dissertation presented by Jacob William Cohen to The Department of Organismic and Evolutionary Biology in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Biology Harvard University Cambridge, Massachusetts December 2019 ©2019 Jacob William Cohen All rights reserved. Dissertation advisor: Peter R. Girguis Jacob William Cohen The ecophysiology of iron-oxidizing Zetaproteobacteria: microbe-mineral interactions, transcriptomic responses, and biomineralization Abstract Neutrophilic microaerobic iron-oxidizing bacteria (FeOB) obtain energy by using reduced Fe(II) as an electron donor with oxygen as their electron acceptor. Much is still unknown about FeOB, however, despite their importance to the cycling of iron, a nutrient that is essential to life on Earth and limiting in many marine environments. In this dissertation I studied pure cultures of two marine hydrothermal vent iron-oxidizing Zetaproteobacteria, Mariprofundus ferrooxydans PV-1 and Ghiorsea bivora TAG-1, to further our understanding of FeOB physiology and the implications this has for their ecology. -
Cluster 1 Cluster 3 Cluster 2
5 9 Luteibacter yeojuensis strain SU11 (Ga0078639_1004, 2640590121) 7 0 Luteibacter rhizovicinus DSM 16549 (Ga0078601_1039, 2631914223) 4 7 Luteibacter sp. UNCMF366Tsu5.1 (FG06DRAFT_scaffold00001.1, 2595447474) 5 5 Dyella japonica UNC79MFTsu3.2 (N515DRAFT_scaffold00003.3, 2558296041) 4 8 100 Rhodanobacter sp. Root179 (Ga0124815_151, 2699823700) 9 4 Rhodanobacter sp. OR87 (RhoOR87DRAFT_scaffold_21.22, 2510416040) Dyella japonica DSM 16301 (Ga0078600_1041, 2640844523) Dyella sp. OK004 (Ga0066746_17, 2609553531) 9 9 9 3 Xanthomonas fuscans (007972314) 100 Xanthomonas axonopodis (078563083) 4 9 Xanthomonas oryzae pv. oryzae KACC10331 (NC_006834, 637633170) 100 100 Xanthomonas albilineans USA048 (Ga0078502_15, 2651125062) 5 6 Xanthomonas translucens XT123 (Ga0113452_1085, 2663222128) 6 5 Lysobacter enzymogenes ATCC 29487 (Ga0111606_103, 2678972498) 100 Rhizobacter sp. Root1221 (056656680) Rhizobacter sp. Root1221 (Ga0102088_103, 2644243628) 100 Aquabacterium sp. NJ1 (052162038) Aquabacterium sp. NJ1 (Ga0077486_101, 2634019136) Uliginosibacterium gangwonense DSM 18521 (B145DRAFT_scaffold_15.16, 2515877853) 9 6 9 7 Derxia lacustris (085315679) 8 7 Derxia gummosa DSM 723 (H566DRAFT_scaffold00003.3, 2529306053) 7 2 Ideonella sp. B508-1 (I73DRAFT_BADL01000387_1.387, 2553574224) Zoogloea sp. LCSB751 (079432982) PHB-accumulating bacterium (PHBDraf_Contig14, 2502333272) Thiobacillus sp. 65-1059 (OJW46643.1) 8 4 Dechloromonas aromatica RCB (NC_007298, 637680051) 8 4 7 7 Dechloromonas sp. JJ (JJ_JJcontig4, 2506671179) Dechloromonas RCB 100 Azoarcus -
(II) of Basaltic Glass As an Energy Source for Zetaproteobacteria in an Abyssal Plain Environment, Off the Mid A
Structural Iron (II) of Basaltic Glass as an Energy Source for Zetaproteobacteria in an Abyssal Plain Environment, Off the Mid Atlantic Ridge Pauline Henri, Céline Rommevaux-Jestin, Françoise Lesongeur, Adam Mumford, David Emerson, Anne Godfroy, Bénédicte Ménez To cite this version: Pauline Henri, Céline Rommevaux-Jestin, Françoise Lesongeur, Adam Mumford, David Emerson, et al.. Structural Iron (II) of Basaltic Glass as an Energy Source for Zetaproteobacteria in an Abyssal Plain Environment, Off the Mid Atlantic Ridge. Frontiers in Microbiology, Frontiers Media, 2015,6, pp.1518. 10.3389/fmicb.2015.01518. insu-01472806 HAL Id: insu-01472806 https://hal-insu.archives-ouvertes.fr/insu-01472806 Submitted on 21 Feb 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ORIGINAL RESEARCH published: 21 January 2016 doi: 10.3389/fmicb.2015.01518 Structural Iron (II) of Basaltic Glass as an Energy Source for Zetaproteobacteria in an Abyssal Plain Environment, Off the Mid Atlantic Ridge Pauline A. Henri1*, Céline Rommevaux-Jestin1, Françoise Lesongeur2,AdamMumford3, -
Comparison of Prokaryotic Communities Associated with Different TOC Concentrations in Dianchi Lake
water Article Comparison of Prokaryotic Communities Associated with Different TOC Concentrations in Dianchi Lake Cheng-Peng Li 1,2, Ya-Ping Li 1,2, Qing-Qing Huo 1,2, Wei Xiao 1 , Chang-Qun Duan 3 , Yong-Xia Wang 1,* and Xiao-Long Cui 1,2,* 1 Yunnan Institute of Microbiology, School of Life Sciences, Yunnan University, Kunming 650091, China; [email protected] (C.-P.L.); [email protected] (Y.-P.L.); [email protected] (Q.-Q.H.); [email protected] (W.X.) 2 State Key Laboratory for Conservation and Utilization of Bio-Resources in Yunnan, Yunnan University, Kunming 650091, China 3 School of Ecology and Environmental Science, Yunnan University, Kunming 650091, China; [email protected] * Correspondence: [email protected] (Y.-X.W.); [email protected] (X.-L.C.); Tel.: +86-0871-65034621 (X.-L.C.) Received: 12 August 2020; Accepted: 10 September 2020; Published: 13 September 2020 Abstract: The effect of total organic carbon (TOC) on the prokaryotic community structure in situ has been rarely known. This study aimed to determine the effect of TOC level on the composition and networks of archaeal and bacterial communities in the sediments of Dianchi Lake, one of the most eutrophic lakes in China. Microbial assemblages showed significantly associations with TOC. Moreover, relatively high and low TOC formed taxonomic differences in prokaryotic assemblages. According to the results, the most abundant bacteria across all samples were identified as members of the phyla Proteobacteria, Nitrospirae, Chloroflexi, Firmicutes and Ignavibacteriae. The dominant groups of archaea consisted of Euryarchaeota, Woesearchaeota DHVEG-6, Bathyarchaeota and WSA2. -
Soil Ph Is the Primary Factor Driving the Distribution and Function of Microorganisms in Farmland Soils in Northeastern China
Annals of Microbiology (2019) 69:1461–1473 https://doi.org/10.1007/s13213-019-01529-9 ORIGINAL ARTICLE Soil pH is the primary factor driving the distribution and function of microorganisms in farmland soils in northeastern China Cheng-yu Wang1 & Xue Zhou1 & Dan Guo1 & Jiang-hua Zhao1 & Li Yan1 & Guo-zhong Feng1 & Qiang Gao1 & Han Yu2 & Lan-po Zhao1 Received: 26 May 2019 /Accepted: 3 November 2019 /Published online: 19 December 2019 # The Author(s) 2019 Abstract Purpose To understand which environmental factors influence the distribution and ecological functions of bacteria in agricultural soil. Method A broad range of farmland soils was sampled from 206 locations in Jilin province, China. We used 16S rRNA gene- based Illumina HiSeq sequencing to estimated soil bacterial community structure and functions. Result The dominant taxa in terms of abundance were found to be, Actinobacteria, Acidobacteria, Gemmatimonadetes, Chloroflexi, and Proteobacteria. Bacterial communities were dominantly affected by soil pH, whereas soil organic carbon did not have a significant influence on bacterial communities. Soil pH was significantly positively correlated with bacterial opera- tional taxonomic unit abundance and soil bacterial α-diversity (P<0.05) spatially rather than with soil nutrients. Bacterial functions were estimated using FAPROTAX, and the relative abundance of anaerobic and aerobic chemoheterotrophs, and nitrifying bacteria was 27.66%, 26.14%, and 6.87%, respectively, of the total bacterial community. Generally, the results indicate that soil pH is more important than nutrients in shaping bacterial communities in agricultural soils, including their ecological functions and biogeographic distribution. Keywords Agricultural soil . Soil bacterial community . Bacterial diversity . Bacterial biogeographic distribution . -
Size-Fraction Partitioning of Community Gene Transcription and Nitrogen Metabolism in a Marine Oxygen Minimum Zone
The ISME Journal (2015), 1–15 © 2015 International Society for Microbial Ecology All rights reserved 1751-7362/15 www.nature.com/ismej ORIGINAL ARTICLE Size-fraction partitioning of community gene transcription and nitrogen metabolism in a marine oxygen minimum zone Sangita Ganesh1,3, Laura A Bristow2,3, Morten Larsen2, Neha Sarode1, Bo Thamdrup2 and Frank J Stewart1 1School of Biology, Georgia Institute of Technology, Atlanta, GA, USA and 2Department of Biology and Nordic Center for Earth Evolution (NordCEE), University of Southern Denmark, Odense, Denmark The genetic composition of marine microbial communities varies at the microscale between particle- associated (PA; 41.6 μm) and free-living (FL; 0.2–1.6 μm) niches. It remains unclear, however, how metabolic activities differ between PA and FL fractions. We combined rate measurements with metatranscriptomics to quantify PA and FL microbial activity in the oxygen minimum zone (OMZ) of the Eastern Tropical North Pacific, focusing on dissimilatory processes of the nitrogen (N) cycle. Bacterial gene counts were 8- to 15-fold higher in the FL compared with the PA fraction. However, rates of all measured N cycle processes, excluding ammonia oxidation, declined significantly following particle (41.6 μm) removal. Without particles, rates of nitrate reduction to nitrite − 1 − 1 (1.5–9.4 nM Nd ) fell to zero and N2 production by denitrification (0.5–1.7 nM Nd ) and anammox − (0.3–1.9 nM Nd 1) declined by 53–85%. The proportional representation of major microbial taxa and N cycle gene transcripts in metatranscriptomes followed fraction-specific trends. Transcripts encoding nitrate reductase were uniform among PA and FL fractions, whereas anammox-associated transcripts were proportionately enriched up to 15-fold in the FL fraction. -
Chemosynthetic and Photosynthetic Bacteria Contribute Differentially to Primary Production Across a Steep Desert Aridity Gradient
The ISME Journal https://doi.org/10.1038/s41396-021-01001-0 ARTICLE Chemosynthetic and photosynthetic bacteria contribute differentially to primary production across a steep desert aridity gradient 1,2 3,4 5 6 2 Sean K. Bay ● David W. Waite ● Xiyang Dong ● Osnat Gillor ● Steven L. Chown ● 3 1,2 Philip Hugenholtz ● Chris Greening Received: 23 November 2020 / Revised: 16 April 2021 / Accepted: 28 April 2021 © The Author(s) 2021. This article is published with open access Abstract Desert soils harbour diverse communities of aerobic bacteria despite lacking substantial organic carbon inputs from vegetation. A major question is therefore how these communities maintain their biodiversity and biomass in these resource-limiting ecosystems. Here, we investigated desert topsoils and biological soil crusts collected along an aridity gradient traversing four climatic regions (sub-humid, semi-arid, arid, and hyper-arid). Metagenomic analysis indicated these communities vary in their capacity to use sunlight, organic compounds, and inorganic compounds as energy sources. Thermoleophilia, Actinobacteria, and Acidimicrobiia 1234567890();,: 1234567890();,: were the most abundant and prevalent bacterial classes across the aridity gradient in both topsoils and biocrusts. Contrary to the classical view that these taxa are obligate organoheterotrophs, genome-resolved analysis suggested they are metabolically flexible, withthecapacitytoalsouseatmosphericH2 to support aerobic respiration and often carbon fixation. In contrast, Cyanobacteria were patchily distributed and only abundant in certain biocrusts. Activity measurements profiled how aerobic H2 oxidation, chemosynthetic CO2 fixation, and photosynthesis varied with aridity. Cell-specific rates of atmospheric H2 consumption increased 143-fold along the aridity gradient, correlating with increased abundance of high-affinity hydrogenases. Photosynthetic and chemosynthetic primary production co-occurred throughout the gradient, with photosynthesis dominant in biocrusts and chemosynthesis dominant in arid and hyper-arid soils.