How Do Quorum-Sensing Signals Mediate Algae–Bacteria Interactions?
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Inter Scientific Inquiry • Nature • Technology • Evolution • Research
Inter Scientific InquIry • nature • technology • evolutIon • research vol. 5 - august 2018 INTER SCIENTIFIC CONTENIDO CONTENTS MENSAJE DEL RECTOR/ MESSAGE FROM THE CHANCELLOR………………………………………………………..1 MENSAJE DE LA DECANA DE ASUNTOS ACADÉMICOS/ MESSAGE FROM THE DEAN OF ACADEMIC AFFAIRS………………………………………………………………………………………………1 DESDE EL ESCRITORIO DE LA EDITORA/ FROM THE EDITOR’S DESK…………………………………………....2 INVESTIGACIÓN/ RESEARCH ARTICLES………………………………………………………………………….....3-19 Host plant preference of Danaus plexippus larvae in the subtropical dry forest in Guánica, Puerto Rico………………………………………………………………………………………………......…3 Preferencia de plantas hospederas por parte de las larvas de Danaus plexippus en el bosque seco de Guánica, Puerto Rico López, Laysa, Santiago, Jonathan, and Puente-Rolón, Alberto Predatory behavior and prey preference of Leucauge sp. in Mayaguez, Puerto Rico……….…...7 Comportamiento de depredación y preferencia de presa de arañas del género Leucauge en Mayaguez, Puerto Rico Geli-Cruz, Orlando, Ramos-Maldonado, Frank, and Puente-Rolón, Alberto Construction and screening of soil metagenomic libraries: identification of hydrolytic metabolic activity………………………………………………………………………..……..…………....13 Construcción y prueba de bibliotecas metagenómicas de suelo: identificación de actividad metabólica hidrolítica Jiménez-Serrano, Edgar, Justiniano-Santiago, Jeydien, Reyes, Yazmin, Rosa-Matos, Raquel, Vélez- Cardona, Wilmarie, Huertas-Meléndez, Stephanie and Pagán-Jiménez, María LA INVESTIGACIÓN EN EL CAMPUS/ RESEARCH ON CAMPUS ……………………………………………………20 -
Pulse Generation in the Quorum Machinery of Pseudomonas Aeruginosa
This is a repository copy of Pulse generation in the quorum machinery of Pseudomonas aeruginosa. White Rose Research Online URL for this paper: https://eprints.whiterose.ac.uk/116745/ Version: Published Version Article: Alfiniyah, Cicik Alfiniyah, Bees, Martin Alan and Wood, Andrew James orcid.org/0000- 0002-6119-852X (2017) Pulse generation in the quorum machinery of Pseudomonas aeruginosa. Bulletin of Mathematical Biology. pp. 1360-1389. ISSN 1522-9602 https://doi.org/10.1007/s11538-017-0288-z Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Bull Math Biol (2017) 79:1360–1389 DOI 10.1007/s11538-017-0288-z ORIGINAL ARTICLE Pulse Generation in the Quorum Machinery of Pseudomonas aeruginosa Cicik Alfiniyah1,2 · Martin A. Bees1 · A. Jamie Wood1,3 Received: 28 September 2016 / Accepted: 3 May 2017 / Published online: 19 May 2017 © The Author(s) 2017. This article is an open access publication Abstract Pseudomonas aeruginosa is a Gram-negative bacterium that is responsible for a wide range of infections in humans. -
Coral Feeding on Microalgae Assessed with Molecular Trophic Markers
Molecular Ecology (2013) doi: 10.1111/mec.12486 Coral feeding on microalgae assessed with molecular trophic markers MIGUEL C. LEAL,*† CHRISTINE FERRIER-PAGES,‡ RICARDO CALADO,* MEGAN E. THOMPSON,† MARC E. FRISCHER† and JENS C. NEJSTGAARD† *Departamento de Biologia & CESAM, Universidade de Aveiro, Campus Universitario de Santiago, 3810-193 Aveiro, Portugal, †Skidaway Institute of Oceanography, 10 Ocean Science Circle, 31411 Savannah, GA, USA, ‡Centre Scientifique de Monaco, Avenue St-Martin, 98000 Monaco, Monaco Abstract Herbivory in corals, especially for symbiotic species, remains controversial. To investi- gate the capacity of scleractinian and soft corals to capture microalgae, we conducted controlled laboratory experiments offering five algal species: the cryptophyte Rhodo- monas marina, the haptophytes Isochrysis galbana and Phaeocystis globosa, and the diatoms Conticribra weissflogii and Thalassiosira pseudonana. Coral species included the symbiotic soft corals Heteroxenia fuscescens and Sinularia flexibilis, the asymbiotic scleractinian coral Tubastrea coccinea, and the symbiotic scleractinian corals Stylophora pistillata, Pavona cactus and Oculina arbuscula. Herbivory was assessed by end-point PCR amplification of algae-specific 18S rRNA gene fragments purified from coral tissue genomic DNA extracts. The ability to capture microalgae varied with coral and algal species and could not be explained by prey size or taxonomy. Herbivory was not detected in S. flexibilis and S. pistillata. P. globosa was the only algal prey that was never captured by any coral. Although predation defence mechanisms have been shown for Phaeocystis spp. against many potential predators, this study is the first to suggest this for corals. This study provides new insights into herbivory in symbiotic corals and suggests that corals may be selective herbivorous feeders. -
Taurine Is a Major Carbon and Energy Source for Marine Prokaryotes in the North Atlantic Ocean Off the Iberian Peninsula
Microbial Ecology https://doi.org/10.1007/s00248-019-01320-y MICROBIOLOGY OF AQUATIC SYSTEMS Taurine Is a Major Carbon and Energy Source for Marine Prokaryotes in the North Atlantic Ocean off the Iberian Peninsula Elisabeth L. Clifford1 & Marta M. Varela2 & Daniele De Corte3 & Antonio Bode2 & Victor Ortiz1 & Gerhard J. Herndl1,4 & Eva Sintes1,5 Received: 28 June 2018 /Accepted: 3 January 2019 # The Author(s) 2019 Abstract Taurine, an amino acid-like compound, acts as an osmostress protectant in many marine metazoans and algae and is released via various processes into the oceanic dissolved organic matter pool. Taurine transporters are widespread among members of the marine prokaryotic community, tentatively indicating that taurine might be an important substrate for prokaryotes in the ocean. In this study, we determined prokaryotic taurine assimilation and respiration throughout the water column along two transects in the North Atlantic off the Iberian Peninsula. Taurine assimilation efficiency decreased from the epipelagic waters from 55 ± 14% to 27 ± 20% in the bathypelagic layers (means of both transects). Members of the ubiquitous alphaproteobacterial SAR11 clade accounted for a large fraction of cells taking up taurine, especially in surface waters. Archaea (Thaumarchaeota + Euryarchaeota) were also able to take up taurine in the upper water column, but to a lower extent than Bacteria. The contribution of taurine assimilation to the heterotrophic prokaryotic carbon biomass production ranged from 21% in the epipelagic layer to 16% in the bathypelagic layer. Hence, we conclude that dissolved free taurine is a significant carbon and energy source for prokaryotes throughout the oceanic water column being utilized with similar efficiencies as dissolved free amino acids. -
Specificity Re-Evaluation of Oligonucleotide Probes for the Detection of Marine Picoplankton by Tyramide Signal Amplification-Fl
fmicb-08-00854 May 24, 2017 Time: 20:18 # 1 ORIGINAL RESEARCH published: 29 May 2017 doi: 10.3389/fmicb.2017.00854 Specificity Re-evaluation of Oligonucleotide Probes for the Detection of Marine Picoplankton by Tyramide Signal Amplification-Fluorescent In Situ Hybridization Virginie Riou, Marine Périot and Isabelle C. Biegala* Centre National de la Recherche Scientifique, Mediterranean Institute of Oceanography – Institut de Recherche pour le Développement, Aix Marseille Université – Université de Toulon, Marseille, France Edited by: Sophie Rabouille, Oligonucleotide probes are increasingly being used to characterize natural microbial Centre National de la Recherche Scientifique (CNRS), France assemblages by Tyramide Signal Amplification-Fluorescent in situ Hybridization (TSA- Reviewed by: FISH, or CAtalysed Reporter Deposition CARD-FISH). In view of the fast-growing rRNA Fernanda De Avila Abreu, databases, we re-evaluated the in silico specificity of eleven bacterial and eukaryotic Federal University of Rio de Janeiro, Brazil probes and competitor frequently used for the quantification of marine picoplankton. Tom Bibby, We performed tests on cell cultures to decrease the risk for non-specific hybridization, University of Southampton, before they are used on environmental samples. The probes were confronted to recent United Kingdom databases and hybridization conditions were tested against target strains matching *Correspondence: Isabelle C. Biegala perfectly with the probes, and against the closest non-target strains presenting one [email protected] -
Major Evolutionary Transitions in Individuality COLLOQUIUM
PAPER Major evolutionary transitions in individuality COLLOQUIUM Stuart A. Westa,b,1, Roberta M. Fishera, Andy Gardnerc, and E. Toby Kiersd aDepartment of Zoology, University of Oxford, Oxford OX1 3PS, United Kingdom; bMagdalen College, Oxford OX1 4AU, United Kingdom; cSchool of Biology, University of St. Andrews, Dyers Brae, St. Andrews KY16 9TH, United Kingdom; and dInstitute of Ecological Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit, 1081 HV, Amsterdam, The Netherlands Edited by John P. McCutcheon, University of Montana, Missoula, MT, and accepted by the Editorial Board March 13, 2015 (received for review December 7, 2014) The evolution of life on earth has been driven by a small number broken down into six questions. We explore what is already known of major evolutionary transitions. These transitions have been about the factors facilitating transitions, examining the extent to characterized by individuals that could previously replicate inde- which we can generalize across the different transitions. Ultimately, pendently, cooperating to form a new, more complex life form. we are interested in the underlying evolutionary and ecological For example, archaea and eubacteria formed eukaryotic cells, and factors that drive major transitions. cells formed multicellular organisms. However, not all cooperative Defining Major Transitions groups are en route to major transitions. How can we explain why major evolutionary transitions have or haven’t taken place on dif- A major evolutionary transition has been most broadly defined as a change in the way that heritable information is stored and ferent branches of the tree of life? We break down major transi- transmitted (2). We focus on the major transitions that lead to a tions into two steps: the formation of a cooperative group and the new form of individual (Table 1), where the same problems arise, transformation of that group into an integrated entity. -
PROTISTS Shore and the Waves Are Large, Often the Largest of a Storm Event, and with a Long Period
(seas), and these waves can mobilize boulders. During this phase of the storm the rapid changes in current direction caused by these large, short-period waves generate high accelerative forces, and it is these forces that ultimately can move even large boulders. Traditionally, most rocky-intertidal ecological stud- ies have been conducted on rocky platforms where the substrate is composed of stable basement rock. Projec- tiles tend to be uncommon in these types of habitats, and damage from projectiles is usually light. Perhaps for this reason the role of projectiles in intertidal ecology has received little attention. Boulder-fi eld intertidal zones are as common as, if not more common than, rock plat- forms. In boulder fi elds, projectiles are abundant, and the evidence of damage due to projectiles is obvious. Here projectiles may be one of the most important defi ning physical forces in the habitat. SEE ALSO THE FOLLOWING ARTICLES Geology, Coastal / Habitat Alteration / Hydrodynamic Forces / Wave Exposure FURTHER READING Carstens. T. 1968. Wave forces on boundaries and submerged bodies. Sarsia FIGURE 6 The intertidal zone on the north side of Cape Blanco, 34: 37–60. Oregon. The large, smooth boulders are made of serpentine, while Dayton, P. K. 1971. Competition, disturbance, and community organi- the surrounding rock from which the intertidal platform is formed zation: the provision and subsequent utilization of space in a rocky is sandstone. The smooth boulders are from a source outside the intertidal community. Ecological Monographs 45: 137–159. intertidal zone and were carried into the intertidal zone by waves. Levin, S. A., and R. -
Microalgae Strain Catalogue
Microalgae strain catalogue A strain selection guide for microalgae users: cultivation and chemical characteristics for high added-value products CONTENTS 1. INTRODUCTION .......................................................................................... 4 2. Strain catalogue ......................................................................................... 5 Anabaena cylindrica ........................................................................................... 6 Arthrospira platensis .......................................................................................... 8 Botryococcus braunii ........................................................................................ 10 Chlorella luteoviridis ......................................................................................... 12 Chlorella sorokiniana ........................................................................................ 14 Chlorella vulgaris .............................................................................................. 16 Dunaliella salina ............................................................................................... 18 Dunaliella tertiolecta ......................................................................................... 20 Haematococcus pluvialis .................................................................................. 22 Microcystis aeruginosa ..................................................................................... 24 Nannochloropsis occulata ............................................................................... -
21 Pathogens of Harmful Microalgae
21 Pathogens of Harmful Microalgae RS. Salomon and I. Imai 2L1 Introduction Pathogens are any organisms that cause disease to other living organisms. Parasitism is an interspecific interaction where one species (the parasite) spends the whole or part of its life on or inside cells and tissues of another living organism (the host), from where it derives most of its food. Parasites that cause disease to their hosts are, by definition, pathogens. Although infection of metazoans by other metazoans and protists are the more fre quently studied, there are interactions where both host and parasite are sin gle-celled organisms. Here we describe such interactions involving microal gae as hosts. The aim of this chapter is to review the current status of research on pathogens of harmful microalgae and present future perspec tives within the field. Pathogens with the ability to impair and kill micro algae include viruses, bacteria, fungi and a number of protists (see reviews by Elbrachter and Schnepf 1998; Brussaard 2004; Park et al. 2004; Mayali and Azam 2004; Ibelings et al. 2004). Valuable information exists from non-harm ful microalgal hosts, and these studies will be referred to throughout the text. Nevertheless, emphasis is given to cases where hosts are recognizable harmful microalgae. 21.2 Viruses Viruses and virus-like particles (VLPs) have been found in more than 50 species of eukaryotic microalgae, and several of them have been isolated in laboratory cultures (Brussaard 2004; Nagasaki et al. 2005). These viruses are diverse both in size and genome type, and some of them infect harmful algal bloom (HAB)-causing species (Table 21.1). -
Bacterial Community Composition of Size-Fractioned Aggregates Within the Phycosphere of Cyanobacterial Blooms in a Eutrophic Freshwater Lake
Bacterial Community Composition of Size-Fractioned Aggregates within the Phycosphere of Cyanobacterial Blooms in a Eutrophic Freshwater Lake Haiyuan Cai1, Helong Jiang1*, Lee R. Krumholz2, Zhen Yang1 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China, 2 Department of Botany and Microbiology, University of Oklahoma, Norman, Oklahoma, United States of America Abstract Bacterial community composition of different sized aggregates within the Microcystis cyanobacterial phycosphere were determined during summer and fall in Lake Taihu, a eutrophic lake in eastern China. Bloom samples taken in August and September represent healthy bloom biomass, whereas samples from October represent decomposing bloom biomass. To improve our understanding of the complex interior structure in the phycosphere, bloom samples were separated into large (.100 mm), medium (10–100 mm) and small (0.2–10 mm) size aggregates. Species richness and library coverage indicated that pyrosequencing recovered a large bacterial diversity. The community of each size aggregate was highly organized, indicating highly specific conditions within the Microcystis phycosphere. While the communities of medium and small-size aggregates clustered together in August and September samples, large- and medium-size aggregate communities in the October sample were grouped together and distinct from small-size aggregate community. Pronounced changes in the absolute and relative percentages of the dominant genus from the two most important phyla Proteobacteria and Bacteroidetes were observed among the various size aggregates. Bacterial species on large and small-size aggregates likely have the ability to degrade high and low molecular weight compounds, respectively. Thus, there exists a spatial differentiation of bacterial taxa within the phycosphere, possibly operating in sequence and synergy to catalyze the turnover of complex organic matters. -
Which Organisms Are Used for Anti-Biofouling Studies
Table S1. Semi-systematic review raw data answering: Which organisms are used for anti-biofouling studies? Antifoulant Method Organism(s) Model Bacteria Type of Biofilm Source (Y if mentioned) Detection Method composite membranes E. coli ATCC25922 Y LIVE/DEAD baclight [1] stain S. aureus ATCC255923 composite membranes E. coli ATCC25922 Y colony counting [2] S. aureus RSKK 1009 graphene oxide Saccharomycetes colony counting [3] methyl p-hydroxybenzoate L. monocytogenes [4] potassium sorbate P. putida Y. enterocolitica A. hydrophila composite membranes E. coli Y FESEM [5] (unspecified/unique sample type) S. aureus (unspecified/unique sample type) K. pneumonia ATCC13883 P. aeruginosa BAA-1744 composite membranes E. coli Y SEM [6] (unspecified/unique sample type) S. aureus (unspecified/unique sample type) graphene oxide E. coli ATCC25922 Y colony counting [7] S. aureus ATCC9144 P. aeruginosa ATCCPAO1 composite membranes E. coli Y measuring flux [8] (unspecified/unique sample type) graphene oxide E. coli Y colony counting [9] (unspecified/unique SEM sample type) LIVE/DEAD baclight S. aureus stain (unspecified/unique sample type) modified membrane P. aeruginosa P60 Y DAPI [10] Bacillus sp. G-84 LIVE/DEAD baclight stain bacteriophages E. coli (K12) Y measuring flux [11] ATCC11303-B4 quorum quenching P. aeruginosa KCTC LIVE/DEAD baclight [12] 2513 stain modified membrane E. coli colony counting [13] (unspecified/unique colony counting sample type) measuring flux S. aureus (unspecified/unique sample type) modified membrane E. coli BW26437 Y measuring flux [14] graphene oxide Klebsiella colony counting [15] (unspecified/unique sample type) P. aeruginosa (unspecified/unique sample type) graphene oxide P. aeruginosa measuring flux [16] (unspecified/unique sample type) composite membranes E. -
Archaeal Distribution and Abundance in Water Masses of the Arctic Ocean, Pacific Sector
Vol. 69: 101–112, 2013 AQUATIC MICROBIAL ECOLOGY Published online April 30 doi: 10.3354/ame01624 Aquat Microb Ecol FREEREE ACCESSCCESS Archaeal distribution and abundance in water masses of the Arctic Ocean, Pacific sector Chie Amano-Sato1, Shohei Akiyama1, Masao Uchida2, Koji Shimada3, Motoo Utsumi1,* 1University of Tsukuba, Tennodai, Tsukuba, Ibaraki 305-8572, Japan 2National Institute for Environmental Studies, Onogawa, Tsukuba, Ibaraki 305-8506, Japan 3Tokyo University of Marine Science and Technology, Konan, Minato-ku, Tokyo 108-8477, Japan ABSTRACT: Marine planktonic Archaea have been recently recognized as an ecologically impor- tant component of marine prokaryotic biomass in the world’s oceans. Their abundance and meta- bolism are closely connected with marine geochemical cycling. We evaluated the distribution of planktonic Archaea in the Pacific sector of the Arctic Ocean using fluorescence in situ hybridiza- tion (FISH) with catalyzed reporter deposition (CARD-FISH) and performed statistical analyses using data for archaeal abundance and geochemical variables. The relative abundance of Thaum - archaeota generally increased with depth, and euryarchaeal abundance was the lowest of all planktonic prokaryotes. Multiple regression analysis showed that the thaumarchaeal relative abundance was negatively correlated with ammonium and dissolved oxygen concentrations and chlorophyll fluorescence. Canonical correspondence analysis showed that archaeal distributions differed with oceanographic water masses; in particular, Thaumarchaeota were abundant from the halocline layer to deep water, where salinity was higher and most nutrients were depleted. However, at several stations on the East Siberian Sea side of the study area and along the North- wind Ridge, Thaumarchaeota and Bacteria were proportionally very abundant at the bottom in association with higher nutrient conditions.