esistance exists as a continuum between highly sensitive and resistant.Acquisition of resistance and subsequent proliferation of resistant strainswas demonstrated on model particles as well as in solution. Loss ofsusceptibility to phage infection was associated with a reduction in thestrains' ability to metabolize various carbon sources. Our work with thismodel system indicates that phage-host dynamics are extremely complex. Ifthe observed patterns are valid for indigenous marine phage-host systems,they imply that i) continuous ranges of infectivity and susceptibility toinfection exist in phage-host system, ii) in turn, that the concept of virushostsystem has limited use, and iii) that functional diversification ofbacterial hosts occurs at the clonal level. Thus far, the ecologicalconsequences of this intriguing complexity are poorly understood.EMV029Aggregate-colonizing microbial communities - acomparison of marine vs. freshwater systemsM. Bizic-Ionescu* 1,2 , B. Fuchs 1 , R. Amann 1 , H.-P. Grossart 21 Department forMolecular Ecology, Max Planck Institute for MarineMicrobiology, Bremen, Germany2 Department of Stratified Lakes, Leibniz Institute of Freshwater Ecologyand Inland Fisheries, Stechlin, GermanyWe observed the formation of particulate organic matter (POM) aggregatesafter a dinoflagellate bloom in coastal waters at Helgoland Roads in autumn2009. These structures are known to function, both, as a sink for colloidalparticles that adhere to the aggregates during the process of sinking as wellas a source for dissolved substances due to rapid decomposition. The latter isgreatly due to the dense colonization by microorganisms. Such an enhancedmicrobial activity affects the biochemical cycles of carbon, nitrogen,phosphorus, iron and other potential nutrients in the respective aquaticenvironment. We analyzed samples applying CAtalyzed ReporterDeposition-Fluorescence In Situ Hybridization (CARD-FISH) andepifluorescence microscopy, using different oligonucleotide probes on sizefractionated plankton, >10 μm, 10-3 μm, and 3-0.2 μm. The total number ofcells in the 3-0.2 μm fraction decreased after the algal bloom beforestabilizing after 2 months. Despite this trend the total number remained highand the general ratio between Archaea and Bacteria was maintained. A morein-depth observation showed that different phyla followed different trends asa reaction to the environmental conditions. For example at the group level,in the 3-0.2 μm fraction, Alphaproteobacteria appeared to be the mostdominant ranging between 30-50% of the total community. The relativeabundances of the Bacteroidetes in this fraction decreased after the algalbloom (from 37% to 12%) whereas Gammaproteobacteria increased (from9% to 14%). In case of particle associated bacteria (>10 μm) the relativeabundance of Gammaproteobacteria (reaching 40%) was significantly higherthan that in the free-water phase (reaching 25%). Their number on theaggregates decreased after the bloom whereas the number of Roseobacterincreased. SAR11 as well as Crenarchaeota and Actinobacteria clearlypreferred the non-attached phase. These data are to be compared with similaranalysis on freshwater samples. Lake samples were chosen based on aDenaturing Gradient Gel Electrophoresis (DGGE) analysis which showedseasonal fluctuations in both the epilimnion and the hypolimnion of LakeStechlin similar to that observed in the marine system. Preliminary resultsshow that in the fraction smaller than 3 μm Gammaproteobacteria consist aminor part of the community (~1%) while the Betaproteobacteria are muchmore significant than in the marine system, reaching 11% in the epilimnionand 16% in the hypolimnion of Lake Stechlin.EMV015The bacterial community in the digestive tract of thesmall aquatic crustacean Daphnia magnaH. Freese*, B. SchinkDepartment of Biology, University Konstanz, Konstanz, Germanywhether they compete for food. The aim of this study was to characterise theintestinal microbial community and to estimate if Daphnia have aspecialised stable gut microbiota or if the community just reflectssurrounding bacteria. Therefore, the intestinal microbial community of D.magna clones was analysed via 16S rDNA clone libraries. To investigate thestability of their microbiota, Daphnia were incubated under differentconditions (food sources, exposure to defined bacteria) while changes in theintestinal community composition were followed by T-RFLP. The D. magnamicrobiota was dominated by clones affiliated to the β-proteobacteriaLimnohabitans sp., which were described to respond rapidly toenvironmental changes. Overall, the intestinal microbial community did notcontain known fermentative or obligately anaerobic gut bacteria.Limnohabitans spp. were also always prominent in the T-RFLP profilesdespite changing food sources and independent of applied bacteria, thusindicating that they are specialised stable community members. Otherintestinal microorganisms were stimulated by differing food sources butnever dominated the community. Just when Daphnia spp. were starved todeath their microbial community changed distinctly.EMV016Microbial engineers control sediment dynamics inaquatic habitatsS.U. Gerbersdorf* 1 , H.V. Lubarsky 1,2 , D.M. Paterson 2 , S. Wieprecht 1 ,W. Manz 31 Institut for Hydraulic Engineering, Department of Hydraulic Engineeringand Water Resources Management, University Stuttgart, Stuttgart, Germany2 Scottish Oceans Institute, Sediment Ecology Research Group, UniversitySt. Andrews, St. Andrews, United Kingdom3 Institute for Integrated Natural Sciences,University Koblenz, Koblenz,GermanyBackground. Sediments and their microbial communities (biofilms) featureto a great extend the essential functionality of marine and freshwater habitatsand provide important ecosystem services such as nutrient (re)-cycling orself-purification. This study addresses the ecosystem functionbiostabilisation where the microorganisms modify the response of theaquatic sediments to erosive forces (flow velocity, turbulence) by thesecretion of extracellular polymeric substances (EPS).Methods. The colonization of natural assemblages of estuarine bacteria anddiatoms, as well as freshwater biofilms, was studied over several weeksusing non-cohesive glass beads (< 63μm) as an artificial substratum. Theadhesion capacity and the substratum stability of the growing biofilms hasbeen determined by Magnetic Particle Induction (MagPI) and CohesiveStrength Meter (CSM), respectively. In parallel, bacterial cell numbers,microalgal biomass, the composition of the bacterial and microalgalassemblages as well as EPS quantity and quality (carbohydrates, proteins)have been monitored.Results. Microbial colonization resulted in significant enhancement ofadhesion and stability of the substratum as compared to the controls (up to afactor of 12) irrespective of the environment (freshwater, marine). Thestabilization potential of the bacteria exceeded that of the axenic diatomassemblages; however, the overall stabilization was highest in mixedassemblages. The assemblage composition, their physiology and thesecretion of EPS quantity and quality were important for sedimentstabilization, but strongly influenced by changing abiotic conditions.Conclusions. While biostabilisation has been mainly linked to microalgae(ecosystem engineers), our results point out the importance of bacterialassemblages for microbial sediment stabilization. Thereby, changes inabiotic conditions can significantly affect the ecosystem servicebiostabilisation by microbes. The data further suggest that the EPS matrixdetermines sediment adhesion and stability; however the binding strengthwas less related to quantity than to quality with possible synergistic effectsbetween proteins and carbohydrates. This information contributes to ourconceptual understanding of microbial sediment engineering that representsan important ecosystem service.In aquatic environments, bacteria play a key role in the carbon cycle buttheir importance in zooplankton guts remains mostly unknown, althoughtheir presence was regularly documented. Recently, denitrification byingested bacteria in anoxic guts of benthic aquatic invertebrates wasdemonstrated indicating their possible symbiotic participation in digestion.However, the guts of most important zooplankton organisms, e.g. smallDaphnia spp. which are a significant trophic link in freshwater systems, areprobably only partly anoxic if at all. This leads to the question how themicroorganisms interact with their host, i.e., whether they symbioticallyparticipate in digestion, whether they prevent success of pathogens orspektrum | Tagungsband <strong>2011</strong>
EMV017Calcite biomineralization in a karstic cave - bacteriahidden in the darkA. Rusznyak* 1 , D.M. Akob 1 , S. Nietzsche 2 , T.R. Neu 3 , K. Küsel 11 Institute of Ecology, AG Aquatic Geomicrobiology, Friedrich-Schiller-University, Jena, Germany2 Center of Electron Microscopy, Friedrich-Schiller-University, Jena,Germany3 Helmholtz Center for Environmental Research (UFZ), Magdeburg,GermanyKarstic caves represent one of the most important subterranean carbonstorages on Earth and provide excellent „windows” to the subsurface. Ourmultidisciplinary study took advantage of the recent discovery of theHerrenberg Cave to investigate its mineralogy and the diversity and potentialrole of bacteria in carbonate mineral formation. Stalactites consisted ofcalcite, while dolomite and calcite (besides quartz, muscovite and clayminerals) were found in sediments, suggesting that only calcite wasprecipitating from seepage water as stalactites. Confocal laser scanningmicroscopy detected bacterial cells on the surface and in the interior ofstalactites. Molecular analyses revealed the dominance of Proteobacteriainhabiting stalactites and fluvial sediments in addition to the phylaBacteroidetes, Acidobacteria, Nitrospira, Chloroflexi, Planctomycetes,Verrucomicrobia, Actinobacteria and Firmicutes. Up to 16 % of thesequences were related to yet unclassified Bacteria. A large fraction of thesebacteria were metabolically active. Arthrobacter sulfonivorans andRhodococcus globerulus strains isolated from the cave formed mixtures ofcalcite, vaterite and monohydrocalcite. R. globerulus precipitatedidiomorphous, rhombohedral carbonate crystals, while with A. sulfonivoransxenomorphous globular crystals were observed. The different crystalmorphologies refer to species dependent calcite formation and underline theimportance for biomineralization in karstic habitats.EMV018Abundance of microbes involved in nitrogentransformation in the rhizosphere of Leucanthemopsisalpina (L.) Heywood grown in soils from different sites ofthe Damma glacier forefieldS. Töwe* 1 , A. Albert 2 , K. Kleineidam 3 , R. Brankatschk 4 , J.C. Munch 1 ,J. Zeyer 4 , M. Schloter 31 Department of Soil Ecology, Technical University Munich, Neuherberg,Germany2 Department of Environmental Engineering, Helmholtz Center Munich,Neuherberg, Germany3 Department of Terrestrial Ecogenetics, Helmholtz Center Munich,Neuherberg, Germany4 Institute of Biogeochemistry and Pollutant Dynamics, Swiss FederalInstitute of Technology, Zurich, SwitzerlandGlacier forefields are an ideal playground to investigate the role ofdevelopment stages of soils on the formation of plant-microbe interactions,as within the last decades many alpine glaciers retreated, whereby releasingand exposing parent material for soil development. Especially the status ofmacronutrients like nitrogen differs between soils of different developmentstages in these environments and may influence plant growth significantly.Thus in this study, we reconstructed major parts of the nitrogen cycle in therhizosphere soil/root system of Leucanthemopsis alpina (L.) Heywood aswell as the corresponding bulk soil by quantifying functional genes ofnitrogen fixation (nifH), nitrogen mineralization (chiA, aprA), nitrification(amoA AOB, amoA AOA) and denitrification (nirS, nirK, and nosZ) in a 10-year and a 120-year ice-free soil of the Damma glacier forefield. We linkedthe results to the ammonium and nitrate concentrations of the soils as well asto the nitrogen and carbon status of the plants. The experiment wasperformed in a greenhouse simulating the climatic conditions of the glacierforefield. Samples were taken after 7 and 13 weeks of plant growth. HighestnifH gene abundance in connection with lowest nitrogen content of L. alpinawas observed in the 10-year soil after 7 weeks of plant growth,demonstrating the important role of associative nitrogen fixation for plantdevelopment in this soil. In contrast, in the 120-year soil copy numbers ofgenes involved in denitrification, mainly nosZ, were increased after 13weeks of plant growth, indicating an overall increased microbial activitystatus as well as higher concentrations of nitrate in this soil.EMV019Ultrastructural, genomic and ecological analysis of„Candidatus Magnetobacrterium bavaricum” reveals amechanism homologous to proteobacterial magnetosomeformationC. Jogler* 1 , G. Wanner 2 , S. Kolinko 2 , M. Niebler 2 , W. Lin 3 , Y. Pan 3 ,P. Stief 4 , A. Beck 4 , D. de Beer 4 , R. Amann 4 , N. Petersen 2 , M. Kube 5 ,R. Reinhardt 5 , D. Schüler 21 Department of Microbiology and Molecular Genetics, Harvard MedicalSchool, Boston, USA2 Ludwig-Maximilians-University, Munich, Germany3 Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing, China4 Max Planck Institute for Marine Microbiology, Bremen, Germany5 Max Planck Institute for Molecular Genetics, Berlin, GermanyMagnetotactic bacteria (MTB) are phylogenetically diverse. They useintracellular membrane-enclosed magnetite crystals called magnetosomesfor navigation in their aquatic habitats, which are of broad interdisciplinaryinterest. Due to the lack of cultivated representatives from other phyla, thegenetic background of magnetosome formation was exclusively analyzed ina few closely related members of the Proteobacteria thus far, in which allessential functions required for magnetosome formation are encoded withina large genomic magnetosome island. However, the evolutionary origin andphylogenetic distribution of this magnetosome island has been unknown,and it has been questioned whether homologous genes are present in MTBfrom other phyla.Here, we present the analysis of the uncultivated „CandidatusMagnetobacterium bavaricum” (Mbav) from the Nitrospira-phylum bycombining ecological and geochemical techniques with metagenomics,single cell sorting and a variety of advanced electron microscopic methods.Micromanipulation and whole genome amplification of individual sortedcells revealed Mbav-specific sequences that were used for screening ofmetagenomic libraries. This led to the identification of a genomic clustercontaining several magnetosome genes with homology to those inProteobacteria. Different electron microscopic imaging techniques, such asfocused ion beam milling or ultrathin sectioning of high-pressure frozen andfreeze-substituted cells revealed a complex cell envelope and an intricatemagnetosome architecture. In particular, the presence of magnetosomemembranes as well as cytoskeletal magnetosome filaments suggests asimilar mechanism of magnetosome formation in Mbav as inProteobacteria. Altogether, our findings suggest a monophyletic origin ofmagnetotaxis, and relevant genes were likely transferred horizontallybetween Proteobacteria and representatives of the Nitrospira-phylum.EMV020Comparison of Genotypic, Proteotypic and PhenotypicMethods for the Identification of BacteriaM. Patel, S. Polson, U. Herbert*Accugenix, Marketing, Newark, USAAccurate classification of unknown bacterial isolates is an essential first stepin understanding the impact these organisms have on an environmentalmonitoring program. There are many methods, technologies, and strategiesutilized to determine the identity of unknown microorganisms, however, theselection of these methods is often impacted by more than the performanceof the technology. Cost, time and the amount of expertise required toperform an assay are major points to consider during the selection process.Current available methods of identification range from genotypic tophenotypic, with 16S sequencing being universally acknowledged as thestandard for routine bacterial identifications. Still, there is even variabilitywithin this process as not all 16S sequencing methods are comparable.When identifications are based on phenotypic characteristics, the methodsare more subjective and results can be impacted by many variables. The firstpractical proteotypic identification systems utilize matrix-assisted laserdesorption/ionization - time of flight (MALDI-TOF) spectroscopy formicrobial identification. This technology is based on whole cell proteinprofiles that are subject to less expression variability than phenotypicsystems. This study directly compared performance between several of thesetechnologies, including metabolic profiling (bioMerieux VITEK® 2Compact), MALDI-TOF (Bruker BioTyper), automated DNA sequenceanalysis (ABI MicroSEQ® 2.1), and DNA sequencing with a referencequality,customized data analysis process and curated libraries (Accugenix).These microbial identification methods were used to analyze 60 unknownenvironmental bacterial isolates. Accuracy, as well as assay cost, time, andspektrum | Tagungsband <strong>2011</strong>
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3Vereinigung für Allgemeine und An
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22 INSTITUTSPORTRAITMicrobiology in
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264 AUTORENBreinig, F.FBP010FBP023B
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266 AUTORENGoerke, C.Goesmann, A.Go
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268 AUTORENKlaus, T.Klebanoff, S. J
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270 AUTORENMüller, Al.Müller, Ane
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272 AUTORENScherlach, K.Scheunemann
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274 AUTORENWagner, J.Wagner, N.Wahl
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276 PERSONALIA AUS DER MIKROBIOLOGI
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278 PROMOTIONEN 2010Lars Schreiber:
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280 PROMOTIONEN 2010Universität Je
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282 PROMOTIONEN 2010Universität Ro
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Die EINE, auf dieSie gewartet haben