222grow<strong>in</strong>g all over the North, Central and East India <strong>in</strong> a variety of habitatsand soil types. The capability of native bacterial stra<strong>in</strong>s from root nodulesto behave as plant growth promot<strong>in</strong>g bacteria and biocontrol agents was<strong>in</strong>vestigated.Methodology: Isolation of root-nodule symbiont (Palnaippan et al., 2010)Basic characters of isolate (Palnaippan et al., 2010)Genomic DNA isolation, 16S rRNA amplification, 16S rRNA sequenc<strong>in</strong>g,Phylogeny and accession number (Palnaippan et al., 2010)Plant Growth Promot<strong>in</strong>g Characters (Li et al., 2008)Antagonistic characters (Senthilkumar et al., 2009)Germ<strong>in</strong>ation AssayResults: One stra<strong>in</strong> (RCP6) over 21 isolates from the root nodules of C.purpurea were able to grow on Ashby`s N free media over sevensuccessive generation <strong>in</strong>dicative of presumptive N 2-fixation, an IAAproducer, solubilised organic P from calcium phytate, able to release watersoluble <strong>in</strong>organic phosphate from tri-calcium phosphate, di-calciumphosphate and z<strong>in</strong>c phosphate with organic acid production on MM9medium, show halo on ZnPo 4 tris-m<strong>in</strong>imal media <strong>in</strong>dicative of z<strong>in</strong>csolubilisation apart from zone on Aleksandrov`s medium exhibit<strong>in</strong>gsolubilisation of potassium. Isolate had the capability to antagonizeMacrophom<strong>in</strong>a phaseol<strong>in</strong>a, Fusarium udum, F. oxysporum, F. solani,Rhizoctania solani, Sclerot<strong>in</strong>ia sclerotiorum <strong>in</strong> dual culture as well as cellfreeculture filtrate but show no activity aga<strong>in</strong>st Colletotrichum spp.Conventional identification tests, Hi-media Carbokit TM <strong>in</strong>dicated thatRCP6 behaves like the Paenibacillus genus. Molecular identication by16S rRNA sequence analysis identified the stra<strong>in</strong> as Paenibacilluspolymyxa. The 1492 base pair sequence of P. polymyxa RCP6(GU369972) showed maximum similarity to P. polymyxa IAM 13419T(D16276). Stra<strong>in</strong> also showed the ability to improve early vegetativegrowth of C. purpurea <strong>in</strong> germ<strong>in</strong>ation assay.Conclusion: This study disclosed features of Plant growth promot<strong>in</strong>g andantagonistic stra<strong>in</strong> P.polymyxa RCP6 that deserve further studies aimed atconfirm<strong>in</strong>g its importance as a putative endophyte.Palaniappan, P., Chauhan, P. S., Saravanan, V. S., Anandham, R. and Sa, T.-M. (2010). Isolationand characterization of plant growth promot<strong>in</strong>g endophytic bacterial isolates from root noduleofLespedezasp.Biol.Fert.Soil. 46: 807-816.Li, J. H., Wang, E. T., Chen, W. F. and Chen, W. X. (2008). Genetic diversity and potential forpromotion of plant growth detected <strong>in</strong> nodule endophytic bacteria of soybean grown <strong>in</strong>Heliongjiang prov<strong>in</strong>ce of Ch<strong>in</strong>a.Soil.Biol.Biochem. 40: 238-246.Senthilkumar, M., Gov<strong>in</strong>dasamy, V. and Annapurna, K. (2007). Role of antibiosis <strong>in</strong> suppression ofcharcoal rot disease by soybean endophytePaenibacillussp. HKA-15.Curr.Microbiol. 55: 25-29.SMP036Competition between subalp<strong>in</strong>e plants and microbes fornitrogen under different redox conditions and nitrogenfertilization regimes - a greenhouse approachE.-M. Kastl* 1 , S. Gschwendtner 2 , J.C. Munch 2 , M. Schloter 11 Helmholtz Zentrum München, Research Unit Environmental Genomics,Neuherberg, Germany2 Technische Universität München, Chair of soil ecology, Neuherberg, GermanyNatural grasslands are important hotspots for biodiversity and otherecosystem services of soils. The gram<strong>in</strong>eous species of these naturalgrasslands differ greatly <strong>in</strong> nitrogen uptake strategies: Whereasexploitative plants need high amounts of nitrogen compounds for grow<strong>in</strong>g,conservative plants require lower amounts. So far, the <strong>in</strong>fluence of plantnitrogen uptake strategies on microbial community is largely unknown.However, it can be hypothesized that the microbial rhizosphere communityof exploitative plants differ from that of conservative plants due to highcompetition between exploitative plants and microbes for availablenitrogen.The aim of this study was to <strong>in</strong>vestigate the microbial rhizospherecommunity of subalp<strong>in</strong>e gram<strong>in</strong>eous plants with different nitrogen uptakestrategies. Furthermore, the <strong>in</strong>fluence of low oxygen content due to highsoil water content was exam<strong>in</strong>ed, as anoxic conditions are known to favourdenitrification processes and thus might facilitate microbes dur<strong>in</strong>g thecompetition for nitrate. Therefore, a greenhouse experiment with Achilleamillefolium(exploitative), Bromus erectus (<strong>in</strong>termediary) and Brizamedia(conservative) was performed <strong>in</strong> sandy, nutrient poor soil. Plantsreceived 40 kg NH 4NO 3 ha -1 after 7 days and 60 kg NH 4NO 3 ha -1 after 21days of growth. After 28 days plants were sampled. The microbialrhizosphere community was <strong>in</strong>vestigated by quantification of functionalgenes <strong>in</strong>volved <strong>in</strong> nitrification (bacterial and archaeal amoA) anddenitrification (nirK,nirS and nosZ) by real-time PCR. Soil ammonium andnitrate concentrations were determ<strong>in</strong>ed. Furthermore potential enzymeactivities of nitrification and denitrification were analyzed. Thepresentation will give detailed results on the allocation pattern.SMP037Population analysis of iron deposit<strong>in</strong>g bacterial communities<strong>in</strong> technical water systemsJ. Schröder*, H. Danner, B. Braun, U. SzewzykTechnische Universität Berl<strong>in</strong>, Fachgebiet Umweltmikrobiologie, Berl<strong>in</strong>,GermanyThis subproject of the BMBF project „Antiocker“ focuses on theidentification and characterization of iron deposit<strong>in</strong>g bacteria under neutralpH. Iron bacteria have caused problems <strong>in</strong> water s<strong>in</strong>ce the 19th century andthere have been many references to red water becom<strong>in</strong>g undr<strong>in</strong>kablepresumably due to the growths of iron bacteria. The aim of this project isto identify the key bacteria which are <strong>in</strong>volved <strong>in</strong> deposition of oxidizediron compounds. Their activity becomes a very important economicconcern as a result of the <strong>in</strong>tense deposition of iron oxides <strong>in</strong> technicalwater systems. Examples are the process<strong>in</strong>g of groundwater, dr<strong>in</strong>k<strong>in</strong>gwater production or operation of water wells. Therefore ochreous samplesfrom several technical water systems were exam<strong>in</strong>ed to get an overview ofthe composition of the bacterial population.For this purpose, traditional cultivation techniques such as bacterialisolation and molecular methods like PCR-DGGE, FISH <strong>in</strong> comb<strong>in</strong>ationwith epifluorescence-and confocal laser scann<strong>in</strong>g microscopy werecomb<strong>in</strong>ed. The isolation of different iron precipitat<strong>in</strong>g bacteria has beensuccessful and their liv<strong>in</strong>g conditions can be characterized now. In additionto that a 16S rDNA genomic clone library of seven different samples fromochreous water wells (opencast m<strong>in</strong>e and well reactors) was generated. 384clones based on the 16S rDNA are available to make a molecularevolutionary analysis. Besides classical iron bacteria like Gallionella andLeptothrix, representatives of typical soil bacteria of the generaSph<strong>in</strong>gomonas, Novosph<strong>in</strong>gobium, Hyphomicrobium and Arthrobacterwere <strong>in</strong>side.Based on this data, different specific oligonucleotide probes and primerswill be developed for iron bacteria to detect them <strong>in</strong> their natural habitatand make a fast sample screen<strong>in</strong>g possible.SMP038Hydrolytic bacteria <strong>in</strong>volved <strong>in</strong> degradation of plant biomass<strong>in</strong> the biogas processT. Köllmeier*, V.V. Zverlov, W.H. SchwarzTU München, Lehrstuhl für Mikrobiologie, Freis<strong>in</strong>g, GibraltarAs fossil energy supplies are on a decl<strong>in</strong>e, technologies that employregrow<strong>in</strong>g resources have become of mutual <strong>in</strong>terest. Biogas plants employsuch resources as substrate for microbial fermentation processes whichconverte the conta<strong>in</strong>ed energy <strong>in</strong> the energy carrier biogas. Improvementof these processes is of general <strong>in</strong>terest. The aim of this work is to get<strong>in</strong>sights <strong>in</strong>to the composition of hydrolytic bacteria <strong>in</strong> biogas plants tooptimize the hydrolysis of lignocellulosic material. This leads to improvedmethan yield and <strong>in</strong>creased efficiency of the biogas process. We focusedon the development of hydrolytic mixed cultures, their analysis and thedevelopment of monitor<strong>in</strong>g methods to <strong>in</strong>vestigate the abundance ofhydrolytic bacteria <strong>in</strong> (<strong>in</strong>oculated) biogas fermenter. Another approach wasto purify cellulolytic cultures to <strong>in</strong>vestigate their capabilities.SMP039Selective transport of bacterial populations through thevadose zone dur<strong>in</strong>g groundwater rechargeD. Dibbern* 1 , A. Schmalwasser 2 , K.U. Totsche 2 , T. Lueders 11 Helmholtz Center Munich, Institute of Groundwater Ecology, München,Germany2 University of Jena, Department of Hydrogeology, Jena, GermanyPlants <strong>in</strong>troduce abundant carbon <strong>in</strong>to soil, were it can be sequestered <strong>in</strong>microbial biomass and recalcitrant organic matter. However, proportionsof these pools can be relocated, by event-driven transport to deeper vadosezones and even to the groundwater dur<strong>in</strong>g groundwater recharge, such asheavy ra<strong>in</strong>falls or after snowmelt. It is postulated that large fractions of thisefflux are biocolloids, or microbial biomass <strong>in</strong> specific. Relevant questionsare, whether only selected microbial populations are exported from topsoils and what is the fate of this biomass <strong>in</strong> deeper zones and groundwater.Is it merely a carbon <strong>in</strong>put for subsurface microbial food webs or dotransported populations survive?Here, at an agricultural experimental field site, we analyzed thecomposition of mobile bacterial communities collected <strong>in</strong> seepage waterdirectly after recharge events at different depths (35 and 65 cm) andcompared it to the correspond<strong>in</strong>g bacterial communities from soil andvadose depths. Us<strong>in</strong>g T-RFLP and high-throughput pyrotag sequenc<strong>in</strong>g,we reveal that top soil bacteria are washed out selectively, and that theirfate <strong>in</strong> deeper zones may be dist<strong>in</strong>ct, but taxon-specific. These f<strong>in</strong>d<strong>in</strong>gsgreatly extend our understand<strong>in</strong>g of the event-driven and organismic flowof carbon from soil <strong>in</strong>to the subsurface.BIOspektrum | Tagungsband <strong>2012</strong>
223SMP040amoA-based consensus phylogeny of ammonia-oxidiz<strong>in</strong>garchaea and deep sequenc<strong>in</strong>g of amoA genes from soils of fourdifferent geographic regionsM. Pester* 1 , T. Rattei 2 , S. Flechl 1 , A. Gröngröft 3 , A. Richter 4 , J. Overmann 5 ,B. Re<strong>in</strong>hold-Hurek 6 , A. Loy 1 , M. Wagner 11 University of Vienna, Department of Microbial Ecology, Vienna, Austria2 University of Vienna, Department of Computational Systems Biology, Vienna,Austria3 University of Hamburg, Institute of Soil Science, Hamburg, Germany4 University of Vienna, Department of Chemical Ecology and EcosystemResearch, Vienna, Austria5 Leibniz-Institut DSMZ-Deutsche Sammlung von Mikroorganismen undZellkulturen, Braunschweig, Germany6 University of Bremen, Department of Microbe-Plant Interactions, Bremen,GermanyAmmonia-oxidiz<strong>in</strong>g archaea (AOA) play an important role <strong>in</strong> nitrificationand many studies exploit their amoA genes as marker for their diversityand abundance. We present an archaeal amoA consensus phylogeny basedon all publicly available sequences (status June 2010) and provideevidence for the diversification of AOA <strong>in</strong>to four previously recognizedclusters and one newly identified major cluster. These clusters, for whichwe suggest a new nomenclature, harbored 83 AOA species-level OTUs(us<strong>in</strong>g an <strong>in</strong>ferred species threshold of 85% amoA identity). 454pyrosequenc<strong>in</strong>g of amoA amplicons from 16 soils sampled <strong>in</strong> Austria,Costa Rica, Greenland, and Namibia revealed that only 2% of retrievedsequences had no database representative on the species-level andrepresented 30-37 additional species-level OTUs. With the exception of anacidic soil from which mostly amoA amplicons of the Nitrosotalea clusterwere retrieved, all soils were dom<strong>in</strong>ated by amoA amplicons from theNitrososphaera cluster (also called group I.1b), <strong>in</strong>dicat<strong>in</strong>g that thepreviously reported AOA from the Nitrosopumilus cluster (also calledgroup I.1a) are absent or represent m<strong>in</strong>or populations <strong>in</strong> soils. AOArichness estimates on the species level ranged from 8-83 co-exist<strong>in</strong>g AOAsper soil. Presence/absence of amoA OTUs (97% identity level) correlatedwith geographic location, <strong>in</strong>dicat<strong>in</strong>g that besides contemporaryenvironmental conditions also dispersal limitation across differentcont<strong>in</strong>ents and/or historical environmental conditions might <strong>in</strong>fluenceAOA biogeography <strong>in</strong> soils.SMP041Organic propagation of olive nursery plants us<strong>in</strong>g Pantoeaeucr<strong>in</strong>a stra<strong>in</strong> AG9M.D.C. Montero-Calasanz* 1,2 , C. Santamaría 2 , A. Daza 2 , E. Lang 1 , H.-P. Klenk 1 , M. Camacho 21 Leibniz Institute DSMZ- Deutsche Sammlung von Mikroorganism undZellKulturen GmbH , Department of Microbiology, Braunschweig, Germany2 IFAPA Centro Las Torres-Tomejil. Junta de Andalucia., Department ofNatural Resources and Organic Production, Alcala del Rio (Sevilla). SPAIN.,Spa<strong>in</strong>The demand for organic olive oil is <strong>in</strong>creas<strong>in</strong>g exponentially each year(MARM, 2010). However, nowadays there is not a commercial methodthat can replace the use of a synthetic hormone <strong>in</strong> organic propagation ofolive nursery plants.The goal of this work is the development of an organic olive propagationmethod based on the use of the stra<strong>in</strong> AG9 (Pantoea eucr<strong>in</strong>a), previouslycharacterized as a Plant Growth Promot<strong>in</strong>g Rhizobacteria (PGPR). Thisstra<strong>in</strong> has been used <strong>in</strong> monoxenic model systems show<strong>in</strong>g both, higherroot<strong>in</strong>g <strong>in</strong>duction and root elongation than negative controls, <strong>in</strong> mung beanand canola assays. Moreover, this bacterium has been tested <strong>in</strong> four olivecultivars, under nursery conditions, display<strong>in</strong>g higher or similareffectiveness than the hormonal treatments. These results underwrite theworth of this method.On the other hand, by means of Confocal Laser Scann<strong>in</strong>g Microscope(CLSM) and GFP tagged bacterial cells, it was confirmed that this stra<strong>in</strong> isable to colonize the plant roots permanently as an endophyte and topromote the plant growth a long-term.MARM. Anuario de Estadística. M<strong>in</strong>isterio de Medio Ambiente, MedioRural y Mar<strong>in</strong>o. Gorbierno de Espana (2010).SMP042Temperature effects of geothermal energy use on themicrobial community <strong>in</strong> subsurface environmentsF. Hegler* 1 , T. Lüders 1 , G. Bisch 2 , P. Blum 3 , C. Griebler 11 Helmholtz Zentrum München, Institute of Groundwater Ecology, Neuherberg,Germany2 University of Stuttgart, VEGAS - Institut für Wasser- undUmweltsystemmodellierung, Stuttgart, Germany3 Karlsruhe Institute of Technology (KIT), Institute for Applied Geosciences,Karlsruhe, GermanyGeothermal energy use has boomed <strong>in</strong> the last years. In w<strong>in</strong>ter, theexploitation of geothermal energy can be used to heat build<strong>in</strong>gs and <strong>in</strong>summer to cool them. Especially geothermal heat exchangers up to 100 mdepth are <strong>in</strong>stalled frequently. Although geothermal energy use is acceptedas be<strong>in</strong>g environmentally friendly, several aspects need to be considered <strong>in</strong>an evaluation of its use. While complications dur<strong>in</strong>g drill<strong>in</strong>g (e.g. lead<strong>in</strong>gto cracks <strong>in</strong> houses) or dur<strong>in</strong>g the operation of geothermal heat systems(e.g. leakage of anti-freez<strong>in</strong>g agents to the aquifer) are caused bymisjudgment or accidents, other effects cannot be avoided.Generally, temperature <strong>in</strong> the subsurface deeper than 15 m is constant overthe year. Geothermal heat exchangers may decrease or <strong>in</strong>crease thetemperature locally. Therefore, <strong>in</strong> our study we focus on the effects oftemperature changes on the subsurface environment adjacent togeothermal heat exchangers. Temperature shifts <strong>in</strong>fluence the viscosity anddensity of water but also the solubility of liquids, solids, gases andgenerally the geochemical equilibrium. Not only may geochemicalequilibria shift but also the microbial communities and fauna may be<strong>in</strong>fluenced by temperature. While temperature effects on the microbialcommunity for open, nearer surface geothermal systems are documented[1,2] the current project aims to evaluate possible shifts <strong>in</strong>duced bygeothermal heat exchangers.With this study we are present<strong>in</strong>g first results for the effect of chang<strong>in</strong>gtemperatures on the microbial community <strong>in</strong> a usually constanttemperature environment such as the subsurface.1. Brielmann, H., et al., Oberflächennahe Geothermie und ihre potentiellen Auswirkungen aufGrundwasserökologie. Grundwasser, 2011.16: p. 77-91.2. Brielmann, H., et al., Effects of thermal energy discharge on shallow groundwater ecosystems.FEMS Microbiology Ecology, 2009.68: p. 273-286.SMP043Microbial carbon decomposition under anoxic conditions <strong>in</strong>permafrost-affected soil of the Q<strong>in</strong>ghai-Xizang PlateauS. Yang*, D. WagnerAlfred Wegener Institute for Polar and Mar<strong>in</strong>e Research,Geomicrobiology, Potsdam, GermanyThe Q<strong>in</strong>ghai-Xizang Plateau (QXP) <strong>in</strong> high Asia is the third permafrostunit outside polar regions, about 54.3% of it is covered by permafrost,reta<strong>in</strong><strong>in</strong>g 23% SOM of Ch<strong>in</strong>ese soils or 2.5% of the global pool (Wang etal., 2002). Affected by India and Asian monsoon, the plateau differs <strong>in</strong>temperature and moisture gradients along the monsoon routes, mak<strong>in</strong>g thefate of SOM with<strong>in</strong> QXP soil more complicated. The SOM turnover isma<strong>in</strong>ly driven by microbial communities which decompose permafrostSOM via a sequence of microbial processes to CH 4 under anaerobicconditions (methanogenesis), which is a rather strong greenhouse gas. Inresponse to climate warm<strong>in</strong>g, QXP permafrost degradation has beenenhanced over the past decades, the methane turnover via methanogens istherefore our focus from the view of global change research. An<strong>in</strong>terdiscipl<strong>in</strong>ary project is conducted along the two different monsoongradients to l<strong>in</strong>k the<strong>in</strong>-situ methane flux with temporal and spatialvariations of permafrost soil carbon (e.g. ST, SM, SRP, SOMs, TOC, pH)and dynamics of methanogenic consortia. Attention will be paid on theanaerobic carbon decomposition, dynamics of archaeal communities andtheir reaction to global change by us<strong>in</strong>g methane produc<strong>in</strong>g rate analysisand a diverse molecular biotechniques <strong>in</strong>clud<strong>in</strong>g DGGE and t-RFLPf<strong>in</strong>gerpr<strong>in</strong>ts, clon<strong>in</strong>g, FISH and real-time PCR to quantitatively andqualitatively <strong>in</strong>vestigate the diversity, abundance and the changes of thecomposition of archaeal communities. On this basis, it is expected to beable to improve our understand<strong>in</strong>g about the potential anoxicdecomposition of permafrost SOMs under different the climate gradientsand its future development under global warm<strong>in</strong>g.Wang G.X., Ju Q., Cheng G.D., and Lai Y.M.. 2002. Soil organic carbon pool of grassland soils onthe Q<strong>in</strong>ghai-Tibetan Plateau and its global implication. Science of The Total Environment,291(1-3):207-217.BIOspektrum | Tagungsband <strong>2012</strong>
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Instruments that are music to your
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General Information2012 Annual Conf
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SPONSORS & EXHIBITORS9Sponsoren und
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16 AUS DEN FACHGRUPPEN DER VAAMFach
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22 AUS DEN FACHGRUPPEN DER VAAMMitg
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24 INSTITUTSPORTRAITin the differen
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26 INSTITUTSPORTRAITProf. Dr. Lutz
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28 CONFERENCE PROGRAMME | OVERVIEWS
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30 CONFERENCE PROGRAMME | OVERVIEWT
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32 CONFERENCE PROGRAMMECONFERENCE P
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34 CONFERENCE PROGRAMMECONFERENCE P
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36 SPECIAL GROUPSACTIVITIES OF THE
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40 SPECIAL GROUPSACTIVITIES OF THE
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42 SHORT LECTURESMonday, March 19,
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44 SHORT LECTURESMonday, March 19,
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48 SHORT LECTURESWednesday, March 2
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52ISV01Die verborgene Welt der Bakt
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54protein is reversibly uridylylate
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56that this trapping depends on the
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58Here, multiple parameters were an
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60BDP016The paryphoplasm of Plancto
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62of A-PG was found responsible for
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64CEV012Synthetic analysis of the a
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66CEP004Investigation on the subcel
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68CEP013Role of RodA in Staphylococ
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70MurNAc-L-Ala-D-Glu-LL-Dap-D-Ala-D
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72CEP032Yeast mitochondria as a mod
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74as health problem due to the alle
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76[3]. In summary, hypoxia has a st
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78This different behavior challenge
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80FUP008Asc1p’s role in MAP-kinas
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82FUP018FbFP as an Oxygen-Independe
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84defence enzymes, were found to be
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86DNA was extracted and shotgun seq
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88laboratory conditions the non-car
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90MEV003Biosynthesis of class III l
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92provide an insight into the regul
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94MEP007Identification and toxigeni
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96various carotenoids instead of de
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98MEP025Regulation of pristinamycin
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100that the genes for AOH polyketid
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102Knoll, C., du Toit, M., Schnell,
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104pathogenicity of NDM- and non-ND
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106MPV013Bartonella henselae adhesi
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108Yfi regulatory system. YfiBNR is
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110identification of Staphylococcus
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112that a unit increase in water te
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114MPP020Induction of the NF-kb sig
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116[3] Liu, C. et al., 2010. Adhesi
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118virulence provides novel targets
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120proteins are excreted. On the co
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122MPP054BopC is a type III secreti
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124MPP062Invasiveness of Salmonella
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126Finally, selected strains were c
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128interactions. Taken together, ou
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130forS. Typhimurium. Uncovering th
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132understand the exact role of Fla
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134heterotrimeric, Rrp4- and Csl4-c
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136OTV024Induction of systemic resi
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13816S rRNA genes was applied to ac
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140membrane permeability of 390Lh -
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142bacteria in situ, we used 16S rR
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144bacteria were resistant to acid,
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1461. Ye, L.D., Schilhabel, A., Bar
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148using real-time PCR. Activity me
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150When Ms. mazei pWM321-p1687-uidA
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152OTP065The role of GvpM in gas ve
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154OTP074Comparison of Faecal Cultu
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156OTP084The Use of GFP-GvpE fusion
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158compared to 20 ºC. An increase
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160characterised this plasmid in de
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162Streptomyces sp. strain FLA show
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164The study results indicated that
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166have shown direct evidences, for
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168biosurfactant. The putative lipo
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170the absence of legally mandated
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- Page 244 and 245: 244 AUTORENJung, Kr.Jung, P.Junge,
- Page 246: 246 AUTORENNajafi, F.MEP007Naji, S.
- Page 249 and 250: 249van Dijk, G.van Engelen, E.van H
- Page 251 and 252: 251Eckhard Boles von der Universit
- Page 253 and 254: 253Anna-Katharina Wagner: Regulatio
- Page 255 and 256: 255Vera Bockemühl: Produktioneiner
- Page 257 and 258: 257Meike Ammon: Analyse der subzell
- Page 259 and 260: springer-spektrum.deDas große neue