@phdthesis{Lerm2012,
  author    = {Lerm, Stephanie},
  title     = {Mikroorganismen in geothermischen Aquiferen : Einfluss mikrobieller Prozesse auf den Anlagenbetrieb},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-63705},
  school      = {Universit{\"a}t Potsdam},
  year      = {2012},
  abstract  = {In Fluid-, Filter- und Sedimentproben von vier geothermischen Anlagen des Norddeutschen Beckens wurden mit molekulargenetischen Verfahren unterschiedliche mikrobielle Gemeinschaften nachgewiesen. Die mikrobielle Zusammensetzung in den Prozessw{\"a}ssern wurde dabei durch die Aquiferteufe, die Salinit{\"a}t, die Temperatur und den verf{\"u}gbaren Elektronendonatoren und -akzeptoren beeinflusst. Die in den anoxischen Prozessw{\"a}ssern identifizierten Organismen zeichneten sich durch einen chemoheterotrophen oder chemoautotrophen Stoffwechsel aus, wobei Nitrat, Sulfat, Eisen (III) oder Bikarbonat als terminale Elektronenakzeptoren fungierten. Mikroorganismen beeinflussten den Betrieb von zwei Anlagen negativ. So reduzierten im Prozesswasser des K{\"a}ltespeichers am Berliner Reichstag vorhandene Eisenoxidierer, nahe verwandt zu der Gattung Gallionella, die Injektivit{\"a}t der Bohrungen durch Eisenhydroxidausf{\"a}llungen in den Filterschlitzen. Biofilme, die von schwefeloxidierenden Bakterien der Gattung Thiothrix in den Filtern der obert{\"a}gigen Anlage gebildet wurden, f{\"u}hrten ebenfalls zu Betriebsst{\"o}rungen, indem sie die Injektion des Fluids in den Aquifer behinderten. Beim W{\"a}rmespeicher in Neubrandenburg waren Sulfatreduzierer vermutlich an der Bildung von Eisensulfidausf{\"a}llungen in den obert{\"a}gigen Filtern und im bohrlochnahen Bereich beteiligt und verst{\"a}rkten Korrosionsprozesse an der Pumpe im Bohrloch der kalten Aquiferseite. Organische S{\"a}uren in den Fluiden sowie mineralische Ausf{\"a}llungen in den Filtern der obert{\"a}gigen Anlagen waren Belege f{\"u}r die Aktivit{\"a}t der in den verschiedenen Anlagen vorhandenen Mikroorganismen. Es wurde zudem deutlich, dass Mikroorganismen auf Grund der hohen Durchflussraten in den Anlagen chemische Ver{\"a}nderungen in den Prozessw{\"a}ssern deutlich sensitiver anzeigen als chemische Analyseverfahren. So deuteten {\"A}nderungen in der Zusammensetzung der mikrobiellen Bioz{\"o}nosen und speziell die Identifikation von Indikatororganismen wie Eisen- und Schwefeloxidierern, fermentativen Bakterien und Sulfatreduzierern auf eine erh{\"o}hte Verf{\"u}gbarkeit von Elektronendonatoren oder akzeptoren in den Prozessw{\"a}ssern hin. Die Ursachen f{\"u}r die an den Geothermieanlagen auftretenden Betriebsst{\"o}rungen konnten dadurch erkannt werden.},
  language  = {de}
}
@phdthesis{Dunsing2020,
  author    = {Dunsing, Valentin},
  title     = {Fluorescence fluctuation spectroscopy techniques to quantify molecular interactions and dynamics in complex biological systems},
  doi       = {10.25932/publishup-47849},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-478494},
  school      = {Universit{\"a}t Potsdam},
  pages     = {VII, 164, XXV},
  year      = {2020},
  abstract  = {Living cells rely on transport and interaction of biomolecules to perform their diverse functions. A powerful toolbox to study these highly dynamic processes in the native environment is provided by fluorescence fluctuation spectroscopy (FFS) techniques. In more detail, FFS takes advantage of the inherent dynamics present in biological systems, such as diffusion, to infer molecular parameters from fluctuations of the signal emitted by an ensemble of fluorescently tagged molecules. In particular, two parameters are accessible: the concentration of molecules and their transit times through the observation volume. In addition, molecular interactions can be measured by analyzing the average signal emitted per molecule - the molecular brightness - and the cross-correlation of signals detected from differently tagged species. In the present work, several FFS techniques were implemented and applied in different biological contexts. In particular, scanning fluorescence correlation spectroscopy (sFCS) was performed to measure protein dynamics and interactions at the plasma membrane (PM) of cells, and number and brightness (N\&B) analysis to spatially map molecular aggregation. To account for technical limitations and sample related artifacts, e.g. detector noise, photobleaching, or background signal, several correction schemes were explored. In addition, sFCS was combined with spectral detection and higher moment analysis of the photon count distribution to resolve multiple species at the PM. Using scanning fluorescence cross-correlation spectroscopy and cross-correlation N\&B, the interactions of amyloid precursor-like protein 1 (APLP1), a synaptic membrane protein, were investigated. It is shown for the first time directly in living cells, that APLP1 undergoes specific interactions at cell-cell contacts. It is further demonstrated that zinc ions induce formation of large APLP1 clusters that enrich at contact sites and bind to clusters on the opposing cell. Altogether, these results provide direct evidence that APLP1 is a zinc ion dependent neuronal adhesion protein. In the context of APLP1, discrepancies of oligomeric state estimates were observed, which were attributed to non-fluorescent states of the chosen red fluorescent protein (FP) tag mCardinal (mCard). Therefore, multiple FPs and their performance in FFS based measurements of protein interactions were systematically evaluated. The study revealed superior properties of monomeric enhanced green fluorescent protein (mEGFP) and mCherry2. Furthermore, a simple correction scheme allowed unbiased in situ measurements of protein oligomerization by quantifying non-fluorescent state fractions of FP tags. The procedure was experimentally confirmed for biologically relevant protein complexes consisting of up to 12 monomers. In the last part of this work, fluorescence correlation spectroscopy (FCS) and single particle tracking (SPT) were used to characterize diffusive transport dynamics in a bacterial biofilm model. Biofilms are surface adherent bacterial communities, whose structural organization is provided by extracellular polymeric substances (EPS) that form a viscous polymer hydrogel. The presented study revealed a probe size and polymer concentration dependent (anomalous) diffusion hindrance in a reconstituted EPS matrix system caused by polymer chain entanglement at physiological concentrations. This result indicates a meshwork-like organization of the biofilm matrix that allows free diffusion of small particles, but strongly hinders diffusion of larger particles such as bacteriophages. Finally, it is shown that depolymerization of the matrix by phage derived enzymes rapidly facilitated free diffusion. In the context of phage infections, such enzymes may provide a key to evade trapping in the biofilm matrix and promote efficient infection of bacteria. In combination with phage application, matrix depolymerizing enzymes may open up novel antimicrobial strategies against multiresistant bacterial strains, as a promising, more specific alternative to conventional antibiotics.},
  language  = {en}
}
@phdthesis{Leiser2021,
  author    = {Leiser, Rico},
  title     = {Biogeochemical processes governing microplastic transport in freshwater reservoirs},
  doi       = {10.25932/publishup-52024},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-520240},
  school      = {Universit{\"a}t Potsdam},
  pages     = {ix, 143},
  year      = {2021},
  abstract  = {The presented study investigated the influence of microbial and biogeochemical processes on the physical transport related properties and the fate of microplastics in freshwater reservoirs. The overarching goal was to elucidate the mechanisms leading to sedimentation and deposition of microplastics in such environments. This is of importance, as large amounts of initially buoyant microplastics are found in reservoir sediments worldwide. However, the transport processes which lead to microplastics accumulation in sediments, were up to now understudied. The impact of biofilm formation on the density and subsequent sedimentation of microplastics was investigated in the eutrophic Bautzen reservoirs (Chapter 2). Biofilms are complex microbial communities fixed to submerged surfaces through a slimy organic film. The mineral calcite was detected in the biofilms, which led to the sinking of the overgrown microplastic particles. The calcite was of biogenic origin, most likely precipitated by sessile cyanobacteria within the biofilms. Biofilm formation was also studied in the mesotrophic Malter reservoir. Unlike in Bautzen reservoir, biofilm formation did not govern the sedimentation of different microplastics in Malter reservoir (Chapter 3). Instead autumnal lake mixing led to the formation of sinking aggregates of microplastics and iron colloids. Such colloids form when anoxic, iron-rich water from the hypolimnion mixes with the oxygenated epilimnetic waters. The colloids bind organic material from the lake water, which leads to the formation of large and sinking iron-organo flocs. Hence, iron-organo floc formation and their influence on the buoyancy or burial of microplastics into sediments of Bautzen reservoir was studied in laboratory experiments (Chapter 4). Microplastics of different shapes (fiber, fragment, sphere) and sizes were readily incorporated into sinking iron-organo flocs. By this initially buoyant polyethylene microplastics were transported on top of sediments from Bautzen reservoir. Shortly after deposition, the microplastic bearing flocs started to subside and transported the pollutants into deeper sediment layers. The microplastics were not released from the sediments within two months of laboratory incubation. The stability of floc microplastic deposition was further investigated employing experiments with the iron reducing model organism Shewanella oneidensis (Chapter 5). It was shown, that reduction or re-mineralization of the iron minerals did not affect the integrity of the iron-organo flocs. The organic matrix was stable under iron reducing conditions. Hence, no incorporated microplastics were released from the flocs. As similar processes are likely to take place in natural sediments, this might explain the previous described low microplastic release from the sediments. This thesis introduced different mechanisms leading to the sedimentation of initially buoyant microplastics and to their subsequent deposition in freshwater reservoirs. Novel processes such as the aggregation with iron-organo flocs were identified and the understudied issue of biofilm densification through biogenic mineral formation was further investigated. The findings might have implications for the fate of microplastics within the river-reservoir system and outline the role of freshwater reservoirs as important accumulation zone for microplastics. Microplastics deposited in the sediments of reservoirs might not be transported further by through flowing river. Hence the study might contribute to better risk assessment and transport balances of these anthropogenic contaminants.},
  language  = {en}
}