@phdthesis{Hornick2019,
  author    = {Hornick, Thomas},
  title     = {Impact of climate change effects on diversity and function of pelagic heterotrophic bacteria studied in large-scale mesocosm facilities},
  doi       = {10.25932/publishup-42893},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-428936},
  school      = {Universit{\"a}t Potsdam},
  pages     = {199},
  year      = {2019},
  abstract  = {Seit der Industriellen Revolution steigt die Konzentration von Kohlenstoffdioxid (CO2) und anderen Treibhausgasen in der Erdatmosph{\"a}re stetig an, wodurch wesentliche Prozesse im Erdsystem beeinflusst werden. Dies wird mit dem Begriff „Klimawandel" umschrieben. Aquatische {\"O}kosysteme sind sehr stark davon betroffen, da sie als Integral vieler Prozesse in einer Landschaft fungieren. Ziel dieser Doktorarbeit war zu bestimmen, wie verschiedene Auswirkungen des Klimawandels die Gemeinschaftsstruktur und Aktivit{\"a}t von heterotrophen Bakterien in Gew{\"a}ssern ver{\"a}ndert, welche eine zentrale Rolle bei biogeochemischen Prozessen einnehmen. Diese Arbeit konzentriert sich auf zwei Aspekte des Klimawandels: (1) Ozeane nehmen einen Großteil des atmosph{\"a}rischen CO2 auf, welches im Meerwasser das chemische Gleichgewicht des Karbonatsystems verschiebt („Ozeanversauerung"). (2) Durch kontinuierlichen Anstieg der Erdoberfl{\"a}chentemperatur werden Ver{\"a}nderungen im Klimasystem der Erde vorhergesagt, welche u. a. die H{\"a}ufigkeit und Heftigkeit von episodischen Wetterereignissen (z.B. St{\"u}rme) verst{\"a}rken wird. Insbesondere Sommer-St{\"u}rme sind dabei in der Lage die sommerliche Temperaturschichtung der Wassers{\"a}ule in Seen zu zerst{\"o}ren. Beide Effekte des Klimawandels k{\"o}nnen weitreichende Auswirkungen auf Wasserchemie/-physik sowie die Verteilung von Organismen haben, was mittels Mesokosmen simuliert wurde. Dabei untersuchten wir den Einfluss der Ozeanversauerung auf heterotrophe bakterielle Prozesse in der Ostsee bei geringen Konzentrationen an gel{\"o}sten N{\"a}hrstoffen. Unsere Ergebnisse zeigen, dass Ozeanversauerungseffekte in Kombination mit N{\"a}hrstofflimitation indirekt das Wachstum von heterotrophen Bakterien durch ver{\"a}nderte trophische Interaktionen beeinflussen k{\"o}nnen und potentiell zu einer Erh{\"o}hung der Autotrophie des {\"O}kosystems f{\"u}hren. In einer weiteren Studie analysierten wir, wie Ozeanversauerung die Umsetzung und Qualit{\"a}t gel{\"o}sten organischen Materials (DOM) durch heterotrophe Bakterien beeinflussen kann. Die Ergebnisse weisen jedoch darauf hin, dass {\"A}nderungen in der DOM-Qualit{\"a}t durch heterotrophe bakterielle Prozesse mit zunehmender Ozeanversauerung unwahrscheinlich sind. Desweiteren wurde der Einfluss eines starken Sommer-Sturmes auf den stratifizierten, oligotroph-mesotrophen Stechlinsee simuliert. Mittels oberfl{\"a}chlicher Durchmischung in Mesokosmen wurde die bestehende Thermokline zerst{\"o}rt und die durchmischte Oberfl{\"a}chenwasserschicht vergr{\"o}ßert. Dies {\"a}nderte die physikalischen und chemischen Gradienten innerhalb der Wassers{\"a}ule. Effekte der Einmischung von Tiefenwasser {\"a}nderten in der Folge die Zusammensetzung der bakteriellen Gemeinschaftsstruktur und stimulierten das Wachstum filament{\"o}ser Cyanobakterien, die zu einer Cyanobakterien-Bl{\"u}te f{\"u}hrte und so maßgeblich die metabolischen Prozesse von heterotrophen Bakterien bestimmte. Unsere Studie gibt ein mechanistisches Verst{\"a}ndnis, wie Sommer-St{\"u}rme bakterielle Gemeinschaften und Prozesse f{\"u}r l{\"a}ngere Zeit w{\"a}hrend der sommerlichen Stratifizierung beeinflussen k{\"o}nnen. Die in dieser Arbeit pr{\"a}sentierten Ergebnisse zeigen Ver{\"a}nderungen bakterieller Gemeinschaften und Prozesse, welche mit dem einhergehenden Klimawandel erwartet werden k{\"o}nnen. Diese sollten bei Beurteilung klimarelevanter Fragen hinsichtlich eines zuk{\"u}nftigen Gew{\"a}sser-managements Ber{\"u}cksichtigung finden.},
  language  = {en}
}
@phdthesis{Barchewitz2021,
  author    = {Barchewitz, Tino},
  title     = {Impact of microcystin on the non-canonical localization of RubisCO in the toxic bloom-forming cyanobacterium Microcystis aeruginosa PCC7806},
  doi       = {10.25932/publishup-50829},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-508299},
  school      = {Universit{\"a}t Potsdam},
  pages     = {vii, 106},
  year      = {2021},
  abstract  = {Cyanobacteria are an abundant bacterial group and are found in a variety of ecological niches all around the globe. They can serve as a real threat for fish or mammals and can restrict the use of lakes or rivers for recreational purposes or as a source of drinking water, when they form blooms. One of the most abundant bloom-forming cyanobacteria is Microcystis aeruginosa. In the first part of the study, the role and possible dynamics of RubisCO in M. aeruginosa during high-light irradiation were examined. Its response was analyzed on the protein and peptide level via immunoblotting, immunofluorescence microscopy and with high performance liquid chromatography (HPLC). It was revealed that large amounts of RubisCO were located outside of carboxysomes under the applied high light stress. RubisCO aggregated mainly underneath the cytoplasmic membrane. There it forms a putative Calvin-Benson-Bassham (CBB) super complex together with other enzymes of photosynthesis. This complex could be part of an alternative carbon-concentrating mechanism (CCM) in M. aeruginosa, which enables a faster, and energy saving adaptation to high light stress of the whole bloom. Furthermore, the re-localization of RubisCO was delayed in the microcystin-deficient mutant ΔmcyB and RubisCO was more evenly distributed over the cell in comparison to the wild type. Since ΔmcyB is not harmed in its growth, possibly other produced cyanopeptides as aeruginosin or cyanopeptolin also play a role in the stabilization of RubisCO and the putative CBB complex, especially in the microcystin-free mutant. In the second part of this work, the possible role of microcystin as an extracellular signaling peptide during the diurnal cycle was studied. HPLC analysis showed a strong increase of extracellular microcystin in the wild type when the population entered nighttime and it resumed into the next day as well. Together with the increase of extracellular microcystin, a strong decrease of protein-bound intracellular microcystin was observed via immunoblot analysis. Interestingly, the signal of the large subunit of RubisCO (RbcL) also diminished when high amounts of microcystin were present in the surrounding medium. Microcystin addition experiments to M. aeruginosa WT and ΔmcyB cultures support this observation, since the immunoblot signal of both subunits of RubisCO and CcmK, a shell protein of carboxysomes, diminished after the addition of microcystin. In addition, the fluctuation of cyanopeptolin during the diurnal cycle indicates a more prominent role of other cyanopeptides besides microcystin as a signaling peptide, intracellularly as well as extracellularly.},
  language  = {en}
}
@phdthesis{Liu2020,
  author    = {Liu, Qi},
  title     = {Influence of CO2 degassing on microbial community distribution and activity in the Hartoušov degassing system, western Eger Rift (Czech Republic)},
  doi       = {10.25932/publishup-47534},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-475341},
  school      = {Universit{\"a}t Potsdam},
  pages     = {146},
  year      = {2020},
  abstract  = {The Cheb Basin (CZ) is a shallow Neogene intracontinental basin located in the western Eger Rift. The Cheb Basin is characterized by active seismicity and diffuse degassing of mantle-derived CO2 in mofette fields. Within the Cheb Basin, the Hartoušov mofette field shows a daily CO2 flux of 23-97 tons. More than 99\% of CO2 released over an area of 0.35 km2. Seismic active periods have been observed in 2000 and 2014 in the Hartoušov mofette field. Due to the active geodynamic processes, the Cheb Basin is considered to be an ideal region for the continental deep biosphere research focussing on the interaction of biological processes with geological processes. To study the influence of CO2 degassing on microbial community in the surface and subsurface environments, two 3-m shallow drillings and a 108.5-m deep scientific drilling were conducted in 2015 and 2016 respectively. Additionally, the fluid retrieved from the deep drilling borehole was also recovered. The different ecosystems were compared regarding their geochemical properties, microbial abundances, and microbial community structures. The geochemistry of the mofette is characterized by low pH, high TOC, and sulfate contents while the subsurface environment shows a neutral pH, and various TOC and sulfate contents in different lithological settings. Striking differences in the microbial community highlight the substantial impact of elevated CO2 concentrations and high saline groundwater on microbial processes. In general, the microorganisms had low abundance in the deep subsurface sediment compared with the shallow mofette. However, within the mofette and the deep subsurface sediment, the abundance of microbes does not show a typical decrease with depth, indicating that the uprising CO2-rich groundwater has a strong influence on the microbial communities via providing sufficient substrate for anaerobic chemolithoautotrophic microorganisms. Illumina MiSeq sequencing of the 16S rRNA genes and multivariate statistics reveals that the pH strongly influences the microbial community composition in the mofette, while the subsurface microbial community is significantly influenced by the groundwater which motivated by the degassing CO2. Acidophilic microorganisms show a much higher relative abundance in the mofette. Meanwhile, the OTUs assigned to family Comamonadaceae are the dominant taxa which characterize the subsurface communities. Additionally, taxa involved in sulfur cycling characterizing the microbial communities in both mofette and CO2 dominated subsurface environments. Another investigated important geo-bio interaction is the influence of the seismic activity. During seismic events, released H2 may serve as the electron donor for microbial hydrogenotrophic processes, such as methanogenesis. To determine whether the seismic events can potentially trigger methanogenesis by the elevated geogenic H2 concentration, we performed laboratory simulation experiments with sediments retrieved from the drillings. The simulation results indicate that after the addition of hydrogen, substantial amounts of methane were produced in incubated mofette sediments and deep subsurface sediments. The methanogenic hydrogenotrophic genera Methanobacterium was highly enriched during the incubation. The modeling of the in-situ observation of the earthquake swarm period in 2000 at the Novy Kostel focal area/Czech Republic and our laboratory simulation experiments reveals a close relation between seismic activities and microbial methane production via earthquake-induced H2 release. We thus conclude that H2 - which is released during seismic activity - can potentially trigger methanogenic activity in the deep subsurface. Based on this conclusion, we further hypothesize that the hydrogenotrophic early life on Earth was boosted by the Late Heavy Bombardment induced seismic activity in approximately 4.2 to 3.8 Ga.},
  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}
}
@phdthesis{Taube2019,
  author    = {Taube, Robert},
  title     = {Characterisations of Fungal Communities in Temperate Lakes},
  school      = {Universit{\"a}t Potsdam},
  pages     = {139},
  year      = {2019},
  language  = {en}
}
@phdthesis{Numberger2019,
  author    = {Numberger, Daniela},
  title     = {Urban wastewater and lakes as habitats for bacteria and potential vectors for pathogens},
  doi       = {10.25932/publishup-43709},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-437095},
  school      = {Universit{\"a}t Potsdam},
  pages     = {VI, 130},
  year      = {2019},
  abstract  = {Wasser ist lebensnotwendig und somit eine essentielle Ressource. Jedoch sind unsere S{\"u}ßwasser-Ressourcen begrenzt und ihre Erhaltung daher besonders wichtig. Verschmutzungen mit Chemikalien und Krankheitserregern, die mit einer wachsenden Bev{\"o}lkerung und Urbanisierung einhergehen, verschlechtern die Qualit{\"a}t unseres S{\"u}ßwassers. Außerdem kann Wasser als {\"U}bertragungsvektor f{\"u}r Krankheitserreger dienen und daher wasserb{\"u}rtige Krankheiten verursachen. Der Leibniz-Forschungsverbund INFECTIONS'21 untersuchte innerhalb der interdisziplin{\"a}ren Forschungsgruppe III - „Wasser", Gew{\"a}sser als zentralen Mittelpunkt f{\"u}r Krankheiterreger. Dabei konzentrierte man sich auf Clostridioides difficile sowie avi{\"a}re Influenza A-Viren, von denen angenommen wird, dass sie in die Gew{\"a}sser ausgeschieden werden. Ein weiteres Ziel bestand darin, die bakterielle Gemeinschaften eines Kl{\"a}rwerkes der deutschen Hauptstadt Berlin zu charakterisieren, um anschließend eine Bewertung des potentiellen Gesundheitsrisikos geben zu k{\"o}nnen. Bakterielle Gemeinschaften des Roh- und Klarwassers aus dem Kl{\"a}rwerk unterschieden sich signifikant voneinander. Der Anteil an Darm-/F{\"a}kalbakterien war relativ niedrig und potentielle Darmpathogene wurden gr{\"o}ßtenteils aus dem Rohwasser entfernt. Ein potentielles Gesundheitsrisiko konnte allerdings von potentiell pathogenen Legionellen wie L. lytica festgestellt werden, deren relative Abundanz im Klarwasser h{\"o}her war als im Rohwasser. Es wurden außerdem drei C. difficile-Isolate aus den Kl{\"a}rwerk-Rohwasser und einem st{\"a}dtischen Badesee in Berlin (Weisser See) gewonnen und sequenziert. Die beiden Isolate aus dem Kl{\"a}rwerk tragen keine Toxin-Gene, wohingegen das Isolat aus dem See Toxin-Gene besitzt. Alle drei Isolate sind sehr nah mit humanen St{\"a}mmen verwandt. Dies deutet auf ein potentielles, wenn auch sporadisches Gesundheitsrisiko hin. (Avi{\"a}re) Influenza A-Viren wurden in 38.8\% der untersuchten Sedimentproben mittels PCR detektiert, aber die Virusisolierung schlug fehl. Ein Experiment mit beimpften Wasser- und Sedimentproben zeigte, dass f{\"u}r die Isolierung aus Sedimentproben eine relativ hohe Viruskonzentration n{\"o}tig ist. In Wasserproben ist jedoch ein niedriger Titer an Influenza A-Viren ausreichend, um eine Infektion auszul{\"o}sen. Es konnte zudem auch festgestellt werden, dass sich „Madin-Darby Canine Kidney (MDCK)―-Zellkulturen im Gegensatz zu embryonierten H{\"u}hnereiern besser eignen, um Influenza A-Viren aus Sediment zu isolieren. Zusammenfassend l{\"a}sst sich sagen, dass diese Arbeit m{\"o}gliche Gesundheitsrisiken aufgedeckt hat, wie etwa durch Legionellen im untersuchten Berliner Kl{\"a}rwerk, deren relative Abundanz in gekl{\"a}rtem Abwasser h{\"o}her ist als im Rohwasser. Desweiteren wird indiziert, dass Abwasser und Gew{\"a}sser als Reservoir und Vektor f{\"u}r pathogene Organismen dienen k{\"o}nnen, selbst f{\"u}r nicht-typische Wasser-Pathogene wie C. difficile.},
  language  = {en}
}
@phdthesis{Fabian2018,
  author    = {Fabian, Jenny},
  title     = {Effects of algae on microbial carbon cycling in freshwaters},
  doi       = {10.25932/publishup-42222},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-422225},
  school      = {Universit{\"a}t Potsdam},
  pages     = {90},
  year      = {2018},
  abstract  = {Microbial processing of organic matter (OM) in the freshwater biosphere is a key component of global biogeochemical cycles. Freshwaters receive and process valuable amounts of leaf OM from their terrestrial landscape. These terrestrial subsidies provide an essential source of energy and nutrients to the aquatic environment as a function of heterotrophic processing by fungi and bacteria. Particularly in freshwaters with low in-situ primary production from algae (microalgae, cyanobacteria), microbial turnover of leaf OM significantly contributes to the productivity and functioning of freshwater ecosystems and not least their contribution to global carbon cycling. Based on differences in their chemical composition, it is believed that leaf OM is less bioavailable to microbial heterotrophs than OM photosynthetically produced by algae. Especially particulate leaf OM, consisting predominantly of structurally complex and aromatic polymers, is assumed highly resistant to enzymatic breakdown by microbial heterotrophs. However, recent research has demonstrated that OM produced by algae promotes the heterotrophic breakdown of leaf OM in aquatic ecosystems, with profound consequences for the metabolism of leaf carbon (C) within microbial food webs. In my thesis, I aimed at investigating the underlying mechanisms of this so called priming effect of algal OM on the use of leaf C in natural microbial communities, focusing on fungi and bacteria. The works of my thesis underline that algal OM provides highly bioavailable compounds to the microbial community that are quickly assimilated by bacteria (Paper II). The substrate composition of OM pools determines the proportion of fungi and bacteria within the microbial community (Paper I). Thereby, the fraction of algae OM in the aquatic OM pool stimulates the activity and hence contribution of bacterial communities to leaf C turnover by providing an essential energy and nutrient source for the assimilation of the structural complex leaf OM substrate. On the contrary, the assimilation of algal OM remains limited for fungal communities as a function of nutrient competition between fungi and bacteria (Paper I, II). In addition, results provide evidence that environmental conditions determine the strength of interactions between microalgae and heterotrophic bacteria during leaf OM decomposition (Paper I, III). However, the stimulatory effect of algal photoautotrophic activities on leaf C turnover remained significant even under highly dynamic environmental conditions, highlighting their functional role for ecosystem processes (Paper III). The results of my thesis provide insights into the mechanisms by which algae affect the microbial turnover of leaf C in freshwaters. This in turn contributes to a better understanding of the function of algae in freshwater biogeochemical cycles, especially with regard to their interaction with the heterotrophic community.},
  language  = {en}
}