@phdthesis{Khawaja2023, author = {Khawaja, Muhammad Asim}, title = {Improving earthquake forecast modeling and testing using the multi-resolution grids}, school = {Universit{\"a}t Potsdam}, pages = {107}, year = {2023}, language = {en} } @phdthesis{Ribacki2023, author = {Ribacki, Enrico}, title = {Intra-granitic pegmatites of the Las Chacras-Potrerillos batholith, Argentina}, school = {Universit{\"a}t Potsdam}, pages = {XVIII, 183}, year = {2023}, language = {en} } @phdthesis{DokhtDolatabadiEsfahani2022, author = {Dokht Dolatabadi Esfahani, Reza}, title = {Time-dependent monitoring of near-surface and ground motion modelling: developing new data processing approaches based on Music Information Retrieval (MIR) strategies}, doi = {10.25932/publishup-56767}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-567671}, school = {Universit{\"a}t Potsdam}, pages = {xiv, 107}, year = {2022}, abstract = {Seismology, like many scientific fields, e.g., music information retrieval and speech signal pro- cessing, is experiencing exponential growth in the amount of data acquired by modern seismo- logical networks. In this thesis, I take advantage of the opportunities offered by "big data" and by the methods developed in the areas of music information retrieval and machine learning to predict better the ground motion generated by earthquakes and to study the properties of the surface layers of the Earth. In order to better predict seismic ground motions, I propose two approaches based on unsupervised deep learning methods, an autoencoder network and Generative Adversarial Networks. The autoencoder technique explores a massive amount of ground motion data, evaluates the required parameters, and generates synthetic ground motion data in the Fourier amplitude spectra (FAS) domain. This method is tested on two synthetic datasets and one real dataset. The application on the real dataset shows that the substantial information contained within the FAS data can be encoded to a four to the five-dimensional manifold. Consequently, only a few independent parameters are required for efficient ground motion prediction. I also propose a method based on Conditional Generative Adversarial Networks (CGAN) for simulating ground motion records in the time-frequency and time domains. CGAN generates the time-frequency domains based on the parameters: magnitude, distance, and shear wave velocities to 30 m depth (VS30). After generating the amplitude of the time-frequency domains using the CGAN model, instead of classical conventional methods that assume the amplitude spectra with a random phase spectrum, the phase of the time-frequency domains is recovered by minimizing the observed and reconstructed spectrograms. In the second part of this dissertation, I propose two methods for the monitoring and characterization of near-surface materials and site effect analyses. I implement an autocorrelation function and an interferometry method to monitor the velocity changes of near-surface materials resulting from the Kumamoto earthquake sequence (Japan, 2016). The observed seismic velocity changes during the strong shaking are due to the non-linear response of the near-surface materials. The results show that the velocity changes lasted for about two months after the Kumamoto mainshock. Furthermore, I used the velocity changes to evaluate the in-situ strain-stress relationship. I also propose a method for assessing the site proxy "VS30" using non-invasive analysis. In the proposed method, a dispersion curve of surface waves is inverted to estimate the shear wave velocity of the subsurface. This method is based on the Dix-like linear operators, which relate the shear wave velocity to the phase velocity. The proposed method is fast, efficient, and stable. All of the methods presented in this work can be used for processing "big data" in seismology and for the analysis of weak and strong ground motion data, to predict ground shaking, and to analyze site responses by considering potential time dependencies and nonlinearities.}, language = {en} } @phdthesis{Schoenfeldt2022, author = {Sch{\"o}nfeldt, Elisabeth}, title = {Giant landslides in Patagonia, Argentina}, pages = {XXII, 156}, year = {2022}, language = {en} } @phdthesis{Liu2021, author = {Liu, Sisi}, title = {The history of plant diversity change and community assemply a high-altitude and high-latitude ecosystems inferred from sedimentary (ancient) DNA and pollen}, school = {Universit{\"a}t Potsdam}, year = {2021}, language = {en} } @phdthesis{Zhao2021, author = {Zhao, Xueru}, title = {Palaeoclimate and palaeoenvironment evolution from the last glacial maximum into the early holocene (23-8 ka BP) derived from Lago Grande di Monticchio sediment record (S Italy)}, pages = {123}, year = {2021}, language = {en} } @phdthesis{Hebert2021, author = {H{\´e}bert, Raphaёl}, title = {Investigation of vegetation and terrestrial climate variablity during the holocene}, school = {Universit{\"a}t Potsdam}, pages = {201}, year = {2021}, language = {en} } @phdthesis{MogrovejoArias2021, author = {Mogrovejo Arias, Diana Carolina}, title = {Assessment of the frequency and relevance of potentially pathogenic phenotypes in microbial isolates from Arctic environments}, school = {Universit{\"a}t Potsdam}, pages = {125}, year = {2021}, abstract = {The Arctic environments constitute rich and dynamic ecosystems, dominated by microorganisms extremely well adapted to survive and function under severe conditions. A range of physiological adaptations allow the microbiota in these habitats to withstand low temperatures, low water and nutrient availability, high levels of UV radiation, etc. In addition, other adaptations of clear competitive nature are directed at not only surviving but thriving in these environments, by disrupting the metabolism of neighboring cells and affecting intermicrobial communication. Since Arctic microbes are bioindicators which amplify climate alterations in the environment, the Arctic region presents the opportunity to study local microbiota and carry out research about interesting, potentially virulent phenotypes that could be dispersed into other habitats around the globe as a consequence of accelerating climate change. In this context, exploration of Arctic habitats as well as descriptions of the microbes inhabiting them are abundant but microbial competitive strategies commonly associated with virulence and pathogens are rarely reported. In this project, environmental samples from the Arctic region were collected and microorganisms (bacteria and fungi) were isolated. The clinical relevance of these microorganisms was assessed by observing the following virulence markers: ability to grow at a range of temperatures, expression of antimicrobial resistance and production of hemolysins. The aim of this project is to determine the frequency and relevance of these characteristics in an effort to understand microbial adaptations in habitats threatened by climate change. The isolates obtained and described here were able to grow at a range of temperatures, in some cases more than 30 °C higher than their original isolation temperature. A considerable number of them consistently expressed compounds capable of lysing sheep and bovine erythrocytes on blood agar at different incubation temperatures. Ethanolic extracts of these bacteria were able to cause rapid and complete lysis of erythrocyte suspensions and might even be hemolytic when assayed on human blood. In silico analyses showed a variety of resistance elements, some of them novel, against natural and synthetic antimicrobial compounds. In vitro experiments against a number of antimicrobial compounds showed resistance phenotypes belonging to wild-type populations and some non-wild type which clearly denote human influence in the acquisition of antimicrobial resistance. The results of this project demonstrate the presence of virulence-associated factors expressed by microorganisms of natural, non-clinical environments. This study contains some of the first reports, to the best of our knowledge, of hemolytic microbes isolated from the Arctic region. In addition, it provides additional information about the presence and expression of intrinsic and acquired antimicrobial resistance in environmental isolates, contributing to the understanding of the evolution of relevant pathogenic species and opportunistic pathogens. Finally, this study highlights some of the potential risks associated with changes in the polar regions (habitat melting and destruction, ecosystem transition and re-colonization) as important indirect consequences of global warming and altered climatic conditions around the planet.}, language = {en} } @phdthesis{Schimpf2020, author = {Schimpf, Stefan}, title = {Herkunft und Ablagerungsmilieu quart{\"a}rer Sedimente im Einzugsgebiet des Heihe, NW China}, school = {Universit{\"a}t Potsdam}, pages = {xi, 186}, year = {2020}, abstract = {Der zentralasiatische Naturraum, wie er sich uns heute pr{\"a}sentiert, ist das Ergebnis eines Zusammenwirkens vieler verschiedener Faktoren {\"u}ber Jahrmillionen hinweg. Im aktuellen Kontext des Klimawandels zeigt sich jedoch, wie stark sich Stofffl{\"u}sse auch kurzfristig {\"a}ndern und dabei das Gesicht der Landschaft verwandeln k{\"o}nnen. Die Gobi-W{\"u}ste in der Inneren Mongolei (China), als Teil der gleichnamigen Trockenregionen Nordwestchinas, ist aufgrund der Ausgestaltung ihrer landschaftspr{\"a}genden Elemente sowie ihrer Landschaftsdynamik, im Zusammenhang mit der Lage zum Tibet-Plateau, in den Fokus der klimageschichtlichen Grundlagenforschung ger{\"u}ckt. Als großes Langzeitarchiv unterschiedlichster fluvialer, lakustriner und {\"a}olischer Sedimente stellt sie eine bedeutende Lokalit{\"a}t zur Rekonstruktion von lokalen und regionalen Stofffl{\"u}ssen dar.. Andererseits ist die Gobi-W{\"u}ste zugleich auch eine bedeutende Quelle f{\"u}r den {\"u}berregionalen Staubtransport, da sie aufgrund der klimatischen Bedingungen insbesondere der Erosion durch Ausblasung preisgegeben wird. Vor diesem Hintergrund erfolgten zwischen 2011 und 2014, im Rahmen des BMBF-Verbundprogramms WTZ Zentralasien - Monsundynamik \& Geo{\"o}kosysteme (F{\"o}rderkennzeichen 03G0814), mehrere deutsch-chinesische Expeditionen in das Ejina-Becken (Innere Mongolei) und das Qilian Shan-Vorland. Im Zuge dieser Expeditionen wurden f{\"u}r eine Bestimmung potenzieller Sedimentquellen erstmals zahlreiche Oberfl{\"a}chenproben aus dem gesamten Einzugsgebiet des Heihe (schwarzer Fluss) gesammelt. Zudem wurden mit zwei Bohrungen im inneren des Ejina-Beckens, erg{\"a}nzende Sedimentbohrkerne zum bestehenden Bohrkern D100 (siehe W{\"u}nnemann (2005)) abgeteuft, um weit reichende, erg{\"a}nzende Informationen zur Landschaftsgeschichte und zum {\"u}berregionalen Sedimenttransfer zu erhalten. Gegenstand und Ziel der vorliegenden Doktorarbeit ist die sedimentologisch-mineralogische Charakterisierung des Untersuchungsgebietes in Bezug auf potenzielle Sedimentquellen und Stofffl{\"u}sse des Ejina-Beckens sowie die Rekonstruktion der Ablagerungsgeschichte eines dort erbohrten, 19m langen Sedimentbohrkerns (GN100). Schwerpunkt ist hierbei die Kl{\"a}rung der Sedimentherkunft innerhalb des Bohrkerns sowie die Ausweisung von Herkunftssignalen und m{\"o}glichen Sedimentquellen bzw. Sedimenttransportpfaden. Die methodische Herangehensweise basiert auf einem Multi-Proxy-Ansatz zur Charakterisierung der klastischen Sedimentfazies anhand von Gel{\"a}ndebeobachtungen, lithologisch-granulometrischen und mineralogisch-geochemischen Analysen sowie statistischen Verfahren. F{\"u}r die mineralogischen Untersuchungen der Sedimente wurde eine neue, rasterelektronenmikroskopische Methode zur automatisierten Partikelanalyse genutzt und den traditionellen Methoden gegen{\"u}bergestellt. Die synoptische Betrachtung der granulometrischen, geochemischen und mineralogischen Befunde der Oberfl{\"a}chensedimente ergibt f{\"u}r das Untersuchungsgebiet ein logisches Kaskadenmodell mit immer wiederkehrenden Prozessbereichen und {\"a}hnlichen Prozesssignalen. Die umfangreichen granulometrischen Analysen deuten dabei auf abnehmende Korngr{\"o}ßen mit zunehmender Entfernung vom Qilian Shan hin und erm{\"o}glichen die Identifizierung von vier texturellen Signalen: den fluvialen Sanden, den D{\"u}nensanden, den Stillwassersedimenten und St{\"a}uben. Diese Ergebnisse k{\"o}nnen als Interpretationsgrundlage f{\"u}r die Korngr{\"o}ßenanalysen des Bohrkerns genutzt werden. Somit ist es m{\"o}glich, die Ablagerungsgeschichte der Bohrkernsedimente zu rekonstruieren und in Verbindung mit eigenen und literaturbasierten Datierungen in einen Gesamtkontext einzuh{\"a}ngen. F{\"u}r das Untersuchungsgebiet werden somit vier Ablagerungsphasen ausgewiesen, die bis in die Zeit des letzten glazialen Maximums (LGM) zur{\"u}ckreichen. W{\"a}hrend dieser Ablagerungsphasen kam es im Zuge unterschiedlicher Aktivit{\"a}ts- und Stabilit{\"a}tsphasen zu einer kontinuierlichen Progradation und {\"U}berpr{\"a}gung des Schwemmf{\"a}chers. Eine besonders aktive Phase kann zwischen 8 ka und 4 ka BP festgestellt werden, w{\"a}hrend der es aufgrund zunehmender fluvialer Aktivit{\"a}ten zu einer deutlich verst{\"a}rkten Schwemmf{\"a}cherdynamik gekommen zu sein scheint. In den Abschnitten davor und danach waren es vor allem {\"a}olische Prozesse, die zu einer {\"U}berpr{\"a}gung des Schwemmf{\"a}chers gef{\"u}hrt haben. Hinsichtlich der mineralogischen Herkunftssignale gibt es eine große Variabilit{\"a}t. Dies spiegelt die enorme Heterogenit{\"a}t der Geologie des Untersuchungsgebietes wider, wodurch die r{\"a}umlichen Signale nicht sehr stark ausgepr{\"a}gt sind. Dennoch, k{\"o}nnen f{\"u}r das Einzugsgebiet drei gr{\"o}ßere Bereiche deklariert werden, die als Herkunftsgebiet in Frage kommen. Das {\"o}stliche Qilian Shan Vorland zeichnet sich dabei durch deutlich h{\"o}here Chloritgehalte als prim{\"a}re Quelle f{\"u}r die Sedimente im Ejina-Becken aus. Sie unterscheiden sich insbesondere durch stark divergierende Chloritgehalte in der Tonmineral- und Gesamtmineralfraktion, was das {\"o}stliche Qilian Shan Vorland als prim{\"a}re Quelle f{\"u}r die Sedimente im Ejina-Becken auszeichnet. Dies steht in Zusammenhang mit den Gr{\"u}nschiefern, Ophioliten und Serpentiniten in diesem Bereich. Geochemisch deutet vor allem das Cr/Rb-Verh{\"a}ltnis eine große Variabilit{\"a}t innerhalb des Einzugsgebietes an. Auch hier ist es das {\"o}stliche Vorland, welches aufgrund seines hohen Anteils an mafischen Gesteinen reich an Chromiten und Spinellen ist und sich somit vom restlichen Untersuchungsgebiet abhebt. Die zeitliche aber auch die generelle Variabilit{\"a}t der Sedimentherkunft l{\"a}sst sich in den Bohrkernsedimenten nicht so deutlich nachzeichnen. Die mineralogisch-sedimentologischen Eigenschaften der erbohrten klastischen Sedimente zeugen zwar von zwischenzeitlichen {\"A}nderungen bei der Sedimentherkunft, diese sind jedoch nicht so deutlich ausgepr{\"a}gt, wie es die Quellsignale in den Oberfl{\"a}chensedimenten vermuten lassen. Ein Grund daf{\"u}r scheint die starke Vermischung unterschiedlichster Sedimente w{\"a}hrend des Transportes zu sein. Die Kombination der Korngr{\"o}ßenergebnisse mit den Befunden der Gesamt- und Schwermineralogie deuten darauf hin, dass es zwischenzeitlich eine Phase mit {\"u}berwiegend {\"a}olischen Prozessen gegeben hat, die mit einem Sedimenteintrag aus dem westlichen Bei Shan in Verbindung stehen. Neben der Zunahme ultrastabiler Schwerminerale wie Zirkon und Granat und der Abnahme opaker Schwerminerale, weisen vor allem die heutigen Verh{\"a}ltnisse darauf hin. Der Vergleich der traditionellen Schwermineralanalyse mit der Computer-Controlled-Scanning-Electron-Microscopy (kurz: CCSEM), die eine automatisierte Partikelauswertung der Proben erm{\"o}glicht, zeigt den deutlichen Vorteil der modernen Analysemethode. Neben einem zeitlichen Vorteil, den man durch die automatisierte Abarbeitung der vorbereiteten Proben erlangen kann, steht vor allem die deutlich gr{\"o}ßere statistische Signifikanz des Ergebnisses im Vordergrund. Zudem k{\"o}nnen mit dieser Methode auch chemische Variet{\"a}ten einiger Schwerminerale bestimmt werden, die eine noch feinere Klassifizierung und sicherere Aussagen zu einer m{\"o}glichen Sedimentherkunft erm{\"o}glichen. Damit ergeben sich außerdem verbesserte Aussagen zu Zusammensetzungen und Entstehungsprozessen der abgelagerten Sedimente. Die Studie verdeutlicht, dass die Sedimentherkunft innerhalb des Untersuchungsgebietes sowie die ablaufenden Prozesse zum Teil stark von lokalen Gegebenheiten abh{\"a}ngen. Die Heterogenit{\"a}t der Geologie und die Gr{\"o}ße des Einzugsgebietes sowie die daraus resultierende Komplexit{\"a}t der Sedimentgenese, machen exakte Zuordnungen zu klar definierten Sedimentquellen sehr schwer. Dennoch zeigen die Ergebnisse, dass die Sedimentzufuhr in das Ejina-Becken in erster Linie durch fluviale klastische Sedimente des Heihe aus dem Qilian Shan erfolgt sein muss. Die Untersuchungsergebnisse zeigen jedoch ebenso die Notwendigkeit einer erg{\"a}nzenden Bearbeitung angrenzender Untersuchungsgebiete, wie beispielsweise den Gobi-Altai im Norden oder den Beishan im Westen, sowie die Verdichtung der Oberfl{\"a}chenbeprobung zur feineren Aufl{\"o}sung von lokalen Sedimentquellen.}, language = {de} } @phdthesis{Angelopoulos2020, author = {Angelopoulos, Michael}, title = {Mechanisms of sub-aquatic permafrost evolution in Arctic coastal environments}, school = {Universit{\"a}t Potsdam}, pages = {165}, year = {2020}, abstract = {Subsea permafrost is perennially cryotic earth material that lies offshore. Most submarine permafrost is relict terrestrial permafrost beneath the Arctic shelf seas, was inundated after the last glaciation, and has been warming and thawing ever since. It is a reservoir and confining layer for gas hydrates and has the potential to release greenhouse gases and affect global climate change. Furthermore, subsea permafrost thaw destabilizes coastal infrastructure. While numerous studies focus on its distribution and rate of thaw over glacial timescales, these studies have not been brought together and examined in their entirety to assess rates of thaw beneath the Arctic Ocean. In addition, there is still a large gap in our understanding of sub-aquatic permafrost processes on finer spatial and temporal scales. The degradation rate of subsea permafrost is influenced by the initial conditions upon submergence. Terrestrial permafrost that has already undergone warming, partial thawing or loss of ground ice may react differently to inundation by seawater compared to previously undisturbed ice-rich permafrost. Heat conduction models are sufficient to model the thaw of thick subsea permafrost from the bottom, but few studies have included salt diffusion for top-down chemical degradation in shallow waters characterized by mean annual cryotic conditions on the seabed. Simulating salt transport is critical for assessing degradation rates for recently inundated permafrost, which may accelerate in response to warming shelf waters, a lengthening open water season, and faster coastal erosion rates. In the nearshore zone, degradation rates are also controlled by seasonal processes like bedfast ice, brine injection, seasonal freezing under floating ice conditions and warm freshwater discharge from large rivers. The interplay of all these variables is complex and needs further research. To fill this knowledge gap, this thesis investigates sub-aquatic permafrost along the southern coast of the Bykovsky Peninsula in eastern Siberia. Sediment cores and ground temperature profiles were collected at a freshwater thermokarst lake and two thermokarst lagoons in 2017. At this site, the coastline is retreating, and seawater is inundating various types of permafrost: sections of ice-rich Pleistocene permafrost (Yedoma) cliffs at the coastline alternate with lagoons and lower elevation previously thawed and refrozen permafrost basins (Alases). Electrical resistivity surveys with floating electrodes were carried out to map ice-bearing permafrost and taliks (unfrozen zones in the permafrost, usually formed beneath lakes) along the diverse coastline and in the lagoons. Combined with the borehole data, the electrical resistivity results permit estimation of contemporary ice-bearing permafrost characteristics, distribution, and occasionally, thickness. To conceptualize possible geomorphological and marine evolutionary pathways to the formation of the observed layering, numerical models were applied. The developed model incorporates salt diffusion and seasonal dynamics at the seabed, including bedfast ice. Even along coastlines with mean annual non-cryotic boundary conditions like the Bykovsky Peninsula, the modelling results show that salt diffusion minimizes seasonal freezing of the seabed, leading to faster degradation rates compared to models without salt diffusion. Seasonal processes are also important for thermokarst lake to lagoon transitions because lagoons can generate cold hypersaline conditions underneath the ice cover. My research suggests that ice-bearing permafrost can form in a coastal lagoon environment, even under floating ice. Alas basins, however, may degrade more than twice as fast as Yedoma permafrost in the first several decades of inundation. In addition to a lower ice content compared to Yedoma permafrost, Alas basins may be pre-conditioned with salt from adjacent lagoons. Considering the widespread distribution of thermokarst in the Arctic, its integration into geophysical models and offshore surveys is important to quantify and understand subsea permafrost degradation and aggradation. Through numerical modelling, fieldwork, and a circum-Arctic review of subsea permafrost literature, this thesis provides new insights into sub-aquatic permafrost evolution in saline coastal environments.}, language = {en} } @phdthesis{Menges2020, author = {Menges, Johanna}, title = {Organic Carbon Storage, Transfer and Transformation in the Himalaya}, school = {Universit{\"a}t Potsdam}, pages = {179}, year = {2020}, abstract = {The transfer of particulate organic carbon from continents to the ocean is an important component of the global carbon cycle. Transfer to and burial of photosynthetically fixed biospheric organic carbon in marine sediments can effectively sequester atmospheric carbon dioxide over geological timescales. The exhumation and erosion of fossil organic carbon contained in sedimentary rocks, i.e. petrogenic carbon, can result in remineralization, releasing carbon to the atmosphere. In contrast, eroded petrogenic organic carbon that gets transferred back to the ocean and reburied does not affect atmospheric carbon content. Mountain ranges play a key role in this transfer since they can source vast amounts of sediment including particulate organic carbon. Globally, the export of both, biospheric and petrogenic organic carbon has been linked to sediment export. Additionally, short transfer times from mountains to the ocean and high sediment concentrations have been shown to increase the likelihood of organic carbon burial. While the importance of mountain ranges in the organic carbon cycle is now widely recognized, the processes acting within mountain ranges to influence the storage, cycling and mobilization of organic carbon, as well as carbon fluxes from mountain ranges remain poorly constrained. In this thesis, I employ different methods to assess the nature and fate of particulate organic carbon in mountain belts, ranging from the molecular to regional landscape scale. These studies are located along the Trans-Himalayan Kali Gandaki River in Central Nepal. This river traverses all major geological and climatic zones of the Himalaya, from the dry northern Tibetan plateau to the high-relief, monsoon dominated steep High Himalaya and the lower relief and abundant vegetation of the Lesser Himalayan region. First, I document how biospheric organic matter has accumulated during the Holocene in the headwaters of the Kali Gandaki River valley, by combining compound specific isotope measurements with different dating methods and grain size data, and investigate the stability of this organic carbon reservoir on millennial timescales. I show, that around 1.6 ka an eco-geomorphic tipping point occurred leading to a destabilization of the landscape resulting in today's high erosion rates and the excavation of the aged organic carbon reservoir. This study highlights the climatic and geomorphic controls on biospheric organic carbon storage and release from mountain ranges. Second, I systematically investigate the spatial variation of particulate organic carbon fluxes across the Himalaya along the Kali Gandaki River, using bulk stable and radioactive isotopes combined with a new Bayesian modeling approach. The detailed dataset allows the distinction of aged and modern biospheric organic carbon as well as petrogenic organic carbon across the Himalayan mountain range and the investigation of the role of climatic and geomorphic factors in their riverine export. The data suggest a decoupling of the particulate organic carbon from the sediment yield along the Kali Gandaki River, partially driven by climatic and geomorphic processes. In contrast to the suspended sediment, a large part of the particulate organic carbon exported by the river originates from the Tibetan part of the catchment and is dominated by petrogenic organic carbon derived from Jurassic shales with only minor contributions of modern and aged biospheric organic carbon. These findings emphasize the importance of organic carbon source distribution and erosion mechanisms in determining the organic carbon export from mountain ranges. In a third step, I explore the potential of ultra-high resolution mass spectrometry for particulate organic carbon transport studies. I have generated a novel and unprecedented high-resolution molecular dataset, which contains up to 103 molecular formulas of the lipid fraction of particulate organic matter for modern and aged biospheric carbon, petrogenic organic carbon and river sediments. First, I test if this dataset can be used to better resolve different organic carbon sources and to identify new geochemical tracers. Using multivariate statistics, I identify up to 10² characteristic molecular formulas for the major organic carbon sources in the upper part of the Kali Gandaki catchment, and trace their transfer from the surrounding landscape into the river sediment. Second, I test the potential of the molecular dataset to trace molecular transformations along source-to-sink pathways. I identify changes in molecular metrics derived from the dataset, which are characteristic of transformation processes during incorporation of litter into soil, the aging of soil material, and the mobilization of the organic carbon into the river. These two studies demonstrate that high-resolution molecular datasets open a promising analytical window on particulate organic carbon and can provide novel insights into the composition, sourcing and transformation of riverine particulate organic carbon. Collectively, these studies advance our understanding of the processes contributing to the storage and mobilization of organic carbon in the Central Himalaya, the mountain belt that dominates global erosional fluxes. They do so by identifying the major sources of particulate organic carbon to the Trans-Himalayan Kali Gandaki River, by elucidating their sensitivity to climate and geomorphic processes, and by identifying some of the transformations of this material on the molecular scale. As a result, the thesis demonstrates that the amount and composition of organic carbon routed from mountain belts is a function of the dynamic interactions of geologic, biologic, geomorphic and climatic processes within the mountain belt. This understanding will ultimately help in answering whether the build-up and erosion of mountain ranges over geological time represents a net carbon source or sink to the atmosphere. Beyond this, the thesis contributes to our technical ability to characterize organic matter and attribute it to sources by scoping the potential of high-end molecular analysis.}, language = {en} } @phdthesis{Holm2020, author = {Holm, Stine}, title = {Methanogenic communities and metaplasmidome-encoded functions in permafrost environments exposed to thaw}, school = {Universit{\"a}t Potsdam}, pages = {VI, 243}, year = {2020}, abstract = {This thesis investigates how the permafrost microbiota responds to global warming. In detail, the constraints behind methane production in thawing permafrost were linked to methanogenic activity, abundance and composition. Furthermore, this thesis offers new insights into microbial adaptions to the changing environmental conditions during global warming. This was assesed by investigating the potential ecological relevant functions encoded by plasmid DNA within the permafrost microbiota. Permafrost of both interglacial and glacial origin spanning the Holocene to the late Pleistocene, including Eemian, were studied during long-term thaw incubations. Furthermore, several permafrost cores of different stratigraphy, soil type and vegetation cover were used to target the main constraints behind methane production during short-term thaw simulations. Short- and long-term incubations simulating thaw with and without the addition of substrate were combined with activity measurements, amplicon and metagenomic sequencing of permanently frozen and seasonally thawed active layer. Combined, it allowed to address the following questions. i) What constraints methane production when permafrost thaws and how is this linked to methanogenic activity, abundance and composition? ii) How does the methanogenic community composition change during long-term thawing conditions? iii) Which potential ecological relevant functions are encoded by plasmid DNA in active layer soils? The major outcomes of this thesis are as follows. i) Methane production from permafrost after long-term thaw simulation was found to be constrained mainly by the abundance of methanogens and the archaeal community composition. Deposits formed during periods of warmer temperatures and increased precipitation, (here represented by deposits from the Late Pleistocene of both interstadial and interglacial periods) were found to respond strongest to thawing conditions and to contain an archaeal community dominated by methanogenic archaea (40\% and 100\% of all detected archaea). Methanogenic population size and carbon density were identified as main predictors for potential methane production in thawing permafrost in short-term incubations when substrate was sufficiently available. ii) Besides determining the methanogenic activity after long-term thaw, the paleoenvironmental conditions were also found to influence the response of the methanogenic community composition. Substantial shifts within methanogenic community structure and a drop in diversity were observed in deposits formed during warmer periods, but not in deposits from stadials, when colder and drier conditions occurred. Overall, a shift towards a dominance of hydrogenotrophic methanogens was observed in all samples, except for the oldest interglacial deposits from the Eemian, which displayed a potential dominance of acetoclastic methanogens. The Eemian, which is discussed to serve as an analogue to current climate conditions, contained highly active methanogenic communities. However, all potential limitation of methane production after permafrost thaw, it means methanogenic community structure, methanogenic population size, and substrate pool might be overcome after permafrost had thawed on the long-term. iii) Enrichments with soil from the seasonally thawed active layer revealed that its plasmid DNA ('metaplasmidome') carries stress-response genes. In particular it encoded antibiotic resistance genes, heavy metal resistance genes, cold shock proteins and genes encoding UV-protection. Those are functions that are directly involved in the adaptation of microbial communities to stresses in polar environments. It was further found that metaplasmidomes from the Siberian active layer originate mainly from Gammaproteobacteria. By applying enrichment cultures followed by plasmid DNA extraction it was possible to obtain a higher average contigs length and significantly higher recovery of plasmid sequences than from extracting plasmid sequences from metagenomes. The approach of analyzing 'metaplasmidomes' established in this thesis is therefore suitable for studying the ecological role of plasmids in polar environments in general. This thesis emphasizes that including microbial community dynamics have the potential to improve permafrost-carbon projections. Microbially mediated methane release from permafrost environments may significantly impact future climate change. This thesis identified drivers of methanogenic composition, abundance and activity in thawing permafrost landscapes. Finally, this thesis underlines the importance to study how the current warming Arctic affects microbial communities in order to gain more insight into microbial response and adaptation strategies.}, language = {en} } @phdthesis{Scheffler2019, author = {Scheffler, Franziska}, title = {Selenite pseudomorphs}, school = {Universit{\"a}t Potsdam}, pages = {154}, year = {2019}, language = {en} } @phdthesis{Kneier2019, author = {Kneier, Fabian}, title = {Subsea permafrost in the Laptev Sea}, school = {Universit{\"a}t Potsdam}, pages = {220}, year = {2019}, abstract = {During lower sea levels in glacial periods, deep permafrost formed on large continental shelf areas of the Arctic Ocean. Subsequent sea level rise and coastal erosion created subsea permafrost, which generally degrades after inundation under the influence of a complex suite of marine, near-shore processes. Global warming is especially pronounced in the Arctic, and will increase the transition to and the degradation of subsea permafrost, with implications for atmospheric climate forcing, offshore infrastructure, and aquatic ecosystems. This thesis combines new geophysical, borehole observational and modelling approaches to enhance our understanding of subsea permafrost dynamics. Three specific areas for advancement were identified: (I) sparsity of observational data, (II) lacking implementation of salt infiltration mechanisms in models, and (III) poor understanding of the regional differences in key driving parameters. This study tested the combination of spectral ratios of the ambient vibration seismic wavefield, together with estimated shear wave velocity from seismic interferometry analysis, for estimating the thickness of the unfrozen sediment overlying the ice-bonded permafrost offshore. Mesoscale numerical calculations (10^1 to 10^2 m, thousands of years) were employed to develop and solve the coupled heat diffusion and salt transport equations including phase change effects. Model soil parameters were constrained by borehole data, and the impact of a variety of influences during the transgression was tested in modelling studies. In addition, two inversion schemes (particle swarm optimization and a least-square method) were used to reconstruct temperature histories for the past 200-300 years in the Laptev Sea region in Siberia from two permafrost borehole temperature records. These data were evaluated against larger scale reconstructions from the region. It was found (I) that peaks in spectral ratios modelled for three-layer, one-dimensional systems corresponded with thaw depths. Around Muostakh Island in the central Laptev Sea seismic receivers were deployed on the seabed. Derived depths of the ice-bonded permafrost table were between 3.7-20.7 m ± 15 \%, increasing with distance from the coast. (II) Temperatures modelled during the transition to subsea permafrost resembled isothermal conditions after about 2000 years of inundation at Cape Mamontov Klyk, consistent with observations from offshore boreholes. Stratigraphic scenarios showed that salt distribution and infiltration had a large impact on the ice saturation in the sediments. Three key factors were identified that, when changed, shifted the modelled permafrost thaw depth most strongly: bottom water temperatures, shoreline retreat rate and initial temperature before inundation. Salt transport based on diffusion and contribution from arbitrary density-driven mechanisms only accounted for about 50 \% of observed thaw depths at offshore sites hundreds to thousands of years after inundation. This bias was found consistently at all three sites in the Laptev Sea region. (III) In the temperature reconstructions, distinct differences in the local temperature histories between the western Laptev Sea and the Lena Delta sites were recognized, such as a transition to warmer temperatures a century later in the western Laptev Sea as well as a peak in warming three decades later. The local permafrost surface temperature history at Sardakh Island in the Lena Delta was reminiscent of the circum-Arctic regional average trends. However, Mamontov Klyk in the western Laptev Sea was consistent to Arctic trends only in the most recent decade and was more similar to northern hemispheric mean trends. Both sites were consistent with a rapid synoptic recent warming. In conclusion, the consistency between modelled response, expected permafrost distribution, and observational data suggests that the passive seismic method is promising for the determination of the thickness of unfrozen sediment on the continental Arctic shelf. The quantified gap between currently modelled and observed thaw depths means that the impact of degradation on climate forcing, ecosystems, and infrastructure is larger than current models predict. This discrepancy suggests the importance of further mechanisms of salt penetration and thaw that have not been considered - either pre-inundation or post-inundation, or both. In addition, any meaningful modelling of subsea permafrost would have to constrain the identified key factors and their regional differences well. The shallow permafrost boreholes provide missing well-resolved short-scale temperature information in the coastal permafrost tundra of the Arctic. As local differences from circum-Arctic reconstructions, such as later warming and higher warming magnitude, were shown to exist in this region, these results provide a basis for local surface temperature record parameterization of climate and, in particular, permafrost models. The results of this work bring us one step further to understanding the full picture of the transition from terrestrial to subsea permafrost.}, language = {en} } @phdthesis{Fuchs2019, author = {Fuchs, Matthias}, title = {Soil organic carbon and nitrogen pools in thermokarst-affected permafrost terrain}, school = {Universit{\"a}t Potsdam}, pages = {203}, year = {2019}, language = {en} } @phdthesis{Caesar2019, author = {Caesar, Levke}, title = {The evolution of the Atlantic Meridional Overturning Circulation and its implications for surface warming}, address = {Potsdam}, school = {Universit{\"a}t Potsdam}, pages = {119}, year = {2019}, abstract = {The Atlantic Meridional Overturning Circulation (AMOC) is likely the most well-known system of ocean currents on Earth, redistributing heat, nutrients and carbon over a large part of the Earth's surface and affecting global climate as a result. Due to enhanced freshwater fluxes into the subpolar North Atlantic as a response to global warming, the AMOC is expected, and may have already started, to weaken and these changes will likely have global impacts. It is therefore of considerable relevance to improve our understanding of past and future AMOC changes. My thesis tries to answer some of the open questions in this field by giving strong evidence that the AMOC has already weakened over the last century, by narrowing future projections of this slowdown and by studying the impacts on global surface warming. While there have been various studies trying to reconstruct the strength of the overturning circulation in the past, often based on model simulations in combination with observations (Jackson et al., 2016, Kanzow et al., 2010) or proxies (Frajka-Williams, 2015, Latif et al., 2006), the results so far, due to lack of direct measurements, have been inconclusive. In the first paper I build on previous work that links the anomalously low sea surface temperatures (SSTs) in the North Atlantic with the reduced meridional heat transport due to a weaker AMOC. Using the output of a high-resolution global climate model, I derive a characteristic spatial and seasonal SST fingerprint of an AMOC slowdown and an improved SST-based AMOC index. The same fingerprint is seen in the observational SSTs since the late 19th Century, giving strong evidence that since then the AMOC has slowed down. In addition, the reconstruction of the historical overturning strength with the new AMOC index agrees well with and extends the results of earlier studies as well as the direct measurements from the RAPID project and shows a strong decline of the AMOC by about 15\% (3±1 Sv) since the mid-20th Century (Caesar et al., 2018). The reconstruction of the historical overturning strength with the AMOC index enables us to weight future AMOC projections based on their skill in modeling the historical AMOC as described in the second paper of this thesis (Olson et al., 2018). Using Bayesian model averaging we considerably narrow the projections of the CMIP5 ensemble to a decrease of -4.0 Sv and -6.8 Sv between the years 1960-1999 and 2060-2099 for the RCP4.5 and RCP8.5 emission scenarios, respectively. These values fit to, yet are at the lower end of, previously published estimates. In the third paper I examine how the AMOC slowdown affects the global mean surface temperature (GMST) with a focus on how it will change the ocean heat uptake (OHC). Accounting for the effect of changes in the radiative forcing on the GMST, I test how AMOC variations correlate with the residual part of surface temperature changes in the past. I find that the correlation is positive which fits the understanding that the deep-water formation that is important in driving the AMOC cools the deep ocean and therefore warms the surface (Caesar et al., 2019). The future weakening of the overturning circulation could therefore delay global surface warming. Due to nonlinear behavior and scale specific changes it can be difficult to study the dominant processes and modes that drive climate variability. In the fourth paper we develop and test a new technique based on the wavelet multiscale correlation (WMC) similarity measure to study climate variability on different temporal and spatial scales (Agarwal et al., 2018). In a fifth contribution to my thesis this method is applied to the observed sea surface temperatures. The results reconfirm well-known relations between SST anomalies such as the El Ni{\~n}o-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO) on inter-annual and decadal timescales, respectively. They furthermore give new insights into the characteristics and origins of long-range teleconnections, for example, that the teleconnection between ENSO and Indian Ocean dipole exist mainly between the northern part of the ENSO tongue and the equatorial Indian Ocean, and provides therefore valuable knowledge about the regions that are necessary to include when modeling regional climate variability at a certain scale (Agarwal et al., 2019). In summary, my PhD thesis investigates past and future AMOC variability and its effects on global mean surface temperature by utilizing a combination of observational sea surface data and the output of historical and future climate model simulations from both the high-resolution CM2.6 model as well as the CMIP5 ensemble. It further includes the development and validation of a new method to study climate variability, that, applied to the observed sea surface temperatures, gives new insight about teleconnections in the Earth System. My findings provide evidence that the AMOC has already slowed down, will continue to do so in the future, and will impact the global mean temperature. Further impacts of an AMOC slowdown may include increased sea-level rise at the U.S. east coast (Ezer, 2015), heat extremes in Europe (Duchez et al., 2016) and increased storm activity in the North Atlantic region (Jackson et al., 2015), all of which have significant socio-economic implications.}, language = {de} } @phdthesis{Coch2019, author = {Coch, Caroline}, title = {The changing Arctic freshwater system}, school = {Universit{\"a}t Potsdam}, pages = {xi, 113, xxxvii}, year = {2019}, language = {en} } @phdthesis{vonSpecht2019, author = {von Specht, Sebastian}, title = {Likelihood - based optimization in strong-motion seismology}, school = {Universit{\"a}t Potsdam}, pages = {153}, year = {2019}, language = {en} } @phdthesis{Heinecke2018, author = {Heinecke, Liv}, title = {Environmental change in the Eastern Pamir Mountains during last 28 cal ka BP}, school = {Universit{\"a}t Potsdam}, pages = {139}, year = {2018}, language = {en} } @phdthesis{Brell2018, author = {Brell, Maximilian}, title = {Physically based fusion of airborne hyperspectral and lidar data}, school = {Universit{\"a}t Potsdam}, pages = {112}, year = {2018}, language = {en} } @phdthesis{Darmawan2018, author = {Darmawan, Herlan}, title = {Morphometric changes at the Merapi lava dome between 2012 and 2017}, school = {Universit{\"a}t Potsdam}, pages = {134}, year = {2018}, language = {en} } @phdthesis{Besendoerfer2018, author = {Besend{\"o}rfer, Christian Ren{\´e}}, title = {Innovationen im nachhaltigen Landmanagement}, school = {Universit{\"a}t Potsdam}, pages = {260}, year = {2018}, language = {de} } @phdthesis{Richter2017, author = {Richter, Nicole}, title = {Investigating hazards and the evolution of volcanic landscapes by means of terrestrial and satellite remote sensing data and modelling}, school = {Universit{\"a}t Potsdam}, pages = {169}, year = {2017}, language = {en} } @phdthesis{Wieczorek2017, author = {Wieczorek, Mareike}, title = {Stand structure patterns in the Siberian treeline under climate change}, school = {Universit{\"a}t Potsdam}, pages = {140}, year = {2017}, language = {en} } @phdthesis{Nitze2017, author = {Nitze, Ingmar}, title = {Remote sensing of rapid permafrost landscape dynamics}, school = {Universit{\"a}t Potsdam}, pages = {151}, year = {2017}, language = {en} } @phdthesis{Irrgang2017, author = {Irrgang, Anna Maria}, title = {Temporal and spatial dynamics of Arctic coastal changes and the resulting impacts: Yukon Territory, Canada}, school = {Universit{\"a}t Potsdam}, pages = {154}, year = {2017}, language = {en} } @phdthesis{Tanski2017, author = {Tanski, George}, title = {Fate of organic matter mobilized from eroding permafrost coasts}, school = {Universit{\"a}t Potsdam}, pages = {IX, 106, 57 S.}, year = {2017}, language = {en} } @phdthesis{Horn2017, author = {Horn, Juliane}, title = {A modelling framework for exploration of a multidimensional factor causing decline in honeybee health}, school = {Universit{\"a}t Potsdam}, pages = {221}, year = {2017}, language = {en} } @phdthesis{Wambura2017, author = {Wambura, Frank Joseph}, title = {Analysis of anthropogenic impacts on water resources in the Wami River basin, Tanzania}, school = {Universit{\"a}t Potsdam}, pages = {116}, year = {2017}, language = {en} } @phdthesis{Kalbe2016, author = {Kalbe, Johannes}, title = {Stepping stones hominin dispersal out of Africa}, school = {Universit{\"a}t Potsdam}, pages = {122}, year = {2016}, language = {en} } @phdthesis{Baese2016, author = {B{\"a}se, Frank}, title = {Interception loss of changing land covers in the humid tropical lowland of Latin America}, school = {Universit{\"a}t Potsdam}, pages = {ix, 85 Seiten}, year = {2016}, abstract = {Das Gebiet der feuchten Tropen ist die am st{\"a}rksten durch den Landnutzungswandel betroffene Region der Erde. Vor allem die Rodung tropischer W{\"a}lder, um Platz f{\"u}r Rinderweiden oder den Anbau von Soja zu schaffen, aber auch seit j{\"u}ngster Zeit die Bem{\"u}hungen um Wiederaufforstungen pr{\"a}gen diesen Landnutzungswandel. Dabei beeinflusst die {\"A}nderung der Vegetationsbedeckung den regionalen Wasserhaushalt auf vielf{\"a}ltige Weise. Betroffen ist unter anderem die Verdunstung von feuchten Oberfl{\"a}chen. Die so genannte Interzeptionsverdunstung bzw. der Interzeptionsverlust tr{\"a}gt erheblich zum Wasserdampfgehalt in der unteren Atmosph{\"a}re und schließlich zur Niederschlagsbildung bei. Ziele dieser Dissertation waren (1) die experimentelle Untersuchung der Interzeptionsverlustunterschiede zwischen einem nat{\"u}rlichen, tropischen Wald und einer Sojaplantage im s{\"u}dlichen Amazonasgebiet, (2) die Modellierung des Interzeptionsverlustes dieser beiden Vegetationsformen im Vergleich zu einem jungen Sekund{\"a}rwald unter dem Aspekt der Unsicherheiten bei der Ableitung notwendiger Modellparameter sowohl im S{\"u}damazonas als auch im Einzugsgebietes des Panamakanals sowie (3) die Wasserhaushaltsanalyse eines vom Landnutzungswandel gepr{\"a}gten Teileinzugsgebietes des Panamakanals in Hinblick auf die Ver{\"a}nderung der Interzeptionsverdunstung durch sich ver{\"a}ndernde Landnutzung und der {\"A}nderung der klimatischen Bedingungen. Die Messung des Interzeptionsverlustes zeigte, dass in der Hauptwachstumsphase vom Soja von dessen Oberfl{\"a}che mehr Wasserverdunstet als von der Oberfl{\"a}che des Waldes. Allerdings ist in der Jahresbilanz der Interzeptionsverlust vom Wald h{\"o}her, da diese Studie nur eine Momentaufnahme zur Zeit der vollen Vegetationsentwicklung des Sojas mit einem Zeitfenster von zwei Monaten widerspiegelt. Durch die geringere ganzj{\"a}hrige Verdunstung von den mit Soja bestandenen Fl{\"a}chen, wird hier der Niederschlag schneller dem Abfluss zugef{\"u}hrt und schell aus der Region ausgetragen. Somit tr{\"a}gt der Landnutzungswandel von Wald zu Soja zu einer mittelfristigen Reduktion des in der Region verf{\"u}gbaren Wassers bei. Die anschließende Modellierung des Interzeptionsverlustes zeigte Einerseits einen starken Einfluss der Datenqualit{\"a}t auf die Plausibilit{\"a}t der Ergebnisse und Andererseits, dass die Sensitivit{\"a}t der einzelnen Parameter zwischen den Untersuchungsgebieten variiert. Eine Schl{\"u}sselrolle nimmt die Wasserspeicherkapazit{\"a}t der Vegetationskrone ein. Dennoch ist die Evaporationsrate die treibende Gr{\"o}ße im Interzeptionsprozess, so dass von ihr die gr{\"o}ßte Unsicherheit ausgeht. Je nach verwendeter Methode zur Ableitung dieses Parameters unterscheiden sich die gewonnenen Parameterwerte erheblich. Die Wirkungsanalyse der Interzeptionsverdunstung auf den Wasserhaushalt im Wirkungsgeflecht der {\"A}nderungen von Temperatur, Niederschlag und Landnutzung im Landschaftsmosaik eines Flusseinzugsgebiets mit Hilfe eines Wasserhaushaltsmodels zeigte den Einfluss der Landnutzungs{\"a}nderung auf die Abflussbildung mittels verschiedener Landnutzungsszenarien. Die Ergebnisse belegen, dass die Landnutzungs{\"a}nderung im Gebiet nur einen geringen Einfluss auf den Jahresabfluss hat. St{\"a}rker scheint sich der gemessene Temperaturanstieg auf die Verdunstung auszuwirken. Der mit einer h{\"o}heren Temperatur einhergehende Anstieg der Transpiration und Interzeptionsverdunstung gleicht die gemessene Zunahme des Gebietsniederschlages aus, sodass keine signifikanten {\"A}nderungen im Jahresabfluss nachgewiesen werden konnten. Die Ergebnisse der drei Studien verdeutlichen den Einfluss der Landnutzung auf die Interzeptionsverdunstung. Allerdings veranschaulichten die Resultate der Wasserhaushalts-modellierung, wie sehr dieser Einfluss durch die Ver{\"a}nderung der {\"a}ußeren Rahmenbedingungen, vor allem durch den Anstieg der Temperatur, {\"u}berpr{\"a}gt werden kann. Dies belegt, dass eine einfache {\"U}bertragung der Ergebnisse zwischen den Untersuchungsgebiet nicht m{\"o}glich ist. Somit bleibt die experimentelle Erhebung von Vegetationsparametern sowie des Interzeptionsverlustes an den jeweils zu untersuchenden Standort f{\"u}r die Anwendung von Modellen unerl{\"a}sslich.}, language = {en} } @phdthesis{Stagl2016, author = {Stagl, Judith C.}, title = {Ecosystems' exposure to climate change - Modeling as support for nature conservation management}, school = {Universit{\"a}t Potsdam}, pages = {127}, year = {2016}, language = {en} } @phdthesis{Vormoor2016, author = {Vormoor, Klaus Josef}, title = {The changing role of snowmelt- and rainfall dominated floods in Norway under climate change}, school = {Universit{\"a}t Potsdam}, pages = {115}, year = {2016}, language = {en} } @phdthesis{Wolter2016, author = {Wolter, Juliane}, title = {Mid- to Late Holocene environmental dynamics on the Yukon Coastal Plain and Herschel Island (Canada) - envidence from polygonal peatlands and lake sediment}, school = {Universit{\"a}t Potsdam}, pages = {176}, year = {2016}, language = {en} } @phdthesis{Niemeyer2016, author = {Niemeyer, Bastian}, title = {Vegetation reconstruction and assessment of plant diversity at the treeline ecotone in northern Siberia}, school = {Universit{\"a}t Potsdam}, pages = {146}, year = {2016}, language = {en} } @phdthesis{Rieckh2016, author = {Rieckh, Helene}, title = {Hydropedological analysis of erosion-affected soils in a hummocky ground-moraine landscape - interactions of water flow, dissolved carbon and particle transport, grop growth, and pedogenesis}, school = {Universit{\"a}t Potsdam}, pages = {154}, year = {2016}, language = {en} } @phdthesis{Hannemann2016, author = {Hannemann, Katrin}, title = {Seismological investigation of the oceanic crust und upper mantle using an ocean bottom station array in the vicinity of the Gloria fault (easter mid Atlantic)}, school = {Universit{\"a}t Potsdam}, pages = {199}, year = {2016}, language = {en} } @phdthesis{Bierkandt2016, author = {Bierkandt, Robert}, title = {Pressure from future sea-level rise on coastal power plants: near-term extremes and long-term commitment}, school = {Universit{\"a}t Potsdam}, pages = {187}, year = {2016}, language = {en} } @phdthesis{Molkenthin2016, author = {Molkenthin, Christian}, title = {Sensitivity analysis in seismic Hazard assessment using algorithmic differentiation}, school = {Universit{\"a}t Potsdam}, pages = {114}, year = {2016}, language = {en} } @phdthesis{Emberson2016, author = {Emberson, Robert}, title = {Chemical weathering driven by bedrock landslides}, school = {Universit{\"a}t Potsdam}, pages = {221}, year = {2016}, language = {en} } @phdthesis{Ramisch2015, author = {Ramisch, Arne}, title = {Lake system development on the northern Tibetan Plateau during the last ~ 12 ka}, school = {Universit{\"a}t Potsdam}, pages = {122}, year = {2015}, language = {en} } @phdthesis{Rach2015, author = {Rach, Oliver}, title = {Qualitative and quantitative estimations of hydrological changes in western Europe during abrupt climate shifts using lipid biomarker derived stable hydrogen isotope records}, school = {Universit{\"a}t Potsdam}, pages = {217}, year = {2015}, language = {en} } @phdthesis{Mielke2015, author = {Mielke, Christian}, title = {Multi- and Hyperspectral Spaceborne Remote Sensing for Mine Waste and Mineral Deposit Characterization, new Applications to the EnMAP and Sentinel-2 Missions}, school = {Universit{\"a}t Potsdam}, pages = {140}, year = {2015}, language = {en} } @phdthesis{Luft2015, author = {Luft, Laura Charlotte}, title = {Bridging the gap between science and nature conservation practice}, school = {Universit{\"a}t Potsdam}, pages = {173}, year = {2015}, language = {en} } @phdthesis{Wang2015, author = {Wang, Rong}, title = {Late quaternary climate and environmental variability inferred from terrigenous sediment records in China and the North Pacific/Bering Sea}, school = {Universit{\"a}t Potsdam}, pages = {91}, year = {2015}, language = {en} } @phdthesis{Karo2015, author = {Karo, Nihad Majeed}, title = {Metamorphic evolution of the Northern Zagros Suture Zone (NZSZ)}, school = {Universit{\"a}t Potsdam}, pages = {127}, year = {2015}, language = {en} } @phdthesis{Abon2015, author = {Abon, Catherine Cristobal}, title = {Radar-based rainfall retrieval for flood forecasting in a meso-scale catchment}, school = {Universit{\"a}t Potsdam}, pages = {93 S.}, year = {2015}, language = {en} } @phdthesis{Kormann2015, author = {Kormann, Christoph Martin}, title = {Regional climate change effects on hydroclimatic conditions in the Alpine region}, school = {Universit{\"a}t Potsdam}, pages = {129}, year = {2015}, language = {en} } @phdthesis{Allroggen2015, author = {Allroggen, Niklas}, title = {Observation of subsurface flow from the surface : applications of ground-penetrating radar}, school = {Universit{\"a}t Potsdam}, pages = {67}, year = {2015}, language = {en} } @phdthesis{Sauma2015, author = {Sauma, Natalia Zamora}, title = {Tsunami hazard analysis in Central America with emphasis on uncertainties}, school = {Universit{\"a}t Potsdam}, pages = {184}, year = {2015}, language = {en} } @phdthesis{Cao2014, author = {Cao, Xianyong}, title = {Vegetation and climate change in eastern continental Asia during the last 22 ka inferred from pollen data synthesis}, pages = {156}, year = {2014}, language = {en} } @phdthesis{Gassmoeller2014, author = {Gaßm{\"o}ller, Ren{\´e}}, title = {The interaction of subducted slabs and plume generation zones in geodynamic models}, school = {Universit{\"a}t Potsdam}, pages = {158}, year = {2014}, language = {en} } @phdthesis{Tympel2014, author = {Tympel, Jens G{\"u}nter}, title = {Numerical modeling of the Cenozoic Pamir-Tien Shan orogeny}, pages = {168}, year = {2014}, language = {en} } @phdthesis{Borchardt2014, author = {Borchardt, Sven}, title = {Rainfall, weathering and erosion}, pages = {x, 90}, year = {2014}, language = {en} } @phdthesis{Maghsoudi2014, author = {Maghsoudi, Samira}, title = {Spatiotemporal microseismicity patterns and detection performance in mining environments}, address = {Potsdam}, pages = {104 S.}, year = {2014}, language = {en} } @phdthesis{Tian2014, author = {Tian, Fang}, title = {Vegetation and environmental changes on millennial, centennial and decadal time-scales in central Mongolia and their driving forces}, school = {Universit{\"a}t Potsdam}, pages = {139}, year = {2014}, language = {en} } @phdthesis{Buhl2013, author = {Buhl, Elmar}, title = {Brittle deformation of porous sandstone in hypervelocity impact experiments}, address = {Potsdam}, pages = {124 S.}, year = {2013}, language = {en} } @phdthesis{Serno2013, author = {Serno, Sascha}, title = {Marine productivity and eolian dust supply in the subarctic north pacific : proxy development and evaluation in marine sediments}, address = {Potsdam}, pages = {216 S.}, year = {2013}, language = {en} } @phdthesis{Arnold2013, author = {Arnold, Gabriele}, title = {Spektrale Fernerkundung der terristrischen Planetoberfl{\"a}chen von Merkur, Venus und Mars vom visuellen bis in den infraroten Wellenl{\"a}ngenbereich}, address = {Potsdam}, pages = {573 S.}, year = {2013}, language = {de} } @phdthesis{Delgado2013, author = {Delgado, Jose Miguel Martins}, title = {Explaning change in flood hazard in the Mekong river : the hypothesis of nonstationary variance}, address = {Potsdam}, pages = {X, 104 S.}, year = {2013}, language = {en} } @phdthesis{Anis2013, author = {Anis, Muhammad Rehan}, title = {Climate change effects on overland flow}, address = {Potsdam}, pages = {127 S.}, year = {2013}, language = {en} } @phdthesis{Muenzel2013, author = {M{\"u}nzel, Sandra}, title = {Aspekte der Evolution von aufgesp{\"u}hltem Abraummaterial des Platinerzbergbaus}, address = {Potsdam}, pages = {141, LX S.}, year = {2013}, language = {de} } @phdthesis{Guenther2013, author = {G{\"u}nther, Frank}, title = {Thermo-erosion of permafrost coasts in East Siberia}, address = {Potsdam}, pages = {125 S.}, year = {2013}, language = {en} } @phdthesis{Duesterhoeft2013, author = {Duesterhoeft, Erik}, title = {The impact of metamorphic processes on physical properties: a view from thermodynamiccs to geodynamics}, address = {Potsdam}, pages = {102 S.}, year = {2013}, language = {en} } @phdthesis{Pantaleo2013, author = {Pantaleo, Michele}, title = {Geothermal and deformation activity observed at volcanoes by using high resolution imaging}, address = {Potsdam}, pages = {117 S.}, year = {2013}, language = {en} } @phdthesis{Donner2013, author = {Donner, Stefanie}, title = {Seismotectonic implications for the Alborz mountains, Iran, from regional moment tensors}, address = {POtsdam}, pages = {138 S.}, year = {2013}, language = {en} } @phdthesis{Dulanya2012, author = {Dulanya, Zuze}, title = {Environmental impact on shallow-lake fisheries in Malawi : a coupled catchment-based and palaeolimnological approach}, address = {Potsdam}, pages = {100 S.}, year = {2012}, language = {en} } @phdthesis{Opitz2012, author = {Opitz, Stephan}, title = {Late Glacial to Holocene paleoenvironment on the north-eastern Tibetan Plateau inferred from lake sediments}, address = {Potsdam}, pages = {128 S.}, year = {2012}, language = {en} } @phdthesis{Waha2012, author = {Waha, Katharina}, title = {Climate change impacts on agricultural vegetation in sub-saharan africa}, address = {Potsdam}, pages = {156 S.}, year = {2012}, language = {en} } @phdthesis{Paschke2012, author = {Paschke, Marco}, title = {A highly resolved P-velocity image of the Messum igneous complex in Namibia obtained by waveform tomography}, address = {Potsdam}, pages = {117 S.}, year = {2012}, language = {en} } @phdthesis{Wittig2012, author = {Wittig, Karen}, title = {Untersuchungen zum Time - Term - Verfahren und seiner Anwendung in der Pn-Tomographie am Beispiel seismischer Feldmessungen in S{\"u}dafrika}, address = {Potsdam}, pages = {233 S.}, year = {2012}, language = {de} } @phdthesis{Langerwisch2012, author = {Langerwisch, Fanny}, title = {The Role of climate and land use change on the riverine carbon fluxes in Amazonia}, address = {Potsdam}, pages = {XII, 135 S.}, year = {2012}, language = {en} } @phdthesis{Wulf2012, author = {Wulf, Sabine}, title = {Methods and applications of tephrochronology in sedimentary archives}, address = {Potsdam}, pages = {141 S.}, year = {2012}, language = {en} } @phdthesis{Hammer2012, author = {Hammer, Conny}, title = {Automatic Tools for Seismic Monitoring Systems}, address = {Potsdam}, pages = {93 S.}, year = {2012}, language = {en} } @phdthesis{Biskaborn2012, author = {Biskaborn, Boris}, title = {Holocene environmental variability inferred from lake diatoms and sediment geochemistry in northeastern Siberia, Russia}, address = {Potsdam}, pages = {139 S.}, year = {2012}, language = {en} } @phdthesis{Ulrich2011, author = {Ulrich, Mathias}, title = {Permafrost landform studies on Earth : Implications for periglacial landscape evolution and habitability on Mars}, address = {Potsdam}, pages = {VIII, 160 S.}, year = {2011}, language = {en} } @phdthesis{Fernandoy2011, author = {Fernandoy, Francisco}, title = {Recent climate variability at the Antartica Peninsula and coastal Dronning Maud Land, based on stable water isotope data}, address = {Potsdam}, pages = {113 S.}, year = {2011}, language = {en} } @phdthesis{Fader2011, author = {Fader, Marianela}, title = {Flows of virtual land and water throught global trade of agricultural products}, address = {Potsdam}, pages = {117 S.}, year = {2011}, language = {en} } @phdthesis{vonNicolai2011, author = {von Nicolai, Christina}, title = {The interplay of salt movements and regional tectonics at the passive continental margin of the South Atlantic, Kwanza Basin}, address = {Potsdam}, pages = {134 S.}, year = {2011}, language = {en} } @phdthesis{Blaser2011, author = {Blaser, Lilian}, title = {Bayesian networks for tsunami early warning}, address = {Potsdam}, pages = {127 S.}, year = {2011}, language = {en} } @phdthesis{MenesesRioseco2011, author = {Meneses Rioseco, Ernesto}, title = {Lithopheric rheology at the Dead Sea Transform Fault constrained by thermo-mechanical modeling}, address = {Potsdam}, pages = {154 S.}, year = {2011}, language = {en} } @phdthesis{Chapligin2011, author = {Chapligin, Bernhard}, title = {From method develoment to climate reconstruction - oxygen isotope analysis of biogenic silica from Lake El'gygytgyn, NE Siberia}, address = {Potsdam}, pages = {195 S.}, year = {2011}, language = {en} } @phdthesis{Meyer2011, author = {Meyer, Sven Walter Heinrich}, title = {Entwicklung und Erprobung von methodischen Grundlagen zur Konzipierung eines Entscheidungshilfesystems f{\"u}r die Begr{\"u}ndung von Extremstandorten}, address = {Potsdam}, pages = {279 S.}, year = {2011}, language = {de} } @phdthesis{Zhang2011, author = {Zhang, Zhuodong}, title = {A regional scale study of wind erosion in the Xilingele grassland based on computational fluid dynamics}, address = {Potsdam}, pages = {143 S.}, year = {2011}, language = {en} } @phdthesis{Fritz2011, author = {Fritz, Michael}, title = {Late quaternary environmental dynamics of the western canadian artic : permafrost and lake sediment archives at the easter beringian edge}, address = {Potsdam}, pages = {119 S.}, year = {2011}, language = {en} } @phdthesis{Bulut2010, author = {Bulut, Fatih}, title = {Seismicity and fault kinematics of the North Anatolian fault zone along the 1999 Izmit rupture and its transition to the Marmara seismic gap}, pages = {VII, 98 S.}, year = {2010}, language = {en} } @phdthesis{Kuehn2010, author = {K{\"u}hn, Nicolas M.}, title = {Empirical ground-motion models for probabilistic seismic hazard analysis : a graphical model perspective}, address = {Potsdam}, pages = {125 S.}, year = {2010}, language = {en} } @phdthesis{Hoff2010, author = {Hoff, Ulrike}, title = {Freshwater diatoms as indicators for Holocene environmental- and climate changes on Kamachatka, Russia}, address = {Potsdam}, pages = {VII, 95, XXXVIII S.}, year = {2010}, language = {en} } @phdthesis{Plenkers2010, author = {Plenkers, Katrin}, title = {On the Characteristics of Mining-Induced Seismicity with Magnitudes -5