TY - THES A1 - Wenk, Sebastian T1 - Engineering formatotrophic growth in Escherichia coli N2 - To meet the demands of a growing world population while reducing carbon dioxide (CO2) emissions, it is necessary to capture CO2 and convert it into value-added compounds. In recent years, metabolic engineering of microbes has gained strong momentum as a strategy for the production of valuable chemicals. As common microbial feedstocks like glucose directly compete with human consumption, the one carbon (C1) compound formate was suggested as an alternative feedstock. Formate can be easily produced by various means including electrochemical reduction of CO2 and could serve as a feedstock for microbial production, hence presenting a novel entry point for CO2 to the biosphere and a storage option for excess electricity. Compared to the gaseous molecule CO2, formate is a highly soluble compound that can be easily handled and stored. It can serve as a carbon and energy source for natural formatotrophs, but these microbes are difficult to cultivate and engineer. In this work, I present the results of several projects that aim to establish efficient formatotrophic growth of E. coli – which cannot naturally grow on formate – via synthetic formate assimilation pathways. In the first study, I establish a workflow for growth-coupled metabolic engineering of E. coli. I demonstrate this approach by presenting an engineering scheme for the PFL-threonine cycle, a synthetic pathway for anaerobic formate assimilation in E. coli. The described methods are intended to create a standardized toolbox for engineers that aim to establish novel metabolic routes in E. coli and related organisms. The second chapter presents a study on the catalytic efficiency of C1-oxidizing enzymes in vivo. As formatotrophic growth requires generation of both energy and biomass from formate, the engineered E. coli strains need to be equipped with a highly efficient formate dehydrogenase, which provides reduction equivalents and ATP for formate assimilation. I engineered a strain that cannot generate reducing power and energy for cellular growth, when fed on acetate. Under this condition, the strain depends on the introduction of an enzymatic system for NADH regeneration, which could further produce ATP via oxidative phosphorylation. I show that the strain presents a valuable testing platform for C1-oxidizing enzymes by testing different NAD-dependent formate and methanol dehydrogenases in the energy auxotroph strain. Using this platform, several candidate enzymes with high in vivo activity, were identified and characterized as potential energy-generating systems for synthetic formatotrophic or methylotrophic growth in E. coli.   In the third chapter, I present the establishment of the serine threonine cycle (STC) – a synthetic formate assimilation pathway – in E. coli. In this pathway, formate is assimilated via formate tetrahydrofolate ligase (FtfL) from Methylobacterium extorquens (M. extorquens). The carbon from formate is attached to glycine to produce serine, which is converted into pyruvate entering central metabolism. Via the natural threonine synthesis and cleavage route, glycine is regenerated and acetyl-CoA is produced as the pathway product. I engineered several selection strains that depend on different STC modules for growth and determined key enzymes that enable high flux through threonine synthesis and cleavage. I could show that expression of an auxiliary formate dehydrogenase was required to achieve growth via threonine synthesis and cleavage on pyruvate. By overexpressing most of the pathway enzymes from the genome, and applying adaptive laboratory evolution, growth on glycine and formate was achieved, indicating the activity of the complete cycle. The fourth chapter shows the establishment of the reductive glycine pathway (rGP) – a short, linear formate assimilation route – in E. coli. As in the STC, formate is assimilated via M. extorquens FtfL. The C1 from formate is condensed with CO2 via the reverse reaction of the glycine cleavage system to produce glycine. Another carbon from formate is attached to glycine to form serine, which is assimilated into central metabolism via pyruvate. The engineered E. coli strain, expressing most of the pathway genes from the genome, can grow via the rGP with formate or methanol as a sole carbon and energy source. N2 - Um den steigenden Bedarf einer wachsenden Weltbevölkerung zu decken und gleichzeitig die CO2-Emissionen zu reduzieren, ist es notwendig, CO2 aufzufangen und zu recyceln. Durch gentechnische Veränderungen von Mikroorganismen ist es möglich diese zur Produktion wertvoller organischer Verbindungen zu nutzen. Da mikrobielle Kulturen primär mit Glucose gefüttert werden und somit mit menschlicher Nahrungsversorgung konkurrieren, wurde die C1-Verbindung Formiat als alternativer bakterieller Nährstoff vorgeschlagen.. Formiat kann durch unterschiedliche Verfahren hergestellt werden, unter anderem durch elektrochemische Reduktion von CO2. Dieses Verfahren ermöglicht das Recycling von CO2 und weiterhin eine Speichermöglichkeit für überschüssige Elektrizität. Formiat ist im Vergleich zum gasförmigen CO2 gut wasserlöslich, was den Transport und die Verwendung als mikrobiellen Nährstoff erleichtert. Natürlich vorkommende formatotrophe Mikroorganismen nutzen Formiat als Kohlenstoff- und Energiequelle. Diese lassen sich allerdings meist schwierig kultivieren und genetisch verändern. In dieser Arbeit stelle ich die Ergebnisse verschiedener Projekte vor, die gemeinsam darauf abzielen, effizientes formatotrophes Wachstum von E. coli – welches natürlicherweise nicht auf Formiat wachsen kann – mittels synthetischer Formiat-Assimilierungswege zu ermöglichen. In der ersten Studie stelle ich eine Strategie für wachstumsgekoppeltes Stoffwechsel-Engineering in E. coli vor. Ich erläutere diese Strategie anhand eines Beispiels, der schrittweisen Etablierung eines synthetischen Formiat- Assimilierungswegs, des PFL-Threonin-Zyklus. Die in diesem Kapitel beschriebenen Methoden sollen einen Leitfaden für Ingenieure bereitstellen, die neue Stoffwechselwege in E. coli und verwandten Organismen etablieren wollen. Im zweiten Kapitel stelle ich eine Studie über die katalytische Effizienz von C1-oxidierenden Enzymen vor. Da formatotrophes Wachstum sowohl die Erzeugung von Energie als auch von Biomasse aus Formiat erfordert, müssen synthetisch formatotrophe E. coli Stämme mit einer hocheffizienten Formiat-Dehydrogenase ausgestattet werden, welche Reduktionsäquivalente und ATP für die Assimilierung von Formiat liefert. Um die Effizienz verschiedener Enzyme testen und vergleichen zu können, entwickelte ich einen E. coli Stamm, der aus Acetat weder Reduktionsäquivalente noch Energie für das Zellwachstum erzeugen kann. Dieser „energie-auxotrophe“ Stamm benötigt eines zusätzlichen enzymatischen Systems zur NADH-Regenerierung, um auf Acetat wachsen zu können. Ich testete verschiedene NAD-abhängige Formiat- und Methanol-Dehydrogenasen in diesem Stamm und konnte zeigen, dass Wachstum auf Acetat durch Zugabe von Formiat oder Methanol ermöglicht wurde. Dies zeigt, dass der Stamm eine zuverlässige Testplattform für C1-oxidierende Enzyme darstellt. Unter Verwendung dieser Plattform wurden mehrere Kandidatenenzyme mit hoher in vivo-Aktivität identifiziert und als Kandidatenenzyme für synthetisches formatotrophes oder methylotrophes Wachstum in E. coli charakterisiert.   Im dritten Kapitel stelle ich die Etablierung des Serin-Threonin-Zyklus (STZ) – eines synthetischen Formiat-Assimilationswegs – in E. coli vor. In diesem Stoffwechselweg wird Formiat über die Formiat-Tetrahydrofolat-Ligase (FtfL) aus Methylobacterium extorquens (M. extorquens) assimiliert. Der Kohlenstoff aus Formiat wird an Glycin gebunden, um Serin zu produzieren, welches im nächsten Schritt in Pyruvat umgewandelt wird und so in den zentralen Kohlenstoffmetabolismus gelangt. Über den natürlichen Threonin-Synthese- und Spaltweg wird Glycin regeneriert und Acetyl-CoA als Produkt des Stoffwechselwegs generiert. Ich entwickelte mehrere E. coli Selektionsstämme, deren Wachstum von verschiedenen STZ-Modulen abhängt, und konnte Schlüsselenzyme bestimmen, die einen hohen Reaktionsfluss durch die Threonin-Synthese und -Spaltung ermöglichen. Ich konnte zeigen, dass die Expression einer Formiat-Dehydrogenase erforderlich ist, um Wachstum auf Pyruvat über Threonin zu erreichen. Durch Integration und Überexpression der meisten Enzyme des STZ auf Genomebene und Anwendung adaptiver Laborevolution wurde Wachstum auf Glycin und Formiat erreicht, was bedeutet, dass der gesamte Serin-Threonin-Zyklus in E. coli aktiv ist. Das vierte Kapitel zeigt die Etablierung des reduktiven Glycinwegs (rGW) – eines kurzen, linearen Formiat-Assimilierungswegs – in E. coli. Wie im STZ wird Formiat über M. extorquens FtfL assimiliert. Dabei wird das Kohlenstoffatom aus Formiat mit CO2 über die umgekehrte Reaktion des Glycin-Spaltungssystems zu Glycin kondensiert. Ein weiteres Kohlenstoffatom aus Formiat wird an Glycin gebunden, um Serin zu bilden, welches über Pyruvat in den Zentralstoffwechsel gelangt. Durch Expression der rGW Enzyme auf Genomebene und adaptive Laborevolution wurde ein E. coli Stamm erzeugt welcher über den rGW auf Formiat oder Methanol als einziger Kohlenstoff- und Energiequelle wachsen kann. KW - metabolic engineering KW - E. coli KW - formate assimilation KW - methanol assimilation KW - energy metabolism Y1 - 2020 ER - TY - THES A1 - Schimpf, Stefan T1 - Herkunft und Ablagerungsmilieu quartärer Sedimente im Einzugsgebiet des Heihe, NW China N2 - Der zentralasiatische Naturraum, wie er sich uns heute präsentiert, ist das Ergebnis eines Zusammenwirkens vieler verschiedener Faktoren über Jahrmillionen hinweg. Im aktuellen Kontext des Klimawandels zeigt sich jedoch, wie stark sich Stoffflüsse auch kurzfristig ändern und dabei das Gesicht der Landschaft verwandeln können. Die Gobi-Wüste in der Inneren Mongolei (China), als Teil der gleichnamigen Trockenregionen Nordwestchinas, ist aufgrund der Ausgestaltung ihrer landschaftsprägenden Elemente sowie ihrer Landschaftsdynamik, im Zusammenhang mit der Lage zum Tibet-Plateau, in den Fokus der klimageschichtlichen Grundlagenforschung gerückt. Als großes Langzeitarchiv unterschiedlichster fluvialer, lakustriner und äolischer Sedimente stellt sie eine bedeutende Lokalität zur Rekonstruktion von lokalen und regionalen Stoffflüssen dar.. Andererseits ist die Gobi-Wüste zugleich auch eine bedeutende Quelle für den überregionalen 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 & Geoökosysteme (Förderkennzeichen 03G0814), mehrere deutsch-chinesische Expeditionen in das Ejina-Becken (Innere Mongolei) und das Qilian Shan-Vorland. Im Zuge dieser Expeditionen wurden für eine Bestimmung potenzieller Sedimentquellen erstmals zahlreiche Oberflächenproben aus dem gesamten Einzugsgebiet des Heihe (schwarzer Fluss) gesammelt. Zudem wurden mit zwei Bohrungen im inneren des Ejina-Beckens, ergänzende Sedimentbohrkerne zum bestehenden Bohrkern D100 (siehe Wünnemann (2005)) abgeteuft, um weit reichende, ergänzende Informationen zur Landschaftsgeschichte und zum überregionalen Sedimenttransfer zu erhalten. Gegenstand und Ziel der vorliegenden Doktorarbeit ist die sedimentologisch-mineralogische Charakterisierung des Untersuchungsgebietes in Bezug auf potenzielle Sedimentquellen und Stoffflüsse des Ejina-Beckens sowie die Rekonstruktion der Ablagerungsgeschichte eines dort erbohrten, 19m langen Sedimentbohrkerns (GN100). Schwerpunkt ist hierbei die Klärung der Sedimentherkunft innerhalb des Bohrkerns sowie die Ausweisung von Herkunftssignalen und möglichen Sedimentquellen bzw. Sedimenttransportpfaden. Die methodische Herangehensweise basiert auf einem Multi-Proxy-Ansatz zur Charakterisierung der klastischen Sedimentfazies anhand von Geländebeobachtungen, lithologisch-granulometrischen und mineralogisch-geochemischen Analysen sowie statistischen Verfahren. Für die mineralogischen Untersuchungen der Sedimente wurde eine neue, rasterelektronenmikroskopische Methode zur automatisierten Partikelanalyse genutzt und den traditionellen Methoden gegenübergestellt. Die synoptische Betrachtung der granulometrischen, geochemischen und mineralogischen Befunde der Oberflächensedimente ergibt für das Untersuchungsgebiet ein logisches Kaskadenmodell mit immer wiederkehrenden Prozessbereichen und ähnlichen Prozesssignalen. Die umfangreichen granulometrischen Analysen deuten dabei auf abnehmende Korngrößen mit zunehmender Entfernung vom Qilian Shan hin und ermöglichen die Identifizierung von vier texturellen Signalen: den fluvialen Sanden, den Dünensanden, den Stillwassersedimenten und Stäuben. Diese Ergebnisse können als Interpretationsgrundlage für die Korngrößenanalysen des Bohrkerns genutzt werden. Somit ist es möglich, die Ablagerungsgeschichte der Bohrkernsedimente zu rekonstruieren und in Verbindung mit eigenen und literaturbasierten Datierungen in einen Gesamtkontext einzuhängen. Für das Untersuchungsgebiet werden somit vier Ablagerungsphasen ausgewiesen, die bis in die Zeit des letzten glazialen Maximums (LGM) zurückreichen. Während dieser Ablagerungsphasen kam es im Zuge unterschiedlicher Aktivitäts- und Stabilitätsphasen zu einer kontinuierlichen Progradation und Überprägung des Schwemmfächers. Eine besonders aktive Phase kann zwischen 8 ka und 4 ka BP festgestellt werden, während der es aufgrund zunehmender fluvialer Aktivitäten zu einer deutlich verstärkten Schwemmfächerdynamik gekommen zu sein scheint. In den Abschnitten davor und danach waren es vor allem äolische Prozesse, die zu einer Überprägung des Schwemmfächers geführt haben. Hinsichtlich der mineralogischen Herkunftssignale gibt es eine große Variabilität. Dies spiegelt die enorme Heterogenität der Geologie des Untersuchungsgebietes wider, wodurch die räumlichen Signale nicht sehr stark ausgeprägt sind. Dennoch, können für das Einzugsgebiet drei größere Bereiche deklariert werden, die als Herkunftsgebiet in Frage kommen. Das östliche Qilian Shan Vorland zeichnet sich dabei durch deutlich höhere Chloritgehalte als primäre Quelle für die Sedimente im Ejina-Becken aus. Sie unterscheiden sich insbesondere durch stark divergierende Chloritgehalte in der Tonmineral- und Gesamtmineralfraktion, was das östliche Qilian Shan Vorland als primäre Quelle für die Sedimente im Ejina-Becken auszeichnet. Dies steht in Zusammenhang mit den Grünschiefern, Ophioliten und Serpentiniten in diesem Bereich. Geochemisch deutet vor allem das Cr/Rb-Verhältnis eine große Variabilität innerhalb des Einzugsgebietes an. Auch hier ist es das östliche 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 Variabilität der Sedimentherkunft lässt sich in den Bohrkernsedimenten nicht so deutlich nachzeichnen. Die mineralogisch-sedimentologischen Eigenschaften der erbohrten klastischen Sedimente zeugen zwar von zwischenzeitlichen Änderungen bei der Sedimentherkunft, diese sind jedoch nicht so deutlich ausgeprägt, wie es die Quellsignale in den Oberflächensedimenten vermuten lassen. Ein Grund dafür scheint die starke Vermischung unterschiedlichster Sedimente während des Transportes zu sein. Die Kombination der Korngrößenergebnisse mit den Befunden der Gesamt- und Schwermineralogie deuten darauf hin, dass es zwischenzeitlich eine Phase mit überwiegend äolischen 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 Verhältnisse darauf hin. Der Vergleich der traditionellen Schwermineralanalyse mit der Computer-Controlled-Scanning-Electron-Microscopy (kurz: CCSEM), die eine automatisierte Partikelauswertung der Proben ermöglicht, 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 größere statistische Signifikanz des Ergebnisses im Vordergrund. Zudem können mit dieser Methode auch chemische Varietäten einiger Schwerminerale bestimmt werden, die eine noch feinere Klassifizierung und sicherere Aussagen zu einer möglichen Sedimentherkunft ermöglichen. 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 abhängen. Die Heterogenität der Geologie und die Größe des Einzugsgebietes sowie die daraus resultierende Komplexität 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 ergänzenden Bearbeitung angrenzender Untersuchungsgebiete, wie beispielsweise den Gobi-Altai im Norden oder den Beishan im Westen, sowie die Verdichtung der Oberflächenbeprobung zur feineren Auflösung von lokalen Sedimentquellen. N2 - The Central Asian natural space, as it presents itself today, is the result of a combination of many different factors over millions of years. However, in the current context of climate change it becoming obvious how strongly material fluxes can change in the short-term and thereby transform the face of the landscape. As a large long-term archive of different fluvial, lacustrine and aeolian sediments, the Gobi Desert in Inner Mongolia (China) represents a significant locality for the reconstruction of local and regional material flows as well as an important source for supra-regional dust transport due to erosion by aeolian processes. This, in connection with its location to the Tibetan Plateau, has moved the Gobi Desert into the focus of climate-historical basic research. Against this background, several German-Chinese expeditions to Ejina Basin (Inner Mongolia) and the Qilian Shan foreland were accomplished between 2011 and 2014. They were part of the BMBF joint program WTZ Central Asia - Monsoon Dynamics & Geo-Ecosystems (Grant No. 03G0814). In the course of these expeditions numerous surface samples from the entire catchment area of the Heihe (Black River) were collected for the determination of potential sediment sources. Additionally, two drillings in the interior of the Ejina Basin were conducted as a continuation of the existing drill-core D100 (see Wünnemann (2005)) and for gathering complementary information on landscape history and supra-regional sediment transfer. The goals of this doctoral thesis are a sedimentological-mineralogical characterization of the study area with regard to potential sediment sources and material fluxes of the Ejina Basin as well as the reconstruction of the sedimentation history of a 19 m sediment drill-core (GN100) drilled in the northern part of the basin. The main focus is on the clarification of the sediment provenance within the drill core as well as the designation of provenance signals and possible sediment sources or sediment transport paths. The methodological approach is based on a multi-proxy approach to characterize the clastic sedimentary facies using field observations, lithological-granulometric and mineralogical-geochemical analyses as well as statistical methods. For the mineralogical investigations of the sediments, a new scanning electron microscopic method for automated particle analysis was used and compared with traditional methods. The synoptic analysis of the granulometric, geochemical and mineralogical findings of the surface sediments result in a logical cascade model with recurring process areas and similar process signals. The results of the extensive granulometric analyses indicate decreasing grain sizes as the distance from the Qilian Shan increases and allow the identification of four textural signals: fluvial sands, dune sands, still water sediments and dusts. They can be used as the basis of interpretation for the grain size analyses of the drill core. This makes it possible to reconstruct the depositional history of the core sediments and to put them in an overall context in conjunction with own and literature-based datings. For the study area four depositional phases can be identified which date back until the time of the Last Glacial Maximum (LGM). During these depositional phases, various phases of activity and stability led to a continuous progradation and overprinting of the alluvial fan. A particularly active phase can be observed between 8 ka and 4 ka BP. During this period there seems to have been a significant increase in alluvial fan dynamics due to increasing fluvial activity. In the periods before and after mainly aeolian processes have led to an overprinting of the alluvial fan. Regarding the mineralogical provenance signals there is a great variability. This reflects the enormous geological heterogeneity of the study area, by which the spatial signals are not very pronounced. Nonetheless, within the catchment three larger areas can be declared which can be considered as possible sediment sources. These are the eastern and western foreland of the Qilian Shan mountains as wells as the Bei Shan in the west of the Ejina basin. They differ, in particular, from strongly diverging chlorite contents in the clay mineral and total mineral fraction. The eastern Qilian Shan foreland is characterized by significantly higher chlorite contents as the primary source for the sediments in the Ejina Basin. This is related to the greenschists, ophiolites and serpentinites in this area. Geochemically, the Cr/Rb-ratio in particular indicates a large variability within the catchment area. In this case its again the eastern Qilian Shan foreland which stands out from the rest of the study area with high values due to its high proportion of mafic rocks which are rich in chromites and spinels. Within the drill core sediments of GN100 the temporal but also the general variability of the sediment provenance according to the surface sediment results cannot be clearly traced. The mineralogical-sedimentological characteristics of the drilled clastic sediments exhibit meantime changes in sediment provenance. However, they are not as pronounced as the source signals within the surface sediments suggest. One reason seems to be the strong mixing of different sediments during transport. The combination of the particle size results with the results of the total and heavy mineralogy indicate that there must have been a phase in the meantime with predominantly aeolian processes.. These processes were connected with a sediment input from the Bei Shan mountains in the west. In addition to the increase in ultrastable heavy minerals such as zirconium and garnet and the decline of opaque heavy minerals, mainly present conditions point to this. The comparison of the traditional heavy mineral analysis (polarized light microscopy) with computer-controlled scanning electron microscopy (short: CCSEM) shows the clear advantage of the modern analysis method. Above all is the significant greater statistical significance of the counting results. In addition, this method can also be used to determine chemical varieties of some heavy minerals, which allows an even finer classification and more reliable conclusions about a possible sediment provenance. Furthermore, better statements can be made about the composition and the development process of the deposited sediments. This thesis shows that the sediment provenance within the study area as well as the ongoing processes partly depend strongly on local conditions. Therefore, the heterogeneity of the geology and the size of the catchment as well as the resulting complexity of the sediment genesis makes it very difficult to make exact assignments to clearly defined sediment sources. Nevertheless, the results indicate a primary input of fluvial clastic sediments of the Heihe coming from the Qilian Shan mountains. However, the findings also indicate the need to complement the study with adjacent study areas such as the Gobi Altai in the north or the Beishan in the west as well as a densification of the surface sampling for a better resolution of possible local sediment sources. KW - Heihe KW - Ejina Becken KW - Gaxun Nur KW - Schwerminerale KW - China KW - CCSEM KW - Herkunftsanalyse KW - Tonminerale KW - Heihe KW - Ejina Basin KW - Gaxun Nur KW - Heavy Minerals KW - China KW - CCSEM KW - Provenance Analysis KW - Clay Minerals Y1 - 2020 ER - TY - JOUR A1 - Omane, Paul Okyere A1 - Höhle, Barbara T1 - Acquiring syntactic variability BT - The production of Wh-questions in children and adults speaking Akan JF - Frontiers in communication N2 - This paper investigates the predictions of the Derivational Complexity Hypothesis by studying the acquisition of wh-questions in 4- and 5-year-old Akan-speaking children in an experimental approach using an elicited production and an elicited imitation task. Akan has two types of wh-question structures (wh-in-situ and wh-ex-situ questions), which allows an investigation of children’s acquisition of these two question structures and their preferences for one or the other. Our results show that adults prefer to use wh-ex-situ questions over wh-in-situ questions. The results from the children show that both age groups have the two question structures in their linguistic repertoire. However, they differ in their preferences in usage in the elicited production task: while the 5-year-olds preferred the wh-in-situ structure over the wh-ex-situ structure, the 4-year-olds showed a selective preference for the wh-in-situ structure in who-questions. These findings suggest a developmental change in wh-question preferences in Akan-learning children between 4 and 5 years of age with a so far unobserved u-shaped developmental pattern. In the elicited imitation task, all groups showed a strong tendency to maintain the structure of in-situ and ex-situ questions in repeating grammatical questions. When repairing ungrammatical ex-situ questions, structural changes to grammatical in-situ questions were hardly observed but the insertion of missing morphemes while keeping the ex-situ structure. Together, our findings provide only partial support for the Derivational Complexity Hypothesis. KW - Akan KW - wh-questions KW - wh-in-situ KW - wh-ex-situ KW - derivational complexity KW - language acquisition Y1 - 2021 U6 - https://doi.org/10.3389/fcomm.2021.604951 SN - 2297-900X VL - 2021 PB - Frontiers Media CY - Lausanne, Schweiz ER - TY - JOUR A1 - Risch, Lucie A1 - Stoll, Josefine A1 - Schomöller, Anne A1 - Engel, Tilman A1 - Mayer, Frank A1 - Cassel, Michael T1 - Intraindividual Doppler Flow Response to Exercise Differs Between Symptomatic and Asymptomatic Achilles Tendons JF - Frontiers in physiology N2 - Objective: This study investigated intraindividual differences of intratendinous blood flow (IBF) in response to running exercise in participants with Achilles tendinopathy. Design: This is a cross-sectional study. Setting: The study was conducted at the University Outpatient Clinic. Participants: Sonographic detectable intratendinous blood flow was examined in symptomatic and contralateral asymptomatic Achilles tendons of 19 participants (42 ± 13 years, 178 ± 10 cm, 76 ± 12 kg, VISA-A 75 ± 16) with clinically diagnosed unilateral Achilles tendinopathy and sonographic evident tendinosis. Intervention: IBF was assessed using Doppler ultrasound “Advanced Dynamic Flow” before (Upre) and 5, 30, 60, and 120 min (U5–U120) after a standardized submaximal constant load run. Main Outcome Measure: IBF was quantified by counting the number (n) of vessels in each tendon. Results: At Upre, IBF was higher in symptomatic compared with asymptomatic tendons [mean 6.3 (95% CI: 2.8–9.9) and 1.7 (0.4–2.9), p < 0.01]. Overall, 63% of symptomatic and 47% of asymptomatic Achilles tendons responded to exercise, whereas 16 and 11% showed persisting IBF and 21 and 42% remained avascular throughout the investigation. At U5, IBF increased in both symptomatic and asymptomatic tendons [difference to baseline: 2.4 (0.3–4.5) and 0.9 (0.5–1.4), p = 0.05]. At U30 to U120, IBF was still increased in symptomatic but not in asymptomatic tendons [mean difference to baseline: 1.9 (0.8–2.9) and 0.1 (-0.9 to 1.2), p < 0.01]. Conclusion: Irrespective of pathology, 47–63% of Achilles tendons responded to exercise with an immediate acute physiological IBF increase by an average of one to two vessels (“responders”). A higher amount of baseline IBF (approximately five vessels) and a prolonged exercise-induced IBF response found in symptomatic ATs indicate a pain-associated altered intratendinous “neovascularization.” KW - achilles tendinopathy KW - tendinosis KW - neovascularization KW - ultrasound KW - advanced dynamic flow KW - sonography Y1 - 2021 U6 - https://doi.org/10.3389/fphys.2021.617497 SN - 1664-042X VL - 12 SP - 1 EP - 8 PB - Frontiers Research Foundation CY - Lausanne, Schweiz ER - TY - JOUR A1 - Wippert, Pia-Maria A1 - Niederer, Daniel A1 - Drießlein, David A1 - Beck, Heidrun A1 - Banzer, Winfried Eberhard A1 - Schneider, Christian A1 - Schiltenwolf, Marcus A1 - Mayer, Frank T1 - Psychosocial Moderators and Mediators of Sensorimotor Exercise in Low Back Pain: A Randomized Multicenter Controlled Trial JF - Frontiers in Psychiatry N2 - The effects of exercise interventions on unspecific chronic low back pain (CLBP) have been investigated in many studies, but the results are inconclusive regarding exercise types, efficiency, and sustainability. This may be because the influence of psychosocial factors on exercise induced adaptation regarding CLBP is neglected. Therefore, this study assessed psychosocial characteristics, which moderate and mediate the effects of sensorimotor exercise on LBP. A single-blind 3-arm multicenter randomized controlled trial was conducted for 12-weeks. Three exercise groups, sensorimotor exercise (SMT), sensorimotor and behavioral training (SMT-BT), and regular routines (CG) were randomly assigned to 662 volunteers. Primary outcomes (pain intensity and disability) and psychosocial characteristics were assessed at baseline (M1) and follow-up (3/6/12/24 weeks, M2-M5). Multiple regression models were used to analyze whether psychosocial characteristics are moderators of the relationship between exercise and pain, meaning that psychosocial factors and exercise interact. Causal mediation analysis were conducted to analyze, whether psychosocial characteristics mediate the exercise effect on pain. A total of 453 participants with intermittent pain (mean age = 39.5 ± 12.2 years, f = 62%) completed the training. It was shown, that depressive symptomatology (at M4, M5), vital exhaustion (at M4), and perceived social support (at M5) are significant moderators of the relationship between exercise and the reduction of pain intensity. Further depressive mood (at M4), social-satisfaction (at M4), and anxiety (at M5 SMT) significantly moderate the exercise effect on pain disability. The amount of moderation was of clinical relevance. In contrast, there were no psychosocial variables which mediated exercise effects on pain. In conclusion it was shown, that psychosocial variables can be moderators in the relationship between sensorimotor exercise induced adaptation on CLBP which may explain conflicting results in the past regarding the merit of exercise interventions in CLBP. Results suggest further an early identification of psychosocial risk factors by diagnostic tools, which may essential support the planning of personalized exercise therapy. Level of Evidence: Level I. Clinical Trial Registration: DRKS00004977, LOE: I, MiSpEx: grant-number: 080102A/11-14. https://www.drks.de/drks_web/navigate.do?navigationId=trial.HTML&TRIAL_ID=DRKS00004977. KW - low-back-pain KW - motor-control-exercise KW - multidisciplinary-therapy KW - MiSpEx-network KW - yellow flags Y1 - 2021 U6 - https://doi.org/10.3389/fpsyt.2021.629474 SN - 1664-0640 VL - 12 SP - 1 EP - 16 PB - Frontiers Research Foundation CY - Lausanne, Schweiz ER - TY - CHAP A1 - Demske, Ulrike ED - Szczepaniak, Renata ED - Flick, Johanna T1 - The grammaticalization of the definite article in German BT - from demonstratives to weak definites T2 - Walking on the Grammaticalization Path of the Definite Article in German: Functional Main and Side Roads N2 - The present paper looks into the grammaticalization of the definite article in the history of German. Starting with the well-known emergence of the definite article from a demonstrative pronoun over the course of Old High German (750–1050), I will consider the rise of so-called weak definites in Early New High German (1350–1650) as a new piece of evidence for the grammaticalization process. Here, the subclass of possessive weak definites is of particular interest for the grammaticalization of the definite article in German, because of a word order change affecting the position of possessor phrases. As soon as the possessor systematically follows the head noun (except for proper names), we observe three alternatives for the prenominal determiner slot: it may remain empty, or it may be filled either by the indefinite or the definite article in Early New High German. In Present-Day German, the definite article is used in the unmarked case, thus pointing to a second stage in the grammaticalization process of the definite article in German, which has so far not been acknowledged in the literature. KW - grammaticalization KW - definite article KW - weak definites KW - Old High German KW - Early New High German KW - Present-Day German Y1 - 2020 SN - 978-9-027204943 SN - 978-9-027261564 SP - 43 EP - 73 PB - John Benjamins Publishing Company CY - Amsterdam ER - TY - JOUR A1 - Thonig, Richard A1 - Del Rio, Pablo A1 - Kiefer, Christoph A1 - Lazaro Touza, Lara A1 - Escribano, Gonzalo A1 - Lechon, Yolanda A1 - Spaeth, Leonhard A1 - Wolf, Ingo A1 - Lilliestam, Johan T1 - Does ideology influence the ambition level of climate and renewable energy policy? BT - Insights from four European countries JF - Energy sources, part B: economics, planning, and policy N2 - We investigate whether political ideology has an observable effect on decarbonization ambition, renewable power aims, and preferences for power system balancing technologies in four European countries. Based on the Energy Logics framework, we identify ideologically different transition strategies (state-centered, market-centered, grassroots-centered) contained in government policies and opposition party programs valid in 2019. We compare these policies and programs with citizen poll data. We find that ideology has a small effect: governments and political parties across the spectrum have similar, and relatively ambitious, decarbonization and renewables targets. This mirrors citizens' strong support for ambitious action regardless of their ideological self-description. However, whereas political positions on phasing out fossil fuel power are clear across the policy space, positions on phasing in new flexibility options to balance intermittent renewables are vague or non-existent. As parties and citizens agree on strong climate and renewable power aims, the policy ambition is likely to remain high, even if governments change. KW - political ideology KW - climate policy KW - energy policy KW - europe KW - european KW - Union KW - renewable energy KW - flexibility Y1 - 2020 U6 - https://doi.org/10.1080/15567249.2020.1811806 SN - 1556-7249 SN - 1556-7257 VL - 16 IS - 1 SP - 4 EP - 22 PB - Taylor & Francis Group CY - Philadelphia ER - TY - THES A1 - Cruz Lemus, Saul Daniel T1 - Enhancing Efficiency of Inverted Perovskite Solar Cells BT - Employing Carbon Nitride and Poly (Ionic -Liquid)s as Interlayers N2 - Carbon nitride and poly(ionic liquid)s (PILs) have been successfully applied in various fields of materials science owing to their outstanding properties. This thesis aims at the successful application of these polymers as innovative materials in the interfaces of hybrid organic–inorganic perovskite solar cells. A critical problem in harnessing the full thermodynamic potential of halide perovskites in solar cells is the design and modification of interfaces to reduce carrier recombination. Therefore, the interface must be properly studied and improved. This work investigated the effect of applying carbon nitride and PILs on a perovskite surface on the device performance. The facile synthetic method for modifying carbon nitride with vinyl thiazole and barbituric acid (CMB-vTA) yields 2.3 nm layers when solution processing is performed using isopropanol. The nanosheets were applied as a metal-free electron transport layer in inverted perovskite solar cells. The application of carbon nitride layers (CMB-vTA) resulted in negligible current-voltage hysteresis with a high open circuit voltage (Voc) of 1.1 V and a short-circuit current (Jsc) of 20.28 mA cm-2, which afforded efficiencies of up to 17%. Thus, the successful implementation of a carbon nitride-based structure enabled good charge extraction with minimized interface recombination between the perovskite and PCBM. Similarly, PILs represent a new strategy of interfacial modification using an ionic polymer in an n-i-p perovskite architecture.. The application of PILs as an interfacial modifier resulted in solar cell devices with an extraordinarily high efficiency of 21.8% and a Voc of 1.17 V. The implementation reduced non-radiative recombination at the perovskite surface through defect passivation. Finally, our work proposes a novel method to efficiently suppress non-radiative charge recombination using the unexplored properties of carbon nitride and PILs in the solar cell field. Additionally, the method for interfacial modification has general applicability because of the simplicity of the post-treatment approach, and therefore has potential applicability in other solar cells. Thus, this work opens the door to a new class of materials to be implemented. Y1 - 2020 ER - TY - JOUR A1 - Tofelde, Stefanie A1 - Bernhardt, Anne A1 - Guerit, Laure A1 - Romans, Brian W. T1 - Times Associated With Source-to-Sink Propagation of Environmental Signals During Landscape Transience JF - Frontiers in Earth Science N2 - Sediment archives in the terrestrial and marine realm are regularly analyzed to infer changes in climate, tectonic, or anthropogenic boundary conditions of the past. However, contradictory observations have been made regarding whether short period events are faithfully preserved in stratigraphic archives; for instance, in marine sediments offshore large river systems. On the one hand, short period events are hypothesized to be non-detectable in the signature of terrestrially derived sediments due to buffering during sediment transport along large river systems. On the other hand, several studies have detected signals of short period events in marine records offshore large river systems. We propose that this apparent discrepancy is related to the lack of a differentiation between different types of signals and the lack of distinction between river response times and signal propagation times. In this review, we (1) expand the definition of the term ‘signal’ and group signals in sub-categories related to hydraulic grain size characteristics, (2) clarify the different types of ‘times’ and suggest a precise and consistent terminology for future use, and (3) compile and discuss factors influencing the times of signal transfer along sediment routing systems and how those times vary with hydraulic grain size characteristics. Unraveling different types of signals and distinctive time periods related to signal propagation addresses the discrepancies mentioned above and allows a more comprehensive exploration of event preservation in stratigraphy – a prerequisite for reliable environmental reconstructions from terrestrially derived sedimentary records. KW - signal propagation KW - landscape transience KW - source-to-sink KW - stratigraphy KW - response time Y1 - 2021 U6 - https://doi.org/10.3389/feart.2021.628315 SN - 2296-6463 VL - 9 SP - 1 EP - 26 PB - Frontiers Media CY - Lausanne, Schweiz ER - TY - JOUR A1 - Granacher, Urs A1 - Nobari, Hadi A1 - Ruivo Alves, Ana A1 - Clemente, Filipe Manuel A1 - Pérez-Gómez, Jorge A1 - Clark, Cain Craig Truman A1 - Zouhal, Hassane T1 - Associations Between Variations in Accumulated Workload and Physiological Variables in Young Male Soccer Players Over the Course of a Season JF - Frontiers in physiology N2 - This study sought to analyze the relationship between in-season training workload with changes in aerobic power (VO2max), maximum and resting heart rate (HRmax and HRrest), linear sprint medium (LSM), and short test (LSS), in soccer players younger than 16 years (under-16 soccer players). We additionally aimed to explain changes in fitness levels during the in-season through regression models, considering accumulated load, baseline levels, and peak height velocity (PHV) as predictors. Twenty-three male sub-elite soccer players aged 15.5 ± 0.2 years (PHV: 13.6 ± 0.4 years; body height: 172.7 ± 4.2 cm; body mass: 61.3 ± 5.6 kg; body fat: 13.7% ± 3.9%; VO2max: 48.4 ± 2.6 mL⋅kg–1⋅min–1), were tested three times across the season (i.e., early-season (EaS), mid-season (MiS), and end-season (EnS) for VO2max, HRmax, LSM, and LSS. Aerobic and speed variables gradually improved over the season and had a strong association with PHV. Moreover, the HRmax demonstrated improvements from EaS to EnS; however, this was more evident in the intermediate period (from EaS to MiS) and had a strong association with VO2max. Regression analysis showed significant predictions for VO2max [F(2, 20) = 8.18, p ≤ 0.001] with an R2 of 0.45. In conclusion, the meaningful variation of youth players’ fitness levels can be observed across the season, and such changes can be partially explained by the load imposed. KW - internal load KW - heart rate KW - linear sprint KW - aerobic power KW - football Y1 - 2021 U6 - https://doi.org/10.3389/fphys.2021.638180 SN - 1664-042X VL - 12 SP - 1 EP - 12 PB - Frontiers Research Foundation CY - Lausanne, Schweiz ER -