TY - THES A1 - Raschke, Stefanie T1 - Characterization of selenium and copper in cell systems of the neurovascular unit T1 - Charakterisierung von Selen und Kupfer in Zellsystemen der neurovaskulären Einheit N2 - The trace elements, selenium (Se) and copper (Cu) play an important role in maintaining normal brain function. Since they have essential functions as cofactors of enzymes or structural components of proteins, an optimal supply as well as a well-defined homeostatic regulation are crucial. Disturbances in trace element homeostasis affect the health status and contribute to the incidence and severity of various diseases. The brain in particular is vulnerable to oxidative stress due to its extensive oxygen consumption and high energy turnover, among other factors. As components of a number of antioxidant enzymes, both elements are involved in redox homeostasis. However, high concentrations are also associated with the occurrence of oxidative stress, which can induce cellular damage. Especially high Cu concentrations in some brain areas are associated with the development and progression of neurodegenerative diseases such as Alzheimer's disease (AD). In contrast, reduced Se levels were measured in brains of AD patients. The opposing behavior of Cu and Se renders the study of these two trace elements as well as the interactions between them being particularly relevant and addressed in this work. N2 - Die Spurenelemente Selen (Se) und Kupfer (Cu) spielen eine wichtige Rolle bei der Aufrechterhaltung einer normalen Ge¬hirnfunktion. Da sie wesentliche Funktionen als Cofaktoren von Enzymen oder Strukturbestandteile von Proteinen haben, sind eine optimale Versorgung sowie eine genau definierte homöostatische Regulierung von entscheidender Bedeutung. Störungen der Spurenelement-homöostase beeinträchtigen den Gesund¬heitszustand und tragen zum Auftreten und zur Schwere verschiedener Krankheiten bei. Insbesondere das Gehirn ist aufgrund seines hohen Sauerstoffverbrauchs und seines hohen Energieumsatzes anfällig für oxi¬dativen Stress. Als Bestandteile einer Reihe von antioxidativen Enzymen sind beide Elemente an der Redox-Homöostase beteiligt. Hohe Konzentrationen werden jedoch auch mit dem Auftreten von oxidati¬vem Stress in Verbindung gebracht, der zu Zellschäden führen kann. Besonders hohe Cu-Konzentrationen in einigen Hirnregionen werden mit der Entwicklung und der Progression neurodegenerativer Erkran¬kungen wie Alzheimer in Verbindung gebracht. Im Gegensatz dazu wurden in den Gehirnen von Alzheimer-Patienten geringere Se-Konzentrationen gemessen. Das gegensätzliche Verhalten von Cu und Se verdeutlicht die Relevanz der Untersuchung dieser beiden Spurenelemente sowie deren Wechselwirkungen und wird in dieser Arbeit thematisiert. KW - selenium KW - copper KW - Selen KW - Kupfer KW - Blut-Hirn-Schranke KW - Neuronen KW - Astrozyten KW - blood-brain barrier KW - neurons KW - astrocytes Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-603666 ER - TY - THES A1 - Stoltnow, Malte T1 - Magmatic-hydrothermal processes along the porphyry to epithermal transition T1 - Magmatisch-hydrothermale Prozesse entlang des porphyrisch-epithermalen Übergangs N2 - Magmatic-hydrothermal systems form a variety of ore deposits at different proximities to upper-crustal hydrous magma chambers, ranging from greisenization in the roof zone of the intrusion, porphyry mineralization at intermediate depths to epithermal vein deposits near the surface. The physical transport processes and chemical precipitation mechanisms vary between deposit types and are often still debated. The majority of magmatic-hydrothermal ore deposits are located along the Pacific Ring of Fire, whose eastern part is characterized by the Mesozoic to Cenozoic orogenic belts of the western North and South Americas, namely the American Cordillera. Major magmatic-hydrothermal ore deposits along the American Cordillera include (i) porphyry Cu(-Mo-Au) deposits (along the western cordilleras of Mexico, the western U.S., Canada, Chile, Peru, and Argentina); (ii) Climax- (and sub−) type Mo deposits (Colorado Mineral Belt and northern New Mexico); and (iii) porphyry and IS-type epithermal Sn(-W-Ag) deposits of the Central Andean Tin Belt (Bolivia, Peru and northern Argentina). The individual studies presented in this thesis primarily focus on the formation of different styles of mineralization located at different proximities to the intrusion in magmatic-hydrothermal systems along the American Cordillera. This includes (i) two individual geochemical studies on the Sweet Home Mine in the Colorado Mineral Belt (potential endmember of peripheral Climax-type mineralization); (ii) one numerical modeling study setup in a generic porphyry Cu-environment; and (iii) a numerical modeling study on the Central Andean Tin Belt-type Pirquitas Mine in NW Argentina. Microthermometric data of fluid inclusions trapped in greisen quartz and fluorite from the Sweet Home Mine (Detroit City Portal) suggest that the early-stage mineralization precipitated from low- to medium-salinity (1.5-11.5 wt.% equiv. NaCl), CO2-bearing fluids at temperatures between 360 and 415°C and at depths of at least 3.5 km. Stable isotope and noble gas isotope data indicate that greisen formation and base metal mineralization at the Sweet Home Mine was related to fluids of different origins. Early magmatic fluids were the principal source for mantle-derived volatiles (CO2, H2S/SO2, noble gases), which subsequently mixed with significant amounts of heated meteoric water. Mixing of magmatic fluids with meteoric water is constrained by δ2Hw-δ18Ow relationships of fluid inclusions. The deep hydrothermal mineralization at the Sweet Home Mine shows features similar to deep hydrothermal vein mineralization at Climax-type Mo deposits or on their periphery. This suggests that fluid migration and the deposition of ore and gangue minerals in the Sweet Home Mine was triggered by a deep-seated magmatic intrusion. The second study on the Sweet Home Mine presents Re-Os molybdenite ages of 65.86±0.30 Ma from a Mo-mineralized major normal fault, namely the Contact Structure, and multimineral Rb-Sr isochron ages of 26.26±0.38 Ma and 25.3±3.0 Ma from gangue minerals in greisen assemblages. The age data imply that mineralization at the Sweet Home Mine formed in two separate events: Late Cretaceous (Laramide-related) and Oligocene (Rio Grande Rift-related). Thus, the age of Mo mineralization at the Sweet Home Mine clearly predates that of the Oligocene Climax-type deposits elsewhere in the Colorado Mineral Belt. The Re-Os and Rb-Sr ages also constrain the age of the latest deformation along the Contact Structure to between 62.77±0.50 Ma and 26.26±0.38 Ma, which was employed and/or crosscut by Late Cretaceous and Oligocene fluids. Along the Contact Structure Late Cretaceous molybdenite is spatially associated with Oligocene minerals in the same vein system, a feature that precludes molybdenite recrystallization or reprecipitation by Oligocene ore fluids. Ore precipitation in porphyry copper systems is generally characterized by metal zoning (Cu-Mo to Zn-Pb-Ag), which is suggested to be variably related to solubility decreases during fluid cooling, fluid-rock interactions, partitioning during fluid phase separation and mixing with external fluids. The numerical modeling study setup in a generic porphyry Cu-environment presents new advances of a numerical process model by considering published constraints on the temperature- and salinity-dependent solubility of Cu, Pb and Zn in the ore fluid. This study investigates the roles of vapor-brine separation, halite saturation, initial metal contents, fluid mixing, and remobilization as first-order controls of the physical hydrology on ore formation. The results show that the magmatic vapor and brine phases ascend with different residence times but as miscible fluid mixtures, with salinity increases generating metal-undersaturated bulk fluids. The release rates of magmatic fluids affect the location of the thermohaline fronts, leading to contrasting mechanisms for ore precipitation: higher rates result in halite saturation without significant metal zoning, lower rates produce zoned ore shells due to mixing with meteoric water. Varying metal contents can affect the order of the final metal precipitation sequence. Redissolution of precipitated metals results in zoned ore shell patterns in more peripheral locations and also decouples halite saturation from ore precipitation. The epithermal Pirquitas Sn-Ag-Pb-Zn mine in NW Argentina is hosted in a domain of metamorphosed sediments without geological evidence for volcanic activity within a distance of about 10 km from the deposit. However, recent geochemical studies of ore-stage fluid inclusions indicate a significant contribution of magmatic volatiles. This study tested different formation models by applying an existing numerical process model for porphyry-epithermal systems with a magmatic intrusion located either at a distance of about 10 km underneath the nearest active volcano or hidden underneath the deposit. The results show that the migration of the ore fluid over a 10-km distance results in metal precipitation by cooling before the deposit site is reached. In contrast, simulations with a hidden magmatic intrusion beneath the Pirquitas deposit are in line with field observations, which include mineralized hydrothermal breccias in the deposit area. N2 - Magmatisch-hydrothermale Systeme bilden eine Vielzahl von Erzlagerstätten in unterschiedlicher Entfernung zu wasserhaltigen Magmakammern in der oberen Erdkruste, von der Greisenbildung in der Dachzone der Intrusion über die Porphyrmineralisierung in mittleren Tiefen bis hin zu epithermalen Ganglagerstätten nahe der Erdoberfläche. Die physikalischen Transportprozesse und chemischen Ausfällungsmechanismen variieren zwischen den verschiedenen Lagerstättentypen und werden immer noch häufig diskutiert. Die meisten magmatisch-hydrothermalen Erzlagerstätten befinden sich entlang des Pazifischen Feuerrings, dessen östlicher Teil durch die mesozoischen bis känozoischen orogenen Gürtel des westlichen Nord- und Südamerikas, zusammen die Amerikanische Kordillere, vertreten ist. Zu den wichtigsten magmatisch-hydrothermalen Erzlagerstätten entlang der Amerikanischen Kordillere gehören (i) Cu(-Mo-Au)-Porphyrlagerstätten (entlang der westlichen Kordilleren Mexikos, der westlichen USA, Kanadas, Chiles, Perus und Argentiniens); (ii) Mo-Lagerstätten vom Climax- (und Sub-)Typ (Colorado Mineral Belt und nördliches New Mexico); und (iii) porphyrische und epithermale Sn(-W-Ag)-Lagerstätten vom IS-Typ des Zentralandinen-Zinngürtels (Bolivien, Peru und Nordargentinien). Die einzelnen Studien dieser Arbeit konzentrieren sich in erster Linie auf die Bildung verschiedener Vererzungsstypen, die sich in unterschiedlicher Entfernung zur Intrusion in magmatisch-hydrothermalen Systemen entlang der amerikanischen Kordillere befinden. Dazu gehören (i) zwei geochemische Einzelstudien über die Sweet Home-Mine im Colorado Mineral Belt (potenzielles Endglied der peripheren Mineralisierung des Climax-Typs); (ii) eine numerische Modellierungsstudie in einem generischen Cu-Porphyr-Setup; und (iii) eine numerische Modellierungsstudie über die Pirquitas-Mine des Zentralandinen-Zinn-Typs in Nordwest-Argentinien. Mikrothermometrische Daten von Fluideinschlüssen, die in Greisenquarz und -fluorit aus der Sweet Home-Mine (Detroit City Portal) eingeschlossen sind, deuten darauf hin, dass die Mineralisierung im Frühstadium aus CO2-haltigen Fluiden mit niedrigem bis mittlerem Salzgehalt (1,5-11,5 Gew.-% NaCl-Äquivalent) bei Temperaturen zwischen 360 und 415 °C und in einer Tiefe von mindestens 3,5 km ausgefällt wurde. Daten zu stabilen Isotopen und Edelgasisotopen zeigen, dass die Greisenbildung und die Buntmetallvererzung in der Sweet Home-Mine mit Fluiden unterschiedlichen Ursprungs in Verbindung stehen. Frühe magmatische Fluide waren die Hauptquelle für aus dem Mantel stammende Volatile (CO2, H2S/SO2, Edelgase), die sich anschließend mit erheblichen Mengen erhitzten meteorischen Wassers vermischten. Die Vermischung von magmatischen Fluiden mit meteorischem Wasser wird durch die Zusammenhänge von δ2Hw-δ18Ow der Fluideinschlüsse belegt. Die tiefe hydrothermale Vererzung in der Sweet Home-Mine weist ähnliche Merkmale auf wie die tiefe hydrothermale Gangvererzung in Mo-Lagerstätten vom Climax-Typ oder in deren Peripherie. Dies deutet darauf hin, dass die Fluidmigration und die Ausfällung von Erz und Gangmineralen in der Sweet Home-Mine durch eine tief sitzende magmatische Intrusion angeregt wurde. Die zweite Studie über die Sweet Home Mine präsentiert ein Re-Os-Molybdänit-Alter von 65,86±0,30 Ma aus einer Mo-vererzten Abschiebung, namentlich der Contact Structure, und ein multimineralisches Rb-Sr-Isochronen-Alter von 26,26±0,38 Ma und 25,3±3,0 Ma von Gangmineralen in Greisenvergesellschaftungen. Die Altersdaten deuten darauf hin, dass die Vererzungen in der Sweet Home Mine während zweier separater Ereignisse entstand: In der späten Kreidezeit (im Zusammenhang mit der Laramidischen Orogenese) und im Oligozän (im Zusammenhang mit dem Rio Grande Rift). Das Alter der Mo-Vererzung in der Sweet Home Mine liegt demnach eindeutig vor dem der oligozänen Climax-Lagerstätten anderswo im Colorado Mineral Belt. Die Re-Os- und Rb-Sr-Alter grenzen auch das Alter der jüngsten Deformation entlang der Contact Structure, die von spätkreidezeitlichen und oligozänen Fluiden genutzt und/oder geschnitten wurde, auf 62,77±0,50 Ma und 26,26±0,38 Ma ein. Entlang der Contact Structure ist spätkreidezeitlicher Molybdänit räumlich mit Mineralen aus dem Oligozän in demselben Gangsystem vergesellschaftet, was eine Rekristallisierung oder Ausfällung von Molybdänit durch oligozäne Fluide ausschließt. Die Erzausfällung in porphyrischen Kupfersystemen ist im Allgemeinen durch eine Metallzonierung (Cu-Mo bis Zn-Pb-Ag) gekennzeichnet, die vermutlich mit der Abnahme der Löslichkeit während der Fluidabkühlung, den Wechselwirkungen zwischen Fluid und Gestein, der Partitionierung während der Phasenseparation des Fluids und der Mischung mit externen Fluiden in Zusammenhang steht. Die numerische Modellierung, die in einer generischen Porphyr-Cu-Umgebung durchgeführt wurde, stellt neue Fortschritte eines numerischen Prozessmodells dar, indem sie veröffentlichte Randbedingungen für die temperatur- und salinitätsabhängige Löslichkeit von Cu, Pb und Zn im Erzfluid berücksichtigt. Diese Studie untersucht die Rolle der Dampf-Sole-Separation, der Halitsättigung, des anfänglichen Metallgehalts, der Fluidmischung und der Remobilisierung als Einflussfaktoren erster Ordnung der physikalischen Hydrologie auf die Erzbildung. Die Ergebnisse zeigen, dass die magmatischen Dampf- und Solephasen mit unterschiedlichen Verweilzeiten, aber als mischbare Fluide aufsteigen, wobei eine Erhöhung des Salzgehalts zu einem metall-ungesättigten Gesamtfluid führt. Die Freisetzungsraten der magmatischen Fluide wirken sich auf die Lage der thermohalinen Fronten aus, was zu widersprüchlichen Mechanismen für die Erzausfällung führt: Höhere Raten führen zu einer Halitsättigung ohne signifikante Metallzonierung, niedrigere Raten erzeugen zonierte Erzschalen aufgrund der Mischung mit meteorischem Wasser. Unterschiedliche Metallgehalte können sich auf die Reihenfolge der endgültigen Metallausfällung auswirken. Die Wiederauflösung bereits ausgefällter Metalle führt zu zonierten Erzschalenmustern in periphereren Bereichen und entkoppelt auch die Halitsättigung von der Erzausfällung. Die epithermale Pirquitas Sn-Ag-Pb-Zn-Mine im Nordwesten Argentiniens befindet sich in einem Bereich metamorphisierter Sedimente ohne geologische Hinweise auf vulkanische Aktivitäten in einer Entfernung von etwa 10 km zur Lagerstätte. Jüngste geochemische Untersuchungen von Fluideinschlüssen im Erzstadium deuten jedoch auf einen bedeutenden Beitrag von magmatischen Volatilen hin. In dieser Studie wurden verschiedene Entstehungsmodelle getestet, indem ein bestehendes numerisches Prozessmodell für porphyrisch-epithermale Systeme mit einer magmatischen Intrusion angewandt wurde, die sich entweder in einer Entfernung von etwa 10 km unterhalb des nächstgelegenen aktiven Vulkans oder verborgen unterhalb der Lagerstätte befindet. Die Ergebnisse zeigen, dass die Migration der Erzflüssigkeit über eine Entfernung von 10 km zu einer Metallausfällung durch Abkühlung führt, bevor die Lagerstätte erreicht wird. Im Gegensatz dazu stimmen die Simulationen mit einer verborgenen magmatischen Intrusion unter der Pirquitas-Lagerstätte mit den Feldbeobachtungen überein, die mineralisierte hydrothermale Brekzien im Lagerstättenbereich umfassen. KW - magmatic KW - hydrothermal KW - ore KW - deposits KW - copper KW - lead KW - zinc KW - molybdenum KW - numerical KW - modeling KW - Sweet KW - Home KW - Pirquitas KW - Colorado KW - Argentina KW - Argentinien KW - Colorado KW - Home KW - Pirquitas KW - Sweet KW - Kupfer KW - Lagerstätte KW - hydrothermal KW - Blei KW - magmatisch KW - Modellierung KW - Molybdän KW - numerisch KW - Erz KW - Zink Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-611402 ER - TY - THES A1 - Brinkmann, Pia T1 - Laserinduzierte Breakdownspektroskopie zur qualitativen und quantitativen Bestimmung von Elementgehalten in geologischen Proben mittels multivariater Analysemethoden am Beispiel von Kupfer und ausgewählten Seltenen Erden N2 - Ein schonender Umgang mit den Ressourcen und der Umwelt ist wesentlicher Bestandteil des modernen Bergbaus sowie der zukünftigen Versorgung unserer Gesellschaft mit essentiellen Rohstoffen. Die vorliegende Arbeit beschäftigt sich mit der Entwicklung analytischer Strategien, die durch eine exakte und schnelle Vor-Ort-Analyse den technisch-praktischen Anforderungen des Bergbauprozesses gerecht werden und somit zu einer gezielten und nachhaltigen Nutzung von Rohstofflagerstätten beitragen. Die Analysen basieren auf den spektroskopischen Daten, die mittels der laserinduzierten Breakdownspektroskopie (LIBS) erhalten und mittels multivariater Datenanalyse ausgewertet werden. Die LIB-Spektroskopie ist eine vielversprechende Technik für diese Aufgabe. Ihre Attraktivität machen insbesondere die Möglichkeiten aus, Feldproben vor Ort ohne Probennahme oder ‑vorbereitung messen zu können, aber auch die Detektierbarkeit sämtlicher Elemente des Periodensystems und die Unabhängigkeit vom Aggregatzustand. In Kombination mit multivariater Datenanalyse kann eine schnelle Datenverarbeitung erfolgen, die Aussagen zur qualitativen Elementzusammensetzung der untersuchten Proben erlaubt. Mit dem Ziel die Verteilung der Elementgehalte in einer Lagerstätte zu ermitteln, werden in dieser Arbeit Kalibrierungs- und Quantifizierungsstrategien evaluiert. Für die Charakterisierung von Matrixeffekten und zur Klassifizierung von Mineralen werden explorative Datenanalysemethoden angewendet. Die spektroskopischen Untersuchungen erfolgen an Böden und Gesteinen sowie an Mineralen, die Kupfer oder Seltene Erdelemente beinhalten und aus verschiedenen Lagerstätten bzw. von unterschiedlichen Agrarflächen stammen. Für die Entwicklung einer Kalibrierungsstrategie wurden sowohl synthetische als auch Feldproben von zwei verschiedenen Agrarflächen mittels LIBS analysiert. Anhand der Beispielanalyten Calcium, Eisen und Magnesium erfolgte die auf uni- und multivariaten Methoden beruhende Evaluierung verschiedener Kalibrierungsmethoden. Grundlagen der Quantifizierungsstrategien sind die multivariaten Analysemethoden der partiellen Regression der kleinsten Quadrate (PLSR, von engl.: partial least squares regression) und der Intervall PLSR (iPLSR, von engl.: interval PLSR), die das gesamte detektierte Spektrum oder Teilspektren in der Analyse berücksichtigen. Der Untersuchung liegen synthetische sowie Feldproben von Kupfermineralen zugrunde als auch solche die Seltene Erdelemente beinhalten. Die Proben stammen aus verschiedenen Lagerstätten und weisen unterschiedliche Begleitmatrices auf. Mittels der explorativen Datenanalyse erfolgte die Charakterisierung dieser Begleitmatrices. Die dafür angewendete Hauptkomponentenanalyse gruppiert Daten anhand von Unterschieden und Regelmäßigkeiten. Dies erlaubt Aussagen über Gemeinsamkeiten und Unterschiede der untersuchten Proben im Bezug auf ihre Herkunft, chemische Zusammensetzung oder lokal bedingte Ausprägungen. Abschließend erfolgte die Klassifizierung kupferhaltiger Minerale auf Basis der nicht-negativen Tensorfaktorisierung. Diese Methode wurde mit dem Ziel verwendet, unbekannte Proben aufgrund ihrer Eigenschaften in Klassen einzuteilen. Die Verknüpfung von LIBS und multivariater Datenanalyse bietet die Möglichkeit durch eine Analyse vor Ort auf eine Probennahme und die entsprechende Laboranalytik weitestgehend zu verzichten und kann somit zum Umweltschutz sowie einer Schonung der natürlichen Ressourcen bei der Prospektion und Exploration von neuen Erzgängen und Lagerstätten beitragen. Die Verteilung von Elementgehalten der untersuchten Gebiete ermöglicht zudem einen gezielten Abbau und damit eine effiziente Nutzung der mineralischen Rohstoffe. N2 - The sustainable use of resources and the environment is an important part of modern mining and the supply of our society with essential raw materials in the future. The present work focuses on the development of analytical strategies that address the technical-practical requirements of the mining process through accurate and rapid on-site analysis, thus contributing to the targeted and sustainable use of raw material deposits. The analyses are based on spectroscopic data obtained by laser-induced breakdown spectroscopy (LIBS) and evaluated by multivariate data analysis. LIB spectroscopy is a promising technique for this task. Its advantages are in particular the possibility to measure field samples on site without sample collection or preparation, but also the detectability of all elements of the periodic table and the independence of the state of matter. In combination with multivariate data analysis, rapid data processing can be performed, allowing statements to be made on the qualitative elemental composition of the samples investigated. With the goal of determining the distribution of elemental contents in a deposit, calibration and quantification strategies are evaluated in this work. Exploratory data analysis methods are used to characterize matrix effects and to classify minerals. Spectroscopic studies are performed on soils and rocks as well as on minerals containing copper or rare earth elements originating from different deposits or from different agricultural sites. To develop a calibration strategy, both synthetic and field samples from two different agricultural sites were analyzed using LIBS. Using calcium, iron and magnesium as example analytes, the evaluation of different calibration methods based on univariate and multivariate methods was performed. Basics of the quantification strategies are the multivariate analysis methods of partial least squares regression (PLSR) and interval PLSR (iPLSR), which consider the whole detected spectrum or partial spectra in the analysis. The investigation is based on synthetic and field samples of copper minerals as well as those containing rare earth elements. The samples are from different deposits and have varying accompanying matrices. Exploratory data analysis was used to characterize these accompanying matrices. The principal component analysis used for this purpose groups data on the basis of differences and regularities. This allows conclusions to be drawn about similarities and differences between the samples examined in terms of their origin, chemical composition or locally determined characteristics. Finally, the classification of copper-bearing minerals was based on non-negative tensor factorization. This method was used with the aim of classifying unknown samples based on their properties. The combination method of LIBS and multivariate data analysis offers the possibility to avoid sampling and the corresponding laboratory analysis as far as possible by an on-site analysis and can thus contribute to environmental protection as well as to a conservation of natural resources during the prospection and exploration of new ore veins and deposits. The distribution of element contents of the investigated areas also enables a precise mining and thus an efficient utilization of the mineral raw materials. KW - LIBS KW - laserinduzierte Breakdownspektroskopie KW - Seltene Erdelemente KW - Kupfer KW - PCA KW - PLSR KW - NTF KW - copper KW - LIBS KW - NTF KW - PCA KW - PLSR KW - rare earth elements KW - laser induced breakdown spectroscopy Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-572128 ER - TY - JOUR A1 - Schwarze, Thomas A1 - Sperlich, Eric A1 - Müller, Thomas A1 - Kelling, Alexandra A1 - Holdt, Hans-Jürgen T1 - Synthesis efforts of acyclic bis(monoalkylamino)maleonitriles and macrocyclic bis(dialkylamino)maleonitriles as fluorescent probes for cations and a new colorimetric copper(II) chemodosimeter JF - Helvetica chimica acta N2 - In this article, we report on the synthesis of acyclic bis(monoalkylamino)maleonitriles and on the intended synthesis of macrocyclic bis(dialkylamino)maleonitriles to get fluorescent probes for cations. During our efforts to synthesize macrocyclic bis(dialkylamino)maleonitriles, we were only able to isolate macrocyclic bis(dialkylamino)-fumaronitriles. The synthesis of macrocyclic bis(dialkylamino)maleonitriles is challenging, due to the fact that bis-(dialkylamino)fumaronitriles are thermodynamically more stable than the corresponding bis(dialkylamino)-maleonitriles. Further, it turned out that the acyclic bis(monoalkylamino)maleonitriles and macrocyclic bis-(dialkylamino)fumaronitriles are no suitable tools to detect cations by a strong fluorescence enhancement. Further, only the bis(monoalkylamino)maleonitriles, which are bearing a 2-pyridyl unit as an additional complexing unit, are able to selectively recognize copper(II) by a color change from yellow to red. KW - copper KW - fumaronitrile KW - ligands KW - macrocycles KW - maleonitrile Y1 - 2021 U6 - https://doi.org/10.1002/hlca.202100028 SN - 1522-2675 VL - 104 IS - 6 SP - e2100028 PB - Wiley-VCH CY - Weinheim ER - TY - GEN A1 - Witt, Barbara A1 - Schaumlöffel, Dirk A1 - Schaumlöffel, Dirk A1 - Schwerdtle, Tanja T1 - Subcellular Localization of Copper BT - Cellular Bioimaging with Focus on Neurological Disorders T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - As an essential trace element, copper plays a pivotal role in physiological body functions. In fact, dysregulated copper homeostasis has been clearly linked to neurological disorders including Wilson and Alzheimer’s disease. Such neurodegenerative diseases are associated with progressive loss of neurons and thus impaired brain functions. However, the underlying mechanisms are not fully understood. Characterization of the element species and their subcellular localization is of great importance to uncover cellular mechanisms. Recent research activities focus on the question of how copper contributes to the pathological findings. Cellular bioimaging of copper is an essential key to accomplish this objective. Besides information on the spatial distribution and chemical properties of copper, other essential trace elements can be localized in parallel. Highly sensitive and high spatial resolution techniques such as LA-ICP-MS, TEM-EDS, S-XRF and NanoSIMS are required for elemental mapping on subcellular level. This review summarizes state-of-the-art techniques in the field of bioimaging. Their strengths and limitations will be discussed with particular focus on potential applications for the elucidation of copper-related diseases. Based on such investigations, further information on cellular processes and mechanisms can be derived under physiological and pathological conditions. Bioimaging studies might enable the clarification of the role of copper in the context of neurodegenerative diseases and provide an important basis to develop therapeutic strategies for reduction or even prevention of copper-related disorders and their pathological consequences. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 862 KW - copper KW - cellular bioimaging KW - neurodegenerative diseases KW - copper-related disorders KW - SIMS techniques KW - TEM KW - S-XRF Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-459544 SN - 1866-8372 IS - 862 ER - TY - JOUR A1 - Witt, Barbara A1 - Schaumlöffel, Dirk A1 - Schwerdtle, Tanja T1 - Subcellular Localization of Copper BT - Cellular Bioimaging with Focus on Neurological Disorders JF - International Journal of Molecular Sciences N2 - As an essential trace element, copper plays a pivotal role in physiological body functions. In fact, dysregulated copper homeostasis has been clearly linked to neurological disorders including Wilson and Alzheimer’s disease. Such neurodegenerative diseases are associated with progressive loss of neurons and thus impaired brain functions. However, the underlying mechanisms are not fully understood. Characterization of the element species and their subcellular localization is of great importance to uncover cellular mechanisms. Recent research activities focus on the question of how copper contributes to the pathological findings. Cellular bioimaging of copper is an essential key to accomplish this objective. Besides information on the spatial distribution and chemical properties of copper, other essential trace elements can be localized in parallel. Highly sensitive and high spatial resolution techniques such as LA-ICP-MS, TEM-EDS, S-XRF and NanoSIMS are required for elemental mapping on subcellular level. This review summarizes state-of-the-art techniques in the field of bioimaging. Their strengths and limitations will be discussed with particular focus on potential applications for the elucidation of copper-related diseases. Based on such investigations, further information on cellular processes and mechanisms can be derived under physiological and pathological conditions. Bioimaging studies might enable the clarification of the role of copper in the context of neurodegenerative diseases and provide an important basis to develop therapeutic strategies for reduction or even prevention of copper-related disorders and their pathological consequences. KW - copper KW - cellular bioimaging KW - neurodegenerative diseases KW - copper-related disorders KW - SIMS techniques KW - TEM KW - S-XRF Y1 - 2020 U6 - https://doi.org/10.3390/ijms21072341 SN - 1422-0067 VL - 21 IS - 7 PB - Molecular Diversity Preservation International CY - Basel ER - TY - JOUR A1 - Hossain, Mohammad Delwar A1 - Chakraborty, Chanchal A1 - Rana, Utpal A1 - Mondal, Sanjoy A1 - Holdt, Hans-Jürgen A1 - Higuchi, Masayoshi T1 - Green-to-black electrochromic copper(I)-based metallo-supramolecular polymer with a perpendicularly twisted structure JF - ACS applied polymer materials N2 - A Cu(I)-based metallo-supramolecular polymer with a perpendicularly twisted structure was synthesized by a 1:1 complexation of tetrakis(acetonitrile)copper(I) triflate with the pi-conjugated dibenzoeilatin ligand. Stepwise complexation behavior of Cu(I) with the ligand was revealed by titrimetric ultraviolet- visible (UV-vis) spectroscopic analysis. Formation of a high-molecular-weight polymer (M-w = 1.21 x 10(5) Da) was confirmed by a size-exclusion chromatography-viscometry-right-angle laser light scattering study. A bundle structure of the polymer chains was observed by scanning electron microscopy. A cyclic voltammogram of the polymer film showed reversible redox waves at a negative potential. A device consisting of indium tin oxide (ITO) glass coated with a film of the polymer exhibited reversible green-to-black electrochromism upon alternate application of -3 and +1 V. KW - electrochromism KW - metallo-supramolecular polymers KW - stepwise complexation KW - metal-to-ligand charge transfer KW - copper KW - dibenzoeilatin Y1 - 2020 U6 - https://doi.org/10.1021/acsapm.0c00559 SN - 2637-6105 VL - 2 IS - 11 SP - 4449 EP - 4454 PB - American Chemical Society CY - Washington, DC ER - TY - GEN A1 - Abbas, Ioana M. A1 - Vranic, Marija A1 - Hoffmann, Holger A1 - El-Khatib, Ahmed H. A1 - Montes-Bayón, María A1 - Möller, Heiko Michael A1 - Weller, Michael G. T1 - Investigations of the Copper Peptide Hepcidin-25 by LC-MS/MS and NMR⁺ T2 - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe N2 - Hepcidin-25 was identified as themain iron regulator in the human body, and it by binds to the sole iron-exporter ferroportin. Studies showed that the N-terminus of hepcidin is responsible for this interaction, the same N-terminus that encompasses a small copper(II) binding site known as the ATCUN (amino-terminal Cu(II)- and Ni(II)-binding) motif. Interestingly, this copper-binding property is largely ignored in most papers dealing with hepcidin-25. In this context, detailed investigations of the complex formed between hepcidin-25 and copper could reveal insight into its biological role. The present work focuses on metal-bound hepcidin-25 that can be considered the biologically active form. The first part is devoted to the reversed-phase chromatographic separation of copper-bound and copper-free hepcidin-25 achieved by applying basic mobile phases containing 0.1% ammonia. Further, mass spectrometry (tandemmass spectrometry (MS/MS), high-resolutionmass spectrometry (HRMS)) and nuclear magnetic resonance (NMR) spectroscopy were employed to characterize the copper-peptide. Lastly, a three-dimensional (3D)model of hepcidin-25with bound copper(II) is presented. The identification of metal complexes and potential isoforms and isomers, from which the latter usually are left undetected by mass spectrometry, led to the conclusion that complementary analytical methods are needed to characterize a peptide calibrant or referencematerial comprehensively. Quantitative nuclear magnetic resonance (qNMR), inductively-coupled plasma mass spectrometry (ICP-MS), ion-mobility spectrometry (IMS) and chiral amino acid analysis (AAA) should be considered among others. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 701 KW - hepcidin-25 KW - copper KW - nickel KW - copper complex KW - ATCUN motif KW - metal complex KW - MS KW - NMR structure KW - metal peptide KW - metalloprotein KW - metallopeptide KW - isomerization KW - racemization KW - purity KW - reference material Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-427926 SN - 1866-8372 IS - 701 ER - TY - GEN A1 - Schwarz, Maria A1 - Lossow, Kristina A1 - Kopp, Johannes F. A1 - Schwerdtle, Tanja A1 - Kipp, Anna Patricia T1 - Crosstalk of Nrf2 with the Trace Elements Selenium, Iron, Zinc, and Copper T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Trace elements, like Cu, Zn, Fe, or Se, are important for the proper functioning of antioxidant enzymes. However, in excessive amounts, they can also act as pro-oxidants. Accordingly, trace elements influence redox-modulated signaling pathways, such as the Nrf2 pathway. Vice versa, Nrf2 target genes belong to the group of transport and metal binding proteins. In order to investigate whether Nrf2 directly regulates the systemic trace element status, we used mice to study the effect of a constitutive, whole-body Nrf2 knockout on the systemic status of Cu, Zn, Fe, and Se. As the loss of selenoproteins under Se-deprived conditions has been described to further enhance Nrf2 activity, we additionally analyzed the combination of Nrf2 knockout with feeding diets that provide either suboptimal, adequate, or supplemented amounts of Se. Experiments revealed that the Nrf2 knockout partially affected the trace element concentrations of Cu, Zn, Fe, or Se in the intestine, liver, and/or plasma. However, aside from Fe, the other three trace elements were only marginally modulated in an Nrf2-dependent manner. Selenium deficiency mainly resulted in increased plasma Zn levels. One putative mediator could be the metal regulatory transcription factor 1, which was up-regulated with an increasing Se supply and downregulated in Se-supplemented Nrf2 knockout mice. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1081 KW - Nrf2 KW - selenium KW - iron KW - copper KW - zinc KW - homeostasis Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-472873 SN - 1866-8372 IS - 1081 ER - TY - JOUR A1 - Schwarz, Maria A1 - Lossow, Kristina A1 - Kopp, Johannes Florian A1 - Schwerdtle, Tanja A1 - Kipp, Anna Patricia T1 - Crosstalk of Nrf2 with the Trace Elements Selenium, Iron, Zinc, and Copper JF - Nutrients N2 - Trace elements, like Cu, Zn, Fe, or Se, are important for the proper functioning of antioxidant enzymes. However, in excessive amounts, they can also act as pro-oxidants. Accordingly, trace elements influence redox-modulated signaling pathways, such as the Nrf2 pathway. Vice versa, Nrf2 target genes belong to the group of transport and metal binding proteins. In order to investigate whether Nrf2 directly regulates the systemic trace element status, we used mice to study the effect of a constitutive, whole-body Nrf2 knockout on the systemic status of Cu, Zn, Fe, and Se. As the loss of selenoproteins under Se-deprived conditions has been described to further enhance Nrf2 activity, we additionally analyzed the combination of Nrf2 knockout with feeding diets that provide either suboptimal, adequate, or supplemented amounts of Se. Experiments revealed that the Nrf2 knockout partially affected the trace element concentrations of Cu, Zn, Fe, or Se in the intestine, liver, and/or plasma. However, aside from Fe, the other three trace elements were only marginally modulated in an Nrf2-dependent manner. Selenium deficiency mainly resulted in increased plasma Zn levels. One putative mediator could be the metal regulatory transcription factor 1, which was up-regulated with an increasing Se supply and downregulated in Se-supplemented Nrf2 knockout mice. KW - Nrf2 KW - selenium KW - iron KW - copper KW - zinc KW - homeostasis Y1 - 2019 U6 - https://doi.org/10.3390/nu11092112 SN - 2072-6643 VL - 11 IS - 9 PB - MDPI CY - Basel ER - TY - JOUR A1 - Abbas, Ioana M. A1 - Vranic, Marija A1 - Hoffmann, Holger A1 - El-Khatib, Ahmed H. A1 - Montes-Bayón, María A1 - Möller, Heiko Michael A1 - Weller, Michael G. T1 - Investigations of the Copper Peptide Hepcidin-25 by LC-MS/MS and NMR⁺ JF - International Journal of Molecular Sciences N2 - Hepcidin-25 was identified as themain iron regulator in the human body, and it by binds to the sole iron-exporter ferroportin. Studies showed that the N-terminus of hepcidin is responsible for this interaction, the same N-terminus that encompasses a small copper(II) binding site known as the ATCUN (amino-terminal Cu(II)- and Ni(II)-binding) motif. Interestingly, this copper-binding property is largely ignored in most papers dealing with hepcidin-25. In this context, detailed investigations of the complex formed between hepcidin-25 and copper could reveal insight into its biological role. The present work focuses on metal-bound hepcidin-25 that can be considered the biologically active form. The first part is devoted to the reversed-phase chromatographic separation of copper-bound and copper-free hepcidin-25 achieved by applying basic mobile phases containing 0.1% ammonia. Further, mass spectrometry (tandemmass spectrometry (MS/MS), high-resolutionmass spectrometry (HRMS)) and nuclear magnetic resonance (NMR) spectroscopy were employed to characterize the copper-peptide. Lastly, a three-dimensional (3D)model of hepcidin-25with bound copper(II) is presented. The identification of metal complexes and potential isoforms and isomers, from which the latter usually are left undetected by mass spectrometry, led to the conclusion that complementary analytical methods are needed to characterize a peptide calibrant or referencematerial comprehensively. Quantitative nuclear magnetic resonance (qNMR), inductively-coupled plasma mass spectrometry (ICP-MS), ion-mobility spectrometry (IMS) and chiral amino acid analysis (AAA) should be considered among others. KW - hepcidin-25 KW - copper KW - nickel KW - copper complex KW - ATCUN motif KW - metal complex KW - MS KW - NMR structure KW - metal peptide KW - metalloprotein KW - metallopeptide KW - isomerization KW - racemization KW - purity KW - reference material Y1 - 2018 U6 - https://doi.org/10.3390/ijms19082271 SN - 1422-0067 SN - 1661-6596 VL - 19 IS - 8 PB - Molecular Diversity Preservation International CY - Basel ER - TY - JOUR A1 - Schwarze, Thomas A1 - Kelling, Alexandra A1 - Müller, Holger A1 - Trautmann, Michael A1 - Klamroth, Tillmann A1 - Baumann, Otto A1 - Strauch, Peter A1 - Holdt, Hans-Jürgen T1 - N-2-Pyridinylmethyl-N '-arylmethyl-diaminomaleonitriles: New Highly Selective Chromogenic Chemodosimeters for Copper(II) JF - Chemistry - a European journal KW - amides KW - chemodosimeter KW - colorimetric detection KW - copper KW - sensors KW - UV KW - Vis spectroscopy Y1 - 2012 U6 - https://doi.org/10.1002/chem.201201731 SN - 0947-6539 VL - 18 IS - 34 SP - 10506 EP - 10510 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Kozlevcar, Bojan A1 - Golobic, Amalija A1 - Strauch, Peter T1 - Dynamic pseudo Jahn-Teller distortion in a compressed octahedral CuO6 complex JF - Polyhedron : the international journal of inorganic and organometallic chemistry N2 - The crystal structure of cis-[Cu(C8H7O3)(2)(H2O)(2)] (115 K data) reveals bidentate vanillinate ions coordinated via methoxy and deprotonated hydroxy oxygen atoms and water molecules in a distorted octahedral CuO6 chromophore. A cis orientation of the ligands enables two non-identical O(methoxy)-Cu-O(water) coordination axes (2.354(l) + 2.163(1); 2.151(1) + 2.020(1) angstrom), and the third shortest O(hydroxy)-Cu-O(hydroxy) axis (1.919(1) + 1.914(1) angstrom). This 115 K coordination sphere differs importantly to the one obtained from the 293 K data of the same compound, where two long 0(methoxy)-Cu-O(water) axes are of the same length, and only minor changes at the short 0(hydroxy)-Cu-O(hydroxy) axis are noticed. An axial symmetry of the complex with an inverse g(1.2)(g(perpendicular to)) > g(3)(g(parallel to)) pattern is observed in the temperature range from 298 to 180 K. A further decrease of temperature reveals gradual changes from axial to rhombic symmetry (g(1) > g(2) > g(3)) that is reversible. A mean-square displacement amplitude (MDSA) analysis reveals a disorder in the Cu-O(methoxy) bonds, but not in the other metal-ligand Cu-O(hydroxy) and Cu-O(water) bonds at 293 and 115 K. The disorder is significantly weaker in the 115 K structure. The MSDA analysis and the structural-EPR agreement show vibrational disorder in two coordination axes, due to the cis conformation of the complex with two 0(methoxy)-Cu-O(water) axes. KW - copper KW - vanillin KW - Jahn-Teller distortion KW - MSDA KW - cis KW - EPR Y1 - 2006 U6 - https://doi.org/10.1016/j.poly.2006.04.009 SN - 0277-5387 VL - 25 IS - 15 SP - 2824 EP - 2828 PB - Elsevier CY - Oxford ER -