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International audience; Gesunder humaner Knochen unterliegt einem permanenten Umbau, um sich den mechanischen Anforderungen anzupassen, Mikrofrakturen zu reparieren und das Mineralgleichgewicht zu erhalten. Der Umbauprozess der extrazellulären Matrix wird durch Osteoblasten und Osteoklasten realisiert. Eine bedeutende Rolle bei der Regulierung der Osteoklasten- und Osteoblastenaktivität wird den Osteozyten zugesprochen, welche in einem komplexen Netzwerk von Zelllakunen und Kanalikuli die extrazelluläre Matrix durchsetzen. Auf Phasenkontrast basierende hochauflösende Nano-Computertomografie erlaubt erstmals, sowohl das Zellnetzwerk als auch die direkt angrenzende mineralisierte Matrix in Untersuchungsvolumen, die hinsichtlich ihrer Größe als repräsentativ angesehen werden können, im nativen Zustand (nicht demineralisiert, nicht eingebettet) zu untersuchen.; Healthy human bone tissue undergoes a continuous remodeling process to i) repair microdamages, ii) adapt to mechanical boundary conditions, and iii) maintain a constant serum calcium level. Bone remodeling is realized by specialized bone synthesizing and resorbing cells, i. e. osteoblasts and osteoclasts, respectively. Osteocytes play an important role in the regulation of osteoblast and osteoclast activities. Osteocytes are embedded in the extracellular matrix in a complex porous lacunar-canalicular network (LCN). Recently developed high-fidelity phase-contrast nanotomography with synchrotron radiation x-ray sources enabled for the first time the simultaneous assessment of both, LCN and the adjacent extracellular mineralized matrix in close-to-native sample conditions.

PALEOFLUID CHEMISTRY OF OROGENIC GOLD DEPOSITS: NOVEL ANALYTICAL METHODS AND CASE STUDIES FROM THE BOHEMIAN MASSIF Tomáš Hrstka1 1 Charles University in Prague, Faculty of Science, Institute of Geochemistry, Mineralogy and Mineral Resources, Albertov 6, Praha 2, CZ-128 43 Abstract of the Ph.D. Thesis Fluid inclusions represent a unique tool for understanding the processes leading to the formation of mineral deposits and fluid-rock interactions in general. Orogenic gold deposits in the central part of the Bohemian Massif (Libčice and Kasejovice deposits) were studied in order to provide a better understanding of their genesis. A multifaceted approach was adopted including a broad spectrum of micro-analytical methods. While traditional methods were used as the basis of this study (e.g., microthermometry, SEM and optical microscopy), the application and improvement/development of modern analytical methods (e.g., LA-ICP- MS and Raman spectroscopy) or introduction of alternative innovative techniques (CLSM, Nano- tomography, QEMSCAN) constituted a significant part of this study. This study reveals the importance of the HCO3 - species in hydrothermal fluids (i.e., >100 řC to ~350 řC). Previously, the prevalence of Cl- and other anions was reported for hydrothermal paleofluids and the majority of studies suggested...