Pure monoparesis: a particular stroke subgroup?

BACKGROUND: Acute stroke presenting as monoparesis is rare, with a pure motor deficit in the arm or leg extending to an isolated facial paresis. OBJECTIVE: To raise the question if acute stroke presenting as monoparesis is a different entity from stroke with a more extensive motor deficit. PATIENTS: In the Lausanne Stroke Registry (1979-2000), 195 (4.1%) of 4802 patients met the clinical criteria for pure monoparesis involving the face (22%), arm (63%), or leg (15%). RESULTS: In the vast majority of cases (> 95%), monoparesis corresponded to ischemic stroke with a favorable outcome, with initial computed tomography scans or magnetic resonance images showing no signs of hemorrhage. The lesion for a facial deficit was most frequently located subcortically (internal capsule); for an arm deficit, in the superficial middle cerebral artery; and for a leg deficit, in the anterior cerebral artery territory. In pure monoparesis, only 17% of the patients had more than 1 risk factor as compared with 26% of those with bimodal and trimodal hemiparesis and with 46% of all patients with stroke other than those with pure motor stroke. The only frequent risk factor was hypertension (53%); however, this frequency was no different from that in other patients with stroke. No major stroke etiology could be identified in any of the 3 subgroups of monoparesis. CONCLUSION: Our finding of a wide range of stroke localization and etiology in monoparesis without any particular subgroup suggests that no specific plan of investigation can be recommended for these patients.

Linking microtubules to the activation of CDC42 in fission yeast

Cell polarity is an essential property of most cell types and relies on a dynamic cytoskeleton of actin filaments and microtubules. In rod-shaped S. pombe cells microtubules are organized along the length of the cell and transport polarity factors to cell tips to regulate cell polarity. An important cell polarity factor is the protein Tea4, which is responsible for correct cell morphogenesis and bipolar growth. During my research I confirmed the known transport mechanism of Tea4 and I also showed alternative localization and anchoring mechanisms at the cell ends. Tea4 contains a conserved SH3 domain, the function of which was unknown and my results show that the SH3 domain of Tea4 is essential for Tea4 function in vivo. First, cells with tea4SH3 mutations show aberrant cell shapes and monopolar growth patterns similar to tea4A and in addition SH3 domain is important for proper localization of multiple cell polarity proteins. Second, I showed that Tea4 associates with Type 1 Phosphatase Dis2 through both its SH3 domain and an RVxF motif. Tea4 also binds the DYRK kinase Pomi through its SH3 domain. In addition Tea4 is proposed to promote the local dephosphorylation of Pomi by Dis2 to induce the formation of a cortical gradient from cell ends essential for cell size homeostasis. Polarized growth is also controlled by cell tip-localized Cdc42. This Rho- family GTPase is activated by the Guanine Exchange Factors Gef1 and Scd1 and inactivated by the Rho GTPase Activating Protein Rga4. In this study, I investigated the mechanisms of how Tea4 promotes Cdc42 activation. My work suggests that Tea4 promotes the local exclusion of Rga4, which in turn allows the accumulation of active Cdc42, which may result in growth. Exclusion of Rga4 by Tea4 is likely to be mediated by Dis2-dependent dephosphorylation. These results suggest a molecular pathway that links the microtubule- associated factor Tea4 with Cdc42 to promote cell polarization and morphogenesis. - La polarité cellulaire est une propriété essentielle de la plupart des types cellulaires et s'appuie sur une dynamique des cytosquelettes d'actine et de microtubules. Dans les cellules en forme de bâtonnet de S. pombe les microtubules sont alignés selon l'axe longitudinal de la cellule et les facteurs de polarité transportés aux extrémité cellulaires afin de réguler la polarité cellulaire. Un facteur important de polarité cellulaire est la protéine Tea4, qui est responsable de la morphogenèse des cellules et leur croissance bipolaire. Au cours de mes recherches, j'ai confirmé les mécanismes connus de transport de Tea4 et j'ai aussi mis en évidence d'autres mechanismes de localisation et d'ancrage de Tea4 aux extrémités cellulaires. Tea4 contient un domaine SH3 conservé, dont la fonction était inconnue et mes résultats montrent que le domaine SH3 est essentiel pour la fonction de Tea4 in vivo. Tout d'abord, les cellules avec des mutations tea4sm ont des formes aberrantes et leur croissance est monopolaire de manière similaire au mutant tea4A. De plus ce domaine SH3 est important pour la localisation correcte de plusieurs protéines de polarité cellulaire. Deuxièmement, j'ai montré que Tea4 s'associe avec la Phosphatase de Type-1 Dis2 par son domaine SH3 et un motif RVxF. Tea4 se lie également la kinase DYRK Pomi par son domaine SH3. De plus, Tea4 pourrait favoriser la déphosphorylation locale de Pomi par Dis2 afin d'induire la formation d'un gradient cortical de Pomi essentiel pour l'homéostasie de la longueur des cellules. La croissance polarisée est également contrôlée par la protéine Cdc42 localisée aux extrémités cellulaires. Cette GTPase de la famille de Rho GTPase est activée par les facteurs échange de guanine Gef1 et Scd1 et inactivée par la protéine "Rho GTPase activating" Rga4. Dans cette étude, j'ai étudié les mécanismes d' activation de Cdc42 par Tea4. Mes résultats suggèrent que Tea4 favorise l'exclusion locale de Rga4, ce qui permet l'accumulation de Cdc42 active, nécessaire à la croissance. L' exclusion de Rga4 par Tea4 est vraisemblablement médiée par une déphosphorylation Dis2- dépendente. Ces résultats suggèrent une voie moléculaire qui lie le facteur associé aux microtubules Tea4 à Cdc42 pour promouvoir la polarisation cellulaire et la morphogenèse. - Cell polarity is important for several essential biological functions such as generation of distinct cell fates during development and function of differentiated cells. Defective cell polarity has been related to uncontrolled cell division and subsequently to cancer initiation. Cell polarity depends on a functional cytoskeleton that consists of actin filaments and microtubules, which maintains cell shape, helps cellular motion, enables intracellular protein transport and plays a vital role in cell division. A component of cytoskeleton is microtubules that regulate cell polarization in diverse cell types. During my research, I worked with Schizosaccharomyces pombe, also named fission yeast, a powerful unicellular model organism that allows combination of genetic, biochemical and microscopic analysis for the proper study of cell polarity. Microtubule-associated protein Tea4 is transported to cell tips where it is thought to organize polarized growth. I showed that Tea4 and its evolutionarily conserved SH3 domain play an important role for maintenance of fission yeast cells shape and growth. Furthermore, Tea4 is responsible for the proper localization of multiple polarity proteins and acts as a mediator to control the local activity of an essential polarity regulator called Cdc42. Thus, my results provide a better understanding of the molecular mechanisms that regulate cell polarity. - La polarité cellulaire est importante pour plusieurs fonctions biologiques essentielles telles que la différenciation cellulaires au cours du développement et de la fonction de cellules différenciées. Les défauts de la polarité cellulaire ont été liés à des divisions cellulaires incontrôlées et à l'initiation de tumeur. La polarité cellulaire dépend d'un cytosquelette fonctionnel, qui maintient la forme des cellules, aide à la migration cellulaire, permet le transport intracellulaire des protéines et joue un rôle essentiel dans la division cellulaire. Un composant du cytosquelette est constitué de microtubules qui régissent la polarisation cellulaire dans divers types cellulaires. Au cours de mes recherches, j'ai travaillé avec Schizosaccharomyces pombe, appelé également levure fissipare, un modèle unicellulare puissant qui permet la combinaison de différentes d'approches expérimentales: génétiques, biochimiques et microscopiques pour l'étude de la polarité cellulaire. La protéine Tea4 associée aux microtubules est transportée aux extrémités cellulaires où elle organise la croissance polarisée. J'ai montré que Tea4 et son domaine conservé SH3 jouent un rôle important pour le maintien de la forme des cellules de levure et leur croissance. De plus, Tea4 est responsable de la localisation correcte de multiples facteurs de polarité et agit comme un médiateur pour contrôler l'activité locale d'un régulateur de polarité essentiel appelé Cdc42. Ainsi, mes résultats permettent de mieux comprendre les mécanismes moléculaires qui régulent la polarité cellulaire.

Magnetic field effect on quantum corrections to the low-temperature conductivity in mettalic perovskite oxides

The transport and magnetotransport properties of the metallic and ferromagnetic SrRuO3 (SRO) and the metallic and paramagnetic LaNiO3 (LNO) epitaxial thin films have been investigated in fields up to 55 T at temperatures down to 1.8 K . At low temperatures both samples display a well-defined resistivity minimum. We argue that this behavior is due to the increasing relevance of quantum corrections to the conductivity (QCC) as temperature is lowered; this effect being particularly relevant in these oxides due to their short mean free path. However, it is not straightforward to discriminate between contributions of weak localization and renormalization of electron-electron interactions to the QCC through temperature dependence alone. We have taken advantage of the distinct effect of a magnetic field on both mechanisms to demonstrate that in ferromagnetic SRO the weak-localization contribution is suppressed by the large internal field leaving only renormalized electron-electron interactions, whereas in the nonmagnetic LNO thin films the weak-localization term is relevant.

Fluid-rock-strain feedbacks in extensional shear zones

La présence de fluide météorique synchrone à l'activité du détachement (Farmin, 2003 ; Mulch et al., 2007 ; Gébelin et al., 2011), implique que les zones de cisaillement sont des systèmes ouverts avec des cellules de convections à l'échelle crustale et un intense gradient géothermique au sein du détachement (Morrison et Anderson, 1998, Gottardi et al., 2011). De plus, les réactions métamorphiques liées à des infiltrations fluides dans les zones de cisaillement extensionnel peuvent influencer les paramètres rhéologiques du système (White and Knipe, 1978), et impliquer la localisation de la déformation dans la croûte. Dans ce manuscrit, deux zones de cisaillement infiltrées par des fluides météoriques sont étudiées, l'une étant largement quartzitique, et l'autre de nature granitique ; les relations entre déformation, fluides, et roches s'appuient sur des approches structurales, microstructurales, chimiques et isotopiques. L'étude du détachement du Columbia river (WA, USA) met en évidence que la déformation mylonitique se développe en un million d'années. La phase de cisaillement principal s'effectue à 365± 30°C d'après les compositions isotopiques en oxygène du quartz et de la muscovite. Ces minéraux atteignent l'équilibre isotopique lors de leur recristallisation dynamique contemporaine à la déformation. La zone de cisaillement enregistre une baisse de température, remplaçant le mécanisme de glissement par dislocation par celui de dissolution- précipitation dans les derniers stades de l'activité du détachement. La dynamique de circulation fluide bascule d'une circulation pervasive à chenalisée, ce qui engendre localement la rupture des équilibres d'échange isotopiques. La zone de cisaillement de Bitterroot (MT, USA) présente une zone mylonitique de 600m d'épaisseur, progressant des protomylonites aux ultramylonites. L'intensité de la localisation de la déformation se reflète directement sur l'hydratation des feldspaths, réaction métamorphique majeure dite de « rock softening ». Une étude sur roche totale indique des transferts de masse latéraux au sein des mylonites, et d'importantes pertes de volume dans les ultramylonites. La composition isotopique en hydrogène des phyllosilicates met en évidence la présence (1) d'une source magmatique/métamorphique originelle, caractérisée par les granodiorites ayant conservé leur foliation magmatique, jusqu'aux protomylonites, et (2) une source météorique qui tamponne les valeurs des phyllosilicates des fabriques mylonitiques jusqu'aux veines de quartz non-déformées. Les compositions isotopiques en oxygène des minéraux illustrent le tamponnement de la composition du fluide météorique par l'encaissant. Ce phénomène cesse lors du processus de chloritisation de la biotite, puisque les valeurs des chlorites sont extrêmement négatives (-10 per mil). La thermométrie isotopique indique une température d'équilibre isotopique de la granodiorite entre 600-500°C, entre 500-300°C dans les mylonites, et entre 300 et 200°C dans les fabriques cassantes (cataclasites et veines de quartz). Basé sur les résultats issus de ce travail, nous proposons un modèle général d'interactions fluide-roches-déformation dans les zones de détachements infiltrées par des fluides météoriques. Les zones de détachements évoluent rapidement (en quelques millions d'années) au travers de la transition fragile-ductile ; celle-ci étant partiellement contrôlée par l'effet thermique des circulations de fluide météoriques. Les systèmes de détachements sont des lieux où la déformation et les circulations fluides sont couplées ; évoluant rapidement vers une localisation de la déformation, et de ce fait, une exhumation efficace. - The presence of meteoric fluids synchronous with the activity of extensional detachment zones (Famin, 2004; Mulch et al., 2007; Gébelin et al., 2011) implies that extensional systems involve fluid convection at a crustal scale, which results in high geothermal gradients within active detachment zones (Morrison and Anderson, 1998, Gottardi et al., 2011). In addition, the metamorphic reactions related to fluid infiltration in extensional shear zones can influence the rheology of the system (White and Knipe, 1978) and ultimately how strain localizes in the crust. In this thesis, two shear zones that were permeated by meteoric fluids are studied, one quartzite-dominated, and the other of granitic composition; the relations between strain, fluid, and evolving rock composition are addressed using structural, microstructural, and chemical/isotopic measurements. The study of the Columbia River detachment that bounds the Kettle core complex (Washington, USA) demonstrates that the mylonitic fabrics in the 100 m thick quartzite- dominated detachment footwall developed within one million years. The main shearing stage occurred at 365 ± 30°C when oxygen isotopes of quartz and muscovite equilibrated owing to coeval deformation and dynamic recrystallization of these minerals. The detachment shear zone records a decrease in temperature, and dislocation creep during detachment shearing gave way to dissolution-precipitation and fracturing in the later stages of detachment activity. Fluid flow switched from pervasive to channelized, leading to isotopic disequilibrium between different minerals. The Bitterroot shear zone detachment (Montana, USA) developed a 600 m thick mylonite zone, with well-developed transitions from protomylonite to ultramylonite. The localization of deformation relates directly to the intensity of feldspar hydration, a major rock- softening metamorphic reaction. Bulk-rock analyses of the mylonitic series indicate lateral mass transfer in the mylonite (no volume change), and significant volume loss in ultramylonite. The hydrogen isotope composition of phyllosilicates shows (1) the presence of an initial magmatic/metamorphic source characterized by the granodiorite in which a magmatic, and gneissic (protomylonite) foliation developed, and (2) a meteoric source that buffers the values of phyllosilicates in mylonite, ultramylonite, cataclasite, and deformed and undeformed quartz veins. The mineral oxygen isotope compositions were buffered by the host-rock compositions until chloritization of biotite started; the chlorite oxygen isotope values are negative (-10 per mil). Isotope thermometry indicates a temperature of isotopic equilibrium of the granodiorite between 600-500°C, between 500-300°C in the mylonite, and between 300 and 200°C for brittle fabrics (cataclasite and quartz veins). Results from this work suggest a general model for fluid-rock-strain feedbacks in detachment systems that are permeated by meteoric fluids. Phyllosilicates have preserved in their hydrogen isotope values evidence for the interaction between rock and meteoric fluids during mylonite development. Fluid flow generates mass transfer along the tectonic anisotropy, and mylonites do not undergo significant volume change, except locally in ultramylonite zones. Hydration of detachment shear zones attends mechanical grain size reduction and enhances strain softening and localization. Self-exhuming detachment shear zones evolve rapidly (a few million years) through the transition from ductile to brittle, which is partly controlled by the thermal effect of circulating surface fluids. Detachment systems are zones in the crust where strain and fluid flow are coupled; these systems. evolve rapidly toward strain localization and therefore efficient exhumation.

ORMDL proteins are a conserved new family of endoplasmic reticulum membrane proteins

Background: Annotations of completely sequenced genomes reveal that nearly half of the genes identified are of unknown function, and that some belong to uncharacterized gene families. To help resolve such issues, information can be obtained from the comparative analysis of homologous genes in model organisms. Results: While characterizing genes from the retinitis pigmentosa locus RP26 at 2q31-q33, we have identified a new gene, ORMDL1, that belongs to a novel gene family comprising three genes in humans (ORMDL1, ORMDL2 and ORMDL3), and homologs in yeast, microsporidia, plants, Drosophila, urochordates and vertebrates. The human genes are expressed ubiquitously in adult and fetal tissues. The Drosophila ORMDL homolog is also expressed throughout embryonic and larval stages, particularly in ectodermally derived tissues. The ORMDL genes encode transmembrane proteins anchored in the endoplasmic reticulum (ER). Double knockout of the two Saccharomyces cerevisiae homologs leads to decreased growth rate and greater sensitivity to tunicamycin and dithiothreitol. Yeast mutants can be rescued by human ORMDL homologs. Conclusions: From protein sequence comparisons we have defined a novel gene family, not previously recognized because of the absence of a characterized functional signature. The sequence conservation of this family from yeast to vertebrates, the maintenance of duplicate copies in different lineages, the ubiquitous pattern of expression in human and Drosophila, the partial functional redundancy of the yeast homologs and phenotypic rescue by the human homologs, strongly support functional conservation. Subcellular localization and the response of yeast mutants to specific agents point to the involvement of ORMDL in protein folding in the ER.

Rockfall induced seismic signals: case study in Montserrat, Catalonia

After a rockfall event, a usual post event survey includes qualitative volume estimation, trajectory mapping and determination of departing zones. However, quantitative measurements are not usually made. Additional relevant quantitative information could be useful in determining the spatial occurrence of rockfall events and help us in quantifying their size. Seismic measurements could be suitable for detection purposes since they are non invasive methods and are relatively inexpensive. Moreover, seismic techniques could provide important information on rockfall size and location of impacts. On 14 February 2007 the Avalanche Group of the University of Barcelona obtained the seismic data generated by an artificially triggered rockfall event at the Montserrat massif (near Barcelona, Spain) carried out in order to purge a slope. Two 3 component seismic stations were deployed in the area about 200 m from the explosion point that triggered the rockfall. Seismic signals and video images were simultaneously obtained. The initial volume of the rockfall was estimated to be 75 m3 by laser scanner data analysis. After the explosion, dozens of boulders ranging from 10¿4 to 5 m3 in volume impacted on the ground at different locations. The blocks fell down onto a terrace, 120 m below the release zone. The impact generated a small continuous mass movement composed of a mixture of rocks, sand and dust that ran down the slope and impacted on the road 60 m below. Time, time-frequency evolution and particle motion analysis of the seismic records and seismic energy estimation were performed. The results are as follows: 1 ¿ A rockfall event generates seismic signals with specific characteristics in the time domain; 2 ¿ the seismic signals generated by the mass movement show a time-frequency evolution different from that of other seismogenic sources (e.g. earthquakes, explosions or a single rock impact). This feature could be used for detection purposes; 3 ¿ particle motion plot analysis shows that the procedure to locate the rock impact using two stations is feasible; 4 ¿ The feasibility and validity of seismic methods for the detection of rockfall events, their localization and size determination are comfirmed.

Differential insertion of GPI-anchored GFPs into lipid rafts of live cells.

Partitioning of proteins in cholesterol and sphingolipid enriched plasma membrane microdomains, called lipid rafts, is critical for many signal transduction and protein sorting events. Although raft partitioning of many signaling molecules remains to be determined, glycosylphosphatidyl-inositol (GPI)-anchored proteins possess high affinity for lipid rafts and are currently exploited as markers to investigate fundamental mechanisms in protein sorting and signal transduction events. In this study, we demonstrate that two recombinant GPI-anchored green fluorescent proteins (GFP-GPIs) that differ in their GPI signal sequence confer distinct localization in plasma membrane microdomains. GFP fused to the GPI signal of the decay accelerating factor GFP-GPI(DAF) partitioned exclusively in lipid rafts, whereas GFP fused to the GPI signal of TRAIL-R3, GFP-GPI(TRAIL-R3), associated only minimally with microdomains. In addition, we investigated the unique ability of purified GFP-GPIs to insert into membrane microdomains of primary lymphocytes. This cell surface painting allows rapid, stable, and functional association of the GPI-anchored proteins with the target cell plasma membrane. The distinct membrane localization of the two GFP-GPIs was observed irrespective of whether the GPI-anchored molecules were painted or transfected. Furthermore, we show that painted GFP-GPI(DAF) was totally dependent on the GPI anchor and that the membrane insertion was increased by the addition of raft-associated lipids such as cholesterol, sphingomyelin, and dipalmitoyl-phosphatidylethanolamine. Thus, this study provides evidence that different GPI signal sequences lead to distinct membrane microdomain localization and that painted GFP-GPI(DAF) serves as an excellent fluorescent marker for lipid rafts in live cells.

Docteur, j'ai un ganglion [Doctor, I have a lymph node]

To investigate a recently developed lymphadenopathy can be simple or complex. The medical history, presence or not of symptoms, the general physical examination, and the localization and characteristics of the adenopathy, most often lead to a diagnosis and therapy when indicated. Among young adults, the etiology is either infectious or reactive, rarely tumoral, as opposed to elderly persons. The most important step is to look at signs of severity (or non banality) such as an increased size, hard consistency, supra-clavicular location, an immunocompromised host, a history of Tb exposition. If present, these signs will trigger a biopsy with cyto- or histopathological examination mostly to rule out a malignant tumor. This article reviews the practical steps of an investigation of an isolated adenopathy in an adult patient.

In situ fluorescence imaging of glutamate-evoked mitochondrial Na+ responses in astrocytes.

Astrocytes can experience large intracellular Na+ changes following the activation of the Na+-coupled glutamate transport. The present study investigated whether cytosolic Na+ changes are transmitted to mitochondria, which could therefore influence their function and contribute to the overall intracellular Na+ regulation. Mitochondrial Na+ (Na+(mit)) changes were monitored using the Na+-sensitive fluorescent probe CoroNa Red (CR) in intact primary cortical astrocytes, as opposed to the classical isolated mitochondria preparation. The mitochondrial localization and Na+ sensitivity of the dye were first verified and indicated that it can be safely used as a selective Na+(mit) indicator. We found by simultaneously monitoring cytosolic and mitochondrial Na+ using sodium-binding benzofuran isophthalate and CR, respectively, that glutamate-evoked cytosolic Na+ elevations are transmitted to mitochondria. The resting Na+(mit) concentration was estimated at 19.0 +/- 0.8 mM, reaching 30.1 +/- 1.2 mM during 200 microM glutamate application. Blockers of conductances potentially mediating Na+ entry (calcium uniporter, monovalent cation conductances, K+(ATP) channels) were not able to prevent the Na+(mit) response to glutamate. However, Ca2+ and its exchange with Na+ appear to play an important role in mediating mitochondrial Na+ entry as chelating intracellular Ca2+ with BAPTA or inhibiting Na+/Ca2+ exchanger with CGP-37157 diminished the Na+(mit) response. Moreover, intracellular Ca2+ increase achieved by photoactivation of caged Ca2+ also induced a Na+(mit) elevation. Inhibition of mitochondrial Na/H antiporter using ethylisopropyl-amiloride caused a steady increase in Na+(mit) without increasing cytosolic Na+, indicating that Na+ extrusion from mitochondria is mediated by these exchangers. Thus, mitochondria in intact astrocytes are equipped to efficiently sense cellular Na+ signals and to dynamically regulate their Na+ content.

Targeting vascular NADPH oxidase 1 blocks tumor angiogenesis through a PPARα mediated mechanism.

Reactive oxygen species, ROS, are regulators of endothelial cell migration, proliferation and survival, events critically involved in angiogenesis. Different isoforms of ROS-generating NOX enzymes are expressed in the vasculature and provide distinct signaling cues through differential localization and activation. We show that mice deficient in NOX1, but not NOX2 or NOX4, have impaired angiogenesis. NOX1 expression and activity is increased in primary mouse and human endothelial cells upon angiogenic stimulation. NOX1 silencing decreases endothelial cell migration and tube-like structure formation, through the inhibition of PPARα, a regulator of NF-κB. Administration of a novel NOX-specific inhibitor reduced angiogenesis and tumor growth in vivo in a PPARα dependent manner. In conclusion, vascular NOX1 is a critical mediator of angiogenesis and an attractive target for anti-angiogenic therapies.

Atomic force microscopy imaging of living cells

Over the last two decades, Atomic Force Microscopy (AFM) has emerged as the tool of choice to image living organisms in a near-physiological environment. Whereas fluorescence microscopy techniques allow labeling and tracking of components inside cells and the observation of dynamic processes, AFM is mainly a surface technique that can be operated on a wide range of substrates including biological samples. AFM enables extraction of topographical, mechanical and chemical information from these samples.

Feasibility of direct mapping of cerebral fluorodeoxy-D-glucose metabolism in situ at subcellular resolution using soft X-ray fluorescence.

Glucose metabolism is difficult to image with cellular resolution in mammalian brain tissue, particularly with (18) fluorodeoxy-D-glucose (FDG) positron emission tomography (PET). To this end, we explored the potential of synchrotron-based low-energy X-ray fluorescence (LEXRF) to image the stable isotope of fluorine (F) in phosphorylated FDG (DG-6P) at 1 μm(2) spatial resolution in 3-μm-thick brain slices. The excitation-dependent fluorescence F signal at 676 eV varied linearly with FDG concentration between 0.5 and 10 mM, whereas the endogenous background F signal was undetectable in brain. To validate LEXRF mapping of fluorine, FDG was administered in vitro and in vivo, and the fluorine LEXRF signal from intracellular trapped FDG-6P over selected brain areas rich in radial glia was spectrally quantitated at 1 μm(2) resolution. The subsequent generation of spatial LEXRF maps of F reproduced the expected localization and gradients of glucose metabolism in retinal Müller glia. In addition, FDG uptake was localized to periventricular hypothalamic tanycytes, whose morphological features were imaged simultaneously by X-ray absorption. We conclude that the high specificity of photon emission from F and its spatial mapping at ≤1 μm resolution demonstrates the ability to identify glucose uptake at subcellular resolution and holds remarkable potential for imaging glucose metabolism in biological tissue. © 2012 Wiley Periodicals, Inc.

Mechanisms of interaction of therapeutic nanoparticles with cells

Nanoparticles (NPs) have gained a lot of interest in recent years due to their huge potential for applications in industry and medicine. Their unique properties offer a large number of attractive possibilities in the biomedical field, providing innovative tools for diagnosis of diseases and for novel therapies. Nevertheless, a deep understanding of their interactions with living tissues and the knowledge about their possible effects in the human body are necessary for the safe use of nanoparticulate formulations. The aim of this PhD project was to study in detail the interactions of therapeutic NPs with living cells, including cellular uptake and release, cellular localization and transport across the cell layers. Moreover, the effects of NPs on the cellular metabolic processes were determined using adapted in vitro assays. We evaluated the biological effect of several NPs potentially used in the biomedical field, including titanium dioxide (Ti02) NPs, 2-sized fluorescent silica NPs, ultrasmall superparamagnetic iron oxide (USPIO) NPs, either uncoated or coated with oleic acid or with polyvinylamine (aminoPVA) and poly(lactic-co-glycolic acid) - polyethylene-oxide (PLGA-PEO) NPs. We have found that the NPs were internalized by the cells, depending on their size, chemical composition, surface coating and also depending on the cell line considered. The uptake of aminoPVA-coated USPIO NPs by endothelial cells was enhanced in the presence of an external magnetic field. None of the tested USPIO NPs and silica NPs was transported across confluent kidney cell layers or brain endothelial cell layers, even in the presence of a magnetic field. However, in an original endothelium-glioblastoma barrier model which was developed, uncoated USPIO NPs were directly transferred from endothelial cells to glioblastoma cells. Following uptake, Ti02 NPs and uncoated USPIO NPs were released by the kidney cells, but not by the endothelial cells. Furthermore, these NPs induced an oxidative stress and autophagy in brain endothelial cells, possibly associated with their enhanced agglomeration in cell medium. A significant DNA damage was found in brain endothelial cells after their exposure to TiO2NPs. Altogether these results extend the existing knowledge about the effects of NPs on living cells with regard to their physicochemical characteristics and provide interesting tools for further investigation. The development of the in vitro toxicological assays with a special consideration for risk evaluation aims to reduce the use of animal experiments. -Les nanoparticules (NPs) présentent beaucoup d'intérêt dans le domaine biomédical et industriel. Leurs propriétés uniques offrent un grand nombre de possibilités de solutions innovantes pour le diagnostique et la thérapie. Cependant, pour un usage sûr des NPs il est nécessaire d'acquérir une connaissance approfondie des mécanismes d'interactions des NPs avec les tissus vivants et de leur effets sur le corps humain. Le but de ce projet de thèse était d'étudier en détail les mécanismes d'interactions de NPs thérapeutiques avec des cellules vivantes, en particulier les mécanismes d'internalisation cellulaire et leur subséquente sécrétion par les cellules, leur localisation cellulaire, leur transport à travers des couches cellulaires, et l'évaluation des effets de NPs sur le métabolisme cellulaire, en adaptant les méthodes existante d'évaluation cyto-toxico logique s in vitro. Pour ces expériences, les effets biologiques de nanoparticules d'intérêt thérapeutique, telles que des NPs d'oxyde de titane (TiO2), des NPs fluorescents de silicate de 2 tailles différentes, des NPs, d'oxyde de fer super-para-magnétiques ultra-petites (USPIO), soit non- enrobées soit enrobées d'acide oléique ou de polyvinylamine (aminoPVA), et des NPs d'acide poly(lactique-co-glycolique)-polyethylene-oxide (PLGA-PEO) ont été évalués. Les résultats ont démontré que les NPs sont internalisées par les cellules en fonction de leur taille, composition chimique, enrobage de surface, et également du type de cellules utilisées. L'internalisation cellulaire des USPIO NPs a été augmentée en présence d'un aimant externe. Aucune des NPs de fer et de silicate n'a été transportée à travers des couches de cellules épithéliales du rein ou endothéliales du cerveau, même en présence d'un aimant. Cependant, en développant un modèle original de barrière endothélium-glioblastome, un transfert direct de NPs d'oxyde de fer de cellule endothéliale à cellule de glioblastome a été démontré. A la suite de leur internalisation les NPs d'oxyde de fer et de titane sont relâchées par des cellules épithéliales du rein, mais pas des cellules endothéliales du cerveau. Dans les cellules endothéliales du cerveau ces NPs induisent en fonction de leur état d'agglomération un stress oxydatif et des mécanismes d'autophagie, ainsi que des dommages à l'ADN des cellules exposées aux NPs d'oxyde de titane. En conclusion, les résultats obtenus élargissent les connaissances sur les effets exercés par des NPs sur des cellules vivantes et ont permis de développer les outils expérimentaux pour étudier ces effets in vitro, réduisant ainsi le recours à des expériences sur animaux.

Rab3D is critical for secretory granule maturation in PC12 cells.

Neuropeptide- and hormone-containing secretory granules (SGs) are synthesized at the trans-Golgi network (TGN) as immature secretory granules (ISGs) and complete their maturation in the F-actin-rich cell cortex. This maturation process is characterized by acidification-dependent processing of cargo proteins, condensation of the SG matrix and removal of membrane and proteins not destined to mature secretory granules (MSGs). Here we addressed a potential role of Rab3 isoforms in these maturation steps by expressing their nucleotide-binding deficient mutants in PC12 cells. Our data show that the presence of Rab3D(N135I) decreases the restriction of maturing SGs to the F-actin-rich cell cortex, blocks the removal of the endoprotease furin from SGs and impedes the processing of the luminal SG protein secretogranin II. This strongly suggests that Rab3D is implicated in the subcellular localization and maturation of ISGs.

Arterial wall dosimetry for non-Hodgkin lymphoma patients treated with radioimmunotherapy.

Tumors in non-Hodgkin lymphoma (NHL) patients are often proximal to the major blood vessels in the abdomen or neck. In external-beam radiotherapy, these tumors present a challenge because imaging resolution prevents the beam from being targeted to the tumor lesion without also irradiating the artery wall. This problem has led to potentially life-threatening delayed toxicity. Because radioimmunotherapy has resulted in long-term survival of NHL patients, we investigated whether the absorbed dose (AD) to the artery wall in radioimmunotherapy of NHL is of potential concern for delayed toxicity. SPECT resolution is not sufficient to enable dosimetric analysis of anatomic features of the thickness of the aortic wall. Therefore, we present a model of aortic wall toxicity based on data from 4 patients treated with (131)I-tositumomab. METHODS: Four NHL patients with periaortic tumors were administered pretherapeutic (131)I-tositumomab. Abdominal SPECT and whole-body planar images were obtained at 48, 72, and 144 h after tracer administration. Blood-pool activity concentrations were obtained from regions of interest drawn on the heart on the planar images. Tumor and blood activity concentrations, scaled to therapeutic administered activities-both standard and myeloablative-were input into a geometry and tracking model (GEANT, version 4) of the aorta. The simulated energy deposited in the arterial walls was collected and fitted, and the AD and biologic effective dose values to the aortic wall and tumors were obtained for standard therapeutic and hypothetical myeloablative administered activities. RESULTS: Arterial wall ADs from standard therapy were lower (0.6-3.7 Gy) than those typical from external-beam therapy, as were the tumor ADs (1.4-10.5 Gy). The ratios of tumor AD to arterial wall AD were greater for radioimmunotherapy by a factor of 1.9-4.0. For myeloablative therapy, artery wall ADs were in general less than those typical for external-beam therapy (9.4-11.4 Gy for 3 of 4 patients) but comparable for 1 patient (32.6 Gy). CONCLUSION: Blood vessel radiation dose can be estimated using the software package 3D-RD combined with GEANT modeling. The dosimetry analysis suggested that arterial wall toxicity is highly unlikely in standard dose radioimmunotherapy but should be considered a potential concern and limiting factor in myeloablative therapy.