Canine distemper virus : persistence and pathology in the central nervous system

Résumé : Le virus de la maladie de Carré (en anglais: canine distemper virus, CDV) qui est pathogène pour les chiens et autres carnivores, est très semblable au virus de la rougeole humaine (en anglais MV). Ces deux virus font partie du genre des Morbillivirus qui appartient à la famille des Paramyxoviridae. Ils induisent des complications dans le système nerveux central (SNC). Au stade précoce et aigu de l'infection du SNC, le CDV induit une démyélinisation (1). Ce stade évolue dans certains cas vers une infection chronique avec progression de la démyélinisation. Pendant le stade précoce, qui suit en général de trois semaines les premiers symptômes, le processus de démyélinisation est associé à la réplication du virus et n'est pas considéré comme inflammatoire (1). Par contre, au stade chronique, la progression des plaques de démyélinisation semble être plutôt liée à des processus immunogènes caractéristiques (2), retrouvés également dans la sclérose en plaques (SEP) chez les humains. Pour cette raison, le CDV est considéré comme un modèle pour la SEP humaine et aussi pour l'étude des maladies et complications induites par les Morbillivirus en général (3). Dans notre laboratoire, nous avons utilisé la souche A75/17-CDV, qui est considérée comme le modèle des souches neurovirulentes de CDV. Nous avons cherché en premier lieu à établir un système robuste pour infecter des cultures neuronales avec le CDV. Nous avons choisi les cultures primaires de l'hippocampe du nouveau-né de rat (4), que nous avons ensuite infecté avec une version modifiée du A75/17, appelée rgA75/17-V (5). Dans ces cultures, nous avons prouvé que le CDV infecte des neurones et des astrocytes. Malgré une infection qui se diffuse lentement entre les cellules, cette infection cause une mort massive aussi bien des neurones infectés que non infectés. En parallèle, les astrocytes perdent leur morphologie de type étoilé pour un type polygonal. Finalment, nous avons trouvé une augmentation importante de la concentration en glutamate dans le milieu de culture, qui laisse présumer une sécrétion de glutamate par les cultures infectées (6). Nous avons ensuite étudié le mécanisme des effets cytopathiques induits par le CDV. Nous avons d'abord démontré que les glycoprotéines de surface F et H du CDV s'accumulent massivement dans le réticulum endoplasmique (RE). Cette accumulation déclenche un stress du RE, qui est caractérisé par une forte expression du facteur de transcription proapoptotique CHOP/GADD 153 et de le la calreticuline (CRT). La CRT est une protéine chaperonne localisée dans le RE et impliquée dans l'homéostasie du calcium (Ca2+) et dans le repliement des protéines. En transfectant des cellules de Vero avec des plasmides codant pour plusieurs mutants de la glycoprotéine F de CDV, nous avons démontré une corrélation entre l'accumulation des protéines virales dans le RE et l'augmentation de l'expression de CRT, le stress du RE et la perte de l'homéostasie du Ca2+. Nous avons obtenu des résultats semblables avec des cultures de cellules primaires de cerveau de rat. Ces résultats suggèrent que la CRT joue un rôle crucial dans les phénomènes neurodégénératifs pendant l'infection du SNC, notamment par le relazgage du glutamate via le Ca2+. De manière intéressante, nous démontrons également que l'infection de CDV induit une fragmentation atypique de la CRT. Cette fragmentation induit une re-localisation et une exposition sélective de fragments amino-terminaux de la CRT, connus pour êtres fortement immunogènes à la surface des cellules infectées et non infectées. A partir de ce résultat et des résultats précédents, nous proposons le mécanisme suivant: après l'infection par le CDV, la rétention dans le RE des protéines F et H provoque un stress du RE et une perte de l'homéostasie du Ca2+. Ceci induit la libération du glutamate, qui cause une dégénération rapide du SNC (sur plusieurs jours ou semaines) correspondant à la phase aiguë de la maladie chez le chien. En revanche, les fragments amino-terminaux de la CRT libérés à la surface des cellules infectées peuvent avoir un rôle important dans l'établissement d'une démyélinisation d'origine immunogène, typique de la phase chronique de l'infection de CDV. Summary : The dog pathogen canine distemper virus (CDV), closely related to the human pathogen measles virus (MV), belongs to the Morbillivirus genus of the Paramyxoviridae family. Both CDV and NIV induce complications in the central nervous system (CNS). In the acute early stage of the infection in CNS, the CDV infection induces demyelination. This stage is sometimes followed by a late persistent stage of infection with a progression of the demyelinating lesions (1). The acute early stage occurs around three weeks after the infection and demyelinating processes are associated with active virus replication and are not associated to inflammation (1). In contrast during late persistent stage, the demyelination plaque progression seems to be mainly due to an immunopathological process (2), which characteristics are shared in many aspects with the human disease multiple sclerosis (MS). For these reasons, CDV is considered as a model for human multiple sclerosis, as well as for the study of Morbillivirus-mediated pathogenesis (3). In our laboratory, we used the A75/17-CDV strain that is considered to be the prototype of neurovirulent CDV strain. We first sought to establish a well characterized and robust model for CDV infection of a neuronal culture. We chose primary cultures from newborn rat hippocampes (4) that we infected with a modified version of A75/17, called rgA75/17-V (5). In these cultures, we showed that CDV infects both neurons and astrocytes. While the infection spreads only slowly to neighbouring cells, it causes a massive death of neurons, which includes also non-infected neurons. In parallel, astrocytes undergo morphological changes from the stellate type to the polygonal type. The pharmacological blocking of the glutamate receptors revealed an implication of glutamatergic signalling in the virus-mediated cytopathic effect. Finally, we found a drastic increase concentration of glutamate in the culture medium, suggesting that glutamate was released from the cultured cells (6). We further studied the mechanism of the CDV-induced cytopathic effects. We first demonstrated that the CDV surface glycoprotein F and H markedly accumulate in the endoplasmic reticulum (ER). This accumulation triggers an ER stress, which is characterized by increased expression of the proapoptotic transcription factor CHOP/GADD 153 and calreticulin (CRT). CRT is an ER resident chaperon involved in the Ca2+ homeostasis and in the response to misfolded proteins. Transfections of Vero cells with plasmids encoding various CDV glycoprotein mutants reveal a correlation between accumulation of viral proteins in the ER, CRT overexpression, ER stress and alteration of ER Ca2+ homeostasis. Importantly, similar results are also obtained in primary cell cultures from rat brain. These results suggest that CRT plays a crucial role in CNS infection, particularly due to CRT involvement in Ca2+ mediated glutamate releases, and subsequent neurodegenerative disorders. Very intriguingly, we also demonstrated that CDV infection induces an atypical CRT fragmentation, with relocalisation and selective exposure of the highly immunogenic CRT N-terminal fragments at the surface of infected and neighbouring non-infected cells. Altogether our results combined with previous findings suggest the following scenario. After CDV infection, F and H retention alter Ca2+ homeostasis, and induce glutamate release, which in turn causes rapid CNS degeneration (within days or a week) corresponding to the acute phase of the disease in dogs. In contrast, the CRT N-terminal fragments released at the surface of infected cells may rather have an important role in the establishment of the autoimmune demyelination in the late stage of CDV infection.

RANTES/CCL5 and risk for coronary events: results from the MONICA/KORA Augsburg case-cohort, Athero-Express and CARDIoGRAM studies.

BACKGROUND: The chemokine RANTES (regulated on activation, normal T-cell expressed and secreted)/CCL5 is involved in the pathogenesis of cardiovascular disease in mice, whereas less is known in humans. We hypothesised that its relevance for atherosclerosis should be reflected by associations between CCL5 gene variants, RANTES serum concentrations and protein levels in atherosclerotic plaques and risk for coronary events. METHODS AND FINDINGS: We conducted a case-cohort study within the population-based MONICA/KORA Augsburg studies. Baseline RANTES serum levels were measured in 363 individuals with incident coronary events and 1,908 non-cases (mean follow-up: 10.2±4.8 years). Cox proportional hazard models adjusting for age, sex, body mass index, metabolic factors and lifestyle factors revealed no significant association between RANTES and incident coronary events (HR [95% CI] for increasing RANTES tertiles 1.0, 1.03 [0.75-1.42] and 1.11 [0.81-1.54]). None of six CCL5 single nucleotide polymorphisms and no common haplotype showed significant associations with coronary events. Also in the CARDIoGRAM study (>22,000 cases, >60,000 controls), none of these CCL5 SNPs was significantly associated with coronary artery disease. In the prospective Athero-Express biobank study, RANTES plaque levels were measured in 606 atherosclerotic lesions from patients who underwent carotid endarterectomy. RANTES content in atherosclerotic plaques was positively associated with macrophage infiltration and inversely associated with plaque calcification. However, there was no significant association between RANTES content in plaques and risk for coronary events (mean follow-up 2.8±0.8 years). CONCLUSIONS: High RANTES plaque levels were associated with an unstable plaque phenotype. However, the absence of associations between (i) RANTES serum levels, (ii) CCL5 genotypes and (iii) RANTES content in carotid plaques and either coronary artery disease or incident coronary events in our cohorts suggests that RANTES may not be a novel coronary risk biomarker. However, the potential relevance of RANTES levels in platelet-poor plasma needs to be investigated in further studies.

Management of patients with uveal metastases at the Liverpool Ocular Oncology Centre.

BACKGROUND: Uveal metastasis is the most common intraocular malignancy. METHODS: This was a retrospective study of all patients with uveal metastases referred to the Liverpool Ocular Oncology Centre between January 2007 and December 2012. Biopsy was performed as a primary investigation if the clinical examination suggested metastasis with no evidence of any extraocular metastases. RESULTS: Ninety-six patients (109 eyes) were included. Breast and lung carcinomas were the most common primary malignancies, affecting 41 and 27 patients, respectively. The median time interval between detection of primary cancer and uveal metastasis was 24 months (range 1-288 months). Thirty-nine patients underwent ocular biopsy, confirming the diagnosis in all patients. The biopsy indicated the site of origin in 24 out of the 27 without a known primary tumour. In 7 of these 27 cases, previous systemic investigations had failed to identify the primary tumour. Seventy-three patients received external beam irradiation; two patients received photodynamic therapy; and two patients had Ru-106 plaque radiotherapy. The visual acuity was stable or improved in 75.5% of the cases. CONCLUSIONS: Immediate biopsy provides a quick diagnosis that may expedite treatment and improve any opportunities for conserving vision while facilitating the general oncologic management on these patients.

Contribution to the geology of Southern Turkey: new insights from the Mersin mélanges and from the Lycian and Antalya nappes

Abstract The study of fossil Tethyan continental margins implies the consideration of the oceanic domains to which they were connected. The advent of plate tectonics confirmed the importance of the detection of accretion-related mélanges. Ophiolitic mélanges are derived from both an upper ophiolitic obducting plate and a lower oceanic plate. Besides ophiolitic elements, the mélanges may incorporate parts of a magmatic arc and dismembered fragments of a passive continental margin. As the lower plate usually totally disappears during the obduction process, it can only be reconstructed from its elements found in the mélanges. Because of their key location at active margin boundaries, preserved accretion-related mélanges provide strong constraints on the geological evolution of former oceanic domains and their adjacent margins. The identification of Palaeotethyan remnants as accretionary series or reworked during the Late Triassic Eo-Cimmerian event, as well as the recognition of HugluPindos marginal sequences in southern Turkey and in the external Hellenides represent the main achievements of this work, making possible to establish new palaeogeographical correlations. The Mersin mélanges (Turkey), together with the Antalya and Mamonia (Cyprus) domains, are characterized by a series of exotic units found now south of the main Taurus range and compose the South-Taurides Exotic Units. The Mersin mélanges are subdivided in a Triassic and a Late Cretaceous unit. These units consist of the remnants of three major Tethyan oceans, the Palaeotethys, the Neotethys and the Huglu-Pindos. The definition and inventory of the Upper Antalya Nappes (Turkey) are still a matter of controversies and often conflicting interpretations. The recognition of Campanian radiolarians on top of the Kerner Gorge unit directly overlain by the Ordovician Seydi§ehir Fm. of the Tahtah Dag Nappe outlines a tectonic contact and demonstrates that the Upper Antalya Nappes system is composed of three different nappes, the Kerner Gorge, Bakirli and the Tahtah Dag nappes. Additionally, a limestone block in a doubtful tectonic position at the base of the Upper Antalya Nappes yielded for the first time two middle Viséan associations of foraminifers and problematic algae. The Tavas Nappe in the Lycian Nappes (Turkey) is classically divided into the Karadag, Teke Dere, Köycegiz and Haticeana units. As for the Mersin mélanges, the Tavas Nappe is highly composite and includes dismembered units belonging to the Palaeotethyan, Neotethyan and HugluPindos realms. The Karadag unit consists of a Gondwana-type platform succession ranging from the Late Devonian to the Late Triassic. It belongs to the Cimmerian Taurus terrane and was part of the northern passive margin of the Neotethys. The Teke Dere unit is composed of different parts of the Palaeotethyan succession including Late Carboniferous OIB-type basalts, Carboniferous MORB-type basalts, an Early Carboniferous siliciclastic series and a Middle Permian arc sequence. The microfauna and microflora identified in different horizons within the Teke Dere unit share strong biogeographical affinities with the northern Palaeotethyan borders. Kubergandian limestones in primary contact above the Early Carboniferous siliciclastics yielded a rich and diverse microfauna and microflora also identified in reworked cobbles within the Late Triassic Gevne Fm. of the Aladag unit (Turkey). The sedimentological evolution of the Köycegiz and Haticeana series is in many points similar to classical Pindos sequences. These series originated in the Huglu-Pindos Ocean along the northern passive margin of the Anatolian (Turkish transect) and Sitia-Pindos (Greek transect) terranes. Conglomerates at the base of the Lentas Unit in southern Crete (Greece) yielded a microfauna and microflora presenting also strong affinities with the northern borders of the Palaeotethys. This type of reworked sediments at the base of Pindos-like series would suggest a derivation from the Palaeotethyan active margin. -Résumé (French abstract) L'étude des marges continentales fossiles de l'espace téthysien implique d'étudier les domaines océaniques qui y étaient rattachés. Les progrès de la tectonique des plaques ont confirmé l'importance de la reconnaissance des mélanges d'accrétion. Les mélanges ophiolitiques dérivent d'une plaque supérieure ophiolitique qui obducte, et d'une plaque inférieure océanique. En plus d'éléments ophiolitiques, les mélanges peuvent aussi incorporer des parties d'un arc magmatique, ou des fragments d'une marge continentale passive. Comme la plaque inférieure disparaît généralement complètement durant le processus d'obduction, elle ne peut être reconstruite qu'au travers de ses éléments trouvés dans les mélanges. A cause de leur situation aux limites de marges actives, les mélanges d'accrétion bien préservés permettent de contraindre l'évolution géologique d'anciens océans et de leurs marges. L'identification de vestiges de la Paléotéthys en série d'accrétion ou remaniés lors de l'orogenèse éo-cimmérienne au Trias supérieur, ainsi que l'observation de séquences marginales de Huglu-Pinde en Turquie du sud et dans les Hellénides externes représentent les principaux résultats de ce travail, permettant d'établir de nouvelles corrélations paléogéographiques. Les mélanges de Mersin (Turquie), avec les domaines d'Antalya et de Mamonia (Chypre), sont caractérisés par des unités exotiques se trouvant au sud de la chaîne taurique, et forment les Unités Exotiques Sud-Tauriques. Les mélanges de Mersin sont subdivisés en une unité triasique, et une autre du Crétacé supérieur. Ces unités comprennent les reliques de trois principaux océans téthysiens, la Paléotéthys, la Néotéthys et Huglu-Pinde. L'inventaire et la définition des nappes supérieures d'Antalya (Turquie) sont encore matière à controverse et donne lieu à des interprétations conflictuelles. La découverte de radiolaires campaniens au sommet de l'unité de la Gorge de Kemer, directement recouverts par la formation ordovicienne de Seydisehir de la nappe du Tahtali Dag met en évidence un contact tectonique et démontre que les nappes supérieures sont composées de trois différentes nappes, celle de la Gorge de Kemer, celle du Bakirli et celle Tahtali Dag. De plus, un bloc de calcaire dont la position tectonique demeure incertaine à la base des nappes supérieures a fourni pour la première fois deux associations viséennes de foraminifères et d'algues problématiques. La nappe de Tavas dans les nappes lyciennes (Turquie) est séparée en unités du Karadag, du Teke Dere, de Köycegiz et d'Haticeana. Comme pour les mélanges de Mersin, la nappe de Tavas est composite et inclut des unités appartenant à la Paléotéthys, à la Néotéthys et à Huglu-Pinde. L'unité du Karadag est une plateforme carbonatée de type Gondwana se développant du Dévonien supérieur au Trias supérieur. Elle appartient au domaine cimmérien du Taurus et formait la marge nord de la Néotéthys. L'unité du Teke Dere est composée de différentes écailles paléotéthysiennes et inclut des basaltes d'île océanique du Carbonifère supérieur, des basaltes de ride océanique du Carbonifère, une série siliciclastique du Carbonifère supérieur et un arc du Permien moyen. Les microfaunes et -flores trouvées à différents niveaux de la série du Teke Dere partagent de fortes affinités paléogéographiques avec les marges nord de la Paléotéthys. Des calcaires du Kubergandien en contact primaire au-dessus de la série siliciclastique a donné de riches microfaunes et -flores, également identifiées dans des galets remaniés dans la formation de Gevne du Trias supérieur de l'Aladag. L'évolution sédimentologique des séries de Köycegiz et d'Haticeana sont très similaires aux séries classiques du Pinde. Ces séquences prennent leur racine dans l'océan de Huglu-Pinde, le long de la marge passive nord anatolienne (profil turc) et de la marge de Sitia-Pinde (profil grec). Des conglomérats à la base de l'unité de Lentas au sud de la Crète (Grèce) ont donné des microfaunes et flores partageant également de fortes similitudes avec les bordures nord de la Paléotéthys. Le type de sédiments remaniés à la base d'unités de type Pinde suggère une dérivation depuis la marge active de la Paléotéthys. -Résumé grand public (non-specialized abstract) Au début du 20ème siècle, Alfred Wegener bouleverse les croyances géologiques de l'époque et publie plusieurs articles sur la dérive ou la translation des continents. En utilisant des arguments géographiques (similarités des lignes de côte), paléontologiques (faunes et flores similaires) et climatiques (dépôts tropicaux et glaciaires), Wegener explique qu'il y a plusieurs millions d'années, les terres émergées actuelles ne devaient former qu'un seul et grand continent. La fin du 20ème siècle verra l'avènement de la théorie de la tectonique des plaques suite à la reconnaissance du cycle de Wilson, des rides médio-océaniques, des anomalies magnétiques dans les océans et des sutures océaniques qui représentent les reliques d'océans disparus. Le Cycle de Wilson se caractérise par une suite d'évènements géologiques majeurs pouvant se résumer de la manière suivante : (1) séparation d'un craton continental en deux parties, créant une limite de plaque divergente. C'est ce que l'on appelle un rift; (2) développement et croissance d'un océan entre ces deux blocs. Des roches magmatiques remontent à la surface de la terre et forment une chaîne de montagne sous-marine que l'on appelle ride médio-océanique ou dorsale. L'océan continue de se développer, et des sédiments se déposent à sa surface formant la suite ophiolitique ou trinité de Steinmann; (3) après une phase d'expansion plus ou moins longue, les conditions imposées aux limites des plaques à la surface de la terre changent, et l'océan se met à se refermer par disparition progressive (subduction) de sa croûte océanique sous une croûte continentale par exemple. Ceci crée une nouvelle limite de plaque, convergente cette fois; (4) la subduction de la plaque océanique sous la plaque continentale provoque une remontée de magma formant des chaînes volcaniques à la surface de la Terre ; (5) une fois que la plaque océanique a complètement disparu, les deux blocs préalablement séparés par l'océan font collision, formant ainsi une chaîne de montagne. Les chaînes de montagnes sont de manière générale formées par un empilement plus ou moins complexe de nappes. C'est au coeur de certaines de ces nappes que se trouvent les vestiges de l'océan disparu. Un des objectifs de ce travail était la recherche de ces vestiges dans le domaine téthysien de la Méditerranée orientale. Pour ce faire, nous avons parcourus une grande partie du sud de la Turquie, nous sommes allés à Chypre, dans le Sultanat d'Oman, en Iran, en Crète, et nous avons visités quelques îles grecques du Dodécanèse. La région de la Méditerranée orientale est une zone qui a été tectoniquement très active, et qui continue de l'être de nos jours par des phénomènes de subduction (ex. les volcans de Santorin), et par des mouvements coulissants entre des plaques continentales (ex. la faille nord-anatolienne) qui donnent régulièrement lieu à des tremblements de terre. Pour le géologue, la complexité de ces zones d'étude réside dans le fait que les chaînes de montagne actuelles ne contiennent en général pas seulement les restes d'un océan, mais bien de plusieurs bassins océaniques qui se sont succédés dans l'espace et dans le temps. Les nappes qui se trouvent au sud de la Turquie et dans le Dodécanèse forment un important jalon dans la chaîne alpine qui s'étend depuis les Alpes jusque dans l'Himalaya. L'idée d'un continuum au coeur de ce système se basait principalement sur l'âge des océans et sur la reconnaissance de similarités dans l'évolution des séries sédimentaires. La localisation des vestiges de la Paléotéthys ainsi que l'identification des séries sédimentaires ayant appartenu à l'océan de HugluPinde repris sous forme de nappes en Turquie et en Grèce sont cruciales pour permettre de bonnes corrélations locales et régionales. La reconnaissance, la compréhension et l'interprétation de ces séries sédimentaires permettront d'élaborer un modèle d'évolution géodynamique régional, s'appuyant sur des faits de terrains indiscutables, et prenant en compte les contraintes globales que ce genre d'exercice implique.

Role of Notch signaling in epidermis and appendages

Résumé Dans la peau, il a été montré que Notch1 induit l'arrêt de la prolifération et la différentiation des keratinocytes. L'inactivation de Notch1 cause une hyperplasie de l'épiderme et la formation de carcinomes basaux cellulaires. Notre groupe a principalement identifié deux voies de signalisations, la voie Shh et la voie Wnt, qui sont dérégulées en conséquence de l'inactivation de Notch1 dans la peau. Nous avons démontré l'habilité de Notch1 à réprimer la voie Wnt induite par ß-catenin dans les keratinocytes primaires ainsi que dans d'autres types de cellules épithéliales humaines. De plus, nous avons pu déterminer que Notch1 régule cette voie, probablement en favorisant la phosphorylation de ß-catenin par le complexe axin/APC/GSK-3ß. La protéine faisant partie de la voie Wnt, ou la protéine affectant la voie Wnt, qui est régulée par Notch1 est sujette à de plus amples investigations. Un autre but de cette étude a été l'identification de potentiels gènes cibles de Notch1 autres que ceux faisant partie des voies de signalisation Shh et Wnt précédemment évoquées. Ce projet fut abordé par l'analyse de puces à ADN (ISREC et Affymetrix) qui ont été utilisées pour des expériences de gain et de perte de fonction de Notch1 dans des keratinocytes prúmaires. En plus de l'hyperplasie épidermale, les souris Notch1 déficiente ont une perte importante de poils. Nous avons montré que Notch1 est nécessaire pour le développement et l'homéostasie des follicules pileux. En effet, l'inactivation du gène Notch1 mediée par l'activation des kératines 5 ou 14 dans l'épiderme, cause des défauts du cycle ainsi que de la structure des poils. De plus, d'autres appendices de la peau, comme les glandes sudoripares et de Meibomius, ont une structure anormale et sont non fonctionnelles dans les souris Notch1 déficiente. Finalement, nous avons observé que la déficience de Notch1 dans l'épithélium cornéen mène à la formation d'une plaque épidermale opaque sur la cornée. Basé sur l'hypothèse que le défaut des glandes de Meibomius des souris Notch1 déficientes cause des lésions de la surface oculaire, nous avons montré que Notch1 est essentiel pour la cicatrisation de la cornée. Lorsque Notch1 est absent, les cellules souches de l'épithélium cornéen ne sont plus capables de se différentier en cellules cornéennes, mais réparent la blessure en se différentiant en épiderme. Ce résultat indique que Notch1 est essentiel pour la différentiation de cellules souches de la cornée qui sont spécifiquement impliquées dans la réparation de la cornée. De plus, nous avons montré que l'expression de CRBP1 dans l'épithélium cornéen est diminuée en l'absence de Notch1, ceci étant possiblement à l'origine de la formation de la plaque épidermale. Abstract: In the skin, Notch1 has been shown to trigger cell growth arrest and differentiation of keratinocytes. Notch1 inactivation results in epidermal hyperplasia and subsequent formation of basal cell carcinoma-like (BCC-like) tumors. So far our group has identified two main pathways, the Shh and the Wnt pathway, that are deregulated as a consequence of Notch1 inactivation in the skin. We showed the ability of Notch1 to represses ß-catenin-mediated Wnt signaling in primary keratinocytes as well as in other types of human epithelial cells. In addition we were able to determine that Notch1 regulates this pathway possibly by enhancing ß-catenin phosphorylation by the axin/APC/GSK-3ß complex. The exact target protein of the Wnt pathway or target protein that affects the Wnt pathway, and that is regulated by Notch1, is subject of current investigation. Another aim of this study was the identification of possible Notch1 target genes in addition to those of the Shh and Wnt signaling pathways. This was addressed by gene chip analysis using ISREC as well as Affymetrix microarrays for gain and loss of function of Notch1 in mouse primary keratinocytes. In addition to epidermal hyperplasia, Notch1 deficient mice show an important hair loss. We showed that Notch1 is required for postnatal development and homeostasis of hair follicles. Indeed, keratin5 or keratinl4-driven Cre recombinase-mediated inactivation of the Notch1 gene in the epidermis causes perturbations of the hair cycle and structural defects of the hair follicle. Moreover, other skin appendages, like the sweat and Meibomian glands show abnormal morphology and are not functional in the Notch 1 deficient mice. Finally, we observed that Notch1 deficiency in the corneal epithelium leads to the formation of an epidermal corneal plaque. Based on the hypothesis that the Meiboinian gland defect in the Notch1 deficient mice results in lesions of the eye surface, we showed that Notch1 is essential for wound-healing of the cornea. In absence of Notch1 the stem cells of the corneal epithelium are no longer able to differentiate in the corneal fate but instead repair the wound by differentiating into skin-like epidermis. This result indicated that Notch1 is essential for the differentiation of corneal stem cells specifically implicated in corneal wound-healing. Moreover, we showed that CRBP1 expression in the corneal epithelium was lost in the absence of Notch1, possibly being at the origin of plaque formation.

Rate and processes of river network rearrangement during incipient faulting: The case of the Cahabon river, Guatemala

Deeply incised river networks are generally regarded as robust features that are not easily modified by erosion or tectonics. Although the reorganization of deeply incised drainage systems has been documented, the corresponding importance with regard to the overall landscape evolution of mountain ranges and the factors that permit such reorganizations are poorly understood. To address this problem, we have explored the rapid drainage reorganization that affected the Cahabon River in Guatemala during the Quaternary. Sediment-provenance analysis, field mapping, and electrical resistivity tomography (ERT) imaging are used to reconstruct the geometry of the valley before the river was captured. Dating of the abandoned valley sediments by the Be-10-Al-26 burial method and geomagnetic polarity analysis allow us to determine the age of the capture events and then to quantify several processes, such as the rate of tectonic deformation of the paleovalley, the rate of propagation of post-capture drainage reversal, and the rate at which canyons that formed at the capture sites have propagated along the paleovalley. Transtensional faulting started 1 to 3 million years ago, produced ground tilting and ground faulting along the Cahabon River, and thus generated differential uplift rate of 0.3 +/- 0.1 up to 0.7 +/- 0.4 mm . y(-1) along the river's course. The river responded to faulting by incising the areas of relative uplift and depositing a few tens of meters of sediment above the areas of relative subsidence. Then, the river experienced two captures and one avulsion between 700 ky and 100 ky. The captures breached high-standing ridges that separate the Cahabon River from its captors. Captures occurred at specific points where ridges are made permeable by fault damage zones and/or soluble rocks. Groundwater flow from the Cahabon River down to its captors likely increased the erosive power of the captors thus promoting focused erosion of the ridges. Valley-fill formation and capture occurred in close temporal succession, suggesting a genetic link between the two. We suggest that the aquifers accumulated within the valley-fills, increased the head along the subterraneous system connecting the Cahabon River to its captors, and promoted their development. Upon capture, the breached valley experienced widespread drainage reversal toward the capture sites. We attribute the generalized reversal to combined effects of groundwater sapping in the valley-fill, axial drainage obstruction by lateral fans, and tectonic tilting. Drainage reversal increased the size of the captured areas by a factor of 4 to 6. At the capture sites, 500 m deep canyons have been incised into the bedrock and are propagating upstream at a rate of 3 to 11 mm . y(-1) deepening at a rate of 0.7 to 1 5 mm . y(-1). At this rate, 1 to 2 million years will be necessary for headward erosion to completely erase the topographic expression of the paleovalley. It is concluded that the rapid reorganization of this drainage system was made possible by the way the river adjusted to the new tectonic strain field, which involved transient sedimentation along the river's course. If the river had escaped its early reorganization and had been given the time necessary to reach a new dynamic equilibrium, then the transient conditions that promoted capture would have vanished and its vulnerability to capture would have been strongly reduced.

Clonal analysis of the BALB/c T cell proliferative response to apo beef cytochrome c.

Murine T cell clones that proliferated specifically in response to the protein antigen apo cytochrome c were derived and maintained in continuous culture. Two distinct clonotypes were observed with respect to the proliferative responses observed when a variety of peptides prepared from several species of cytochrome c were tested. These 2 clonotypes appeared to recognize 2 different regions in the cytochrome c molecule. Only 1 of the 2 clonotypes tested demonstrated helper cell activity for antibody formation in vitro.

Molecular imaging of matrix metalloproteinases in atherosclerotic plaques.

Ischaemic stroke and myocardial infarction often result from the sudden rupture of an atherosclerotic plaque. The subsequent arterial thrombosis occluding the vessel lumen has been widely indicated as the crucial acute event causing peripheral tissue ischaemia. A complex cross-talk between systemic and intraplaque inflammatory mediators has been shown to regulate maturation, remodeling and final rupture of an atherosclerotic plaque. Matrix metalloproteinases (MMPs) are proteolytic enzymes (released by several cell subsets within atherosclerotic plaques), which favour atherogenesis and increase plaque vulnerability. Thus, the assessment of intraplaque levels and activity of MMP might be of pivotal relevance in the evaluation of the risk of rupture. New imaging approaches, focused on the visualisation of inflammation in the vessel wall and plaque, may emerge as tools for individualised risk assessment and prevention of events. In this review, we summarize experimental findings of the currently available invasive and noninvasive imaging techniques, used to detect the presence and activity of MMPs in atherosclerotic plaques.

Maturation of the lymphoid system. III. Induction of selective unresponsiveness by injection of a haptenated carbohydrate into neonatal mice.

Neonatal treatment of A/J mice with DNP-Ficoll reduced or eliminated indirect anti-DNP PFC normally produced in response to adult challenge with DNP-keyhole limpet hemocyanin. The remaining direct anti-DNP PFC response was of low avidity. Spleen cells from neonatal A/J mice inhibited the in vitro but not the in vivo response of adult spleen cells to DNP-Ficoll.

The antimicrobial peptide LL37 is a T-cell autoantigen in psoriasis.

Psoriasis is a common T-cell-mediated skin disease with 2-3% prevalence worldwide. Psoriasis is considered to be an autoimmune disease, but the precise nature of the autoantigens triggering T-cell activation remains poorly understood. Here we find that two-thirds of patients with moderate-to-severe plaque psoriasis harbour CD4(+) and/or CD8(+) T cells specific for LL37, an antimicrobial peptide (AMP) overexpressed in psoriatic skin and reported to trigger activation of innate immune cells. LL37-specific T cells produce IFN-γ, and CD4(+) T cells also produce Th17 cytokines. LL37-specific T cells can infiltrate lesional skin and may be tracked in patients blood by tetramers staining. Presence of circulating LL37-specific T cells correlates significantly with disease activity, suggesting a contribution to disease pathogenesis. Thus, we uncover a role of LL37 as a T-cell autoantigen in psoriasis and provide evidence for a role of AMPs in both innate and adaptive immune cell activation.

Two-stage prograde and retrograde Variscan metamorphism of glaucophane-eclogites, blueschists and greenschists from Ile de Groix (Brittany, France)

On Ile de Groix, Variscan metamorphic former tholeiitic and alkaline basalts occur as glaucophane-eclogites, blueschists and greenschists in isolated lenses and layers within metapelites. Whole-rock delta O-18(SMOW) values of the metabasites show limited variations (10.4-12.0 parts per thousand) and no systematic differences among rock types and metamorphic grades. This provides no argument for large-scale blueschist-to-greenschist transformation driven by infiltration of externally derived fluids. Metamorphic mineralogical changes should have been triggered by internal fluids. Element variations in interlayered blue- and greenschists can be attributed to magmatic fractionation. Assemblages with garnet, clinopyroxene and glaucophane of a high-pressure/low-temperature (HP-LT) metamorphism M1, and NaCa-amphiboles (barroisite, magnesiohornblende, actinolite) of a medium-pressure/medium-temperature metamorphism M2 crystallized during deformation Dl. Detailed core-rim zonation profiles display increasing and then decreasing Al-IV in glaucophane of M1. NaCa-amphiboles of M2, mantling glaucophane and crystallized in porphyroblasts, show first increasing, then decreasing, Al-IV and Al-IV. Empirically calibrated thermobarometers allowed P-T path reconstructions. In glaucophane-eclogites of a metamorphic zone I, a prograde evolution to M1 peak conditions at 400-500 degreesC/10-12 kbar was followed by a retrograde P-T path within the glaucophane stability field. The subsequent M2 evolution was again prograde up to > 600 degreesC at 8 kbar and then retrograde. Similarly, in metamorphic zones II and III, prograde and retrograde paths of MI and M2 at lower maximal temperatures and pressures exist. The almost complete metamorphic cycle during M2 signalizes that the HP-LT rocks escaped from an early erosion by a moderate second burial event and explains the longlasting slow uplift with low average cooling rates.

A mutation in the gene encoding the vaccinia virus 37,000-M(r) protein confers resistance to an inhibitor of virus envelopment and release.

Plaque formation in vaccinia virus is inhibited by the compound N1-isonicotinoyl-N2-3-methyl-4-chlorobenzoylhydrazine (IMCBH). We have isolated a mutant virus that forms wild-type plaques in the presence of the drug. Comparison of wild-type and mutant virus showed that both viruses produced similar amounts of infectious intracellular naked virus in the presence of the drug. In contrast to the mutant, no extracellular enveloped virus was obtained from IMCBH-treated cells infected with wild-type virus. Marker rescue experiments were used to map the mutation conferring IMCBH resistance to the mutant virus. The map position coincided with that of the gene encoding the viral envelope antigen of M(r) 37,000. Sequence analysis of both wild-type and mutant genes showed a single nucleotide change (G to T) in the mutant gene. In the deduced amino acid sequence, the mutation changes the codon for an acidic Asp residue in the wild-type gene to one for a polar noncharged Tyr residue in the mutant.

Leukocyte-derived microparticles in vascular homeostasis.

Leukocyte-derived microparticles (LMPs) may originate from neutrophils, monocytes/macrophages, and lymphocytes. They express markers from their parental cells and harbor membrane and cytoplasmic proteins as well as bioactive lipids implicated in a variety of mechanisms, maintaining or disrupting vascular homeostasis. When they carry tissue factor or coagulation inhibitors, they participate in hemostasis and pathological thrombosis. Both proinflammatory and anti-inflammatory processes can be affected by LMPs, thus ensuring an appropriate inflammatory response. LMPs also play a dual role in the endothelium by either improving the endothelial function or inducing an endothelial dysfunction. LMPs are implicated in all stages of atherosclerosis. They circulate at a high level in the bloodstream of patients with high atherothrombotic risk, such as smokers, diabetics, and subjects with obstructive sleep apnea, where their prolonged contact with the vessel wall may contribute to its overall deterioration. Numbering microparticles, including LMPs, might be useful in predicting cardiovascular events. LMPs modify the endothelial function and promote the recruitment of inflammatory cells in the vascular wall, necessary processes for the progression of the atherosclerotic lesion. In addition, LMPs favor the neovascularization within the vulnerable plaque and, in the ruptured plaque, they take part in coagulation and platelet activation. Finally, LMPs participate in angiogenesis. They might represent a novel therapeutic tool to reset the angiogenic switch in pathologies with altered angiogenesis. Additional studies are needed to further investigate the role of LMPs in cardiovascular diseases. However, large-scale studies are currently difficult to set up because microparticle measurement still requires elaborate techniques which lack standardization.

Carbon isotope stratigraphy and carbonate production during the Early-Middle Jurassic: examples from the Umbria-Marche-Sabina Apennines (Central Italy)

The carbon isotopic signature of carbonates depends on secular variations of organic carbon and carbonate carbon production/burial rates. A decrease in carbonate productivity makes the organic/carbonate carbon ratio unstable up to the point that even minor variations in the organic carbon reservoirs can provoke carbon isotopic shifts. The delta(13)C positive shifts of the middle Carixian (early Pliensbachian) and the early Bajocian recorded in the Umbria-Marche-Sabina domain represent a good example of this mechanism. Both sedimentology and lithostratigraphy of pelagic platform-basin carbonate systems in this area show that important changes in the source of carbonates correspond to the observed isotopic shifts. The middle Carixian event is in fact well correlatable to the drastic reduction of benthic carbonate production on rift-related intrabasinal highs, which then became pelagic carbonate platforms. The early Bajocian event is concomitant with the beginning of a long hiatus on the pelagic carbonate platforms and with a drop of the biodiversity of calcareous organisms followed by the onset of biosiliceous sedimentation in basins. (C) 2002 Elsevier Science B.V. All rights reserved.

Disentangling the Hettangian carbon isotope record: Implications for the aftermath of the end-Triassic mass extinction

This study provides an organic carbon stable isotope (delta(13)C(org)) record calibrated with detailed ammonite biostratigraphy, following the end-Triassic biological crisis. Precise correlation between this crucial fossil group and the delta(13)C(org) record is key to understanding feedbacks between biological and environmental events following mass extinction. The latest Triassic and Hettangian delta(13)C(org) record shows several negative and positive excursions. The end-Triassic negative shift coinciding with the mass extinction interval is followed by a positive excursion in the earliest Hettangian Psiloceras spelae beds, which marks the onset of recovery in the marine ecosystem. This positive trend is interrupted by a second negative delta(13)C(org) excursion in the P. pacificum beds related to a minor ammonite extinction event. This pattern of the delta(13)C(org) curve culminates in the uppermost Hettangian Angulata Zone major positive excursion. This indicates that both the ecosystem and the carbon cycle remained in a state of perturbation for at least 2 Ma, although the recovery of some pelagic taxa already began at the base of Jurassic. The early and late Hettangian positive delta(13)C(org) excursions have been confused in several recent papers. Here, we show that during the Hettangian there are indeed two distinct positive delta(13)C(org) excursions. Phases of anoxia and further pulses of Central Atlantic Magmatic Province volcanism during the Hettangian might have inhibited the full recovery for that interval of time. The main Liasicus-Angulata organic positive CIE (carbon isotope excursion) during the Late Hettangian might be related to gradual decreasing of pCO(2) due to protracted high organic burial, and coincides with a second phase of recovery, as indicated by a pulse of ammonoid diversification.