The ocular albinism type 1 gene product is a membrane glycoprotein localized to melanosomes.

Ocular albinism type 1 (OA1) is an inherited disorder characterized by severe reduction of visual acuity, photophobia, and retinal hypopigmentation. Ultrastructural examination of skin melanocytes and of the retinal pigment epithelium reveals the presence of macromelanosomes, suggesting a defect in melanosome biogenesis. The gene responsible for OA1 is exclusively expressed in pigment cells and encodes a predicted protein of 404 aa displaying several putative transmembrane domains and sharing no similarities with previously identified molecules. Using polyclonal antibodies we have identified the endogenous OA1 protein in retinal pigment epithelial cells, in normal human melanocytes and in various melanoma cell lines. Two forms of the OA1 protein were identified by Western analysis, a 60-kDa glycoprotein and a doublet of 48 and 45 kDa probably corresponding to unglycosylated precursor polypeptides. Upon subcellular fractionation and phase separation with the nonionic detergent Triton X-114, the OA1 protein segregated into the melanosome-rich fraction and behaved as an authentic integral membrane protein. Immunofluorescence and immunogold analyses on normal human melanocytes confirmed the melanosomal membrane localization of the endogenous OA1 protein, consistent with its possible involvement in melanosome biogenesis. The identification of a novel melanosomal membrane protein involved in a human disease will provide insights into the mechanisms that control the cell-specific pathways of subcellular morphogenesis.

Retinal and lenticular ultrastructure in the aestivating salamanderfish, Lepidogalaxias salamandroides (Galaxiidae, Teleostei) with special reference to a new type of photoreceptor mosaic

The salamanderfish, Lepidogalaxias salamandroides (Galaxiidae, Teleostei) is endemic to southwestern Australia and inhabits shallow, freshwater pools which evaporate during the hot summer months. Burrowing into the substrate in response to falling water levels allows these fish to aestivate for extended periods of time while encapsulated in a mucous cocoon even when the pools contain no water. Only a few minutes after a major rainfall, these fish emerge into relatively clear water which subsequently becomes laden with tannin, turning the water black and reducing the pH to approximately 4.3. As part of a large study of the visual adaptations of this unique species, the retinal and lenticular morphology of the aestivating salamanderfish is examined at the level of the light and electron microscopes. The inner retina is highly vascularised by a complex system of vitreal blood vessels, while the outer retina receives a blood supply by diffusion from a choriocapillaris. This increased retinal blood supply may be an adaptation for reducing the oxygen tension during critical periods of aestivation. Large numbers of Muller cells traverse the thickness of the retina from the inner to the outer limiting membranes. The ganglion cells are arranged in two ill-defined layers, separated from a thick inner nuclear layer containing two layers of horizontal cells by a soma-free inner plexiform layer. The photoreceptors can be divided into three types typical of many early actinopterygian representatives; equal double cones, small single cones and large rods (2:1:1). These photoreceptors are arranged into a unique regular square mosaic comprising a large rod bordered by four equal double cones with a small single cone located at the corner of each repeating unit. The double cones may optimise perception of mobile prey which it tracks by flexion of its head and neck and the large rods may increase sensitivity in the dark tannin-rich waters in which it lives. Each single cone also possesses a dense collection of polysomes and glycogen (a paraboloid) beneath its ellipsoid, the first such finding in teleosts. The retinal pigment epithelium possesses melanosomes, pha,oocytes and a large number of mitochondria. The anatomy of the retina and the photoreceptor mosaic is discussed in relation to the primitive phylogeny of this species and its unique life history.

The role of melanocortin-1 receptor polymorphism in skin cancer risk phenotypes

We have examined melanocortin-1 receptor (MC1R) variant allele frequencies in the general population and in a collection of adolescent dizygotic and monozygotic twins to determine statistical associations of pigmentation phenotypes with increased skin cancer risk. This included hair and skin color, freckling, mole count and sun exposed skin reflectance. Nine variants were studied and designated as either strong R (OR = 63; 95% CI 32-140) or weak r (OR = 5; 95% CI 3-11) red hair alleles. Penetrance of each MC1R variant allele was consistent with an allelic model where effects were multiplicative for red hair but additive for skin reflectance. To assess the interaction of the brown eye color gene BEY2/OCA2 on the phenotypic effects of variant MC1R alleles we imputed OCA2 genotype in the twin collection. A modifying effect of OCA2 on MC1R variant alleles was seen on constitutive skin color, freckling and mole count. In order to study the individual effects of these variants on pigmentation phenotype we have established a series of human primary melanocyte strains genotyped for the MC1R receptor. These include strains which are MC1R wild-type consensus, variant heterozygotes, and homozygotes for strong R alleles Arg151Cys and Arg160Trp. Ultrastructural analysis demonstrated that only consensus strains contained stage III and IV melanosomes in their terminal dendrites whereas Arg151Cys and Arg160Trp homozygous strains contained only immature stage I and II melanosomes. Such genetic association studies combined with the functional analysis of MC1R variant alleles in melanocytic cells should provide a link in understanding the association between pigmentary phototypes and skin cancer risk.

Screening of human primary melanocytes of defined melanocortin-1 receptor genotype: Pigmentation marker, ultrastructural and UV-survival studies

Recent population studies have demonstrated an association with the red-hair and fair-skin phenotype with variant alleles of the melanocortin-1 receptor (MC1R) which result in amino acid substitutions within the coding region leading to an altered receptor activity. In particular, Arg151Cys, Arg160Trp and Asp294His were the most commonly associated variants seen in the south-east Queensland population with at least one of these alleles found in 93% of those with red hair. In order to study the individual effects of these variants on melanocyte biology and melanocytic pigmentation, we established a series of human melanocyte strains genotyped for the MC1R receptor which included wild-type consensus, variant heterozygotes, compound heterozygotes and homozygotes for Arg151Cys, Arg160Trp, Val60Leu and Val92Met alleles. These strains ranged from darkly pigmented to amelanotic, with all strains of consensus sequence having dark pigmentation. UV sensitivity was found not to be associated with either MC1R genotype or the level of pigmentation with a range of sensitivities seen across all genotypes. Ultrastructural analysis demonstrated that while consensus strains contained stage IV melanosomes in their terminal dendrites, Arg151Cys and Arg160Trp homozygote strains contained only stage II melanosomes. This was despite being able to show expression of tyrosinase and tyrosinase-related protein-1 markers, although at reduced levels and an ability to convert exogenous 3,4-dihydroxyphenyl-alanine (DOPA) to melanin in these strains.

Human melanoblasts in culture: Expression of BRN2 and synergistic regulation by fibroblast growth factor-2, stem cell factor, and endothelin-3

The BRN2 transcription factor (POU3F2, N-Oct-3) has been implicated in development of the melanocytic lineage and in melanoma. Using a low calcium medium supplemented with stem cell factor, fibroblast growth factor-2, endothelin-3 and cholera toxin, we have established and partially characterised human melanocyte precursor cells, which are unpigmented, contain immature melanosomes and lack L-dihydroxyphenylalanine reactivity. Melanoblast cultures expressed high levels of BRN2 compared to melanocytes, which decreased to a level similar to that of melanocytes when cultured in medium that contained phorbol ester but lacked endothelin-3, stem cell factor and fibroblast growth factor-2. This decrease in BRN2 accompanied a positive L-dihydroxyphenylalanine reaction and induction of melanosome maturation consistent with melanoblast differentiation seen during development. Culture of primary melanocytes in low calcium medium supplemented with stem cell factor, fibroblast growth factor-2 and endothelin-3 caused an increase in BRN2 protein levels with a concomitant change to a melanoblast-like morphology. Synergism between any two of these growth factors was required for BRN2 protein induction, whereas all three factors were required to alter melanocyte morphology and for maximal BRN2 protein expression. These finding implicate BRN2 as an early marker of melanoblasts that may contribute to the hierarchy of melanocytic gene control.

Melanosome transfer between melanocytes and keratinocytes

RESUMO: A pele é o maior órgão do corpo humano e a sua pigmentação é essencial para a sua coloração e proteção contra os efeitos nocivos da radiação ultravioleta (UV). A pigmentação da pele resulta essencialmente de três processos: a síntese e o armazenamento de melanina pelos melanócitos, em organelos especializados denominados melanossomas; o transporte dos melanossomas dentro dos melanócitos; e finalmente, a transferência dos melanossomas para os queratinócitos adjacentes. Nos queratinócitos, a melanina migra para a região perinuclear apical da célula para formar um escudo protetor,responsável pela proteção do DNA dos danos causados pela radiação UV. Os melanócitos estão localizados na camada basal da epiderme e contactam com 30-40 queratinócitos. Em conjunto, estas células formam a “unidade melano-epidérmica”. Apesar dos processos de síntese e transporte de melanina nos melanócitos estarem bastante bem caracterizados, os mecanismos moleculares subjacentes à transferência inter-celular de melanina são menos conhecidos e ainda controversos. Dados preliminares obtidos pelo nosso grupo, que se basearam na observação de amostras de pele humana por microscopia electrónica, indicam que a forma predominante de transferência de melanina na epiderme consiste na exocitose dos melanossomas pelos melanócitos e subsequente endocitose da melanina por queratinócitos. Para além disso sabe-se que as proteínas Rab, que controlam o tráfego membranar, estão envolvidas em várias etapas de pigmentação da pele, nomeadamente na biogénese e no transporte de melanina. Assim, dado o seu papel fundamental nestes processos, questionámo-nos sobre o seu envolvimento na transferência de melanina. Com este trabalho, propomo-nos a expandir o conhecimento atual sobre a transferência de melanina na pele, através do estudo detalhado dos seus mecanismos moleculares, identificando as proteínas Rab que regulam o processo. Pretendemos também confirmar o modelo de exo/endocitose como sendo o mecanismo principal de transferência de melanina. Primeiro, explorámos a regulação da secreção de melanina pelos melanócitos e analisámos o papel de proteínas Rab neste processo. Os resultados foram obtidos recorrendo a um método in vitro, desenvolvido previamente no laboratório, que avalia a quantidade de melanina segregada para o meio de cultura por espectrofotometria, e ainda por microscopia, contando o número de melanossomas transferidos para os queratinócitos. Através de co-culturas de melanócitos e queratinócitos, verificou-se que os queratinócitos estimulam a libertação de melanina dos melanócitos para o meio extra-celular, bem como a sua transferência para os queratinócitos. Além disso, a proteína Rab11b foi identificada como um regulador da exocitose de melanina e da sua transferência para os queratinócitos. De facto, a diminuição da expressão de Rab11b em melanócitos provocou a redução da secreção de melanina estimulada por queratinócitos, bem como da transferência desta. Em segundo lugar, para complementar o nosso estudo, centrámos a nossa investigação na internalização de melanina por queratinócitos. Especificamente, usando uma biblioteca de siRNA, explorámos o envolvimento de proteínas Rab na captação de melanina por queratinócitos. Como primeira abordagem, usámos esferas fluorescentes como substituto de melanina, avaliando os resultados por citometria de fluxo. No entanto, este método revelou-se ineficaz uma vez que a internalização destas esferas é independente do recetor PAR-2 (recetor 2 ativado por protease), que foi previamente descrito como essencial na captação de melanina por queratinócitos Posteriormente, foi desenvolvido um novo protocolo de endocitose baseado em microscopia, usando melanossomas sem a membrana envolvente (melanocores) purificados do meio de cultura de melanócitos, incluindo um programa informático especialmente desenhado para realizar uma análise semi-automatizada. Após internalização, os melanocores acumulam-se na região perinuclear dos queratinócitos, em estruturas que se assemelham ao escudo supranuclear observado na pele humana. Seguidamente, o envolvimento do recetor PAR-2 na captação de melanocores por queratinócitos foi confirmado, utilizando o novo protocolo de endocitose desenvolvido. Para além disso, a necessidade de quatro proteínas Rab foi identificada na internalização de melanocores por queratinócitos. A redução da expressão de Rab1a ou Rab5b em queratinócitos diminuiu significativamente o nível de internalização de melanocores, enquanto o silenciamento da expressão de Rab2a ou Rab14 aumentou a quantidade de melanocores internalizados por estas células. Em conclusão, os resultados apresentados corroboram as observações anteriores, obtidas em amostras de pele humana, e sugerem que o mecanismo de transferência predominante é a exocitose de melanina pelos melanócitos, induzida por queratinócitos, seguida por endocitose pelos queratinócitos. A pigmentação da pele tem implicações tanto ao nível da cosmética, como ao nível médico, relacionadas com foto-envelhecimento e com doenças pigmentares. Assim sendo, ao esclarecer quais os mecanismos moleculares que regulam a transferência de melanina na pele, este trabalho pode conduzir ao desenvolvimento de novas estratégias para modular a pigmentação da pele.----------------ABSTRACT: Skin pigmentation is achieved through the highly regulated production of the pigment melanin in specialized organelles, termed melanosomes within melanocytes. These are transported from their site of synthesis to the melanocyte periphery before being transferred to keratinocytes where melanin forms a supra-nuclear cap to protect the DNA from UVinduced damage. Together, melanocytes and keratinocytes form a functional complex, termed “epidermal-melanin unit”, that confers color and photoprotective properties to the skin. Skin pigmentation requires three processes: the biogenesis of melanin; its intracelular transport within the melanocyte to the cell periphery; and the melanin transfer to keratinocytes. The first two processes have been extensively characterized. However, despite significant advances that have been made over the past few years, the mechanisms underlying inter-cellular transfer of pigment from melanocytes to keratinocytes remain controversial.Preliminary studies from our group using electron microscopy and human skin samples found evidence for a mechanism of coupled exocytosis-endocytosis. Rab GTPases are master regulators of intracellular trafficking and have already been implicated in several steps of skin pigmentation. Thus, we proposed to explore and characterize the molecular mechanisms of melanin transfer and the role of Rab GTPases in this process. Moreover, we investigated whether the exo/endocytosis model is the main mechanism of melanin transfer. We first focused on melanin exocytosis by melanocytes. Then, we started to investigate the key regulatory Rab proteins involved in this step by establishing an in vitro tissue culture model of melanin secretion. Using co-cultures of melanocytes and keratinocytes, we found that keratinocytes stimulate melanin release and transfer. Moreover, depletion of Rab11b decreases keratinocyte-induced melanin exocytosis by melanocytes. In order to determine whether melanin exocytosis is a predominant mechanism of melanin transfer, the amount of melanin transferred to keratinocytes was then assayed in conditions where melanin exocytosis was inhibited. Indeed, Rab11b depletion resulted in a significant decrease in melanin uptake by keratinocytes. Taken together, these observations suggest that Rab11b mediates melanosome exocytosis from melanocytes and transfer to keratinocytes. To complement and extend our study, we of melanin by keratinocytes. Thus, we aimed to explore the effect of depleting Rab GTPases on melanin uptake and trafficking within keratinocytes. As a first approach, we used fluorescent microspheres as a melanin surrogate. However, the uptake of microspheres was observed to be independent of PAR-2, a receptor that is required for melanin uptakecentred our attention in the internalization of melanin by keratinocytes. Thus, we aimed to explore the effect of depleting Rab GTPases on melanin uptake and trafficking within keratinocytes. As a first approach, we used fluorescent microspheres as a melanin surrogate. However, the uptake of microspheres was observed to be independent of PAR-2, a receptor that is required for melanin uptake.Therefore, we concluded that microspheres were uptaken by keratinocytes through a different pathway than melanin. Subsequently, we developed a microscopy-based endocytosis assay using purified melanocores (melanosomes lacking the limiting membrane) from melanocytes, including a program to perform a semi-automated analysis. Melanocores are taken up by keratinocytes and accumulate in structures in the perinuclear area that resemble the physiological supranuclear cap observed in human skin. We then confirmed the involvement of PAR-2 receptor in the uptake of melanocores by keratinocytes, using the newly developed assay. Furthermore, we identified the role of four Rab GTPases on the uptake of melanocores by keratinocytes. Depletion of Rab1a and Rab5b from keratinocytes significantly reduced the uptake of melanocores, whereas Rab2a, and Rab14 silencing increased the amount the melanocores internalized by XB2 keratinocytes. In conclusion, we present evidence supporting keratinocyte-inducedmelanosome exocytosis from melanocytes, followed by endocytosis of the melanin core by keratinocytes as the predominant mechanism of melanin transfer in skin. Although advances have been made, there is a need for more effective and safer therapies directed at pigmentation disorders and also treatments for cosmetic applications. Hence, the understanding of the above mechanisms of skin pigmentation will lead to a greater appreciation of the molecular machinery underlying human skin pigmentation and could interest the pharmaceutical and cosmetic industries.

Shallow-level migmatization of gabbros in a metamorphic contact aureole, Fuerteventura Basal Complex, Canary Islands

Migmatization of gabbroic rocks at 2-3 kbar has occurred in the metamorphic contact aureole of a mafic pluton in the Fuerteventura Basal Complex (Canary Island;). Migmatites are characterized by a dense network: of closely spaced millimetre-wide leucocratic veins with perfectly preserved igneous textures. They are all relatively enriched in Al, Na I: Sr Ba, Nb, Y and the rare earth elements compared with the unaffected country rock beyond the aureole. Migmatization under such low-pressure conditions war possible because of the unusual tectonic and magmatic contact in which ii occurred. Multiple basic intrusions associated with extrusive volcanic activity created high heat flow in a small area. Alkaline and metasomatized rocks present in the country rock of the intruding pluton were leached by high-temperature fluids during contact metamorphism. These enriched fluids then favoured partial melting of the host gabbroic rocks, and contaminated both the leucosomes and melanosomes. A transpressive tectonic setting at the time of intrusion created shearing along the contact between the intrusion and its host rock. This shearing enhanced circulation of the fluids and allowed segregation of the nea-formed melts from their restite by opening tension veins into which the melts migrated. Depending on the relative timing of melt segregation and recrystallization leucosomes range in composition from a 40-60% mixture of clinopyroxene (+/- amphibole) and plagioclase to almost pure feldspathic veins. Comparable occurrences of gabbros migmatized at low pressure are expected only at a snail scale in localized areas of high heat flow in the presence of fluids, such as in. mid-ocean ridges or ocean-islands.

An experimental study on the shallow-level migmatization of ferrogabbros from the Fuerteventura Basal Complex, Canary Islands

Spectacular shallow-level migmatization of ferrogabbroic rocks occurs in a metamorphic contact aureole of a gabbroic pluton of the Tierra Mala massif (TM) on Fuerteventura (Canary Islands). In order to improve our knowledge of the low pressure melting behavior of gabbroic rocks and to constrain the conditions of migmatization of the TM gabbros, we performed partial melting experiments on a natural ferrogabbro, which is assumed as protolith of the migmatites. The experiments were performed in an internally heated pressure vessel (IHPV) at 200 MPa, 930-1150 degreesC at relatively oxidizing conditions. Distinct amounts of water were added to the charge. From 930 to 1000 degreesC, the observed experimental phases are plagioclase (An(60-70)), clinopyroxene, amphibole (titanian magnesiohastingsites), two Fe-Ti oxides, and a basaltic, K-poor melt. Above 1000 degreesC, amphibole is no longer stable. The first melts are very rich in non-native plagioclase (>70 wt.%). This indicates that at the beginning of partial melting plagioclase is the major phase which is consumed to produce melt. In the experiments, plagioclase is stable up to high temperatures (1060 degreesC) showing increasing An content with temperature. This is not compatible with the natural migmatites, in which An-rich plagioclase is absent in the melanosomes, while amphibole is stable. Our results show that the partial melting of the natural rocks cannot be regarded as an ``in-situ'' process that occurred in a closed system. Considerable amounts of alkalis probably transported by water-rich fluids, derived from the mafic pluton underplating the TM gabbro, were necessary to drive the melting reaction out of the stability range of plagioclase. A partial melting experiment with a migmatite gabbro showing typical ``in-situ'' textures as starting material supports this assumption. Crystallization experiments performed at 1000 degreesC on a glass of the fitised ferrogabbro with different water contents added to the charge show that generally high water activities could be achieved (crystallization of amphibole), independently of the bulk water content, even in a system with very low initial bulk water content (0.3 wt.%). Increasing water contents produce plagioclase richer in An, reduces the modal proportion of plagioclase in the crystallizing assemblage and extends the melt fraction. High melt fractions of >30 wt.% could only be observed in systems with high bulk water contents (> - 2 wt.%). This indicates that the migmatites were generated under water-rich conditions (probably water-saturated), since those migmatites, which are characterized as ``in-situ'' formations, show generally high amounts of leucosomes (>30 wt.%). (C) 2003 Elsevier B.V. All rights reserved.

Coat color dilution in mice because of inactivation of the melanoma antigen MART-1.

Melanoma antigen recognized by T cells 1 (MART-1) is a melanoma-specific antigen, which has been thoroughly studied in the context of immunotherapy against malignant melanoma and which is found only in the pigment cell lineage. However, its exact function and involvement in pigmentation is not clearly understood. Melanoma antigen recognized by T cells 1 has been shown to interact with the melanosomal proteins Pmel17 and OA1. To understand the function of MART-1 in pigmentation, we developed a new knockout mouse model. Mice deficient in MART-1 are viable, but loss of MART-1 leads to a coat color phenotype, with a reduction in total melanin content of the skin and hair. Lack of MART-1 did not affect localization of melanocyte-specific proteins nor maturation of Pmel17. Melanosomes of hair follicle melanocytes in MART-1 knockout mice displayed morphological abnormalities, which were exclusive to stage III and IV melanosomes. In conclusion, our results suggest that MART-1 is a pigmentation gene that is required for melanosome biogenesis and/or maintenance.

Characterization of N-cadherin association to lipid rafts in melanoma

RESUME La peau est un organe complex composé de deux parties distinctes: l'épiderme et le derme, séparé par une membrane basale. Dans la couche basale de l'épiderme, les melanocytes synthétisent la mélanine dans des mélanosomes. Les mélanosomes sont ensuite transportés des mélanocytes vers les kératinocytes, protégeant ainsi la peau des dégâts dus aux radiations U.V. La E-cadhérine assure l'adhésion entre les mélanocytes et les kératinocytes. Au cours de la transformation du mélanocyte en cellule malignes, les mélanocytes perdent l'expression de la E-cadhérine et, simultanément, se mettent à exprimer la N-cadhérine, ce phénomène est nommé « cadherin switch ». La perte de l'expression de la E-cadhérine permet au mélanocytes d'échapper au contrôle des kératinocytes, tandis que l'expression de la N-cadhérine promeut l'invasion métastasique des cellules de mélanome. Préalablement, nous avons trouvé qu'une fraction de la N-cadhérine était localisée les microdomaines membranaires spécialisés, enrichi en cholestérol et en glycosphingolipides, appelés « lipid rafts ». Une des particularité des « lipid rafts » est qu'ils sont riches en molécules permettant la transmission de signaux d'activation. De plus, des travaux récents rapportent qu'un sous-type de « lipid rafts » appelé caveolae pourrai contribuer à la progression tumorale. S'appuyant sur le rôle prépondérant de la N-cadhérine dans la progression du mélanome ainsi que sur sa présence dans les « lipid rafts », nous avons émis l'hypothèse que l'association de la N-cadhérine avec les « lipid rafts » pourrai contribuer à la progression du mélanome. Le but de ce projet à été de caractériser l'association de la Ncadhérine avec les « lipid rafts » au cours de la progression du mélanome. Au moyen de lignées cellulaires humaines, dérivées de mélanomes à différents stades de progression, nous avons trouvé que (1) la N-cadhérine est partiellement associée aux «lipid rafts » dans six lignées dérivées de mélanome en phase avancée de progression et dans des tumeurs expérimentales, mais pas dans deux lignées dérivées de mélanome à un stade plus précoce ; (2) l'association de la N-cadhérine dans les « lipid rafts » ne dépent pas de son niveau d'expression ; (3) la E-cadhérine n'est pas présente dans les « lipid rafts »d'une lignée de cellule de mélanome ayant conservé l'expression de la E-cadhérine ; (4) la localisation de la N-cadhérine dans les « lipid rafts »n'est pas modulée par les facteurs de croissance bFGF, IGF-I, et HRG1-β1, ni par des voies de signalisation impliquant MEK, PKA, les kinases de la famille Src, et PI3K ; (5) l'association de la N-cadhérine avec les « lipid rafts » n'est pas requise pour la stabilisation des jonctions adhérentes et n'est pas perturbée par la destruction de ces dernières ; (6) la N-cadhérine dans les « lipid rafts » forme un complexe avec β-caténine, p 120ctn et α-caténine. En conclusion, cette étude originale montre pour la première fois que dans des cellules de mélanome agressifs, une fraction de la N-cadhérine est localisée dans les « lipid rafts » en association avec β-caténine, p 120ctn et α-caténine. Comme la présence de la N-cadhérine dans les « lipid rafts » ne contribue pas à la formation de jonction adhérentes, cette étude suggère une nouvelle fonction pour la N-cadhérine dans les « lipid rafts ». SUMMARY Human skin is a complex organ composed of two layers separated by a basement membrane: the epidermis and the dermis. In the basal layer of the epidermis, the melanin-producing cells of the skin, the melanocytes deliver melanin-containing melanosomes to keratinocytes, thereby protecting the epidermis and the dermis from the deleterious effects of ultraviolet light. Melanocytes physically interact with keratinocytes through E-cadherin-mediated adhesion. During malignant transformation into melanoma cells, melanocytes lose E-cadherin expression and concomitantly gain expression of N-cadherin, a phenomenon referred to as "cadherin switch". Loss of E-cadherin allows melanocytes to escape the regulatory effects of neighbouring keratinocytes, while gain of N-cadherin expression promotes migration, invasion and metastatic abilities of melanoma cells. In preliminary experiments, we found that a fraction of N-cadherin localized to specialized membrane microdomains enriched in cholesterol- and glycosphingolipid, called lipid rafts. One particular feature of lipid rafts is that they are rich in signalling molecules and they possibly modulate transmembrane signalling events. Moreover, recent reports suggested that a specialized type of rafts called caveolae might contribute to tumor progression. Based on the documented role of N-cadherin in melanoma progression and its presence in lipid rafts of melanoma cells, we raised the hypothesis that the association of N-cadherin with lipid rafts might be relevant to melanoma progression. The aim of this project was to characterize N-cadherin associated to lipid rafts during melanoma progression. Using human melanoma cell lines derived from melanoma at different stages of progression, we found that (1) N-cadherin is partly associated to lipid rafts in six cell lines derived from melanomas at late stages of progression and in experimental tumors, but not in two melanoma cell lines derived from early stages; (2) N-cadherin targeting to lipid rafts does not depend on its expression level; (3) E-cadherin is not localized in lipid rafts of a melanoma cell line that retained E-cadherin expression; (4) N-cadherin localization to lipid rafts is not modulated by the growth factors bFGF, IGF-I, and HRG1-β1, nor by MEK-, PKA-, Src family kinases-, and PI3K-mediated signalling events; (5) the association of N-cadherin with lipid rafts is not required for adherens junctions stability nor it is perturbed by adherens junctions disruption; (6) N-cadherin in lipid rafts is in complex with β-catenin, p 120ctm and α-catenin. In conclusion, this study provides original evidence that in aggressive melanoma cells a pool of N-cadherin is localized in lipid rafts in association with β-catenin, p 120 and α-catenin. The presence of N-cadherin in lipid rafts independently of its involvement in adherens junctions formation, suggests a possible new role for N-cadherin recruited to lipid rafts. Further studies investigating the biological meaning of this localization promise to uncover new properties of this molecule.

Partial melting of basic dykes in the contact aureoles of two shallow-level, gabbro-pyroxenite intrusions, Fuerteventura

THESIS ABSTRACT Low-pressure anatexis of basic dykes gave rise to unusual, zebra-like migmatites, in the contact metamorphic aureoles of two layered gabbro-pyroxenite intrusions, PXl and PX2, in the root zone of an ocean island, Fuerteventura Basal Complex (Canary Islands). This thesis focuses on the understanding of processes attributing to the partial melting and formation of these migmatites, characterised by a dense network of closely spaced, millimetre-wide leucocratic segregations with perfectly preserved igneous textures. The presence of fluids are required to decrease the solidus of basic igneous lithologies, to allow partial melting in such aloes-pressure (1-2 kb) environment. An oxygen isotope study was thus carried out on dykes inside and beyond the PX2 aureole, in order to decipher the nature and origin of such fluids. Low or negative δ18O values were obtained for whole rocks and mineral-separates, decreasing towards the contact, with the intrusion itself retaining fairly high values. This trend has been attributed to the advection of meteoric water during magma emplacement, with increasing fluid/rock ratios (higher dyke intensities towards the intrusion acting as fluid-pathways) and higher temperatures promoting increasing exchange during recrystallisation. A comparison of whole rock and mineral major- and trace- element data allowed the redistribution of elements .between different mineral phases and generations, during contact metamorphism and partial melting to be assessed. Certain trace-elements, e.g. Zr, Hf, Y, and REEs, were internally redistributed during contact metamorphic recrystallisation, causing- the enrichment of neocrystallised diopsides compared to relict phenocrysts. This has been assigned to the liberation of trace elements on the breakdown of primary minerals, kaersutite and sphene, on entering the thermal aureole. Major and trace element compositions of minerals in migmatite melanosomes and leucosomes are almost identical, pointing to a syn- or post- solidus reequilibration on cooling of the migmatite terrain. The mineralogical, textural and geochemical evolution of dykes in a contact metamorphic aureole, is recorded around an apophysis of the PX1 intrusion, where there is evidence of incipient partial melting. Hydrothermal mineral pseudomorphs in the outer parts of the aureole are progressively replaced by dry mineral assemblages, with increasingly recrystallised diopside and evidence of partial melting -the extent of which varies from one lithology to another. The appearance of more mafic lithologies towards the intrusion, with lower whole rock SiO2 and mobile element abundances, e.g. Rb, Cs, K, has been explained by the migration and accumulation of feldspathic material into leucosomes outside the samples. A micro-structural study of leucosomes and leucocratic pods, with the aid of high-resolution X-ray computed micro-tomography (HRXµCT), allowing the visualization and quantification of shapes and orientations, was carried out in order to better understand the processes of melt segregation in the PX1 aureole. Leucocratic pods, representing former amygdales, are considered as natural strain ellipsoids. Their short axes are oriented perpendicular to leucosome planes, which sub-parallel the intrusive contact. Leucosomes thus effectively represent foliation planes. This implies that the direction of maximum shortening, during migmatisation, was perpendicular to the orientation of leucosomes, contradicting earlier models that suggest leucosomes represent tension veins. RESUME DE LA THESE Un phénomène rare de fusion partielle de filons basiques à basse pression a été étudié dans les auréoles de contact de deux intrusions litées de gabbro-pyroxénite, PX1 et PX2, localisées dans le soubassement de l'île volcanique de Fuerteventura aux Canaries. Cette anatexie a engendré des migmatites finement zébrées d'aspect très inhabituel, dont les processus de formation ont été étudiés dans le présent travail. Ces roches sont caractérisées par un réseau dense de veinules leucocrates d'épaisseur millimétrique, dont les textures ignées sont parfaitement préservées. La fusion partielle de roches basiques à basse pression (1-2 kbar) requiert la présence d'eau afin d'abaisser le solidus du système à des températures géologiquement réalistes. Une étude comparative des isotopes de l'oxygène a ainsi été menée sur des filons respectivement affectés et non affectés par le métamorphisme de contact, afin de confirmer la présence de ces fluides, de déterminer l'importance de leur interaction avec les roches et leur origine. Des valeurs de δ180 basses ou négatives ont été mesurées sur roche totale et minéraux séparés, décroissantes en direction du contact, alors que l'intrusion elle-même a conservé des valeurs élevées. Ce gradient a été attribué à l'advection d'eau météorique durant la mise en place du magma, les températures les plus élevées favorisant d'autant plus la circulation des fluides et les échanges isotopiques durant la recristallisation des roches. Cette recristallisation engendré une redistribution chimique complète des éléments entre les différentes générations de minéraux résultant du métamorphisme de contact et de l'anatexie, mise en évidence par microanalyse. Certains éléments traces comme Zr, Hf, Y et les REE ont été concentrés dans le diopside néoformé consécutivement à la déstabilisation de minéraux primaires riches en ces éléments comme la kaersutite ou le sphène. Les compositions en éléments majeurs et traces des minéraux des mélanosomes et leucosomes des migmatites sont pratiquement identiques, indiquant une rééquilibration syn- à postsolidus lors du refroidissement de l'auréole de contact. La transformation progressive des filons basiques au niveau de leur minéralogie, textures et composition chimique a pu être observée en détail à l'approche du contact d'une apophyse de l'intrusion PX1. La paragenèse magmatique initiale n'est jamais préservée, les faciès les plus distants du contact étant constitués d'un assemblage pseudomorphique hydrothermal. Ce dernier est progressivement remplacé par des assemblages anhydres incluant du diopside néoformé, puis apparaissent les premiers signes de fusion partielle, dont l'importance varie fortement d'une lithologie à l'autre. L'apparition de faciès plus basiques en direction du contact, avec des teneurs réduites en SiO2 et en éléments incompatibles tels Rb, Cs, K, a été attribuée à l'échappement de leucosomes feldspathiques hors du système. Une étude microstructurale de la distribution spatiale du matériel leucocrate au sein des migmatites par microtomographie X de haute résolution (HRXµCT) a été menée pour mieux comprendre les processus de ségrégation des liquides dans l'auréole de PX1. De petites entités ovoïdes, représentant d'anciennes structures amygdalaires au sein des filons, ont été considérées comme des ellipsoïdes marqueurs de la déformation finie. Leur petit axe est orienté perpendiculairement aux plans définis par les leucosomes, eux-mêmes subparallèles au contact intrusif. Les leucosomes matérialisent donc des plans de clivage. Ainsi, la direction de raccourcissement maximum durant la fusion partielle était perpendiculaire à l'orientation des leucosomes, contrairement à ce qui a été dit dans de précédentes publications, qui suggéraient que les leucosomes représentaient des veines de tension. RESUME DE LA THESE (POUR LE GRAND PUBLIC) L'observation directe du soubassement d'une île volcanique est une occasion rare, accessible dans le «complexe de base » de l'île canarienne de Fuerteventura. Ce dernier a enregistré divers phénomènes magmatiques, métamorphiques et de fusion partielle induits par l'intrusion répétée de magmas alimentant des appareils volcaniques sus jacents, sous forme de petits plutons, essaims de filons et complexes annulaires de gabbros alcalins, pyroxénites, syénites et carbonatites. Dans ce contexte de flux de chaleur élevé, des filons basiques ont subi une fusion partielle au contact de deux intrusions de gabbro-pyroxénite, un phénomène extrêmement rare à une profondeur aussi réduite, estimée à quelque 3-6 km. Les produits de cette fusion partielle sont des liquides très riches en feldspath, concentrés en un réseau dense de veinules blanches (leucosomes) au sein du matériau résiduel sombre non fondu (mélanosome) pour former ce qu'on appelle des migmatites. Outre les aspects pétrologiques liés à la formation de ces migmatites, l'intérêt majeur du phénomène réside dans le fait qu'il puisse représenter la source des magmas évolués parfois observés sur les îles océaniques. A des pressions aussi faibles que dans le soubassement de Fuerteventura (1-2 Kbar), la présence de fluides abondants est nécessaire pour abaisser la température de début de fusion des roches (solidus) à des valeurs géologiquement réalistes. Des expériences ont montré que même en présence de plusieurs %-poids d'eau, une température de 1000°C était encore nécessaire pour obtenir une proportion de liquide équivalente à celle observée sur le terrain, soit 25%. Or les magmas alcalins des îles océaniques, bien qu'hydratés, n'en contiennent de loin pas autant, ce qui implique une source d'eau externe. Une étude isotopique de l'oxygène a été entreprise afin de tester cette hypothèse. Les valeurs obtenues en 5180 sont basses ou négatives et indiquent l'influence d'eau d'origine météorique. Cette eau de pluie se serait infiltrée le long des filons depuis la surface du volcan et les aurait complètement hydrothermalisés en profondeur (situation encore visible à l'extérieur de l'auréole de contact), leur permettant ainsi de stocker l'eau nécessaire à leur fusion partielle ultérieure. L'interaction entre eau de pluie et filons a été d'autant plus importante que ces derniers étaient proches du contact avec l'intrusion, ce qui suggère que la circulation de ces eaux et leur interaction avec les roches a été favorisée par la chaleur fournie par l'intrusion elle-même. Un autre aspect de ce travail s'est focalisé sur la redistribution des éléments traces au sein des minéraux des filons basiques durant le métamorphisme de contact et la fusion partielle. Ainsi, le pyroxène de seconde génération est-il sensiblement enrichi en traces telles Zr, Hf, Y et les terres rares, par rapport au pyroxène magmatique originel, en relation avec la déstabilisation de minéraux primaires riches en ces éléments tels le sphène et la kaersutite. Cependant, les compositions en éléments majeurs et traces des minéraux recristallisés des migmatites sont pratiquement les mêmes dans les leucosomes et les mélanosomes, suggérant une rééquilibration chimique complète durant le refroidissement de ces lithologies. Si certaines migmatites se sont comportées en système chimiquement fermé (hormis l'eau météorique), d'autres filons ont manifestement perdu une partie de leurs leucosomes, ainsi qu'en témoigne leur composition progressivement appauvrie en silice et autres éléments incompatibles mobiles, tels K et Rb à l'approche du contact de l'intrusion. Parallèlement à cette évolution chimique, les paragenèses hydrothermales distantes du contact sont progressivement remplacées par des paragenèses anhydres, puis par l'apparition des premiers leucosomes, tandis que les textures magmatiques initiales sont complètement effacées au profit d'une combinaison de textures magmatique dans les leucosomes et en mosaïque dans les mélanosomes. Enfin, la distribution spatiale des liquides de fusion partielle a été étudiée par microtomographie X de haute résolution, dans des filons contenant des entités ovoïdes leucocrates, sans doute d'anciennes amygdales à zéolites. Ces dernières ont été considérées comme des ellipsoïdes de la déformation finie. L'orientation de leur petit axe, perpendiculaire au plan défini par les veinules de leucosomes, indique que ces derniers représentent des plans de clivage perpendiculaires à la direction de raccourcissement maximum. Ainsi, la ségrégation des liquides de fusion partielle se serait faite dans les plans de compression et non dans des plans de dilatation, contrairement à ce que laisserait penser le sens commun.

Rab27a: A key to melanosome transport in human melanocytes

Normal pigmentation depends on the uniform distribution of melanin-containing vesicles, the melanosomes, in the epidermis. Griscelli syndrome (GS) is a rare autosomal recessive disease, characterized by an immune deficiency and a partial albinism that has been ascribed to an abnormal melanosome distribution. GS maps to 15q21 and was first associated with mutations in the myosin-V gene. However, it was demonstrated recently that GS can also be caused by a mutation in the Rab27a gene. These observations prompted us to investigate the role of Rab27a in melanosome transport. Using immunofluorescence and immunoelectron microscopy studies, we show that in normal melanocytes Rab27a colocalizes with melanosomes. In melanocytes isolated from a patient with GS, we show an abnormal melanosome distribution and a lack of Rab27a expression. Finally, reexpression of Rab27a in GS melanocytes restored melanosome transport to dendrite tips, leading to a phenotypic reversion of the diseased cells. These results identify Rab27a as a key component of vesicle transport machinery in melanocytes.

Trace element distribution among rock-forming minerals from metamorphosed to partially molten basic igneous rocks in a contact aureole (Fuerteventura, Canaries)

Low pressure partial melting of basanitic and ankaramitic dykes gave rise to unusual, zebra-like migmatites, in the contact aureole of a layered pyroxenite-gabbro intrusion, in the root zone of an ocean island (Basal Complex, Fuerteventura, Canary Islands). These migmatites are characterised by a dense network of closely spaced, millimetre-wide leucocratic segregations. Their mineralogy consists of plagioclase (An(32-36)), diopside, biotite, oxides (magnetite, ilmenite), +/-amphibole, dominated by plagioclase in the leucosome and diopside in the melanosome. The melanosome is almost completely recrystallised, with the preservation of large, relict igneous diopside phenocrysts in dyke centres. Comparison of whole-rock and mineral major- and trace-element data allowed us to assess the redistribution of elements between different mineral phases and generations during contact metamorphism and partial melting. Dykes within and outside the thermal aureole behaved like closed chemical systems. Nevertheless, Zr, Hf, Y and REEs were internally redistributed, as deduced by comparing the trace element contents of the various diopside generations. Neocrystallised diopside - in the melanosome, leucosome and as epitaxial phenocryst rims - from the migmatite zone, are all enriched in Zr, Hf, Y and REEs compared to relict phenocrysts. This has been assigned to the liberation of trace elements on the breakdown of enriched primary minerals, kaersutite and sphene, on entering the thermal aureole. Major and trace element compositions of minerals in migmatite melanosomes and leucosomes are almost identical, pointing to a syn- or post-solidus reequilibration on the cooling of the migmatite terrain i.e. mineral-melt equilibria were reset to mineral-mineral equilibria. (C) 2007 Elsevier B.V. All rights reserved.

Generation and suppression of singlet oxygen in hair by photosensitization of melanin

We have studied the spectroscopic properties of hair (white, blond, red, brown, and black) under illumination with visible light, giving special emphasis to the photoinduced generation of singlet oxygen ((1)O(2)). Irradiation of hair shafts (lambda(ex)>400 nm) changed their properties by degrading the melanin. Formation of C3 hydroperoxides in the melanin indol groups was proven by (1)H NMR. After 532-nm excitation, all hair shafts presented the characteristic (1)O(2) emission (lambda(em) = 1270 nm), whose intensity varied inversely with the melanin content. (1)O(2) lifetime was also shown to vary with hair type, being five times shorter in black hair than in blond hair, indicating the role of melanin as a (1)O(2) suppressor. Lifetime ranged from tenths of a nanosecond to a few microseconds, which is much shorter than the lifetime expected for (1)O(2) in the solvents in which the hair shafts were suspended, indicating that (1)O(2) is generated and suppressed inside the hair structure. Both eumelanin and pheomelanin were shown to produce and to suppress (1)O(2), with similar efficiencies. The higher amount of (1)O(2) generated in blond hair and its longer lifetime is compatible with the stronger damage that light exposure causes in blond hair. We propose a model to explain the formation and suppression of (1)O(2) in hair by photosensitization of melanin with visible light and the deleterious effects that an excess of visible light may cause in hair and skin. 2011 Published by Elsevier Inc.

Pigmentação testicular em Physalaemus nattereri (Steindachner) (Amphibia, Anura) com observações anatômicas sobre o sistema pigmentar extracutâneo

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)