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.

Late Jurassic oceanic crust and Upper Cretaceous Caribbean plateau picritic basalts exposed in the Duarte igneous complex, Hispaniola

Four distinct rock units have been recognized near El Aguacate, in the Janico-Juncalito-La Vega area of the Duarte complex (Dominican Republic): (1) serpentinites crosscut by numerous diabasic dikes, (2) basalts interbedded with Late Jurassic ribbon cherts, (3) picrites and ankaramites relatively enriched in incompatible trace elements, and (4) amphibolites and gneissic amphibolites chemically similar to Oceanic Plateau Basalts. Similar Ar-Ar ages of late magmatic amphibole from a picrite, and hornblende from an amphibolite (86.1 +/- 1.3 Ma and 86.7 +/- 1.6 Ma, respectively), suggest that the Duarte picrites are contemporaneous with the Deep Sea Drilling Program Leg 15 and Ocean Drilling Program Leg 126 basalts drilled from the Caribbean oceanic plateau. These basalts are associated with sediments containing Late Cretaceous faunas. Sr, Nd, and Pb data show that enriched picrites and amphibolites are isotopically similar to mafic lavas from previously described Caribbean plateau and Galapagos hotspot basalts. Major element, trace element, and lead isotopic features of Late Jurassic basalts and diabases are consistent with those of normal oceanic crust basalt. However, these basalts differ from typical N-MORB because they have lower epsilon Nd ratios that plot within the range of Ocean Island Basalts. These rocks appear to represent remnants of the Caribbean Jurassic oceanic crust formed from an oceanic ridge possibly close to a hotspot. Later, they were tectonically juxtaposed with Late Cretaceous slices of the Caribbean-Colombian plateau.

Cardiopulmonary support and extracorporeal membrane oxygenation for cardiac assist.

BACKGROUND: Use of cardiopulmonary bypass for emergency resuscitation is not new. In fact, John Gibbon proposed this concept for the treatment of severe pulmonary embolism in 1937. Significant progress has been made since, and two main concepts for cardiac assist based on cardiopulmonary bypass have emerged: cardiopulmonary support (CPS) and extracorporeal membrane oxygenation (ECMO). The objective of this review is to summarize the state of the art in these two technologies. METHODS: Configuration of CPS is now fairly standard. A mobile cart with relatively large wheels allowing for easy transportation carries a centrifugal pump, a back-up battery with a charger, an oxygen cylinder, and a small heating system. Percutaneous cannulation, pump-driven venous return, rapid availability, and transportability are the main characteristics of a CPS system. Cardiocirculatory arrest is a major predictor of mortality despite the use of CPS. In contrast, CPS appears to be a powerful tool for patients in cardiogenic shock before cardiocirculatory arrest, requiring some type of therapeutic procedures, especially repair of anatomically correctable problems or bridging to other mechanical circulatory support systems such as ventricular assist devices. CPS is in general not suitable for long-term applications because of the small-bore cannulas, resulting in significant pressure gradients and eventually hemolysis. RESULTS: In contrast, ECMO can be designed for longer-term circulatory support. This requires large-bore cannulas and specifically designed oxygenators. The latter are either plasma leakage resistent (true membranes) or relatively thrombo-resistant (heparin coated). Both technologies require oxygenator changeovers although the main reason for this is different (clotting for the former, plasma leakage for the latter). Likewise, the tubing within a roller pump has to be displaced and centrifugal pump heads have to be replaced over time. ECMO is certainly the first choice for a circulatory support system in the neonatal and pediatric age groups, where the other assist systems are too bulky. ECMO is also indicated for patients improving on CPS. Septic conditions are, in general, considered as contraindications for ECMO. CONCLUSIONS: Ease of availability and moderate cost of cardiopulmonary bypass-based cardiac support technologies have to be balanced against the significant immobilization of human resources, which is required to make them successful.

La chirurgie combinée phacoémulsification/pelage de membrane épirétinienne et oedème maculaire [Combined phacoemulsification/membrane resection and macular edema].

PURPOSE: To evaluate the occurrence of macular edema (ME) after epiretinal membrane resection, managed either with simple vitrectomy or with combined vitrectomy and phacoemulsification. MATERIAL AND METHODS: Two groups of 12 patients had a vitrectomy for epiretinal membrane associated or not to a phacoemulsification. A fundus fluorescein angiography was performed pre and postoperatively and at least 3 months after the surgery. RESULTS: In the group of patients who had a simple vitrectomy, a ME was observed in 50% of the cases preoperatively and in 25% of the cases at the end of follow-up. In 3 cases, preoperative ME was worsened after the surgery. In the group of patients who were treated by a combined vitrectomy and phacoemulsification, a ME was observed in 25% of the cases preoperatively and in 50% of the cases at the end of follow-up. A de novo ME was observed in 3 cases. CONCLUSION: Combined vitrectomy and cataract surgery could allow a rapid recovery of visual acuity but might increase the occurrence of ME.

Regulation of the epithelial Na+ channel ENaC by Tsg101 in renal epithelial cells

Kidneys are the main regulator of salt homeostasis and blood pressure. In the distal region of the tubule active Na-transport is finely tuned. This transport is regulated by various hormonal pathways including aldosterone that regulates the reabsorption at the level of the ASDN, comprising the late DCT, the CNT and the CCD. In the ASDN, the amiloride-sensitive epithelial Na-channel (ENaC) plays a major role in Na-homeostasis, as evidenced by gain-of function mutations in the genes encoding ENaC, causing Liddle's syndrome, a severe form of salt-sensitive hypertension. In this disease, regulation of ENaC is compromised due to mutations that delete or mutate a PY-motif in ENaC. Such mutations interfere with Nedd4-2- dependent ubiquitylation of ENaC, leading to reduced endocytosis of the channel, and consequently to increased channel activity at the cell surface. After endocytosis ENaC is targeted to the lysosome and rapidly degraded. Similarly to other ubiquitylated and endocytosed plasma membrane proteins (such as the EGFR), it is likely that the multi-protein complex system ESCRT is involved. To investigate the involvement of this system we tested the role of one of the ESCRT proteins, Tsg101. Here we show that Tsg101 interacts endogenously and in transfected HEK-293 cells with all three ENaC sub-units. Furthermore, mutations of cytoplasmic lysines of ENaC subunits lead to the disruption of this interaction, indicating a potential involvement of ubiquitin in Tsg101 / ENaC interaction. Tsg101 knockdown in renal epithelial cells increases the total and cell surface pool of ENaC, thus implying TsglOl and consequently the ESCRT system in ENaC degradation by the endosomal/lysosomal system. - Les reins sont les principaux organes responsables de la régulation de la pression artérielle ainsi que de la balance saline du corps. Dans la région distale du tubule, le transport actif de sodium est finement régulé. Ce transport est contrôlé par plusieurs hormones comme l'aldostérone, qui régule la réabsorption au niveau de l'ASDN, segment comprenant la fin du DCT, le CNT et le CCD. Dans l'ASDN, le canal à sodium épithélial sensible à l'amiloride (ENaC) joue un rôle majeur dans l'homéostasie sodique, comme cela fut démontré par les mutations « gain de fonction » dans les gênes encodant ENaC, causant ainsi le syndrome de Liddle, une forme sévère d'hypertension sensible au sel. Dans cette maladie, la régulation d'ENaC est compromise du fait des mutations qui supprime ou mute le domaine PY présent sur les sous-unités d'ENaC. Ces mutations préviennent l'ubiquitylation d'ENaC par Nedd4-2, conduisant ainsi à une baisse de l'endocytose du canal et par conséquent une activité accrue d'ENaC à la surface membranaire. Après endocytose, ENaC est envoyé vers le lysosome et rapidement dégradé. Comme d'autres protéines membranaires ubiquitylées et endocytées (comme l'EGFR), il est probable que le complexe multi-protéique ESCRT est impliqué dans le transport d'ENaC au lysosome. Pour étudier l'implication du système d'ESCRT dans la régulation d'ENaC nous avons testé le rôle d'une protéine de ces complexes, TsglOl. Notre étude nous a permis de démontrer que TsglOl se lie aux trois sous-unités ENaC aussi bien en co-transfection dans des cellules HEK-293 que de manière endogène. De plus, nous avons pu démontrer l'importance de l'ubiquitine dans cette interaction par la mutation de toutes les lysines placées du côté cytoplasmique des sous-unités d'ENaC, empêchant ainsi l'ubiquitylation de ces sous-unités. Enfin, le « knockdown » de TsglOl dans des cellules épithéliales de rein induit une augmentation de l'expression d'ENaC aussi bien dans le «pool» total qu'à la surface membranaire, indiquant ainsi un rôle pour TsglOl et par conséquent du système d'ESCRT dans la dégradation d'ENaC par la voie endosome / lysosome. - Le corps humain est composé d'organes chacun spécialisé dans une fonction précise. Chaque organe est composé de cellules, qui assurent la fonction de l'organe en question. Ces cellules se caractérisent par : - une membrane qui leur permet d'isoler leur compartiment interne (milieu intracellulaire ou cytoplasme) du liquide externe (milieu extracellulaire), - un noyau, où l'ADN est situé, - des protéines, sortent d'unités fonctionnelles ayant une fonction bien définie dans la cellule. La séparation entre l'extérieure et l'intérieure de la cellule est essentielle pour le maintien des composants de ces milieux ainsi que pour la bonne fonction de l'organisme et des cellules. Parmi ces composants, le sodium joue un rôle essentiel car il conditionne le maintien de volume sanguin en participant au maintien du volume extracellulaire. Une augmentation du sodium dans l'organisme provoque donc une augmentation du volume sanguin et ainsi provoque une hypertension. De ce fait, le contrôle de la quantité de sodium présente dans l'organisme est essentiel pour le bon fonctionnement de l'organisme. Le sodium est apporté par l'alimentation, et c'est au niveau du rein que va s'effectuer le contrôle de la quantité de sodium qui va être retenue dans l'organisme pour le maintien d'une concentration normale de sodium dans le milieu extracellulaire. Le rein va se charger de réabsorber toutes sortes de solutés nécessaires pour l'organisme avant d'évacuer les déchets ou le surplus de ces solutés en produisant l'urine. Le rein va se charger de réabsorber le sodium grâce à différentes protéines, parmi elle, nous nous sommes intéressés à une protéine appelée ENaC. Cette protéine joue un rôle important dans la réabsorption du sodium, et lorsqu'elle fonctionne mal, comme il a pu être observé dans certaines maladies génétiques, il en résulte des problèmes d'hypo- ou d'hypertension. Les problèmes résultant du mauvais fonctionnement de cette protéine obligent donc la cellule à réguler efficacement ENaC par différents mécanismes, notamment en diminuant son expression et en dégradant le « surplus ». Dans cette travail de thèse, nous nous sommes intéressés au mécanisme impliqué dans la dégradation d'ENaC et plus précisément à un ensemble de protéines, appelé ESCRT, qui va se charger « d'escorter » une protéine vers un sous compartiment à l'intérieur de la cellule ou elle sera dégradée.

Arrested kinetic Li isotope fractionation at the margin of the llimaussaq complex, South Greenland: Evidence for open-system processes during final cooling of peralkaline igneous rocks

Li contents [Li] and isotopic composition (delta Li-7) of mafic minerals (mainly amphibole and clinopyroxene) from the alkaline to peralkaline Ilimaussaq plutonic complex, South Greenland, track the behavior of Li and its isotopes during magmatic differentiation and final cooling of an alkaline igneous system. [Li] in amphibole increase from < 10 ppm in Caamphiboles of the least differentiated unit to >3000 ppm in Na-amphiboles of the highly evolved units. In contrast, [Li] in clinopyroxene are comparatively low (<85 ppm) and do not vary systematically with differentiation. The distribution of Li between amphibole and pyroxene is controlled by the major element composition of the minerals (Ca-rich and Na-rich, respectively) and changes in oxygen fugacity (due to Li incorporation via coupled substitution with ferric iron) during magmatic differentiation. delta(7) Li values of all minerals span a wide range from + 17 to - 8 parts per thousand, with the different intrusive units of the complex having distinct Li isotopic systematics. Amphiboles, which dominate the Li budget of whole-rocks from the inner part of the complex, have constant delta Li-7 of + 1.8 +/- 2.2 parts per thousand (2 sigma, n = 15). This value reflects a homogeneous melt reservoir and is consistent with their mantle derivation, in agreement with published O and Nd isotopic data. Clinopyroxenes of these samples are consistently lighter, with Delta Li-7(amph-cpx). as large as 8 parts per thousand and are thus not in Li isotope equilibrium. These low values probably reflect late-stage diffusion of Li into clinopyroxene during final cooling of the rocks, thus enriching the clinopyroxene in 6 Li. At the margin of the complex delta(7) Li in the syenites increases systematically, from +2 to high values of + 14 parts per thousand. This, coupled with the observed Li isotope systematics of the granitic country rocks, reflects post-magmatic open-system processes occurring during final cooling of the intrusion. Although the shape and magnitude of the Li isotope and elemental profiles through syenite and country rock are suggestive of diffusion-driven isotope fractionation, they cannot be modeled by one-dimensional diffusive transport and point to circulation of a fluid having a high 67 Li value (possibly seawater) along the chilled contact. In all, this study demonstrates that Li isotopes can be used to identify complex fluid- and diffusion-governed processes taking place during the final cooling of such rocks. (c) 2007 Elsevier B.V All rights reserved.

SCAP is required for timely and proper myelin membrane synthesis.

Myelination requires a massive increase in glial cell membrane synthesis. Here, we demonstrate that the acute phase of myelin lipid synthesis is regulated by sterol regulatory element-binding protein (SREBP) cleavage activation protein (SCAP), an activator of SREBPs. Deletion of SCAP in Schwann cells led to a loss of SREBP-mediated gene expression involving cholesterol and fatty acid synthesis. Schwann cell SCAP mutant mice show congenital hypomyelination and abnormal gait. Interestingly, aging SCAP mutant mice showed partial regain of function; they exhibited improved gait and produced small amounts of myelin indicating a slow SCAP-independent uptake of external lipids. Accordingly, extracellular lipoproteins partially rescued myelination by SCAP mutant Schwann cells. However, SCAP mutant myelin never reached normal thickness and had biophysical abnormalities concordant with abnormal lipid composition. These data demonstrate that SCAP-mediated regulation of glial lipogenesis is key to the proper synthesis of myelin membrane, and provide insight into abnormal Schwann cell function under conditions affecting lipid metabolism.

Fast subplasma membrane Ca2+ transients control exo-endocytosis of synaptic-like microvesicles in astrocytes

Astrocytes are the most abundant glial cell type in the brain. Although not apposite for long-range rapid electrical communication, astrocytes share with neurons the capacity of chemical signaling via Ca(2+)-dependent transmitter exocytosis. Despite this recent finding, little is known about the specific properties of regulated secretion and vesicle recycling in astrocytes. Important differences may exist with the neuronal exocytosis, starting from the fact that stimulus-secretion coupling in astrocytes is voltage independent, mediated by G-protein-coupled receptors and the release of Ca(2+) from internal stores. Elucidating the spatiotemporal properties of astrocytic exo-endocytosis is, therefore, of primary importance for understanding the mode of communication of these cells and their role in brain signaling. We here take advantage of fluorescent tools recently developed for studying recycling of glutamatergic vesicles at synapses (Voglmaier et al., 2006; Balaji and Ryan, 2007); we combine epifluorescence and total internal reflection fluorescence imaging to investigate with unprecedented temporal and spatial resolution, the stimulus-secretion coupling underlying exo-endocytosis of glutamatergic synaptic-like microvesicles (SLMVs) in astrocytes. Our main findings indicate that (1) exo-endocytosis in astrocytes proceeds with a time course on the millisecond time scale (tau(exocytosis) = 0.24 +/- 0.017 s; tau(endocytosis) = 0.26 +/- 0.03 s) and (2) exocytosis is controlled by local Ca(2+) microdomains. We identified submicrometer cytosolic compartments delimited by endoplasmic reticulum tubuli reaching beneath the plasma membrane and containing SLMVs at which fast (time-to-peak, approximately 50 ms) Ca(2+) events occurred in precise spatial-temporal correlation with exocytic fusion events. Overall, the above characteristics of transmitter exocytosis from astrocytes support a role of this process in fast synaptic modulation.

Distinct ASIC currents are expressed in rat putative nociceptors and are modulated by nerve injury.

The H(+)-gated acid-sensing ion channels (ASICs) are expressed in dorsal root ganglion (DRG) neurones. Studies with ASIC knockout mice indicated either a pro-nociceptive or a modulatory role of ASICs in pain sensation. We have investigated in freshly isolated rat DRG neurones whether neurones with different ASIC current properties exist, which may explain distinct cellular roles, and we have investigated ASIC regulation in an experimental model of neuropathic pain. Small-diameter DRG neurones expressed three different ASIC current types which were all preferentially expressed in putative nociceptors. Type 1 currents were mediated by ASIC1a homomultimers and characterized by steep pH dependence of current activation in the pH range 6.8-6.0. Type 3 currents were activated in a similar pH range as type 1, while type 2 currents were activated at pH < 6. When activated by acidification to pH 6.8 or 6.5, the probability of inducing action potentials correlated with the ASIC current density. Nerve injury induced differential regulation of ASIC subunit expression and selective changes in ASIC function in DRG neurones, suggesting a complex reorganization of ASICs during the development of neuropathic pain. In summary, we describe a basis for distinct cellular functions of different ASIC types in small-diameter DRG neurones.

Plasma membrane cyclic nucleotide gated calcium channels control land plant thermal sensing and acquired thermotolerance.

Typically at dawn on a hot summer day, land plants need precise molecular thermometers to sense harmless increments in the ambient temperature to induce a timely heat shock response (HSR) and accumulate protective heat shock proteins in anticipation of harmful temperatures at mid-day. Here, we found that the cyclic nucleotide gated calcium channel (CNGC) CNGCb gene from Physcomitrella patens and its Arabidopsis thaliana ortholog CNGC2, encode a component of cyclic nucleotide gated Ca(2+) channels that act as the primary thermosensors of land plant cells. Disruption of CNGCb or CNGC2 produced a hyper-thermosensitive phenotype, giving rise to an HSR and acquired thermotolerance at significantly milder heat-priming treatments than in wild-type plants. In an aequorin-expressing moss, CNGCb loss-of-function caused a hyper-thermoresponsive Ca(2+) influx and altered Ca(2+) signaling. Patch clamp recordings on moss protoplasts showed the presence of three distinct thermoresponsive Ca(2+) channels in wild-type cells. Deletion of CNGCb led to a total absence of one and increased the open probability of the remaining two thermoresponsive Ca(2+) channels. Thus, CNGC2 and CNGCb are expected to form heteromeric Ca(2+) channels with other related CNGCs. These channels in the plasma membrane respond to increments in the ambient temperature by triggering an optimal HSR, leading to the onset of plant acquired thermotolerance.

Membrane fluidization triggers membrane remodeling which affects the thermotolerance in Escherichia coli.

Treatment of Escherichia coli with non-lethal doses of heat or benzyl alcohol (BA) causes transient membrane fluidization and permeabilization, and induces the rapid transcription of heat-shock genes in a sigma32-dependent manner. This early response is followed by a rapid adaptation (priming) of the cells to otherwise lethal elevated temperature, in strong correlation with an observed remodeling of the composition and alkyl chain unsaturation of membrane lipids. The acquisition of cellular thermotolerance in BA-primed cells is unrelated to protein denaturation and is not accompanied by the formation of major heat-shock proteins, such as GroEL and DnaK. This suggests that the rapid remodeling of membrane composition is sufficient for the short-term bacterial thermotolerance.

Unraveling the complex network of cuticular structure and function.

A hydrophobic cuticle is deposited at the outermost extracellular matrix of the epidermis in primary tissues of terrestrial plants. Besides forming a protective shield against the environment, the cuticle is potentially involved in several developmental processes during plant growth. A high degree of variation in cuticle composition and structure exists between different plant species and tissues. Lots of progress has been made recently in understanding the different steps of biosynthesis, transport, and deposition of cuticular components. However, the molecular mechanisms that underlie cuticular function remain largely elusive.