921 resultados para HYDRATED PHOSPHOLIPID-BILAYERS
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Microparticles are small phospholipid vesicles of less than 1 µm released into the blood flow by various types of cells such as endothelial, platelet, white or red blood cells. They are involved in many biological and physiological processes including hemostasis. In addition, an elevated number of microparticles in the blood is observed in various pathological situations. In the context of transfusion, erythrocyte-derived microparticles are found in red blood cell concentrates. Their role is not elucidated, and they are considered as a type of storage lesion. The purpose of this review is to present recent data showing that erythrocyte-derived microparticles most likely play a role in transfusion medicine and could cause transfusion complications.
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Geochemical and petrographical studies of lavas and ignimbrites from the Quaternary Nisyros-Yali volcanic system in the easternmost part of the Hellenic arc (Greece) reveal insight into magma generating processes. A compositional gap between 61 and 68 wt.% SiO2 is recognized that coincides with the stratigraphic distinction between pre-caldera and postcaldera volcanic units. Trace element systematics support the subdivision of Nisyros and Yali volcanic units into two distinct suites of rocks. The variation of Nd and Hf present day isotope data and the fact that they are distinct from the isotope compositions of MORB rule out an origin by pure differentiation and require assimilation of a crustal component. Lead isotope ratios of Nisyros and Yali volcanic rocks support mixing of mantle material with a lower crust equivalent. However, Sr-87/Sr-86 ratios of 0.7036-0.7048 are incompatible with a simple binary mixing scenario and give low depleted mantle extraction ages (< 0.1 Ga), in contrast with Pb model ages of 0.3 Ga and Hf and Nd model ages of ca. 0.8 Ga. The budget of fluid-mobile elements Sr and Pb is likely to be dominated by abundant hydrous fluids characterised by mantle-like Sr isotope ratios. Late stage fluids probably were enriched in CO2, needed to explain the high Th concentrations. The occurrence of hydrated minerals (e.g., amphibole) in the first post-caldera unit with the lowermost Sr-87/Sr-86 ratio of 0.7036 +/- 2 can be interpreted as the result of the increased water activity in the source. The presence of two different plagioclase phenocryst generations in the first lava subsequent to the caldera-causing event is indicative for a longer storage time of this magma at a shallower level. A model capable of explaining these observations involves three evolutionary stages. First stage, assimilation of lower crustal material by a primitive magma of mantle origin (as modelled by Nd-Hf isotope systematics). This stage ended by an interruption in replenishment that led to an increase of crystallization and, hence, an increase in viscosity, suppressing eruption. During this time gap, differentiation by fractional crystallization led to enrichment of incompatible species, especially aqueous fluids, to silica depolymerisation and to a decrease in viscosity, finally enabling eruption again in the third stage. (c) 2005 Elsevier B.V. All rights reserved.
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Oxidative modification of LDL is thought to play an important role in the development of atherosclerosis. Susceptibility of LDL to peroxidation may partly depend on the compositional characteristics of the antioxidant and fatty acid content. The aim of this study was to examine the association between levels of antibodies to oxidized LDL and the various serum fatty acids in women. A total of 465 women aged 18-65 years were selected randomly from the adult population census of Pizarra, a town in southern Spain. Measurement of anti-oxidized-LDL was done by ELISA and the fatty acid composition of serum phospholipids was determined by GC. The levels of anti-oxidized-LDL antibodies were significantly related with age (r - 0.341, P < 0.001), BMI (r - 0.239, P < 0.001), waist:hip ratio (r - 0.285, P < 0.001), glucose (r - 0.208, P < 0.001), cholesterol (r - 0.243, P < 0.001), LDL-cholesterol (r - 0.185, P = 0.002), EPA (r - 0.159, P = 0.003), DHA (r - 0.121, P = 0.026), and the sum of the serum phospholipid n-3 PUFA (r - 0.141, P = 0.009). Multiple regression analysis showed that the variables that explained the behaviour of the levels of anti-oxidized-LDL antibodies were age (P < 0.001) and the serum phospholipid EPA (P < 0.001). This study showed that the fatty acid composition of serum phospholipids, and especially the percentage of EPA, was inversely related with the levels of anti-oxidized-LDL antibodies.
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Non-bilayer phospholipid arrangements are three-dimensional structures that form when anionic phospholipids with an intermediate structure of the tubular hexagonal phase II are present in a bilayer of lipids. Antibodies that recognise these arrangements have been described in patients with antiphospholipid syndrome and/or systemic lupus erythematosus and in those with preeclampsia; these antibodies have also been documented in an experimental murine model of lupus, in which they are associated with immunopathology. Here, we demonstrate the presence of antibodies against non-bilayer phospholipid arrangements containing mycolic acids in the sera of lepromatous leprosy (LL) patients, but not those of healthy volunteers. The presence of antibodies that recognise these non-bilayer lipid arrangements may contribute to the hypergammaglobulinaemia observed in LL patients. We also found IgM and IgG anti-cardiolipin antibodies in 77% of the patients. This positive correlation between the anti-mycolic-non-bilayer arrangements and anti-cardiolipin antibodies suggests that both types of antibodies are produced by a common mechanism, as was demonstrated in the experimental murine model of lupus, in which there was a correlation between the anti-non-bilayer phospholipid arrangements and anti-cardiolipin antibodies. Antibodies to non-bilayer lipid arrangements may represent a previously unrecognised pathogenic mechanism in LL and the detection of these antibodies may be a tool for the early diagnosis of LL patients.
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ABSTRACT :Azole antifungal drugs possess fungistatic activity in Candida albicans making this human pathogen tolerant to these agents. The conversion of azoles into fungicidal agents is of interest since their fungistatic properties increase the ability of C. albicans to develop drug resistance. In C. albicans, the phosphatase calcineurin (calcineurin) is essential for antifungal drug tolerance. Up to now, the only known target of calcineurin is Crzl, which is a transcription factor (TF) involved in responses to ionic stress. Thus, most of the components of the calcineurin signaling remain to be identified in C. albicans.In this work, the calcineurin pathway was investigated in order to i) characterize the role of calcineurin in the biology of C. albicans, ii) identify putative targets of calcineurin and iii) characterize the phenomenon of tolerance to antifungal drugs. Towards these aims, four different approaches were used.First, using C. albicans microarrays, an attempt was made to identify a set of calcineurindependent genes (CDGs). Since CDGs were highly dependent upon the external stimulus used to activate calcineurin (Ca2+ or terbinafine), this stimulus bias was bypassed by the construction of strains expressing a truncated autoactive form of calcineurin (Cmp1tr) in a doxycyclinedependent manner. The characterization of Cmpltr was undertaken and results showed that it mimicked awild-type activated calcineurin for all tested phenotypes (i.e. Cnbl-dependence, inhibition by FK506, phosphatase 2B activity, ability to dephosphorylate Crzl and to regulate Crz1-and calcineurin-dependent genes, role in antifungal drug tolerance and susceptibility, role in colony formation on Spider agar). Cmp1tr was therefore considered as a valid tool to study the calcineurin signaling pathway. In silico analysis of CDGs allowed the identification of i) a significant overlap between CDGs and genes regulated by the Cyrl signalíng pathway, ii) putative interactions between calcineurin activation and cell wall reorganization and phospholipid transport, iii) a putative interactión between calcineurin and the regulation of translation and iv) a putative relation between calcineurin and proteasome regulation. Further in silico analyses of the promoters of Crz1-independent CDGs were performed to identify TFs (other than Crz1) that were likely to regulate CDGs and therefore to be a direct target of calcineurin. The analyses revealed that Rpn4 and Mnl1 were TFs likely to be regulated by calcineurin.Second, in order to better characterize azole tolerance, an attempt was made to i) confirm the role of Hsp90 in fluconazole tolerance with a doxycycline-dependent Hsp90 expression system and ii) assess its calcineurin-dependence. Hsp90 was found to be significantly involved in fluconazole tolerance. However, results were not in agreement with the hypothesis that Hsp90 mediates fluconazole tolerance by the only downstream effector calcineurin. Rather Hsp90 is interacting with numerous components for fluconazole tolerance.Third, a collection of C. albicans TFs mutants were screened for loss of tolerance to terbinafine and fluconazole in order to identify TFs involved in antifungal drug tolerance. Out of the 265 TFs mutants screened, only the upc2Δ/Δ mutant showed a loss of fluconazole and terbinafine tolerance. Interestingly, no relation between Upc2 and calcineurin activity was found. These results suggested that the tolerance to antifungal drugs must not be only considered as a calcineurin-dependent phenomenon in C. albicans.Fourth, using FRCS analyses, an attempt was made to identify putative signs of programmed cell death (PCD) in calcineurin mutant cells upon loss of tolerance to terbinafine. A high proportion of cells died from both RO5-dependent (which is a sign of PCD) and ROS-independent (which is a sign of loss of homeostasis) processes in the calcineurin mutant. While these results suggest that calcineurin represses both loss of homeostasis and PCD, the role of calcineurin in PCD is still an open question.In conclusion, this work allowed i) the identification of several putative calcineurin targets, ii) the discovery of several links between calcineurin and signaling pathways and important biological processes and iii) the identification of novel components of calcineurin-independent mechanisms that participate in tolerance to antifungal drugs in C. albicans.RÉSUME :Les azoles sont des antifongiques qui présentent une activité fongistatique contre Candida albicans et rendent cette levure tolérante à ces agents. La conversion des azoles en agents fongicides est d'intérêts car leurs propriétés fongistatiques favorisent le développement de résistance aux drogues chez C. albicans. La calcineurine (calcineurin) est une phosphatase essentielle pour la tolérance aux antifongiques chez C. albicans. La seule cible connue de la calcineurin est Crz1, un facteur de transcription (FT) impliqué dans la réponse aux stress ionique. Ainsi, la plupart des constituants de la voie de signalisation de la calcineurin restent encore à être identifiés chez C. albicans.Dans ce travail de thèse, la voie de signalisation de la calcineurin a été étudiée de sorte à i) caractériser le rôle de la calcineurin dans la biologie de C. albicans, ii) identifier de nouvelles cibles de la calcineurin et iii) caractériser le phénomène de tolérance aux antifongiques. A ce propos, quatre approches ont été entreprises.Premièrement, des puces à ADN de C. albicans ont été utilisées afin d'identifier les gènes dépendants de la calcineurin (GDCs). Les GDCs étant étroitement dépendants du stimulus utilisé pour activer la calcineurin, le biais «stimulus» a été évité via la construction d'une souche exprimant une forme tronquée et autoactive de la calcineurin (Cmp1tr), en présence de doxycycline. La caractérisation de Cmp1tr a été entreprise et les résultats ont montré qu'elle mimait une calcineurin sauvage et activée pour la plupart des phénotypes testés (i.e. dépendance à Cnb1, inhibition par le FK506, activité phosphatase 2B, déphosphorylation de Crz1 et régulation de gènes dépendant de la calcineurin, rôle dans la tolérance et la susceptibilité aux antifongiques, rôle dans la formation des colonies sur milieu Spider). Cmp1tr a donc été considéré comme un outil pertinent pour l'étude de la voie de signalisation de la calcineurin. Les analyses in silico des GDCs ont permis l'identification i) d'un chevauchement entre les GDCs èt les gènes régulés par la voie de signalisation de Cyrl, ii) d'une interaction entre la calcineurin et la réorganisation de la paroi cellulaire ainsi que le transport des phospholipides, iii) d'une interaction entre calcineurin et la régulation de la traduction et iv) une relation entre la calcineurin et la régulation du protéasome. De plus, une analyse in silico des promoteurs des GDCs avec une régulation indépendante de Crz1 a permis d'identifier deux FTs qui pourraient être des cibles directes de la calcineurin, Rpn4 et Mnll.Deuxièmement, afin de caractériser la tolérance aux azoles, il a été entrepris i) de confirmer le rôle de Hsp90 dans la tolérance au fluconazole en utilisant un système d'expression dépendant de la doxycycline et ii) de caractériser sa dépendance à la calcineurin. Hsp90 a été montré impliqué dans la tolérance aux azoles. Cependant, les résultats n'ont pas corroboré une hypothèse expliquant le rôle d'Hsp90 dans la tolérance aux antifongiques par son unique. interaction avec la calcineurin. Il a été proposé que le rôle d'Hsp90 dans la tolérance aux antifongiques soit dû à ces multiples interactions avec le protéome de C. albicans plutôt que par son interaction avec un partenaire unique.Troisièmement, une collection de mutant pour des FTs de C. albicans a été criblée pour une perte de tolérance au fluconazole ou à la terbinafine, de sorte à identifier les FTs impliqués dans la tolérance aux antifongiques. Sur les 265 FTs passés au crible, seul le mutant upc2Δ/Δ a montré une perte de tolérance au fluconazole et à la terbinafine. Aucune relation n'a été trouvée entre la calcineurin et l'activité d'Upc2. Ces résultats suggèrent que la perte de tolérance aux antifongiques ne doit pas être considérée comme un phénomène exclusivement lié à la voie de signalisation de la calcineurin.Quatrièmement, en utilisant la cytométrie de flux, la présence de signes de mort cellulaire programmée (MCP) a été recherchée lors de la perte de tolérance du mutant calcineurin incubé avec de la terbinafine. Une grande proportion de cellules mortes incluant ou non une production de ROS (un signe de MCP) a été détectée dans le mutant calcineurin. Ces résultats préliminaires suggèrent que la calcineurin réprime autant la perte d'homéostasie qu'elle régule l'entrée en MCP. Cependant d'autres analyses sont nécessaires pour démontrer clairement le rôle de la calcineurin dans la régulation de la MCP.En conclusion, ce travail de thèse a permis i) l'identification de plusieurs cibles possibles de la calcineurine, ii) la découverte de plusieurs interactions entre la calcineurine et d'autres voies de signalisation et processus biologiques importants et iii) de démontrer la présence de voies indépendantes de la calcineurine impliquées dans la tolérance aux antifongiques chez C. albicans.
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Les poliamines (PAs) putrescina (Put), espermidina (Spd) i espermina (Spm) són mol•lècules policatiòniques de baix pes molecular, presents en els microorganismes, animals i plantes. Les PAs han estat implicades en diversos processos cel•lulars importants, incloent la resposta de les plantes a l'estrès. No obstant això, el seu mode d'acció està es desconeix. En les plantes, es van acumulant evidències de que les PAs interactuen amb macromolècules i estructures cel•lulars, com ara proteïnes de membrana, i la seva possible participació en transducció de senyals s'ha convertit en una creixent i interessant àrea d'estudi. En aquesta tesi, la possible interacció entre les poliamines i les vies de senyalització de fosfolípids és investigada. Resultats previs, han posat de manifest que alteracions en els nivells endògens de poliamines (PAs), per sobreexpressió gènica o pèrdua de funció de gens de biosíntesi, redueixen o milloren, respectivament, la capacitat de les plantes d'Arabidopsis per tolerar agressions per estrès abiòtic, produint en alguns casos notables alteracions en el desenvolupament. En aquestes plantes amb nivells alterats de PAs s'han detectat canvis importants en l'expressió gènica i s'ha trobat una connexió entre el contingut de PAs ii la biosíntesi / senyalització d'àcid abscísic (ABA). La hipòtesi actual de treball és que aquestes alteracions en l'expressió gènica poden estar mediades, si més no en part, pel catabolisme de PAs, i l’acció directa o indirecta de les espècies reactives d'oxigen (ROS) que se’n deriven.
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OBJECTIVES: A lipidomic approach was employed in a clinically well-defined cohort of healthy obese women to explore blood lipidome phenotype ascribed to body fat deposition, with emphasis on epicardial adipose tissue (EAT). METHODS: The present investigation delivered a lipidomics signature of epicardial adiposity under healthy clinical conditions using a cohort of 40 obese females (age: 25-45 years, BMI: 28-40 kg/m(2) ) not showing any metabolic disease traits. Lipidomics analysis of blood plasma was employed in combination with in vivo quantitation of mediastinal fat depots by computerized tomography. RESULTS: All cardiac fat depots correlated to indicators of hepatic dysfunctions (ALAT and ASAT), which describe physiological connections between hepatic and cardiac steatosis. Plasma lipidomics encompassed overall levels of lipid classes, fatty acid profiles, and individual lipid species. EAT and visceral fat associated with diacylglycerols (DAG), triglycerides, and distinct phospholipid and sphingolipid species. A pattern of DAG and phosphoglycerols was specific to EAT. CONCLUSIONS: Human blood plasma lipidomics appears to be a promising clinical and potentially diagnostic readout for patient stratification and monitoring. Association of blood lipidomics signature to regio-specific mediastinal and visceral adiposity under healthy clinical conditions may help provide more biological insights into obese patient stratification for cardiovascular disease risks.
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Visceral adiposity is increasingly recognized as a key condition for the development of obesity related disorders, with the ratio between visceral adipose tissue (VAT) and subcutaneous adipose tissue (SAT) reported as the best correlate of cardiometabolic risk. In this study, using a cohort of 40 obese females (age: 25-45 y, BMI: 28-40 kg/m(2)) under healthy clinical conditions and monitored over a 2 weeks period we examined the relationships between different body composition parameters, estimates of visceral adiposity and blood/urine metabolic profiles. Metabonomics and lipidomics analysis of blood plasma and urine were employed in combination with in vivo quantitation of body composition and abdominal fat distribution using iDXA and computerized tomography. Of the various visceral fat estimates, VAT/SAT and VAT/total abdominal fat ratios exhibited significant associations with regio-specific body lean and fat composition. The integration of these visceral fat estimates with metabolic profiles of blood and urine described a distinct amino acid, diacyl and ether phospholipid phenotype in women with higher visceral fat. Metabolites important in predicting visceral fat adiposity as assessed by Random forest analysis highlighted 7 most robust markers, including tyrosine, glutamine, PC-O 44∶6, PC-O 44∶4, PC-O 42∶4, PC-O 40∶4, and PC-O 40∶3 lipid species. Unexpectedly, the visceral fat associated inflammatory profiles were shown to be highly influenced by inter-days and between-subject variations. Nevertheless, the visceral fat associated amino acid and lipid signature is proposed to be further validated for future patient stratification and cardiometabolic health diagnostics.
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Contact aureoles provide an excellent geologic environment to study the mechanisms of metamorphic reactions in a natural system. The Torres del Paine (TP) intrusion is one of the most spectacular natural laboratories because of its excellent outcrop conditions. It formed in a period from 12.59 to 12.43 Ma and consists of three large granite and four smaller mafic batches. The oldest granite is on top, the youngest at the bottom of the granitic complex, and the granites overly the mafic laccolith. The TP intruded at a depth of 2-3 km into regional metamorphic anchizone to greenschist facies pelites, sandstones, and conglomerates of the Cerro Toro and Punta Barrosa formations. It formed a thin contact aureole of 150-400 m width. This thesis focuses on the reaction kinetics of the mineral cordierite in the contact aureole using quantitative textural analysis methods. First cordierite was formed from chlorite break¬down (zone I, ca. 480 °C, 750 bar). The second cordierite forming reaction was the muscovite break-down, which is accompanied by a modal decrease in biotite and the appearance of k- feldspar (zone II, 540-550 °C, 750 bar). Crystal sizes of the roundish, poikiloblastic cordierites were determined from microscope thin section images by manually marking each crystal. Images were then automatically processed with Matlab. The correction for the intersection probability of each crystal radius yields the crystal size distribution in the rock. Samples from zone I below the laccolith have the largest crystals (0.09 mm). Cordierites from zone II are smaller, with a maximum crystal radius of 0.057 mm. Rocks from zone II have a larger number of small cordierite crystals than rocks from zone I. A combination of these quantitative analysis with numerical modeling of nucleation and growth, is used to infer nucleation and growth parameters which are responsible for the observed mineral textures. For this, the temperature-time paths of the samples need to be known. The thermal history is complex because the main body of the intrusion was formed by several intrusive batches. The emplacement mechanism and duration of each batch can influence the thermal structure in the aureole. A possible subdivision of batches in smaller increments, so called pulses, will focus heat at the side of the intrusion. Focusing all pulses on one side increases the contact aureole size on that side, but decreases it on the other side. It forms a strongly asymmetric contact aureole. Detailed modeling shows that the relative thicknesses of the TP contact aureole above and below the intrusion (150 and 400 m) are best explained by a rapid emplacement of at least the oldest granite batch. Nevertheless, temperatures are significantly too low in all models, compared to observed mineral assemblages in the hornfelses. Hence, an other important thermal mechanisms needs to take place in the host rock. Clastic minerals in the immature sediments outside the contact aureole are hydrated due to small amounts of expelled fluids during contact metamorphism. This leads to a temperature increase of up to 50 °C. The origin of fluids can be traced by stable isotopes. Whole rock stable isotope data (6D and δ180) and chlorine concentrations in biotite document that the TP intrusion induced only very small amounts of fluid flow. Oxygen whole rock data show δ180 values between 9.0 and 10.0 %o within the first 5 m of the contact. Values increase to 13.0 - 15.0 %o further away from the intrusion. Whole rock 6D values display a more complex zoning. First, host rock values (-90 to -70 %o) smoothly decrease towards the contact by ca. 20 %o, up to a distance of ca. 150 m. This is followed by an increase of ca. 20 %o within the innermost 150 m of the aureole (-97.0 to -78 %o at the contact). The initial decrease in 6D values is interpreted to be due to Rayleigh fractionation accompanying the dehydration reactions forming cordierite, while the final increase reflects infiltration of water-rich fluids from the intrusion. An over-estimate on the quantity and the corresponding thermal effect yields a temperature increase of less than 30 °C. This suggests that fluid flow might have contributed only for a small amount to the thermal evolution of the system. A combination of the numerical growth model with the thermal model, including the hydration reaction enthalpies but neglecting fluid flow and incremental growth, can be used to numerically reproduce the observed cordierite textures in the contact aureole. This yields kinetic parameters which indicate fast cordierite crystallization before the thermal peak in the inner aureole, and continued reaction after the thermal peak in the outermost aureole. Only small temperature dependencies of the kinetic parameters seem to be needed to explain the obtained crystal size data. - Les auréoles de contact offrent un cadre géologique privilégié pour l'étude des mécanismes de réactions métamorphiques associés à la mise en place de magmas dans la croûte terrestre. Par ses conditions d'affleurements excellentes, l'intrusion de Torres del Paine représente un site exceptionnel pour améliorer nos connaissances de ces processus. La formation de cette intrusion composée de trois injections granitiques principales et de quatre injections mafiques de volume inférieur couvre une période allant de 12.50 à 12.43 Ma. Le plus vieux granite forme la partie sommitale de l'intrusion alors que l'injection la plus jeune s'observe à la base du complexe granitique; les granites recouvrent la partie mafique du laccolite. L'intrusion du Torres del Paine s'est mise en place a 2-3 km de profondeur dans un encaissant métamorphique. Cet encaissant est caractérisé par un métamorphisme régional de faciès anchizonal à schiste vert et est composé de pélites, de grès, et des conglomérats des formations du Cerro Toro et Punta Barrosa. La mise en place des différentes injections granitiques a généré une auréole de contact de 150-400 m d'épaisseur autour de l'intrusion. Cette thèse se concentre sur la cinétique de réaction associée à la formation de la cordiérite dans les auréoles de contact en utilisant des méthodes quantitatives d'analyses de texture. On observe plusieurs générations de cordiérite dans l'auréole de contact. La première cordiérite est formée par la décomposition de la chlorite (zone I, environ 480 °C, 750 bar), alors qu'une seconde génération de cordiérite est associée à la décomposition de la muscovite, laquelle est accompagnée par une diminution modale de la teneur en biotite et l'apparition de feldspath potassique (zone II, 540-550 °C, 750 bar). Les tailles des cristaux de cordiérites arrondies et blastic ont été déterminées en utilisant des images digitalisées des lames minces et en marquant individuellement chaque cristal. Les images sont ensuite traitées automatiquement à l'aide du programme Matlab. La correction de la probabilité d'intersection en fonction du rayon des cristaux permet de déterminer la distribution de la taille des cristaux dans la roche. Les échantillons de la zone I, en dessous du lacolite, sont caractérisés par de relativement grands cristaux (0.09 mm). Les cristaux de cordiérite de la zone II sont plus petits, avec un rayon maximal de 0.057 mm. Les roches de la zone II présentent un plus grand nombre de petits cristaux de cordiérite que les roches de la zone I. Une combinaison de ces analyses quantitatives avec un modèle numérique de nucléation et croissance a été utilisée pour déduire les paramètres de nucléation et croissance contrôlant les différentes textures minérales observées. Pour développer le modèle de nucléation et de croissance, il est nécessaire de connaître le chemin température - temps des échantillons. L'histoire thermique est complexe parce que l'intrusion est produite par plusieurs injections successives. En effet, le mécanisme d'emplace¬ment et la durée de chaque injection peuvent influencer la structure thermique dans l'auréole. Une subdivision des injections en plus petits incréments, appelés puises, permet de concentrer la chaleur dans les bords de l'intrusion. Une mise en place préférentielle de ces puises sur un côté de l'intrusion modifie l'apport thermique et influence la taille de l'auréole de contact produite, auréole qui devient asymétrique. Dans le cas de la première injection de granite, une modélisation détaillée montre que l'épaisseur relative de l'auréole de contact de Torres del Paine au-dessus et en dessous de l'intrusion (150 et 400 m) est mieux expliquée par un emplacement rapide du granite. Néanmoins, les températures calculées dans l'auréole de con¬tact sont trop basses pour que les modèles thermiques soient cohérants par rapport à la taille de cette auréole. Ainsi, un autre mecanisme exothermique est nécessaire pour permettre à la roche encais¬sante de produire les assemblages observés. L'observation des roches encaissantes entourant les granites montre que les minéraux clastiques dans les sédiments immatures au-dehors de l'auréole sont hydratés suite à la petite quantité de fluide expulsée durant le métamorphisme de contact et/ou la mise en place des granites. Les réactions d'hydratation peuvent permettre une augmentation de la température jusqu'à 50 °C. Afin de déterminer l'origine des fluides, une étude isotopique de roches de l'auréole de contact a été entreprise. Les isotopes stables d'oxygène et d'hydrogène sur la roche totale ainsi que la concentration en chlore dans la biotite indiquent que la mise en place des granites du Torres del Paine n'induit qu'une circulation de fluide limitée. Les données d'oxygène sur roche totale montrent des valeurs δ180 entre 9.0 et 10.0%o au sein des cinq premiers mètres du contact. Les valeurs augmentent jusqu'à 13.0 - 15.0 plus on s'éloigne de l'intrusion. Les valeurs 5D sur roche totale montrent une zonation plus complexe. Les valeurs de la roche encaissante (-90 à -70%o) diminuent progressivement d'environ 20%o depuis l'extérieur de l'auréole jusqu'à une distance d'environ 150 m du granite. Cette diminution est suivie par une augmentation d'environ 20%o au sein des 150 mètres les plus proches du contact (-97.0 à -78%o au contact). La diminution initiale des valeurs de 6D est interprétée comme la conséquence du fractionnement de Rayleigh qui accompagne les réactions de déshydratation formant la cordiérite, alors que l'augmentation finale reflète l'infiltration de fluide riche en eau venant de l'intrusion. A partir de ces résultats, le volume du fluide issu du granite ainsi que son effet thermique a pu être estimé. Ces résultats montrent que l'augmentation de température associée à ces fluides est limitée à un maximum de 30 °C. La contribution de ces fluides dans le bilan thermique est donc faible. Ces différents résultats nous ont permis de créer un modèle thermique associé à la for¬mation de l'auréole de contact qui intègre la mise en place rapide du granite et les réactions d'hydratation lors du métamorphisme. L'intégration de ce modèle thermique dans le modèle numérique de croissance minérale nous permet de calculer les textures des cordiérites. Cepen¬dant, ce modèle est dépendant de la vitesse de croissance et de nucléation de ces cordiérites. Nous avons obtenu ces paramètres en comparant les textures prédites par le modèle et les textures observées dans les roches de l'auréole de contact du Torres del Paine. Les paramètres cinétiques extraits du modèle optimisé indiquent une cristallisation rapide de la cordiérite avant le pic thermique dans la partie interne de l'auréole, et une réaction continue après le pic thermique dans la partie la plus externe de l'auréole. Seules de petites dépendances de température des paramètres de cinétique semblent être nécessaires pour expliquer les don¬nées obtenues sur la distribution des tailles de cristaux. Ces résultats apportent un éclairage nouveau sur la cinétique qui contrôle les réactions métamorphiques.
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BACKGROUND AND OBJECTIVES: Microparticles (MPs) are small phospholipid vesicles of less than 1 microm, shed in blood flow by various cell types. These MPs are involved in several biological processes and diseases. MPs have also been detected in blood products; however, their role in transfused patients is unknown. The purpose of this study was to characterize those MPs in blood bank conditions. MATERIALS AND METHODS: Qualitative and quantitative experiments using flow cytometry or proteomic techniques were performed on MPs derived from erythrocytes concentrates. In order to count MPs, they were either isolated by various centrifugation procedures or counted directly in erythrocyte concentrates. RESULTS: A 20-fold increase after 50 days of storage at 4 degrees C was observed (from 3370 +/- 1180 MPs/microl at day 5 to 64 850 +/- 37 800 MPs/microl at day 50). Proteomic analysis revealed changes of protein expression comparing MPs to erythrocyte membranes. Finally, the expression of Rh blood group antigens was shown on MPs generated during erythrocyte storage. CONCLUSIONS: Our work provides evidence that storage of red blood cell is associated with the generation of MPs characterized by particular proteomic profiles. These results contribute to fundamental knowledge of transfused blood products.
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Although hemoglobin (Hb) is mainly present in the cytoplasm of erythrocytes (red blood cells), lower concentrations of pure, cell-free Hb are released permanently into the circulation due to an inherent intravascular hemolytic disruption of erythrocytes. Previously it was shown that the interaction of Hb with bacterial endotoxins (lipopolysaccharides, LPS) results in a significant increase of the biological activity of LPS. There is clear evidence that the enhancement of the biological activity of LPS by Hb is connected with a disaggregation of LPS. From these findings one questions whether the property to enhance the biological activity of endotoxin, in most cases proven by the ability to increase the cytokine (tumor-necrosis-factor-alpha, interleukins) production in human mononuclear cells, is restricted to bacterial endotoxin or is a more general principle in nature. To elucidate this question, we investigated the interaction of various synthetic and natural virulence (pathogenicity) factors with hemoglobin of human or sheep origin. In addition to enterobacterial R-type LPS a synthetic bacterial lipopeptide and synthetic phospholipid-like structures mimicking the lipid A portion of LPS were analysed. Furthermore, we also tested endotoxically inactive LPS and lipid A compounds such as those from Chlamydia trachomatis. We found that the observations made for endotoxically active form of LPS can be generalized for the other synthetic and natural virulence factors: In every case, the cytokine-production induced by them is increased by the addition of Hb. This biological property of Hb is connected with its physical property to convert the aggregate structures of the virulence factors into one with cubic symmetry, accompanied with a considerable reduction of the size and number of the original aggregates.
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La fecundidad de la sardina peruana, Sardinops sagax, fue determinada por primera vez contando el número de ovocitos hidratados. El análisis de varianza mostró que las diferencias entre submuestras tomadas de diferentes áreas del ovario fueron en unos casos significativas al nivel del 5%. Estas diferencias son insignificantes a nivel de la población tomando en consideración la alta variación de la fecundidad entre diferentes hembras del mismo peso.
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Un nuevo método, el conteo de ovocitos hidratados, se aplica por primera vez para determinar la fecundidad de la caballa peruana (Scomber Japonicus peruanus) . En febrero de 1985, la fecundidad relativa media fue 278 huevos por gramo de hembra y la fecundidad parcial media de la muestra fue 78,174 huevos por hembra. Se muestra que la caballa del Perú es un desovador múltiple.
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Microparticles are phospholipid vesicles shed mostly in biological fluids, such as blood or urine, by various types of cells, such as red blood cells (RBCs), platelets, lymphocytes, endothelial cells. These microparticles contain a subset of the proteome of their parent cell, and their ready availability in biological fluid has raised strong interest in their study, as they might be markers of cell damage. However, their small size as well as their particular physico-chemical properties makes them hard to detect, size, count and study by proteome analysis. In this review, we report the pre-analytical and methodological caveats that we have faced in our own research about red blood cell microparticles in the context of transfusion science, as well as examples from the literature on the proteomics of various kinds of microparticles.
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Apart from its role during labor and lactation, oxytocin is involved in several other functions. Interestingly, oxytocin- and oxytocin receptor-deficient mice develop late-onset obesity with normal food intake, suggesting that the hormone might exert a series of beneficial metabolic effects. This was recently confirmed by data showing that central oxytocin infusion causes weight loss in diet-induced obese mice. The aim of the present study was to unravel the mechanisms underlying such beneficial effects of oxytocin. Chronic central oxytocin infusion was carried out in high fat diet-induced obese rats. Its impact on body weight, lipid metabolism and insulin sensitivity was determined. We observed a dose-dependent decrease in body weight gain, increased adipose tissue lipolysis and fatty acid β-oxidation, as well as reduced glucose intolerance and insulin resistance. The additional observation that plasma oxytocin levels increased upon central infusion suggested that the hormone might affect adipose tissue metabolism by direct action. This was demonstrated using in vitro, ex vivo, as well as in vivo experiments. With regard to its mechanism of action in adipose tissue, oxytocin increased the expression of stearoyl-coenzyme A desaturase 1, as well as the tissue content of the phospholipid precursor, N-oleoyl-phosphatidylethanolamine, the biosynthetic precursor of the oleic acid-derived PPAR-alpha activator, oleoylethanolamide. Because PPAR-alpha regulates fatty acid β-oxidation, we hypothesized that this transcription factor might mediate the oxytocin effects. This was substantiated by the observation that, in contrast to its effects in wild-type mice, oxytocin infusion failed to induce weight loss and fat oxidation in PPAR-alpha-deficient animals. Altogether, these results suggest that oxytocin administration could represent a promising therapeutic approach for the treatment of human obesity and type 2 diabetes.