Molecular insights into T cell activation : study of the TRAF, Bcl10 and Carma 1 proteins

Abstract : Activation of naïve T lymphocytes is essential for the onset of an adaptive immune response against a pathogenic threat. T lymphocytes are activated through the engagement of their highly specific cell surface antigen-receptor (TCR), together with co-stimulatory receptors, by activated antigen-presenting cells that display antigenic peptide fragments from the pathogen that they have detected. Dissection of the mechanisms that modulate TCR- and co-stimulation- induced signals is therefore crucial for the understanding of the molelcular basis of adaptive immune responses. Following antigen-receptor triggering, the Carma1, Bcl10 and Malt1 (CBM) proteins assemble into an oligomeric complex, which is essential for activation of the NF-κB and JNK signaling pathways in lymphocytes. In this work, by using human epithelial and lymphocytic cell lines, we identified the TNF-receptor-associated factor (TRAF) proteins TRAF3 and TRAF7 as new binding partners of Bcl10 and Carma1, respectively. We could show that TRAF3 is required for the proper transcriptional upregulation of IL-2 in activated T cells, and that endogenous TRAF3 is recruited to Bcl10 following TCR engagement. Although the mechanisms used by TRAF3 to modulate the transcriptional activation of the IL-2 promoter are not elucidated, the stimulus-dependent association ofTRAF3 with its direct binding partner Bcl10 suggests that TRAF3 is regulating Bcl10 function in TCR-activated lymphocytes. We also demonstrated that TRAF7 acts as a negative regulator of Carma1-induced NFκB-and AP1-dependent transcription by overexpression in 293T cells. These data suggest that TRAF7 could contribute to the negative regulation of TCR-dependent Carma1 functions. Finally, we showed that Carma1 is processed upon antigen-receptor triggering in B and T cell lines, as well as in primary human CTLs, and that this processing is dependent on the proteolytic activity of Malt1. Collectively, this work contributes to describe new proteins and regulatory mechanisms that modulate CBM-dependent functions in activated lymphocytes. Furthermore, it uncovers new tracks that could lead to a better molecular understanding of the complex interplay between the activatory and inhibitory regulators associated with the CBM complex. Résumé : L'activation des lymphocytes T naifs est une étape essentielle à la mise en place d'une réponse immunitaire adaptative pour combattre une infection. Après la détection d'un pathogène, les cellules présentatrices d'antigènes exposent à leur surface des fragments peptidiques provenant du pathogène, qui activent le récepteur à antigène (TCR) spécifique des lymphocytes T, ainsi que des molécules co-stimulatrices qui contribuent à l'activation complète des lymphocytes T. La caractérisation des mécanismes qui modulent les cascades de signaux émanant du TCR et des récepteurs de co-stimulation est essentielle à la compréhension du fonctionnement moléculaire de la réponse immunitaire adaptative. La ligation du TCR induit la formation d'un complexe oligomérique comprenant les protéines Carma1, Bcl10 et Malt1, qui est essentiel à l'activation des voies de signalisation cellulaires NF-κB et JNK induisant l'activation complète des lymphorctes T. Dans cette étude, à l'aide de lignées de cellules humaines épithéliales et lymphocytaires, nous avons identifié que deux protéines de la famille des TRAF (Tumor Necrosis Factor Receptor-Associated Factor), TRAF3 et TRAF7, s'associent à Bc110 et à Carma1, respectivement. Les TRAFs sont d'importants régulateurs des voies de signalisation dans les cellules du système immunitaire inné et adaptatif. Nous avons démontré que TRAF3 était important pour permettre la transcription de l'interleukine-2 (IL-2) dans les lymphocytes T activés, et que TRAF3 s'associait à Bc110 à la suite de la stimulation du TCR Les mécanismes que TRAF3 utilise pour moduler l'activation du promoteur de l'IL-2 ne sont pas connus, mais l'association de TRAF3 à Bc110 suite à la stimulation du TCR suggère que TRAF3 régule la fonction de Bc110. Nous avons également identifié TRAF7 comme un nouveau régulateur négatif des voies NF-κB et JNK induites par surexpression de la protéine Carma1. Nos données suggèrent que TRAF7 pourrait également contribuer à la régulation négative de la fonction de Carma1 dans les lymphocytes activés. Enfin, nous avons découvert que Carma1 était clivé suite à la stimulation du TCR, et que ce clivage dépendait de l'activité protéolytique de Malt1. Cette étude contribue ainsi à la description de nouvelles protéines et de nouveaux mécanismes qui modulent l'activité du complexe CBM dans les lymphocytes activés, et ouvre la voie à la caractérisation moléculaire de ces nouveaux mécanismes importants pour la régulation de la réponse immunitaire adaptative.

RAE-1, a novel PHR binding protein, is required for axon termination and synapse formation in Caenorhabditis elegans.

Previous studies in Caenorhabditis elegans showed that RPM-1 (Regulator of Presynaptic Morphology-1) regulates axon termination and synapse formation. To understand the mechanism of how rpm-1 functions, we have used mass spectrometry to identify RPM-1 binding proteins, and have identified RAE-1 (RNA Export protein-1) as an evolutionarily conserved binding partner. We define a RAE-1 binding region in RPM-1, and show that this binding interaction is conserved and also occurs between Rae1 and the human ortholog of RPM-1 called Pam (protein associated with Myc). rae-1 loss of function causes similar axon and synapse defects, and synergizes genetically with two other RPM-1 binding proteins, GLO-4 and FSN-1. Further, we show that RAE-1 colocalizes with RPM-1 in neurons, and that rae-1 functions downstream of rpm-1. These studies establish a novel postmitotic function for rae-1 in neuronal development.

The Gronnedal-Ika carbonatite-syenite complex, South Greenland: Carbonatite formation by liquid immiscibility

The Gronnedal-Ika complex is dominated by layered nepheline syenites which were intruded by a xenolithic syenite and a central plug of calcite to calcite-siderite carbonatite. Aegirine-augite, alkali feldspar and nepheline are the major mineral phases in the syenites, along with rare calcite. Temperatures of 680-910degreesC and silica activities of 0.28-0.43 were determined for the crystallization of the syenites on the basis of mineral equilibria. Oxygen fugacities, estimated using titanomagnetite compositions, were between 2 and 5 log units above the fayalite-magnetite-quartz buffer during the magmatic stage. Chondrite-normalized REE patterns of magmatic calcite in both carbonatites and syenites are characterized by REE enrichment (La-CN-Yb-CN = 10-70). Calcite from the carbonatites has higher Ba (similar to5490 ppm) and lower HREE concentrations than calcite from the syenites (54-106 ppm Ba). This is consistent with the behavior of these elements during separation of immiscible silicate-carbonate liquid pairs. epsilon(Nd)(T = 1.30 Ga) values of clinopyroxenes from the syenites vary between +1.8 and +2.8, and epsilon(Nd)(T) values of whole-rock carbonatites range from +2.4 to +2.8. Calcite from the carbonatites has delta(18)O values of 7.8 to 8.6parts per thousand and delta(13)C values of -3.9 to -4.6parts per thousand. delta(18)O values of clinopyroxene separates from the nepheline syenites range between 4.2 and 4.9parts per thousand. The average oxygen isotopic composition of the nepheline syenitic melt was calculated based on known rock-water and mineral-water isotope fractionation to be 5.7 +/- 0.4parts per thousand. Nd and C-O isotope compositions are typical for mantle-derived rocks and do not indicate significant crustal assimilation for either syenite or carbonatite magmas. The difference in delta(18)O between calculated syenitic melts and carbonatites, and the overlap in epsilon(Nd) values between carbonatites and syenites, are consistent with derivation of the carbonatites from the syenites via liquid immiscibility.

Geochemical study of vertebrate fossils from the Upper Cretaceous (Santonian) Csehbanya Formation (Hungary): Evidence for a freshwater habitat of mosasaurs and pycnodont fish

The diverse vertebrate remains from the Upper Cretaceous freshwater settings at Iharkut, Hungary, contain two fossil groups, Pycnodontiformes fish and Mosasauridae that are almost exclusively known from marine palaeo-environments. Hence, their appearance in alluvial sediments is very unusual. Trace element and isotope compositions of the remains have been analyzed to investigate the taphonomy and the ecological differences among the different fossil groups present at Iharkut. All examined fossils have undergone post-depositional diagenetic alteration, which resulted in high concentrations of REE, U, and Fe, together with almost complete homogenization of delta(18)O(CO3) values. Similar REE patterns in different fossils suggest a common origin for all remains, hence the discovered species most likely lived in the same local ecosystem. Despite partial diagenetic overprinting, the delta(18)O(PO4) values of the fossils indicate sufficient taxon-specific isotopic diversity to permit some broad conclusions on the palaeo-environment of the fossils. In particular, it is apparent that the isotopic composition of the Pycnodontiformes fish and Mosasauridae remains is most compatible with a freshwater palaeo-habitat and incompatible with a marine palaeo-environment. In addition, the Sr concentration and isotope data indicate that the Pycnodontiformes and Mosasauridae likely lived predominantly in a freshwater environment and were not simply occasional visitors to the Iharkut river ecosystem. Regarding other fossil groups, high delta(18)O(PO4) values of Alligatoroidea and Iharkutosuchus teeth suggest that these small crocodile species might have inhabited swamps and ponds where the water was relatively rich in (18)O due to evaporation. (c) 2009 Elsevier B.V. All rights reserved.

The influence of bacterial activity on phosphorite formation in the Miocene Monterey Formation, California

Authigenic phosphorites from the Miocene Monterey Formation (California) including an autochthonous phosphatic laminite were analyzed for molecular biomarkers, element content, and sulfur isotopic composition of associated pyrite and sulfate to evaluate the role of bacterial activity in the precipitation of phosphate minerals. The phosphorites formed in a depositional environment typified by upwelling with dynamic bottom currents and hardground formation. Pyrite enclosed in the phosphorites shows delta S-34 values as low as -36.5 parts per thousand VCDT, which is consistent with bacterial sulfate reduction. In a three-step extraction phosphorite dissolution extraction procedure, molecular fossils of sulfate-reducing bacteria (di-O-alkyl glycerol ethers and short-chain branched fatty acids i- and ai-C-15:0, i- and ai-C-17:0, and 10MeC(16:0)) were preferentially released from the mineral lattice. This suggests that the molecular fossils were tightly bound to carbonate fluorapatite, indicating that sulfate-reducing bacteria were involved in mineral formation. A close association of sulfate-reducing bacteria with large sulfide-oxidizing bacteria, which was previously suggested to favor carbonate fluorapatite precipitation, could neither be confirmed nor excluded for the Miocene Monterey Formation phosphorites. (C) 2012 Elsevier B.V. All rights reserved.

Climate and vegetation history of western Portugal inferred from Albian near-shore deposits (Gale Formation, Lusitanian Basin)

The late Early Cretaceous greenhouse climate has been studied intensively based on proxy data derived essentially from open marine archives. In contrast, information on continental climatic conditions and on the accompanying response of vegetation is relatively scarce, most notably owing to the stratigraphic uncertainties associated with many Lower Cretaceous terrestrial deposits. Here, we present a palynological record from Albian near-shore deposits of the Lusitanian Basin of W Portugal, which have been independently dated using Sr-isotope signals derived from low-Mg oyster shell calcite. Sr-87/Sr-86 values fluctuate between 0.707373 +/- 0.00002 and 0.707456 +/- 0.00003; absolute values and the overall stratigraphic trend match well with the global open marine seawater signature during Albian times. Based on the new Sr-isotope data, existing biostratigraphic assignments of the succession are corroborated and partly revised. Spore-pollen data provide information on the vegetation community structure and are flanked by sedimentological and clay mineralogical data used to infer the overall climatic conditions prevailing on the adjacent continent. Variations in the distribution of climate-sensitive pollen and spores indicate distinct changes in moisture availability across the studied succession with a pronounced increase in hygrophilous spores in late Early Albian times. Comparison with time-equivalent palynofloras from the Algarve Basin of southern Portugal shows pronounced differences in the xerophyte/hygrophyte ratio, interpreted to reflect the effect of a broad arid climate belt covering southern and southeastern Iberia during Early Albian times.

Choisir une carrière, faire carrière: les femmes médecins en France et en Grande-Bretagne

Cet article propose d'analyser les processus de construction de la ségrégation sexuée des professions dans une perspective comparative. Une étude comparative des carrières professionnelles et familiales des femmes médecins en France et en Grande-Bretagne permet de démontrer que, bien que la distribution des hommes et des femmes au sein de la profession médicale paraisse, à première vue, assez divergente, les processus de répartition sexuée entre les différentes positions au sein de la profession sont globalement identiques dans les deux pays. Ainsi, les résultats de cette recherche laissent penser que la structure sexuée de la profession médicale reste relativement peu changée par l'augmentation récente des taux de féminisation. Cette conclusion nous amène à inscrire notre travail dans le cadre des débats sociologiques récents sur l'analyse théorique des processus de reproduction de la division sexuelle du travail et de la ségrégation sexuée des emplois en Europe. This article proposes to analyse the process of the development of gendered segregation in a comparative perspective. A comparative study of the professional and family careers of women doctors in France and Britain makes it possible to show that, although at first sight the distribution of women and men in the medical profession seems rather different, the processes of gendered allocation between the different positions within the profession is generally the same in the two countries. The results of this research lead us to think that the gendered structure of the medical profession has been changed relatively little by the recent increase in the rate of feminisation. These conclusion leads us to situate our work within the framework of the recent sociological discussion of the theoretical analysis of the process of reproduction of the sexual division of labour and the gendered segregation of employment in Europe.

Astrocyte-neuron lactate transport is required for long-term memory formation.

We report that, in the rat hippocampus, learning leads to a significant increase in extracellular lactate levels that derive from glycogen, an energy reserve selectively localized in astrocytes. Astrocytic glycogen breakdown and lactate release are essential for long-term but not short-term memory formation, and for the maintenance of long-term potentiation (LTP) of synaptic strength elicited in vivo. Disrupting the expression of the astrocytic lactate transporters monocarboxylate transporter 4 (MCT4) or MCT1 causes amnesia, which, like LTP impairment, is rescued by L-lactate but not equicaloric glucose. Disrupting the expression of the neuronal lactate transporter MCT2 also leads to amnesia that is unaffected by either L-lactate or glucose, suggesting that lactate import into neurons is necessary for long-term memory. Glycogenolysis and astrocytic lactate transporters are also critical for the induction of molecular changes required for memory formation, including the induction of phospho-CREB, Arc, and phospho-cofilin. We conclude that astrocyte-neuron lactate transport is required for long-term memory formation.