Institutions, Public Debt and Foreign Finance

We study the role of domestic financial institutions in sustaining capital flows to the private and public sector of a country whose government can default on its debt. As in recent public debt crises, in our model public defaults weaken banks' balance sheets, disrupting domestic financial markets. This effect leads to a novel complementarity between private capital inflows and public borrowing, where the former sustain the latter by boosting the government's cost of default. Our key message is that, by shaping the direction of private capital flows, financial institutions determine whether financial integration improves or reduces government discipline. We explore the implications of this complementarity for financial liberalization and debt-financed bailouts of banks. We present some evidence consistent with complementarity.

Calcium antagonists as first-line therapy in hypertension: results of the Swiss Isradipine Study. Swiss Hypertension Society

In this study of the efficacy and safety of isradipine as first-line therapy in hypertension, 1,647 patients enrolled; 1,472 completed the 4-week placebo run-in period and began treatment with isradipine at 2.5 mg twice daily for 4 weeks. During placebo, 11% (n = 175) of the 1,647 patients withdrew because of normalization of blood pressure, side effects, noncompliance, violation of the study protocol, side effects from concomitant therapy, or other reasons. During isradipine therapy (n = 1,376), blood pressure decreased from 168 +/- 18/102 +/- 8 mm Hg at the end of the placebo period to 155 +/- 17/94 +/- 9 mm Hg after 2 weeks (p less than 0.001) and 151 +/- 16/92 +/- 9 mm Hg after 4 weeks (p less than 0.001). During active treatment, 6.4% (n = 94) were withdrawn because of flushing, headache, edema, palpitations, gastrointestinal side effects, skin rashes, or other side effects, and two patients because of lack of efficacy. The side effect score in the remaining patients worsened for flushing, remained unchanged for edema, but significantly improved for palpitations, fatigue, dizziness, headache, and nervousness. After 4 weeks, 60% of patients had diastolic blood pressures of less than or equal to 90 mm Hg. Thus, isradipine is effective and safe as first-line therapy in patients with primary hypertension as seen in general practice.

Reverse transcription quantitative real-time polymerase chain reaction reference genes in the spared nerve injury model of neuropathic pain: validation and literature search.

BACKGROUND: The reverse transcription quantitative real-time polymerase chain reaction (RT-qPCR) is a widely used, highly sensitive laboratory technique to rapidly and easily detect, identify and quantify gene expression. Reliable RT-qPCR data necessitates accurate normalization with validated control genes (reference genes) whose expression is constant in all studied conditions. This stability has to be demonstrated.We performed a literature search for studies using quantitative or semi-quantitative PCR in the rat spared nerve injury (SNI) model of neuropathic pain to verify whether any reference genes had previously been validated. We then analyzed the stability over time of 7 commonly used reference genes in the nervous system - specifically in the spinal cord dorsal horn and the dorsal root ganglion (DRG). These were: Actin beta (Actb), Glyceraldehyde-3-phosphate dehydrogenase (GAPDH), ribosomal proteins 18S (18S), L13a (RPL13a) and L29 (RPL29), hypoxanthine phosphoribosyltransferase 1 (HPRT1) and hydroxymethylbilane synthase (HMBS). We compared the candidate genes and established a stability ranking using the geNorm algorithm. Finally, we assessed the number of reference genes necessary for accurate normalization in this neuropathic pain model. RESULTS: We found GAPDH, HMBS, Actb, HPRT1 and 18S cited as reference genes in literature on studies using the SNI model. Only HPRT1 and 18S had been once previously demonstrated as stable in RT-qPCR arrays. All the genes tested in this study, using the geNorm algorithm, presented gene stability values (M-value) acceptable enough for them to qualify as potential reference genes in both DRG and spinal cord. Using the coefficient of variation, 18S failed the 50% cut-off with a value of 61% in the DRG. The two most stable genes in the dorsal horn were RPL29 and RPL13a; in the DRG they were HPRT1 and Actb. Using a 0.15 cut-off for pairwise variations we found that any pair of stable reference gene was sufficient for the normalization process. CONCLUSIONS: In the rat SNI model, we validated and ranked Actb, RPL29, RPL13a, HMBS, GAPDH, HPRT1 and 18S as good reference genes in the spinal cord. In the DRG, 18S did not fulfill stability criteria. The combination of any two stable reference genes was sufficient to provide an accurate normalization.

EBV+ cutaneous B-cell lymphoproliferation of the leg in an elderly patient with mycosis fungoides and methotrexate treatment.

A 77-year-old man with a 5-year history of mycosis fungoides (MF) who had received several lines of therapy, including intravenous courses of Methotrexate (MTX) for the past 2 years, went on to develop several ulcerated cutaneous nodules on the left leg. Biopsy revealed diffuse sheets of EBV-positive large B cells (CD20+ CD30 ± IgM Lambda), with an angiocentric distribution and a monoclonal IGH gene rearrangement. Although the pathological features were diagnostic for an EBV-positive diffuse large B-cell lymphoma (DLBCL), several possibilities could be considered for assignment to a specific entity: EBV-positive DLBCL of the elderly, methotrexate-induced lymphoproliferative disorder (LPD), lymphomatoid granulomatosis, or the more recently described EBV-positive mucocutaneous ulcer. The development of EBV+ lymphoproliferations has been reported in two other patients with MF under MTX, and occurred as skin lesions of the leg in one of these and in the current case, which may question the relatedness to primary cutaneous DLCBL, leg-type.

Importância da normalização contabilística na análise económica e financeira da empresa

O presente trabalho tem como objectivo demonstrar a importância da normalização contabilística para a análise da informação financeira, tendo em conta o meio envolvente em que, hoje, as empresas encontram-se inseridas. As mudanças que ocorreram na economia global levou a que as empresas passassem a adoptar novas formas de elaborar o reporte financeiro como forma de acompanhar essa evolução. A harmonização contabilística, surge neste contexto, como forma de reduzir as diferenças existentes no relato financeiro dos vários países. Nesse sentido o trabalho abordará as várias iniciativas que tem sido feitas em favor da harmonização/normalização contabilística e a sua relevância no contexto internacional e nacional bem como o caso de Cabo Verde, que recentemente aderiu ao processo da normalização. O caso prático baseia-se na transposição das demonstrações financeiras para o novo normativo em vigor e também na análise destas. A metodologia utilizada no trabalho baseia-se na revisão bibliográfica em livros, revistas, pela consulta de sites na Internet e legislação. The purpose of this paper is to demonstrate the importance of the accounting standard for the analysis of financial information, taking into account the environment in which, today, the companies are incorporated. The changes that occurred in the global economy have led companies to introduce new ways of preparing the financial reporting as a way to monitor these developments. The accounting harmonization, it is in this context as a way of reducing the differences existing in the financial reporting of the several countries. In this sense the work will address a variety of initiatives that have been made in favor of harmonization / normalization accounting and its relevance in the international and national context as well as the case of Cape Verde, who recently joined the process of standardization. The practical case is based in on the translation of financial statements for the new rules enforced and also in their analysis. The follows methodology used in the process is based on the literature review in books, magazines, by consulting Web sites and legislation

Primetime for antiangiogenic therapy.

PURPOSE OF REVIEW: To review the current experience with angiogenesis inhibitors in the treatment of gliomas. RECENT FINDINGS: Antiangiogenic therapy has recently reached the clinic with the approval of bevacizumab for recurrent glioblastomas. A number of promising antiangiogenic and vasculature-modifying agents are under investigation for newly diagnosed and recurrent malignant gliomas. A recurrence under ongoing or after antiangiogenic therapy is often characterized by a more aggressive and, in particular, invasive phenotype. SUMMARY: Despite impressively high radiological response rates in patients with recurrent malignant glioma, the duration of response is usually short-lived, and the observed effect to a large extent may be due to normalization of the disrupted blood-brain barrier and less due to a direct antitumor effect. Overall survival remains poor. Induction of invasive phenotypes and escape with proangiogenic alternative pathways are contributing to resistance. Investigation of combination regimes targeting several pathways will determine the possibilities to overcome the resistance to antiangiogenic therapy in malignant gliomas. This article summarizes the results of recent clinical trials in this field, points towards mechanisms of resistance arising under angiogenesis inhibition and discusses the challenges for the future.

State Fiscal Year 2006 Fact Sheet

INAPIS SFY06 Fact Sheets - INAPIS data is reported to DEA from AAAs and the Fact Sheets below represent information about consumers and services provided from July 1, 2005 through June 30, 2006. Information on these Fact Sheets comes from the INAPIS Activity Report (State Fiscal Year 2006).

The Hippo Transducer YAP1 Transforms Activated Satellite Cells and Is a Potent Effector of Embryonal Rhabdomyosarcoma Formation.

The role of the Hippo pathway effector YAP1 in soft tissue sarcomas is poorly defined. Here we report that YAP1 activity is elevated in human embryonal rhabdomyosarcoma (ERMS). In mice, sustained YAP1 hyperactivity in activated, but not quiescent, satellite cells induces ERMS with high penetrance and short latency. Via its transcriptional program with TEAD1, YAP1 directly regulates several major hallmarks of ERMS. YAP1-TEAD1 upregulate pro-proliferative and oncogenic genes and maintain the ERMS differentiation block by interfering with MYOD1 and MEF2 pro-differentiation activities. Normalization of YAP1 expression reduces tumor burden in human ERMS xenografts and allows YAP1-driven ERMS to differentiate in situ. Collectively, our results identify YAP1 as a potent ERMS oncogenic driver and a promising target for differentiation therapy.

PPARβ/δ governs Wnt signaling and bone turnover.

Peroxisome proliferator-activated receptors (PPARs) act as metabolic sensors and central regulators of fat and glucose homeostasis. Furthermore, PPARγ has been implicated as major catabolic regulator of bone mass in mice and humans. However, a potential involvement of other PPAR subtypes in the regulation of bone homeostasis has remained elusive. Here we report a previously unrecognized role of PPARβ/δ as a key regulator of bone turnover and the crosstalk between osteoblasts and osteoclasts. In contrast to activation of PPARγ, activation of PPARβ/δ amplified Wnt-dependent and β-catenin-dependent signaling and gene expression in osteoblasts, resulting in increased expression of osteoprotegerin (OPG) and attenuation of osteoblast-mediated osteoclastogenesis. Accordingly, PPARβ/δ-deficient mice had lower Wnt signaling activity, lower serum concentrations of OPG, higher numbers of osteoclasts and osteopenia. Pharmacological activation of PPARβ/δ in a mouse model of postmenopausal osteoporosis led to normalization of the altered ratio of tumor necrosis factor superfamily, member 11 (RANKL, also called TNFSF11) to OPG, a rebalancing of bone turnover and the restoration of normal bone density. Our findings identify PPARβ/δ as a promising target for an alternative approach in the treatment of osteoporosis and related diseases.

O Dualismo Cultural: os Luso-Caboverdianos entre a Escola a Família e a Comunidade (Estudo de Caso)

A tese que ora findamos visa a obtenção do grau de doutora em Educação, na Especialidade de Desenvolvimento Curricular, pelo Departamento do Currículo e Tecnologia Educativa, do Instituto de Educação e Psicologia, da Universidade do Minho. Intitulado o dualismo cultural: os luso-caboverdianos entre a escola, a família e a comunidade, o presente estudo centra-se numa abordagem crítica da escolaridade básica obrigatória, no qual procurámos compreender e explicar as condições de realização deste nível de ensino pelos jovens de ascendência caboverdiana, nascidos em Portugal, na qualidade de sujeitos biculturais em consequência da simbiose das culturas caboverdeana e portuguesa. Isto para concluirmos se na oferta do serviço educativo e de formação estão acautelados os seus direitos de cidadania e de participação na sociedade em que se encontram inseridos e a que pertencem de facto. Nesta investigação foi fundamental analisar a oferta de educação básica, entender as representações de alunos lusocaboverdeanos acerca da sua identidade cultural e das suas percepções sobre a formação académica que recebem; reconhecer representações e percepções de professores acerca da realidade educativa portuguesa, o enquadramento da multiculturalidade e a docência em turmas com alunos luso-caboverdianos, e compreender as percepções de pais e encarregados da educação caboverdeanos acerca da realidade educativa portuguesa e do enquadramento dos seus filhos na escola, para perceber se o insucesso educativo dos luso-caboverdeanos está relacionado com a condição de aluno “culturalmente diferente” ou se tem a sua origem na escola e no currículo da escolaridade obrigatória e, assim, contribuir com subsídios teóricos e práticos para o aprofundamento da problemática da multiculturalidade em Portugal, com vista à sua potenciação e normalização no sistema educativo. Estando perante uma sociedade de formação multicultural reafirmada com a colonização, justifica-se, em Portugal, a preocupação com a temática da diversidade cultural nas políticas educativas, resultante da consciencialização da manifestação da diversidade cultural no contexto escolar, podendo a sua omissão constituir num factor de insucesso educativo. Por isso, integramos nesta investigação matérias como: uma conceptualização do multiculturalismo com vista a questionar e clarificar os conceitos e as perspectivas inerentes a este fenómeno. Uma tentativa de desocultar para perceber o conteúdo simbólico e os porquês das políticas de integração das minorias etnicoculturais que, ao que parece, nos tempos que correm, por quase toda a parte, se converteram numa prioridade absoluta e inadiável. Estabelecemos uma ponte entre a génese do campo curricular e a construção de um currículo multi e/ou intercultural, merecendo devida atenção as tendências que dominam as discussões e a produção científica actuais nestes domínios. Problematizámos o currículo e identidade na escolaridade obrigatória nas dimensões inserção sociocultural, promoção da igualdade de sucesso educativo e inclusão dos sujeitos e o currículo e a educação para o exercício da cidadania numa escola que se quer plural. Neste último debatemos o conteúdo político da educação para a cidadania, as políticas educativas e curriculares e a escolaridade básica obrigatória como uma proposta que continua em aberto, por isso, passível de adequação às necessidades de uma educação da e para a diversidade. Procurámos fazer uma análise das políticas de integração socioeducativa da diversidade cultural, com destaque para o quadro legal que regula a integração das minorias étnicas na escola básica portuguesa, com particular incidência sobre as crianças pertencentes à comunidade caboverdeana nascidas em território português, procurando concluir acerca da existência, ou não, de posições e opções de políticas educativas concretas face à necessidade de dar prosseguimento à educação multicultural neste contexto. Tratou-se de uma investigação qualitativa holística, que permitiu desenvolver compreensões profundas dos fenómenos a partir das evidências reunidas, do estudo das representações dos sujeitos sobre quem recaem os resultados da investigação, mas também de sujeitos que, assim como o meio envolvente, estabelecem uma relação indirecta com os mesmos resultados. Circunscrito a um estudo de caso, a reflexão e a partilha de conhecimento e informações possibilitou desenvolver uma compreensão sobre a problemática estudada. Dos resultados obtidos, destacámos aqui que, em Portugal, apesar da absorvência da diversidade cultural nas política educativa, não se concretizou, ainda, uma proposta que, na prática, crie a reciprocidade entre as questões etnicoculturais e o sucesso e/ou insucesso educativos das minorias em educação com ganhos decisivos no combate ao insucesso e ao abandono escolar. Continua-se a desenvolver uma educação igualitarista monocultural pela via da homogeneização curricular, assente na noção de que povos e grupos podem estar em condições de igualdade se reunidos numa cultura comum. Aparentemente sob pilares democráticos, esta educação multicultural segue a concepção liberal associando essencialismo, universalismo e igualitarismo, resultando num propósito civilizacional excludente das minorias etnicoculturais. As conclusões chegadas permitem-nos defender a dessacralização do currículo nacional comum e uniforme e a defesa de uma proposta curricular baseada numa cultura científica global e necessária, de acordo com as faixas etárias e níveis de ensino, com campos de integração obrigatória de conteúdos territorializados alicerçados no interculturalismo como estratégia promotora da interacção crítica e solidária entre diferentes sujeitos e grupos culturais, permissiva da construção de identidades próprias e da confissão da diferença cultural, associada ao intraculturalismo como uma via permeabilizadora da educação democrática como garante da cidadania plena a todos os indivíduos, como condição fundamental para o estabelecimento das condições de igualdade e de garantia de sucesso em educação.

ViralZone: a knowledge resource to understand virus diversity.

The molecular diversity of viruses complicates the interpretation of viral genomic and proteomic data. To make sense of viral gene functions, investigators must be familiar with the virus host range, replication cycle and virion structure. Our aim is to provide a comprehensive resource bridging together textbook knowledge with genomic and proteomic sequences. ViralZone web resource (www.expasy.org/viralzone/) provides fact sheets on all known virus families/genera with easy access to sequence data. A selection of reference strains (RefStrain) provides annotated standards to circumvent the exponential increase of virus sequences. Moreover ViralZone offers a complete set of detailed and accurate virion pictures.

Geometry, petrology and growth of a shallow crustal laccolith : the Torres del Paine Mafic Complex (Patagonia)

1. ABSTRACTS - RÉSUMÉSSCIENTIFIC ABSTRACT - ENGLISH VERSIONGeometry, petrology and growth of a shallow crustal laccolith: the Torres del Paine Mafi c Complex (Patagonia)The Torres del Paine intrusive complex (TPIC) is a composite mafic-granitic intrusion, ~70km2, belonging to a chain of isolated Miocene plutons in southern Patagonia. Their position is intermediate between the Mesozoic-Cenozoic calc-alkaline subduction related Patagonian batholith in the West and the late Cenozoic alkaline basaltic back-arc related plateau lavas in the East. The Torres del Paine complex formed during an important reconfiguration of the Patagonian geodynamic setting, with a migration of magmatism from the arc to the back-arc, possibly related to the Chile ridge subductionThe complex intruded the flysch of the Cretaceous Cerro Toro and Punta Barrosa Formations during the Miocene, creating a well-defined narrow contact aureole of 200-400 m width.In its eastern part, the Torres del Paine intrusive complex is a laccolith, composed of a succession of hornblende-gabbro to diorite sills at its base, with a total thickness of ~250m, showing brittle contacts with the overlying granitic sills, that form spectacular cliffs of more than 1000m. This laccolith is connected, in the western part, to its feeding system, with vertical alternating sheets of layered gabbronorite and Hbl-gabbro, surrounded and percolated by diorites. ID-TIMS U-Pb on zircons on feeder zone (FZ) gab- bros yield 12.593±0.009Ma and 12.587±0.009Ma, which is identifcal within error to the oldest granite dated so far by Michel et al. (2008). In contrast, the laccolith mafic complex is younger than than the youngest granite (12.50±0.02Ma), and has been emplaced from 12.472±0.009Ma to 12.431 ±0.006Ma, by under-accretion beneath the youngest granite at the interface with previously emplaced mafic sills.The gabbronorite crystallization sequence in the feeder zone is dominated by olivine, plagioclase, clinopyroxene and orthopyroxene, while amphibole forms late interstitial crystals. The crystallization sequence is identical in Hornblende-gabbro from the feeder zone, with higher modal hornblende. Gabbronorite and Hornblende-gabbro both display distinct Eu and Sr positive anomalies. In the laccolith, a lower Hornblende-gabbro crystallized in sills and evolved to a high alkali shoshonitic series. The Al203, Ti02, Na20, K20, Ba and Sr composition of these gabbros is highly variable and increases up to ~50wt% Si02. The lower hornblende-gabbro is characterized by kaersutite anhedral cores with inclusions of olivine, clino- and orthopyroxene and rare apatite and An70 plagioclase. Trace element modelling indicates that hornblende and clinopyroxene are in equilibrium with a liquid whose composition is similar to late basaltic trachyandesitic dikes that cut the complex. The matrix in the lower hornblende gabbro is composed of normally zoned oligoclase, Magnesio-hornblende, biotite, ilmenite and rare quartz and potassium feldspar. This assemblage crystallized in-situ from a Ba and Sr-depleted melts. In contrast, the upper Hbl-gabbro is high-K calc-alkaline. Poikilitic pargasite cores have inclusions of euhedral An70 plagioclase inclusions, and contain occasionally clinopyroxene, olivine and orthopyroxene. The matrix composition is identical to the lower hornblende-gabbro and similar to the diorite. Diorite bulk rock compositions show the same mineralogy but different modal proportions relative to hornblende-gabbrosThe Torres del Paine Intrusive Complex isotopic composition is 87Sr/86Sr=0.704, 143Nd/144Nd=0.5127, 206Pb/204Pb=18.70 and 207Pb/204Pb=15.65. Differentiated dioritic and granitic units may be linked to the gabbroic cumulates series, with 20-50% trapped interstitial melt, through fractionation of olivine-bearing gabbronorite or hornblende-gabbro fractionation The relative homogeneity of the isotopic compositions indicate that only small amounts of assimilation occurred. Two-pyroxenes thermometry, clinopyroxene barometry and amphibole-plagioclase thermometry was used to estimate pressure and temperature conditions. The early fractionation of ultramafic cumulates occurs at mid to lower crustal conditions, at temperatures exceeding 900°C. In contrast, the TPIC emplacement conditions have been estimated to ~0.7±0.5kbar and 790±60°C.Based on field and microtextural observations and geochemical modelling, fractionation of basaltic-trachyandesitic liquids at intermediate to lower crustal levels, has led to the formation of the Torres del Paine granites. Repetitive replenishment of basaltic trachy- andesitic liquid in crustal reservoirs led to mixed magmas that will ascend via the feeder zone, and crystallize into a laccolith, in the form of successive dioritic and gabbroic sills. Dynamic fractionation during emplacement concentrated hornblende rich cumulates in the center of individual sills. Variable degrees.of post-emplacement compaction led to the expulsion of felsic liquids that preferentially concentrated at the top of the sills. Incremental sills amalgamation of the entire Torres del Paine Intrusive Complex has lasted for ~160ka.RESUME SCIENTIFIQUE - VERSION FRANÇAISEGéométrie, pétrologie et croissance d'un laccolite peu profond : Le complexe ma- fique du Torres del Paine (Patagonie)Le Complexe Intrusif du Torres del Paine (CITP) est une intrusion bimodale, d'environ 70km2, appartenant à une chaîne de plutons Miocènes isolés, dans le sud de la Patago-nie. Leur position est intermédiaire entre le batholite patagonien calco-alcalin, à l'Ouest, mis en place au Mesozoïque-Cenozoïque dans un contexte de subduction, et les basal-tes andésitiques et trachybasaltes alcalins de plateau, plus jeune, à l'Est, lié à l'ouverture d'un arrière-arc.A son extrémité Est, le CITP est une succession de sills de gabbro à Hbl et de diorite, sur une épaisseur de ~250m, avec des évidences de mélange. Les contacts avec les sills de granite au-dessus, formant des parois de plus de 1000m, sont cassants. Ce laccolite est connecté, dans sa partie Ouest, à une zone d'alimentation, avec des intrusions sub-ver- ticales de gabbronorite litée et de gabbro à Hbl, en alternance. Celles-ci sont traversées et entourées par des diorites. Les zircons des gabbros de la zone d'alimentation, datés par ID-TIMS, ont cristallisés à 12.593±0.009Ma et 12.587±0.009Ma, ce qui correspond au plus vieux granite daté à ce jour par Michel et al. (2008). A l'inverse, les roches manques du laccolite se sont mises en place entre 12.472±0.009Ma et 12.431 ±0.006Ma, par sous-plaquage successifs à l'interface avec le granite le plus jeune daté à ce jour (12.50±0.02Ma).La séquence de cristallisation des gabbronorites est dominée par Ol, Plg, Cpx et Opx, alors que la Hbl est un cristal interstitiel. Elle est identique dans les gabbros à Hbl de la zone d'alimentation, avec ~30%vol de Hbl. Les gabbros de la zone d'alimentation montrent des anomalies positives en Eu et Sr distinctes. Dans le laccolite, le gabbro à Hbl inférieur évolue le long d'une série shoshonitique, riche en éléments incompatibles. Sa concentration en Al203, Ti02, Na20, K20, Ba et Sr est très variable et augmente rapide-ment jusqu'à ~50wt% Si02. Il est caractérisé par la présence de coeurs résorbés de kaer- sutite, entourés de Bt, et contenant des inclusions d'OI, Cpx et Opx, ou alors d'Ap et de rares Plg (An70). Hbl et Cpx ont cristallisés à partir d'un liquide de composition similaire aux dykes trachy-andesite basaltique du CITP. La matrice, cristallisée in-situ à partir d'un liquide pauvre en Ba et Sr, est composée d'oligoclase zoné de façon simple, de Mg-Hbl, Bt, llm ainsi que de rares Qtz et KF. Le gabbro à Hbl supérieur, quant à lui, appartient à une suite chimique calco-alcaline riche en K. Des coeurs poecilitiques de pargasite con-tiennent de nombreuses inclusions de Plg (An70) automorphe, ainsi que des Ol, Cpx et Opx. La composition de la matrice est identique à celle des gabbros à Hbl inférieurs et toutes deux sont similaires à la minéralogie des diorites. Les analyses sur roches totales de diorites montrent la même variabilité que celles de gabbros à Hbl, mais avec une ten-eur en Si02 plus élevée.La composition isotopique des liquides primitifs du CITP a été mesurée à 87Sr/86Sr=0.704, 143Nd/144Nd=0.5127, 206Pb/204Pb=18.70 et 207Pb/204Pb=15.65. Les granites et diorites différenciés peuvent être reliés à des cumulais gabbronoritiques (F=0.74 pour les granites et F=1-0.5 pour les diorites) et gabbroïques à Hbl (fractionnement supplémentaire pour les granites, avec F=0.3). La cristallisation de 20 à 50%vol de liquide interstitiel piégé dans les gabbros du CITP explique leur signature géochimique. Seules de faibles quantités de croûte continentale ont été assimilées. La température et la pression de fractionnement ont été estimées, sur la base des thermobaromètres Opx-Cpx, Hbl-Plg et Cpx, à plus de 900°C et une profondeur correspondant à la croûte inférieure-moyenne. A l'inverse, les conditions de cristallisation de la matrice des gabbros et diorites du laccolite ont été estimées à 790±60°C et ~0.7±0.5kbar.Je propose que les liquides felsiques du CITP se soient formés par cristallisation frac-tionnée en profondeur des assemblages minéralogiques observés dans les gabbros du CITP, à partir d'un liquide trachy-andesite basaltique. La percolation de magma dans les cristaux accumulés permet la remontée du mélange à travers la zone d'alimentation, vers le laccolite, où des sills se mettent en place successivement. L'amalgamation de sills dans le CITP a duré ~160ka.Le CITP s'est formé durant une reconfiguration importante du contexte géodynamique en Patagonie, avec un changement du magmatisme d'arc vers un volcanisme d'arrière- arc. Ce changement est certainement lié à la subduction de la ride du Chili.RESUME GRAND PUBLIC - VERSION FRANÇAISEGéométrie, pétrologie et croissance d'une chambre magmatique peu profonde : Le complexe mafique du Torres del Paine (Patagonie)Le pourtour de l'Océan Pacifique est caractérisé par une zone de convergence de plaques tectoniques, appelée zone de subduction, avec le plongement de croûte océa-nique sous les Andes dans le cas de la Patagonie. De nombreux volcans y sont associés, formant la ceinture de feu. Mais seuls quelques pourcents de tout le magma traversant la croûte terrestre parviennent à la surface et la majeure partie cristallise en profondeur, dans des chambres magmatiques. Quelles est leur forme, croissance, cristallisation et durée de vie ? Le complexe magmatique du Torres del Paine représente l'un des meilleurs endroits au monde pour répondre à ces questions. Il se situe au sud de la Patagonie, formant un massif de 70km2. Des réponses peuvent être trouvées à différentes échelles, variant de la montagne à des minéraux de quelques 1000ème de millimètres.Il est possible de distinguer trois types de roches : des gabbros et des diorites sur une épaisseur de 250m, surmontées par des parois de granite de plus de 1000m. Les contacts entre ces roches sont tous horizontaux. Entre granites et gabbro-diorite, le contact est net, indiquant que le second magma s'est mis en place au contact avec un magma plus ancien, totalement solidifié. Entre gabbros et diorites, les contacts sont diffus, souvent non-linéaires, indiquant à l'inverse la mise en contact de magmas encore partiellement liquides. Dans la partie Ouest de cette chambre magmatique, les contacts entre roches sont verticaux. Il s'agit certainement du lieu de remplissage de la chambre magmatique.Lors du refroidissement d'un magma, différents cristaux vont se former. Leur stabilité et leur composition varient en fonction de la pression, de la température ou de la chimie du magma. La séquence de cristallisation peut être définie sur la base d'observations microscopiques et de la composition chimique des minéraux. Différents gabbros sont ainsi distingués : le gabbro à la base est riche en hornblende, d'une taille de ~5mm, sans inclusion de plagioclase mais avec des cristaux d'olivine, clinopyroxene et orthopyroxene inclus ; le gabbro supérieur est lui-aussi riche en hornblende (~5mm), avec les mêmes inclusions additionnées de plagioclase. Ces cristaux se sont formés à une température supérieure à 900°C et une profondeur correspondant à la croûte moyenne ou inférieure. Les minéraux plus fin, se trouvant hors des cristaux de hornblende des deux gabbros, sont similaires à ceux des diorites : plagioclase, biotite, hornblende, apatite, quartz et feldspath alcalin. Ces minéraux sont caractéristiques des granites. Ils ont cristallisé à ~790°C et ~2km de profondeur.La cristallisation des minéraux et leur extraction du magma par gravité provoque un changement progressif de la composition de ce dernier. Ainsi, après extraction d'olivine et d'orthopyroxene riches en Mg, de clinopyroxene riche en Ca, de plagioclase riche en Ca et Al et d'hornblende riche en Ca, Al et Mg, le liquide final sera appauvri en ces élé-ments. Un lien peut ainsi être proposé entre les diorites dont la composition est proche du liquide de départ, les granites dont la composition est similaire au liquide final, et les gabbros dont la minéralogie correspond aux minéraux extraits.L'utilisation de zircons, un minéral riche en U dont les atomes se transforment en Pb par décomposition radioactive au cours de millions d'années, permet de dater le refroidissement des roches qui les contiennent. Ainsi, il a été observé que les roches de la zone d'alimentation, à l'Ouest du complexe magmatique, ont cristallisés il y a 12.59±0.01 Ma, en même temps que les granites les plus vieux, se trouvant au sommet de la chambre magmatique, datés par Michel et al. (2008). Les deux roches pourraient donc avoir la même origine. A l'inverse, les gabbros et diorites de la chambre magmatique ont cristallisé entre 12.47±0.01Ma et 12.43±0.01Ma, les roches les plus vieilles étant à la base.En comparant la composition des roches du Torres del Paine avec celles d'autres en-tités géologiques de Patagonie, les causes du magmatisme peuvent être recherchées. A l'Ouest, on trouve en effet des intrusions granitiques, plus anciennes, caractéristiques de zones de convergence de plaque tectonique, alors qu'à l'Est, des laves basaltiques plus jeunes sont caractéristiques d'une dynamique d'extension. Sur la base des compositions chimiques des roches de ces différentes entités, l'évolution progressive de l'une à l'autre a pu être démontrée. Elle est certainement due à l'arrivée d'une dorsale océanique (zone d'extension crustale et de création de croûte océanique par la remontée de magma) dans la zone de subduction, le long des Andes.Je propose que, dans un premier temps, des magmas granitiques sont remontés dans la chambre magmatique, laissant d'importants volumes de cristaux dans la croûte pro-fonde. Dans un second épisode, les cristaux formés en profondeur ont été transportés à travers la croûte continentale, suite au mélange avec un nouveau magma injecté. Ces magmas chargés de cristaux ont traversé la zone d'alimentation avant de s'injecter dans la chambre magmatique. Différents puises ont été distingués, injectés dans la chambre magmatique du sommet à la base concernant les granites, puis à la base du granite le plus jeune pour les gabbros et diorites. Le complexe magmatique du Torres del Paine s'est construit sur une période totale de 160'000±20'000 ans.

Biología de la anchoveta peruana, Engraulis ringens Jenyns

La anchoveta es la especie clave de la cadena alimentaria del sistema de afloramiento del mar peruano, que se caracteriza por sus altos niveles de productividad no superados por ningún otro ecosistema marino. Se analizaron los principales aspectos biológicos de la anchoveta en periodos de abundancia del recurso, y cuando disminuyeron los niveles poblacionales de esta especie. La recuperación de la población de la anchoveta es rápida después de los eventos cálidos debido a que la población responde a la normalización de las condiciones ambientales, disminuyendo también su mortalidad

Hazardous substances in frequently used professional cleaning products.

A growing number of studies have identified cleaners as a group at risk for adverse health effects of the skin and the respiratory tract. Chemical substances present in cleaning products could be responsible for these effects. Currently, only limited information is available about irritant and health hazardous chemical substances found in cleaning products. We hypothesized that chemical substances present in cleaning products are known health hazardous substances that might be involved in adverse health effects of the skin and the respiratory tract. We performed a systematic review of cleaning products used in the Swiss cleaning sector. We surveyed Swiss professional cleaning companies (n = 1476) to identify the most used products (n = 105) for inclusion. Safety data sheets (SDSs) were reviewed and hazardous substances present in cleaning products were tabulated with current European and global harmonized system hazard labels. Professional cleaning products are mixtures of substances (arithmetic mean 3.5 +/- 2.8), and more than 132 different chemical substances were identified in 105 products. The main groups of chemicals were fragrances, glycol ethers, surfactants, solvents; and to a lesser extent, phosphates, salts, detergents, pH-stabilizers, acids, and bases. Up to 75% of products contained irritant (Xi), 64% harmful (Xn) and 28% corrosive (C) labeled substances. Hazards for eyes (59%) and skin (50%), and hazards by ingestion (60%) were the most reported. Cleaning products potentially give rise to simultaneous exposures to different chemical substances. As professional cleaners represent a large workforce, and cleaning products are widely used, it is a major public health issue to better understand these exposures. The list of substances provided in this study contains important information for future occupational exposure assessment studies.

Propane Regulatory Assistance Guilty,

This fact sheets summarizes, in brief form, the compliance requirements for transportation, storage, handling and use of propane. It is not intended to provide comprehensive guidance on regulatory compliance for those dealing with propane, but to highlight those requirements and to assist those who may be affected by the various requirements to obtain detailed information when needed. Information about requirements which apply to the use of propane as a motor fuel is not included.