949 resultados para obesity I and II


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Large amounts of organic carbon are stored in Arctic permafrost environments, and microbial activity can potentially mineralize this carbon into methane, a potent greenhouse gas. In this study, we assessed the methane budget, the bacterial methane oxidation (MOX) and the underlying environmental controls of arctic lake systems, which represent substantial sources of methane. Five lake systems located on Samoylov Island (Lena Delta, Siberia) and the connected river sites were analyzed using radiotracers to estimate the MOX rates, and molecular biology methods to characterize the abundance and the community composition of methane-oxidizing bacteria (MOB). In contrast to the river, the lake systems had high variation in the methane concentrations, the abundance and composition of the MOB communities, and consequently, the MOX rates. The highest methane concentrations and the highest MOX rates were detected in the lake outlets and in a lake complex in a floodplain area. Though, in all aquatic systems we detected both, Type I and II MOB, in lake systems we observed a higher diversity including MOB, typical of the soil environments. The inoculation of soil MOB into the aquatic systems, resulting from permafrost thawing, might be an additional factor controlling the MOB community composition and potentially methanotrophic capacity.

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Upwelling intensity in the South China Sea has changed over glacial-interglacial cycles in response to orbital-scale changes in the East Asian Monsoon. Here, we evaluate new multi-proxy records of two sediment cores from the north-eastern South China Sea to uncover millennial-scale changes in winter monsoondriven upwelling over glacial Terminations I and II. On the basis of U/Th-based speleothem chronology, we compare these changes with sediment records of summer monsoondriven upwelling east of South Vietnam. Ocean upwelling is traced by reduced (UK'37-based) temperature and increased nutrient and productivity estimates of sea surface water (d13C on planktic foraminifera, accumulation rates of alkenones, chlorins, and total organic carbon). Accordingly, strong winter upwelling occurred north-west of Luzon (Philippines) during late Marine Isotope Stage 6.2, Heinrich (HS) and Greenland stadials (GS) HS-11, GS-26, GS-25, HS-1, and the Younger Dryas. During these stadials, summer upwelling decreased off South Vietnam and sea surface salinity reached a maximum suggesting a drop in monsoon rains, concurrent with speleothem records of aridity in China. In harmony with a stadial-to-interstadial see-saw pattern, winter upwelling off Luzon in turn was weak during interstadials, in particular those of glacial Terminations I and II, when summer upwelling culminated east of South Vietnam. Most likely, this upwelling terminated widespread deep-water stratification, coeval with the deglacial rise in atmospheric CO2. Yet, a synchronous maximum in precipitation fostered estuarine overturning circulation in the South China Sea, in particular as long as the Borneo Strait was closed when sea level dropped below -40 m.

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Abundant and various diagenetic carbonates were recovered from a 1084-m-thick, Quaternary to lower Miocene section at ODP Site 799 in the Japan Sea. Petrographic, XRD, SEM, EDS-chemical, and isotopic analyses revealed wide variations in occurrence and textural relations and complex mineralogy and chemistry. Diagenetic carbonates include calcite, calcium-rich rhodochrosite, iron- and manganese-rich magnesite, iron- and manganese-rich dolomite and ankerite, and iron- and manganeserich lansfordite (hydrous Mg-carbonate). Rhodochrosite commonly occurs as small, solid nodules and semi-indurated, thin layers in bioturbated, mottled sediments of Units I and II (late Miocene to Quaternary). Lansfordite occurs as unindurated nodules and layers in Unit II (late Miocene and Pliocene), whereas magnesite forms indurated beds a few centimeters thick in slightly bioturbated-to-faintly laminated sediments of Unit III (middle and late Miocene). Some rhodochrosite nodules have dark-colored, pyritic cores, and some pyrite-rhodochrosite nodules are overgrown by and included within magnesite beds. Dolomite and ankerite tend to form thick beds (>10 cm) in bedded to laminated sediments of Units III, IV, and V (early to late Miocene). Calcite occurs sporadically throughout the Site 799 sediments. The d18O values of carbonates and the interstitial waters, and the measured geothermal gradient indicate that almost all of the Site 799 carbonates are not in isotopic equilibrium with the ambient waters, but were precipitated in the past when the sediments were at shallower depths. Depths of precipitation obtained from the d18O of carbonates span from 310 to 510 mbsf for magnesite and from 60 to 580 mbsf for dolomite-ankerite. Rhodochrosite and calcite are estimated to have formed within sediments at depths shallower than 80 mbsf. Diagenetic history in the Site 799 sediments have been determined primarily by the environment of deposition; in particular, by the oxidation-reduction state of the bottom waters and the alkalinity level of the interstitial waters. Under the well-oxygenated bottom-water conditions in the late Miocene and Pliocene, manganese initially accumulated on the seafloor as hydrogenous oxides and subsequently was mobilized and reprecipitated as rhodochrosite within the shallow sulfate-reduction, sub-oxic zone. Precipitation of lansfordite occurred in the near-surface sediments with abundant organic carbon and an extremely high alkalinity during the latest Miocene and Pliocene. The lansfordite was transformed to magnesite upon burial in the depth interval 310 to 510 mbsf. Dolomite first precipitated at shallow depths in Mn-poor, anoxic, moderately biocalcareous sediments of early to late Miocene. With increasing temperature and depth, the dolomite recrystallized and reequilibrated with ambient waters at depths below about 400 mbsf.

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Ocean Drilling Program Hole 990A penetrated 131 m of subaerially emplaced Paleocene flood basalts on the Southeast Greenland margin with a recovery of 74%. Shipboard P-wave velocity (Vp), density, and magnetic susceptibility were measured with 2- to 15-cm intervals on the core. Individual flow units were divided into four zones based on the observed petrophysical characteristics. From the top, these are Zone I (<7 m thick with a Vp of ~2.5 km/s), Zone II (3-5 m thick with a strongly increasing Vp from 2.5 to 5.5 km/s), Zone III (up to 20 m thick with a Vp of ~5.5-6.0 km/s), and Zone IV (<2 m thick with a strongly decreasing Vp from 6.0 to 2.5 km/s). Eighteen samples were selected from three of the fourteen penetrated basalt units for geochemical, petrological, and petrophysical studies focusing on the altered, low-velocity upper lava Zones I and II. Zone I is strongly altered to >50% clay minerals (smectite) and iron hydroxides, and the petrophysical properties are primarily determined by the clay properties. Zone II is intermediately altered with 5%-20% clay minerals, where the petrophysical properties are a function of both the degree of alteration and porosity variations. Shipboard and shore-based measurements of the same samples show that storage permanently lowers the elastic moduli of basalt from Zones I to III. This is related to the presence of even small quantities of swelling clays. The data show that alteration processes are important in determining the overall seismic properties of flood basalt constructions. The degree and depth of alteration is dependent on the primary lava flow emplacement structures and environment. Thus, the interplay of primary emplacement and secondary alteration structures determine the elastic properties of basalt piles. Rock property theories for sand-clay systems are further used to model the physical property variations in these altered crystalline rocks.

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Abstract: BRIGUICHE. H, ZIDANE. L. Floristic And Ethnobotanical Studies Of Medicinal Plants Of The City Of El -Jadida (MOROCCO). In the framework of the ethnobotanical studies on medicinal plants undertaken by the Laboratory of Biodiversity and Natural Resources of the Faculty of Sciences of Kenitra (Morocco), we are interested in the area of El Jadida which presents a rather important floristic richness thanks to changes in its ecological conditions By using 204 questionnaire, the ethnobotanical surveys were conducted in the field during the years 2012-2013. The location of the different sampling sites was determined by the stratified sampling method. The analysis of the results obtained from the questionnaires and forms using statistical processing allowed us to identify 70 plant species distributed in 69 genera and 37 families. These results also show that most of these species are mainly used in the care of the digestive system and respiratory system. The seed is the most used part in local traditional medicines and the decoction is the most frequent mode with a rate of 31%. The species Origanum compactum is the most used by the population of the city of El Jadida 47 quotes.  

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AIMS: Our aims were to evaluate the distribution of troponin I concentrations in population cohorts across Europe, to characterize the association with cardiovascular outcomes, to determine the predictive value beyond the variables used in the ESC SCORE, to test a potentially clinically relevant cut-off value, and to evaluate the improved eligibility for statin therapy based on elevated troponin I concentrations retrospectively.

METHODS AND RESULTS: Based on the Biomarkers for Cardiovascular Risk Assessment in Europe (BiomarCaRE) project, we analysed individual level data from 10 prospective population-based studies including 74 738 participants. We investigated the value of adding troponin I levels to conventional risk factors for prediction of cardiovascular disease by calculating measures of discrimination (C-index) and net reclassification improvement (NRI). We further tested the clinical implication of statin therapy based on troponin concentration in 12 956 individuals free of cardiovascular disease in the JUPITER study. Troponin I remained an independent predictor with a hazard ratio of 1.37 for cardiovascular mortality, 1.23 for cardiovascular disease, and 1.24 for total mortality. The addition of troponin I information to a prognostic model for cardiovascular death constructed of ESC SCORE variables increased the C-index discrimination measure by 0.007 and yielded an NRI of 0.048, whereas the addition to prognostic models for cardiovascular disease and total mortality led to lesser C-index discrimination and NRI increment. In individuals above 6 ng/L of troponin I, a concentration near the upper quintile in BiomarCaRE (5.9 ng/L) and JUPITER (5.8 ng/L), rosuvastatin therapy resulted in higher absolute risk reduction compared with individuals <6 ng/L of troponin I, whereas the relative risk reduction was similar.

CONCLUSION: In individuals free of cardiovascular disease, the addition of troponin I to variables of established risk score improves prediction of cardiovascular death and cardiovascular disease.

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LEÃO, Adriano de Castro; DÓRIA NETO, Adrião Duarte; SOUSA, Maria Bernardete Cordeiro de. New developmental stages for common marmosets (Callithrix jacchus) using mass and age variables obtained by K-means algorithm and self-organizing maps (SOM). Computers in Biology and Medicine, v. 39, p. 853-859, 2009

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A report developed for the Department of Health by the institute of Public Health in Ireland. This report presents a summary of the feedback of key stakeholders based on a consultation document presenting options for action to address Ireland’s overweight and obesity epidemic. There was a very significant level of engagement by a wide range of stakeholders which has resulted in a useful set of considerations for policy development. The findings from this consultation strand along with those from the other two strands of consultation will be studied to inform and enrich the forthcoming Obesity Policy and Action Plan.

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O conteúdo de ciências no Ensino Fundamental dos ciclos I e II é ministrado por um professor polivalente com formação em Pedagogia. Sua formação deve possibilitar uma visão global do fenômeno educativo, o que implica a construção de conhecimentos múltiplos e contextualizados, porém com pouco aprofundamento. Este trabalho objetiva identificar as opiniões e dificuldades de licenciandos de Pedagogia a respeito dos conteúdos de Ciências nos dois primeiros ciclos do Ensino Fundamental, mediado por dois questionamentos: Com relação aos conteúdos de ciências ministrados no I e II ciclos, você os considera fácil ou difícil? Sendo solicitado que justificasse sua resposta; De acordo com seus conhecimentos sobre ciências, cite as principais dificuldades que você teria (tem/teve) em ensinar ciências nos ciclos I e II. Participaram do estudo 29 licenciandas da turma de Ensino das Ciências Naturais II do Curso de Pedagogia da Universidade Federal do Rio Grande do Norte. Com relação ao questionamento referente à consideração dos conteúdos de ciências, 52% das licenciandas consideraram fácil, 31% difícil e 17% não responderam a questão. Foram identificadas três categorias de respostas: processo de elaboração do planejamento (20,5% fácil e 20,5% difícil), nível de conhecimento dos alunos (7% fácil e 0% difícil) e natureza dos conteúdos abordados (14% fácil e 10,5% difícil). Foram classificadas três categorias distintas em relação às dificuldades em ensinar ciências: natureza dos conteúdos abordados (50%), aspectos metodológicos (25%), e conhecimento básico (25%). A análise dos resultados revelou que a principal dificuldade das licenciandas em Pedagogia quanto à aplicabilidade do ensino de ciências nos primeiros ciclos do Ensino Fundamental esta diretamente relacionada à falta de conhecimento básico destes conteúdos, que somente foram estudados por elas no Ensino Básico, indicando a necessidade de incorporação de abordagens de conteúdos de ciências no currículo do curso de Pedagogia.

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Tutorial en el que se explica cómo matricularse en el curso Adquisición de habilidades en información. Niveles I y II.

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LEÃO, Adriano de Castro; DÓRIA NETO, Adrião Duarte; SOUSA, Maria Bernardete Cordeiro de. New developmental stages for common marmosets (Callithrix jacchus) using mass and age variables obtained by K-means algorithm and self-organizing maps (SOM). Computers in Biology and Medicine, v. 39, p. 853-859, 2009

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Soil-dwelling Streptomyces bacteria are known for their ability to produce biologically active compounds such as antimicrobial, immunosuppressant, antifungal and anticancer drugs. S. nogalater is the producer of nogalamycin, a potential anticancer drug exhibiting high cytotoxicity and activity against human topoisomerases I and II. Nogalamycin is an anthracycline polyketide comprising a four-ring aromatic backbone,a neutral deoxy sugar at C7, and an amino sugar attached via an O–C bond at C1 and a C–C bond between C2 and C5´´. This kind of attachment of the amino sugar is unusual thus making the structure of the compound highly interesting. The sugar is also associated with the biological activity of nogalamycin, as it facilitates binding to DNA. Furthermore, the sugar moieties of anthracyclines are often crucial for their biological activity. Together the interesting attachment of the amino sugar and the general reliance of polyketides on the sugar moieties for bioactivity have made the study of the biosynthesis of nogalamycin attractive. The sugar moieties are typically attached by glycosyltransferases, which use two substrates: the donor and the acceptor. The literature review of the thesis is focused on the glycosylation of polyketides and the possibilities to alter their glycosylation patterns. My own thesis work revolves around the biosynthesis of nogalamycin. We have elucidated the individual steps that lead to its rather unique structure. We reconstructed the whole biosynthetic pathway in the heterologous host S. albus using a cosmid and a plasmid. In the process, we were able to isolate new compounds when the cosmid, which contains the majority of the nogalamycin gene cluster, was expressed alone in the heterologous host. The new compounds included true intermediates of the pathway as well as metabolites, which were most likely altered by the endogenous enzymes of the host. The biological activity of the most interesting new products was tested against human topoisomerases I and II, and they were found to exhibit such activities. The heterologous expression system facilitated the generation of mutants with inactivated biosynthetic genes. In that process, we were able to identify the functions of the glycosyltransferases SnogE and SnogD, solve the structure of SnogD, discover a novel C1-hydroxylase system comprising SnoaW and SnoaL2, and establish that the two homologous non-heme α-ketoglutarate and Fe2+ dependent enzymes SnoK and SnoN catalyze atypical reactions on the pathway. We demonstrated that SnoK was responsible for the formation of the additional C–C bond, whereas SnoN is an epimerase. A combination of in vivo and in vitro techniques was utilized to unravel the details of these enzymes. Protein crystallography gave us an important means to understand the mechanisms. Furthermore, the solved structures serve as platforms for future rational design of the enzymes.

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Objetivo: Relatar a experiência das atividades de educação alimentar e nutricional (EAN) desenvolvidas em pacientes com sobrepeso e obesidade. Síntese de dados: Realizaramse sessões de educação alimentar e nutricional (EAN) com pacientes com sobrepeso e obesidade graus I e II atendidos no ambulatório do Hospital Universitário da Universidade Federal de Juiz de Fora (HU/UFJF), integrantes do projeto de extensão “Saúde na Balança”. As sessões ocorreram em grupo, semanalmente no 1º mês, quinzenalmente no 2º e 3º mês e mensalmente até o 6º mês, no período de setembro de 2012 a setembro de 2013. Durante um ano de atividades, foram realizados 4 grupos, com um total de 46 integrantes, que aceitaram participar das sessões. Nestas, foram abordados temas em nutrição que apoiavam o atendimento individual. A equipe identificou que local, horário, periodicidade das sessões, disponibilidade de tempo e falta de recursos financeiros eram fatores que influenciavam a adesão do paciente ao tratamento, sendo alguns deles modificados, já se observando melhora da adesão no último grupo. Entretanto, ainda foram registradas 17 desistências. Com o autorrelato dos pacientes, foi possível perceber mudanças positivas nos hábitos alimentares e na forma de se relacionar com a obesidade e as comorbidades associadas. Conclusão: No decorrer das atividades, criou-se vínculo entre equipe e participantes, permitindo identificação de demandas e de formas efetivas de atuação nos grupos, demonstrando que a EAN auxilia a abordagem individual, na medida em que permite troca de experiências e informações, ampliando o poder de escolha por hábitos de vida saudáveis.

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O conteúdo de ciências no Ensino Fundamental dos ciclos I e II é ministrado por um professor polivalente com formação em Pedagogia. Sua formação deve possibilitar uma visão global do fenômeno educativo, o que implica a construção de conhecimentos múltiplos e contextualizados, porém com pouco aprofundamento. Este trabalho objetiva identificar as opiniões e dificuldades de licenciandos de Pedagogia a respeito dos conteúdos de Ciências nos dois primeiros ciclos do Ensino Fundamental, mediado por dois questionamentos: Com relação aos conteúdos de ciências ministrados no I e II ciclos, você os considera fácil ou difícil? Sendo solicitado que justificasse sua resposta; De acordo com seus conhecimentos sobre ciências, cite as principais dificuldades que você teria (tem/teve) em ensinar ciências nos ciclos I e II. Participaram do estudo 29 licenciandas da turma de Ensino das Ciências Naturais II do Curso de Pedagogia da Universidade Federal do Rio Grande do Norte. Com relação ao questionamento referente à consideração dos conteúdos de ciências, 52% das licenciandas consideraram fácil, 31% difícil e 17% não responderam a questão. Foram identificadas três categorias de respostas: processo de elaboração do planejamento (20,5% fácil e 20,5% difícil), nível de conhecimento dos alunos (7% fácil e 0% difícil) e natureza dos conteúdos abordados (14% fácil e 10,5% difícil). Foram classificadas três categorias distintas em relação às dificuldades em ensinar ciências: natureza dos conteúdos abordados (50%), aspectos metodológicos (25%), e conhecimento básico (25%). A análise dos resultados revelou que a principal dificuldade das licenciandas em Pedagogia quanto à aplicabilidade do ensino de ciências nos primeiros ciclos do Ensino Fundamental esta diretamente relacionada à falta de conhecimento básico destes conteúdos, que somente foram estudados por elas no Ensino Básico, indicando a necessidade de incorporação de abordagens de conteúdos de ciências no currículo do curso de Pedagogia.

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Dissertação de Mestrado apresentada no Instituto Superior de Psicologia Aplicada para obtenção do grau de Mestre na especialidade de Psicologia Clínica