929 resultados para Pliny, the Younger.


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Objective: This study aimed to investigate associations between violence and younger women's reproductive events using Survey 1 (1996) data of the Younger cohort of the Australian Longitudinal Study of Women's Health (ALSWH). Methods: Multinomial regression, using composite variables for both violence and reproductive events, adjusting for socioeconomic variables and weighted for rural and remote areas. Results: 23.8% of 14,784 women aged 18 to 23 years reported violence; 12.6% reported non-partner violence in the previous year; and 11.2% reported ever having had a violent relationship with a partner. Of the latter group, 43% (4.8% overall) also reported violence in the past year. Compared with women reporting no violence, women reporting partner but not recent violence (OR 2.55, 95% Cl 2.10-3.09) or partner and recent violence (OR 3.96, 95% Cl 3.18-4.93) were significantly more likely to have had one or more pregnancies. Conversely, having had a pregnancy (2,561) was associated with an 80% increase in prevalence of any violence and a 230% increase in partner violence. Among women who had a pregnancy, having had a miscarriage or termination was associated with violence. Partner and recent violence is strongly associated with having had a miscarriage, whether alone (OR = 2.85, 95% Cl 1.74-4.66), with a termination (OR = 4.60, 2.26-9.35), or with birth, miscarriage and a termination (OR 4.12, 1.89-9.00). Conclusions and implications: Violence among young women of childbearing age is a factor for which doctors should be vigilant, well-trained and supported to identify and manage effectively.

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Coal is widely used in PR China. Unfortunately, coal from some areas in Guizhou Province contains elevated levels of arsenic. This has caused arsenicosis in individuals who use arsenic-contaminated coal for the purposes of heating, cooking and drying of food in poorly ventilated dwellings. The population at risk has been estimated to be approximately 200,000 people. Clinical symptoms of arsenicosis may include changes of skin pigmentation, hyperkeratosis of hand and feet, skin cancers, liver damage, persistent cough and chronic bronchitis. We analyzed the porphyrin excretion profile using a HPLC method in urine samples collected from 113 villagers who lived in Xing Ren district, a coal-bome arsenicosis endemic area and from 30 villagers from Xing Yi where arsenicosis is not prevalent. Urinary porphyrins were higher in the arsenic exposed group than those in the control group. The correlation between urinary arsenic and porphyrin concentrations demonstrated the effect of arsenic on heme biosynthesis resulting in increased porphyrin excretion. Both uroporphyrin and coproporphyrin III showed significant increases in the excretion profile of the younger age (< 20 years) arsenic-exposed group, suggesting that porphyrins could be used as early warning biomarkers of chronic arsenic exposure in humans. Greater increases of urinary arsenic and porphyrins in women, children and older age groups who spend much of their time indoors suggest that they might be at a higher risk. Whether elevated porphyrins could predict adverse health effects associated with both cancer and non-cancer end-points in chronically arsenic-exposed populations need further investigation. (c) 2005 Elsevier Inc. All rights reserved.

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We recorded reflexive OKN in ten younger (32.3±5.98 years) and older (65.6±6.53) visually normal subjects under viewing conditions designed to differentiate M-pathway functioning from other pathways. Subjects were required to gaze straight ahead while viewing vertical gratings of either 0.43 or 1.08 cpd, drifting at either 5 or 20°/sec and presented at either 8 or 80% contrast. Gratings were presented as full field stimulation, central stimulation or peripheral (>15°) stimulation. The order of presentation of conditions was pseudo-randomised at two blocked light levels: ‘mesopic’ or twilight conditions (1.8 cdm-2) and ‘photopic’ or full light conditions (71.5 cdm-2). For the partial fields, central stimulation, mesopic light level, lower temporal frequencies (i.e. number of stripes passing per second) each contributed to greater OKN strength as measured by slow-phase velocity (SPV). For full field stimulation, and especially for higher temporal frequencies and low contrast, there was a significant interaction between age group × light level (p = 0.017): SPV diminished much more among the older than the younger group for the twilight condition compared to full light. Such a clear diminution in M-pathway sensitivity revealed by OKN response has important implications for everyday situations like crash avoidance under twilight driving conditions.

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Este presente trabalho, tem por objetivo analisar o conflito geracional e a formação da identidade dos jovens adventistas, com o objetivo de verificar se o conflito geracional é uma demonstração que os jovens estão rompendo com a igreja ou, reconstruindo a identidade. O conflito geracional pode ser notado em diversas esferas da sociedade e inclusive dentro da Igreja Adventista. Todavia, o conflito geracional não é causado por rebeldia, mas sim, por diferentes maneiras de reagir e conviver com as características contemporâneas da sociedade. Sendo assim, os mais velhos não concordam com as novas propostas dos jovens e tão pouco, os mais novos desejam continuar convivendo com as coisas antigas. A Igreja Adventista tem vivido o conflito geracional em dois aspectos principais: o primeiro se evidencia na comunicação; o segundo na cosmovisão. A linguagem sofreu alterações na hora de se comunicar; no contexto atual, a imagem tomou a função das palavras. Por essa razão, uma comunicação pode não alcançar seu objetivo, principalmente aos mais novos, quando expressa somente através de palavras. O outro aspecto que tem causado conflito é a compreensão de mundo que os mais novos possuem. Para eles, o mundo não é sinônimo de pecado como algumas pessoas mais velhas entendem. Por conta desta diferença, certas questões não são aceitáveis dentro da igreja, por serem vinculadas ao mundo e o mundo ser entendido como pecado. Porém, a constatação que faço é que, embora o jovem não entenda o mundo em si como pecado, ele compreende que existem aspectos do mundo que sejam errados. Esses aspectos não são aceitáveis para eles e por isso, eles não desejam romper com a igreja. Mas estão em busca de mudanças significativas que se encaixam com sua visão de mundo. É possível evidenciar essa mesma linha de raciocínio em alguns líderes da igreja, mas os relatos dos jovens expressam que isso não alcançou a prática local. Uma vez que, concebo o pensamento de Hervieu-Leger de que a identidade não é transmitida intacta de pai para filho, mas construída individualmente. Entendo que os jovens estão formando sua própria identidade. Para que essa identidade seja formada de maneira sólida nos princípios adventistas, e aberta as mudanças necessárias da sociedade, se faz necessário, sob minha percepção, uma releitura de Ellen White baseada no pensamento liminar de Walter Mignolo, apresentado e explanado por Adolfo S. Suárez.

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Este trabalho teve como objetivo principal investigar o sentimento de solidão e a saúde mental de mulheres casadas, procurando comparar a maneira de compreender e vivenciar este sentimento em mulheres solteiras e casadas, bem como verificar em que medida este sentimento pode ser mitigado pela presença do outro no casamento (coabitação) e em que condições isto ocorria. Partiu-se da hipótese de que esse sentimento é compartilhado por todas as pessoas, já que o ser humano é uno e individual. Logo, a separação eterna do outro, que se inicia quando o bebê percebe que é diferente da mãe e, assim, um indivíduo único, está associado a uma sensação de solidão que acompanha o ser humano por toda a vida. Desta forma, é muito comum ver pessoas se envolver em relacionamentos para diminuir este sentimento, que se vê intensificado a cada dia em função da superficialidade dos vínculos emocionais. A presença de outrem pode ser aproveitada numa relação interpessoal quando se diminui a intensidade da hostilidade, associada ao sentimento de solidão. O antídoto contra tal sentimento vem do fortalecimento do auto-conhecimento, da autonomia, e da amizade por um companheiro que mostra aceitação incondicional pelo verdadeiro self. Para análise deste sentimento em mulheres casadas, foi realizada uma pesquisa quantitativa e qualitativa com mulheres solteiras e universitárias. A escolha da amostra foi aleatória e por conglomerado, em três estágios. Participaram do estudo 184 mulheres, 38% casadas, 7,6% separadas e 52,7% solteiras. Da pesquisa quantitativa foi possível analisar que a percepção das mulheres sobre a solidão vem, em muitos aspectos, de encontro com a teoria psicanalítica. Pelas respostas encontradas percebeu-se que a grande maioria das participantes tem um baixo sentimento de solidão (58,7%) e 41,3% se classificaram com um escore de alto a médio sentimento de solidão, nestes dois grupos a maioria são de mulheres casadas e separadas, sendo que quanto mais nova a mulher maior a tendência a buscar um relacionamento para fugir da solidão, sendo entre as casadas também que isto ocorre com mais freqüência. A partir destes escores, 18 mulheres foram convidadas a participar de uma entrevista diagnóstica. Destas dezoito, seis mulheres apresentavam alto sentimento de solidão, sendo duas casadas, duas solteiras e duas separadas. Da mesma forma as mulheres com média e baixa solidão. Os resultados encontrados nestas entrevistas foram que todas as mulheres que apresentaram um alto sentimento de solidão demonstram uma adaptação ineficaz perante a vida, enquanto que aquelas que apresentaram médio ou baixo sentimento de solidão dificilmente apresentam adaptação ineficaz. Do grupo de médio sentimento de solidão, três mulheres apresentaram adaptação eficaz, e do grupo de baixo sentimento de solidão apenas uma participante apresentou adaptação ineficaz leve. Com isso concluímos que a solidão, quando em alta medida, além de dolorosa indica uma grande dificuldade do indivíduo em lidar com seus aspectos emocionais e produtivos, necessitando de ajuda psíquica.

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Este trabalho teve como objetivo principal investigar o sentimento de solidão e a saúde mental de mulheres casadas, procurando comparar a maneira de compreender e vivenciar este sentimento em mulheres solteiras e casadas, bem como verificar em que medida este sentimento pode ser mitigado pela presença do outro no casamento (coabitação) e em que condições isto ocorria. Partiu-se da hipótese de que esse sentimento é compartilhado por todas as pessoas, já que o ser humano é uno e individual. Logo, a separação eterna do outro, que se inicia quando o bebê percebe que é diferente da mãe e, assim, um indivíduo único, está associado a uma sensação de solidão que acompanha o ser humano por toda a vida. Desta forma, é muito comum ver pessoas se envolver em relacionamentos para diminuir este sentimento, que se vê intensificado a cada dia em função da superficialidade dos vínculos emocionais. A presença de outrem pode ser aproveitada numa relação interpessoal quando se diminui a intensidade da hostilidade, associada ao sentimento de solidão. O antídoto contra tal sentimento vem do fortalecimento do auto-conhecimento, da autonomia, e da amizade por um companheiro que mostra aceitação incondicional pelo verdadeiro self. Para análise deste sentimento em mulheres casadas, foi realizada uma pesquisa quantitativa e qualitativa com mulheres solteiras e universitárias. A escolha da amostra foi aleatória e por conglomerado, em três estágios. Participaram do estudo 184 mulheres, 38% casadas, 7,6% separadas e 52,7% solteiras. Da pesquisa quantitativa foi possível analisar que a percepção das mulheres sobre a solidão vem, em muitos aspectos, de encontro com a teoria psicanalítica. Pelas respostas encontradas percebeu-se que a grande maioria das participantes tem um baixo sentimento de solidão (58,7%) e 41,3% se classificaram com um escore de alto a médio sentimento de solidão, nestes dois grupos a maioria são de mulheres casadas e separadas, sendo que quanto mais nova a mulher maior a tendência a buscar um relacionamento para fugir da solidão, sendo entre as casadas também que isto ocorre com mais freqüência. A partir destes escores, 18 mulheres foram convidadas a participar de uma entrevista diagnóstica. Destas dezoito, seis mulheres apresentavam alto sentimento de solidão, sendo duas casadas, duas solteiras e duas separadas. Da mesma forma as mulheres com média e baixa solidão. Os resultados encontrados nestas entrevistas foram que todas as mulheres que apresentaram um alto sentimento de solidão demonstram uma adaptação ineficaz perante a vida, enquanto que aquelas que apresentaram médio ou baixo sentimento de solidão dificilmente apresentam adaptação ineficaz. Do grupo de médio sentimento de solidão, três mulheres apresentaram adaptação eficaz, e do grupo de baixo sentimento de solidão apenas uma participante apresentou adaptação ineficaz leve. Com isso concluímos que a solidão, quando em alta medida, além de dolorosa indica uma grande dificuldade do indivíduo em lidar com seus aspectos emocionais e produtivos, necessitando de ajuda psíquica.

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Low German is a West-germanic language, which is used mainly as a spoken language in the coastal areas of Northwest Germany, North-eastern parts of the Netherlands and along the German coasts of the Baltic Sea. Although still a variety used by millions of speakers, Low German must be counted among the languages threatened by decline if not extinction within the next twenty years because it is no longer used by the younger generations. Apart from the question of whether Low German will survive altogether, the variety is in a process of linguistic change due to the contact situation with the dominant language of the media and almost all written official communications, Standard German. Low German, therefore, is a field for research in all areas of language contact, e.g. codeswitching, language shift, mixed languages or language death. Within Low German, the variety spoken in East Frisia has a distinct history of language contact and language change over the last six hundred years. It is based on a Frisian substratum and has been in close linguistic contact with Dutch since the 16th century.

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Last year (2009) marked the bicentenary of Charles Darwin's birth and the sesquicentenary of The Origin of Species. This article examines the influence of Erasmus Darwin on Charles's evolutionary thought and shows how, in many ways, Erasmus anticipated his much better-known grandson. It discusses the similarity in the mindsets of the two Darwins, asks how far the younger Darwin was exposed to the elder's evolutionary thought, examines the similarities and differences in their theories of evolution, and ends by showing the surprising similarity between their theories of inheritance. Erasmus's influence on Charles is greater than customarily acknowledged, and now is an opportune time to bring the grandfather out from behind the glare of his stellar grandson.

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Neurons in the developing brain die via apoptosis after DNA damage, while neurons in the adult brain are generally resistant to these insults. The basis for this resistance is a matter of conjecture. We report here that cerebellar granule neurons (CGNs) in culture lose their competence to die in response to DNA damage as a function of time in culture. CGNs at either 1 day in vitro (DIV) or 7 DIV were treated with the DNA damaging agents camptothecin, UV or gamma-irradiation and neuronal survival measured. The younger neurons were effectively killed by these agents, while the older neurons displayed a significant resistance to killing. Neuronal survival did not change with time in culture when cells were treated with C2-ceramide or staurosporine, agents which do not target DNA. The resistance to UV irradiation developed over time in culture and was not due to changes in mitotic rate. Increases in DNA strand breakage, up-regulation of the levels of both p53 and its phosphorylated form and nuclear translocation of p53 were equivalent in both older and younger neurons, indicating a comparable p53 stress response. In addition, we show that treatment of older neurons with pharmacological inhibitors of distinct components of the DNA repair machinery promotes the accumulation of DNA damage and sensitizes these cells to the toxic effects of UV exposure. These data demonstrate that older neurons appear to be more proficient in DNA repair in comparison to their younger counterparts, and that this leads to increased survival after DNA damage.

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The Priestlaw and Cockburn Law intrusions are zoned granitoid plutons intruded into Lower Palaeozoic sediments at the margin of, and prior to closure of, the Iapetus Ocean. They vary from marginal basic rocks to more acid rocks towards their centres. The parental magmas to the plutons were derived from an isotopically depleted mantle modified by melts/fluids during subduction. Zonation in the plutons was caused by combined assimilation and fractional crystallisation (AFC), and rates of assimilation were low relative to rates of fractionation. A series of pyroxene-mica diorites in Priestlaw are however hybrids formed by simple mixing. Porphyrite-acid porphyrite dykes, associated with the plutons, represent chilled portions of the pluton magmas; more evolved quartz porphyry dykes represent crustal melts. Lamprophyre dykes have high LILE and LREE abundances and relative depletions of HFS elements, typical of subduction related ultra-potassic magmas. High Mg numbers, Ni and Cr contents and experimental constraints, imply near primary status for the least evolved lamprophyres. Their enrichments in incompatible elements, high La/Nb, La/Yb, Sr and low Nd indicate derivation from a previously metasomatised mantle source. Granitoid plutons and lavas in the northern Southern Uplands have high Nd and low Sr, whereas the younger plutons of the southern Southern Uplands have higher Sr, La/Yb and lower Nd, consistent with derivation from a more enriched source. No plutons however have remained as closed systems. Three magmatic suites are present in southern Scotland: (1) Midland Valley Suite (2) Northern Southern Uplands Suite and (3) Southern Southern Uplands Suite, consistent with previous models indicating northward underthrusting of English lithosphere below the southern Southern Uplands. Further underthrusting of decoupled lithospheric mantle is indicated by the presence of lamorophyres in the eastern Southern Uplands, and took place between 410 Ma and 400 Ma.

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Aims: To compare all-cause mortality in older people with or without diabetes and consider the associated risk of comorbidity and polypharmacy. Methods: A 10-year cohort study using data from the Health Innovation Network database (2003-2013) comparing mortality in people aged ≥ 70 years with diabetes (DM cohort) (n = 35 717) and without diabetes (No DM cohort) (n = 307 918). Results: The mean age of the DM cohort was 78.1 ± 5.8 years vs. 79.0 ± 6.3 years in the No DM cohort. Mean diabetes duration was 8.2 ± 8.1 years, and 30% had diabetes for > 10 years. The DM cohort had a greater comorbidity load and people in this cohort were prescribed more therapies than the No DM cohort. The 5- and 10-year survival rates were lower in the DM cohort at 64% and 39%, respectively, compared with 72% and 50% in the No DM cohort. The excess mortality in the DM cohort was greatest in those aged <75 years with longer duration diabetes, the relative hazard for mortality was higher in females. Although comorbidity and polypharmacy were associated with increased mortality risk in the DM cohort, this risk was lower compared with the No DM cohort. The hazard ratios (95% confidence interval) for comorbidities > 4 and medicines ≥ 7 were 1.29 (1.19 to 1.41) and 1.34 (1.25 to 1.43) in the DM cohort and 1.63 (1.57 to 1.70) and 1.48 (1.40 to 1.56) in the No DM cohort, respectively. Conclusions: There is significant excess mortality in older people with diabetes, which is unexplained by comorbidity or polypharmacy. This excess is greatest in the younger old with longer disease duration, suggesting that it may be related to the effect of diabetes exposure.

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Continental margin sediments off Nova Scotia accumulate at high rates (up to 360 cm/kyr) and contain a history of millennial-scale environmental changes which are dominated by the proximity of the Laurentide ice sheet during the latest Quaternary. Using stable isotope ratios of oxygen, accelerator mass spectrometer radiocarbon dating, micropaleontology, and sedimentology, we document these changes in six piston cores ranging in water depth from ab. 450 to ab. 4300 m. We find that maximum d18O in N. pachyderma occurred about 15 ka and preceded the maximum abundance of this species in these cores by ab. 1000 years. Between 13 and 14 ka we find a second peak in abundance of N. pachyderma, minimum d18O, and two pulses of ice rafting. The sediment lithology supports terrestrial studies which indicate that there was a general withdrawal of ice beyond the upper Paleozoic and Mesozoic red beds by 14 ka in southeastern Canada, so the ice rafting events between 13 and 14 ka probably reflect ice stream activity in the St. Lawrence valley. The Younger Dryas event is recognized as a peak in abundance of N. pachyderma and ice rafting (dated as ab. 11.3 ka), but meltwater discharge to the Gulf of St. Lawrence was either too small or occurred over too long a time to leave a distinct d18O minimum off Nova Scotia. At 7.1 ka, in the middle of Holocene warming, we find a third peak in abundance of N. pachyderma and another d18O minimum but no ice rafting. We interpret these data as evidence of a late-occurring meltwater event which, if correct, could have originated in the Great Lakes, in the Labrador-Ungava region, or in both. The final millennial-scale phenomenon off Nova Scotia is the onset of "Neoglaciation," marked by increased ice rafting and increased % N. pachyderma beginning about 5 kyr ago.

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The Laurentide Ice Sheet (LIS) was a large, dynamic ice sheet in the early Holocene. The glacial events through Hudson Strait leading to its eventual demise are recorded in the well-dated Labrador shelf core, MD99-2236 from the Cartwright Saddle. We develop a detailed history of the timing of ice-sheet discharge events from the Hudson Strait outlet of the LIS during the Holocene using high-resolution detrital carbonate, ice rafted detritus (IRD), d18O, and sediment color data. Eight detrital carbonate peaks (DCPs) associated with IRD peaks and light oxygen isotope events punctuate the MD99-2236 record between 11.5 and 8.0 ka. We use the stratigraphy of the DCPs developed from MD99-2236 to select the appropriate DeltaR to calibrate the ages of recorded glacial events in Hudson Bay and Hudson Strait such that they match the DCPs in MD99-2236. We associate the eight DCPs with H0, Gold Cove advance, Noble Inlet advance, initial retreat of the Hudson Strait ice stream (HSIS) from Hudson Strait, opening of the Tyrrell Sea, and drainage of glacial lakes Agassiz and Ojibway. The opening of Foxe Channel and retreat of glacial ice from Foxe Basin are represented by a shoulder in the carbonate data. DeltaR of 350 years applied to the radiocarbon ages constraining glacial events H0 through the opening of the Tyrell Sea provided the best match with the MD99-2236 DCPs; DeltaR values and ages from the literature are used for the younger events. A very close age match was achieved between the 8.2 ka cold event in the Greenland ice cores, DCP7 (8.15 ka BP), and the drainage of glacial lakes Agassiz and Ojibway. Our stratigraphic comparison between the DCPs in MD99-2236 and the calibrated ages of Hudson Strait/Bay deglacial events shows that the retreat of the HSIS, the opening of the Tyrell Sea, and the catastrophic drainage of glacial lakes Agassiz and Ojibway at 8.2 ka are separate events that have been combined in previous estimates of the timing of the 8.2 ka event from marine records. SW Iceland shelf core MD99-2256 documents freshwater entrainment into the subpolar gyre from the Hudson Strait outlet via the Labrador, North Atlantic, and Irminger currents. The timing of freshwater release from the LIS Hudson Strait outlet in MD99-2236 matches evidence for freshwater forcing and LIS icebergs carrying foreign minerals to the SW Iceland shelf between 11.5 and 8.2 ka. The congruency of these records supports the conclusion of the entrainment of freshwater from the retreat of the LIS through Hudson Strait into the subpolar gyre and provides specific time periods when pulses of LIS freshwater were present to influence climate.