993 resultados para Nostradamus, 1503-1566.
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Objetivo: La equidad de género es un determinante estructural de las desigualdades en salud. Por ello, se pretende visibilizar su evolución en las comunidades autónomas (CC.AA.) desde 2006, previamente a la promulgación de la Ley de Igualdad (2007) y la crisis económica (2008), hasta 2014. Método: Estudio ecológico sobre la equidad de género en las 17 CC.AA. en 2006-2011-2014. Cálculo de: 1) índice de equidad de género modificado (IEGM) de las CC.AA. (0 = equidad, ±1 = inequidad); 2) convergencia interregional y temporal en equidad de género. Resultados: El IEGM de las CC.AA.2014 toma valores negativos próximos a 0 (inequidad desfavorable a las mujeres). No hay convergencia interregional en la equidad de género, pues aumenta la dispersión (2006: 0,1503; 2011: 0,2280; 2014: 0,4964). Tampoco existe convergencia temporal, al no evolucionar mejor las CC.AA. menos equitativas. La brecha de género en actividad económica sigue desfavorable a las mujeres. En 2006-2011 disminuye en todas las CC.AA., y en 2014 aumenta en seis CCAA. La brecha de género en educación tiene valores positivos próximos a 0 (desfavorable a los hombres) en 2006-2011-2014, y en empoderamiento es desfavorable a las mujeres, siendo la dimensión que más pesa en la equidad de género. Se mantiene la dispersión entre CC.AA. en 2006-2014 en actividad económica y educación, y aumenta en empoderamiento. Conclusiones: El contexto de equidad de género alcanzado en las CC.AA. españolas en 2006 se ha perdido durante la crisis económica, al aumentar la desigualdad en la equidad de género entre CC.AA. en 2014. La inequidad de género sigue siendo desfavorable a las mujeres.
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Letter, undated, from committee of eight members of the Church of England in Boston, John Barnes, Thomas Greaves, Anthony Blount, John Gibbins, George Cradock, Thomas Selbey and two others, appealing to Nicholson to help support the founding and building of Christ Church.
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This layer is a georeferenced raster image of the historic paper map entitled: Map of the country around Philadelphia : with the good roads specially marked. It was published by J. L. Smith in 1897. Scale [1:63,360]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Pennsylvania South State Plane Coordinate System NAD83 (in Feet) (Fipszone 3702). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads ("Good roads" are shown in red), railroads, drainage, canals, selected buildings, towns, county and state boundies, and more. Includes explanation of signs. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.
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بسم الله الرحمن الرحيم الفصل الاول الحمد لله الذي نثر على وجه عروس الارض ... :Incipit
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Relatório de estágio para a obtenção do grau de mestre em Educação pré-escolar
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Marca tip. en port. (Vindel, 322) y de Guillermo de Millis en 2O8r (Vindel, 166)
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Marine organic matter (OM) sinks from surface waters to the seafloor via the biological pump. Benthic communities, which use this sedimented OM as energy and carbon source, produce dissolved organic matter (DOM) in the process of remineralization, enriching the sediment porewater with fresh DOM compounds. We hypothesized that in the oligotrophic deep Arctic basin the molecular signal of freshly deposited primary produced OM is restricted to the surface sediment pore waters which should differ from bottom water and deeper sediment pore water in DOM composition. This study focused on: 1) the molecular composition of the DOM in sediment pore waters of the deep Eurasian Arctic basins, 2) whether the signal of marine vs. terrigenous DOM is represented by different compounds preserved in the sediment pore waters and 3) whether there is any relation between Arctic Ocean ice cover and DOM composition. Molecular data, obtained via 15 Tesla Fourier transform ion cyclotron resonance mass spectrometer, were correlated with environmental parameters by partial least square analysis. The fresher marine detrital OM signal from surface waters was limited to pore waters from < 5 cm sediment depth. The productive ice margin stations showed higher abundances of peptides, unsaturated aliphatics and saturated fatty acids formulae, indicative of fresh OM/pigments deposition, compared to northernmost stations which had stronger aromatic signals. This study contributes to the understanding of the coupling between the Arctic Ocean productivity and its depositional regime, and how it will be altered in response to sea ice retreat and increasing river runoff.
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Includes indexes.
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Mode of access: Internet.
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The prefaces, biographical introductions, analytical notes and bibliographies are in Spanish and French.
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Editors and imprints vary.