A presença inglesa no Brasil e sua influência nas obras de escritores brasileiros do século XIX

Esta dissertação tem por objetivo investigar a presença dos escritores ingleses nas obras de escritores brasileiros do século XIX. Os romancistas ingleses que se destacaram na Inglaterra do século XVIII foram Daniel Defoe, Samuel Richardson e Henry Fielding. Eles contribuíram para ascensão e consolidação do romance como gênero literário. No Brasil, o romance desenvolveu-se com maior liberdade e atraiu o público leitor. O novo público começa a ler romances que recriavam a cidade, as ruas e a vida de uma classe social emergente: a burguesia. O novo gênero que surgiu na Inglaterra promoveu o crescimento do comércio, a proliferação de revistas e jornais, de cunho popular e literário. Os escritores brasileiros como José de Alencar e Machado de Assis sofreram influências dos escritores ingleses, no entanto, essa influência não foi refletida somente nos romances desses escritores, foi sentida também nos negócios, na cultura e na vida social do Brasil. Alguns exemplos dessa presença são igualmente revelados nas obras de Machado de Assis por meio das citações, das referências e das alusões. Machado de Assis, sempre quando possível, faz referências aos escritores ingleses tanto dos séculos XVI e XVIII quanto do século XIX, tais como Shakespeare, Swift, Fielding. Sterne, Lamb e Dickens entre outros romancistas ingleses.

Terrestrial and submarine evidence for the extent and timing of the Last Glacial Maximum and the onset of deglaciation on the maritime-Antarctic and sub-Antarctic islands

This paper is the maritime and sub–Antarctic contribution to the Scientific Committee for Antarctic Research (SCAR) Past Antarctic Ice Sheet Dynamics (PAIS) community Antarctic Ice Sheet reconstruction. The overarching aim for all sectors of Antarctica was to reconstruct the Last Glacial Maximum (LGM) ice sheet extent and thickness, and map the subsequent deglaciation in a series of 5000 year time slices. However, our review of the literature found surprisingly few high quality chronological constraints on changing glacier extents on these timescales in the maritime and sub–Antarctic sector. Therefore, in this paper we focus on an assessment of the terrestrial and offshore evidence for the LGM ice extent, establishing minimum ages for the onset of deglaciation, and separating evidence of deglaciation from LGM limits from those associated with later Holocene glacier fluctuations. Evidence included geomorphological descriptions of glacial landscapes, radiocarbon dated basal peat and lake sediment deposits, cosmogenic isotope ages of glacial features and molecular biological data. We propose a classification of the glacial history of the maritime and sub–Antarctic islands based on this assembled evidence. These include: (Type I) islands which accumulated little or no LGM ice; (Type II) islands with a limited LGM ice extent but evidence of extensive earlier continental shelf glaciations; (Type III) seamounts and volcanoes unlikely to have accumulated significant LGM ice cover; (Type IV) islands on shallow shelves with both terrestrial and submarine evidence of LGM (and/or earlier) ice expansion; (Type V) Islands north of the Antarctic Polar Front with terrestrial evidence of LGM ice expansion; and (Type VI) islands with no data. Finally, we review the climatological and geomorphological settings that separate the glaciological history of the islands within this classification scheme.

Sketches

by Charles Dickens

Major and trace element concentrations of sediments from the IODP Exp302 sites

We analyzed a suite of sediment samples recovered in the central Arctic Ocean for major, trace, and rare earth elements in order to assess changes in terrigenous source material throughout the Cenozoic. The terrigenous component consists of two end-members. Input from a shale-like composition dominates bulk sediments, especially those deposited during the Paleocene and since the Miocene, and may represent sediment supply from the eastern Laptev Sea. Therefore, even though the environment and transport mechanisms may have varied from ice free to ice dominated, sequences of the early Paleogene and later Neogene appear to have been influenced by a single major terrigenous source. This suggests similar transport capabilities and trajectories for both ocean and drift currents through significant parts of the Cenozoic. Influence from a more mafic source appears to be more important through the early Eocene to the middle Miocene and most likely represents material from the western Laptev Sea or Kara Sea. Thus, Eocene major changes in surface water productivity appear broadly synchronous with those in terrigenous provenance. A combination of regional sea level variations, local shelf processes, and transport mechanisms are among the more probable causes for the observed source changes. Although the assignment of sources using chemistry presently is constrained by a lack of data from certain regions (e.g., eastern Siberian Sea) our results generally agree with inferences based on mineralogy or radiogenic isotopes and shed further light on long-term reconstructions of the central Arctic Ocean.

Manganese concentrations and flux data of sediments from Broken and Ninetyeast Ridge

Decomposition of organic matter combined with density stratification generate a pronounced intermediate water oxygen minimum zone (OMZ) in the northwest Indian Ocean. This zone currently lies between water depths of 200 and 2000 m and extends approximately 5000 km southeast from the Arabian coast. Based upon benthic foraminiferal assemblage changes, it has been suggested that this OMZ was even more extensive during the late Miocene-early Pliocene (6.5-3.0 Ma), with a maximum volume and/or intensity at approximately 5.0 Ma. While this inference may contribute to an understanding of the history of northwest Indian Ocean upwelling, corroborating geochemical evidence for this interpretation has heretofore been lacking. Ocean Drilling Program (ODP) sites 752, 754, and 757 on Broken and Ninetyeast ridges are located within central Indian Ocean intermediate water depths (1086-1650 m) but outside the present lateral dimensions of the Indian Ocean OMZ. High-resolution chemical analyses of sediment from these sites indicate significant reductions in the flux of Mn and normalized Mn concentrations between 6.5 and 3.0 Ma that are most pronounced at approximately 5.0 Ma. Because late Miocene-Pliocene paleodepths for these sites were essentially the same as at present and because extremely low sedimentation rates (0.3-1.3 cm/ky) most likely precluded sedimentary metal oxide diagenesis, we suggest that the observed Mn depletions reflect diminished deposition of reducible Mn oxyhydroxide phases within O2 deficient intermediate waters and that this effect was most intense at approximately 5.0 Ma. This interpretation implies that waters with less than 2.0 mL/L O2 extended at least 1500 km beyond their present limits and is consistent with changes in benthic foraminifera assemblages. We further suggest this expanded Indian Ocean OMZ is related to regionally and/or globally increased biological productivity.

Manejo prenatal de la anencefalia: consideraciones éticas y legales en la salud reproductiva

Texto traducido con autorización de la Federación Internacional de Ginecología y Obstetricia (FIGO): Cook, R. J., Erdman, J.N., Hevia, M, Dickens, B.M, Prenatal management of anencephaly. International Journal of Gynecology and Obstetrics.

Problemáticas éticas y legales en la salud reproductiva: responsabilidades en los servicios de salud y objeción de conciencia

Traducido de: Cook, R.J, M. Arango Olaya y B. M. Dickens. Healthcare Responsibilities and Conscientious Objection. International Journal of Gynecology and Obstetrics. 2009

Servicios de salud reproductiva y el Derecho y ética de la objeción de conciencia.

http://utdt.edu/download.php?fname=_127947914868664100.pdf

Los derechos reproductivos: un debate necesario

Planned Parenthood Federation of America (PPFA) y el Centro de Promoción y Defensa de los Derechos Sexuales y Reproductivos (PROMSEX), como organizaciones auspiciantes del Primer Congreso Latinoamericano Jurídico sobre Derechos Reproductivos (Congreso Jurídico), quieren agradecer especialmente a Oscar Cabrera por sus aportaciones y su invaluable compromiso en coordinar, editar y escribir parte de esta publicación. Queremos expresar también nuestro profundo agradecimiento a las académicas que aportaron sus artículos sobre temas centrales para la región en relación al ejercicio de los derechos reproductivos. A ellas, Agustina Ramón Michell, Lidia Casas Becerra, Mercedes Cavallo y Claudia Ahumada, mil gracias. A las profesoras Rebecca Cook y Joanna Erdman y al profesor Bernard Dickens, nuestro sincero reconocimiento por su constante apoyo. Y un especial agradecimiento al Dr. Luis Lamas Puccio, ex vicedecano del Ilustre Colegio de Abogados de Lima, por su compromiso en la defensa de los derechos de las mujeres.

Planktonic foraminifera, nannofossils and stable isotope record across tghe Paleocene-Eocene thermal maximum of ODP Hole 113-690B

The carbonate saturation profile of the oceans shoaled markedly during a transient global warming event known as the Paleocene-Eocene thermal maximum (PETM) (circa 55 Ma). The rapid release of large quantities of carbon into the ocean-atmosphere system is believed to have triggered this intense episode of dissolution along with a negative carbon isotope excursion (CIE). The brevity (120-220 kyr) of the PETM reflects the rapid enhancement of negative feedback mechanisms within Earth's exogenic carbon cycle that served the dual function of buffering ocean pH and reducing atmospheric greenhouse gas levels. Detailed study of the PETM stratigraphy from Ocean Drilling Program Site 690 (Weddell Sea) reveals that the CIE recovery period, which postdates the CIE onset by ~80 kyr, is represented by an expanded (~2.5 m thick) interval containing a unique planktic foraminiferal assemblage strongly diluted by coccolithophore carbonate. Collectively, the micropaleontological and sedimentological changes preserved within the CIE recovery interval reflect a transient state when ocean-atmosphere chemistry fostered prolific coccolithophore blooms that suppressed the local lysocline to relatively deeper depths. A prominent peak in the abundance of the clay mineral kaolinite is associated with the CIE recovery interval, indicating that continental weathering/runoff intensified at this time as well (Robert and Kennett, 1994). Such parallel stratigraphic changes are generally consonant with the hypothesis that enhanced continental weathering/runoff and carbonate precipitation helped sequester carbon during the PETM recovery period (e.g., Dickens et al., 1997, doi:10.1130/0091-7613(1997)025<0259:ABOGIT>2.3.CO;2 ; Zachos et al., 2005, doi:10.1126/science.1109004).