988 resultados para Georges Perec
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Incluye Bibliografía
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Considering the premise that there are few theoretical reflections in the Portuguese language, concerning the autobiography as a genre, we propose to present a work addressing this issue by discussing the writings of George Gusdorf (1912-2000). One of the most expressive French scholars on this field, alongside Philippe Lejeune and Jean George May, and Starobinsky, Gusdorf stands out for his vast production centered on theoretical issues concerning the writings of the self. The study presented here aims at disseminating Gusdorf writings in Brazil, as well as presenting a critical analysis of the most pertinent issues related to the autobiographical genre, including aspects such as its origins, the blurred boundaries of genre, truth and sincerity, the relations between time and memory, self-knowledge and knowledge of the world.
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This paper explores the religious implications of eroticism in Western culture since the Sexual Revolution, a period at once applauded for its open and immanent view of sexuality and denounced for its shamelessness and promiscuity. After discussing the work and effects of Alfred C. Kinsey, the father of the Sexual Revolution, I focus on a critical appraisal of Kinsey written by French theorist Georges Bataille (“Kinsey, the Underworld and Work,” in L’Erotisme, 1957). Bataille situates contemporary Western sexuality within a larger historical movement towards the “desacralization” of all aspects of human life: sex, under the scientific gaze of the Kinsey team, became simply another “object” to be analyzed and classified, and “good” sex defined solely in terms of frequency and explosiveness of orgasm. For many, including Hugh Hefner, this approach to sex occasioned a refreshing awakening from the long dark night of Victorian sexual repression. However, as Bataille’s protégé Foucault has shown, the scientific approach to sexuality often masks a desire to control and delimit sexual behaviour, not “liberate” it. Moreover, Bataille makes the point that the desacralization of sexuality denudes sex of a vital component—eroticism—which is necessary for real pleasure and ecstasy. Beyond the “moral” critiques one often hears leveled against Kinsey and his work, Bataille provides a “religious” critique, one that stands, perhaps surprisingly, on the “near side” of sexuality.
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The dynamics of phytoplankton and nutrients before, during and after the winter-spring bloom on Georges Bank were studied on 6 monthly survey cruises from January to June 1999. We measured hydrography, phytoplankton cell densities, chlorophyll a, dissolved inorganic nutrients (NO3 + NO2, NH4, Si(OH)(4), PO4), dissolved organic nitrogen (DON) and phosphorus (DOP), particulate organic carbon (POC) and nitrogen (PON) and total particulate phosphorus (TPP). We present evidence that phytoplankton production may be significant year-round, and that the winter-spring bloom may have started in January. From January to April the phytoplankton was comprised almost exclusively of diatoms, reaching cell densities in March and April of ca. 450 cells ml(-1); chlorophyll a concentrations exceeded 10 mug l(-1) in April. Diatoms decreased to relatively low levels in May (< 50 x 10(3) cells l(-1)) and increased again in June (>300 x 10(3) cells l(-1)). Densities of dinoflagellates and nanoflagellates were low (< 10 x 10(3) cells l(-1)) from January to April, and increased in May and June to nearly 300 x 10(3) cells l(-1). Nitrate + nitrite concentrations in January were <3 muM in the shallow, central portion of the bank and decreased steadily each month. Silicate was also <3 muM over an even larger area of the central bank in January and declined to <1.5 muM over most of the Bank in April. The data suggest that silicate depletion, not DIN, contributed to the cessation of the diatom bloom. Regeneration of silicate occurred in May and June, presumably as a result of rising water temperatures in late spring which increased the dissolution rate of diatom frustules from the earlier diatom bloom. Dissolved organic nitrogen may have been utilized at the start of the winter-spring bloom; concentrations were ca, 14 muM in January, dropping to < 6 mug l(-1) in February, after which DON concentrations steadily rose to > 15 mug l(-1) in June. Overall micro-and nanoplankton biomass, measured as POC, PON and TPP, increased over the 6 mo period, as did nutritional quality of that biomass as indicated by declining C:N ratios. Our results suggest there may have been an increase in the heterotrophic component of the plankton in May and June which coincided with a second burst in diatom abundance. We discuss general features of planktonic production and nutrient dynamics with respect to year-round production on the Bank.
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Joseph Derenbourg