The Uncanny in the Themes of Evil, Transgression and the Double in Nathaniel Hawthorne's "Rappaccini's Daughter"

El propósito de este artículo consiste en explorar los mecanismos y representaciones de lo siniestro en "La hija de Rappacci" de Nathaniel Hawthome como expresión del mal dentro de los límites del género gótico del siglo XIX; como expresión del tema del doble en tres personajes humanos y en uno no humano que aparecen en el cuento; y como expresión de trasgresión en el personaje principal, Giovanni Guasconte. El concepto de lo siniestro que se usará será el de la teoría psicoanalítica, siguiendo especialmente los aportes de Sigmund Freud y Jacques Lacan. The purpose of this artide is to explore the mechanisms and representations of the uncanny in Nathaniel Hawthome's "Rappaccini's Daughter" as an expression of evil within nineteenth century Gothic boundaries; as an expression of the theme of the double in three human characters and in one non-human component of Rappaccini's garden; and as an expression of transgression in Giovanni Guasconte, the main character. The concept of the uncanny to be used will be that of psychoanalytic theory, especially reliant on the contributions on the topic by Sigmund Freud and Jacques Lacan.

Interações entre evolução sedimentar e ocupação humana pré-histórica na costa centro-sul de Santa Catarina, Brasil

Desde o começo da ocupação humana no litoral centro-sul de Santa Catarina, Brasil, a articulação entre processos naturais e antrópicos modelou uma paisagem fortemente domesticada, marcada pela construção massiva de concheiros de dimensões monumentais e pela permanência milenar. Na planície costeira entre Passagem da Barra (município de Laguna) e lago Figueirinha (município de Jaguaruna), 76 sambaquis foram mapeados, dos quais 48 possuem datação. O levantamento sistemático de sítios e datações permitiu identificar padrões de distribuição espacial nos sambaquis da região, quanto a contexto sedimentar da época de construção, estratigrafia e idade. Desse modo, reconheceram-se nos sítios da região: cinco contextos geológico-geomorfológicos de localização; três padrões estratigráficos; e quatro fases de ocupação sambaquieira baseadas na quantidade de sítios e no tipo de padrão construtivo dominante. O modelo integrado de evolução sedimentar e distribuição tempo-espacial de sambaquis indica que estes sítios eram construídos em áreas já emersas e pouco alagáveis, e que sítios interiores, afastados dos corpos lagunares, podem não se ter preservado ou não estarem expostos devido ao processo de assoreamento contínuo que caracterizou a região após a máxima transgressão holocênica. O cruzamento de dados aqui proposto evidencia a importância de abordagens integradas entre arqueologia e geociências no estudo da evolução das paisagens.

Marine influence in the Barreiras Formation, State of Alagoas, northeastern Brazil

Tidal processes were important for deposition of the Barreiras Formation located in northern Brazil, while correlatable deposits in northeastern Brazil have been traditionally related to continental environments. Facies analysis in southern Alagoas revealed that the Barreiras Formation consists of cross-stratified conglomerates and sandstones (facies Sx and Cgx), compound cross-stratified sandstones (facies Cx), and heterolithic beddings (facies H). A significant portion of these deposits occurs within channel morphologies displaying fining and thinning upward successions. An abundance of sedimentary features is comparable to those from the northern Brazilian counterpart. These include: tidal bundles; herringbone cross-stratification; heterolithic beddings with sandstone and mudstone beds in sharp contacts; and ichnofossils mostly consisting of Ophiomorpha nodosa, Skolithos and Planolites. Altogether, these features point to a marginal marine depositional setting dominated by tidal processes, which are related to an estuarine system, an interpretation also provided for the Barreiras Formation in northern Brazil. The widespread occurrence of deposits with unambiguous evidence of tidal processes in the Barreiras Formation of northern Brazil, and now in the State of Alagoas, leads to argue that the early/middle Miocene worldwide marine transgression might have left a much more widespread sedimentary record along the Brazilian coast than currently regarded.

Facies, delta(13)C, delta(15)N and C/N analyses in a late Quaternary compound estuarine fill, northern Brazil and relation to sea level

The present work integrates sedimentary facies, (14)C dating, delta(13)C, delta(15)N, and C/N with geologic and geomorphologic data available from literature. The aim was to characterize the depositional settings of a late Quaternary estuary in northeastern Marajo Island and analyze its evolution within the context of relative sea level fluctuations. The data derive from four continuous cores along a proximal-to-distal transect of a paleoestuary, previously recognized using remote sensing information. Fifteen sediment samples recorded ages ranging from 42,580 +/- 1430 to 3184 +/- 37 (14)C yr B.P. Fades analysis indicated fine- to coarse-grained sands with parallel lamination or cross stratification, massive or laminated muds and heterolithic deposits. delta(13)C (-28.1 parts per thousand to -19.7 parts per thousand, mean = -23.0 parts per thousand), delta(15)N (+ 14.8 parts per thousand to + 4.7 parts per thousand, mean = + 9.2 parts per thousand) and C/N (14.5 to 1.5, mean = 7.9) indicate mostly marine and freshwater phytoplankton sources for the organic matter. The results confirm a large late Quaternary paleoestuary in northeastern Marajo Island. The distribution of delta(13)C, delta(15)N, and C/N, together with fades associations, led to identify depositional settings related to fluvial channel, floodplain, tidal channel/tidal flat, central basin, tidal delta, and tidal inlet/sand barrier. These deposits are consistent with a wave-dominated estuary. Variations in stratigraphy and geochemistry are controlled by changes in relative sea level, revealing a main transgression from an undetermined time around 42,000 (14)C yr B.P. and 29,340 (+/- 200) (14)C yr B.P., which is synchronous to the overall drop in sea level after the last interglacial. Following this period, and probably until 9110 +/- 37 (14)C yr B.P., i.e., during a time interval encompassing two glacial episodes including the Last Glacial and the Younger Dryas, there was a pronounced drop in sea level, recorded by the development of a major erosional discontinuity due to valley re-incision. Sea level rose again until 5464 +/- 40 (14)C yr B.P, just before the main worldwide mid-Holocene transgressive peak. Mid to late Holocene coastal progradation ended the Marajo paleoestuarine history, and promoted the establishment of continental conditions throughout the island. The divergence comparing the Marajo sea level behavior with the eustatic curve allows hypothesizing that post-rifting tectonics along the Brazilian Equatorial margin influenced the sedimentary evolution of the studied paleoestuary. Considering that sedimentary facies in estuarine settings are highly variable both laterally and vertically, the present integration of facies with isotope and elemental analyses was crucial to provide a more precise interpretation of the Late Pleistocene and Holocene Marajo paleoestuary, and analyze its sea level history within the eustatic and tectonic context. (C) 2010 Elsevier B.V. All rights reserved.

Quaternary paleoenvironments and relative sea-level changes in Marajo Island (Northern Brazil): Facies, delta(13)C, delta(15)N and C/N

The reconstruction of physical environments of Amazonian areas is of great interest to determine the dynamic evolution of the Amazon drainage basin. However. few studies have emphasized the Quaternary deposits in this region. which is mostly due to the lack of natural exposures imposed by the low topography. This work integrates facies analysis. radiocarbon dating, delta(13)C, delta(15)N, and C/N of an 124 m-thick core from an area located at the mouth of the Amazon River. northeastern Amazonia. The study records deposits up to 50.795 (14)C yr B P. in age. which formed in a variety of depositional environments including fluvial channel, tidal flat, outer estuarine basin to shallow marine. inner estuarine basin, estuarine channel and lagoon. Facies interpretation was significantly improved with the inclusion of delta(13)C, delta(15)N, and C/N analyses of organic matter extracted from the sediments The obtained values conform to a transitional. mostly estuarine paleosetting evolved during successive relative sea-level fluctuations. The results suggest fluvial deposition between 40,950 (+/- 590) and 50.795 (14)C yr B P, with a rise in relative sea level that commenced between 35,567 (+/- 649) and 39,079 (+/- 1114) (14)C yr B P. An overall transgression took place until 29,340 (+/- 340) (14)C yr B P., after which the relative sea level dropped, favoring valley rejuvenation and incision. Following this time up to 10,479 (+/- 34) (14)C yr B.P. a rise in relative sea level filled up the valley with estuarine deposits After 10.479(+/- 34) (14)C yr B.P., the estuary was replaced by a lagoon At the end of the Holocene, the coastline prograided approximately 45 km northward, replaci ng the lagoon by a lake system Despite the influence of eustatic fluctuations. regional tectonics played a significant role to create new space where these Late Pleistocene and Holocene sediments accumulated. (C) 2009 Elsevier B V All rights reserved.

TOPOGRAPHIC REGISTERS OF PALEO-VALLEYS ON THE SOUTHEASTERN BRAZILIAN CONTINENTAL SHELF

The evolution of paleo-incised-valleys in the Sao Paulo State region of the southeastern Brazilian continental shelf is presented in this study in relation to the post Last Glacial Maximum (LGM) sea-level rises based on the submarine topography modeled by a detailed Digital Elevation Model and evidences noted in high resolution seismic profiles. The hypothesis that has guided this study is that the set of paleo-valley characteristics (i.e. the fluvial parameters of modern coastal drainage systems, the topographical shape and dimensions of the valleys and of the subsurface channels) may indicate aspects of the relation between the influence of the fluvial and the eustatic variation regime in geomorphological-stratigraphic registers. Models described in the literature sustain the view that faster marine transgressions tend to increase erosion in estuaries, which may explain the lack of registers of paleo-drainage both in topography and the sub-surface in areas with wider shelves. On the other hand, on narrower shelves, with a higher slope angle, the transgression process can preserve, or even enhance, the incised valley registers during shoreface retreat. In the area studied, we observed that the dimensions and form of the continental shelf varies from the northern to the southern part of the area, affecting aspects of the geomorphological registers of the submerged incised valleys.

Late Quaternary cycles of mangrove development and decline on the north Australian continental shelf

Mangrove communities in the Australian tropics presently occur as narrow belts of vegetation in estuaries and on sheltered, muddy coasts. Palynological data from continental shelf and deep-sea cores indicate a long-term cyclical component of mangrove development and decline at a regional scale, which can be linked to specific phases of late Quaternary sealevel change. Extensive mangrove development, relative to today, occurs during periods of marine transgression, whereas very diminished mangrove occurs during marine regressions and during rarer periods of relative sea-level stability. Episodes of flourishing mangrove cannot be linked to phases of humid climate, as has been suggested in studies elsewhere. Rather, the cycle of expansion and decline of mangrove communities on a grand scale is explained in terms of contrasting physiographic settings characteristic of continental-shelf coasts during transgressive and regressive phases, in particular by the existence, or lack, of well-developed tidal estuaries. Copyright (C) 1999 John Wiley & Sons, Ltd.

Pea rms6 mutants exhibit increased basal branching

Our studies on two branching mutants of pea (Pisum sativum L.) have identified a further Ramosus locus, Rms6, with two recessive or partially recessive mutant alleles: rms6-1 (type line S2-271) and rms6-2 (type line K586). Mutants rms6-1 and rms6-2 were derived from dwarf and tall cultivars, Solara and Torsdag, respectively. The rms6 mutants are characterized by increased branching from basal nodes. In contrast, mutants rms1 through rms5 have increased branching from both basal and aerial (upper stem) nodes. Buds at the cotyledonary node of wild-type (WT) plants remain dormant but in rms6 plants these buds were usually released from dormancy. Their growth was either subsequently inhibited, sometimes even prior to emergence above ground, or they grew into secondary stems. The mutant phenotype was strongest for rms6-1 on the dwarf background. Although rms6-2 had a weak single-mutant phenotype, the rms3-1 rms6-2 double mutant showed clear transgression and an additive branching phenotype, with a total lateral length almost 2-fold greater than rms3-1 and nearly 5-fold greater than rms6-2 . Grafting studies between WT and rms6-1 plants demonstrated the primary action of Rms6 may be confined to the shoot. Young WT and rms6-1 shoots had similar auxin levels, and decapitated plants had a similar magnitude of response to applied auxin. Abscisic acid levels were elevated 2-fold at node 2 of young rms6-1 plants. The Rms6 locus mapped to the R to Gp segment of linkage group V (chromosome 3). The rms6 mutants will be useful for basic research and also have possible agronomical value.

Mid- to Late-Holocene estuarine infilling processes studied by radiocarbon dates, high resolution seismic and biofacies at Vitoria Bay, Espirito Santo, Southeastern Brazil

A Baía de Vitória é um estuário com 20 km de comprimento, morfologicamente estreito, com um regime de micromaré e, como outros estuários modernos, formado durante a última transgressão pós-glacial. A morfologia de fundo do estrato estuarino é caracterizada por um canal natural principal limitado por planícies de maré com manguezais desenvolvidos. Datações de radiocarbono originais foram obtidas para a área. Cinco idades de radiocarbono estendendo-se de 1.010 a 7.240 anos AP foram obtidas através de dois testemunhos de sedimento, representando uma sequência estratigráfica de 5 m de espessura. Os resultados indicam que até aproximadamente 4.000 anos cal. AP, as condições ambientais da Baía de Vitória eram ainda de uma baía aberta, com uma conexão livre e aberta com águas marinhas. Durante os últimos 4.000 anos a baía experimentou uma fase de regressão importante, tornando-se mais restrita em termos de circulação da água do mar e provavelmente aumentando a energia de marés. Três superfícies estratigráficas principais foram reconhecidas, limitando fácies transgressiva, transgressiva/nível de mar alto e regressiva. A morfologia do canal atual representa um diastema de maré, mostrando fácies regressivas truncadas e erodidas. Biofácies de foraminíferos, passando de ambiente marinho para ambiente salobro e de manguezais em planície de maré confirmam a interpretação sismoestratigráfica. A ausência de biofácies de mangue em um dos dois testemunhos é tambémuma indicação de ravinamento de maré atual.

O mal-estar na civilização entre desejo e gozo

Mal-estar na civilização (Freud S.) inclui os elementos que vêm inaugurar uma querela sobre a ética da psicanálise, tal como Lacan a circunscreveu. A tese de base é que a resignação em relação às pulsões da demanda contem uma certa satisfação.

Adolescente e ato infracional : uma investigação acerca da medida socioeducativa de internação na cidade do Recife-PE

RESUMO: Este estudo procura avaliar a Medida Socioeducativa de Internação decretada a adolescentes autores de ato infracional na Cidade do Recife no ano de 2009. É um trabalho de grande importância para a sociedade brasileira, sobretudo, no que diz respeito ao combate à violência juvenil, à criminalidade em geral, e à construção de um mundo mais justo e solidário. Escolhemos a Cidade do Recife, Capital do Estado de Pernambuco, localizada na região Nordeste do Brasil, para ser o local da nossa pesquisa, por ser esta uma das mais violentas cidades do país. No decorrer desta pesquisa fizemos ainda uma breve análise do cenário sociológico da adolescência na Cidade do Recife. Em seguida estudamos o cenário jurídico dos adolescentes autores de ato infracional com base no Estatuto da Criança e do Adolescente – Lei nº 8.069/1990, analisando a evolução histórica do tratamento legal dispensado a estes jovens, abordando o conceito de adolescente e ato infracional, e investigando as Medidas Socioeducativas previstas na legislação brasileira, sobretudo, a Medida de Internação, pelo fato de ser a mais grave delas. Assim, além investigarmos através de dados estatísticos o quantitativo por gênero de adolescentes autores de ato infracional aos quais foram decretadas Medida de Internação, observamos os tipos de atos infracionais mais praticados. Intentamos, dessa forma, questionar a violência juvenil e o modo como a sociedade e as instituições envolvidas têm tratado a questão. Para tanto, foram realizadas entrevistas com servidores da Fundação de Atendimento Socioeducativo- FUNASE, entidade que trabalham diretamente com a reeducação de adolescentes autores de ato infracional submetidos à Internação na Cidade do Recife, para analisar como estão sendo aplicadas essas medidas. ABSTRACT: This study aims to evaluate the Socioeducational Measure of Internation decreed to transgressor teenagers in the City of Recife at the year 2009. This study has a big importance to Brazilian society, above all, because focalize the combat of the juvenile violence in Recife, Capital of the State of Pernambuco on the northwest of the Brazil, one of the most violent city of Brazil. During this investigation, was done a brief analysis of sociological scenery of teenage in this City. It was studied too, the juridical scenery of teenagers that committed any kind of transgression, based on the Statue of Child and the Adolescent- law n° 8.069/1990, analyzing the historical evolution of lawful treatment put into practice to this people, using the concept of adolescent and infracional act, and observing the social and educative punishment in the penal justice system of Brazil, and detaching the measure of internation, that is the gravest form of punishment. So, in this study it was investigated the quantity of transgressors adolescents based in gender and the kinds of transgression most practiced by them which results on internation measure decreed. This way, the purpose of this study is discuss about young violence and the way that society and institutions have faced this question. For this, it was realized interviews with Foundation of Socioeducative Attendance – FUNASE workers, that work directly with re-education of adolescents that committed any transgression and were submitted to internation punishment, in order to analyze how are being applied these measures.

À descoberta das emoções sociais: vergonha e culpa : implementação e avaliação de duas sessões de um programa para a promoção de competências emocionais : um enfoque comunitário

Dissertação de Mestrado em Psicologia da Educação, especialidade em Contextos Comunitários.

Keep calm enfrenta a vergonha : contributos para um programa de competências sócio-emocionais

Trabalho apresentado em XIII Congreso Internacional Galego-Portugués de Psicopedagoxía, Área 1 Aprendizaje, memoria y motivación. Universidad da Coruña, 2 de Setembro de 2015.

La médecine indigène comme instrument normatif social: l’exemple du corps malade navajo

La médecine traditionnelle indigène peut parfois se poser comme un instrument normatif désignant le malade comme celui qui transgresse l‘ordre établi par les ancêtres sacrés et permet à la maladie d‘advenir. Un tiers malveillant ou un sorcier peuvent également être les causes du désordre physiologique et moral du corps social communautaire. L‘étiologie navajo repose sur deux phénomènes : l‘existence de sociosomas (troubles liés à une mauvaise relation à l‘entourage) et de mouvements d‘exclusion ou d‘inclusion du corps étranger, de la conduite déviante. L‘étude de la figure du malade dans les mythes soulignera l‘aspect normatif des thérapeutiques navajo. Enfin, une réflexion sur la justification idéologique de l‘intégration des pratiques ancestrales au protocole de soin montrera dans quelle mesure la collaboration entre praticiens traditionnels et personnels de santé contribue à stigmatiser le malade comme l‘épitome de toutes les déviances : par rapport à la tradition mais aussi au modèle social dominant.

Alcipe, Nathercia e Tirse: Considerações sobre as luzes no feminino no Portugal de setecentos

O presente artigo desenvolve-se em torno de três damas esclarecidas da sociedade portuguesa de setecentos: D. Leonor de Almeida (1750-1839), ou Alcipe; D. Catarina de Lencastre (1749-1824), ou Nathercia; e D. Teresa de Mello Breyner (1739-1798?), ou Tirse. Sabendo que o século XVIII foi um período marcado por mudança e controvérsia, pela emergência de novos paradigmas, pelo reequacionamento de estruturas mentais e tradições seculares – ainda que em Portugal se experimentasse uma certa resistência às teorias filosóficas emergentes – a questão que lançamos e procuramos analisar é: qual o reflexo destas transformações no universo feminino? Assim, partindo dos três exemplos referidos e a eles tornando, pretendemos problematizar três questões centrais no discurso iluminista – educação, leituras e viagens – observando como estas matérias, assaz discutidas e teorizadas ao longo do século XVIII, se repercutiram na formação feminina em solo português e, por outro lado, analisar o modesto mas expressivo papel que as referidas damas assumiram na propagação da cultura das luzes em Portugal.