A brief history of the scientific study of tropical African inland waters

An account is given of a study of African tropical waters, drawing on the personal experiences of the author. Reviewing developments since 1900, the author examines the way in which research has developed and the influence the changes in the policitcal map of Africa, in particular the change from colonial rule, has had on research.

History, origins and importance of temporary ponds

In Europe, temporary ponds are a naturally common and widespread habitat occurring, often in abundance, in all biogeographical regions from the boreal snow-melt pools of northern Scandinavia to the seasonally inundated coastal dune pools of southern Spain. Ecological studies in Europe and elsewhere also emphasise that temporary ponds are a biologically important habitat type, renowned both for their specialised assemblages and the considerable numbers of rare and endemic species they support. They are, however, a habitat currently under considerable threat. Most temporary ponds are inherently shallow and the majority are destroyed even by limited soil drainage for agriculture or urban development. The paper gives an overview of definitions of temporary ponds and examines their formation and abundance. The authors also summarise a visit to the Bialowieza Forest in Poland to investigate the occurrence of temporary ponds.

Complexity of rupture propagation in large earthquakes in relation to tectonic environment

Complexity in the earthquake rupture process can result from many factors. This study investigates the origin of such complexity by examining several recent, large earthquakes in detail. In each case the local tectonic environment plays an important role in understanding the source of the complexity.

Several large shallow earthquakes (M_s > 7.0) along the Middle American Trench have similarities and differences between them that may lead to a better understanding of fracture and subduction processes. They are predominantly thrust events consistent with the known subduction of the Cocos plate beneath N. America. Two events occurring along this subduction zone close to triple junctions show considerable complexity. This may be attributable to a more heterogeneous stress environment in these regions and as such has implications for other subduction zone boundaries.

An event which looks complex but is actually rather simple is the 1978 Bermuda earthquake (M_s ~ 6). It is located predominantly in the mantle. Its mechanism is one of pure thrust faulting with a strike N 20°W and dip 42°NE. Its apparent complexity is caused by local crustal structure. This is an important event in terms of understanding and estimating seismic hazard on the eastern seaboard of N. America.

A study of several large strike-slip continental earthquakes identifies characteristics which are common to them and may be useful in determining what to expect from the next great earthquake on the San Andreas fault. The events are the 1976 Guatemala earthquake on the Motagua fault and two events on the Anatolian fault in Turkey (the 1967, Mudurnu Valley and 1976, E. Turkey events). An attempt to model the complex P-waveforms of these events results in good synthetic fits for the Guatemala and Mudurnu Valley events. However, the E. Turkey event proves to be too complex as it may have associated thrust or normal faulting. Several individual sources occurring at intervals of between 5 and 20 seconds characterize the Guatemala and Mudurnu Valley events. The maximum size of an individual source appears to be bounded at about 5 x 10²⁶ dyne-cm. A detailed source study including directivity is performed on the Guatemala event. The source time history of the Mudurnu Valley event illustrates its significance in modeling strong ground motion in the near field. The complex source time series of the 1967 event produces amplitudes greater by a factor of 2.5 than a uniform model scaled to the same size for a station 20 km from the fault.

Three large and important earthquakes demonstrate an important type of complexity --- multiple-fault complexity. The first, the 1976 Philippine earthquake, an oblique thrust event, represents the first seismological evidence for a northeast dipping subduction zone beneath the island of Mindanao. A large event, following the mainshock by 12 hours, occurred outside the aftershock area and apparently resulted from motion on a subsidiary fault since the event had a strike-slip mechanism.

An aftershock of the great 1960 Chilean earthquake on June 6, 1960, proved to be an interesting discovery. It appears to be a large strike-slip event at the main rupture's southern boundary. It most likely occurred on the landward extension of the Chile Rise transform fault, in the subducting plate. The results for this event suggest that a small event triggered a series of slow events; the duration of the whole sequence being longer than 1 hour. This is indeed a "slow earthquake".

Perhaps one of the most complex of events is the recent Tangshan, China event. It began as a large strike-slip event. Within several seconds of the mainshock it may have triggered thrust faulting to the south of the epicenter. There is no doubt, however, that it triggered a large oblique normal event to the northeast, 15 hours after the mainshock. This event certainly contributed to the great loss of life-sustained as a result of the Tangshan earthquake sequence.

What has been learned from these studies has been applied to predict what one might expect from the next great earthquake on the San Andreas. The expectation from this study is that such an event would be a large complex event, not unlike, but perhaps larger than, the Guatemala or Mudurnu Valley events. That is to say, it will most likely consist of a series of individual events in sequence. It is also quite possible that the event could trigger associated faulting on neighboring fault systems such as those occurring in the Transverse Ranges. This has important bearing on the earthquake hazard estimation for the region.

Application of diatom analysis for the study of the history of the lakes of north-west USSR. [Translation from: Istoriya Ozer; Trudy Vses.Simp.Vilnius p1-7. Vilnius, 1970.]

During late - and post-glacial times lakes played a leading role in the development of the landscape of the North-west European part of USSR. A variety of geographic circumstances created great variegation of natural conditions in lakes and determined the composition of their diatoms. The basic stages of the development of the diatom flora of lakes are linked with general climatic changes. The deepwater regions of large periglacial lakes of the North-west USSR are inhabited by plankton diatoms of the genera Melosira and Cyclotella. Diatom analysis is further applied for the study of the history of the lakes of north-west USSR.

Que mulher é essa?: identidade, política e saúde no movimento de travestis e transexuais

O objeto desta dissertação é explorar os discursos militantes relativos à diferenciação entre as identidades coletivas de travestis e transexuais no âmbito do movimento de travestis e transexuais brasileiro e sua repercussão nas demandas e proposições de políticas públicas de saúde, mais especificamente no que tange às transformações corporais. Realizei entrevistas semi-estruturadas com ativistas reconhecidas como lideranças desse movimento, tendo como principais eixos: trajetória militante, diferenciação entre travestis e transexuais, organização do movimento, agenda política, transformações corporais e demandas relativas à saúde. Além disso, realizei etnografias em encontros gerais do movimento LGBT, assim como nos específicos de travestis e transexuais, com destaque para o XVI e XVII Encontro Nacional de Travestis e Transexuais (ENTLAIDS), realizados no Rio de Janeiro em 2009 e em Aracaju em 2010; a V Conferência Regional para América Latina e Caribe da ILGA (International Lesbian and Gay Association), realizada em Curitiba em 2009; e a I Marcha Nacional Contra a Homofobia, realizada em 19 de maio de 2010 em Brasília. A partir dos resultados das entrevistas e das etnografias, busco construir um histórico do movimento de travestis e transexuais no Brasil, no qual é possível localizar a emergência das categorias identitárias e seus conflitos. Assim, minha investigação passa pela análise da relação com categorias estigmatizantes como a prostituição e, especialmente, das capacidades de incorporação ou de apropriação de discursos médicos e psiquiátricos na construção de identidades, o que inclui a influência de fatores de classe e de acesso a serviços de saúde especializados, notoriamente o processo transexualizador no SUS. A análise das principais demandas do movimento me levou a uma relação entre políticas de reconhecimento e processos de purificação. Por fim, busco compreender o processo de construção de uma carreira militante no movimento de travestis e transexuais.

Regional variations in upper mantle structure beneath North America

Several types of seismological data, including surface wave group and phase velocities, travel times from large explosions, and teleseismic travel time anomalies, have indicated that there are significant regional variations in the upper few hundred kilometers of the mantle beneath continental areas. Body wave travel times and amplitudes from large chemical and nuclear explosions are used in this study to delineate the details of these variations beneath North America.

As a preliminary step in this study, theoretical P wave travel times, apparent velocities, and amplitudes have been calculated for a number of proposed upper mantle models, those of Gutenberg, Jeffreys, Lehman, and Lukk and Nersesov. These quantities have been calculated for both P and S waves for model CIT11GB, which is derived from surface wave dispersion data. First arrival times for all the models except that of Lukk and Nersesov are in close agreement, but the travel time curves for later arrivals are both qualitatively and quantitatively very different. For model CIT11GB, there are two large, overlapping regions of triplication of the travel time curve, produced by regions of rapid velocity increase near depths of 400 and 600 km. Throughout the distance range from 10 to 40 degrees, the later arrivals produced by these discontinuities have larger amplitudes than the first arrivals. The amplitudes of body waves, in fact, are extremely sensitive to small variations in the velocity structure, and provide a powerful tool for studying structural details.

Most of eastern North America, including the Canadian Shield has a Pn velocity of about 8.1 km/sec, with a nearly abrupt increase in compressional velocity by ~ 0.3 km/sec near at a depth varying regionally between 60 and 90 km. Variations in the structure of this part of the mantle are significant even within the Canadian Shield. The low-velocity zone is a minor feature in eastern North America and is subject to pronounced regional variations. It is 30 to 50 km thick, and occurs somewhere in the depth range from 80 to 160 km. The velocity decrease is less than 0.2 km/sec.

Consideration of the absolute amplitudes indicates that the attenuation due to anelasticity is negligible for 2 hz waves in the upper 200 km along the southeastern and southwestern margins of the Canadian Shield. For compressional waves the average Q for this region is > 3000. The amplitudes also indicate that the velocity gradient is at least 2 x 10^-3 both above and below the low-velocity zone, implying that the temperature gradient is < 4.8°C/km if the regions are chemically homogeneous.

In western North America, the low-velocity zone is a pronounced feature, extending to the base of the crust and having minimum velocities of 7.7 to 7.8 km/sec. Beneath the Colorado Plateau and Southern Rocky Mountains provinces, there is a rapid velocity increase of about 0.3 km/sec, similar to that observed in eastern North America, but near a depth of 100 km.

Complicated travel time curves observed on profiles with stations in both eastern and western North America can be explained in detail by a model taking into account the lateral variations in the structure of the low-velocity zone. These variations involve primarily the velocity within the zone and the depth to the top of the zone; the depth to the bottom is, for both regions, between 140 and 160 km.

The depth to the transition zone near 400 km also varies regionally, by about 30-40 km. These differences imply variations of 250 °C in the temperature or 6 % in the iron content of the mantle, if the phase transformation of olivine to the spinel structure is assumed responsible. The structural variations at this depth are not correlated with those at shallower depths, and follow no obvious simple pattern.

The computer programs used in this study are described in the Appendices. The program TTINV (Appendix IV) fits spherically symmetric earth models to observed travel time data. The method, described in Appendix III, resembles conventional least-square fitting, using partial derivatives of the travel time with respect to the model parameters to perturb an initial model. The usual ill-conditioned nature of least-squares techniques is avoided by a technique which minimizes both the travel time residuals and the model perturbations.

Spherically symmetric earth models, however, have been found inadequate to explain most of the observed travel times in this study. TVT4, a computer program that performs ray theory calculations for a laterally inhomogeneous earth model, is described in Appendix II. Appendix I gives a derivation of seismic ray theory for an arbitrarily inhomogeneous earth model.

Rotas migratórias, áreas de uso intenso e padrões de mergulho de tartarugas-de couro (Dermochelys coriacea) no Atlântico Sul Ocidental

As tartarugas marinhas são espécies ameaçadas, altamente migratórias que apresentam um ciclo de vida longo e uma ampla distribuição geográfica. Assim, melhorar a nossa compreensão sobre a ecologia espacial das tartarugas marinhas é essencial para a elucidação de aspectos da sua história de vida e para o desenvolvimento de medidas eficazes de conservação. Esta tese compreende um conjunto de artigos ou capítulos que visam contribuir ao conhecimento da ecologia espacial da tartaruga-de-couro, Dermochelys coriacea. Este estudo utilizou novas tecnologias como à telemetria por satélite (que proporciona um método útil para monitorar os movimentos de espécies migratórias) e um conjunto de ferramentas de geoprocessamento como abordagem metodológica que visou: examinar os movimentos e migrações da tartaruga-de-couro, identificar áreas de uso intenso e padrões espaço-temporais no uso do habitat, e integrar dados biológicos e oceanográficos para descrever as estratégias comportamentais desta espécie. Cinco tartarugas-de-couro (um subaduto, dois machos adultos e duas fêmeas adultas) foram equipadas com transmissores por satélite no Atlântico Sul Ocidental entre 2005 e 2008. Além de fornecer dados de localização geográfica os tansmissores permitiram registrar informações de mergulho tais como profundidade e duração máxima e media dos mergulhos, perfis completos de mergulhos individuais e dados de temperatura do mar. Movimentos e migrações de tartarugas-de-couro marcadas no Atlântico Sul foram documentados pela primeira vez. Alem disso, foi posível identificar áreas de uso intenso (ou alimentação) previamente desconhecidas para a espécie, assim como uma residência sazonal nestas áreas localizadas em águas tropicais e temperadas fora da costa sul-americana (19-45S). A sazonalidade dos movimentos esteve intimamente associada a processos físicos sazonais de pequena e mesoescala. Dependendo do ambiente marinho explorado, durante os períodos de residência, as tartarugas apresentaram diferentes estratégias alimentares identificadas através da análise dos padrões de mergulho.

Tipperary, by Frank Delaney: a reading of the rewriting of history of Ireland

O objetivo da presente pesquisa é o de discutir a reescrita da história da Irlanda, mais especificamente aspectos relacionados à construção da identidade nacional e de marcas da tradição, a partir da leitura do romance Tipperary, de Frank Delaney. Publicada em 2007, essa obra aborda de forma singular as querelas sobre identidade nacional, nacionalismo, passado, memória, e seus personagens principais e a trama estão significativamente ligados ao contexto político-social da história da Irlanda. Nessa reconstrução da história, o passado é revisitado através de diferentes pontos de vista. Nossa atenção estará voltada para a seleção de elementos/momentos da história do país que ganham foco na narrativa, e as possíveis repercussões deste processo. Além disso, nos concentraremos na questão das tênues fronteiras entre história e ficção, ou seja, as fronteiras pouco delimitadas entre o discurso histórico e o discurso ficcional. Na escrita da história em Tipperary, Delaney aborda questões relativas a mitos, lendas e tradições como importantes fatores de identidade nacional em uma Irlanda que emerge como uma nação independente. No romance em questão, podemos observar como história e memória se unem na jornada do protagonista, em sua empreitada de narrar a história de sua vida e de seu país

From organism to population: the role of life-history theory

The role of life-history theory in population and evolutionary analyses is outlined. In both cases general life histories can be analysed, but simpler life histories need fewer parameters for their description. The simplest case, of semelparous (breed-once-then-die) organisms, needs only three parameters: somatic growth rate, mortality rate and fecundity. This case is analysed in detail. If fecundity is fixed, population growth rate can be calculated direct from mortality rate and somatic growth rate, and isoclines on which population growth rate is constant can be drawn in a ”state space” with axes for mortality rate and somatic growth rate. In this space density-dependence is likely to result in a population trajectory from low density, when mortality rate is low and somatic growth rate is high and the population increases (positive population growth rate) to high density, after which the process reverses to return to low density. Possible effects of pollution on this system are discussed. The state-space approach allows direct population analysis of the twin effects of pollution and density on population growth rate. Evolutionary analysis uses related methods to identify likely evolutionary outcomes when an organism's genetic options are subject to trade-offs. The trade-off considered here is between somatic growth rate and mortality rate. Such a trade-off could arise because of an energy allocation trade-off if resources spent on personal defence (reducing mortality rate) are not available for somatic growth rate. The evolutionary implications of pollution acting on such a trade-off are outlined.

E se o gringo for negão ? Raça, gênero e sexualidade no Rio de Janeiro a experiência de turistas negros norte-americanos

O turismo étnico é, hoje, uma das áreas potenciais para o desenvolvimento daatividade turística nacional, quando o histórico interesse de negros norteamericanos pelo Brasil amplia-se via massificação do produto turístico de recorte identitário. Esta dissertação é o resultado da pesquisa realizada com turistas negros norte-americanos no Rio de Janeiro, que aponta para a forma com que estes turistas, enquanto consumidores, influenciam na reorganização do mercado turístico carioca por meio de demandas racializadas. Curiosamente, por trás de tais demandas desvelou-se um fundo político, marcado por papéis de gênero, que fornece instrumentos para o mapeamento inicial do turismo sexual envolvendo aquela população na Cidade Maravilhosa. A pesquisa aponta que este universo está basicamente dividido em dois grupos de turistas: o do turismo étnico, majoritariamente formado por mulheres; e o do turismo sexual, composto, com raras exceções, inteiramente por homens. Esta diferença sugere que a racialização imposta no turismo étnico seja uma exigência das mulheres americanas e indica a preocupação delas em estabelecer identidades e constatar diferenças com os negros em lugares onde eles tenham participado da história, preocupação que não atinge os turistas sexuais".

Estado e administração no Rio de Janeiro Joanino: a Secretaria do Estado de Negócios do Brasil (1808-1821)

A transmigração da Corte portuguesa para a América no ano de 1808 implicou na transferência de boa parte do aparato administrativo existente em Lisboa, de modo a permitir que o príncipe regente, D. João, pudesse governar o Império, a partir do Rio de Janeiro. Esta tese de doutorado analisa um dos órgãos então estabelecidos: a Secretaria de Estado dos Negócios do Brasil. Partindo-se do princípio de que a dominação se estabelece pela administração, pretendeu-se, pelo estudo dessa instituição, atentar para determinados aspectos que envolveram a instalação dos órgãos de poder no continente americano. Nesse sentido, duas questões nortearam a estruturação e o desenvolvimento dos capítulos deste trabalho. Em um nível mais recortado, atentou-se para um exame sobre as principais caraterísticas da estrutura administrativa dessa instituição, percebendo quem eram os seus oficiais, os cargos ocupados e os seus respectivos ordenados, de modo a compreender as especificidades, o perfil do seu corpo burocrático; bem como a importância desse grupo de funcionários na configuração de um estilo administrativo na nova Corte. No tocante a um âmbito mais amplo, inseriu-se a Secretaria de Estado dos Negócios do Brasil no quadro que a relaciona a outros órgãos de poder então existentes. A partir deste aspecto, tentou-se apreender o eixo da política do príncipe regente para o Brasil. O exame dos tópicos de ação político-administrativa dessa instituição permitiu demonstrar o sentido da administração joanina, durante os quatro primeiros anos de permanência no Rio de Janeiro.