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.

Desiccation tolerance of three moss species from continental Antarctica

Tolerance of desiccation was examined in three species of moss, Grimmia antarctici Card., Ceratodon purpureus (Hedw.) Brid. and Bryum pseudotriquetrum (Hedw.) Gaertn., Meyer et Scherb. collected from two sites of contrasting water availability in the Windmill Islands, continental Antarctica. Physiological tolerance to desiccation was measured using chlorophyll fluorescence in plugs of moss during natural drying in the laboratory. Differences in relative water content, rate of drying and the response of photosynthesis to desiccation were observed among the three species and between sites. Of the three species studied, G. antarctici showed the lowest capacity to sustain photosynthetic processes during desiccation, B. pseudotriquetrum had an intermediate response and showed the greatest plasticity and C. purpureus showed the greatest capacity to sustain photosynthesis during desiccation. These results fit well with the known distribution of the three species with G. antarctici being limited to relatively wet sites, C. purpureus being common in the driest sites and B. pseudotriquetrum showing a wide distribution between these two extremes. Levels of soluble carbohydrates were also measured in these samples following desiccation and these indicate the presence of stachyose, an oligosaccharide known to be important in desiccation tolerance in seeds, in B. pseudotriquetrum. Both gross morphology and carbohydrate content are likely to contribute to differences in desiccation tolerance of the moss species. These results indicate that if the Casey region continues to dry out, as a result of local geological uplifting or global climate change, we would expect to see not only reductions in the moss community but also changes in community composition. G. antarctici is likely to become more limited in distribution as C. purpureus and B. pseudotriquetrum expand into drying areas.

Longevity and stability of cratonic lithosphere: Insights from numerical simulations of coupled mantle convection and continental tectonics

[1] The physical conditions required to provide for the tectonic stability of cratonic crust and for the relative longevity of deep cratonic lithosphere within a dynamic, convecting mantle are explored through a suite of numerical simulations. The simulations allow chemically distinct continents to reside within the upper thermal boundary layer of a thermally convecting mantle layer. A rheologic formulation, which models both brittle and ductile behavior, is incorporated to allow for plate-like behavior and the associated subduction of oceanic lithosphere. Several mechanisms that may stabilize cratons are considered. The two most often invoked mechanisms, chemical buoyancy and/or high viscosity of cratonic root material, are found to be relatively ineffective if cratons come into contact with subduction zones. High root viscosity can provide for stability and longevity but only within a thick root limit in which the thickness of chemically distinct, high-viscosity cratonic lithosphere exceeds the thickness of old oceanic lithosphere by at least a factor of 2. This end-member implies a very thick mechanical lithosphere for cratons. A high brittle yield stress for cratonic lithosphere as a whole, relative to oceanic lithosphere, is found to be an effective and robust means for providing stability and lithospheric longevity. This mode does not require exceedingly deep strength within cratons. A high yield stress for only the crustal or mantle component of the cratonic lithosphere is found to be less effective as detachment zones can then form at the crust-mantle interface which decreases the longevity potential of cratonic roots. The degree of yield stress variations between cratonic and oceanic lithosphere required for stability and longevity can be decreased if cratons are bordered by continental lithosphere that has a relatively low yield stress, i.e., mobile belts. Simulations that combine all the mechanisms can lead to crustal stability and deep root longevity for model cratons over several mantle overturn times, but the dominant stabilizing factor remains a relatively high brittle yield stress for cratonic lithosphere.

Continental extension: From core complexes to rigid block faulting

Extension of overthickened continental crust is commonly characterized by an early core complex stage of extension followed by a later stage of crustal-scale rigid block faulting. These two stages are clearly recognized during the extensional destruction of the Alpine orogen in northeast Corsica, where rigid block faulting overprinting core complex formation eventually led to crustal separation and the formation of a new oceanic backarc basin (the Ligurian Sea). Here we investigate the geodynamic evolution of continental extension by using a novel, fully coupled thermomechanical numerical model of the continental crust. We consider that the dynamic evolution is governed by fault weakening, which is generated by the evolution of the natural-state variables (i.e., pressure, deviatoric stress, temperature, and strain rate) and their associated energy fluxes. Our results show the appearance of a detachment layer that controls the initial separation of the brittle crust on characteristic listric faults, and a core complex formation that is exhuming strongly deformed rocks of the detachment zone and relatively undeformed crustal cores. This process is followed by a transitional period, characterized by an apparent tectonic quiescence, in which deformation is not localized and energy stored in the upper crust is transferred downward and causes self-organized mobilization of the lower crust. Eventually, the entire crust ruptures on major crosscutting faults, shifting the tectonic regime from core complex formation to wholesale rigid block faulting.

Quaternary continental weathering geochronology by laser-heating Ar-40/Ar-39 analysis of supergene cryptomelane

Incremental laser-heating analyses of supergene cryptomelane clusters extracted from three distinct weathering profiles from the Mary Valley region, southeast Queensland, Australia, yield reproducible and well-defined plateau ages ranging from 346 +/- 15 to 291 +/- 14 ka (2 a). Precipitation of supergene cryptomelane in this period implies that relative humid climate prevailed in southeast Queensland from 340 to 290 ha, a result consistent with oxygen isotope analyses of marine sediments from Ocean Drilling Program Site 820 and with regional pollen and spore records. These results, the first report on the precise Ar-40/Ar-39 dating of Quaternary supergene cryptomelane, indicate that Ar-40/Ar-39 analysis of pedogenic minerals provides a reliable geochronometer for the study of Quaternary surficial processes useful in the study of soil formation rates, continental paleoclimates, and archaeological sites devoid of datable volcanic minerals.

The geochemistry of late Archaean microbial carbonate: Implications for ocean chemistry and continental erosion history

Trace element concentrations and combined Sr- and Nd-isotope compositions were determined on stromatolitic carbonates (microbialites) from the 2.52 Ga Campbellrand carbonate platform (South Africa). Shale-normalised rare earth element and yttrium patterns of the ancient samples are similar to those of modern seawater in having positive La and Y anomalies and in being depleted in light rare earth elements. In contrast to modem seawater (and microbialite proxies), the 2.52 Ga samples lack a negative Ce anomaly but possess a positive Eu anomaly. These latter trace element characteristics are interpreted to reflect anoxic deep ocean waters where, unlike today, hydrothermal Fe input was not oxidised, and scavenged and rare earth elements were not coprecipitated with Fe-oxyhydroxides. The persistence of a positive Eu anomaly in relatively shallow Campbellrand platform waters indicates a dramatic reversal from hydrothermally dominated (Archaean) to continental erosion-dominated (Phanerozoic) rare earth element flux ratio. The dominant hydrothermal input is also expressed in the initial Sr- and Nd-isotope ratios. There is collinear variation in Sr-Nd systematics, which range from primitive values (Sr-87/Sr-86 of 0.702386 and epsilon (Nd) of +2.1) to more evolved crustal ratios. Mixing calculations show that the range in trace element ratios (e.g., Y/Ho) and initial isotope ratios is not a result of contamination by trapped sediment, but that the chemical band isotopic variation reflects carbonate deposition in an environment where different water masses mixed. Calculated Nd flux ratios yield a hydrothermal input into the 2.52 Ga oceans one order of magnitude larger than continental input. Such a change in flux ratio most likely required substantially reduced continental inputs, which could, in turn, reflect a plate tectonic causation (e.g., reduced topography or expansion of epicontinental seas). Copyright (C) 2001 Elsevier Science Ltd.

Cenozoic continental weathering and its implications for the palaeoclimate: evidence from Ar-40/Ar-39 geochronology of supergene K-Mn oxides in Mt Tabor, central Queensland, Australia

One hundred and twenty-five mineral grains from 45 visually pure K-bearing Mn oxide (hollandite group) samples collected from weathering profiles in the Mt Tabor region of central Queensland, Australia, were analysed by the Ar-40/Ar-39 laser probe technique. These K-Mn oxides precipitated mainly through a process of cavity filling (direct precipitation from weathering solution), with botryoidal texture formed by micrometric mineral bands. Well-defined and reproducible plateau ages have been obtained for most samples, ranging from 27.2 +/- 0.8 to 6.8 +/- 0.5 Ma (2 sigma). Statistical analysis of the geochronological results by mixture modelling suggests an episodic mineral precipitation history, with two major peaks at 20.2 +/- 0.22 Ma and 16.5 +/- 0.17 Ma. The geochronological results, when combined with information on paragenetic relationships and mineralogical textures obtained from petrographic, scanning electron microscopy, and electron microprobe investigations, indicate that warm and humid palaeoclimatic conditions favourable to intense chemical weathering prevailed in central Queensland from late Oligocene to middle Miocene, particularly in the early Miocene. These results, in conjunction with previous and ongoing investigations in NW and eastern Queensland, suggest that most of Queensland was dominated by humid climates during the Miocene. (C) 2002 Elsevier Science BN. All rights reserved.

Say, Sismondi e o debate continental sobre os mercados

O artigo versa sobre o debate travado entre Say e Sismondi a respeito da possibilidade de saturação geral dos mercados. Na primeira seção, descreve-se o contexto histórico da Europa continental nas primeiras décadas do século 19, destacando-se as particularidades da experiência francesa de industrialização ante a liderança britânica nesse campo. A seguir, traça-se breve perfil da formação intelectual de Say a fim de apresentar sua visão sobre o funcionamento dos mercados. Na continuação, examina-se a perspectiva histórica de Sismondi em sua crítica da ortodoxia clássica, bem como sua versão para a tendência do sistema capitalista à superprodução. Nas duas últimas partes, recuperam-se os comentários recíprocos de Say e Sismondi a respeito de suas divergências teóricas sobre os limites da acumulação de capital.

Ocupação urbana em áreas de preservação permanente : o caso do manguezal da área continental de Vitória/ES

This research aims to diagnose the environmental impacts caused by the growth of urban occupations over the mangrove in the continental area of Vitória. It is justified by the gradual degradation of mangroves in Vitória that has inestimable importance to the landscape, to the environment and to the economy. With the growth of urban population in Brazil and around the world, researches like this, about environmental management, are essential to allow cities to grow more sustainably and well planned. The thesis was initially based on the study of occupations of Permanent Preservation Areas in general, with the presentation of the basic concepts and reflections, and later on territorial analysis of some protected areas and their surroundings, and the study of the empirical object, a polygon that covers urban areas and mangroves on the continental part of Vitória. The study hopes to promote a reflection and a discussion about the importance of maintenance of protected natural areas inside the cities, generating knowledge about the importance of mangrove and diagnose how it has been urbanized, protected or degraded over the years

O Brasil e o regionalismo continental frente a uma ordem mundial em transição

No artigo aborda-se a questão de em que medida as mudanças ocorridas no cenário nacional e internacional justificam que o Brasil leve adiante uma política externa de potência emergente, no nosso continente e no mundo. Para fundamentar suas conclusões, o artigo considera alguns aspectos relevantes da política mundial desde o fim da Segunda Guerra Mundial, bem como a importância de uma base regional para o exercício de uma política internacional mais assertiva e os desafios que isso nos coloca, particularmente na América do Sul.

Considerations about the recommendations of the Commission on the Limits of the Continental Shelf on the Amazon fan

In 2004, Brazil submitted to the Commission on the Limits of the Continental Shelf (CLCS) a Submission for the outer limit of the Brazilian continental shelf for its extension beyond the limits of 200 nautical miles. In 2007, the CLCS presented its recommendations, however it did not recommend four areas proposed by Brazil, the Amazon Fan among them. The objective of this study is to present the main legal and technical aspects of the controversy about the Amazon Fan, in order to evaluate some alternatives for a future submission, new or revised.

Modelização de um sistema de simulação de uma aeronave aplicado a uma plataforma electromecânica de Gough-Stewart

Esta tese apresenta o desenvolvimento de um simulador de voo, através da aplicação de um modelo dinâmico de uma aeronave e de sistemas de realidade virtual a uma plataforma electromecânica de Gough-Stewart. Para o efeito, utiliza-se o modelo da aeronave Cessna-172. Neste sentido, apresenta-se o estudo e a análise do sistema de realidade virtual utilizado, confirma-se o funcionamento do modelo matemático da aeronave em ferramenta de cálculo e apresenta-se o modelo da cinemática inversa da plataforma, cuja validação é realizada recorrendo-se a um sensor inercial. Desenvolve-se programação específica para a comunicação entre o software de cálculo numérico e a plataforma electromecânica de Gough-Stewart.

Plataforma de desenvolvimento de aplicações web orientadas a mensagens

O projecto apresentado neste relatório consiste na implementação de uma plataforma de desenvolvimento de aplicações Web orientada a mensagens, capaz de facilitar a construção de páginas Web e de automatizar o acesso a dados com base nos requisitos do problema. O foco da solução é baseado nos requisitos que forem definidos, de modo a desenvolver uma aplicação Web que responda a esses requisitos. A estratégia adoptada visa reduzir o acoplamento e aumentar a coesão dos módulos funcionais. Para reduzir o acoplamento e aumentar a coesão dos módulos funcionais separou-se a apresentação dos dados, permitindo assim que o desenvolvimento e os testes sejam realizados independentemente um do outro. O desenvolvimento é baseado em normas padronizadas (standards) de modo a facilitar a integração com outras tecnologias. Para o desenvolvimento do trabalho foi adoptada uma metodologia ágil. A gestão de projecto foi realizada com recurso a uma plataforma de gestão de projecto, que permitiu registar e organizar todas as informações e tarefas realizadas ao longo do projecto. Após a conclusão da plataforma e como caso de estudo, foi realizada uma aplicação baseada num cenário real de gestão académica (Portal Académico) para aferir os conceitos envolvidos.

Plataforma de controlo e simulação robótica

A robótica tem evoluído no sentido de criar robots e componentes cada vez mais evoluídos a preços acessíveis. Este facto permitiu que o desenvolvimento de aplicações no âmbito da robótica se tenha massificado e que a utilidade dos robots se tenha alargado a diferentes áreas de aplicação. Apesar da evolução dos robots e dos componentes para os mesmos, subsistem limitações que restringem a utilização de robots a certas aplicações, nomeadamente quando a capacidade de processamento e de memória não é suficiente para executar as aplicações. A forma para ultrapassar estas limitações tem residido essencialmente em duas abordagens: limitar as aplicações desenvolvidas à medida dos recursos disponíveis no hardware; ou estender as capacidades do robot usando recursos externos ao robot, quer por extensão do hardware do robot, quer por controlo remoto dos componentes do robot. Atendendo a esta problemática, foi desenvolvida uma plataforma que estende as capacidades dos robots segundo uma abordagem que usa o controlo remoto do robot, para capacitar as aplicações de controlo desenvolvidas de mais recursos, nomeadamente em termos de capacidade de processamento e memória. A plataforma desenvolvida disponibiliza ainda um simulador que virtualiza um campo de simulação e um robot, e simula a forma como estes interagem. O simulador é integrado na plataforma de forma semelhante aos adaptadores para robots, para que as aplicações desenvolvidas possam ser usadas quer em robots reais como no simulador.