Genetic structure of Mycosphaerella fijiensis populations from Australia, Papua New Guinea and the Pacific Islands

Single-copy restriction fragment length polymorphism (RFLP) markers were used to determine the genetic structure of Mycosphaerella fijiensis, the cause of black leaf streak (black Sigatoka) disease of banana and plantain, in the Torres Strait, Papua New Guinea (PNG), and the Pacific Islands. A moderate level of genetic variation was observed in all populations with genotypic diversity values of 60-78% of the theoretical maximum, and gene diversity (H) values between 0.269 and 0.336. All populations were at gametic equilibrium, and with the high level of genotypic diversity observed this indicated that sexual reproduction has a major role in the genetic structure of the M. fijiensis populations examined. Population differentiation was tested on several hierarchical scales. No evidence of population differentiation was observed between sites on Mer Island. A moderate level of population differentiation was observed within the Torres Strait, between Badu and Mer Islands (F-ST = 0.097). On a regional scale, the greatest differentiation was found between the populations of the Torres Strait and the Pacific. Populations from these regions were more closely related to the PNG population than to each other, suggesting they were founded in separate events from the same population.

Performing race, culture, and gender in an Indigenous Australian women's music and dance classroom

One perpetual concern among Indigenous Australian peoples is authenticity of voice. Who has the right to speak for, and to make representations about, the knowledges and cultures of Indigenous Australian peoples? Whose voice is more authentic, and what happens to these ways of knowing when they make the journey into mainstream Western academic classrooms? In this paper, I examine these questions within the politics of “doing” Indigenous Australian studies by focusing on my own experiences as a lecturer in the Aboriginal and Torres Strait Islander Studies Unit at the University of Queensland. My findings suggest that representation is a matter of problematizing positionality and, from a pedagogical standpoint, being aware of, and willing to address, the ways in which power, authority, and voice are performed and negotiated as teachers and learners of Indigenous Australian studies.

Editorial

The year 2003 marks the 30th anniversary of The Australian Journal of Indigenous Education (AJIE) and coincides with the re-launching of the journal as a peer reviewed research journal.Beginning life in 1973 as The Aboriginal Child at School, AJIE has played a vital role in raising awareness of educational issues for Aboriginal and Torres Strait Islander peoples; fostering debate amongst researchers, government representatives and community groups; and sharing stories of success between both Indigenous and non- Indigenous practitioners positioned in the broad area of Aboriginal and Torres Strait Islander education. The dialogue which has taken place in AJIE over the past 30 years maps out the social, political and cultural history of Indigenous education in Australia, and draws attention to the shifting paradigms,problems and practical outcomes.

Editorial: Celebrating 30 years - 1973-2003

In 2003 The Australian Journal of Indigenous Education celebrates its 30th anniversary. Beginning in 1973 as The Aboriginal Child at School, the journal was a practical response to a recommendation made at the National Workshop on Aboriginal Education held in May 1971 “that a periodical publication be commenced to provide a medium for the exchange of ideas and developments in the teaching of Aborigines, for the examination of practical implications of research findings and for the recording of Aboriginal achievements” (Watts, 1973, p. 2). Funded by the Department of Aboriginal Affairs in Canberra and housed in the Department of Education and later the Aboriginal and Torres Strait Islander Studies Unit at the University of Queensland, The Aboriginal Child at School was published at two monthly intervals. It aimed to provide a medium whereby teachers in the field of Aboriginal and Torres Strait Islander education could share their thinking and their strategies for successful teaching and thereby enter into a meaningful and productive dialogue with one another (Watts, 1973, p. 2). An overarching concern of the journal was to improve and optimise children’s development and the types of pedagogies employed to provide challenging and rewarding learning experiences for Aboriginal and Torres Strait Islander children.The journal was enthusiastically embraced by a broad range of professionals and proved to be a useful resource for both experienced and beginning teachers, particularly in the primary sector.

Tsunami vulnerability assessment of Casablanca-Morocco using numerical modelling and GIS tools

Earthquakes and tsunamis along Morocco's coasts have been reported since historical times. The threat posed by tsunamis must be included in coastal risk studies. This study focuses on the tsunami impact and vulnerability assessment of the Casablanca harbour and surrounding area using a combination of tsunami inundation numerical modelling, field survey data and geographic information system. The tsunami scenario used here is compatible with the 1755 Lisbon event that we considered to be the worst case tsunami scenario. Hydrodynamic modelling was performed with an adapted version of the Cornell Multigrid Coupled Tsunami Model from Cornell University. The simulation covers the eastern domain of the Azores-Gibraltar fracture zone corresponding to the largest tsunamigenic area in the North Atlantic. The proposed vulnerability model attempts to provide an insight into the tsunami vulnerability of building stock. Results in the form of a vulnerability map will be useful for decision makers and local authorities in preventing the community resiliency for tsunami hazards.

Design of a sea-level tsunami detection network for the Gulf of Cadiz

The devastating impact of the Sumatra tsunami of 26 December 2004, raised the question for scientists of how to forecast a tsunami threat. In 2005, the IOC-UNESCO XXIII assembly decided to implement a global tsunami warning system to cover the regions that were not yet protected, namely the Indian Ocean, the Caribbean and the North East Atlantic, the Mediterranean and connected seas (the NEAM region). Within NEAM, the Gulf of Cadiz is the more sensitive area, with an important record of devastating historical events. The objective of this paper is to present a preliminary design for a reliable tsunami detection network for the Gulf of Cadiz, based on a network of sea-level observatories. The tsunamigenic potential of this region has been revised in order to define the active tectonic structures. Tsunami hydrodynamic modeling and GIS technology have been used to identify the appropriate locations for the minimum number of sea-level stations. Results show that 3 tsunameters are required as the minimum number of stations necessary to assure an acceptable protection to the large coastal population in the Gulf of Cadiz. In addition, 29 tide gauge stations could be necessary to fully assess the effects of a tsunami along the affected coasts of Portugal, Spain and Morocco.

Auxílios de Estado sob a forma fiscal: O caso Açores - Proc. C-88/03

Mestrado em Fiscalidade

Tsunamigenic earthquakes in the Gulf of Cadiz: fault model and recurrence

The Gulf of Cadiz, as part of the Azores-Gibraltar plate boundary, is recognized as a potential source of big earthquakes and tsunamis that may affect the bordering countries, as occurred on 1 November 1755. Preparing for the future, Portugal is establishing a national tsunami warning system in which the threat caused by any large-magnitude earthquake in the area is estimated from a comprehensive database of scenarios. In this paper we summarize the knowledge about the active tectonics in the Gulf of Cadiz and integrate the available seismological information in order to propose the generation model of destructive tsunamis to be applied in tsunami warnings. The fault model derived is then used to estimate the recurrence of large earthquakes using the fault slip rates obtained by Cunha et al. (2012) from thin-sheet neotectonic modelling. Finally we evaluate the consistency of seismicity rates derived from historical and instrumental catalogues with the convergence rates between Eurasia and Nubia given by plate kinematic models.

NEE: inclusão e relação escola-família

Dissertação apresentada à Escola Superior de Educação de Lisboa para obtenção do grau de Mestre em Educação Especial - Especialidade Problemas de Cognição e Multideficiência

Demonstração dos fluxos de caixa: a análise da importância no relato financeiro

Mestrado em Contabilidade Internacional

A Bacia Lusitaniana: estratigrafia, paleogeografia e tectónica

A Bacia Lusitaniana é uma bacia sedimentar que se desenvolveu na Margem Ocidental Ibérica (MOI) durante parte do Mesozóico, e a sua dinâmica enquadra-se no contexto da fragmentação da Pangeia, mais especificamente da abertura do Atlântico Norte. Caracteriza-se como uma bacia distensiva, pertencente a uma margem continental do tipo atlântico de rift não vulcânica. Ocupa mais de 20 000 km2 na parte central da MOI, alongando-se por cerca de 200 km segundo direcção aproximada NNW-SSE e por mais de 100 km na direcção perpendicular; cerca de 2/3 aflora na área continental emersa e a restante área, encontra-se imersa, na plataforma continental. Trata-se da única bacia das margens do Atlântico Norte com extensa exposição superficial, pelo que tem atraído nas últimas décadas um número considerável de geólogos, especialistas de variados domínios, para a realização de trabalhos de investigação integrados em equipas nacionais e internacionais, muitos delas ligadas à indústria do petróleo. Ao longo das várias décadas de prospecção foram efectuadas cerca de 50 sondagens profundas e mais de 37 000 km de perfis sísmicos de reflexão 2D. A evolução tectónica da Bacia Lusitaniana foi condicionada por falhas que se formaram durante o episódio de gracturação tardi-varisca aproximadamente entre os 300 e os 280 M.a. Este episódio tardi-orogénico resulta de imposição de regime de cisalhamento direito à micro-placa ibérica nos seus paleolimites E-W setentrional e meridional, dos quais resultariam as falhas de desligamento esquerdo de direcção aproximada NNE-SSW a NE-SW. Outras falhas orogénicas variscas de orientação N-S (falha de Porto-Tomar) e NW-SE foram também importantes na estruturação da Bacia Lusitaniana, como adiante ficará patente. Esta é a herança tectónica da Bacia que levou, durante o estiramento crostal mesozóico, à formação do conjunto de bacias marginais na MOI. A evolução tectónica da Bacia Lusitaniana está condicionada pela distensão mesozóica relacionada com a abertura do Atlântico Norte, na proximidade do Atlântico Central, domínios oceânicos distintos separados pela Zona de Falha de Açores-Gibraltar (ZFAG). Esta constitui limite transformante entre placas, que numa fase inicial do ciclo alpino, ou seja da rotura da Pangea, separou dois grandes continentes, a Laurásia a Norte e a Gondwana a Sul. A Ibéria localiza-se, assim, durante o Mesozóico, numa posição de charneira, cuja actividade está também relacionada com a evolução dos limites de placa: i) a sul, entre África e a Eurásia, limite transcorrente ao longo da Zona de Falha de Açores Gibraltar e ii) a Oeste, entre a Ibéria e a Terra Nova limite divergente associado à evolução do Atlântico. Nas fases iniciais de desenvolvimento do proto-Atlântico norte, desde o Triásico, a Ibéria encontra-se solidária ao continente norte-americano, mas por estiramento litosférico progressivo, acabará por ocorrer rotura crostal e consequente oceanização no final do Cretácico Inf. Este conjunto de interações será assim responsável por uma evolução também complexa da Margem Ocidental da Ibéria, onde se encontra a Bacia Lusitaniana, bacia intracratónica, interna, separada de uma zona externa por um relevo estrutural, o horst da Berlenga. Desta forma, alguns processos complexos, uns exógenos, outros de clara influência endógena, vão ficando registados na Bacia. Referimo-nos a episódios de inversão tectónica precoce, a um magmatismo muito ténue - para todos os efeitos podendo-se considerar como uma margem continental de rift, não vulcânica - e a diapirismo que se encontra registado na sua área geográfica.