Origem e taxonomia dos Ostracodes (Crustacea) da Ilha da Trindade, Brasil

A Ilha da Trindade dista aproximadamente 1.167 km da costa, estando situada no mesmo paralelo de Vitória, capital do estado do Espírito Santo. Diversos estudos sobre a biologia de organismos da Ilha e do mar no seu entorno já foram realizados, mas nenhum sobre a fauna de ostracodes. Nas amostras analisadas foram encontrados 19 gêneros e 21 espécies de ostracodes, sendo que destes apenas Australimoosella Hartmann não era conhecido para o Oceano Atlântico. Uma diagnose para Loxoconcha bullata Hartmann, é aqui proposta e também está sendo apresentada uma descrição mais detalhada da morfologia da carapaça, uma vez que no trabalho original não há diagnose e a descrição é baseada principalmente em características das partes moles. É provável que a maioria das espécies de ostracodes da Ilha da Trindade tenha migrado da costa brasileira através dos seamounts do lineamento Vitória-Trindade. Apenas duas espécies de Caudites, uma de Auradilus e outra de Australimoosella se originaram nos oceanos Índico ou Pacífico, e tiveram sua migração para o Atlântico Oeste facilitada por esta feição geomorfológica do fundo oceânico. Um número significativo das espécies identificadas ocorre também em outras ilhas oceânicas, sendo típicas de águas rasas e quentes.

Entre a Madeira e as Antilhas: a emigração para a Ilha de Trindade: século XIX

As crises agrícolas, o sistema de colonia vigente na ilha, o excesso demográfico, a Guerra Civil entre 1820-1834, e um recrutamento militar obrigatório sem precedentes, afectaram o quotidiano dos madeirenses. Também a indústria do vinho, âncora da economia de exportação vinícola insular, entrou em declínio na segunda metade do século XIX, originando graves crises de subsistência. Todo este panorama contribuiu para uma onda emigratória dos insulares Madeirenses. Na ilha da Madeira existia uma colónia de mercadores ingleses e a ínsula era um importante interposto comercial britânico, nas rotas atlânticas das embarcações para as Índias Ocidentais. Na sequência da crise de mão-de-obra nas Antilhas Britânicas, com as proprietários a procurarem colonos para substituírem os antigos escravos, emancipados em 1834, os madeirenses eram vistos como bons candidatos, descritos como excelentes trabalhadores e artífices competentes. Surgiu, desde cedo, um sistema de aliciamento dos ilhéus para as plantações inglesas do Caribe. Em 1834-35 ocorreram as primeiras levas para a Ilha de Trindade, viagens garantidas pelo armador João de Freitas Martins e financiadas pelos proprietários da possessão inglesa. Entre 1834-47 saiu o maior número de madeirenses para a Ilha de Trindade, em toda a centúria oitocentista. O Anglicanismo praticado pelos britânicos na Ilha da Madeira era tolerado, mas não ensinado aos insulares, visto que havia uma religião de Estado em Portugal, o Catolicismo Apostólico Romano. Com a chegada do escocês Robert Kalley, em 1838, o pregador desencadeará um trabalho de propagação do protestantismo na Madeira e criará um número crescente de seguidores na ilha. Em 1846, criticado e acusado pelas autoridades civis e eclesiásticas, repudiado pela comunidade anglicana britânica, e perseguido pela população, sairá clandestinamente da Madeira. Muitos outros insulares também sairão da ilha, desembarcando a maior parte em Trindade, que estando próxima da costa da Venezuela, se tornará ilha de passagem para o vasto continente americano. Muitos ilhéus são os antepassados dos madeirenses presentes em Trindade, hoje elos de ligação com o passado, luso-descendentes activos da comunidade madeirense, a exemplo da Associação Portuguesa Primeiro de Dezembro, na história de Trindade e Tobago.

Upper-mantle seismic anisotropy from SKS splitting in the South American stable platform: A test of asthenospheric flow models beneath the lithosphere

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Size distributions of fine silicate and other particles in Masaya's volcanic plume

Direct-sampling and remote-sensing measurements were made at the crater rim of Masaya volcano (Nicaragua) to sample the aerosol plume emanating from the active vent. We report the first measurements of the size distribution of fine silicate particles (d <10 mu m) in Masaya's plume, by automated scanning electron microscopy (QEMSCAN) analysis of a particle filter. The particle size distribution was approximately lognormal with modal d similar to 1.15 mu m. The majority of these particles were found to be spherical. These particles are interpreted to be droplets of quenched magma produced by a spattering process. Compositional analyses confirm earlier reports that the fine silicate particles show a range of compositions between that of the degassing magma and nearly pure silica and that the extent of compositional variability decreases with increasing particle size. These results indicate that fine silicate particles are altered owing to reactions with acidic droplets in the plume. The emission flux of fine silicate particles was estimated as similar to 10(11) s(-1), equivalent to similar to 55 kg d(-1). Sun photometry, aerosol spectrometry, and thermal precipitation were used to determine the overall particle size distribution of the plume (0.01 < d(mu m) < 10). Sun photometry and aerosol spectrometry measurements indicate the presence of a large number of particles (assumed to be aqueous) with d similar to 1 mu m. Aerosol spectrometry measurements further show an increase in particle size as the nighttime approached. The emission flux of particles from Masaya was estimated as similar to 10(17) s(-1), equivalent to similar to 5.5 Mg d(-1) where d < 4 mu m.

Including the sub-grid scale plume rise of vegetation fires in low resolution atmospheric transport models

We describe and begin to evaluate a parameterization to include the vertical transport of hot gases and particles emitted from biomass burning in low resolution atmospheric-chemistry transport models. This sub-grid transport mechanism is simulated by embedding a 1-D cloud-resolving model with appropriate lower boundary conditions in each column of the 3-D host model. Through assimilation of remote sensing fire products, we recognize which columns have fires. Using a land use dataset appropriate fire properties are selected. The host model provides the environmental conditions, allowing the plume rise to be simulated explicitly. The derived height of the plume is then used in the source emission field of the host model to determine the effective injection height, releasing the material emitted during the flaming phase at this height. Model results are compared with CO aircraft profiles from an Amazon basin field campaign and with satellite data, showing the huge impact that this mechanism has on model performance. We also show the relative role of each main vertical transport mechanisms, shallow and deep moist convection and the pyro-convection (dry or moist) induced by vegetation fires, on the distribution of biomass burning CO emissions in the troposphere.

Exumação tectônica e evolução associada do relevo no arco de Ponta Grossa, sul-sudeste do Brasil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Gnaisse Turvo: registro de magmatismo paleoproterozoico no Terreno Paraguá - sudoeste do Cráton Amazônico, Vila Bela da Santíssima Trindade, Mato Grosso

O Gnaisse Turvo, objeto deste trabalho, corresponde a um ortognaisse polideformado exposto na região de Vila Bela da Santíssima Trindade, sudoeste do estado de Mato Grosso. Do ponto de vista geotectônico, está inserido no Cráton Amazônico e representa o embasamento paleoproterozoico do Terreno Paraguá, um dos blocos crustais que formam a Província Rondoniana-San Ignácio (1,55 - 1,3 Ga). Duas fácies foram identificadas a partir do estudo petrográfico: ¬granada-anfibólio-biotita gnaisse formada por granodioritos e ¬anfibólio-biotita gnaisse, mais abundante, de composição granodiorítica a sienogranítica. A paragênese identificada caracteriza o metamorfismo responsável por esses gnaisses como da fácies anfibolito. A análise estrutural caracteriza duas fases de deformação em nível crustal dúctil. A mais antiga (F₁) é responsável pelo desenvolvimento do bandamento gnáissico, enquanto as estruturas da fase (F₂), orientadas segundo a direção N30-60W, indicam esforços compressivos com transporte tectônico de SW para NE. A idade mínima de cristalização do Gnaisse Turvo, definida pelo método Pb-Pb em evaporação de zircão, corresponde a 1651 ± 4 Ma, sendo interpretada como idade de colocação do protólito ígneo. Os dados litogeoquímicos indicam que significativo magmatismo calcioalcalino de alto-K, metaluminoso a peraluminoso, associado à evolução de arcos magmáticos em ambiente de subducção (Orogenia Lomas Manechis - 1,7 a 1,6 Ga), dominava o período estateriano no Terreno Paraguá. A unidade ortognáissica estudada foi posteriormente retrabalhada metamórfica e tectonicamente, durante a Orogenia San Ignácio (1,4 a 1,3 Ga), que provavelmente corresponde à fase de deformação F₂.

MicroRNA Signature Obtained From the Comparison of Aggressive With Indolent Non-Hodgkin Lymphomas: Potential Prognostic Value in Mantle-Cell Lymphoma

Purpose Mantle-cell lymphoma (MCL) has a variable natural history but is incurable with current therapies. MicroRNAs (miRs) are useful in prognostic assessment of cancer. We determined an miR signature defining aggressiveness in B-cell non-Hodgkin lymphomas (NHL) and assessed whether this signature aids in MCL prognosis.MethodsWe assessed miR expression in a training set of 43 NHL cases. The miR signature was validated in 44 additional cases and examined on a training set of 119 MCL cases from four institutions in Canada. miRs significantly associated with overall survival were examined in an independent cohort of 114 MCL cases to determine association with patient outcome. miR expression was combined with current clinical prognostic factors to develop an enhanced prognostic model in patients with MCL.ResultsFourteen miRs were differentially expressed between aggressive and indolent NHL; 11 of 14 were validated in an independent set of NHL (excluding MCL). miR-127-3p and miR-615-3p were significantly associated with overall survival in the MCL training set. Their expression was validated in an independent MCL patient set. In comparison with Ki-67, expression of these miRs was more significantly associated with overall survival among patients with MCL. miR-127-3p was combined with Ki-67 to create a new prognostic model for MCL. A similar model was created with miR-615-3p and Mantle Cell Lymphoma International Prognostic Index scores.ConclusionEleven miRs are differentially expressed between aggressive and indolent NHL. Two novel miRs were associated with overall survival in MCL and were combined with clinical prognostic models to generate novel prognostic data for patients with MCL. (C) 2013 by American Society of Clinical Oncology

Mapeamento da ilha da Trindade, Atlântico Sul

The area chosen for this study is the island of Trinidade, which is located 1167 km off the Brazilian coast, in parallel Victory at 20 ° 30'S and 29 º 19'W, being the most easterly point of our continent. The isolation of oceanic island of Trinidade leaves no noticeable that she is part of a large submarine volcanic chain oriented east-west lineament known as Vitória- Trindade. Along with the island of Martin Vaz, who is Federal Territory is administered by the Navy of Brazil. Both correspond to Source alkaline volcanic islands. The area of the island of Trinidad has approximately 10 km2. Geologically consisting ankaratritic spills, spills tannbuschiticos, volcanic tuff spills analcite-ankaratrite, phonolite spills, spills nefelinite, pyroclastics, spills grazinite, tinguaitos, olivine-analcitito, calcarenite dunes and wind according to Almeida (1961). The island has its base on the ocean floor, at 5,800 m depth. It is the only place still recognizes preserved volcanic necks and plugs, as well as remnants of a volcano in Brazil. Magmatism occurred here a sodium alkali-silica subsaturated where his wrist was last 50,000 years according to Almeida (1961). It is a place with restricted access due to their distance from the coast, his contribution and hard to be an exclusive area of the Navy. On the island with peaks occur up to 620 meters high, and its rugged mountainous terrain and difficult access to very specific points, as the peak of Desire, peak Fazendinha, Monument and other points on the island. Because of its location far from the coast, its small infrastructure, difficulty of landing and restricted access by sea, the island of Trinidad offers no possibility of tourism, being a military outpost, and scientific basis of great importance, which conduct research in area of marine biology, oceanography, geology and others

The spin-orbit resonant problem including core-mantle gravitational coupling

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Caridean Shrimps Associated with the Slimy Sea Plume (Pseudopterogorigia americana) in Midsummer at Guana Island, British Virgin Islands, West Indies

Fifty-one slimy sea plumes (Pseudopterogorgia americana Gmelin, 1791) were sampled for caridean shrimps at Guana Island, British Virgin Islands, during one week in July 1992. Sam- pling depth ranged from 3-22 m. Nine species were collected: Hippolyte nicholsoni Chace, 1972; Latreutes sp.; Neopontonides chacei Heard, 1986; Perclimenes cf. patae Heard and Spotte, 1991; Periclimenes cf. pauper Holthuis, 1951; Periclimenes sp.; Pseudocoutierea antillensis Chace, 1972; Tozeuma cf. cornutum Milne Edwards, 1881; and Trachycaris rugosa (Bate, 1888). A total of 1,418 specimens (including fragments) was obtained. The number of shrimp species per gorgonian ranged from 1-5; one gorgonian harbored 156 shrimps. The two predominant species, N. chacei and H. nicholsoni, occupy different mean depths (12.6 and 8.2 m, respectively). Sexual dimorphism assessed with Mann-Whitney U-tests was not apparent in the specimens of N. chacei (P > 0.05), but females of H. nicholsoni were significantly larger than males (P < 0.001). Minimum carapace length (CL, the tip of the rostrum to the posterior dorsal margin of the carapace) at which male N. chacei acquire a single appendix masculina spine is 1.25 mm; male H. nicholsoni can acquire a single spine at 0.9 mm CL. Histological sections of male N. chacei showed that shrimp with 0 or 1 spine are least likely to be mature. Female N. chacei can become ovigerous at 1.9 mm CL and female H. nicholsoni at 1.2 mm CL. The taxonomic status of 5 of the 9 species collected is uncertain.