5 resultados para Mergulho scuba

em Biblioteca Digital da Produção Intelectual da Universidade de São Paulo


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Calcium carbonate production by marine organisms is an essential process in the global budget of CO32-, and coralline reefs are the most important benthic carbonate producers. Crustose coralline algae (CCA) are well recognized as the most important carbonate builders in the tropical Brazilian continental shelf, forming structural reefs and extensive rhodolith beds. However, the distribution of CCA beds, as well as their role in CO32- mineralization in mesophotic communities and isolated carbonate banks, is still poorly known. To characterize the bottom features of several seamount summits in the Southwestern Atlantic (SWA), side-scan sonar records, remotely operated vehicle imagery, and benthic samples with mixed-gas scuba diving were acquired during two recent research cruises (March 2009 and February 2011). The tops of several seamounts within this region are relatively shallow (similar to 60 m), flat, and dominated by rhodolith beds (Vitoria, Almirante Saldanha, Davis, and Jaseur seamounts, as well as the Trindade Island shelf). On the basis of abundance, dimensions, vitality, and growth rates of CCA nodules, a mean CaCO3 production was estimated, ranging from 0.4 to 1.8 kg m(-2) y(-1) with a total production reaching 1.5 x 10(-3) Gt y(-1). Our results indicate that these SWA seamount summits provide extensive areas of shallow reef area and represent 0.3% of the world's carbonate banks. The importance of this habitat has been highly neglected, and immediate management needs must be fulfilled in the short term to ensure long-term persistence of the ecosystem services provided by these offshore carbonate realms.

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Rhodoliths are nodules of non-geniculate coralline algae that occur in shallow waters (<150 m depth) subjected to episodic disturbance. Rhodolith beds stand with kelp beds, seagrass meadows, and coralline algal reefs as one of the world's four largest macrophyte-dominated benthic communities. Geographic distribution of rhodolith beds is discontinuous, with large concentrations off Japan, Australia and the Gulf of California, as well as in the Mediterranean, North Atlantic, eastern Caribbean and Brazil. Although there are major gaps in terms of seabed habitat mapping, the largest rhodolith beds are purported to occur off Brazil, where these communities are recorded across a wide latitudinal range (2 degrees N - 27 degrees S). To quantify their extent, we carried out an inter-reefal seabed habitat survey on the Abrolhos Shelf (16 degrees 50' - 19 degrees 45'S) off eastern Brazil, and confirmed the most expansive and contiguous rhodolith bed in the world, covering about 20,900 km(2). Distribution, extent, composition and structure of this bed were assessed with side scan sonar, remotely operated vehicles, and SCUBA. The mean rate of CaCO3 production was estimated from in situ growth assays at 1.07 kg m(-2) yr(-1), with a total production rate of 0.025 Gt yr(-1), comparable to those of the world's largest biogenic CaCO3 deposits. These gigantic rhodolith beds, of areal extent equivalent to the Great Barrier Reef, Australia, are a critical, yet poorly understood component of the tropical South Atlantic Ocean. Based on the relatively high vulnerability of coralline algae to ocean acidification, these beds are likely to experience a profound restructuring in the coming decades.

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OBJETIVO: Avaliar casos de espondilolistese traumática do áxis e descrevê-los com relação à epidemiologia, classificação, déficit neurológico, tempo de consolidação e tratamento. MÉTODO: Análise retrospectiva dos prontuários dos pacientes tratado de 2002 a 2010 no IOT-HCFMUSP. Critério de inclusão: fratura da pars interarticularis de C2. RESULTADOS: 68% dos pacientes do sexo masculino com idade média de 39,1 anos. Utilizamos a classificação de Effendi, modificada por Levine-Edwards. Observamos fratura do tipo I em cinco pacientes (31,2%) e tipo II em oito pacientes (50%). Apenas três pacientes (18%) apresentaram fratura do tipo IIa. Não houve casos do tipo III. Mecanismo: Oito acidentes automobilísticos e quatro quedas. Outros mecanismos: atropelamento e mergulho. Tratamento: tração com halo craniano em onze pacientes. Foram usados gesso minerva e halo-gesso. Tempo de consolidação: 3,6 meses. Tempo de seguimento: 9,6 meses. DISCUSSÃO: Nossos resultados confirmam que fratura do enforcado apresenta bom prognóstico. Não houve necessidade de cirurgia em nenhum caso. A incidência de déficit neurológico é baixa. Nenhum paciente apresentou fratura instável, tipo III. CONCLUSÃO: Este trabalho sugere que a espondilolistese traumática do áxis continua sendo uma lesão satisfatoriamente tratada de forma conservadora na maioria dos casos. Nível de Evidência IV, Série de casos.

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Este trabalho examina os Escritos sobre a Música e os Músicos, do compositor alemão Robert Schumann, em especial as resenhas escritas entre 1834 e 1836, com vistas a identificar ecos das principais ideias sobre linguagem e tradução desenvolvidas na Alemanha entre o final do séc. XVIII e o início do séc. XIX. Os eixos escolhidos para construir essa ideia são os eixos do sujeito e do tempo perpassados pela noção de movimento. Do primeiro, destaca-se a ancoragem vertical, personalíssima, operada no interior do sujeito que transita de um sistema sígnico para outro, que traduz seus pensamentos, ou ainda que empreende a passagem de uma língua para outra. Do segundo, tem-se em conta a configuração desse mergulho num produto que desmantela as barreiras do tempo e, de um só golpe, contemporiza o passado e inclui o futuro.

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A new species of cheilostome bryozoan, Fenestrulina commensalis n. sp., was collected in December 2008 by scuba at 5–10 meters depth at Guaibura Beach, Guarapari, Espírito Santo state, southeastern Brazil. The specimen was found associated with tubes of the cerianthid Pachycerianthus sp., representing the first commensal association between a bryozoan and a tube-dwelling anemone. Fenestrulina commensalis n. sp. is the third species of the genus found in Brazilian waters; it is distinguished from other Atlantic species of Fenestrulina by its small angular orificial condyles, a single oral spine and basal anchoring rhizoids arising from abfrontal pore chambers. Morphological adaptations to encrust the tubes of cerianthids include anchoring rootlets and weakly contiguous zooids. These morphological features allow the colony the flexibility to grow around the tube and feed relatively undisturbed by silt and detritus, being raised well above the softsediment substratum in which the tube-anemone grows.