Composition of sediments and cores from DSDP Legs 54 and 61-63

The monograph gives results of studies of sediments and rocks collected from D/S Glomar Challenger in the Pacific Ocean. These studies have been based on the lithological facial analysis applied for the first time for identificating genesis of ocean sediments. These results include new ideas on formation of the Earth's sedimentary cover and can be used for constructing regional and global schemes of ocean paleogeography, reconstructing some structures, correlating sedimentation on continents and in oceans, estimating perspectives of oil- and gas-bearing deposits and ore formation. The monograph also gives the first petrographic classification of organic matter in black shales.

Chemical and mineral compositions of sedimentary deposits and magmatic rocks from DSDP Legs 41, 45, 48, and 49

This collective monography by a group of lithologists from the Geological Institute of the USSR Academy of Sciences summarizes materials of the Deep-Sea Drilling Project from the Atlantic Ocean. It gives results of processing materials on the sequences drilled during DSDP Legs 41, 45, 48 and 49. These studies were based on lithological-facial analysis combined with detailed mineralogical-petrographic description. Its chapters give a number of ideas on formation of the Earth sedimentary cover, which can be used for compilation of regional and global schemes of ocean paleogeography, reconstruction of history of some structures in the World Ocean, correlation between sedimentary processes on continents and in oceans, estimation of perspectives for oil and gas fields and ore formation.

Geochemistry of serpentenites from DSDP Hole 84-566C

We studied a unique chrysotile-antigorite serpentinite, drilled on Deep Sea Drilling Project Leg 84 (Site 566) in the Guatemala forearc. Our in situ major and trace element data provide new constraints on possible reactions and associated trace element mobilisation during shallow serpentinite subduction. Chrysotile of the studied serpentinite, formed by the hydration of an upper mantle peridotite precursor, is partially replaced by antigorite (alone) which also occurs in 0.5 mm wide unoriented veins crosscutting the rock. Based on textural relationships and the P-T-X stability of the rock forming phases, the replacement of chrysotile by antigorite occurred at T < 300 °C, due to interaction between the chrysotile-serpentinite and an aqueous fluid. A comparison of the chemical compositions of reactant and product phases reveals that about 90% of the Cl, more than 80% of the B and about 50% of the Sr hosted originally by chrysotile was lost during fluid-assisted chrysotile-to-antigorite transformation and accompanying partial dehydration, and documents the much lower affinity of antigorite for trace element uptake than that of chrysotile. The fluid-assisted chrysotile-to-antigorite transformation and associated trace element loss documented here can occur in the shallow (< 30 km) region of subduction zones. This transformation decreases notably the Cl and B inventory of subducting serpentinites, which are regarded as one of the most important carriers of these elements into subduction zones. The evolution of serpentinites during initial subduction stages thus appears to be critical in the recycling of specific trace elements such as B or Cl from forearc to subarc depths.

Geochemistry of selected minerals at DSDP Leg 65 Holes

The majority of the basalts drilled on Leg 65 in the Gulf of California are aphyric to sparsely phyric massive flows ranging in average thickness between 5 meters in the upper part of the sections in Holes 483 and 483B, where they are interlayered with sediment, and 14 meters in Hole 485A, where interlayered sediments constitute more than half of the section. Massive flows interlayered with pillows are generally less than 4 meters thick. The pillow lavas recovered are more phyric (up to 15 modal%) and contain two to three generations of plagioclase and olivine ± clinopyroxene. Plagioclase generally exceeds 60% of any given phenocryst assemblage. Resorbed olivine, clinopyroxene, and plagioclase megacrysts may reflect a high-pressure stage, the phenocrysts crystallizing in the main magma chamber and the skeletal microphenocrysts in dikes. Precise measurements of length/width ratios of different phenocryst types and compositions show low aspect ratios and large crystal volumes for early crystals and high ratios and low volumes for late crystals grown under strong undercooling conditions. The minerals examined show wide ranges in composition: in particular, plagioclase ranges from An92 to An36; clinopyroxene ranges from Ca41Mg51Fe8 in the cores of phenocrysts to Ca40**36 Mg45**49Fe15**20 in the groundmass; and olivine ranges from Fo86 to Fo81. The wide range in mineral compositions, together with evidence of disequilibrium based on textures and comparisons of glass and mineral compositions, indicate complex crystallization histories involving both polybaric crystal fractionation and magma mixing.

Composition of bottom sediments from the Guinea Basin

Geomorphology of the Guinea Basin is described along with sediments from cores collected on the abyssal plain, within the abyssal hill zone, and in the eastern part of the Chain Fracture Zone. Stratigraphic differentiation of deep-sea sediments was based on diatom analysis, geochemical and lithological data. Holocene and Pleistocene were identified by these criteria. The lower boundary of Holocene is was found from a marked decrease in CaCO3 concentration and total diatom count. Mineral and chemical compositions are given for coarse silt fraction of various Late Pleistocene sediments. It is shown that this facial complex is determined by tectonic position of the Guinea Basin.

Automation; economic implications and impact upon collective bargaining.

Includes bibliographies.

Unity Committee meeting /

Deals with a proposed merger with the International Woodworkers of America.

Record of pre-conference of the Pacific Coast local unions affiliated with the International Brotherhood of Pulp, Sufphite & Papermill Workers, the International Brotherhood of Paper Makers, May 21, 1942 to May 25, 1942, Portland Oregon /

"O.E.U., union label, # 16821."

Avaliação da anchoita (engraulis anchoita) salgada maturada acondicionada em atmosfera modificada

A anchoita foi capturada e acondicionada a bordo sob-resfriamento a 0°C com gelo em escamas. Após o recebimento, o pescado foi processado na forma salgado-maturado. Após a maturação foram processadas e embaladas em sacos de polietileno e armazenadas sob-refrigeração a 5°C durante 84 dias. As amostras foram divididas grupos: (1) sob pressão atmosfera normal, (2) vácuo, (3) atmosfera modificada com 50% CO2 + 20% O2 + 30% N2 e (4) 60% CO2 + 10% O2 + 30% N2, em embalagens de polietileno e aluminizadas, termo-seladas e armazenadas sob-refrigeração a 5°C. Os valores de textura tiveram uma redução de 2277,8 N (Kg.m/s2 ) para 821,90 N (Kg.m/s2 ) para o tratamento controle. A qualidade inicial do pescado atendeu aos padrões legais vigentes, apresentando ausência Salmonella sp e enumerações aceitáveis aos padrões de Staphylococcus coagulase positiva, Clostridium sulfito redutores, coliforme totais e a 45ºC. Com relação ao pH, houve diferenças significativas durante o tempo de processamento (p<0,05), o valor passou de 6,3 (início) para 6,4 (final). Com relação aos resultados correspondentes aos parâmetros L*, a* e b* (cor), em todos os tratamentos e ao longo do tempo de processamento (ambas as embalagens), ocorreram diferenças significativas (p<0,05). Os valores de L* variaram de 34,80 para 18,00 (controle) 23,00 (vácuo), 20,21 (T3) e 22,00 (T4) embalagens de polietileno. Nas embalagens de alumínio os valores de L* variaram de 34,00 para 25,00 (controle), 29,00(vácuo), 22,10 (T3) e 26,00 (T4).

Avaliação de alguns parâmetros da qualidade da anchoita (Engraulis anchoita) enlatada em óleo de girassol e em molho de tomate

O consumo de pescado no Brasil cresceu 40% nos últimos 7 anos passando de 6,46 para 9,03 kg/habitante/ano, valor que se aproxima do recomendado pela Organização Mundial de Saúde. A razão está relacionada com a subutilização de determinadas espécies e a falta de diversificação da indústria processadora para a produção de alimentos com maior valor agregado. Considerando o esgotamento de determinadas espécies com a utilização da sobrepesca, é possível o emprego da anchoita na forma de conservas através da utilização de meios de cobertura como molho de tomate e óleo comestível. Este trabalho teve como objetivo elaborar conservas de anchoita (Engraulis anchoita) com a utilização de 2 meios de cobertura: molho de tomate e óleo de girassol, submetidas a tempos de salmouragem diferenciados, 2 e 5 min e com o emprego ou não de pré-cozimento. De acordo com os padrões estabelecidos, as amostras de pescado fresco utilizadas para a execução dos enlatados apresentaram resultados físico químicos adequados comprovando o frescor do pescado envolvido no processo, ou sejam: 16,29 mg/100 g amostra para N-BVT, 7,90 mg/100 g amostra para N-TMA e pH 6,5. As conservas em molho de tomate submetidas a operação de salmouragem durante 2 min, com e sem pré-cozimento apresentaram, respectivamente, 16,57 e 16,24% proteínas, 3,94 e 4,66% lipídios, 73,0 e 73,28% umidade, 3,22 e 3,67% cinzas, 0,17 e 0,19% de cloretos (NaCl). As conservas com molho de tomate, utilizando anchoita eviscerada salmourada por 5 min, com e sem pré-cozimento, apresentaram respectivamente, 15,94 e 15,31% proteínas, 3,15 e 4,90 lipídios%, 73,70 e 73,98% umidade, 3,80 e 4,10% cinzas, 0,21 e 0,24% cloretos (NaCl). Para as conservas de anchoita em óleo de girassol, utilizando tempo de salmouragem de 2 min, com e sem pré-cozimento, apresentaram 16,97 e 16,76% proteínas, 7,68 e 5,70% lipídios, 65,87 e 68,74% umidade, 3,16 e 3,28% cinzas, 0,10 e 0,12% cloretos (NaCl), respectivamente. As conservas utilizando o pescado previamente submetido a salmouragem por 5 min e posteriormente enlatado com a adição de óleo de girassol, com e sem pré-cozimento apresentaram respectivamente, 15,97 e 15,89% proteínas, 7,91 e 5,19% lipídios, 66,26 e 68,23% umidade, 3,78 e 3,87% cinzas, 0,13 e 0,21% NaCl. As análises microbiológicas das conservas submetidas aos diferentes tratamentos mostraram ausência de Salmonella spp, Staphylococcus coagulase positiva e Clostridium sulfito-redutor, resultados estes, de acordo com o estabelecido pela legislação higiênico-sanitária brasileira. Nos testes de esterilidade comercial não foram constatadas alterações visíveis nos enlatados submetidos a incubação por 5 dias a 36 ± 1°C (determinação de micro-organismos aeróbios viáveis) e a 7-10 dias a 55 ± 1°C (termófilos). Considerando as quantidades de pescado enlatado (80, 90 e 100g), o rendimento para todas as amostras apresentaram, no mínimo, 50% de pescado em relação ao peso líquido. A avaliação sensorial realizada por teste de ordenação para a avaliação da preferência não apresentou diferenças significativas entre as amostras.

Estudo da imobilização das proteases aspárticas da flor de Cynara cardunculus L. Reologia da coalhada

Mestrado em Biotecnologia, Faculdade de Engenharia de Recursos Naturais, Univ. do Algarve, 2005

Avaliação da biodessulfurização de 4-metildibenzotiofeno por Rhodococus rhodochrous (NRRL B-2149)

Crude oil has between 0.04 up to 5% of sulphur, the higher the oil the higher the sulphur levels. Sulphur usually gives problems such as corrosion in refinery, and once burnt produces SO2 that goes to atmosphere. This work aim to investigate the capacity of Rhodococcus rhodochrous (NRRL B-2149) to metabolize the model compound 4-methyldibenzotiophene (4-MDBT), to remove the sulphur and transform it in 2-hydroxybiphenyl (2-HBF) and sulphite using the 4S pathway. Kynetic runs were carried out in shaker at 120 rpm and 32°C. Samples were taken every 12h to assay substrate consume as well as cells production using HPLC. Results showed that R. rhodochrous NRRL B-2149 can use the 4S pathway in order to remove sulphur without change the carbon chain of the molecule as well as that cells and 4-MDBT affects the product formation. The production of 2-hydroxybiphenyl has interest for industry once it is a potent biocide. However, evaluation is necessary in order to obtain better results compatible with industry needs