Glikia régina / Paul Gad et Aleco Ahiadis, duo voc. [acc. mandolines et p]. I accro thalassia / Paul Gad, Aleco Ahiadis, duo voc. [acc. instr.]

[Traditions. Europe. Grèce]

Les natures mortes de Paul Gauguin: une production picturale méconnue

Gauguin's first attempts at still-life painting, around 1875, followed the Dutch tradition, influenced mainly by Manet's palette. But he did take occasional liberties in depicting flowers with more fluid colour and dynamic backgrounds. From 1879 his style shows the influence of the Impressionists: Pissarro in the landscapes and Degas in the composition of his still-lifes. He was also open to the new trends which were developing among artists in Paris and applied them in his paintings, using still-lifes as his main means for testing them. He did not escape the contemporary fascination with Japonism, and even experimented briefly with Pointillism in Still Life with Horse's Head. His stays in Britain between 1886 and 1890 correspond to an extremely rich and innovative period for him, in which still-lifes served for increasing experimentation. "Fête Gloanec" and Three Puppies reflect his preoccupations: rejection of perspective, use of areas of flat colour, and mixed styles. These pictures amount to an aesthetic manifesto; many of them are also imbued with strong symbolism, as in the Portrait of Meyer de Haan, which is a melancholic reflection on the fall of man. In Still-Life with Japanese Print, frail blue flowers seem to come out of the head of the artist-martyr, a pure product of the painter's "restless imagination". Thus Gauguin showed that art is an "abstraction" through a genre which was reputed to lend itself with difficulty to anything other than mimesis. Although he moved away from still-life after 1890, Gauguin is one of the first artists to radically renew its role and the status of still-life at the end of the 19th century, well before the Fauvists and Cubists.

Mi nostalgia / Paul Gad et Aleco Ahiadis, duo voc. [acc. mandolines et p]. Coquetta / Paul Gad, chant [acc. choeur et instr.]

[Traditions. Europe. Grèce]

Yasmina / Paul Gad [acc. mandolines et p]. Tha fio corri sta xéna / Paul Gad, chant [acc. choeur et instr.]

[Traditions. Europe. Grèce]

Mana / Paul Gad [acc. mandolines et p]. Stone affro tis thallassass : yalo… yalo… / Paul Gad, chant [acc. choeur et instr.]

[Traditions. Europe. Grèce]

Aghapi qué filia / Paul Gad, chant ; M. Angelo. R, p. Thimasse / Paul Gad, chant [acc. instr.]

[Traditions. Europe. Grèce]

Espassess ta piatta ; Osso yirizi i sphera / Paul Gad, chant [acc. choeur et instr.]

[Traditions. Europe. Grèce]

Idha Mattia / Paul Gad, chant ; M. Angelo. R, p. Yatti pino / Paul Gad, Aleco Ahiadis, duo voc. [acc. instr.]

[Traditions. Europe. Grèce]

I modhistroulla / Paul Gad, chant [acc. choeur et instr.]. Sou ippa mou ippess / Paul Gad, chant ; M. Angelo. R, p

[Traditions. Europe. Grèce]

Paul Otlet: um pioneiro da organização das redes mundiais de tratamento e difusão da informação registrada

Estudo da obra de Paul Otlet, com ênfase no Princípio Monográfico, uma de suas principais contribuições para a constituição da documentação e da ciência da informação e predecessora da idéia de hipertexto. Sua obra Traité de Documentation: le livre sur le livre: théorie et pratique, publicada em 1934, antecipa muitas das idéias hoje adotadas sobre a organização de redes internacionais de cooperação para tratamento e troca de informações documentadas. Nessa obra, Otlet define o campo da documentação e sistematiza teorias, métodos e técnicas para organizar o conhecimento registrado e distribuí-lo. Revisitar a obra de Otlet é fundamental para compreender muitos aspectos teóricos, metodológicos e epistemológicos que construíram o campo da documentação e da ciência da informação.

Monitoring detrital input and resuspension effects on sediment trap material using mineralogy and stable isotopes (δ18O and δ13C): the case of Lake Neuchatel (Switzerland)

Isotopic analyses on bulk carbonates are considered a useful tool for palaeoclimatic reconstruction assuming calcite precipitation occurring at oxygen isotope equilibrium with local water and detrital carbonate input being absent or insignificant. We present results from Lake Neuchatel (western Switzerland) that demonstrate equilibrium precipitation of calcite, except during high productivity periods, and the presence of detrital and resuspended calcite. Mineralogy, geochemistry and stable isotope values of Lake Neuchatel trap sediments and adjacent rivers suspension were studied. Mineralogy of suspended matter in the major inflowing rivers documents an important contribution of detrital carbonates, predominantly calcite with minor amounts of dolomite and ankerite. Using mineralogical data, the quantity of allochthonous calcite can be estimated by comparing the ratio ankerite + dolomite/calcite + ankerite + dolomite in the inflowing rivers and in the traps. Material taken from sediment traps shows an evolution from practically pure endogenic calcite in summer (10-20% detrital material) to higher percentages of detrital material in winter (up to 20-40%). Reflecting these mineralogical variations, delta(13)C and delta(18)O values of calcite from sediment traps are more negative in summer than in winter times. Since no significant variations in isotopic composition of lake water were detected over one year, factors controlling oxygen isotopic composition of calcite in sediment traps are the precipitation temperature, and the percentage of resuspended and detrital calcite. Samples taken close to the river inflow generally have higher delta values than the others, confirming detrital influence. SEM and isotopic studies on different size fractions (<2, 2-6, 6-20, 20-60, >60 mu m) of winter and summer samples allowed the recognition of resuspension and to separate new endogenic calcite from detrital calcite. Fractions >60 and (2 mu m have the highest percentage of detritus, Fractions 2-6 and 6-20 mu m are typical for the new endogenic calcite in summer, as given by calculations assuming isotopic equilibrium with local water. In winter such fractions show similar values than in summer, indicating resuspension. Using the isotopic composition of sediment traps material and of different size fractions, as well as the isotopic composition of lake water, the water temperature measurements and mineralogy, we re-evaluated the bulk carbonate potential for palaeoclimatic reconstruction in the presence of detrital and re-suspended calcite. This re-evaluation leads to the following conclusion: (1) the endogenic signal can be amplified by applying a particle-size separation, once the size of endogenic calcite is known from SEM study; (2) resuspended calcite does not alter the endogenic signal, but it lowers the time resolution; (3) detrital input decreases at increasing distances from the source, and it modifies the isotopic signal only when very abundant; (4) influence of detrital calcite on bulk sediment isotopic composition can be calculated. (C) 1998 Elsevier Science B.V. All rights reserved.