Espaços Ibero-Americanos

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Juventude e coessao social na Ibero-América: um modelo a ser construído

Incluye Bibliografía

Sociabilidade e política: Oliveira Lima, Joaquim Nabuco e o Pan-Americanismo (1899-1907)

Pós-graduação em História - FCHS

A construção do pan-americanismo na revista Em Guarda: o olhar americano pela defesa das Américas (1941-1946)

Pós-graduação em História - FCLAS

A defesa do pan-americanismo nas páginas de Américas: (1949-1968)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

A construção do pan-americanismo na revista em guarda: o olhar norte-americano pela defesa das Américas (1941-1946)

O presente artigo discorre sobre o período de divulgação da revista Em Guarda (1941-1946). No decorrer de sua publicação, os norte-americanos apareciam como modelo de sociedade (político, cultural e social), enquanto aos latino-americanos cabia o papel de fornecer matérias-primas para a fabricação de produtos voltados à guerra. Pretendo discutir as estratégias adotadas pelo mensário na construção do discurso de união interamericana sob a ótica dos Estados Unidos. Desse modo, surgem novas possibilidades para o estudo das relações entre Brasil- Estados Unidos, em particular do pan-americanismo.

Televisão digital: matrizes teóricas no espaço Ibero-Americano : o caso do México, da Colômbia e da Costa Rica

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Diálogos entre Mário de Andrade e Francisco Curt Lange: nacionalismo e americanismo musicais nas décadas de 1930 e 1940

Pós-graduação em História - FCLAS

Americanismo e iberismo: a questão do atraso na América Latina

This article aims to analyze some aspects os interpretations of Brazil listed in Tavares Bastos, André Rebouças and Oliveira Viana. In this context, the debate on the concepts of americanism and “iberismo” become fundamental to the analysis of the development of the modernization process which it lasted from the second half of the nineteenth century to the mid of the twenty century.

Moliendo en ibero, moliendo en griego: aculturación y resistentcia tecnológica en el Mediterráneo occidental durante la Edad del Hierro

[ES] Durante el primer milenio a.C., y especialmente a partir de aproximadamente el siglo V a.C., los sistemas de molienda experimentan una serie de innovaciones técnicas de importancia crucial en la historia de esta tecnología. Dos de las más importantes son el molino rotatorio (manual e ibérico de palanca) y el molino de Olinto. Cada uno pertenece a una tradición: el primero a la cultura ibérica y el segundo a la griega clásica. En este artículo se analizan los datos existentes sobre el origen, evolución y expansión de cada uno de ellos, manifestándose el escaso intercambio tecnológico entre estas dos culturas en lo referente a la molienda del cereal.

Gómez Martínez, José Luis (ed.). Anuario bibliográfico de historia del pensamiento ibero e iberoamericano 1986. EE.UU., The University of Georgia, 1989, 136 p.

Fil: Jalif de Bertranou, Clara Alicia.

Americanismo y europeismo en Alberdi y Groussac

Fil: Pró, Diego F.. Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto de Filosofía Argentina y Americana

Siliceous fossils in sediments of the Ibero-Moroccan shelf and adjacent deep sea plains

Siliceous skeletons were investigated in two core profiles (9 cores), one off Cap de Sines, Portugal and the other off Cap de Mazagan, Morocco. Total number of skeletons was determined per gram of dried sediment at different core depths of the fraction >21 µ. Results are compared with a core profile from the Arabian Sea. Diatoms are of four groups: (A) marine-planktonic, B) marine-benthic, (C) freshwater and (D) Tertiary species (Trinacria e.g.). Species from groups (B), (C) and (D) are redeposited in all cores taken at a water depth of greater than 100 m. Small numbers of Silicoflagellates and Radiolarians were found throughout the cores from the Ibero-Moroccan shelf. In the Arabian Sea core, Radiolarians were concentrated in distinct horizons in which Tertiary material was redeposited (40-50, 140-150, 250-260 cm). The number of siliceous skeletons per gram of dried sediment decreases more or less rapidly with increasing depth in all cores. Whereas about 2500 skeletons were found in sediments close to the surface, approximately 100 skeletons only were found in deeper (>40 cm) layers. Deeper horizons with more than 100 specimens were interpreted as redeposited material. This sediment contained robust skeletons, resistant against dissolution, as well as benthic and Tertiary material. The decrease of siliceous skeletons relative to core depth depends upon the sedimentation rate. Where the sedimentation rate is high, the opal dissolution zone extends down to 30-60 cm, where the sedimentation rate is low, it is located at 10-30 cm. Below these depths opals disappears. These zones also have approximately the same age (4000 years) everywhere. Siliceous skeletons dissolve differentially, first the Silicoflagellates disappear, second the Diatoms, third the Radiolarians, and fourth the Sponge Spicules. Surface structure of skeletons from near the opal dissolution zones are similar to those of skeletons treated with NaOH. Tertiary diatoms (Trinacria e. g.) and benthic diatoms (Campylodiscus e.g.) dissolve less rapidly than skeletons of modern planktonic diatoms (Coscinodiscus e.g.). The time control of the opal dissolution zones appeared rather independent of various oceanic influences. No evidence was found for effects from upwelling either off Portugal or off Morocco. No difference in dissolution rates was recorded between the abyssal plains lying off these two areas. Likewise, there was no change in solution rates from Pleistocene to Holocene within either one of the abyssal plains. The Mediterranean outflow, which is enriched in dissolved silica, apparently had no effect on dissolution rates of siliceous skeletons in the sediment.