Ictiólogos de la Argentina: Juan Manuel Cordini.

This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina.

Ictiólogos de la Argentina: Francisco Juan José Risso Ceriani.

This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina.

Carta enviada por Juan Alcorta Maiz a Justo Garate en 1981

1 carta (mecanografiada) ; 210x274 mm. Ubicación: Caja 1 - Carpeta 19

Cartas enviadas por Aranzazu Amezaga Iribarren a Justo Garate entre 1985 y 1986

2 cartas (mecanografiadas) ; 210x297mm. Ubicación: Caja 1 - Carpeta 27

Cartas enviadas por José Atin a Justo Garate entre 1982 y 1986

5 cartas y 1 tarjeta de visita (mecanografiadas y manuscritas) ; entre 215x275mm y 172x222mm. Ubicación: Caja 1 - Carpeta 74

Synopse dos trabalhos da Camara dos Srs. Deputados : relativos ao anno de 1918 : acompanhados de differentes documentos : organizados na Secretaria da mesma Camara

Sinopse dos trabalhos da Câmara dos Deputados, em 1918.

Northwest Fish Culture Conference, Eugene, Oregon, December 2-4, 1986 [proceedings of the 37th conference]

(PDF contains 226 pages)

^(18)O/^(16)O and D/H studies on the interactions between heated meteoric ground waters and igneous intrusions: Western San Juan Mountains, Colorado and the Isle of Skye, Scotland

Detailed oxygen, hydrogen and carbon isotope studies have been carried out on igneous and metamorphic rocks of the Stony Mountain complex, Colorado, and the Isle of Skye, Scotland, in order to better understand the problems of hydrothermal meteoric water-rock interaction.

The Tertiary Stony Mountain stock (~1.3 km in diameter), is composed of an outer diorite, a main mass of biotite gabbro, and an inner diorite. The entire complex and most of the surrounding country rocks have experienced various degrees of ¹⁸O depletion (up to 10 per mil) due to interaction with heated meteoric waters. The inner diorite apparently formed from a low-¹⁸O magma with δ¹⁸O ≃ +2.5, but most of the isotopic effects are a result of exchange between H₂O and solidified igneous rocks. The low-¹⁸O inner diorite magma was probably produced by massive assimilation and/or melting of hydrothermally altered country rocks. The δ¹⁸O values of the rocks generally increase with increasing grain size, except that quartz typically has δ¹⁸O = +6 to +8, and is more resistant to hydrothermal exchange than any other mineral studied. Based on atom % oxygen, the outer diorites, gabbros, and volcanic rocks exhibit integrated water/rock ratios of 0.3 ± 0.2, 0.15 ± 0.1, and 0.2 ± 0.1, respectively. Locally, water/rock ratios attain values greater than 1.0. Hydrogen isotopic analyses of sericites, chlorites, biotites, and amphiboles range from -117 to -150. δD in biotites varies inversely with Fe/Fe+Mg, as predicted by Suzuoki and Epstein (1974), and positively with elevation, over a range of 600 m. The calculated δD of the mid-to-late-Tertiary meteoric waters is about -100. Carbonate δ¹³C values average -5.5 (PDB), within the generally accepted range for deep-seated carbon.

Almost all the rocks within 4 km of the central Tertiary intrusive complex of Skye are depleted in ¹⁸O. Whole-rock δ¹⁸O values of basalts (-7. 1 to +8.4), Mesozoic shales (-0.6 to + 12.4), and Precambrian sandstones (-6.2 to + 10.8) systematically decrease inward towards the center of the complex. The Cuillin gabbro may have formed from a ¹⁸O-depleted magma (depleted by about 2 per mil); δ¹⁸O of plagioclase (-7.1 to + 2.5) and pyroxene (-0.5 to + 3.2) decrease outward toward the margins of the pluton. The Red Hills epigranite plutons have δ¹⁸O quartz (-2.7 to + 7.6) and feldspar (-6.7 to + 6.0) that suggest about 3/4 of the exchange took place at subsolidus temperatures; profound disequilibrium quartz-feldspar fractionations (up to 12) are characteristic. The early epigranites were intruded as low-¹⁸O melts (depletions of up to 3 per mil) with δ¹⁸O of the primary, igneous quartz decreasing progressively with time. The Southern Porphyritic Epigranite was apparently intruded as a low-¹⁸O magma with δ¹⁸O ≃ -2.6. A good correlation exists between grain size and δ¹⁸O for the unique, high-¹⁸O Beinn an Dubhaich granite which intrudes limestone having a δ¹⁸O range of +0.5 to +20.8, and δ¹³C of -4.9 to -1.0. The δD values of sericites (-104 to -107), and amphiboles, chlorites, and biotites (-105 to -128) from the igneous rocks , indicate that Eocene surface waters at Skye had δD ≃ -90. The average water/rock ratio for the Skye hydrothermal system is approximately one; at least 2000 km³ of heated meteoric waters were cycled through these rocks.

Thus these detailed isotopic studies of two widely separated areas indicate that (1) ¹⁸O-depleted magmas are commonly produced in volcanic terranes invaded by epizonal intrusions; (2) most of the ¹⁸O-depletion in such areas are a result of subsolidus exchange (particularly of feldspars); however correlation of δ¹⁸O with grain size is generally preserved only for systems that have undergone relatively minor meteoric hydrothermal exchange; (3) feldspar and calcite are the minerals mos t susceptible to oxygen isotopic exchange, whereas quartz is very resistant to oxygen isotope exchange; biotite, magnetite, and pyroxene have intermediate susceptibilities; and (4) basaltic country rocks are much more permeable to the hydrothermal convective system than shale, sandstone, or the crystalline basement complex.

Análise de sobrevida dos pacientes com AIDS atendidos em um centro de pesquisa no Rio de Janeiro : 1986 a 2000

O objetivo deste trabalho é determinar o tempo decorrido e fatores relacionados a sobrevida, a partir do diagnóstico da AIDS dos pacientes atendidos no Centro de Pesquisa Hospital Evandro Chagas (CPqHEC). Comparar a sobrevida segundo os critérios definição de caso de AIDS estabelecidos pelo Centro de controle de doenças e prevenção dos EUA (CDC) em 1987 e 1993 e pelo Ministério da Saúde Brasil em 1998. De um total de 1591 indivíduos com sorologia positiva para HIV, cadastrados entre 1986 a 1999, foi selecionada uma amostra aleatória sistemática com 392 indivíduos, sendo identificados 193 casos de AIDS pelo critério CDC 1993. A sobrevida foi considerada como o tempo decorrido da data do diagnóstico da AIDS ao óbito (falha), sendo a censura definida para os pacientes com perda de seguimento ou que permaneceram vivos até dezembro de 2000, com a data da censura igual a data do último atendimento. A duração da sobrevida foi descrita através do método de Kaplan-Meier, sendo comparadas as funções de sobrevida das categorias das variáveis pelo teste log-rank. Um modelo com os co-fatores de maior relevância na sobrevida foi ajustado, utilizando-se o modelo dos riscos proporcionais de Cox. Dos 193 pacientes com AIDS, 92 (47,7%) morreram, 21 (10,9%) abandonaram o tratamento, e 80 (41,7%) permaneceram vivos até o fim do estudo. Encontramos sobrevida relativamente alta nos três critérios de definição de caso avaliados, em parte explicada pelos casos serem procedentes de um único hospital de pesquisa, com alto grau de conhecimento na condução da doença. A profilaxia primária para PPC foi preditor de melhor sobrevida. Casos com AIDS definida por herpes zoster apresentaram melhor prognóstico e os definidos por duas doenças o pior prognóstico.

Front pages with contents of No. 43, 1986

Front cover. Contents. (PDF contains 2 pages)

Back pages of No. 43, 1986

Back cover. Map of Galápagos. Galapagos Penguin, Photo by G.T. Corley Smith.

Report of the Inter-American Tropical Tuna Commission for the year 1986

ENGLISH: The Inter-American Tropical Tuna Commission operates under the authority and direction of a convention originally entered into by Costa Rica and the United States. The convention, which came into force in 1950, is open to adherence by other governments whose nationals fish for tropical tunas in the eastern Pacific Ocean. Under this provision Panama adhered in 1953, Ecuador in 1961, Mexico in 1964, Canada in 1968, Japan in 1970, and France and Nicaragua in 1973. Ecuador withdrew from the Commission in 1968, Mexico in 1978, Costa Rica in 1979, and Canada in 1984. No Commission meeting was held in 1986. SPANISH: La Comisión Interamericana del Atún Tropical funciona bajo la autoridad y dirección de un convenio establecido originalmente por la República de Costa Rica y los Estados Unidos de América. El convenio, vigente desde 1950, está abierto a la afiliación de otros gobiernos cuyos ciudadanos pescan atún en el Pacífico oriental tropical. Bajo esta estipulación, Panamá se afilió en 1953, Ecuador en 1961, los Estados Unidos Mexicanos en 1964, Canadá en 1968, Japón en 1970, Francia y Nicaragua en 1973. Ecuador se retiró de la Comisión en 1968, México en 1978, Costa Rica en 1979 y Canadá en 1984. En 1986 no hubo reunión de la Comisión. (PDF contains 264 pages.)

Museos, memoria y turismo

Cap. 1. Museos y patrimonio: de la distancia retórica a la interlocución democrática. Iñaki Díaz Balerdi. Cap. 2. Au coeur des conflits entre memoire, histoire et developpement economique, les nouveaux enjeux des musees de société aujourd’hui. François Hubert. Cap. 3. Elites, Instituciones Públicas, identidad cultural y turismo en los orígenes del Museo Municipal de Donostia-San Sebastián. Iñaki Arrieta Urtizberea. Cap. 4. Los orígenes de la museografía etnográfica en Cataluña: el Arxiu-Museu Folklòric de Ripoll. Oriol Beltran Costa. Cap. 5. Museo de la Pesca en Palamós: espacio para la memoria de los pescadores. Miquel Martí i Llambrich. Cap. 6. Arqueología y museos en Gipuzkoa; las experiencias del Centro de Estudios ARKEOLAN (1986-2005). Mª Mercedes Urteaga Artigas. Cap. 7. Penser un Musée des Confluences: un autre discours sur soi et les autres que soi. Thierry Valentin. Cap. 8. Turismo cultural y museos: oportunidades de desarrollo comunes. El caso de Cesis, Letonia. María Fernández Sabau. Cap. 9. La gestión y el uso turístico de los museos: la experiencia de Barcelona. Jordi Juan Tresserras y Juan Carlos Matamala. Cap. 10. Museos, turismo y desarrollo local en el norte de Portugal: el Ecomuseo del Barroso. Xerardo Pereiro. Cap. 11. Turismo y patrimonio cultural en las pequeñas y medianas ciudades: el Barri Vell de Girona y el Museu d’Art de Girona. Josep Manuel Rueda Torres.