Proyecto de un programa de Educación Compensatoria, en una zona rural de actuación educativa preferente en función de los factores de rendimiento escolar en el primer curso de EGB.

1) analizar los diferentes factores que influyen en el rendimiento escolar al finalizar el primer curso EGB, 2) examinar las características de las variables socioculturales de la comarca de actuación compensatoria y el status del profesorado de la población escolar estudiada, 3) la preescolarización como factor determinantes del rendimiento escolar y etapa preventiva del fracaso escolar, 4) análisis de los criterios del profesorado acerca de la madurez cognoscitiva adquirida por los niños en preescolar, 5) visión general de las aptitudes para el aprendizaje escolar y su influencia en el rendimiento escolar, 6) estudio del modelo de interacción de factores que implique causa y efectos de los fenómenos observados, 7) desarrollo programa de Educación Compensatoria y ciclo inicial para la comarca estudiada.. 119 alumnos de primer curso en 15 centros estatales de EGB de quince localidades de la comarca del Rio Aranda, provincia de Zaragoza. Objeto: Educación Compensatoria. Método de investigación. Variable dependiente: el rendimiento escolar que se obtiene al finalizar el primer curso de EGB. Variables independientes: 1) variables educacionales en la etapa preescolar, 2) nivel aptitudinal de los alumnos para el aprendizaje, 3) variables socioculturales del medio: origen sociocultural-conocimientos previos-aptitudes escolares. Status profesorado, rendimiento escolar. Cuestionario sobre aspectos educacionales y madurativos del alumno (factores de escolarización, nivel de conocimientos instrumentales y nivel de conocimientos formativos). Cuestionario sociocultural aplicado a los padres (nivel socioeconómico familiar, nivel cultural familiar y habitat familiar). Batería de aptitudes para el aprendizaje escolar (comprensión verbal, aptitud numérica, aptitud perceptiva y espacial). Pruebas objetivas para evaluar el rendimiento académico en las áreas de Lenguaje y Matemáticas para alumnos que finalizan primero de EGB. 1) La preescolarización y la preparación cognoscitiva que posee el alumno a su ingreso en primero de EGB es determinante en su posterior rendimiento escolar al finalizar este curso (25,57 por ciento de la varianza total). 2) Las variables de carácter social y cultural determinan la madurez cognoscitiva del alumno y en consecuencia su aprovechamiento escolar (15,62 por ciento de la varianza total). 3) Las aptitudes escolares adquiridas por el alumno durante primero de EGB explican el rendimiento escolar (5,68 por ciento de la varianza total). 4) Las condiciones y status del profesorado explican el rendimiento escolar (2,84 por ciento de la varianza total). De los resultados encontrados se diseñó un programa de Educación Compensatoria para la comarca de Illueca y 15 poblaciones colindantes.

Municipio y provincias

A complex process has been started by the status change of national territories that gained recognition as provinces, with the right to elect their own government and send representatives to the national legislative branch. This process incorporates a new governmental sphere into heterogeneous spaces, for which administrative roles that did not address any particularities used to be performed until then by the Governor’s offi ce designated by the National Government. Therefore, by asking how the province formation and the relations redefi nition were carried out, the review of national pressures’ incorporation in local terms has been enabled. The case addressed by this paper is the provincialization of Rio Negro and the particular circumstances of the dialog between the San Carlos de Bariloche commune and the incipient governmental space opened since 1958.

Alternativa productiva para el aprovechamiento del residuo cachaza

Este trabajo de investigación, busca ofrecer al sector panelero de Colombia nuevas estrategias eco-eficientes y amigables con el medio ambiente, en pro de fortalecer las buenas prácticas agrícolas, que contribuyan con la gestión óptima de los residuos que se crean alrededor de la cadena de producción de la panela. Teniendo en cuenta que la obtención de desechos tanto orgánicos como inorgánicos, genera un impacto medioambiental negativo, se pudo identificar una de estas fuentes de contaminación, a través de un proceso de observación. Ésta es conocida como la Cachaza, la cual se genera dentro de un procedimiento denominado Limpieza del Dulce de Caña. Inicialmente, la caña se muele a través de una trituradora que exprime dulce sin tratamiento, el cual pasa por un ducto hasta regarse sobre una primera paila, donde se le aplica balso. Por medio del calor que produce una hornilla sobre la que se coloca dicha paila, se realiza un proceso de separación, el residuo consolidado en una espuma espesa, comienza a flotar por encima del dulce, siendo extraída a medida que va saliendo y depositada en otros recipientes. Considerando constantes prácticas como el vertimiento de la Cachaza sobre algunas fuentes hídricas (ríos, lagunas, etc.) y cultivos de caña ya fermentados (que elaboran nutrientes negativos sobre los mismos); se profundizará sobre los diferentes impactos ambientales que se originan en éste proceso agroindustrial. El objetivo principal del presente trabajo de investigación, consiste en la implementación de un proyecto de logística inversa, formulando estrategias para el procesamiento de la Cachaza a implementar en un trapiche de la zona de Rio negro a fin de reutilizar este residuo generando subproductos que aporten a la mitigación del impacto ambiental, dando así un valor agregado a toda la cadena. Mediante un análisis costo beneficio se evaluará qué tan fácil o difícil resulta la implementación de dicho proyecto, el cual al incluir un proceso adicional a la cadena de producción de la panela generara un suplemento alimenticio para los equinos y aprovechara el 100% de sus residuos a muy bajo costo.

Desarrollo de actitudes hacia el cuidado de la energía : experiencia en la formación de maestros.

Resumen basado en el de la publicación

Potamotrygon tigrina, a new species of freshwater stingray from the upper Amazon basin, closely related to Potamotrygon schroederi Fernandez-Yepez, 1958 (Chondrichthyes: Potamotrygonidae)

A new species of Neotropical freshwater stingray, family Potamotrygonidae, is described from the Rio Nanay in the upper Rio Amazonas basin of Peru. Potamotrygon tigrina, n. sp., is easily distinguished from all congeners by its conspicuous dorsal disc coloration, composed of bright yellow to orange vermiculations strongly interwoven with a dark-brown to deep-black background. Additional features that in combination diagnose P. tigrina, n. sp., include the presence of a single angular cartilage, low and not closely grouped dorsal tail spines, and coloration of tail composed of relatively wide and alternating bands of creamy white and dark brown to black. Potamotrygon tigrina is closely related to Potamotrygon schroederi Fernandez-Yepez, 1958, which occurs in the Rio Negro (Brazil) and Rio Orinoco (Venezuela, Colombia). Both species are very similar in proportions and counts, and share features hypothesized to be derived within Potamotrygonidae, related to their specific angular cartilage morphology, distal tail color, dorsal tail-spine pattern, and ventral lateral-line system. To further substantiate the description of P. tigrina, n. sp., we provide a redescription of P. schroederi based on material from the Rio Negro (Brazil) and Rio Orinoco (Venezuela). Specimens from the two basins differ in number of vertebral centra and slightly in size and frequency of rosettes on dorsal disc, distinctions that presently do not warrant their specific separation. Potamotrygon tigrina is frequently commercialized in the international aquarium trade but virtually nothing is known of its biology or conservation status.

The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview

The Rondonian-San Ignacio Province (1.56-1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent-continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the Rio Negro-Juruena Province (Rondonia region), considering that the province was affected by later collision-related deformation and metamorphism during the Sunsas Orogeny (1.25-1.00 Ga). The Rondonian-San Ignacio Province comprises: (1) the Jauru Terrane (1.78-1.42 Ga) that hosts Paleoproterozoic basement (1.78-1.72 Ga), and the Cachoeirinha (1.56-1.52 Ga) and the Santa Helena (1.48-1.42 Ga) accretionary orogens, both developed in an Andean-type magmatic arc; (2) the Paragua Terrane (1.74-1.32 Ga) that hosts pre-San Ignacio units (>1640 Ma: Chiquitania Gneiss Complex, San Ignacio Schist Group and Lomas Manechis Granulitic Complex) and the Pensamiento Granitoid Complex (1.37-1.34 Ga) developed in an Andean-type magmatic arc; (3) the Rio Alegre Terrane (1.51-1.38 Ga) that includes units generated in a mid-ocean ridge and an intra-oceanic magmatic arc environments; and (4) the Alto Guapore Belt (<1.42-1.34 Ga) that hosts units developed in passive marginal basin and intra-oceanic arc settings. The collisional stage (1.34-1.32 Ga) is characterized by deformation, high-grade metamorphism, and partial melting during the metamorphic peak, which affected primarily the Chiquitania Gneiss Complex and Lomas Manechis Granulitic Complex in the Paragua Terrane, and the Colorado Complex and the Nova Mamore Metamorphic Suite in the Alto Guapore Belt. The Paragua Block is here considered as a crustal fragment probably displaced from its Rio Negro-Juruena crustal counterpart between 1.50 and 1.40 Ga. This period is characterized by extensive A-type and intra-plate granite magmatism represented by the Rio Crespo Intrusive Suite (ca. 1.50 Ga), Santo Antonio Intrusive Suite (1.40-1.36 Ga), and the Teotonio Intrusive Suite (1.38 Ga). Magmatism of these types also occur at the end of the Rondonian-San Ignacio Orogeny, and are represented by the Alto Candeias Intrusive Suite (1.34-1.36 Ga), and the Sao Lourenco-Caripunas Intrusive Suite (1.31-1.30 Ga). The cratonization of the province occurred between 1.30 and 1.25 Ga. (C) 2009 Elsevier Ltd. All rights reserved.

Trace element geochemistry and Sr-Nd characteristics of Mesoproterozoic mafic intrusive rocks from Rondonia, Brazil, SW Amazonian Craton: Petrogenetic and tectonic inferences

The Amazonian Craton comprises an Archean domain surrounded by four successively younger Proterozoic tectonic provinces. Within the Rio-Negro-Juruena province the Serra da Providencia Intrusive Suite (1.60 and 1.53 Ga) consists of A-type rapakivi granites, charnockites and mangerites genetically associated with diabase dikes, gabbros and amphibolites lites. The original mafic melts were derived from a depleted mantle source (epsilon(Nd(T)) + 2.5 to +2.8; epsilon(Sr(T)) - 12.1). Underplated mafic magma induced melting of a short-lived fielsic crust, thus originating coeval felsic-inafic magmatism in a continental intraplate setting. The Colorado Complex, assigned to the Rondonian-San Ignacio province, comprises 1.35-1.36 Ga intrusive bimodal magmatism represented by monzonite gneisses associated with amphibolite, gabbro and metadiabase dikes intercalated with metasediments with detrital zircon that yield U-Pb ages of 1.35 to 1.42 Ga. Mafic samples display juvenile signatures (epsilon(Nd(T)) 0.0 to +5.2; epsilon(Sr(T)) -5.0 to -30.7) and are less contaminated than the Serra da Previdencia and Nova Brasiladndia ones. The generation of the basaltic magma is related to the subduction of an oceanic slab below the peridotite wedge (intraoceanic arc setting). Fluids and/or small melts from the slab impregnated the mantle. The Nova Brasilandia Sequence (Sunsas-Aguapei province) comprises a metasedimentary sequence intruded by 1.10-1.02 Ga metadiabases, gabbros, meta-gabbros, and amphibolites associated with granitic plutons (bimodal magmatism). The original tholeiitic magmas, derived from a depleted source (epsilon(Nd(T)) = +3.1 to +5.0), in a proto-oceanic setting, underwent subsequent contamination by the host rocks, as indicated by the isotopic and trace element data.

Cryptic sexual populations account for genetic diversity and ecological success in a widely distributed, asexual fungus-growing ant

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Astyanax ajuricaba: a new species from the Amazon basin in Brazil (Characiformes: Characidae)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Substâncias húmicas aquáticas: fracionamento molecular e caracterização de rearranjos internos após complexação com íons metálicos

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Características das águas subterrâneas numa faixa norte-sul na cidade de Manaus (AM)

A cidade de Manaus está localizada numa região próxima ao centro da bacia Amazônica, cujo abastecimento de água é realizado pelas águas do Amazonas, sendo efetuado por captação da drenagem superficial do rio Negro e por poços tubulares, que exploram aqüíferos constituídos pela Formação Alter do Chão. Com o objetivo de investigar a hidroquímica das águas subterrâneas de Manaus, para caracterizar e avaliar a qualidade dos recursos hídricos em subsuperfície, aferiram-se os parâmetros físicos, físico-químicos e químicos das amostras de águas de poços tubulares selecionados. Os resultados obtidos dos parâmetros analisados mostraram que as águas estudadas são excelentes para consumo humano e industrial, por situarem-se dentro dos limites de potabilidade estabelecidos pela legislação vigente.

Controle químico do crestamento bacteriano comum do feijoeiro e seu efeito na transmissão de Xanthomonas campestris pv. phaseoli (Smith) Dye pelas sementes.

Dois ensaios foram conduzidos durante a safra das águas de 1987, no estado do Paraná, visando o controle químico do crestamento bacteriano comum do feijoeiro (Phaseolus vulgaris L.), na cultivar Rio Negro. Os produtos sulfato de estreptomicina + oxitetraciclina, oxicloreto de cobre + zineb, oxicloreto de cobre + mancozeb e oxicloreto de cobre, foram aplicados em pulverização, por três vezes, durante a safra. Foi observada baixa eficiência no controle dessa bacteriose, diante da elevada severidade do crestamento bacteriano nas folhas, alta incidência em vagens e elevada população de X. camnpestris pv. phaseoli nas sementes. Houve incremento na produtividade devido à aplicação de oxicloreto de cobre + zineb e oxicloreto de cobre + mancozeb.

Mesoproterozoic rapakivi granites of the Rondonia Tin Province, southwestern border of the Amazonian craton, Brazil - I. Reconnaissance U-Pb geochronology and regional implications

Rapakivi granites and associated mafic and ultramafic rocks in the Rondonia Tin Province, southwestern Amazonian craton, Brazil were emplaced during six discrete episodes of magmatism between ca 1600 and 970 Ma. The seven rapakivi granite suites emplaced at this time were the Serra da Providencia Intrusive Suite (U-Pb ages between 1606 and 1532 Ma); Santo Antonio Intrusive Suite(U-Pb age 1406 Ma), Teotonio Intrusive Suite (U-Pb age 1387 Ma); Alto Candeias Intrusive Suite (U-Pb ages between 1346 and 1338 Ma); Sao Lourenco-Caripunas Intrusive Suite (U-Pb ages between 1314 and 1309 Ma); Santa Clara Intrusive Suite (U-Pb ages between 1082 and 1074 Ma); and Younger Granites of Rondonia (U-Pb ages between 998 and 974 Ma). The Serra da Providencia Intrusive Suite intruded the Paleoproterozoic (1.80 to 1.70 Ga) Rio Negro-Juruena crust whereas the other suites were emplaced into the 1.50 to 1.30 Ga Rondonia-San Ignacio crust. Their intrusion was contemporaneous with orogenic activity in other parts of the southwestern Amazonian craton, except for the oldest, Serra da Providencia Intrusive Suite. Orogenic events coeval with emplacement of the Serra da Providencia Intrusive Suite are not clearly recognized in the region. The Santo Antonio, Teotonio, Alto Candeias and Sao Lourenco-Caripunas Intrusive Suites are interpreted to represent extensional anorogenic magmatism associated with the terminal stages of the Rondonian-San Ignacio orogeny. At least the Sao Lourenco-Caripunas rapakivi granites and coeval intra-continental rift sedimentary rocks may, in contrast, represent the products of extensional tectonics and rifting preceding the Sunsas/Aguapei orogeny (1.25 to 1.0 Ga). The two youngest rapakivi suites, the Santa Clara Intrusive Suite and Younger Granites of Rondonia, seemingly represent inboard magmatism in the Rondonian-San Ignacio Province during a younger episode of reworking in the Rio Negro-Juruena Province during the waning stages of the collisional 1.1 to 1.0 Ga Sunsas/Aguapei orogeny. The six intra-plate rapakivi granite episodes in the southwestern part of the Amazonian craton form three broad periods of anorogenic magmatism that have age-correlative events composed of similar rocks and geologic environments in eastern Laurentia and Baltica, although the exact timing of magmatism appears slightly different. Recognition of lithologic and chronological correlations between various cratons provide important constraints to models explaining the interplay between rapakivi granite magmatism and deep crustal evolution of an early Mesoproterozoic supercontinent. They are, furthermore, important to plate tectonic models for the assembly, dispersal and reassembly of Amazonia, Laurentia and Baltica in the Mesoproterozoic and Neoproterozoic. (C) 1999 Elsevier B.V. B.V. All rights reserved.

Bird species of black water inundation forests in the Jau National Park (Amazonas state, Brazil): their contribution to regional species richness

We compared the relative contribution of blackwater inundation forest (igapo) and unflooded (terra firme) forest for regional bird species diversity in the lower Rio Negro region. For analyses of habitat preference we used mist-net samples and an unpublished bird species check-list. The igapo forest had lower bird species diversity than the terra firme forest. However, some 14% of the forest bird species in the region are restricted to igapo forest. Species composition was found to be distinct between the understories of the two forest types. Common forest bird guilds in the Neotropics such as ant-following birds avoid igapo forest. The differential habitat selection among birds in the inundated and unflooded forest is likely to result from vegetation structure and biological interactions such as aggressive behaviour. Since the inundated forest has a typical biota, conservation efforts needs to be directed to protect these habitats. Unfortunately, inundation forests are threatened by several human actions, especially dam construction. The extent of protected areas in the Brazilian Amazon is insufficient for the adequate protection of the inundated habitats, because it includes only 3% of the total area.

Geological evolution of the basement rocks in the east-central part of the Rondonia Tin Province, SW Amazonian craton, Brazil: U-Pb and Sm-Nd isotopic constraints

On the basis of geologic, petrologic, and U-Pb geochronologic data the basement rocks in the east-central part of the Rondonia Tin Province (RTP, southwestern Amazonian craton) are grouped into five lithologic associations: (1) tonalitic gneiss (1.75 Ga); (2) enderbitic granulite (1.73 Ga); (3) paragneiss; (4) granitic and charnockitic augen gneisses (1.57-1.53 Ga); and (5) fine-grained granitic gneiss and charnockitic granulite (1.43-1.42 Ga). The first three are related to development of the Paleoproterozoic Rio Negro-Juruena Province and represent the oldest crust in the region. The tonalitic gneisses and enderbitic granulites show calc-alkaline affinities and Nd isotopic compositions (initial epsilon(Nd) = +0-1 to -1.5; T-DM of 2.2-2.1 Ga) that suggest a continental arc margin setting for the original magmas. The paragneisses yield T-DM values of 2.2-2.1 Ga suggesting that source material was primarily derived from the Ventuari-Tapajos and Rio Negro-Juruena crusts, but detrital zircon ages and an intrusive granitoid bracket deposition between 1.67 and 1.57 Ga. The granitic and charnockitic augen gneisses show predominantly A-type and within-plate granite affinities, but also some volcanic arc granite characteristics. The initial epsilon(Nd) values (+0.6 to +2.0) indicate mixing of magmas derived from depleted mantle and older crustal sources. These rocks are correlated to the 1.60-1.53 Ga Serra da Providencia intrusive suite that reflects inboard magmatism coeval with the Cachoeirinha orogen located to the southeast. The fine-grained granitic gneiss and charnockitic granulites represent the first record of widespread magmatism at 1.43-1.42 Ga in northern Rondonia. Their geochemical signatures and the slightly positive initial epsilon(Nd) values (+0.7 to +1.2) are very similar to those of the most evolved granites of the calc-alkaline Santa Helena batholith farther southeast. U-Pb monazite and Sm-Nd whole-rock-garnet ages demonstrate that a high-grade tectonometa-morphic episode occurred in this region at 1.33-1.30 Ga. This episode attained upper-amphibolite conditions and is interpreted as the peak of the Rondonian-San Ignacio orogeny. The U-Pb and Sm-Nd data presented here and data published on rapakivi granites elsewhere indicate that the east-central part of the RTP is a poly-orogenic region characterized by successive episodes of magmatism, metamorphism, and deformation between 1.75 and 0.97 Ga. (C) 2002 Elsevier B.V. B.V. All rights reserved.