955 resultados para CHACO AUSTRAL


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Spiders are thought to play a significant role in limiting pest outbreaks in agroecosystems such as vineyards, orchards and cotton. The diversity and impact of spiders in vegetable crops are less well understood, although there is evidence that predators may be important for suppression of lepidopteran pests in Brassica crops, particularly early in the season before parasitoids become established. Sampling was conducted in early season plantings of Brassicas in the Lockyer Valley (South East Queensland, Australia) in order to determine the most commonly occurring spider families. The most numerous were Theridiidae, which were more strongly associated with cauliflower and poorly associated with cabbage. The Lycosidae and Clubionidae/Miturgidae (formerly in the ‘catch-all’ family Clubionidae) also occurred commonly. Lycosidae (and to a lesser extent Salticidae) had above average abundance in Chinese cabbage and below average abundance in broccoli compared with average abundance for these spider families; Clubionidae/Miturgidae had above average abundance in cauliflower. Laboratory studies were then conducted to explore the predatory capacity of these three most commonly occurring spider families. All three were capable of feeding on larvae of the diamondback moth, Plutella xylostella (Linnaeus), and cabbage cluster caterpillar, Crocidolomia pavonana (Fabricius), under laboratory conditions. Theridiidae, which are thought to prey on small pests such as leafhoppers and aphids, were able to successfully attack larvae up to five times their body size. Predation rates varied from an average of 1.7 (SE = 0.47) (1.6 control corrected) larvae consumed over a 24 h period in the case of the Theridiidae, to 3.3 (SE = 0.60) larvae for the Clubionidae/Miturgidae.

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The Antarctic system comprises of the continent itself, Antarctica, and the ocean surrounding it, the Southern Ocean. The system has an important part in the global climate due to its size, its high latitude location and the negative radiation balance of its large ice sheets. Antarctica has also been in focus for several decades due to increased ultraviolet (UV) levels caused by stratospheric ozone depletion, and the disintegration of its ice shelves. In this study, measurements were made during three Austral summers to study the optical properties of the Antarctic system and to produce radiation information for additional modeling studies. These are related to specific phenomena found in the system. During the summer of 1997-1998, measurements of beam absorption and beam attenuation coefficients, and downwelling and upwelling irradiance were made in the Southern Ocean along a S-N transect at 6°E. The attenuation of photosynthetically active radiation (PAR) was calculated and used together with hydrographic measurements to judge whether the phytoplankton in the investigated areas of the Southern Ocean are light limited. By using the Kirk formula the diffuse attenuation coefficient was linked to the absorption and scattering coefficients. The diffuse attenuation coefficients (Kpar) for PAR were found to vary between 0.03 and 0.09 1/m. Using the values for KPAR and the definition of the Sverdrup critical depth, the studied Southern Ocean plankton systems were found not to be light limited. Variabilities in the spectral and total albedo of snow were studied in the Queen Maud Land region of Antarctica during the summers of 1999-2000 and 2000-2001. The measurement areas were the vicinity of the South African Antarctic research station SANAE 4, and a traverse near the Finnish Antarctic research station Aboa. The midday mean total albedos for snow were between 0.83, for clear skies, and 0.86, for overcast skies, at Aboa and between 0.81 and 0.83 for SANAE 4. The mean spectral albedo levels at Aboa and SANAE 4 were very close to each other. The variations in the spectral albedos were due more to differences in ambient conditions than variations in snow properties. A Monte-Carlo model was developed to study the spectral albedo and to develop a novel nondestructive method to measure the diffuse attenuation coefficient of snow. The method was based on the decay of upwelling radiation moving horizontally away from a source of downwelling light. This was assumed to have a relation to the diffuse attenuation coefficient. In the model, the attenuation coefficient obtained from the upwelling irradiance was higher than that obtained using vertical profiles of downwelling irradiance. The model results were compared to field measurements made on dry snow in Finnish Lapland and they correlated reasonably well. Low-elevation (below 1000 m) blue-ice areas may experience substantial melt-freeze cycles due to absorbed solar radiation and the small heat conductivity in the ice. A two-dimensional (x-z) model has been developed to simulate the formation and water circulation in the subsurface ponds. The model results show that for a physically reasonable parameter set the formation of liquid water within the ice can be reproduced. The results however are sensitive to the chosen parameter values, and their exact values are not well known. Vertical convection and a weak overturning circulation is generated stratifying the fluid and transporting warmer water downward, thereby causing additional melting at the base of the pond. In a 50-year integration, a global warming scenario mimicked by a decadal scale increase of 3 degrees per 100 years in air temperature, leads to a general increase in subsurface water volume. The ice did not disintegrate due to the air temperature increase after the 50 year integration.

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Volatile organic compounds (VOCs) in the headspace of bubble chambers containing branches of live coral in filtered reef seawater were analysed using gas chromatography with mass spectrometry (GC-MS). When the coral released mucus it was a source of dimethyl sulfide (DMS) and isoprene; however, these VOCs were not emitted to the chamber headspace from mucus-free coral. This finding, which suggests that coral is an intermittent source of DMS and isoprene, was supported by the observation of occasional large pulses of atmospheric DMS (DMSa) over Heron Island reef on the southern Great Barrier Reef (GBR), Australia, in the austral winter. The highest DMSa pulse (320 ppt) was three orders of magnitude less than the DMS mixing ratio (460 ppb) measured in the headspace of a dynamically purged bubble chamber containing a mucus-coated branch of Acropora aspera indicating that coral reefs can be strong point sources of DMSa. Static headspace GC-MS analysis of coral fragments identified mainly DMS and seven other minor reduced sulfur compounds including dimethyl disulfide, methyl mercaptan, and carbon disulfide, while coral reef seawater was an indicated source of methylene chloride, acetone, and methyl ethyl ketone. The VOCs emitted by coral and reef seawater are capable of producing new atmospheric particles < 15 nm diameter as observed at Heron Island reef. DMS and isoprene are known to play a role in low-level cloud formation, so aerosol precursors such as these could influence regional climate through a sea surface temperature regulation mechanism hypothesized to operate over the GBR.

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Bactrocera tryoni (Froggatt) is Australia's major horticultural insect pest, yet monitoring females remains logistically difficult. We trialled the ‘Ladd trap’ as a potential female surveillance or monitoring tool. This trap design is used to trap and monitor fruit flies in countries other (e.g. USA) than Australia. The Ladd trap consists of a flat yellow panel (a traditional ‘sticky trap’), with a three dimensional red sphere (= a fruit mimic) attached in the middle. We confirmed, in field-cage trials, that the combination of yellow panel and red sphere was more attractive to B. tryoni than the two components in isolation. In a second set of field-cage trials, we showed that it was the red-yellow contrast, rather than the three dimensional effect, which was responsible for the trap's effectiveness, with B. tryoni equally attracted to a Ladd trap as to a two-dimensional yellow panel with a circular red centre. The sex ratio of catches was approximately even in the field-cage trials. In field trials, we tested the traditional red-sphere Ladd trap against traps for which the sphere was painted blue, black or yellow. The colour of sphere did not significantly influence trap efficiency in these trials, despite the fact the yellow-panel/yellow-sphere presented no colour contrast to the flies. In 6 weeks of field trials, over 1500 flies were caught, almost exactly two-thirds of them being females. Overall, flies were more likely to be caught on the yellow panel than the sphere; but, for the commercial Ladd trap, proportionally more females were caught on the red sphere versus the yellow panel than would be predicted based on relative surface area of each component, a result also seen the field-cage trial. We determined that no modification of the trap was more effective than the commercially available Ladd trap and so consider that product suitable for more extensive field testing as a B. tryoni research and monitoring tool.

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The synthesis of the title compound is described and results of some experiments on the degradation of patchouli alcohol are reported.

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Cyclohexanone and 2-, 3- and 4-methylcyclohexanones have been condensed with acetylene to give the respective 1-ethinylcyclohexanola. The 1-ethinylcyclohexanols were hydrogenated to the respective 1-vinyl- and 1-ethylcyclohexanols. The 1-vinylcyclohexanols have been treated with phosphorus tribromide to give the corresponding rearranged β-cyclohexylidenethyl bromides which have been converted to the pyridinium salts. The latter were treated with p-nitrosodimethylaniline and alkali (Krohnke's method) to give the corresponding nitrones which were hydrolyzed to the corresponding aldehydes. The 1-ethinyl-, 1-vinyl- and 1-ethylcyclohexanols prepared were subjected to pharmacological tests.

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Earth s ice shelves are mainly located in Antarctica. They cover about 44% of the Antarctic coastline and are a salient feature of the continent. Antarctic ice shelf melting (AISM) removes heat from and inputs freshwater into the adjacent Southern Ocean. Although playing an important role in the global climate, AISM is one of the most important components currently absent in the IPCC climate model. In this study, AISM is introduced into a global sea ice-ocean climate model ORCA2-LIM, following the approach of Beckmann and Goosse (2003; BG03) for the thermodynamic interaction between the ice shelf and ocean. This forms the model ORCA2-LIM-ISP (ISP: ice shelf parameterization), in which not only all the major Antarctic ice shelves but also a number of minor ice shelves are included. Using these two models, ORCA2-LIM and ORCA2-LIM-ISP, the impact of addition of AISM and increasing AISM have been investigated. Using the ORCA2-LIM model, numerical experiments are performed to investigate the sensitivity of the polar sea ice cover and the Antarctic Circumpolar Current (ACC) transport through Drake Passage (DP) to the variations of three sea ice parameters, namely the thickness of newly formed ice in leads (h0), the compressive strength of ice (P*), and the turning angle in the oceanic boundary layer beneath sea ice (θ). It is found that the magnitudes of h0 and P* have little impact on the seasonal sea ice extent, but lead to large changes in the seasonal sea ice volume. The variation in turning angle has little impact on the sea ice extent and volume in the Arctic but tends to reduce them in the Antarctica when ignored. The magnitude of P* has the least impact on the DP transport, while the other two parameters have much larger influences. Numerical results from ORCA2-LIM and ORCA2-LIM-ISP are analyzed to investigate how the inclusion of AISM affects the representation of the Southern Ocean hydrography. Comparisons with data from the World Ocean Circulation Experiment (WOCE) show that the addition of AISM significantly improves the simulated hydrography. It not only warms and freshens the originally too cold and too saline bottom water (AABW), but also warms and enriches the salinity of the originally too cold and too fresh warm deep water (WDW). Addition of AISM also improves the simulated stratification. The close agreement between the simulation with AISM and the observations suggests that the applied parameterization is an adequate way to include the effect of AISM in a global sea ice-ocean climate model. We also investigate the models capability to represent the sea ice-ocean system in the North Atlantic Ocean and the Arctic regions. Our study shows both models (with and without AISM) can successfully reproduce the main features of the sea ice-ocean system. However, both tend to overestimate the ice flux through the Nares Strait, produce a lower temperature and salinity in the Hudson Bay, Baffin Bay and Davis Strait, and miss the deep convection in the Labrador Sea. These deficiencies are mainly attributed to the artificial enlargement of the Nares Strait in the model. In this study, the impact of increasing AISM on the global sea ice-ocean system is thoroughly investigated. This provides a first idea regarding changes induced by increasing AISM. It is shown that the impact of increasing AISM is global and most significant in the Southern Ocean. There, increasing AISM tends to freshen the surface water, to warm the intermediate and deep waters, and to freshen and warm the bottom water. In addition, increasing AISM also leads to changes in the mixed layer depths (MLD) in the deep convection sites in the Southern Ocean, deepening in the Antarctic continental shelf while shoaling in the ACC region. Furthermore, increasing AISM influences the current system in the Southern Ocean. It tends to weaken the ACC, and strengthen the Antarctic coastal current (ACoC) as well as the Weddell Gyre and the Ross Gyre. In addition to the ocean system, increasing AISM also has a notable impact on the Antarctic sea ice cover. Due to the cooling of seawater, sea ice concentration and thickness generally become higher. In austral winter, noticeable increases in sea ice concentration mainly take place near the ice edge. In regards with sea ice thickness, large increases are mainly found along the coast of the Weddell Sea, the Bellingshausen and Amundsen Seas, and the Ross Sea. The overall thickening of sea ice leads to a larger volume of sea ice in Antarctica. In the North Atlantic, increasing AISM leads to remarkable changes in temperature, salinity and density. The water generally becomes warmer, more saline and denser. The most significant warming occurs in the subsurface layer. In contrast, the maximum salinity increase is found at the surface. In addition, the MLD becomes larger along the Greenland-Scotland-Iceland ridge. Global teleconnections due to AISM are studied. The AISM signal is transported with the surface current: the additional freshwater from AISM tends to enhance the northward spreading of the surface water. As a result, more warm and saline water is transported from the tropical region to the North Atlantic Ocean, resulting in warming and salt enrichment there. It would take about 30 40 years to establish a systematic noticeable change in temperature, salinity and MLD in the North Atlantic Ocean according to this study. The changes in hydrography due to increasing AISM are compared with observations. Consistency suggests that increasing AISM is highly likely a major contributor to the recent observed changes in the Southern Ocean. In addition, the AISM might contribute to the salinity contrast between the North Atlantic and North Pacific, which is important for the global thermohaline circulation.

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Resumen: El presente estudio analiza el rol de la simpatía en la conducta prosocial infantil, determinando posibles diferencias en función del sexo y la edad. La muestra estuvo constituida por 275 niños de ambos sexos, escolarizados, de 6 y 7 años de edad de las provincias de Chaco y Corrientes, Argentina. Previo consentimiento informado de los padres, se administró la Escala de simpatía para niños de 6 y 7 años de edad, de Oros (2006), el Prosocial BehaviorScale de Caprara y Pastorelli (1993) traducido y adaptado al español por Del Barrio, Moreno y López, (2001), y el Cuestionario de Conducta Prosocial (PBQ) de Weiner y Duveen (1981).En función de los objetivos propuestos, se realizó un análisis univariado de varianza (ANOVA) y análisis multivariados de variancia (MANOVAs). Los diferentes resultados obtenidos, se discuten en función de los desarrollos teóricos y empíricos encontrados hasta el momento, hallando una consistencia general entre los mismos

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La lectura “política” de la Biblia / Armando J. Levoratti -- Las opciones misionales en el Chaco del siglo XVII ¿Evangelización o guerra justa? / Ernesto J. A. Maeder -- Dios y el hombre creador. Método teológico para un análisis estructural de “Amadeus”, film de Milos Forman y Peter Shaffer / Fernando Ortega -- Crónica de la semana anual de estudio y reflexión teológica de la Sociedad Argentina de Teología -- Notas bibliográficas -- Libros recibidos -- Crónica de la Facultad -- Índice del Tomo XXIII

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El 19 de noviembre de 2015 se realizó en la Facultad de Derecho de la Pontificia Universidad Católica Argentina un workshop organizado por la Cátedra Internacional Ley Natural y Persona Humana de esa Facultad, sobre el tema “De F.A.L. a M.A.D.: el derecho a la vida en la Corte Suprema de Justicia de la Nación”. El encuentro fue coordinado por el Prof. Carlos Gabriel Maino y comenzó con una bienvenida a cargo del Decano, Dr. Daniel Herrera. Luego expuso el Dr. Alfonso Santiago, Profesor de la Universidad Austral, quien desarrolló tres temas: a) la protección constitucional y convencional del derecho a la vida; b) la jurisprudencia previa de la Corte Suprema; c) los casos “F.A.L.” y “M.A.D.”. Respecto a la protección constitucional y convencional del derecho a la vida, Santiago se refirió a la importancia del art. 29 de la Constitución Nacional. También señaló la protección expresa que surge del art. 4º de la Convención Americana de Derechos Humanos y del art. 6º de la Convención sobre los Derechos del Niño. Resaltó la claridad y fuerza de los textos convencionales, especialmente en cuanto prohíben que un ser humano sea privado de la vida arbitrariamente. También destacó la mención al carácter intrínseco del derecho a la vida y a la obligación del Estado de protegerlo en la máxima medida posible...

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The Argentine Republic is situated in the southernmost portion of the American continent, occupying over 2,785,600 km2 not including the Antarctic territory. The country ranges from subtropical areas (21º46’S) to subantarctic regions (55º03’S), extending latitudinally over about 4,000 km. It possesses significant latitudinal and altitudinal variation (33º of latitudinal range, and heights from Bajo de San Julián in Santa Cruz province at 105 m below sea level, up to Mt. Aconcagua, 6,959 m over sea level), as well as two gradients of physical variability, extending in north-south and east-west directions. Owing to these features, the country presents a wide range of climates and soil types, being one of the countries with greatest diversity of biogeographical units (Lean et al., 1990, In: Bertonatti & Corcuera, 2000). There are four main hydrographic systems: Río de la Plata basin, the Atlantic and Pacific drainages, and several endorrheic systems. Within these basins, the ichthyofaunistic assemblage is well represented, with different magnitude in accordance with the different taxonomic groupings and regions considered. From an ichthyogeographic standpoint, and according to the works of Ringuelet (1975) and Arratia et al. (1983), Argentina is included in the Brasilic and Austral Subregions. The first of these is represented by two domains: the Andean Domain, comprising the southernmost portion of Titicaca Province, and the Paranensean Domain, including part of Alto Paraná and Paranoplatensean Provinces. The Austral Subregion is represented in Argentina by the Subandean-Cuyan and Patagonian Provinces. The present survey indicates that there are about 441 fish species in Argentina, distributed throughout the country; this number represents less than 10% of the total fish species occurring in the Neotropical Region. There is a recognizable trend of faunal impoverishment, both in North-South and East-West direction, reaching its maximum expression in the provinces of Tierra del Fuego (situated at approximately 52º30’S to 55ºS, and 65ºS to 68º50’W) and San Juan (approximately 28º50’S and 67ºW to 70º45’W), which have 4 and 5 fish species respectively. In north-south direction, one of the regional indicators of this phenomenon is the Salado river basin in Buenos Aires province, which constitutes the southern distributional boundary for the majority of the paranoplatensean ichthyofauna; 12 of the families occurring in the Paraná-Plata system are absent from this pauperized paranensean ichthyofaunal assemblage. Most of the continental fish fauna of Argentina belongs to the primary division of Myers (1949), while some elements are included in the secondary division and others in an amphibiotic or ‘marine penetration’ category. This ichthyofaunistic scope encompasses a wide range of morphological, biological, ecological and ethological types (benthic and pelagic, migrating and sedentary, haematophagous or parasites, annual species, inhabitants of plains or heights, estivation-adapted, etc.) inhabiting different regions within the national territory.

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La historia de las instituciones está construida por una serie de hechos y determinaciones de sus protagonistas. En algunos casos, estos momentos son registrados en documentos dispersos, mientras que una gran mayoría están sumergidos en el tiempo con la amenaza de no poder rescatarlos. Esta situación, entre otras cosas, impide a las generaciones futuras la comprensión del pasado, ya que no cuentan con los elementos básicos para analizar y entender los hechos originados por las mujeres y hombres que conformaron dicha historia. En este documento el Programa para el estudio y uso sustentable de la biota austral (ProBiota) reúne en cinco capítulos una serie de hechos y documentos que son parte del patrimonio histórico de nuestro país. I - Actos realizados en la Facultad de Ciencias Naturales y Museo (FCNyM, UNLP) generados por la División Zoología Vertebrados y el Instituto de Limnología “Dr. Raúl A. Ringuelet”. II - Semblanzas de algunos limnólogos argentinos. III - Reseñas de instituciones y escritos referidos a aspectos históricos de la limnología en nuestro país. IV - Sociedades y eventos relacionados a esta disciplina. V - Obras, documentos y revistas. Los documentos publicados son citados formalmente, mientras que las alocuciones se presentan con su título y el nombre del autor al final. Esta modesta contribución tiene como objetivo ser el inicio de sucesivas recopilaciones que confluyan en un documento exhaustivo y profundo de la rica historia de las ciencias naturales en la Argentina.

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En el transcurso del año 2007 se cumplieron cuarenta años de la publicación de la obra Los peces argentinos de agua dulce de Raúl A. Ringuelet, Raúl H. Arámburu y Armonía Alonso de Arámburu, la que representó un hito dentro de la ictiología nacional y regional. Por este motivo, el Programa para el estudio y uso sustentable de la Biota Austral Probiota), como un modesto homenaje a sus autores, quiere rescatar parte de la misma, ya que su reedición total para nosotros es hoy un objetivo imposible de cumplir. Para ello, hemos elegido reproducir su iconografía la cuál esta compuesta de 10 láminas y 37 figuras cuyos autores fueron A. Alonso de Arámburu, Carmen Castellano, Irma Cicchini, María E. Costa, María L. Fuster, E. Maristany, Ana Thörmalen y Carlos. A. Tremouilles. En este documento se agrupan las láminas en una primera sección y posteriormente las figuras, para finalizar con un apéndice que contiene la lista de las especies mencionadas con su sistemática actualizada. Este es otro paso dirigido a la consolidación de nuestra disciplina, ya que manteniendo siempre el recuerdo vivo del pasado lograremos afianzar el presente, lo que nos permitirá planificar con fundamentos nuestro futuro. (PDF tiene 60 paginas.)

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Este trabajo es el resultado de la tesis de Maestría en Recursos Naturales y Medio Ambiente (Orientación Recursos Faunísticos), realizada por el autor en la Facultad de Ciencias Naturales de la Universidad Nacional de Salta y bajo la dirección del Dr. Sergio Gustavo Mosa. La pesca artesanal con fines comerciales es practicada en el sector salteño del Río Bermejo desde hace décadas, por pobladores de localidades ribereñas como Orán, Embarcación y Rivadavia Banda Sur, los cuales pescan hasta el límite Salta – Chaco, dependiendo de la época del año. Esta pesquería se desarrolló por más de 50 años fuera del marco de las normas legales vigentes en la provincia (Ley 5513), siendo una actividad marginal perseguida por la justicia, y mal vista por la opinión pública en general. Entre Julio de 2001 y Julio de 2003, la Cooperativa de Pescadores Artesanales “La Unión” fue habilitada como empresa pesquera comercial de tipo artesanal por la Secretaria de Medio Ambiente y Desarrollo Sustentable de Salta. El monitoreo de esta actividad fue efectuado por la Cátedra de Piscicultura y Pesquerías (IRNED) de la Facultad de Ciencias Naturales de la Universidad Nacional de Salta. Las reglamentaciones y regulaciones legales de esta actividad se tomaron originariamente bajo el principio de precaución ante la falta de conocimiento científico. A la luz de la nueva información colectada, algunas de ellas resultan contrarias al principio prioritario de la gestión pesquera, el cual propone: Obtener la mejor utilización posible del recurso en provecho de la comunidad, recordando que mejor utilización implica mayor captura, mejor precio, más ganancias y más empleo. La presente Tesis de Maestría demuestra la sustentabilidad de la pesquería artesanal en el Bermejo, tanto desde a) el punto de vista biológico, analizando las capturas en función de las normas y reglamentaciones legales vigentes y de la biología y hábitos reproductivos de cada especie, como desde b) el punto de vista económico, teniendo en cuenta la relación costo-beneficio y las posibles alternativas para optimizar la misma. Asimismo, formula una serie de recomendaciones destinadas a mejorar la gestión pesquera. Para las 4 especies más importantes de la pesquería: sábalo Prochilodus lineatus, surubí Pseudoplatystoma coruscans, dorado Salminus brasiliensis y bagre blanco Pimelodus albicans, a) los cupos asignados para la captura anual por especie no son alcanzados; b) las tallas mínimas de captura observadas superan las tallas mínimas de captura autorizadas; c) las tallas medias de captura se encuentran muy por encima de las tallas medias de madurez sexual; d) la captura exclusiva de ejemplares maduros para todas las especies prueba que el grueso del stock pesquero ha podido superar por lo menos un evento reproductivo antes de ser capturado; e) el actual período de veda resulta demasiado amplio por lo que uno de dos meses, de mediados de noviembre a mediados de enero resultaría biológicamente adecuado. En cuanto a la sustentabilidad económica de la actividad, cada unidad económica de pesca debe realizar entre 45 y 50 excursiones de pesca anuales para obtener rendimientos económicos equivalentes a un ingreso mensual de aproximadamente $ 1000. (PDF tiene 92 paginas.)

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El 29 de abril del año próximo pasado se cumplieron veinte años del fallecimiento de Raúl Adolfo Ringuelet, quién fuera uno de los científicos más destacados que han dado las ciencias naturales de la Argentina. Salvo contadas excepciones, no hubo recordatorios sobre este acontecimiento, pero el Dr. Ringuelet es uno de los casos que no necesita de la magnanimidad y el tiempo de los mortales para tenerlo presente, ya que la vigencia y el peso de su obra, hacen cumplir con aquello de que “mientras el recuerdo permanece, la muerte no existe”. El Programa para el Estudio y Uso Sustentable de la Biota Austral (ProBiota) quiere recordarlo reproduciendo la publicación de una serie de conferencias dictadas en su juventud, durante 1943 y 1944, en LS 11 Radio Provincia de Buenos Aires y que fueron publicadas en 1946 bajo el título de “Temas de Ciencias Naturales”. En ese año, Raúl A. Ringuelet contaba con treinta dos años y el mundo se encontraba en su mayor parte lacerado y bajo ruinas por la conducta recurrente de la “especie hipócrita” que, en nombre de las ideologías y la paz universal, había concretado la matanza de varios millones de personas. En nuestro país se asistía al nacimiento de un nuevo movimiento histórico y el comienzo de profundos desencuentros en nuestra sociedad, los cuales, lamentablemente, aún no han terminado. En esta década la ciencia argentina sería destacada con el Premio Nóbel a través del Dr. Bernardo Houssay y en las ciencias naturales se habían publicado, entre otras obras, los rasgos principales de la Fitogeografía argentina de J. Frenguelli, la Zoogeografía de Cabrera y Yepes, la última entrega del catalógo sistemático de las aves de Argentina de Steullet y Deautier, y el estudio de la Selva Marginal de Punta Lara de A. L. Cabrera (hijo) y G. Dawson. La lectura de estas conferencias, un total de diez, nos muestra, ya entonces, el espíritu rico, inquieto y polifacético de Raúl A. Ringuelet, el cuál lo distinguiría pocos años después. En algunas de ellas realiza la reseña de la vida y obra de diferentes científicos y naturalistas de nuestro país; en las restantes, expresa ingeniosamente conceptos precursores sobre biodiversidad, conservación y manejo de los recursos naturales y su transferencia a los diferentes niveles de la sociedad. Finalmente, desde ProBiota consideramos que la trascripción de este tipo de documentos constituye un aporte para aquellos interesados en la historia de las ciencias naturales y, asimismo, una contribución para que nuestras jóvenes generaciones de biólogos y naturalistas posean una noción más clara de quienes marcaron rumbos e hicieron escuela en nuestra disciplina con un genuino sentido nacional.