Revista de Literaturas Modernas

La Revista de Literaturas Modernas (RLM) fue creada con el objetivo de reunir en una sola entrega anual una visión de conjunto del trabajo del entonces llamado Instituto de Lenguas y Literaturas Modernas de la Facultad de Filosofía y Letras (Universidad Nacional de Cuyo) y comenzó a aparecer anualmente desde 1956. En ella se priorizan las publicaciones circunscriptas a la especialidad de cada una de las secciones del Instituto que posteriormente se bifurcó en dos: Lingüística y Literaturas Modernas (área que sigue editando la RLM). Desde sus comienzos, esta publicación da a conocer los trabajos de los profesores de la Facultad, y también de colaboradores del exterior, cuyos aportes han sido y son acordes con la temática y jerarquía propuestas como objetivo. En sus artículos y notas, se apunta a relacionar la literatura con otras disciplinas para posibilitar un análisis dinámico de los textos, enmarcados en su contexto de producción cultural. Si bien la periodicidad se vio interrumpida en algunas ocasiones, actualmente existe el objetivo de publicar un número por año, con la meta siempre presente de su difusión internacional. Por último, cabe aclarar que las siglas que abrevian su título deben ser utilizadas en citas, notas a pie de página y referencias bibliográficas.

Stable carbon and hydrogen isotope record of n-Alkanoic acids of sediment core SO189/2_144KL

The Indo-Pacific Warm Pool (IPWP) is a key site for the global hydrologic cycle, and modern observations indicate that both the Indian Ocean Zonal Mode (IOZM) and the El Niño Southern Oscillation exert strong influence on its regional hydrologic characteristics. Detailed insight into the natural range of IPWP dynamics and underlying climate mechanisms is, however, limited by the spatial and temporal coverage of climate data. In particular, long-term (multimillennial) precipitation patterns of the western IPWP, a key location for IOZM dynamics, are poorly understood. To help rectify this, we have reconstructed rainfall changes over Northwest Sumatra (western IPWP, Indian Ocean) throughout the past 24,000 y based on the stable hydrogen and carbon isotopic compositions (dD and d13C, respectively) of terrestrial plant waxes. As a general feature of western IPWP hydrology, our data suggest similar rainfall amounts during the Last Glacial Maximum and the Holocene, contradicting previous claims that precipitation increased across the IPWP in response to deglacial changes in sea level and/or the position of the Intertropical Convergence Zone. We attribute this discrepancy to regional differences in topography and different responses to glacioeustatically forced changes in coastline position within the continental IPWP. During the Holocene, our data indicate considerable variations in rainfall amount. Comparison of our isotope time series to paleoclimate records from the Indian Ocean realm reveals previously unrecognized fluctuations of the Indian Ocean precipitation dipole during the Holocene, indicating that oscillations of the IOZM mean state have been a constituent of western IPWP rainfall over the past ten thousand years.

Geochemistry of lavas from the Lau-Tonga arc and back-arc system

Detailed comparison of mineralogy, and major and trace geochemistry are presented for the modern Lau Basin spreading centers, the Sites 834-839 lavas, the modern Tonga-Kermadec arc volcanics, the northern Tongan boninites, and the Lau Ridge volcanics. The data clearly confirm the variations from near normal mid-ocean-ridge basalt (N-MORB) chemistries (e.g., Site 834, Central Lau Spreading Center) to strongly arc-like (e.g., Site 839, Valu Fa), the latter closely comparable to the modern arc volcanoes. Sites 835 and 836 and the East Lau Spreading Center represent transitional chemistries. Bulk compositions range from andesitic to basaltic, but lavas from Sites 834 and 836 and the Central Lau Spreading Center extend toward more silica-undersaturated compositions. The Valu Fa and modern Tonga-Kermadec arc lavas, in contrast, are dominated by basaltic andesites. The phenocryst and groundmass mineralogies show the strong arc-like affinities of the Site 839 lavas, which are also characterized by the existence of very magnesian olivines (up to Fo90-92) and Cr-rich spinels in Units 3 and 6, and highly anorthitic plagioclases in Units 2 and 9. The regional patterns of mineralogical and geochemical variations are interpreted in terms of two competing processes affecting the inferred magma sources: (1) mantle depletion processes, caused by previous melt extractions linked to backarc magmatism, and (2) enrichment in large-ion-lithophile elements, caused by a subduction contribution. A general trend of increasing depletion is inferred both eastward across the Lau Basin toward the modern arc, and northward along the Tongan (and Kermadec) Arc. Numerical modeling suggests that multistage magma extraction can explain the low abundances (relative to N-MORB) of elements such as Nb, Ta, and Ti, known to be characteristic of island arc magmas. It is further suggested that a subduction jump following prolonged slab rollback could account for the initiation of the Lau Basin opening, plausibly allowing a later influx of new mantle, as required by the recognition of a two-stage opening of the Lau Basin.

Guidance in the diversity: a glance from Latin America

Guidance and Diversity, for the majority of the European countries and North America , are related to the attention to children and young people with special necessities, that are attend in an educative institution and for those who are elaborated educative programs directed to obtain one better adaptation to the prevailing social system. In most of the cases is considered that the problematic of the special necessities is imputable to genetic or personal factors that only respond to internal factors to the individuals that display them avoiding the external factors that in some cases can be more decisive determinants at the time of the conductual manifestation. In this work is pleaded because the professionals of the Guidance, as much private or public scenes of the European countries, make more specific considerations at the time of taking care of children, young people and adults, as immigrants, coming of Latin America . In an ample sense one sets out to make Guidance in the Diversity more than Guidance for the Diversity under the conception of a Guidance for All which implies the elimination of the expression "special necessities", whose connotation in our countries is not most appropriate, and than it includes the idea of an Ethnic Guidance. Perhaps the best way of boarding of these conceptions is promoting a process of Guidance from the School and not only in the School.

Formas de abandonar un laberinto : Sor Juana y la figura sorjuanina del escritor americano

Tradicionalmente, la figura de sor Juana Inés de la Cruz (1648-1695) ocupa un lugar central en la literatura y la crítica latinoamericanas y -de manera muy especial- mexicanas. Mujer y monja desiguales, poeta e 'inteligencia americana' inigualables, esa figura no ha tardado en construir cierto mito en torno de su obra, como cierta 'clave' que vela o desvela los caminos que conducen al corazón no sólo de su singular literatura sino de su borrascosa historia. Curiosa pero no casualmente, más de una vez la mexicana -en sus poemas así como en sus cartas- ha desalentado esas imágenes e ideas que son, también o principalmente, las de cierta concepción de la escritura y la lectura. En este sentido, el siguiente artículo se propone trazar las coordenadas de dicho problema (el mito sorjuanino y la desmitificación de sor Juana) a fin de deslindar dos aspectos (inseparables) de dicho fenómeno: el que hace a la lectura crítica e incluso a la edición y fijación de sus textos; y el que refiere a la concepción y práctica de la literatura en América Latina en uno de sus momentos inaugurales: el siglo XVII, y a través de una de sus figuras más elusivas: la sorjuanina

Interculturalidad y dinámicas comerciales : Interacciones entre indígenas y españoles en la América colonial hispana

En este artículo se plantea el análisis de la complejidad de las relaciones comerciales entre castellanos e indígenas a lo largo del periodo colonial. Para ello, se comparará la práctica sobre el terreno desde el siglo XVI hasta el XVIII con los debates teóricos medievales y modernos alrededor del comercio intercultural y de las diferencias en las formas de vida rural y urbana. Se tratará, asimismo, la dualidad campo-ciudad en relación con el traslado a América del importante papel que el pensamiento occidental otorgó tradicionalmente a la ciudad como núcleo de civilización y como foco irradiador de la misma. Dicho planteamiento arroja una perspectiva muy compleja sobre las relaciones interculturales, ya que ambos grupos -castellanos e indígenas- actuaron de maneras muy diversas según el contexto social, político y económico de cada momento. Frente a la idea de una actitud siempre hostil entre los dos grupos, se presenta un panorama de búsqueda de la amistad por medios pacíficos, entre los que se destaca el comercio como principal catalizador

Size-related stable isotope changes in Late Cretaceous and Recent planktic foraminifera from the western tropical Atlantic

The paleoecology of Cretaceous planktic foraminifera during the Late Cenomanian to Coniacian period (~95-86 Ma) remains controversial since much of the tropical marine record is preserved as chalk and limestone with uncertain geochemical overprints. Here we present delta13C and delta18O data from sieve size fractions of monospecific samples of exceptionally well preserved planktic foraminifera recovered during Ocean Drilling Program Leg 207 (Demerara Rise, western tropical Atlantic). Our results suggest that all species studied (Hedbergella delrioensis, Heterohelix globulosa, Marginotruncana sinuosa, Whiteinella baltica) grew primarily in surface waters and did not change their depth habitat substantially during their life cycle. Comparison of size-related ontogenetic trends in delta13C in Cretaceous and modern foraminifera further suggests that detection of dinoflagellate photosymbiosis using delta13C is confounded by physiological effects during the early stages of foraminifer growth, raising doubts about previous interpretations of photosymbiosis in small foraminifera species. We propose that obligate photosymbiosis involving dinoflagellates may not have evolved until the Campanian or Maastrichtian since our survey of Cenomanian-Coniacian species does not find the delta18O and delta13C size-related trends observed in modern foraminifer-dinoflagellate symbioses.

Guidance in the diversity: a glance from Latin America

Guidance and Diversity, for the majority of the European countries and North America , are related to the attention to children and young people with special necessities, that are attend in an educative institution and for those who are elaborated educative programs directed to obtain one better adaptation to the prevailing social system. In most of the cases is considered that the problematic of the special necessities is imputable to genetic or personal factors that only respond to internal factors to the individuals that display them avoiding the external factors that in some cases can be more decisive determinants at the time of the conductual manifestation. In this work is pleaded because the professionals of the Guidance, as much private or public scenes of the European countries, make more specific considerations at the time of taking care of children, young people and adults, as immigrants, coming of Latin America . In an ample sense one sets out to make Guidance in the Diversity more than Guidance for the Diversity under the conception of a Guidance for All which implies the elimination of the expression "special necessities", whose connotation in our countries is not most appropriate, and than it includes the idea of an Ethnic Guidance. Perhaps the best way of boarding of these conceptions is promoting a process of Guidance from the School and not only in the School.

Formas de abandonar un laberinto : Sor Juana y la figura sorjuanina del escritor americano

Tradicionalmente, la figura de sor Juana Inés de la Cruz (1648-1695) ocupa un lugar central en la literatura y la crítica latinoamericanas y -de manera muy especial- mexicanas. Mujer y monja desiguales, poeta e 'inteligencia americana' inigualables, esa figura no ha tardado en construir cierto mito en torno de su obra, como cierta 'clave' que vela o desvela los caminos que conducen al corazón no sólo de su singular literatura sino de su borrascosa historia. Curiosa pero no casualmente, más de una vez la mexicana -en sus poemas así como en sus cartas- ha desalentado esas imágenes e ideas que son, también o principalmente, las de cierta concepción de la escritura y la lectura. En este sentido, el siguiente artículo se propone trazar las coordenadas de dicho problema (el mito sorjuanino y la desmitificación de sor Juana) a fin de deslindar dos aspectos (inseparables) de dicho fenómeno: el que hace a la lectura crítica e incluso a la edición y fijación de sus textos; y el que refiere a la concepción y práctica de la literatura en América Latina en uno de sus momentos inaugurales: el siglo XVII, y a través de una de sus figuras más elusivas: la sorjuanina

Interculturalidad y dinámicas comerciales : Interacciones entre indígenas y españoles en la América colonial hispana

En este artículo se plantea el análisis de la complejidad de las relaciones comerciales entre castellanos e indígenas a lo largo del periodo colonial. Para ello, se comparará la práctica sobre el terreno desde el siglo XVI hasta el XVIII con los debates teóricos medievales y modernos alrededor del comercio intercultural y de las diferencias en las formas de vida rural y urbana. Se tratará, asimismo, la dualidad campo-ciudad en relación con el traslado a América del importante papel que el pensamiento occidental otorgó tradicionalmente a la ciudad como núcleo de civilización y como foco irradiador de la misma. Dicho planteamiento arroja una perspectiva muy compleja sobre las relaciones interculturales, ya que ambos grupos -castellanos e indígenas- actuaron de maneras muy diversas según el contexto social, político y económico de cada momento. Frente a la idea de una actitud siempre hostil entre los dos grupos, se presenta un panorama de búsqueda de la amistad por medios pacíficos, entre los que se destaca el comercio como principal catalizador

Organic-walled dinoflagellate cysts analysis and statistical analysis of 116 surface sediment samples from the eastern Indian Ocean

Assemblages of organic-walled dinoflagellate cysts (dinocysts) from 116 marine surface samples have been analysed to assess the relationship between the spatial distribution of dinocysts and modern local environmental conditions [e.g. sea surface temperature (SST), sea surface salinity (SSS), productivity] in the eastern Indian Ocean. Results from the percentage analysis and statistical methods such as multivariate ordination analysis and end-member modelling, indicate the existence of three distinct environmental and oceanographic regions in the study area. Region 1 is located in western and eastern Indonesia and controlled by high SSTs and a low nutrient content of the surface waters. The Indonesian Throughflow (ITF) region (Region 2) is dominated by heterotrophic dinocyst species reflecting the region's high productivity. Region 3 is encompassing the area offshore north-west and west Australia which is characterised by the water masses of the Leeuwin Current, a saline and nutrient depleted southward current featuring energetic eddies.

Guidance in the diversity: a glance from Latin America

Guidance and Diversity, for the majority of the European countries and North America , are related to the attention to children and young people with special necessities, that are attend in an educative institution and for those who are elaborated educative programs directed to obtain one better adaptation to the prevailing social system. In most of the cases is considered that the problematic of the special necessities is imputable to genetic or personal factors that only respond to internal factors to the individuals that display them avoiding the external factors that in some cases can be more decisive determinants at the time of the conductual manifestation. In this work is pleaded because the professionals of the Guidance, as much private or public scenes of the European countries, make more specific considerations at the time of taking care of children, young people and adults, as immigrants, coming of Latin America . In an ample sense one sets out to make Guidance in the Diversity more than Guidance for the Diversity under the conception of a Guidance for All which implies the elimination of the expression "special necessities", whose connotation in our countries is not most appropriate, and than it includes the idea of an Ethnic Guidance. Perhaps the best way of boarding of these conceptions is promoting a process of Guidance from the School and not only in the School.

Strontium chemistry of anhydrite from DSDP/ODP Hole 504B

A unique record of the chemical evolution of seawater during hydrothermal recharge into oceanic crust is preserved by anhydrite from the volcanic sequences and sheeted dike complex in ODP Hole 504B. Chemical and isotopic analyses 87Sr/86Sr, delta18O, delta34S of anhydrite constrain the changing composition of fluids due to reaction with basalt. There is a general trend of decreasing 87Sr/86Sr of anhydrite, corresponding to the minor incorporation of basaltic strontium with depth in the volcanic rocks. 87Sr/86Sr ratios decrease rapidly with depth in the dikes to values identical to host basalt (0.7029). Sr/Ca ratios (<0.1 mmol/mol) suggest that recharge fluids have very low Sr concentrations and fluids evolve by first precipitating Sr-bearing phases before extensive exchange of Sr with the host basalt. There is a background trend of decreasing sulfate delta18O with depth from +12-13? in the lower volcanics to +7? in the lower sheeted dikes recording an increase in recharge fluid temperature from c. 150° to c. 250°C, and confirming the presence of sulfate in hydrothermal fluids at elevated temperatures. From the amount of anhydrite recovered from Hole 504B and the amount of seawater sulfur that has been reduced to sulfide, a minimum seawater recharge flux can be calculated. This value is 4-25 times lower than estimates of high-temperature fluid fluxes based on either thermal constraints or global chemical budgets and suggests that there is significant deficit of seawater-derived sulfur in the oceanic crust. Only a minor proportion of the seawater that percolates into the crust near the axis is heated to high temperatures and exits as black smoker-type fluids. A significant proportion of the axial heat loss must be advected at 200-250°C by sulfate-bearing hydrothermal solutions that egress diffusely from the crust. These fluids penetrate into the dikes and exchange both heat and chemical tracers without the extensive clogging of porosity by anhydrite precipitation, which would halt hydrothermal circulation for any reasonable fluid flux. The heating of the major proportion of hydrothermal fluids to only moderate temperatures (c. 250°C) reconciles estimates of hydrothermal fluxes derived from thermal models and global geochemical budgets. The flux of hydrothermal sulfate would be of a magnitude similar to the riverine input, and oxygen-isotopic exchange at 200-250°C between dissolved sulfate and recharge fluids during hydrothermal circulation provides a mechanism to continuously buffer seawater sulfate oxygen to the light isotopic composition observed.