Tradición Clásica en Iberoamerica

La Tradición Clásica en Iberoamérica presenta la relación de los países sudamericanos con Europa occidental, desde el punto de vista de la vinculación estrictamente cultural. El estudio incluye dieciocho países de habla hispana, uno de habla portuguesa y, en cierto aspecto, Puerto Rico. Se señalan tres etapas culturales que presentan diferentes inidencias de la antigüedad clásica en Iberoamérica. Ellas son: 1. La Conquista, 2. La independenicia y 3. El siglo XX en adelante. Iberoamérica constituye el mito de la utopía descubierta por Europa y retiene en su esencia vital el sentimiento utópico por la búsqueda constante de la unidad en la pluralidad.

Biocombustibles en Argentina, Brasil y Colombia : Avances y limitaciones

Los biocombustibles introducen espacios agrícolas en la producción energética. Luego modifican la gobernanza de las redes energéticas y de los territorios productivos. Las principales críticas a los biocombustibles se dirigen a su producción a partir de cultivos tradicionales, pero interesa preguntarse también sobre la sostenibilidad de su producción a partir de cultivos alternativos, que no competirían con los cultivos alimentarios, puesto que se ubicarían en regiones agrícolas marginales. El texto trata sobre las producciones de biocombustibles de los países de América del Sur, en sus contextos internacionales, nacionales y locales. Se profundiza la mirada sobre Argentina, Brasil y Colombia, líderes continentales en el sector. Se analizan la evolución del mercado energético, los actores involucrados y las políticas implementadas. A otra escala, se plantea la puesta en marcha de las cadenas de biocombustibles alternativos.

Panorama de la literatura griega en Iberoamérica (1767-1850)

En este trabajo se estudian los escasos testimonios que encontramos de la literatura griega en Iberoamérica, desde la expulsión de los jesuitas (1767) hasta mediados del siglo XIX, coincidiendo con los últimos años del periodo colonial español y los primeros de la independencia de la mayoría de los países sudamericanos. El conocimiento de los autores griegos es indirecto, salvo contadas excepciones, y el estudio del griego avanza tímidamente en algunos países, coincidiendo también con el tipo de país que los próceres de la patria pretenden construir

Tradición Clásica en Iberoamerica

La Tradición Clásica en Iberoamérica presenta la relación de los países sudamericanos con Europa occidental, desde el punto de vista de la vinculación estrictamente cultural. El estudio incluye dieciocho países de habla hispana, uno de habla portuguesa y, en cierto aspecto, Puerto Rico. Se señalan tres etapas culturales que presentan diferentes inidencias de la antigüedad clásica en Iberoamérica. Ellas son: 1. La Conquista, 2. La independenicia y 3. El siglo XX en adelante. Iberoamérica constituye el mito de la utopía descubierta por Europa y retiene en su esencia vital el sentimiento utópico por la búsqueda constante de la unidad en la pluralidad.

Geochemistry and Nd-Pb isotope ratios of sediments from the Lesser Antilles arc

The Lesser Antilles arc is a particularly interesting island arc because it is presently very active, it is located perpendicular to the South American continent and its chemical and isotopic compositions display a strong north-south gradient. While the presence in the south of a thick pile of sedimentary material coming from the old South American continent has long been suspected to explain the geochemical gradient, previous studies failed to demonstrate unambiguously a direct link between the arc lava compositions and the subducted sediment compositions. Here, we present new Nd, Sm, Th, U and Pb concentrations and Nd-Pb isotopic data for over 60 sediments from three sites located in the fore arc region of the Lesser Antilles arc. New data for DSDP Site 543 drill core located east of Dominica Island complement the data published by White et al. (1985, doi:10.1016/0016-7037(85)90082-1) and confirm their relatively uniform isotopic compositions (i.e., 206Pb/204Pb between 19.13 and 19.53). In contrast, data obtained on DSDP Site 144 located further south, on the edge of the South American Rise and on sediments from Barbados Island are much more variable (206Pb/204Pb ranges from 18.81 to 27.69). The very radiogenic Pb isotopic compositions are found in a 60 m thick black shale unit, which has no age equivalent in the Site 543 drill core. We interpret the peculiar composition of the southern sediments as being due to two factors, (a) the proximity of the South American craton, which contributes coarse grain old detrital material that does not travel far from the continental shelf, and (b) the presence of older sediments including the thick black shale unit formed during Oceanic Anoxic events 2 and 3. The north-south isotopic change known along the Lesser Antilles arc can be explained by the observed geographical changes in the composition of the subducted sediments. About 1% contamination of the mantle wedge by Site 543 sediments explains the composition of the northern islands while up to 10% sediments like those of Site 144 is required in the source of the southern island lavas. The presence of black shales in the subducted pile provides a satisfactory explanation for the very low Delta8/4 values that characterize the Lesser Antilles arc.

Biocombustibles en Argentina, Brasil y Colombia : Avances y limitaciones

Los biocombustibles introducen espacios agrícolas en la producción energética. Luego modifican la gobernanza de las redes energéticas y de los territorios productivos. Las principales críticas a los biocombustibles se dirigen a su producción a partir de cultivos tradicionales, pero interesa preguntarse también sobre la sostenibilidad de su producción a partir de cultivos alternativos, que no competirían con los cultivos alimentarios, puesto que se ubicarían en regiones agrícolas marginales. El texto trata sobre las producciones de biocombustibles de los países de América del Sur, en sus contextos internacionales, nacionales y locales. Se profundiza la mirada sobre Argentina, Brasil y Colombia, líderes continentales en el sector. Se analizan la evolución del mercado energético, los actores involucrados y las políticas implementadas. A otra escala, se plantea la puesta en marcha de las cadenas de biocombustibles alternativos.

Nd, Sm and carbon isotopic data for samples from ODP Legs 115, 145, 171, and 207

Late Cretaceous fish debris from Demerara Rise exhibits a dramatic positive excursion of 8 e-Nd units during ocean anoxic event 2 (OAE2) that is superimposed on extremely low e-Nd(t) values (-14 to -16.5) observed throughout the rest of the studied interval. The OAE2 e-Nd excursion is the largest yet documented in marine sediments, and the majority of the shift is estimated to have occurred over <20 k.y. Low background e-Nd values on Demerara Rise are explained as the Nd isotopic signature of the South American craton, whereas eruptions of the Caribbean large igneous province or enhanced mixing of intermediate waters in the North Atlantic could have caused the excursion.

Panorama de la literatura griega en Iberoamérica (1767-1850)

En este trabajo se estudian los escasos testimonios que encontramos de la literatura griega en Iberoamérica, desde la expulsión de los jesuitas (1767) hasta mediados del siglo XIX, coincidiendo con los últimos años del periodo colonial español y los primeros de la independencia de la mayoría de los países sudamericanos. El conocimiento de los autores griegos es indirecto, salvo contadas excepciones, y el estudio del griego avanza tímidamente en algunos países, coincidiendo también con el tipo de país que los próceres de la patria pretenden construir

Tradición Clásica en Iberoamerica

La Tradición Clásica en Iberoamérica presenta la relación de los países sudamericanos con Europa occidental, desde el punto de vista de la vinculación estrictamente cultural. El estudio incluye dieciocho países de habla hispana, uno de habla portuguesa y, en cierto aspecto, Puerto Rico. Se señalan tres etapas culturales que presentan diferentes inidencias de la antigüedad clásica en Iberoamérica. Ellas son: 1. La Conquista, 2. La independenicia y 3. El siglo XX en adelante. Iberoamérica constituye el mito de la utopía descubierta por Europa y retiene en su esencia vital el sentimiento utópico por la búsqueda constante de la unidad en la pluralidad.

Biocombustibles en Argentina, Brasil y Colombia : Avances y limitaciones

Los biocombustibles introducen espacios agrícolas en la producción energética. Luego modifican la gobernanza de las redes energéticas y de los territorios productivos. Las principales críticas a los biocombustibles se dirigen a su producción a partir de cultivos tradicionales, pero interesa preguntarse también sobre la sostenibilidad de su producción a partir de cultivos alternativos, que no competirían con los cultivos alimentarios, puesto que se ubicarían en regiones agrícolas marginales. El texto trata sobre las producciones de biocombustibles de los países de América del Sur, en sus contextos internacionales, nacionales y locales. Se profundiza la mirada sobre Argentina, Brasil y Colombia, líderes continentales en el sector. Se analizan la evolución del mercado energético, los actores involucrados y las políticas implementadas. A otra escala, se plantea la puesta en marcha de las cadenas de biocombustibles alternativos.

Chemical composition of basalts and minerals from basalts of the Bouvet triple junction

This study focuses on mafic volcanic rocks from the Bouvet triple junction, which fall into six geochemically distinct groups: (1) N-MORB, the most widespread type, encountered throughout the study area. (2) Subalkaline volcanics, hawaiites and mugearites strongly enriched in lithophile elements and radiogenic isotopes and composing the Bouvet volcanic rise, and compositionally similar basalts and basaltic andesites from the Spiess Ridge, generated in a deeper, fertile mantle region. (3) Relatively weakly enriched basalts, T-MORB derived by the mixing of Type 1 and 2 melts and exposed near the axes of the Mid-Atlantic, Southwest Indian, and America-Antarctic Ridges. (4) Basalts with a degree of trace lithophile element enrichment similar to the Spiess Ridge and Bouvet Island rocks, but higher in K, P, Ti, and Cr. These occur within extensional structures: the rift valley of the Southwest Indian Ridge, grabens of the East Dislocation Zone, and the linear rise between the Spiess Ridge and Bouvet volcano. Their parental melts presumably separated from plume material that spread from the main channels and underwent fluid-involving differentiation in the mantle. (5) A volcanic suite ranging from basalt to rhyolite, characterized by low concentrations of lithophile elements, particularly TiO2, and occurring on the Shona Seamount and other compressional features within the Antarctic and South American plates near the Bouvet triple junction. Unlike Types 1 to 4, which display tholeiitic differentiation trends, this suite is calc-alkaline. Its parental melts were presumably related to the plume material as well but, subsequently, they underwent a profound differentiation involving fluids and assimilated surrounding rocks in closed magma chambers in the upper mantle. Alternatively, the Shona Seamount might be a fragment of an ancient oceanic island arc. (6) Enriched basalts, distinguished from the other enriched rock types in very high P and radiogenic isotope abundances and composing a tectonic uplift near the junction of the three rifts. It thus follows that the main factors responsible for the compositional diversity of volcanic rocks in this region include (i) mantle source heterogeneity, (ii) plume activity, (iii) an intricate geodynamic setup at the triple junction giving rise to stresses in adjacent plate areas, and (iv) the geological prehistory. The slow spreading rate and ensuing inefficient mixing of the heterogeneous mantle material result in strong spatial variations in basaltic compositions.

Lead isotopes inthe Eastern Equatorial Pacific

The influence of atmospheric dust on climate and biogeochemical cycles in the oceans is well understood but poorly quantified. Glacial atmospheric dust loads were generally greater than those during the Holocene, as shown, for example, by the covariation of dust fluxes in the Equatorial Pacific and Antarctic ice cores. Nevertheless, it remains unclear whether these increases in dust flux were associated with changes in sources of dust, which would in turn suggest variations in wind patterns, climate or paleo-environment. Such questions can be answered using radiogenic isotope tracers of dust provenance. Here, we present a 160-kyr high-precision lead isotope time-series of dust input to the Eastern Equatorial Pacific (EEP) from core ODP Leg 138, Site 849 (0°11.59' N, 110°31.18' W). The Pb isotope record, combined with Nd isotope data, rules out contributions from Northern Hemisphere dust sources, north of the Intertropical Convergence Zone, such as Asia or North Africa/Sahara; similarly, eolian sources in Australia, Central America, the Northern Andes and Patagonia appear insignificant based upon the radiogenic isotope data. Fluctuations in Pb isotope ratios throughout the last 160 kyr show, instead, that South America remained the prevailing source of dusts to the EEP. There are two distinct South American Pb isotope end-members, constrained to be located in the south Central Volcanic Zone (CVZ, 22° S - 27.5° S) and the South Volcanic Zone (SVZ, 33° S - 43° S), with the former most likely originating in the Atacama Desert. Dust availability in the SVZ appears to be related to the weathering of volcanic deposits and the development of ash-derived Andosols, and influenced by local factors that might include vegetation cover. Variations in the dust fluxes from the two sources are in phase with both the dust flux and temperature records from Antarctican ice cores. We show that the forcing of dust provenance over time in the EEP overall is influenced by high-southerly-latitude climate conditions, leading to changes in the latitudinal position and strength of the South Westerlies as well as the coastal winds that blow northward along the Chilean margin. The net result is a modulation of dust emission from the Atacama Desert and the SVZ via a northward migration of the South Westerlies during cold periods and southward retreat during glacial terminations.

Mineral dust deposition in interglacial and glacial climate conditions: model results

The global aerosol/climate model ECHAM5-HAM is used in order to investigate the dust cycle for four interglacial and one glacial climate conditions. The 20-year time-slices are the pre-industrial control (CTRL), mid-Holocene (6000 years BP), last glacial inception (115000 years BP), Eemian (126000 years BP) and Last Glacial Maximum (LGM) (21000 years BP) time intervals. The study is focused on the Antarctic region. The model is able to reproduce the magnitude order of dust deposition globally for the pre-industial and LGM climates. Correlation coefficient of the natural logarithm of the observed and modeled values is 0.78 for the CTRL and 0.81 for the LGM. For the pre-industrial simulation the model overestimates observed values in Antarctica by a factor of about 2-3 due to overestimation of the Australian dust source and too high wet deposition in the Antarctica interior. In the LGM, the model underestimates dust deposition in eastern Antarctica by a factor of about 4-5 due to underestimation of the South American dust source. More records are needed to validate dust deposition for the past interglacial time-slices. The modeled results show that dust deposition in Antarctica in the past interglacial time-slices is higher than in the CTRL simulation. The largest increase of dust deposition in Antarctica is simulated for the LGM, showing about 10-fold increase compared to CTRL.

Geochemistry of terrigenous material in deep-sea sediments of the equatorial Pacific

Biological productivity in the modern equatorial Pacific Ocean, a region with high nutrients and low chlorophyll, is currently limited by the micronutrient Fe. In order to test whether Fe was limiting in the past and to identify potential pathways of Fe delivery that could drive Fe fertilization (i.e., dust delivery from eolian inputs vs. Fe supplied by the Equatorial Undercurrent), we chemically isolated the terrigenous material from sediment along a cross-equatorial transect in the central equatorial Pacific at 140°W and at Ocean Drilling Program Site 850 in the eastern equatorial Pacific. We quantified the contribution from each potential Fe-bearing terrigenous source using a suite of chemical- and isotopic discrimination strategies as well as multivariate statistical techniques. We find that the distribution of the terrigenous sources (i.e., Asian loess, South American ash, Papua New Guinea, and ocean island basalt) varies through time, latitude, and climate. Regardless of which method is used to determine accumulation rate, there also is no relationship between flux of any particular Fe source and climate. Moreover, there is no connection between a particular Fe source or pathway (eolian vs. Undercurrent) to total productivity during the Last Glacial Maximum, Pleistocene glacial episodes, and the Miocene "Biogenic Bloom". This would suggest an alternative process, such as an interoceanic reorganization of nutrient inventories, may be responsible for past changes in total export in the open ocean, rather than simply Fe supply from dust and/or Equatorial Undercurrent processes. Additionally, perhaps a change in Fe source or flux is related to a change in a particular component of the total productivity (e.g., the production of organic matter, calcium carbonate, or biogenic opal).

Stable organic carbon isotope record and total organic carbon content from the Cenomanian-Turonian boundary

Ocean Drilling Program (ODP) Leg 207 recovered expanded sections of organic-carbon-rich laminated shales on Demerara Rise (western tropical Atlantic). High-resolution organic carbon isotope and total organic carbon (TOC) records are presented, which span the Cenomanian-Turonian boundary interval (CTBI), including the Oceanic Anoxic Event (OAE) 2, from four sites oriented along a NW striking depth transect. These records represent the first high-resolution carbon isotope records across OAE 2 from the South American margin of the tropical Atlantic. Due to the scarcity of age significant fossils, the main purpose of this study was to develop a detailed carbon isotope stratigraphy in order to correlate the CTBI across the depth transect and to tie this to biostratigraphically well-defined sections in the Western Interior Basin (Pueblo, USA), boreal shelf seas (Eastbourne, England), and western Tethys (Oued Mellegue, Tunisia). All four sections studied document a 6 per mil increase of d13Corg values at the base of the CTBI, which is followed by an interval of elevated d13Corg values and a subsequent decrease. Our results supply an important stratigraphic base for subsequent paleoceanographic studies on Late Cenomanian to Early Turonian sediments from Demerara Rise and elsewhere.