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

Reference datasets and pollen record from sediment core YAK, Yakumo, SW Hokkaido

This study reconstructs middle and late Holocene vegetation and climate dynamics in the Oshima Peninsula, SW Hokkaido, using the published method of biome reconstruction and modern analogue technique applied to the Yakumo pollen record (42°17'03''N, 140°15'34''E) spanning the last 5500 years. Two previously published matrices assigning Japanese plant/pollen taxa to the major vegetation types (biomes) are tested using a newly compiled dataset of 78 surface pollen spectra from Hokkaido. With both matrices showing strengths and weaknesses in reconstructing cool mixed and temperate deciduous forests of Hokkaido, the results suggest the necessity to consider the whole list of identified terrestrial pollen taxa for generating robust vegetation reconstructions for northern Japan. Applied to the fossil pollen data, both biome-reconstruction approaches demonstrate consistently that oak-dominated cool mixed forest spread in the study region between 5.5 and 3.6 cal ka BP and was subsequently replaced by beech-dominated temperate deciduous forest. The pollen-based climate reconstruction suggests this change in the vegetation composition was caused by a shift from cooler and drier than present climate to warmer and wetter, similar to modern conditions about 3.6 cal ka BP. Comparing the pollen-based reconstruction results with the published marine records from the NW Pacific, the reconstructed vegetation and climate dynamics can be satisfactorily explained by the greater role played by the warm Tsushima Current in the Sea of Japan and in the Tsugaru Strait during the middle and late Holocene. An increase in sea surface temperatures west and south of the study site would favour air temperature rise and moisture uptake and cause an increase in precipitation and snow accumulation in the western part of Hokkaido during the late Holocene.

Ordinary and duplicate analysis from major and trace elements of ODP Holes 146-888B and 168-1027B

Oceanic sediments deposited at high rate close to continents are dominated by terrigenous material. Aside from dilution by biogenic components, their chemical compositions reflect those of nearby continental masses. This study focuses on oceanic sediments coming from the juvenile Canadian Cordillera and highlights systematic differences between detritus deriving from juvenile crust and detritus from old and mature crust. We report major and trace element concentrations for 68 sediments from the northernmost part of the Cascade forearc, drilled at ODP Sites 888 and 1027. The calculated weighted averages for each site can then be used in the future to quantify the contribution of subducted sediments to Cascades volcanism. The two sites have similar compositions but Site 888, located closer to the continent, has higher sandy turbidite contents and displays higher bulk SiO2/Al2O3 with lower bulk Nb/Zr, attributed to the presence of zircons in the coarse sands. Comparison with published data for other oceanic sedimentary piles demonstrates the existence of systematic differences between modern sediments deriving from juvenile terranes (juvenile sediments) and modern sediments derived from mature continental areas (cratonic sediments). The most striking systematic difference is for Th/Nb, Th/U, Nb/U and Th/Rb ratios: juvenile sediments have much lower ratios than cratonic sediments. The small enrichment of Th over Nb in cratonic sediments may be explained by intracrustal magmatic and metamorphic differentiation processes. In contrast, their elevated Th/U and Nb/U ratios (average values of 6.87 and 7.95, respectively) in comparison to juvenile sediments (Th/U ~ 3.09, Nb/U ~ 5.15) suggest extensive U and Rb losses on old cratons. Uranium and Rb losses are attributed to long-term leaching by rain and river water during exposure of the continental crust at the surface. Over geological times, the weathering effects create a slow but systematic increase of Th/U with exposure time.

Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediments of the Sierra Leone Rise

Causes of change in deep water delta13C can be either global or local in extent. Global causes include (1) climatically-induced changes in the amount of terrestrial biomass which alter the average carbon isotopic composition of the oceanic reservoir (Shackleton, 1977), and (2) erosion and deposition of organic-rich, continental shelf sediments during sea level fluctuations which change the mean oceanic carbon: phosphorus ratio (Broecker, 1982 doi:10.1016/0079-6611(82)90007-6). Regional gradients of delta13C are created by remineralization of organic detritus within the deep ocean itself thus reflecting the distribution of water masses and modern thermohaline flow. Changes in a single geological record of benthic foraminiferal delta13C can result from any combination of these global and abyssal circulation effects. By sampling a large number of cores collected over a wide bathymetric range yet confined to a small geographical region we have minimized the ambiguity. We can assume that each delta13C record was equally affected by global causes of delta13C variation. The differences seen between the delta13C records must, therefore, reflect changes in the distribution of delta13C in the deep ocean. We interpret these differences in distribution in terms of changes in the ocean's abyssal circulation. Benthic foraminiferal carbon isotopic evidence from a suite of Sierra Leone Rise cores indicates that the deeper parts of the eastern Atlantic basins underwent a reduction in [O2] during the maximum of the last glaciation. Reduced advection of O2-rich deep water through low-latitude fracture zones, associated with increased delivery of organic matter to the deep ocean, lowered the delta13C of deep water SumCO2 at all depths below the sill separating the eastern and western Atlantic basins (Metcalf et al., 1964 doi:10.1016/0011-7471(64)91078-2). This decreased advection into the eastern Atlantic Ocean coincides with the overall decrease in deep water production in the North Atlantic during the last glacial maximum (Curry and Lohmann, 1982 doi:10.1016/0033-5894(82)90071-0; Boyle and Keigwin, 1982 doi:10.1126/science.218.4574.784; Schnitker, 1979 doi:10.1016/0377-8398(79)90020-3; Streeter and Shackleton, 1979 doi:10.1126/science.203.4376.168).

Stable carbon and oxygen isotope ratios of benthic foraminifera from Paleocene to Oligocene sediments

Benthic oxygen and carbon isotopic results from a depth transect on Maud Rise, Antarctica, provide the first evidence for Warm Saline Deep Water (WSDW) in the Paleogene oceans. Distinct reversals occur in the oxygen isotopic gradient between the shallower Hole 689B (Eocene depth ~1400 m; present-day depth 2080 m) and the deeper Hole 690B (Eocene depth ~2250 m; present-day depth 2914 m). The isotopic reversals, well developed by at least 46 Ma (middle middle Eocene), existed for much of the remaining Paleogene. We do not consider these reversals to be artifacts of differential diagenesis between the two sites or to have resulted from other potentially complicating factors. This being so, the results show that deep waters at Hole 690B were significantly warmer than deep waters at the shallower Hole 689B. A progressive decrease and eventual reversal in benthic to planktonic delta18O gradients in Hole 690B, demonstrate that the deeper waters became warmer relative to Antarctic surface waters during the Eocene. The warmer deep waters of the Paleogene are inferred to have been produced at middle to low latitudes, probably in the Tethyan region which contained extensive shallow-water platforms, ideal sites for the formation of high salinity water through evaporative processes. The ocean during the Eocene, and perhaps the Paleocene, is inferred to have been two-layered, consisting of warm, saline deep waters formed at low latitudes and overlain by cooler waters formed at high latitudes. This thermospheric ocean, dominated by halothermal circulation we name Proteus. The Neogene and modern psychrospheric ocean Oceanus is dominated by thermohaline circulation of deep waters largely formed at high latitudes. An intermediate condition existed during the Oligocene, with a three-layered ocean that consisted of cold, dense deep waters formed in the Antarctic (Proto-AABW), overlain by warm, saline deep waters from low latitudes, and in turn overlain by cool waters formed in the polar regions. This we name Proto-oceanus which combined both halothermal and thermohaline processes. The sequence of high latitude, major, climatic change inferred from the oxygen isotopic records is as follows: generally cooler earlier Paleocene; warming during the late Paleocene; climax of Cenozoic warmth during the early Eocene and continuing into the early middle Eocene; cooling mainly in a series of steps during the remainder of the Paleogene. Superimposed upon this Paleogene pattern, the Paleocene/Eocene boundary is marked by a brief but distinct warming that involved deep to surface waters and a reduction in surface to deep carbon and oxygen isotopic gradients. This event coincided with major extinctions among the deep-sea benthic foraminifers as shown by Thomas (1990 doi:10.2973/odp.proc.sr.113.123.1990). Salinity has played a major role in deep ocean circulation, and thus paleotemperatures cannot be inferred directly from the oxygen isotopic composition of Paleogene benthic foraminifers without first accounting for the salinity effect.

U-Pb, trace element, and Hf isotope analysis for Macquarie Island detrital zircon

Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the reliability of oceanic zircon as an indicator of mantle melting conditions. The Macquarie Island ophiolite in the Southern Ocean provides a unique testing ground for this approach due to its formation within a mid-ocean ridge that gradually changed into a transform plate boundary. Detrital zircon recovered from the island records this change through a progressive enrichment in incompatible trace elements. Oligocene age (33-27 Ma) paleo-detrital zircon in ophiolitic sandstones and breccias interbedded with pillow basalt have trace element compositions akin to a MORB crustal source, whereas Late Miocene age (8.5 Ma) modern-detrital zircon collected from gabbroic colluvium on the island have highly enriched compositions unlike typical oceanic zircon. This compositional disparity between age populations is not complimented by analytically equivalent eHf data that primarily ranges from 14 to 13 for sandstone and modern-detrital populations. A wider compositional range for the sandstone population reflects a multiple pluton source provenance and is augmented by a single cobble clast with eHf equivalent to the maximum observed composition in the sandstone (~17). Similar sandstone and colluvium Hf-isotope signatures indicate inheritance from a similar mantle reservoir that was enriched from the depleted MORB mantle average. The continuity in Hf-isotope signature relative to trace element enrichment in Macquarie Island zircon populations, suggests the latter formed by reduced partial melting linked to spreading-segment shortening and transform lengthening along the dying spreading ridge.

Distribution of Florisphaera profunda and Helicosphaera carteri in down core and surface sediments

A detailed assessment of the respective roles of production, export, and subsequent preservation of organic carbon (Corg) in the eastern Mediterranean (EMED) sediments during the formation of sapropels remains elusive. Here we present new micropaleontological results for both surface samples taken at several locations in the EMED and last interglacial sapropel S5 from core LC21 in the southeastern Aegean Sea. A strong exponential anticorrelation between relative abundances of the lower photic zone coccolithophore Florisphaera profundain the surface sediments and modern concentrations of chlorophyll a (Chl-a) at the sea surface suggests thatF. profunda percentages can be used to track past productivity changes in the EMED. Prior to S5 deposition, an abrupt and large increase of F. profunda percentages in LC21 coincided (within the multidecadal resolution of the records) with the marked freshening of EMED surface waters. This suggests a strong coupling between freshwater-bound surface to intermediate water (density) stratification and enhanced upward advection of nutrients to the base of the photic zone, fuelling a productive deep chlorophyll maximum (DCM) underneath a nutrient-starved surface layer. Our findings imply that (at least) at the onset of sapropel formation physical and biogeochemical processes likely operated in tandem, enabling high Corg accumulation at the seafloor.

Uranium-Thorium dating and sea surface temperatures from corals from Hainan Island, South China Sea

Three mid-Holocene sea surface temperature (SST) records spanning more than 30 years were reconstructed for the northern South China Sea using Sr/Ca ratios in Porites corals. The results indicate warmer than present climates between circa 6100 yr B.P. and circa 6500 yr B.P. with the mid-Holocene average minimum monthly winter SSTs, the average maximum monthly summer SSTs, and the average annual SSTs being about 0.5°-1.4°C, 0°-2.0°C, and 0.2°-1.5°C higher, respectively, than they were during 1970-1994. Summer SSTs decrease from circa 6500 yr B.P. to circa 6100 yr B.P. with a minimum centered at circa 6300 yr B.P. The higher average summer SSTs are consistent with a stronger summer monsoon during the mid-Holocene, and the decreasing trend indicates a secular decrease of summer monsoon strength, which reflects the change in summer insolation in the Northern Hemisphere. El Niño-Southern Oscillation (ENSO) cycles were apparent in both the mid-Holocene coral and modern instrumental records. However, the ENSO variability in the mid-Holocene SSTs was weaker than that in the modern record, and the SST record with the highest summer temperatures from circa 6460 yr B.P. to 6496 yr B.P. shows no robust ENSO cycle. This agrees with other studies that indicate that stronger summer monsoon circulation may have been associated with suppressed ENSO variability during the mid-Holocene.

Chemical analyses and results of sediments from different DSDP Holes from the North Atlantic

Chemical analyses of North Atlantic D.S.D.P. (Deep Sea Drilling Project) sediments indicate that basal sediments generally contain higher concentrations of Fe, Mn, Mg, Pb, and Ni, and similar or lower concentrations of Ti, Al, Cr, Cu, Zn, and Li than the material overlying them. Partition studies on selected samples indicate that the enriched metals in the basal sediments are usually held in a fashion similar to that in basal sediments from the Pacific, other D.S.D.P. sediments, and modern North Atlantic ridge and non-ridge material. Although, on average, chemical differences between basal sediments of varying ages are apparent, normalization of the data indicates that the processes leading to metal enrichment on the crest of the Mid-Atlantic Ridge appear to have been approximately constant in intensity since Cretaceous times. In addition, the bulk composition of detrital sediments also appears to have been relatively constant over the same time period. Paleocene sediments from site 118 are, however, an exception to this rule, there apparently having been an increased detrital influx during this period. The bulk geochemistry, partitioning patterns, and mineralogy of sediments from D.S.D.P. 9A indicates that post-depositional migration of such elements as Mn, Ni, Cu, Zn, and Pb may have occurred. The basement encountered at the base of site 138 is thought to be a basaltic sill, but the overlying basal sediments are geochemically similar to other metalliferous basal sediments from the North Atlantic. These results, as well as those from site 114 where true oceanic basement was encountered, but where there was an estimated 7 m.y. hiatus between basaltic extrusion and basal sediment deposition, indicate that ridge-crest sediments are not necessarily deposited during active volcanism but can be formed after the volcanism has ceased. The predominant processes for metal enrichment in these deposits and those formed in association with other submarine volcanic features is a combination of shallow hydrothermal activity, submarine weathering of basalt, and the formation of ferromanganese oxides which can scavenge metals from seawater. In addition, it seems as though the formation of submarine metalliferous sediments is not restricted to active-ridge areas.

Heterogeneous firms and cost sharing in China's marketplaces

This study extends Melitz's model with heterogeneous firms by introducing shared fixed costs in a marketplace. It aims to explain heterogeneous firms' choice between traditional marketplaces and modern distribution channels on the basis of their productivities. The results reveal that the co-existence of a traditional marketplace and modern distribution channels improves social welfare. In addition, a deregulation policy for firm entry outside a marketplace and accumulation of human capital are factors that contribute to improve the social welfare.

Offshore stereo measurements of gravity waves: classical epipolar and novel variational techniques

Stereo video techniques are effective for estimating the space-time wave dynamics over an area of the ocean. Indeed, a stereo camera view allows retrieval of both spatial and temporal data whose statistical content is richer than that of time series data retrieved from point wave probes. Classical epipolar techniques and modern variational methods are reviewed to reconstruct the sea surface from the stereo pairs sequentially in time. Current improvements of the variational methods are presented.

OER Development and Promotion. Outcomes of an International Research Project on the OpenCourseWare Model

In this paper, we describe the successful results of an international research project focused on the use of Web technology in the educational context. The article explains how this international project, funded by public organizations and developed over the last two academic years, focuses on the area of open educational resources (OER) and particularly the educational content of the OpenCourseWare (OCW) model. This initiative has been developed by a research group composed of researchers from three countries. The project was enabled by the Universidad Politécnica de Madrid OCW Office�s leadership of the Consortium of Latin American Universities and the distance education know-how of the Universidad Técnica Particular de Loja (UTPL, Ecuador). We give a full account of the project, methodology, main outcomes and validation. The project results have further consolidated the group, and increased the maturity of group members and networking with other groups in the area. The group is now participating in other research projects that continue the lines developed here

Planning and community development: case studies

Planning and Comunity Development: Case Studies, presents the findings of the inter-university Seminar held on 28?29 July 2011 and organized by researchers from the Technical University of Madrid and the University of California, Berkeley, who were fortunate to have the presence of the renowned Professor John Friedmann. Professors, researchers and PhD students from our research groups presented their works as scientific communications that were enriched by the debate among the different researches who attended the Seminar. All of them appear in the picture below in front of the gate of Haviland Hall at UC Berkeley. This book analyses the concept of planning and its evolution so far, leading to the conceptualization of governance as an expression of the planning practice. It also studies the role of social capital and cooperation as tools for the community development. The conceptual analysis is complemented by the development of six case studies that put forward experiences of planning and community development carried out in diverse social and cultural contexts of Latin-America, Europe and North America. This publication comes after more than 20 years of work of the researchers that met at the seminar. Through their work in managing development initiatives, they have learned lessons and have contribute to shape their own body of teaching that develops and analyses the role of planning in public domain to promote community development. This knowledge is synthesized in the model Planning as Working With People, that shows that development is not effective unless is promoted in continuous collaboration with all the actors involved in the process.

Contexto, criptoanálisis y propuesta de solución de la inscripción de la talla (original) de la Virgen de Candelaria de Tenerife (Canarias, España)

Esta investigación es un ejemplo de simbiosis entre criptoanálisis y desciframiento de lenguas. Es la búsqueda del sentido de una inscripción, un conjunto de casi doscientas letras latinas, en una talla de la Virgen María que estaba en la isla de Tenerife, en la localidad hoy de Candelaria, en las islas Canarias. La imagen desapareció en un temporal en el año 1826. No obstante, es posible lograr una gran certeza sobre qué letras tenía, acudiendo a las fuentes documentales textuales y artísticas. El conocimiento del significado, si lo hubiera, de la inscripción mariana, creemos que no puede lograrse sin la adecuada comprensión del contexto. Esto significa indagar en la historia de la misma talla, que se remonta hasta el siglo XIV o XV, en el estudio de la población autóctona canaria, así como de los pueblos que allí llegaron en sus diferentes momentos históricos. Además, es necesario conocer el redescubrimiento del archipiélago canario y sus procesos de conquista y evangelización. Todos estos datos irán ofreciendo un panorama nuevo y sorprendente para comprender no sólo las letras sino la misma imagen escultórica en madera. A partir de este momento la indagación se moverá en ver si las letras corresponden a alguna lengua posible, lo que nos ha llevado a analizar un amplísimo conjunto de textos lo más cercanos a la época bajo estudio, pertenecientes a alrededor de un centenar de lenguas. Tras el examen lingüístico se ha procedido a un estudio de las posibles formas criptográficas que se hubieran utilizado para generar el texto de la inscripción. Se ofrece un detallado y minucioso elenco de técnicas posibles que pudieran haberse adoptado y se criptoanaliza con exhaustividad las letras de la talla mariana. Al mismo tiempo se ofrece un nuevo marco criptológico de métodos y sistemas más ordenado y completo que el que hasta ahora venía considerándose, en especial desde el surgimiento de la criptografía de clave asimétrica. Continuamos la investigación sopesando la posible generación pseudo-aleatoria del texto, un texto que pudiera no tener sentido alguno. En este momento, y habiendo completado todas las posibilidades e hipótesis, habiéndose negado todas, volvemos a reconsiderar el cuerpo de conjeturas y supuestos. Desde ahí analizamos en profundidad el ámbito etnográfico y lingüístico bereber como hipótesis más plausible y probable. Tras la profundización en esta lengua y la corrección de los errores que nos llevaron a no detectarla en nuestro análisis precedente, llegamos a la conclusión de encontrarnos ante una lengua arcaica bereber, un conjunto de letras pertenecientes a una lengua y familia hoy no desaparecida, si bien muy modelada y difuminada por otras lenguas, en especial el árabe. Esto nos llevará a rescatar aspectos léxicos, morfológicos, sintácticos y fonéticos de este habla arcaica. Con todos estos datos realizamos un amplio estudio semántico de la talla tanto desde la perspectiva aborigen autóctona como cristiana. Finalmente, desde las voces lexicales y sus raíces de las lenguas bereberes e insulares amazigh, ofrecemos el significado de las letras inscritas en la talla mariana de Candelaria. ABSTRACT This research is an example of symbiosis between cryptanalysis and deciphering of languages. It is the search for meaning in an inscription, a group of about two hundred latin letters on a carving of the Virgin Mary that was on the island of Tenerife, in the town of Candelaria today, in the Canary islands. The image disappeared in a storm in 1826. However, it is possible to achieve a great certainty about what letters had, going to the textual and artistic documentary sources. The knowledge of the meaning, if any, of the marian inscription, can not be achieved without an adequate knowledge of the context. This means researching into the history of the same carving, which dates back to the fourteenth and fifteen century; the study of the canarian indigenous people and of the people who came there at different historical moments. Furthermore, it is necessary to know the rediscovery of the Canary islands and their processes of conquest and evangelization. All these data will offer a new and surprising outlook to understanding not only the letters but the same wood sculpture. From this moment the inquiry will move to see if the letters correspond to any possible language, which has led us to analyze a very large set of texts as close to the time under study, in a hundred languages. After the language examination, has been carried out a study of possible cryptographic forms used to generate the text of the inscription. A detailed and thorough list of possible techniques that could be adopted is offered. Then exhaustively we cryptanalyze the letters of the marian carving. At the same time a new crypto framework of methods and systems more orderly and complete, especially since the emergence of asymmetric key cryptography, is provided. We continue researching the possible pseudo-random generation of the text, a text that would not make any sense. At this time, and having completed all the possibilities and hypotheses, all having refused, we return to rethink our assumptions. From there we analyze in depth the ethnographic and linguistic berber sphere as the most likely hypothesis. Following the deepening of this language and correcting the mistakes that led us not to detect it in our analysis above, we conclude that this is an archaic berber language, a set of letters belonging to a language and family not extinct today but very modeled and influenced by other languages, primarily arabic. This will lead us to rescue lexical, morphological, syntactic and phonetic aspects of this archaic speech. With all this data we make a wide semantic study of the carving from the indigenous and christian perspective. Finally, from the lexical voices and roots of the berber languages amazigh and island-amazigh, we give the meaning of the letters inscribed in the marian carving of Candelaria.