Diferencias e intercambios culturales entre el campo y la ciudad respecto de las mujeres en la España del siglo XVIII

Este artículo es una síntesis que pone en relación los niveles culturales femeninos en el campo y en las ciudades de España en el siglo XVIII con los movimientos migratorios femeninos entre ambos mundos. La autora propone algunas vías para estudiar las diferencias de alfabetización y la diversidad de idiomas, y para observar si las migraciones temporales o permanentes a las ciudades sirvieron como forma de transmisión de ideas o costumbres entre las ciudades y el campo. El texto subraya en especial las diferencias territoriales entre el Norte y el Sur españoles, y ofrece explicaciones sobre estos contrastes

Los migrantes del noroeste hispánico en el Buenos Aires tardo colonial : La construcción de un tejido relacional luego del traslado ultramarino

A fines del siglo XVIII las migraciones de gallegos y asturianos a la ciudad de Buenos Aires se incrementaron. Estos desplazamientos estuvieron condicionados por diferentes factores, que operaron de ambos lados del Atlántico: la instauración de una línea regular de transporte oficial entre La Coruña y Montevideo (los Correos Marítimos); la larga tradición marítima y migratoria de las zonas costeras de Galicia y Asturias; o el desarrollo económico de la capital virreinal, con sus oportunidades de movilidad social ascendente, entre otros. Dentro de Buenos Aires, los oriundos del noroeste hispánico generaron un tejido de relaciones sociales, que incluyó vínculos con paisanos y con el componente nativo de la sociedad de recepción. A lo largo de este trabajo analizaremos esta ambigua dirección de los lazos sociales postmigratorios, a partir del examen de algunas fuentes primarias básicas, tales como las actas matrimoniales, los testamentos o los padrones de habitantes.

Producciones identitarias y relaciones interculturales en el periurbano platense

El presente artículo se inscribe en una serie de trabajos focalizados en experiencias migratorias y construcción de identidades y alteridades étnico-nacionales que venimos realizando tanto en el área periurbana de producción hortícola como en el casco urbano de la ciudad de La Plata. (1) En ellos abordamos aspectos de la inserción local de los migrantes -en especial con respecto al caso boliviano- desde distintos ejes analíticos como son la adscripción étnico-nacional, el trabajo, el género, la participación institucional, la construcción de categorías de alteridad con respecto a los migrantes por parte de sujetos, instituciones y medios de comunicación locales, el uso de medios como estrategia de identificación / afirmación / participación desde los propios migrantes. En el caso específico de la migración boliviana a Argentina, tanto al área plenamente urbana como a la rural periurbana -en donde adquiere especial importancia-, constituye un fenómeno estructurado y con características propias, situación reforzada por el subempleo en las áreas de economía campesina en Bolivia y la demanda de algunos sectores de la economía argentina, como actualmente el de la construcción urbana y el de la producción hortiflorícola periurbana. En tal sentido el tema se constituye en referente privilegiado para destacar los aspectos dinámicos de la ciudad y su región. En este contexto expondremos algunas reflexiones conceptuales y resultados de trabajo de campo referidos a la auto y hetero demarcación de la pertenencia étnico-nacional como espacio identificatorio en las dimensiones de trabajo y género.

La dialéctica macro-microhistoria en el estudio de las migraciones europeas a la Argentina

El autor analiza la evolución de la producción académica argentina sobre migraciones, poniendo el acento sobre los avances registrados desde a partir de los aportes realizados desde la historia local y la microhistoria. Los nuevos trabajos permitieron establecer diversidades temáticas y metodológicas en un clima historiográfico con elementos compartidos, como el papel de las redes sociales examinadas a partir de fuentes personales que hacen posible establecer, en una perspectiva comparada de la labor llevada adelante en la materia, un nuevo punto de partida para una generalizar que no excluya la vida de las personas de la historia.

Aportes para una nueva visión en los estudios geográficos del concepto de nación desde las perspectivas cultural y política

La Nación ha sido una de las más importantes construcciones políticoculturales de la Modernidad. Las premisas que le han dado mayor vitalidad han sido y son, pues, su afirmación como imaginario de identidad para los pueblos y su significación en el desarrollo de las denominadas "relaciones internacionales", en cuanto formas de expresión de las interrelaciones globales de los sectores dominantes. Este estudio se basa en el análisis de esas premisas a la luz de algunas de las nuevas perspectivas emanadas de los paradigmas político y cultural, desarrollados en las ciencias sociales a partir de las últimas décadas del siglo pasado, y aplicadas a los estudios del territorio nacional, su construcción, sus mutaciones y los imaginarios espaciales que de ellos derivan. A partir de algunas de las visiones críticas mencionadas, en la actualidad el concepto de nación parece haber entrado en un proceso de erosión o descomposición. Fenómenos sociales, económicos, políticos y culturales ligados a los procesos de reestructuración global (migraciones intercontinentales, sistemas mediáticos globales, exclusión social, discriminación étnica y religiosa, marginación y falta de participación política, nuevas formas de manifestación social...) y a la construcción de los discursos posmodernos hacen aparecer la nación como un concepto, al menos, puesto en tela de juicio. Los más audaces hablan del virtual ingreso a un mundo "posnacional". ¿Significará esto la extinción de una idea y una realidad con la que se han formado culturalmente millones de personas de numerosas generaciones en los puntos más lejanos del planeta? La respuesta deberá estar planteada en el estudio real y especializado de esos fenómenos y de las nuevas realidades que de ellos emergen.

La migración en la unidad doméstica: un estudio de caso en dos municipios de la frontera argentino-boliviana (Los Toldos, Salta y Padcaya, Tarija)

El trabajo estudia las migraciones regionales e internacionales en un contexto de economías campesinas de frontera, que comprende los actuales municipios de Los Toldos (Salta, Argentina) y Padcaya (Tarija, Bolivia). El valle de Los Toldos perteneció a Bolivia hasta 1938, año en el que se oficializó su traspaso hacia Argentina. Si bien, hasta esa fecha, el área de estudio conformaba una misma región, la diferente pertenencia estatal fue marcando ciertas diferencias entre ambos sectores, principalmente debido a la influencia de las políticas que fue adoptando cada nación. Mediante un estudio etnográfico y, especialmente, el análisis comparado de 110 encuestas semi-estructuradas a unidades domésticas, se observa la movilidad espacial de sus integrantes. Diferentes tipos de migración se constituyen en función de las estrategias reproductivas de tales unidades. Dada la creciente subdivisión de las tierras las migraciones permanentes se entienden como un mecanismo compensatorio en la etapa de redistribución de los medios de producción entre los descendientes. Mientras que las migraciones temporarias se constituyen en una actividad más, que se suma a las actividades económicas convencionales.

La lírica popular-tradicional argentina : Límites difusos

La sociedad argentina puede caracterizarse como "nueva", producto de proyectos poblacionales y migraciones internas y externas. Esta condición determinó que la cultura popular, y la poesía en particular, se manifestaran en distintas tradiciones superpuestas. Una tradición hispánica procedente del período colonial se asentó en el noroeste del país, área de población más antigua en la que fueron documentados romances y coplas tradicionales. Paralelamente, una tradición criolla heredera de la hispánica tuvo expresiones autóctonas en relación con los movimientos independentistas (romancero criollo, pero también décimas y coplas). Por último, una tradición europea se incorporó entre fines del siglo xix y principios del xx con el denominado aluvión inmigratorio. Esta última corriente impregnó todo lo anterior con nuevos temas procedentes especialmente de España, pero en contacto con diversas formas populares de otros países como Italia, Francia y Portugal. El propósito de este artículo es ofrecer un panorama de la superposición de estos distintos estratos culturales tal como se manifiesta en las coplas que se cantaron y se imprimieron en la primera mitad del Siglo xx

Neogene and Quaternary paleoenvironmental history at DSDP Leg 71 Holes

The Neogene and Quaternary sedimentary record of Leg 71 and previously drilled sequences from the Southern Ocean reveal evidence of a major late Miocene change of oceanic and glacial conditions in the southern high latitudes during paleomagnetic Chron 9. The characteristics of late Miocene sedimentation and in particular the study of erosional patterns and ice-rafted debris suggest the following conclusions. 1) In the late Miocene, the Polar Front first migrated to the northern latitudes of the Southern Ocean and surface water temperatures became similar to those of today. 2) Extensive ice shelves or ice tongues were not present along the Antarctic margin until late Chron 9 (about 9.0 Ma). 3) Before Chron 9, West Antarctica was occupied by an archipelago and the West Antarctic Sea. 4) Extensive ice shelves formed in the West Antarctic region, eventually coalescing and thickening to form the grounded West Antarctic ice sheet by Chron 9. 5) The newly formed West Antarctic ice sheet was probably unstable and frequently became an ungrounded ice shelf, thus accounting for the scarcity of late Miocene ice-rafted debris. 6) Extensive erosion or nondeposition of sediment was probably the result of increased Antarctic Bottom Water (AABW) formation in the West Antarctic region during the initial formation of extensive West Antarctic ice shelves and during periods when the West Antarctic ice sheet was ungrounded. 7) In the Southwest Atlantic, AABW velocity waned during the latest Miocene. During the late Gilbert Chron a major and permanent change occurred in the pattern of ice-rafting to the South Atlantic, and after 4.35 Ma the increased IRD accumulation rate and frequency of major episodes of IRD accumulation suggest increased stability of the West Antarctic ice sheet. In addition, radiolarian faunas of Hole 514 record at least eight migrations of the Polar Front to the north of the site during the past 4.07 m.y. An apparent increase in the frequency of Polar Front migrations occurred about 2.7-2.6 Ma, possibly in response to oceanic change induced by fluctuations in glacial conditions of the Northern Hemisphere.

Epístolas de Max Aub a Ignacio Soldevila Durante (y viceversa) : El devenir de una preciosa amistad

A las migraciones de intelectuales como consecuencia de la Guerra Civil española, iniciadas ya en 1936, se sumaron posteriormente las de universitarios que desarrollaron su tarea allende las fronteras. Entre ellos, Ignacio Soldevila Durante, valenciano, quien se instaló en la ciudad de Québec en 1956. Dos años antes había dirigido una carta al escritor Max Aub, del que con el tiempo se convertiría en amigo y en su mejor especialista. El epistolario Aub-Soldevila (1954-1972) pone sobre el tapete, entre otros datos, detalles biográficos y elementos relacionados con la obra del escritor y con aquellas decisivas décadas del pasado siglo; asimismo, enuncia rasgos definitorios de cuantos la guerra arrojó a las playas del éxodo.

Age model for the time between 3.45 and 2.45 Ma of ODP Site 189-1172

Calcareous nannoplankton assemblages and benthic d18O isotopes of Pliocene deep-sea sediments of ODP site 1172 (East of Tasmania) have been studied to improve our knowledge of the Southern Ocean paleoceanography. Our study site is located just north of the Subtropical Front (STF), an ideal setting to monitor migrations of the STF during our study period, between 3.45 and 2.45 Ma. The assemblage identified at ODP site 1172 has been interpreted as characteristic for the transitional zone water mass, located south of the STF, based on: (i) the low abundances (< 1%) of subtropical taxa, (ii) relatively high percentages of Coccolithus pelagicus, a subpolar type species, (iii) abundances from 2-10% of Calcidiscus leptoporus, a species that frequently inhabits the zone south of the STF and (iv) the high abundances of small Noelaerhabdaceae which at present dominates the zone south of the STF. Across our interval the calcareous nannoplankton manifests glacial-interglacial variability. We have identified cold events, characterized by high abundances of C. pelagicus which coincide with glacial periods, except during G7. After 3.1 Ma cold events are more frequent, in concordance with global cooling trends. Around 2.75 Ma, the interglacial stage G7 is characterized by anomalous low temperatures which most likely are linked to definite closure of the Central American Seaway (CAS), an event that is believed to have had global consequences. A gradual increase of very small Reticulofenestra across our section marks a significant trend in the small Noelaerhabdaceae species group and has been linked to a general enhanced mixing of the water column in agreement with previous studies. It is suggested that a rapid decline of small Gephyrocapsa after isotopic stage G7 might be related to the cooling observed in our study site after the closure of the CAS.

Mid-Miocene planktonic foraminifera of the Kerguelen Plateau, Antarctica

Miocene deep-sea sediments from ODP Site 744 (Kerguelen Plateau, southern Indian Ocean) contain abundant and diverse planktonic foraminiferal assemblages. Their analysis led to the identification of the interval between 17.0 and 14.2 Ma as a time of mid-Miocene warmth, which is investigated here in detail. This investigation includes reconstruction of trends in foraminiferal faunal composition and diversity through time, as well as in morphology and coiling direction within Globorotalia praescitula and Globorotalia zealandica plexi. These two large-globorotaliid plexi constitute the most characteristic component of the mid-Miocene foraminiferal faunas at ODP Site 744. Selected benthic (Cibicidoides sp.) and planktonic foraminifera were also analyzed for delta18O and delta13C ratios. Distinctive planktonic assemblages were the basis for identification of three foraminiferal biofacies between 17.0 and 14.2 Ma. The most prominent faunal changes took place between Biofacies 2 and 3 (15.5-15.0 Ma). Six of 11 macroperforate planktonic foraminifera from the >150-µm size fraction occur principally within Biofacies 3. Three other taxa are present throughout the interval analyzed. Moreover, both aforementioned globorotaliid plexi exhibit an increase in morphological diversity between Biofacies 2 and 3. Within the same interval, the G. zealandica plexus shows a switch from random coiling (50% sinistral) to clearly sinistral-dominated coiling. The faunal changes recognized are interpreted as the result of foraminiferal immigrations (increase in faunal diversity) and evolutionary trends (increase in morphological variability and change in coiling mode among the globorotaliid plexi). The stable isotopic results allow paleoenvironmental interpretation of these faunal changes. According to the delta18O values, no significant change in sea-surface temperature occurred between 17.0 and 14.2 Ma. However, the same data suggest an increase in ecological distance between various niches, which is expressed by a rising delta18O gradient recorded between various planktonic taxa upward within the section. This trend suggests niche-space availability as a likely factor responsible for the faunal changes recognized. Changes in the shape and depth of the thermocline, as well as in seasonality and eutrophication are considered as possible causes. Among these an increase in seasonality appears to have been responsible for the increase in species and morphological diversities between 15.5 and 15.0 Ma. The proposed scenario suggests that changes in seasonality may be an important factor driving faunal migrations and evolution. Variable seasonality may also affect the oxygen isotopic record of planktonic foraminiferal taxa.

Late Quaternary benthic foraminiferal record of the Bounty Trough, east of New Zealand

The Bounty Trough, east of New Zealand, lies along the southeastern edge of the present-day Subtropical Front (STF), and is a major conduit via the Bounty Channel, for terrigenous sediment supply from the uplifted Southern Alps to the abyssal Bounty Fan. Census data on 65 benthic foraminiferal faunas (>63 µm) from upper bathyal (ODP 1119), lower bathyal (DSDP 594) and abyssal (ODP 1122) sequences, test and refine existing models for the paleoceanographic and sedimentary history of the trough through the last 150 ka (marine isotope stages, MIS 6-1). Cluster analysis allows recognition of six species groups, whose distribution patterns coincide with bathymetry, the climate cycles and displaced turbidite beds. Detrended canonical correspondence analysis and comparisons with modern faunal patterns suggest that the groups are most strongly influenced by food supply (organic carbon flux), and to a lesser extent by bottom water oxygen and factors relating to sediment type. Major faunal changes at upper bathyal depths (1119) probably resulted from cycles of counter-intuitive seaward-landward migrations of the Southland Front (SF) (north-south sector of the STF). Benthic foraminiferal changes suggest that lower nutrient, cool Subantarctic Surface Water (SAW) was overhead in warm intervals, and higher nutrient-bearing, warm neritic Subtropical Surface Water (STW) was overhead in cold intervals. At lower bathyal depths (594), foraminiferal changes indicate increased glacial productivity and lowered bottom oxygen, attributed to increased upwelling and inflow of cold, nutrient-rich, Antarctic Intermediate Water (AAIW) and shallowing of the oxygen-minimum zone (upper Circum Polar Deep Water, CPDW). The observed cyclical benthic foraminiferal changes are not a result of associations migrating up and down the slope, as glacial faunas (dominated by Globocassidulina canalisuturata and Eilohedra levicula at upper and lower bathyal depths, respectively) are markedly different from those currently living in the Bounty Trough. On the abyssal Bounty Fan (1122), faunal changes correlate most strongly with grain size, and are attributed to varying amounts of mixing of displaced and in-situ faunas. Most of the displaced foraminifera in turbiditic sand beds are sourced from mid-outer shelf depths at the head of the Bounty Channel. Turbidity currents were more prevalent during, but not restricted to, glacial intervals.

Siliceous components of Pliocene-Holocene sediments of the South Atlantic

The Pliocene-Holocene sediments recovered on ODP Leg 114 from Holes 699A, 701C, and 704B are the subject of a detailed investigation to interpret changes in the Oceanographic environment of the South Atlantic in the vicinity of the Polar Front Zone (PFZ). The cores sample sediments at shallow (Hole 704B, 2532 m), intermediate (Hole 699A, 3716 m), and basinal (Hole 701C, 4647 m) depths. Sites 699 and 704 come under the influence of the Antarctic Circumpolar Current (ACC) and Circumpolar Deep Water. It is possible that the upper reaches of Antarctic Bottom Water (AABW) may also affect Hole 699A. Site 701 is influenced by AABW. Closely spaced samples were analyzed for grain-size distribution, sand fraction components, biosiliceous microfossils, organic carbon, and water content. PFZ migrations are traced using changes in bulk sedimentaccumulation rates and the abundance of the diatoms Actiniscus ssp. and Genus et species indet. 1 Fenner (1991), as well as changes in sediment grain size and composition. Diatomaceous sediments of Gilbert age in Hole 699A indicate that the PFZ was positioned over this site, but during the Gauss it migrated north, bringing in less productive Antarctic Surface Water. All cores document a very gradual southerly movement of the PFZ throughout the Matuyama (with some sharp fluctuations of the northen PFZ border over Site 704 between 1.45 and 1.83 m.y.). This regressive shift culminated in the late Matuyama. The latest Matuyama to earliest Brunhes record in Hole 699A has been removed by a hiatus lasting from 1.0 to 0.6 m.y., which was probably caused by intensification of the deep-reaching ACC. The corresponding interval in Hole 704B, the shallowest core, contains evidence of winnowing. Sharp fluctuations of large amplitude and high frequency in the lithology of the sediments from Hole 704B in the eastern South Atlantic, starting at about 0.75 m.y. and characterizing the whole Brunhes Epoch, record the rapid movement of the northern border of the PFZ over the site. These reflect strong glacial/interglacial alternations in climate. To a lesser extent, lithologic fluctuations in Hole 701C reflect the same phenomenon, whereas in Hole 699A the lithology does not vary as dramatically.

Chronology and stable carbon isotopic ratios of sediments from the Western Pacific Warm Pool region

Instrumental data suggest that major shifts in tropical Pacific atmospheric dynamics and hydrology have occurred within the past century, potentially in response to anthropogenic warming. To better understand these trends, we use the hydrogen isotopic ratios of terrestrial higher plant leaf waxes (DDwax) in marine sediments from southwest Sulawesi, Indonesia, to compile a detailed reconstruction of central Indo-Pacific Warm Pool (IPWP) hydrologic variability spanning most of the last two millennia. Our paleodata are highly correlated with a monsoon reconstruction from Southeast Asia, indicating that intervals of strong East Asian summer monsoon (EASM) activity are associated with a weaker Indonesian monsoon (IM). Furthermore, the centennial-scale oscillations in our data follow known changes in Northern Hemisphere climate (e.g., the Little Ice Age and Medieval Warm Period) implying a dynamic link between Northern Hemisphere temperatures and IPWP hydrology. The inverse relationship between the EASM and IM suggests that migrations of the Intertropical Convergence Zone and associated changes in monsoon strength caused synoptic hydrologic shifts in the IPWP throughout most of the past two millennia.

Glacial-interglacial record of ODP Site 181-1119 in the Canterbury Bright, Southwest Pacific Ocean

Ocean Drilling Program (ODP) Site 1119 is located at water depth 395 m near the subtropical front (STF; here represented by the Southland Front), just downslope from the shelf edge of eastern South Island, New Zealand. The upper 86.19 metres composite depth (mcd) of Site 1119 sediment was deposited at an average sedimentation rate of 34 cm/kyr during Marine Isotope Stages (MIS) 1-8 (0-252 ka), and is underlain across a ~25 kyr intra-MIS 8 unconformity by MIS 8.5-11 (277-367 ka) and older sediment deposited at ~14 cm/kyr. A time scale is assigned to Site 1119 using radiocarbon dates for the period back to ~39 ka, and, prior to then, by matching its climatic record with that of the Vostok ice core, which it closely resembles. Four palaeoceanographic proxy measures for surface water masses vary together with the sandy-muddy, glacial-interglacial (G/I) cyclicity at the site. Interglacial intervals are characterised by heavy delta13C, high colour reflectance (a proxy for carbonate content), low Q-ray (a proxy for clay content) and light delta18O; conversely, glacial intervals exhibit light delta13C, low reflectance, high Q-ray and heavy delta18O signatures. Early interglacial intervals are represented by silty clays with 10-105-cm-thick beds of sharp-based (Chondrites-burrowed), shelly, graded, fine sand. The sands are rich in foraminifera, and were deposited distant from the shoreline under the influence of longitudinal flow in relatively deep water. Glacial intervals comprise mostly micaceous silty clay, though with some thin (2-10 cm thick) sands present also at peak cold periods, and contain the cold-water scallop Zygochlamys delicatula. Interglacial sandy intervals are characterised by relatively low sedimentation rates of 5-32 cm/kyr; cold climate intervals MIS 10, 6 and 2 have successively higher sedimentation rates of 45, 69 and 140 cm/kyr. Counter-intuitively,and forced by the bathymetric control of a laterally-moving shoreline during G/I and I/G transitions, the 1119 core records a southeasterly (seaward) movement of the STF during early glacial periods, accompanied by the incursion of subtropical water (STW) above the site, and northwesterly (landward) movement during late glacial and interglacial times, resulting in a dominant influence then of subantarctic surface water (SAW). The history of passage of these different water masses at the site is clearly delineated by their characteristic delta13C values. The intervals of thin, graded sands-muds which occur within MIS 2-3, 6, 7.4 and 10 indicate the onset at times of peak cold of intermittent bottom currents caused by strengthened and expanded frontal flows along the STF, which at such times lay near Site 1119 in close proximity to seaward-encroaching subantarctic waters within the Bounty gyre. In common with other nearby Southern Hemisphere records, the cold period which represents the last glacial maximum lasted between ~23-18 ka at Site 1119, during which time the STF and Subantarctic Front (SAF) probably merged into a single intense frontal zone around the head of the adjacent Bounty Trough.