Primeras aproximaciones para el estudio de los procesos de estratificación en los aglomerados urbanos en Argentina

El presente artículo se propone explorar las estratificaciones sociales en los grandes aglomerados urbanos en Argentina en el período 2003-2011. Los alcances y objetivos de este artículo son descriptivos. En este sentido, propone un esquema de clases apto para instrumentos como la EPH y describe los procesos de asalarización de los cuadros más capacitados, el crecimiento espurio de la clase media y la persistencia de una clase baja marginal a pesar del crecimiento económico. El aglomerado Gran Mendoza es analizado por separado ya que parece exhibir tendencias diferenciales.

Paraná y su región : Criterios básicos para proyectar políticas de gestión metropolitana

El propósito del presente trabajo es reconocer, cómo a partir de las tensiones globales y locales, de carácter socio - espacial e imbricadas en el proceso de metropolización que acusa el ámbito expandido de la ciudad de Paraná, es factible identificar y analizar los criterios básicos para proyectar una inédita gestión metropolitana dentro del espacio regional que constituyen tanto el ejido de la capital de la Provincia de Entre Ríos como el de sus tres municipios conurbados. En consecuencia y a tal fin, se intenta aquí establecer los nuevos desafíos incorporados a la gestión urbano-ambiental, tanto provincial como municipal, dentro de los que se platea articular la intervención estatal y la participación comunitaria, en el marco de un proceso de ordenamiento territorial del ámbito metropolizado en esas cuatro jurisdicciones en las que hoy habitan más de trescientos mil comprovincianos. Se trata, por tanto, de un proyecto estratégico que institucionalmente persiga la posibilidad de articular en simultáneo cuatro criterios políticos considerados aquí básicos para la gestión democrática del territorio metropolitano: la gobernabilidad, la competitividad, la sustentabilidad y la inclusión social. Criterios que, dentro de esa inteligencia, guiarán el análisis desarrollado sobre propuestas de actuación, jurídico-normativas y de gestión para abordar la compleja problemática del espacio urbano-regional. Es en tal contexto entonces, y dentro de esos principios primordiales para la intervención urbano-territorial, en el que se estima posible plantear, desde el ámbito institucional del Gobierno de la Provincia y de los gobiernos municipales, un acotado y preciso conjunto de políticas sectoriales básicas de ordenamiento que habiliten al despliegue de estrategias comunes y de consenso social posible, destinadas a transformar las críticas condiciones por las que atraviesa la conurbación en su conjunto, sin por eso vulnerar la autonomía de la jurisdicciones municipales incluidas en el espacio geográfico. Concluyendo, en el presente trabajo se analizan e identifican en forma iniciática, los criterios esenciales para el logro de los objetivos territoriales y las metas institucionales que dentro de la gestión metropolitana, puedan asumir el Estado Provincial y las jurisdicciones municipales, en tanto dispositivos gubernamentales destinados a que legal y orgánicamente, sean orientadas las políticas que tengan el propósito de afrontar tanto los procesos territoriales distorsivos como los déficit, las asimetrías y las carencias socio-ambientales que acusa la población del Gran Paraná

Biopolítica, población y control

Los estudios del poder han volteado hace tiempo a la biopolítica, vista como la intromisión e injerencia del poder y la política sobre la vida. Se da en positivo y en negativo. De ahí la discusión sobre el control social, como una expresión de la biopolítica moderna. La conexión entre biopolítica y población no es menos significativa que la manera cómo el poder administra y regula los nacimientos y la migración así como la calidad de vida de los conglomerados sociales

Biopolítica, población y control

Los estudios del poder han volteado hace tiempo a la biopolítica, vista como la intromisión e injerencia del poder y la política sobre la vida. Se da en positivo y en negativo. De ahí la discusión sobre el control social, como una expresión de la biopolítica moderna. La conexión entre biopolítica y población no es menos significativa que la manera cómo el poder administra y regula los nacimientos y la migración así como la calidad de vida de los conglomerados sociales

Paraná y su región : Criterios básicos para proyectar políticas de gestión metropolitana

El propósito del presente trabajo es reconocer, cómo a partir de las tensiones globales y locales, de carácter socio - espacial e imbricadas en el proceso de metropolización que acusa el ámbito expandido de la ciudad de Paraná, es factible identificar y analizar los criterios básicos para proyectar una inédita gestión metropolitana dentro del espacio regional que constituyen tanto el ejido de la capital de la Provincia de Entre Ríos como el de sus tres municipios conurbados. En consecuencia y a tal fin, se intenta aquí establecer los nuevos desafíos incorporados a la gestión urbano-ambiental, tanto provincial como municipal, dentro de los que se platea articular la intervención estatal y la participación comunitaria, en el marco de un proceso de ordenamiento territorial del ámbito metropolizado en esas cuatro jurisdicciones en las que hoy habitan más de trescientos mil comprovincianos. Se trata, por tanto, de un proyecto estratégico que institucionalmente persiga la posibilidad de articular en simultáneo cuatro criterios políticos considerados aquí básicos para la gestión democrática del territorio metropolitano: la gobernabilidad, la competitividad, la sustentabilidad y la inclusión social. Criterios que, dentro de esa inteligencia, guiarán el análisis desarrollado sobre propuestas de actuación, jurídico-normativas y de gestión para abordar la compleja problemática del espacio urbano-regional. Es en tal contexto entonces, y dentro de esos principios primordiales para la intervención urbano-territorial, en el que se estima posible plantear, desde el ámbito institucional del Gobierno de la Provincia y de los gobiernos municipales, un acotado y preciso conjunto de políticas sectoriales básicas de ordenamiento que habiliten al despliegue de estrategias comunes y de consenso social posible, destinadas a transformar las críticas condiciones por las que atraviesa la conurbación en su conjunto, sin por eso vulnerar la autonomía de la jurisdicciones municipales incluidas en el espacio geográfico. Concluyendo, en el presente trabajo se analizan e identifican en forma iniciática, los criterios esenciales para el logro de los objetivos territoriales y las metas institucionales que dentro de la gestión metropolitana, puedan asumir el Estado Provincial y las jurisdicciones municipales, en tanto dispositivos gubernamentales destinados a que legal y orgánicamente, sean orientadas las políticas que tengan el propósito de afrontar tanto los procesos territoriales distorsivos como los déficit, las asimetrías y las carencias socio-ambientales que acusa la población del Gran Paraná

Paraná y su región : Criterios básicos para proyectar políticas de gestión metropolitana

El propósito del presente trabajo es reconocer, cómo a partir de las tensiones globales y locales, de carácter socio - espacial e imbricadas en el proceso de metropolización que acusa el ámbito expandido de la ciudad de Paraná, es factible identificar y analizar los criterios básicos para proyectar una inédita gestión metropolitana dentro del espacio regional que constituyen tanto el ejido de la capital de la Provincia de Entre Ríos como el de sus tres municipios conurbados. En consecuencia y a tal fin, se intenta aquí establecer los nuevos desafíos incorporados a la gestión urbano-ambiental, tanto provincial como municipal, dentro de los que se platea articular la intervención estatal y la participación comunitaria, en el marco de un proceso de ordenamiento territorial del ámbito metropolizado en esas cuatro jurisdicciones en las que hoy habitan más de trescientos mil comprovincianos. Se trata, por tanto, de un proyecto estratégico que institucionalmente persiga la posibilidad de articular en simultáneo cuatro criterios políticos considerados aquí básicos para la gestión democrática del territorio metropolitano: la gobernabilidad, la competitividad, la sustentabilidad y la inclusión social. Criterios que, dentro de esa inteligencia, guiarán el análisis desarrollado sobre propuestas de actuación, jurídico-normativas y de gestión para abordar la compleja problemática del espacio urbano-regional. Es en tal contexto entonces, y dentro de esos principios primordiales para la intervención urbano-territorial, en el que se estima posible plantear, desde el ámbito institucional del Gobierno de la Provincia y de los gobiernos municipales, un acotado y preciso conjunto de políticas sectoriales básicas de ordenamiento que habiliten al despliegue de estrategias comunes y de consenso social posible, destinadas a transformar las críticas condiciones por las que atraviesa la conurbación en su conjunto, sin por eso vulnerar la autonomía de la jurisdicciones municipales incluidas en el espacio geográfico. Concluyendo, en el presente trabajo se analizan e identifican en forma iniciática, los criterios esenciales para el logro de los objetivos territoriales y las metas institucionales que dentro de la gestión metropolitana, puedan asumir el Estado Provincial y las jurisdicciones municipales, en tanto dispositivos gubernamentales destinados a que legal y orgánicamente, sean orientadas las políticas que tengan el propósito de afrontar tanto los procesos territoriales distorsivos como los déficit, las asimetrías y las carencias socio-ambientales que acusa la población del Gran Paraná

Biopolítica, población y control

Los estudios del poder han volteado hace tiempo a la biopolítica, vista como la intromisión e injerencia del poder y la política sobre la vida. Se da en positivo y en negativo. De ahí la discusión sobre el control social, como una expresión de la biopolítica moderna. La conexión entre biopolítica y población no es menos significativa que la manera cómo el poder administra y regula los nacimientos y la migración así como la calidad de vida de los conglomerados sociales

Geochemistry at DSDP Hole 57-439

Acidic to intermediate volcanic rocks were obtained as boulders, pebbles, and clasts with intercalated matrix sediments near the Japan Trench. A 47.5-meter conglomerate bed unconformably overlies acoustic basement consisting of Upper Cretaceous siltstone and is overlain in turn by massive coarse-sandstone and siltstone beds with many fossil mollusks. The volcanic cobbles and boulders in the conglomerate show pronounced porphyritic texture. Their phenocrysts are plagioclase, hornblende, and biotite; the groundmass consists of plagioclase, K-feldspar, quartz, iron oxide, and altered interstitial glass. The Plagioclase content of these volcanic rocks is very high, whereas iron oxide minerals are rare. The chemical composition of these volcanic rocks was analyzed to determine the rock series. Matrix sediments were also analyzed chemically, and their chemical composition was found to be similar to that of volcanic rocks, except for a lower CaO content. SiO2 content of the volcanic rocks ranges from 60.23 to 73.90, corresponding to that of andesite to rhyolite. All the samples show extremely high Al2O3 content, which reflects the high amounts of modal plagioclase. These volcanic rocks belong to both the calc-alkalic and tholeiitic rock series, and the differentiation trend is controlled by fractional crystallization, mainly of plagioclase, K-feldspar, and hornblende. The assemblage of calc-alkalic and tholeiitic rock series is frequently observed in island arcs and active continental margins. These volcanic rocks are derived from the Oyashio ancient landmass, which is a slightly matured island arc.

Miocene to Pleistocene planktonic foraminifer biostratigraphy of ODP Leg 135 sites

Diverse and well-preserved planktonic foraminifers were recovered from six sites (834-839) drilled in the Lau Basin. Planktonic faunas from the Tongan Platform sites varied from those of the Lau Basin sites by being less well preserved (Site 840) to being very poorly preserved and very sparse (Site 841); at Site 841 most samples were barren. All sites penetrated a volcaniclastic sequence in which thick ash beds were encountered; foraminifer populations within the ash beds were often very small, making it difficult to obtain biostratigraphic data. No hiatuses were encountered in the upper Miocene to Pleistocene sections of the Lau Basin, but a possible break occurs at Site 840 on the Tongan Platform. Site 834 penetrated through a Quaternary-Pliocene sequence overlying basaltic basement, and topmost Miocene (Zone N17B) sediments interbedded within the volcanic sequence. Site 835 penetrated into the lower Pliocene (Zones N19 to N19-20). Site 836 penetrated the shortest section, with Zone N22 {Globorotalia (Truncorotalia) crassaformis hessi Subzone) directly overlying basalts. Site 837 penetrated into the basal part of Zone N22 (Globigerinoides quadrilobatus fistulosus Subzone) overlying basalt. Site 838 failed to encounter basalts, with the oldest sediment being from Zone N22 (Globigerinoides quadrilobatus fistulosus Subzone). Site 839, within the same basin as Site 838, located Zone N22 (Globigerinoides quadrilobatus fistulosus Subzone) sediments directly overlying igneous basement. Site 840 penetrated into the upper Miocene Zone N17A without encountering any major unconformity. Site 841, studied mainly from core-catcher samples, penetrated a Quaternary to questionable upper Miocene sequence that was in fault contact with middle Miocene (Zones N8 to N9) sediments. For the Lau Basin sites, reworking was encountered only in Sites 834 and 835. Site 834 was drilled adjacent to the Lau Ridge, on which are developed numerous reef al and shallow-water environments, where erosional conditions could have been expected during sea-level lowstands. Site 835 was drilled in a narrow basin that has been remote from these erosional influences; slumping and erosion of material from the adjacent basin slopes appears to have been the source of the reworking. For the Tongan Platform sites, reworking was observed only in the lower part of the upper Miocene section at Site 841, where late Eocene larger foraminifers are present in conglomerates and grits. The presence of Globorotalia (Globorotalia) multicamerata and small specimens of Sphaeroidinellopsis spp. in the Pleistocene of Site 840 may indicate reworking, but this is not clear. Unit I, which marks a reduction in volcanic activity in the Lau Basin, ranges in age from the lower part of Zone N22 (Globigerinoides quadrilobatus fistulosus Subzone) at Sites 834 and 835, to within Zone N22 (Globorotalia crassaformis hessi Subzone) at Sites 836 to 838, and within the upper part of Zone N22 (Bolliella praeadamsi Subzone) at Site 839. Units II and III are generally represented by thick to very thick ash beds, which generally contain low-diversity and often poorly preserved assemblages. Igneous sources seem to have remained important contributors of sediment up to the present day.

Coccoliths in phytoplankton of the Eastern Bering Sea in August 2001

Based on results of field observations in August 1998, July 2000, and August 2001 composition and quantitative distribution of coccolithophorids in the middle part of the Eastern Bering Sea shelf between 56°052'N and 59°019'N was characterized. Emiliania huxleyi abundance, biomass, and population structure as well as role of species in the coccolithophorid community and phytoplankton as a whole were evaluated. Abundance of the species in the upper mixed layer in bloom areas was 1-3 mln cells/l and biomass made up 30-75 mg C/m**3. E. huxleyi share in total phytoplankton numbers and biomass at that reached 98% and 84% respectively. Significant spatial heterogeneity of E. huxleyi, quantitative distribution and population size structure, as well as asynchronism in population development in neighboring parts of the bloom area were shown. The time period, during which population structure in certain part of the area shifts from domination of juvenile cells without coccoliths to a phase of active detritus formation with dying coccolithophorid cells involved, may be estimated as two weeks. A conclusion is made that after anomalous E. huxleyi bloom in 1997 mass development of coccolithophorids became a characteristic feature of phytoplankton community's seasonal succession in the middle part of the Eastern Bering Sea shelf.

Sedimentology of ODP Leg 126 deep-water volcaniclastics

Three sites were drilled in the Izu-Bonin forearc basin during Ocean Drilling Program (ODP) Leg 126. High-quality formation microscanner (FMS) data from two of the sites provide images of part of a thick, volcaniclastic, middle to upper Oligocene, basin-plain turbidite succession. The FMS images were used to construct bed-by-bed sedimentary sections for the depth intervals 2232-2441 m below rig floor (mbrf) in Hole 792E, and 4023-4330 mbrf in Hole 793B. Beds vary in thickness from those that are near or below the resolution of the FMS tool (2.5 cm) to those that are 10-15 m thick. The bed thicknesses are distributed according to a power law with an exponent of about 1.0. There are no obvious upward thickening or thinning sequences in the bed-by-bed sections. Spaced packets of thick and very thick beds may be a response to (1) low stands of global sea level, particularly at 30 Ma, (2) periods of increased tectonic uplift, or (3) periods of more intense volcanism. Graded sandstones, most pebbly sandstones, and graded to graded-stratified conglomerates were deposited by turbidity currents. The very thick, mainly structureless beds of sandstone, pebbly sandstone, and pebble conglomerate are interpreted as sandy debris-flow deposits. Many of the sediment gravity flows may have been triggered by earthquakes. Long recurrence intervals of 0.3-1 m.y. for the very thickest beds are consistent with triggering by large-magnitude earthquakes (M = 9) with epicenters approximately 10-50 km away from large, unstable accumulations of volcaniclastic sand and ash on the flanks of arc volcanoes. Paleocurrents were obtained from the grain fabric of six thicker sandstone beds, and ripple migration directions in about 40 thinner beds; orientations were constrained by the FMS images. The data from ripples are very scattered and cannot be used to specify source positions. They do, however, indicate that the paleoenvironment was a basin plain where weaker currents were free to follow a broad range of flow paths. The data from sandstone fabric are more reliable and indicate that turbidity currents flowed toward 150? during the time period from 28.9 to 27.3 Ma. This direction is essentially along the axis of the forearc basin, from north to south, with a small component of flow away from the western margin of the basin.

Mineral composition, major element oxides and trace element concentration of sediments from ODP Leg 180 sites

Middle Miocene to Holocene fine-grained argillaceous sediments (clays, claystones/muds, and mudstones), which volumetrically dominated the sediment recovery in the Woodlark Basin during Leg 180, were chemically analyzed for major elements, trace elements, and some rare earth elements by X-ray fluorescence. Selected samples also underwent X-ray diffraction (XRD) analysis for mineral determination. The results shed light on sediment provenance when combined with shipboard sediment descriptions, smear slide study, and XRD. The oldest sediments recovered (Site 1108) of middle-late Miocene age include volcanogenic muds with distinctive high MgO and K2O, indicative of a relatively basic calc-alkaline source related to an inferred Miocene forearc succession. The forearc basement, composed of diabase and basalt, was locally exposed (Site 1109) and eroded in the late Miocene (<5.4-9.93 Ma), giving rise to fluvial conglomerates (Sites 1109, 1115, and 1118). Chemically distinctive fine-grained claystones and siltstones (with relatively high Ti, low K) are compatible with derivation from tropically weathered basic igneous rocks, correlated with the Paleogene Papuan ophiolite. Overlying latest Miocene-Pleistocene fine-grained sediments throughout the Woodlark Basin were partly derived from calc-alkaline volcanic sources. However, relatively high abundances of Al2O3 and related element oxides (K2O and Na2O) and trace elements (e.g., Rb and Y) reflect an additional terrigenous input throughout the basin, correlated with pelitic metamorphic rocks exposed on Papua New Guinea and adjacent areas. In addition, sporadic high abundances of Cr and Ni, some other trace metals, and related minerals (talc, crysotile, and chlorite) reflect input from an ophiolitic terrain dominated by ultramafic rocks, correlated with the Paleogene Papuan ophiolite. The source areas possibly included serpentinized ultramafic ophiolitic rocks exposed in the Papua New Guinea interior highlands. Chemical evidence further indicates that fine-grained terrigenous sediment reached the Woodlark Basin throughout its entire late Miocene-Holocene history. Distinctive high-K volcanogenic muds rich in tephra and volcanic ash layers that appear at <2.3 Ma (Sites 1109 and 1115) are indicative of high-K calc-alkaline volcanic centers, possibly located in the Dawson Strait, Moresby Strait, or Dobu Seamount area. Chemical diagenesis of fine-grained sediments within the Woodlark Basin is reflected in clay neomorphism and localized formation of minerals including dolomite, ankerite, and zeolite but has had little effect on the bulk chemical composition of most samples.

Tab. 1: Mineralogical composition and chemical analyses of major and trace elements of Ameghino Formation rocks

As a result of a petrographical, mineralogical and geochemical characterization of the Ameghino Formation mudstones (Upper Jurassic- Lower Cretaceous, Antarctic Peninsula), "epiclastic" radiolaria-rich and mixed (radiolaria-rich + tuff) mudstone types were recognized. Contents of clastic material in the mudstones generally increase with younger paleontological age, but local exceptions to this trend have been found. The anoxic environment of the lower part of the sequence changes to more oxidizing conditions towards the top, in transition to the Hauterivian - Barrêmian conglomerates. Element to element correlations show good agreement with the normal differentiation trends of volcanic (andesite-rhyolite) rocks, suggesting that the overall sequence is mainly volcanic in origin with various grade of reworking. For example, the radiolaria-rich mudstone matrix could have been originated from very fine touffaceous suspensions deposited very slowly after the main fall of the tuffs. However, in the upper part of the sequence, some epiclastic supply is revealed by petrographic evidence and illite crystallinity index. The clay mineral association (illite, chlorite and illite-smectite mixed layers) is mainly of diagenetic origin in the stratigraphically lower sections. Low percentages of expandable layers in the illite-smectite mixed layers, as well as the general mineralogical association, suggest a late mesodiagenetic stage, and together with geological evidence, a relatively deep burial (> 1000 m - probably > 2500 m) and temperatures exceeding 100°C.

Sandstone and siltstone beds overlying conglomerate at DSDP Hole 59-439

Massive sandstone and siltstone beds with many shallow-water megafossils overlie acidic volcanic conglomerates at DSDP Site 439. Smear-slides, thin sections from coarse fractions, and heavy minerals of the sandstone and siltstone beds were analyzed. The sandstones and siltstones are very rich in lithic fragments and are classified as lithic arenite and (or) lithic wacke. Hornblende and clinopyroxene are abundant, and zircon is present in most of the examined samples. The proportions of sandstone, chert, and volcanic rock in the coarse fraction are variable, but fragments of clastic rocks and cherts are predominant. Plagioclase crystals of volcanic-rock origin, such as highly zoned plagioclase and very fine, euhedral, lath-shaped plagioclase, are frequently observed. Metamorphic-rock fragments and metamorphic minerals are also observed. Thus, the provenance of the sandstone and siltstone beds appears to have been a slightly mature island arc, the Oyashio ancient landmass, consisting of clastic sediments and metamorphic and volcanic rocks.

Conglomerate and sandstone petrography at DSDP Hole 58-445

Conglomerates and sandstones in lithologic unit V at DSDP Site 445 comprise lithic clasts, detrital minerals, bioclasts, and authigenic minerals. The lithic clasts are dominantly plagioclase-phyric basalt and microdolerite, followed by plagioclase-clinopyroxene-phyric basalt, aphyric basalt, chert, and limestone. A small amount of hornblende schist occurs. Detrital minerals are dominantly plagioclase, augite, titaniferous augite, olivine, green to pale-brown hornblende, and dark-brown hornblende, with subordinate chromian spinel, epidote, ilmenite, and magnetite, and minor amounts of diopside, enstatite, actinolite, and aegirine-augite. Bioclasts are Nummulites boninensis, Asterocyclina sp. cf. A. penuria, and some other larger foraminifers. Correlation of cored and dredged samples indicates that the Daito Ridge is mainly composed of igneous, metamorphic, ultramafic, and sedimentary rocks. The igneous rocks are mafic (probably tholeiitic) and alkalic. The metamorphic rocks are hornblende schist, tremolite schist, and diopside-chlorite schist. The ultramafic rocks are alpinetype peridotites. Mineralogical data suggest that there were two metamorphic events in the Daito Ridge. The older one was intermediate- to high-pressure metamorphism. The younger one was contact metamorphism caused by a Paleocene volcanic event, possibly related to the beginning of spreading of the west Philippine Basin. The ultramafic rocks suffered from the same contact metamorphism. During the Eocene, exposed volcanic and metamorphic rocks on the uplifted Daito Ridge may have supplied pebble clasts to the surrounding coast and shallow sea bottom. The steep slope offshore may have caused frequent slumping and transportation of the pebble clasts and shallow-water benthic organisms into deeper water, forming the conglomerates and sandstones treated here.