Iron and manganese in bottom sediments and interstitial waters sampled in the White Sea on August 21-30, 2003

Iron and manganese in bottom sediments studied along the sublatitudinal transect from Kandalaksha to Arkhangelsk are characterized by various contents and speciations depending on sedimentation environment, grain size of sediments, and diagenetic processes. The latter include redistribution of reactive forms leading to enrichment in Fe and Mn of surface sediments, formation of films, incrustations, and ferromanganese nodules. Variations in total Fe content (2-8%) are accompanied by changes in concentration of its reactive forms (acid extraction) and concentration of dissolved Fe in interstitial waters (1-14 µM). Variations in Mn content in bottom sediments (0.03-3.7%) and interstitial waters (up to 500 µM) correspond to high diagenetic mobility of this element. Changes in oxidation degree of chemical elements result in redox stratification of sediment strata with maximum concentrations of Fe, Mn, and sulfides. Organic matter of bottom sediments with considerable terrestrial constituent is oxidized by bottom water oxygen mainly at the sediment surface or in anaerobic conditions within the sediment strata. The role of inorganic components in organic matter oxidation changes from surface layer bottom sediments (where manganese oxyhydroxide dominates among oxidants) to deeper layers (where sulfate of interstitial water serves as the main oxidant). Differences in river runoff and hydrodynamics are responsible for geochemical asymmetry of the transect. The deep Kandalaksha Bay serves as a sediment trap for manganese (Mn content in sediments varies within 0.5-0.7%), whereas the sedimentary environment in the Dvina Bay promotes its removal from bottom sediments (Mn 0.05%).

Geochemistry and mineralogy of Eocene-Oligocene sediments of IODP Hole 302-M0002A

In 2004, Integrated Ocean Drilling Program Expedition 302 (Arctic Coring Expedition, ACEX) to the Lomonosov Ridge drilled the first Central Arctic Ocean sediment record reaching the uppermost Cretaceous (~430 m composite depth). While the Neogene part of the record is characterized by grayish-yellowish siliciclastic material, the Paleogene part is dominated by biosiliceous black shale-type sediments. The lithological transition between Paleogene and Neogene deposits was initially interpreted as a single sedimentological unconformity (hiatus) of ~26 Ma duration, separating Eocene from Miocene strata. More recently, however, continuous sedimentation on Lomonosov Ridge throughout the Cenozoic was proclaimed, questioning the existence of a hiatus. In this context, we studied the elemental and mineralogical sediment composition around the Paleogene-Neogene transition at high resolution to reconstruct variations in the depositional regime (e.g. wave/current activity, detrital provenance, and bottom water redox conditions). Already below the hiatus, mineralogical and geochemical proxies imply drastic changes in sediment provenance and/or weathering intensity in the hinterland, and point to the existence of another, earlier gap in the sediment record. The sediments directly overlying the hiatus (the Zebra interval) are characterized by pronounced and abrupt compositional changes that suggest repeated erosion and re-deposition of material. Regarding redox conditions, euxinic bottom waters prevailed at the Eocene Lomonosov Ridge, and became even more severe directly before the hiatus. With detrital sedimentation rates decreasing, authigenic trace metals were highly enriched in the sediment. This continuous authigenic trace metal enrichment under persistent euxinia implies that the Arctic trace metal pool was renewed continuously by water mass exchange with the world ocean, so the Eocene Arctic Ocean was not fully restricted. Above the hiatus, extreme positive Ce anomalies are clear signs of a periodically well-oxygenated water column, but redox conditions were highly variable during deposition of the Zebra interval. Significant Mn enrichments only occur above the Zebra interval, documenting the Miocene establishment of stable oxic conditions in the Arctic Ocean. In summary, extreme and abrupt changes in geochemistry and mineralogy across the studied sediment section do not suggest continuous sedimentation at the Lomonosov Ridge around the Eocene-Miocene transition, but imply repeated periods of very low sedimentation rates and/or erosion.

Sedimentology of the Vietnam shelf

On the Vietnam Shelf more than 1000 miles of shallow high-resolution seismics were analyzed to unravel post-glacial evolution in a tropical, siliciclastic environment together with 25 sediment cores from water depths between 21 and 169 m to determine stratigraphy, distribution and style of sedimentation. Fourty-seven samples were dated with the AMS-14C technique. The shelf was grouped into three regions: a southern part, a central part, and a northern part. On the broad Southern Shelf, sedimentation is influenced by the Mekong River, which drains into the SCS in this area. Here, incised valley fills are abundant that were cut into the late Pleistocene land surface by the Paleo-Mekong River during times of sea level lowstand. Those valleys are filled with transgressive deposits. The Holocene sedimentation rate in this low gradient accommodation-dominated depositional system is in the range of 5-10 and 25-40 cm/ky at locations sheltered from currents. The Central Shelf is narrow and the sedimentary strata are conformable. Here, numerous small mountainous rivers reach the SCS and transport large amounts of detrital sediment onto the shelf. Therefore, the Holocene sedimentation rate is high with values of 50-100 cm/ky in this supply-dominated depositional system. The broad Northern Shelf in the vicinity of the Red River Delta shows, as on the Southern Shelf, incised valleys cut into the Pleistocene land surface by paleo river channels. In this accommodation-dominated shelf area, the sedimentation rate is low with values of 5-10 cm/ky. Where applicable, we assigned the sampled deposits to different paleo-facies. The latter are related to certain intervals of water depths at their time of deposition. Comparison with the sea-level curve of (Hanebuth et al., 2000, doi:10.1126/science.288.5468.1033) indicates subsidence on the Central Shelf, which is in agreement with the high sedimentation rates in this area. In contrast, data from the Northern Shelf suggest tectonic uplift that might be related to recent tectonic movements along the Ailao Shan-Red River Fault zone. Data from the Southern Shelf are generally in agreement with the sea-level curve mentioned above.

Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica

Early Oligocene siliceous microfossils were recovered in the upper c. 193 m of the CRP-3 drillcore. Although abundance and preservation are highly variable through this section, approximately 130 siliceous microfossil taxa were identified, including diatoms, silicoflagellates, ebridians, chrysophycean cysts, and endoskeletal dinoflagellates. Well-preserved and abundant assemblages characterize samples in the upper c. 70 m and indicate deposition in a coastal setting with water depths between 50 and 200 m. Abundance fluctuations over narrow intervals in the upper c. 70 mbsf are interpreted to reflect environmental changes that were either conducive or deleterious to growth and preservation of siliceous microfossils. Only poorly-preserved (dissolved, replaced, and/or fragmented) siliceous microfossils are present from c. 70 to 193 mbsf. Diatom biostratigraphy indicates that the CRP-3 section down to c. 193 mbsf is early Oligocene in age. The lack of significant changes in composition of the siliceous microfossil assemblage suggests that no major hiatuses are present in this interval. The first occurrence (FO) of Cavitatus jouseanus at 48.44 mbsf marks the base of the Cavitatus jouseanus Zone. This datum is inferred to be near the base of Subchron C12n at c. 30.9 Ma. The FO of Rhizosolenia antarctica at 68.60 mbsf marks the base of the Rhizosolenia antarctica Zone. The FO of this taxon is correlated in deep-sea sections to Chron C13 (33.1 to 33.6 Ma). However, the lower range of R. antarctica is interpreted as incomplete in the CRP-3 drillcore, as it is truncated at an underlying interval of poor preservation: therefore, an age of c. 33.1 to 30.9 Ma is inferred for interval between c. 70 and 50 mbsf. The absence of Hemiaulus caracteristicus from diatom-bearing interval of CRP-3 further indicates an age younger than c. 33 Ma (Subchron C13n) for strata above c. 193 mbsf. Siliceous microfossil assemblages in CRP-3 are significantly different from the late Eocene assemblages reported CIROS-1 drillcore. The absence of H. caracteristicus, Stephanopyxis splendidus, and Pterotheca danica, and the ebridians Ebriopsis crenulata, Parebriopsis fallax, and Pseudoammodochium dictyoides in CRP-3 indicates that the upper 200 m of the CRP-3 drillcore is equivalent to part of the stratigraphic interval missing within the unconformity at c. 366 mbsf in CIROS-1.

Calcareous nannofossils of ODP Holes 114-699A and 114-700B

Ocean Drilling Program (ODP) Leg 114 recovered nannofossil-bearing sediments from seven sites in the high latitudes of the South Atlantic Ocean. Cretaceous sections were recovered from Sites 698 and 700, located on the Northeast Georgia Rise and its lower flanks, respectively. These contain distinctive high-latitude nannofossil floras similar to those from high-latitude areas of the Northern Hemisphere. Most of the biostratigraphic datums used to date the upper Campanian to Maestrichtian interval appear to lie at approximately the same level in both hemispheres. The FAD of Nephrolithus frequens is confirmed to be diachronous with an earlier occurrence in high latitudes. The LAD of Monomarginatus primus n. sp. also appears to be diachronous with a later LAD in the high latitudes of the Southern Hemisphere. Fossiliferous Paleocene to lowermost Miocene sediments were recovered at all seven sites, from the Northeast Georgia Rise in the west to the Meteor Rise in the east. These nannofossil floras, although restricted in diversity and only poorly preserved, are sufficiently distinctive to allow the recognition of 19 zones and three subzones, which are used to date and correlate the cores recovered. Only Site 704 on the Meteor Rise yielded a substantial section of Miocene to Quaternary nannofossil-rich sediments. The nannofossil floras of this section are of very low diversity, with usually fewer than eight species present. Some stratigraphic ranges of important biostratigraphic datum species are observed to be different in the high-latitude sections from those recorded from low-latitude areas. The LAD of Reticulofenestra bisecta, when calibrated by magnetostratigraphy, appears to occur earlier in Hole 699A (within Chron C6CR) than in Hole 703A and possibly Hole 704B and in other published accounts of lower latitude sites in the South Atlantic. The FAD of Nannotetrina fulgens/N. cristata appears to occur later in Hole 702B (Chron C20R) than it does in other published accounts of lower latitude sites in the South Atlantic. Diachroneity is also suspected in the stratigraphic ranges of Chiasmolithus solitus and Chiasmolithus oamaruensis, although poor magnetostratigraphic results through the critical interval prevent confirmation of this. Differences in the relative stratigraphic ranges of lsthmolithus recurvus and Cribrocentrum coenurumlC. reticulatum at Sites 699 and 703 are noted. These possibly suggest warmer surface waters on the eastern side (Site 703) of the middle to late Eocene South Atlantic than those on the western side (Site 699). The diversities of the nannofossil floras and the presence of the warm-water genera Discoaster, Sphenolithus, Helicosphaera, and Amaurolithus reflect the changing surface water temperatures throughout the Cenozoic. Warmer periods are inferred for the late Paleocene to early middle Eocene, late middle Eocene to late Eocene, latest Oligocene to earliest Miocene, and possibly the Pliocene. Colder periods are inferred for the middle Eocene, most of the Oligocene, and the Miocene. Dramatic changes in the nannofossil floras of the Pleistocene of Site 704 are thought to reflect a rapidly changing environment. Monomarginatus primus, a new species from the Upper Cretaceous strata of Hole 700B, is described.

Organic geochemical character of selected cores at DSDP Hole 75-530A

The Albian/Cenomanian strata in Hole 530A are organically richer than are the post-Cenomanian strata. Organic matter is thermally immature and appears to be of dominantly marine origin with either variable levels of oxidation or variable amounts of terrestrial input. Geochemical data alone cannot establish whether the black shales present in Hole 530A represent deposition within a stagnant basin or within an expanded oxygen-minimum layer

Apuntes para el estudio del ocio y las formas de sociabilidad de los estratos superiores en la Argentina contemporánea

En este trabajo sostengo que existe una relación entre ocio y estratificación social, o más específicamente, entre las formas de sociabilidad del tiempo libre y los estratos superiores, donde las prácticas de sociabilidad, esparcimiento y deporte operan como instancias de producción y reproducción, así como también de reconversión y recomposición social y simbólica de las categorías sociales de los estratos superiores. En el primer capítulo abordo buena parte de la bibliografía sobre estratificación social, clases sociales y elites para fundamentar el valor analítico de esta dimensión para las ciencias sociales en términos generales, y para el estudio de los fenómenos ligados a la sociabilidad del tiempo libre entre los estratos superiores, en particular. En el segundo capítulo intento fundamentar el valor sociológico de la dimensión del ocio y el tiempo libre, así como sus formas de sociabilidad, especialmente en función de su articulación en torno a los estratos superiores. En el tercer capítulo procuro abordar la relación entre estratos superiores y sociabilidad del tiempo libre para (y desde) el contexto argentino contemporáneo. Intentaré trabajar en torno al modo en que ha sido pensada y es posible pensar esa relación para la escena local, y al mismo tiempo, sobre el modo en que la reflexión enfocada en el contexto local nos permite elaborar marcos de análisis para el estudio del fenómeno de la sociabilidad del tiempo libre entre los estratos superiores, en general. Finalmente, la perspectiva que desarrollo aboga por un desplazamiento analítico que vaya desde las interpretaciones unidimensionales de los fenómenos ligados a la sociabilidad, el deporte y el ocio entre los estratos superiores hacia las lecturas multidimensionales. Un desplazamiento que nos permita interpretar la relación entre los procesos estructurales, las instancias de sociabilidad y las prácticas de los agentes en términos de afinidades, reponiendo la positividad de cada dimensión sin la necesidad de recurrir a las sobredeterminaciones o los reduccionismos de las más variadas especies

Organic matter composition of Cretaceous sediments of the central Pacific Ocean

Complete records of organic-carbon-rich Cretaceous strata were continuouslycored on the flanks of the Mid-Pacific Mountains and southern Hess Rise in the central North Pacific Ocean during DSDP Leg 62. Organic-carbon-rich laminated silicified limestones were deposited in the western Mid-Pacific Mountains during the early Aptian, a time when that region was south of the equator and considerably shallower than at present. Organic-carbon-rich, laminated limestone on southern Hess Rise overlies volcanic basement and includes 136 m of stratigraphic section of late Albian to early Cenomanian age. This limestone unit was deposited rapidly as Hess Rise was passing under the equatorial high-productivity zone and was subsiding from shallow to intermediate depths. The association of volcanogenic components with organic-carbon-rich strata on Hess Rise in the Mid-Pacific Mountains is striking and suggests that there was a coincidence of mid-plate volcanic activity and the production and accumulation of organic matter at intermediate water depths in the tropical Pacific Ocean during the middle Cretaceous. Pyrolysis assays and analyses of extractable hydrocarbons indicate that the organic matter in the limestone on Hess Rise is composed mainly of lipid-rich kerogen derived from aquatic marine organisms and bacteria. Limestones from the Mid-Pacific Mountains generally contain low ratios of pyrolytic hydrocarbons to organic carbon and low hydrogen indices, suggesting that the organic matter may contain a significant proportion of land-derived material, possibly derived from numerous volcanic islands that must have existed before the area subsided. The organic carbon in all samples analyzed is isotopically light (d13C -24 to -29 per mil) relative to most modern rine organic carbon, and the lightest carbon is also the most lipid-rich. There is a positive linear correlation between sulfur and organic carbon in samples from Hess Rise and from the Mid-Pacific Mountains. The slopes and intercepts of C-S regression lines however, are different for each site and all are different from regression lines for samples from modern anoxic marine sediments and from Black Sea cores. The organic-carbon-rich limestones on Hess Rise, the Mid-Pacific Mountains, and other plateaus and seamounts in the Pacific Ocean are not synchronous but do occur within the same general middle Cretaceous time period as organic-carbon-rich lithofacies elsewhere in the world ocean, particularly in the Atlantic Ocean. Strata of equivalent age in the deep basins of the Pacific Ocean are not rich in organic carbon, and were deposited in oxygenated environments. This observation, together with the evidence that the plateau sites were considerably shallower and closse to the equator during the middle Creataceous suggests that local tectonic and hydrographic conditions may have resulted in high surface-water productivity and the preservation of organic matter in an oxygen-deficient environment where an expanded mid-water oxygen minimum developed and impinged on elevated platforms and seamounts.

Perspectivas clásicas y contemporáneas sobre la estratificación social : Aportes de análisis de clase y de la perspectiva de las elites para el estudio de los estratos superiores

El presente artículo procura poner en consideración algunos elementos analíticos, presentes tanto en los estudios sociales de las elites como en las perspectivas sobre las clases sociales, que representan un aporte para la investigación de los procesos de estratificación social en general, y de los estratos superiores en particular. En esta dirección, se analizan los supuestos de los cuales derivan las dos principales perspectivas de clase, la relacional y la gradacional, así como las diferentes revisiones y reelaboraciones desarrolladas a lo largo del siglo XX. Por otro lado, se aborda críticamente el aporte de la perspectiva clásica de las elites y de algunos intentos de articulación entre dicho enfoque y la perspectiva de clase. El artículo concluye considerando algunas problematizaciones desarrolladas dentro de la bibliografía reciente sobre elites, con el fin de recuperar ciertos elementos analíticos valiosos para el estudio de los estratos superiores. En este sentido, intenta resaltar el aporte de los enfoques que procuran articular la dinámica de la reproducción con las de la recomposición e incluso disolución, operantes entre los grupos de elite y los estratos superiores

Los mapas de la fragmentación territorial en Tandil a partir de la escolarización

Los actuales procesos de globalización han reforzado las tendencias hacia la fragmentación social. El problema de la educación no existe en forma singular, sino que es plural y diferenciado según el segmento social de que se trate. La desigualdad y la exclusión social educativa, en una ciudad intermedia como Tandil, se manifiestan y materializan territorialmente. La finalidad de este trabajo es dar cuenta del proceso de fragmentación territorial, a través del análisis e interpretación de la escolarización a partir de los resultados del Censo 2001.

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

El avance de los agronegocios en regiones marginales del agro pampeano : Concentración de la producción y tensiones entre las fracciones del capital agrario

En la Argentina, durante la última década las actividades agrícolas han avanzado sobre regiones marginales para la agricultura como la Depresión del Salado de la provincia de Buenos Aires. El objetivo central de este trabajo es identificar la diversidad de formas en que se expresan los agronegocios en los partidos de Chascomús y Lezama. Para ello nos proponemos caracterizar los principales agentes socioeconómicos que intervienen en la producción de granos y analizar las disputas que se generan por el uso del suelo. La metodología utilizada consiste en el análisis cualitativo de entrevistas semiestructuradas a informantes clave y a agentes de empresas agrícolas, combinado con el análisis de fuentes de información secundaria.Los resultados del trabajo constatan la intensificación en la competencia por el uso del suelo en la región, concluyendo que las nuevas reglas de juego han implicado la consolidación de algunos sectores (agentes externos y actores locales reconvertidos) y la subordinación de otros, entre ellos los estratos de la pequeña producción.

Ocio, consumo y deporte entre los estratos superiores : Aportes para la elaboración de un campo problemático

Este artículo tiene como propósito abordar un campo de preocupaciones que giran en torno a la productividad social de los espacios y prácticas del ocio, el consumo y el deporte, en particular en lo relativo a los estratos superiores y sus formas de sociabilidad. En esta dirección, se desarrolla un trabajo crítico en torno a las principales perspectivas sobre ocio y consumo, poniendo de relieve los supuestos normativos subyacentes en algunos casos, y los aportes conceptuales relativos a la positividad del ocio y el consumo como terrenos de estructuración de las categorías sociales, en otros. Finalmente, el artículo analiza los aportes de la sociología y la antropología del deporte para el estudio de la relación entre prácticas deportivas y posiciones sociales, argumentando a favor de la jerarquización del estudio de los fenómenos relativos al deporte, el ocio y el consumo como campos legítimos de investigación de las transformaciones recientes en la estructura social, y en particular, en lo referido a los estratos superiores

Upper Cenozoic dinoflagellate cysts from the continental slope and rise off New Jersey

This report contains the occurrence data for dinoflagellate cysts recorded from 163 samples taken from Sites 902 through 906, during Ocean Drilling Program (ODP) Leg 150. The dinoflagellate cyst (dinocyst) stratigraphy has been presented in Mountain, Miller, Blum, et al. (1994, doi:10.2973/odp.proc.ir.150.1994), and was based on these data. This report provides the full dinocyst data set supporting the dinocyst stratigraphic interpretations made in Mountain, Miller, Blum, et al. (1994). For Miocene shipboard dinocyst stratigraphy, I delineated 10 informal zones: pre-A, and A through I, in ascending stratigraphic order. These zones are defined in Shipboard Scientific Party (1994a, doi:10.2973/odp.proc.ir.150.103.1994), and are based on my studies of Miocene dinocyst stratigraphy in the Maryland and Virginia coastal plain (de Verteuil and Norris, 1991, 1992; de Verteuil, 1995). This zonation has been slightly revised (de Verteuil and Norris, 1996), and the new formal zone definitions are repeated below. Each new zone has an alpha-numeric abbreviation starting with "DN" (for Dinoflagellate Neogene). The equivalence between the informal zones reported in Mountain, Miller, Blum, et al. (1994), and the new DN zones is illustrated in Figure 1. For clarity, I delineated both zonations in the range charts that accompany this report (Tables 1-6). De Verteuil and Norris (1996a), using these and other data, correlated the DN zonation with the geological time scale of Berggren et al. (1995). Figure 2 summarizes these correlations and can be used to check the chronostratigraphic position of samples in this report, as determined by dinocyst stratigraphy. A thorough discussion of the basis for, and levels of uncertainty associated with, these correlations to the Cenozoic time scale can be found in de Verteuil and Norris (1996a). The Appendix lists all the dinocyst taxa recorded during shipboard analyses of Leg 150 samples. Open nomenclature is used for undescribed taxa. The range charts and Appendix also include reference to several new taxa that de Verteuil and Norris (1996b) described from Miocene coastal plain strata in Maryland and Virginia. Names of these taxa in Tables 1 through 6 and in the Appendix of this report are not intended for effective publication as defined in the International Code of Botanical Nomenclature (ICBN, Greuter et al., 1994). Therefore, taxonomic nomenclature contained in this report is not to be treated as meeting the conditions of effective and valid publication (ICBN; Article 29).

Apuntes para el estudio del ocio y las formas de sociabilidad de los estratos superiores en la Argentina contemporánea

En este trabajo sostengo que existe una relación entre ocio y estratificación social, o más específicamente, entre las formas de sociabilidad del tiempo libre y los estratos superiores, donde las prácticas de sociabilidad, esparcimiento y deporte operan como instancias de producción y reproducción, así como también de reconversión y recomposición social y simbólica de las categorías sociales de los estratos superiores. En el primer capítulo abordo buena parte de la bibliografía sobre estratificación social, clases sociales y elites para fundamentar el valor analítico de esta dimensión para las ciencias sociales en términos generales, y para el estudio de los fenómenos ligados a la sociabilidad del tiempo libre entre los estratos superiores, en particular. En el segundo capítulo intento fundamentar el valor sociológico de la dimensión del ocio y el tiempo libre, así como sus formas de sociabilidad, especialmente en función de su articulación en torno a los estratos superiores. En el tercer capítulo procuro abordar la relación entre estratos superiores y sociabilidad del tiempo libre para (y desde) el contexto argentino contemporáneo. Intentaré trabajar en torno al modo en que ha sido pensada y es posible pensar esa relación para la escena local, y al mismo tiempo, sobre el modo en que la reflexión enfocada en el contexto local nos permite elaborar marcos de análisis para el estudio del fenómeno de la sociabilidad del tiempo libre entre los estratos superiores, en general. Finalmente, la perspectiva que desarrollo aboga por un desplazamiento analítico que vaya desde las interpretaciones unidimensionales de los fenómenos ligados a la sociabilidad, el deporte y el ocio entre los estratos superiores hacia las lecturas multidimensionales. Un desplazamiento que nos permita interpretar la relación entre los procesos estructurales, las instancias de sociabilidad y las prácticas de los agentes en términos de afinidades, reponiendo la positividad de cada dimensión sin la necesidad de recurrir a las sobredeterminaciones o los reduccionismos de las más variadas especies