Lista de los peces continentales de la provincia de Tierra del Fuego, Antartida e Islas del Atlantico Sur

Esta serie tiene como finalidad dar a conocer las especies presentes en los diferentes estados provinciales.

Lista comentada de la ictiofauna del Canal Beagle, Tierra del Fuego, Argentina. Iconografía.

A ciento veintidós años de las primeras menciones realizadas por Perugia en 1891 sobre peces del Canal Beagle, editamos la presente iconografía que incluye alrededor de treinta especies de las mencionadas por López et al., en 1996. Este trabajo, desarrollado en el CADIC dentro del proyecto Biología de los recursos ictícos del Canal de Beagle financiado por el CONICET, junto al publicado por Lloris y Rucabado (1991), proveyeron elementos de base para tener una visión más profunda del componente ictiofaunistíco de la región. En la presente publicación se destaca la magnífica obra del maestro Miguel Barbagallo, quién vuelca su capacidad y espíritu en estas láminas, las que además de su valor artístico son un aporte más a la consolidación del conocimiento de los recursos naturales de nuestro país.

Late Holocene climatic changes in Tierra del Fuego based on multiproxy analyses of peat deposits

A ca. 1400-yr record from a raised bog in Isla Grande, Tierra del Fuego, Argentina, registers climate fluctuations, including a Medieval Warm Period, although evidence for the 'Little Ice Age' is less clear. Changes in temperature and/or precipitation were inferred from plant macrofossils, pollen, fungal spores, testate amebae, and peat humification. The chronology was established using a C-14 wiggle-matching technique that provides improved age control for at least part of the record compared to other sites. These new data are presented and compared with other lines of evidence from the Southern and Northern Hemispheres. A period of low local water tables occurred in the bog between A.D. 960-1020, which may correspond to the Medieval Warm Period date range of A.D. 950-1045 generated from Northern Hemisphere tree-ring data. A period of cooler and/or wetter conditions was detected between ca. A.D. 1030 and I 100 and a later period of cooler/wetter conditions estimated at ca. cal A.D. 1800-1930, which may correspond to a cooling episode inferred from Law Dome, Antarctica. (C) 2004 University of Washington. All rights reserved.

Postglacial vegetation dynamics of western Tierra del Fuego

The southern fringes of the South American landmass provide a rare opportunity to examine the development of moorland vegetation with sparse tree cover in a wet, cool temperate climate of the Southern Hemisphere. We present a record of changes in vegetation over the past 17,000 years, from a lake in extreme southern Chile (Isla Santa Inés, Magallanes region, 53°38.97S; 72°25.24W), where human influence on vegetation is negligible. The western archipelago of Tierra del Fuego remained treeless for most of the Lateglacial period; Lycopodium magellanicum, Gunnera magellanica and heath species dominated the vegetation. Nothofagus may have survived the last glacial maximum at the eastern edge of the Magellan glaciers from where it spread southwestwards and established in the region at around 10,500 cal. yr BP. Nothofagus antarctica was likely the earlier colonizing tree in the western islands, followed shortly after by Nothofagus betuloides. At 9000 cal. yr BP moorland communities expanded at the expense of Nothofagus woodland. Simultaneously, Nothofagus species shifted to dominance of the evergreen Nothofagus betuloides and the Magellanic rain forest established in the region. Rapid and drastic vegetation changes occurred at 5200 cal. yr BP, after the Mt Burney MB2 eruption, including the expansion and establishment of Pilgerodendron uviferum and the development of mixed Nothofagus-Pilgerodendron-Drimys woodland. Scattered populations of Nothofagus, as they occur today in westernmost Tierra del Fuego may be a good analogue for Nothofagus populations during the Lateglacial in eastern sites.

Salud en los extremos. Escenario epidemiológico y sanitario en Tierra del Fuego, 1890-1930

Objetivo: Caracterizar epidemiológica y sanitariamente la ciudad de Ushuaia (territorio nacional de Tierra del Fuego) entre 1890 y 1930, momento clave en el que se profundizan paralela y articuladamente dos procesos: el contacto interétnico y la consolidación del Estado-Nación argentino Metodología: Se analizaron todas las actas de defunción disponibles para el lapso 1890-1930, lo mismo que los documentos de la gobernación pertinentes y su cruce con fuentes secundarias a fin de obtener el perfil sanitario de la ciudad y su relación con el país en cuanto al tipo de fase epidemiológica, las tasas de mortalidad, la estructura demográfica y la estructura en la atención sanitaria. Resultados: Se concluye sobre la relevancia de las enfermedades infecciosas —y dentro de estas la tuberculosis—, en la ciudad, en general, y en la población indígena y penal, en particular. Dicho perfil epidemiológico evidenció las falencias de un sistema sanitario nacional aún no consolidado, especialmente en una región de dificultoso alcance.

Bases y estrategias para animar y promover el cambio educativo en Tierra del Fuego : propuesta para la Nueva Provincia Argentina.

El objetivo del trabajo es la elaboración de las bases y estrategias que permitan promover el cambio educativo en la Tierra del Fuego, último territorio nacional de la República Argentina. En primer lugar trata de delimitar el significado y alcance de los siguientes conceptos: bases, estrategias, cambio, reforma e innovación. Analiza la problemática concreta del cambio de la educación fueguina, teniendo en cuenta tanto las bases teóricas como la práctica de procesos de cambio generados desde los distintos estamentos de la educación. Estudia tanto las fuentes del cambio y los factores coadyuvantes, como los agentes intervinientes en el mismo, fundamentando la necesidad de una intervención planificada en la educación de dicho territorio. Constata la lentitud en los procesos de cambio en la educación argentina y propone una serie de estrategias partiendo del modelo de investigación, desarrollo y difusión del cambio educativo.

Towards high-resolution shell midden archaeology: Experimental and ethnoarchaeology in Tierra del Fuego (Argentina)

This paper discusses the ongoing ethnoarchaeological research carried out in Yamana shell middens of Tierra del Fuego. Ethnoarchaeology is used in this research as a tool to improve the archaeological methodology by testing it against anthropological, ethnographical and ethnological sources for achieving more accurate reconstructions of past societies. The ethnographical/ethnological information also is coupled with an experimental approach devised to understand physical and social processes, such as site formation processes and resource use and management. Specifically, this experimental approach was applied to the archaeological sites Tunel VII and Lanashuaia I (Tierra del Fuego, Argentina). (C) 2011 Elsevier Ltd and INQUA. All rights reserved.

Experimental micromorphology in Tierra del Fuego (Argentina): building a reference collection for the study of shell middens in cold climates

Commonly used in archaeological contexts, micromorphology did not see a parallel advance in the field of experimental archaeology. Drawing from early work conducted in the 1990`s on ethnohistoric sites in the Beagle Channel, we analyze a set of 25 thin sections taken from control features and experimental tests. The control features include animal pathways and environmental contexts (beach samples, forest litter, soils from the proximities of archaeological sites), while the experimental samples comprise anthropic structures, such as hearths, and valves of Mytilus edulis (the most important component of shell middens in the region) heated from 200 degrees C to 800 degrees C. Their micromorphological study constitutes a modern analogue to assist archaeologists studying site formation and ethnographical settings in cold climates, with particular emphasis on shell midden contexts. (c) 2010 Elsevier Ltd. All rights reserved.

La industrialización reciente de Tierra del Fuego

Incluye Bibliografía

Integrated reconstruction of Holocene millennial-scale environmental changes in Tierra del Fuego, southernmost South America

This study presents new paleoenvironmental data obtained from sedimentary cores from Lago Fagnano, an elon- gated lake located at 54°S in southernmost South America. Data from palynomorphs (pollen, spores and algae) and associated palynofacies as well as from diatom taxa retrieved from these cores compared with other regional proxies contribute to evaluate the similarities and differences in the climate patterns based on different proxies from southernmost Patagonia. The pollen analysis reveals that a grass steppe environment existed during the early Holocene (11,300–~8000 cal a BP) followed by a major vegetation change characterized by development of forest-steppe ecotone communities between ~8000 and ~6500 cal a BP, under more humid conditions. Between ~ 6500 and ~ 4000 cal a BP, expansion and colonization by Nothofagus forests reflect an increase in effec- tive moisture levels, while openness in the forest communities characterizes the region after ~ 1100 cal a BP. The palynological organic matter combined with the algal content reflects hydrological changes occurring in the lake and its nutrient status, probably in close relation with past climate oscillations. All these past ecological changes are closely related to oscillations in precipitation and temperature as a response to the variations in the latitudinal position and/or strength of the Southern Westerlies wind belt during the Holocene.

Chemical Composition of Fresh Snow from Glaciar Marinelli, Tierra Del Fuego, Chile

A fresh-snow sampling campaign was conducted during the late austral summer of 2006 in the accumulation zone of Glaciar Marinelli, located in the Cordillera Darwin, Tierra del Fuego, Chile. Snow samples were analyzed for stable isotopes (delta(18)O, major soluble ions (Na', K', Ca, Mg, a NO(3)(-), SO(4)(2-), MS(-)) and major and trace elements (Na, Mg, Al, Fe, Ca, Sr, Cd, Cs, Ba, La, Ce, Pr, Dy, Ho, Er, Bi, U, As, Ti, V, Cr, Mn). The dominance of marine chemistry resembles that in studies from Patagonian glaciers. Snow chemistry was dominantly loaded by marine species (Cl(-), Na(+) and ssSO(4)(2-)), while contributions of crustal species (e.g. Al and Fe) were very low. Empirical orthogonal function analysis suggests two possible dust sources, one represented by Al and Fe and the other by La, Ce and Pr. Enrichment-factor calculations suggest the majority of elements are within average upper-crustal ratios, but major enrichments of Bi and Cd (hundreds of times) suggest possible anthropogenic sources. Linear correlation of delta(18)O and barometric pressure (r = 0.60, p < 0.007) suggests a potential 'amount effect' relationship between depleted delta(18)O ratios and stronger storm conditions (e.g. greater precipitation). The snow-chemistry records from Glaciar Marinelli are the first measured in Tierra del Fuego, the southernmost glaciated region outside Antarctica.