903 resultados para Late-colonial period


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This book deals with bodily pain in the late Victorian period, considering the ways in which its understanding is shaped by medicine and theology.

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Lake records from northern Eurasia show regionally coherent patterns of changes during the late Quaternary. Lakes peripheral to the Scandinavian ice sheet were lower than those today but lakes in the Mediterranean zone were high at the glacial maximum, reflecting the dominance of glacial anticyclonic conditions in northern Europe and a southward shift of the Westerlies. The influence of the glacial anticyclonic circulation attenuated through the late glacial period, and the Westerlies gradually shifted northward, such that drier conditions south of the ice sheet were confined to a progressively narrower zone and the Mediterranean became drier. The early Holocene shows a gradual shift to conditions wetter than present in central Asia, associated with the expanded Asian monsoon, and in the Mediterranean, in response to local, monsoon-type circulation. There is no evidence of mid-continental aridity in northern Eurasia during the mid-Holocene. In contrast, the circum-Baltic region was drier, reflecting the increased incidence of blocking anticyclones centered on Scandinavia in summer. There is a gradual transition to modern conditions after ca. 5000 yr B.P. Although these broad-scale patterns are interrupted by shorter term fluctuations, the long-term trends in lake behavior show a clear response to changes in insolation and glaciation.

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Pós-graduação em História - FCHS

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Pós-graduação em Letras - IBILCE

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A historiografia sobre o período colonial na Amazônia supõe uma realidade moldada pela oposição entre um projeto colonial agrícola e a ocorrência de situações concretas de economias extrativistas, a depender da disponbilidade de capital a ser aplicado no principal meio de produção, o escravo negro. De modo que um longo período de escassez de recursos teria conformado o ciclo da economia extrativista na Região dominado pelas "drogas do sertão", substituído por esforços da gestão pombalina por um ciclo agrícola. A gestão pombalina seria a inflexão para uma dinâmica estruturada pela agricultura que, alimentada adiante por conjunturas do mercado mundial, sobretudo as ligadas à guerra da independência americana, só encontraria limitação importante na emergência do novo ciclo extrativista centrado na borracha. Os resultados aqui discutidos não demonstram ser a período pombalino o momento em que, enfim, se estabeleceram os fundamentos da economia amazônica. Trata-se, na verdade, de fundamental e criativo momento de uma trajetória que, todavia, já iniciara quase ¾ de século antes, se impôs ao protagonismo reformador que marcou o período e dele recebeu condicionantes que marcaram indelevelmente a história da Região até os dias atuais.

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The information technology and the increasing interest in the American Latin studies, especially about Brazil, are the objective of these reflections. In the research about the colonial period in Brazil, a group of works, systematized and divulged by electronic means, beyond the usual sources – Portuguese, Italian and Brazilian Universities and Institutes – are from Europe and North America, and its access is facilitated by the worldwide network. Platforms and collections such as Europeana and others less known constitute important sources to the studies of this field. We will comment here some fundamentals to contribute to the subject sources of colonial Brazil.

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Pós-graduação em Artes - IA

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Very well-preserved Pliocene diatoms from a diatomite unit interbedded within glacial sediments at Ocean Drilling Program Site 742 in Prydz Bay, Antarctica are documented and illustrated. The presence of Thalassiosira kolbei, T torokina, Actinocyclus actinochilus, A karstenii and the absence of Nitzschia interfrigidaria, T. insigna and T. vulnifica in Sample 119-742A-15R-4, 44-46 cm constrain its age to ca. 2.2-1.8 Ma (late Pliocene). Diatoms associated with sea ice constitute 35% of the Pliocene diatom assemblage, compared with 71% of the modern sediment assemblage at the site, suggesting that sea ice was present during the late Pliocene period of deposition of the sample, although it probably was not the significant feature it is today.

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PURPOSE: To evaluate the nutritional status of patients in the late postoperative period of pancreaticoduodenectomy (PD) and compare the long-term outcome according to pylorus-preserving (PPPD) or the standard technique (SPD) in which the pylorus is resected. METHODS: This prospective study was conducted twelve months prior or more in patients who had underwent PD (PD Group, n=15) and health volunteers (Control Group, n=15). At a post hoc analysis, the PD Group was divided in PPPD Subgroup (n=9) and SPD Subgroup (n=6), according to the PD techniques. Gastrointestinal complaints and nutritional status were evaluated, apart from a biochemical assessment; Student t-test or Mann-Whitney test were used. RESULTS: The patients recovered their body weight and the gastrointestinal complaints were uncommon. The PD Group showed higher energy and protein intake even though BMI was lower than in Control Group. There were no differences in laboratorial data, except for higher glycemia, serum alkaline phosfatase and C-reactive protein in PD Group. There was no difference in the various parameters evaluated when the Subgroups (PPPD and SPD) were compared. CONCLUSION: For long-term pancreaticoduodenectomy, the gastrointestinal symptoms are minimal and the patients had the clinical and nutritional status preserved, regardless of pylorus preservation.

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The prehistoric cemetery of Barshalder is located along the main road on the boundary between Grötlingbo and Fide parishes, near the southern end of the island of Gotland in the Baltic Sea. The ceme-tery was used from c. AD 1-1100. The level of publication in Swedish archaeology of the first millennium AD is low compared to, for instance, the British and German examples. Gotland’s rich Iron Age cemeteries have long been intensively excavated, but few have received monographic treatment. This publication is intended to begin filling this gap and to raise the empirical level of the field. It also aims to make explicit and test the often somewhat intuitively conceived re-sults of much previous research. The analyses deal mainly with the Migration (AD 375–540), Vendel (AD 520–790) and Late Viking (AD 1000–1150) Periods. The following lines of inquiry have been prioritised. 1. Landscape history, i.e. placing the cemetery in a landscape-historical context. (Vol. 1, section 2.2.6) 2. Migration Period typochronology, i.e. the study of change in the grave goods. (Vol. 2, chapter 2) 3. Social roles: gender, age and status. (Vol. 2, chapter 3) 4. Religious identity in the 11th century, i.e. the study of religious indicators in mortuary cus-toms and grave goods, with particular emphasis on the relationship between Scandinavian paganism and Christianity. (Vol. 2, chapter 4) Barshalder is found to have functioned as a central cemetery for the surrounding area, located on pe-ripheral land far away from contemporary settle-ment, yet placed on a main road along the coast for maximum visibility and possibly near a harbour. Computer supported correspondence analysis and seriation are used to study the gender attributes among the grave goods and the chronology of the burials. New methodology is developed to distin-guish gender-neutral attributes from transgressed gender attributes. Sub-gender grouping due to age and status is explored. An independent modern chronology system with rigorous type definitions is established for the Migration Period of Gotland. Recently published chronology systems for the Vendel and Viking Periods are critically reviewed, tested and modified to produce more solid models. Social stratification is studied through burial wealth with a quantitative method, and the results are tested through juxtaposition with several other data types. The Late Viking Period graves of the late 10th and 11th centuries are studied in relation to the contemporary Christian graves at the churchyards. They are found to be symbolically soft-spoken and unobtrusive, with all pagan attributes kept apart from the body in a space between the feet of the deceased and the end of the over-long inhumation trench. A small number of pagan reactionary graves with more forceful symbolism are however also identified. The distribution of different 11th cen-tury cemetery types across the island is used to in-terpret the period’s confessional geography, the scale of social organisation and the degree of alle-giance to western and eastern Christianity. 11th century society on Gotland is found to have been characterised by religious tolerance, by an absence of central organisation and by slow piecemeal Christianisation.

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Central Switzerland lies tectonically in an intraplate area and recurrence rates of strong earthquakes exceed the time span covered by historic chronicles. However, many lakes are present in the area that act as natural seismographs: their continuous, datable and high-resolution sediment succession allows extension of the earthquake catalogue to pre-historic times. This study reviews and compiles available data sets and results from more than 10 years of lacustrine palaeoseismological research in lakes of northern and Central Switzerland. The concept of using lacustrine mass-movement event stratigraphy to identify palaeo-earthquakes is showcased by presenting new data and results from Lake Zurich. The Late Glacial to Holocene mass-movement units in this lake document a complex history of varying tectonic and environmental impacts. Results include sedimentary evidence of three major and three minor, simultaneously triggered basin-wide lateral slope failure events interpreted as the fingerprints of palaeoseismic activity. A refined earthquake catalogue, which includes results from previous lake studies, reveals a non-uniform temporal distribution of earthquakes in northern and Central Switzerland. A higher frequency of earthquakes in the Late Glacial and Late Holocene period documents two different phases of neotectonic activity; they are interpreted to be related to isostatic post-glacial rebound and relatively recent (re-)activation of seismogenic zones, respectively. Magnitudes and epicentre reconstructions for the largest identified earthquakes provide evidence for two possible earthquake sources: (i) a source area in the region of the Alpine or Sub-Alpine Front due to release of accumulated north-west/south-east compressional stress related to an active basal thrust beneath the Aar massif; and (ii) a source area beneath the Alpine foreland due to reactivation of deep-seated strike-slip faults. Such activity has been repeatedly observed instrumentally, for example, during the most recent magnitude 4.2 and 3.5 earthquakes of February 2012, near Zug. The combined lacustrine record from northern and Central Switzerland indicates that at least one of these potential sources has been capable of producing magnitude 6.2 to 6.7 events in the past.

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The palynostratigraphy of two sediment cores from Soppensee, Central Switzerland (596 m asl) was correlated with nine regional pollen assemblage zones defined for the Swiss Plateau. This biostratigraphy shows that the sedimentary record of Soppensee includes the last 15 000 years, i.e. the entire Late-glacial and Holocene environmental history. The vegetation history of the Soppensee catchment was inferred by pollen and plant-macrofossil analyses on three different cores taken in the deepest part of the lake basin (27 m). On the basis of a high-resolution varve and calibrated radiocarbonchronology it was possible to estimate pollen accumulation rates, which together with the pollen percentage data, formed the basis for the interpretation of the past vegetation dynamics. The basal sediment dates back to the last glacial. After reforestation with juniper and birch at ca. 12 700 B.P., the vegetation changed at around 12 000 B.P. to a pine-birch woodland and at the onset of the Holocene to a mixed deciduous forest. At ca. 7000 B.P., fir expanded and dominated the vegetation with beech becoming predominant at ca. 50014C-years later until sometime during the Iron Age. Large-scale deforestation, especially during the Middle Ages, altered the vegetation cover drastically. During the Late-glacial period two distinct regressive phases in vegetation development are demonstrated, namely, the Aegelsee oscillation (equivalent to the Older Dryas biozone) and the Younger Dryas biozone. No unambiguous evidence for Holocene climatic change was detected at Soppensee. Human presence is indicated by early cereal pollen and distinct pulses of forest clearance as a result of human activity can be observed from the Neolithic period onwards.

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La Universidad Nacional de La Plata y los estudios históricos en la Facultad de Humanidades y Ciencias de la Educación se construyeron con la impronta de Ricardo Levene, la cual dejó su estela por años en muchos de sus discípulos. Dentro de esa escuela histórica se desarrolló y consolidó la figura de Enrique Barba en la ciudad de La Plata y en su Universidad. Sus libros, folletos y colaboraciones suman más de 50 trabajos a lo largo de 55 años de labor, sin embargo en estas líneas que siguen a continuación nos referiremos a su veta menos divulgada y es ella el aporte historiográfico que realizó Enrique Barba para la construcción del pasado colonial rioplatense como también quiénes fueron los que continuaron por el camino que Barba trazó en el campo de los estudios coloniales.

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En este artículo pondremos en tensión la construcción del NOA, Catamarca y específicamente Santa María, a través del tiempo, como ámbitos periféricos desde un punto de vista hegemónico. Desde la perspectiva de la colonialidad del poder, problematizaremos entonces sobre la manera de realizar periodizaciones desde un locus de enunciación que podemos denominar colonialista-capitalista-neoliberal, el que se tornó hegemónico desde la conquista de América. Primero en el período colonial, luego en el desarrollo del capitalismo, y actualmente en el neoliberalismo este locus habilitó una dinámica expropiatoria en el presente vinculada a la mega-minería, que en las últimas dos décadas acentúa la condición de periferia de la región. Esta dinámica entendida como la continuidad de un patrón de poder colonial operó configurando territorios, subjetividades y naturaleza, a lo que agregaremos, la manera de periodizar el tiempo

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Este trabajo tiene como propósito analizar el comportamiento y las estrategias sociales de los portugueses más destacados dentro de la comunidad porteña de Buenos Aires colonial tardío. Para este análisis, debemos tener en cuenta el crecimiento que tuvo la ciudad desde mediados del siglo XVIII lo que se denota claramente en la expansión del comercio atlántico. Es durante ese período que Buenos Aires pierde rápidamente las características de los pueblos predominantemente rurales para adquirir, en forma definitiva, los rasgos de una ciudad.