O PODER DE ZEFERINA NO QUILOMBO DO URUBU UMA RECONSTRUÇÃO HISTÓRICA POLÍTICO-SOCIAL

Os ideais de liberdade exigiram do povo negro diferenciadas práticas para romper com o sistema escravista. Eram as rebeliões em navios, os atos de infanticídio, os justiçamentos dos feitores, as revoltas, além de participações em movimentos libertários e formações de quilombos. Dentre estas formas de organização, o quilombo foi fenômeno essencial nos mais de 300 anos de escravismo no Brasil. Em cada região existiam quilombos, pois para a população negra, cativa ou não, esse era o melhor meio de alcançar a liberdade, um meio coletivo para enfrentar o sistema. O Quilombo do Urubu representou a insistência em garantir a condição humana que o regime escravista negava, sobretudo às mulheres, aos homens e às crianças negras. Essa era uma força que saía de suas entranhas como grito de liberdade, configurada nas fugas em busca de um lugar que lhes assegurasse aproximação de uma vida digna e que pudessem orgulhar-sedo seu porte físico e da sua cultura. Todo esse desprendimento, além de uma força física, exigia um completo conhecimento histórico e espiritual, resguardado pela religiosidade que fortalecia seus espíritos para lutar contra toda negação de humanidade do século XIX no subúrbio da capital baiana. A líder Zeferina, inconformada com a exclusão social de seu povo negro, e entusiasmada pelo poder de herança de ancestralidade, pelo conhecimento de raiz da cultura matrilinear angolana, pelo profundo conhecimento histórico de resistência da rainha Nzinga Mbandi e pela tradição de quilombolas e guerreiras, viveu e lutou pelo sonho de liberdade. Hoje, a chama desse poder é mantida acesa na caminhada de celebração do 20 de novembro pela comunidade de Pirajá e arredores, enquanto referencial de resistência negra na luta contra as exclusões sociais vigentes.(AU)

Polyaromatic hydrocarbons in sediments from the Barents and White Seas

Polycyclic aromatic hydrocarbons (PAHs) are common environmental contaminants which can be derived from anthropogenic sources, such as combustion and discharges from extraction and transport, and natural processes, including leakage and erosion of fossil carbon. Natural PAH sources contribute, along with biological activities and terrestrial run-off, to the organic carbon content in sediments.The Barents Sea region is far from many anthropogenic sources of PAH, but production and trans-shipment of hydrocarbons is increasing. We present data for polycyclic aromatic hydrocarbon (PAH) concentrations in bottom sediments from 510 stations in the Barents and White Seas, and along the northern coast of Norway.

The pathogenesis of migraine - 17th to early 20th Century understandings

The modern understanding of the pathogenesis of migraine, based on the concept that it is a neurovascular disorder, is often thought to have emerged from the work of Harold Wolff in the period 1932-1962. However, over the preceding 300 years, from William Harvey onwards, various hypotheses of the pathogenesis of migraine had been proposed, a few bearing reasonably strong resemblances to Wolff's ideas, though based on less adequate evidence. Many of these earlier hypotheses regarded migraine either primarily as a vascular (e.g., Willis, Wepfer, Latham) or as a neural disorder (e.g., Harvey, Lieving and his 'nerve storms'). There were also variations around these two major themes and in the 19th Century a number of neurovascufar type hypotheses emerged assigning a major role in migraine pathogenesis to the autonomic nervous system. In addition, during the three centuries there were a number of other hypotheses based on different postulated pathogenic mechanisms, some quite ingenious, which had relatively brief vogues. No hypothesis has yet proved capable of explaining all the features of migraine satisfactorily. (c) 2005 Elsevier Ltd. All rights reserved.

Thorium-230 coral chronology of a late prehistoric Hawaiian chiefdom

Documenting the history of settlement in Hawaii during the last few Centuries before European contact, is crucial to charting the evolution of the most complex chiefdom in Polynesia. It is precisely this period that Hawaii. and many Polynesian Societies, Underwent their most rapid changes in political, economic and social organisation. The last similar to 500 to 300 years in the C-14 calibration curve is problematic with wide fluctuations Often rendering large age spans that do not precisely date single events, especially troubling with a culture-historical record of similar to 1000 years duration. Here we present in extremely high precision Th-230 chronology for archaeologically constrained coral samples from a range of occupancy sites. Our high precision dates allow the time of site use to be clearly demonstrated. They also provide the first dates for habitation sites in Hawaii that clearly show contemporaneous occupation-the major problem in settlement pattern archaeology. We demonstrate that two sites were occupied within the same year. Our refined chronology, provides new and exciting oppurtunities for tracking sociopolitical and economic developments during the last few centuries-the crucial period in the evolution and transformation of Polynesian societies. (c) 2005 Elsevier Ltd. All rights reserved.

O PODER DE ZEFERINA NO QUILOMBO DO URUBU UMA RECONSTRUÇÃO HISTÓRICA POLÍTICO-SOCIAL

Os ideais de liberdade exigiram do povo negro diferenciadas práticas para romper com o sistema escravista. Eram as rebeliões em navios, os atos de infanticídio, os justiçamentos dos feitores, as revoltas, além de participações em movimentos libertários e formações de quilombos. Dentre estas formas de organização, o quilombo foi fenômeno essencial nos mais de 300 anos de escravismo no Brasil. Em cada região existiam quilombos, pois para a população negra, cativa ou não, esse era o melhor meio de alcançar a liberdade, um meio coletivo para enfrentar o sistema. O Quilombo do Urubu representou a insistência em garantir a condição humana que o regime escravista negava, sobretudo às mulheres, aos homens e às crianças negras. Essa era uma força que saía de suas entranhas como grito de liberdade, configurada nas fugas em busca de um lugar que lhes assegurasse aproximação de uma vida digna e que pudessem orgulhar-sedo seu porte físico e da sua cultura. Todo esse desprendimento, além de uma força física, exigia um completo conhecimento histórico e espiritual, resguardado pela religiosidade que fortalecia seus espíritos para lutar contra toda negação de humanidade do século XIX no subúrbio da capital baiana. A líder Zeferina, inconformada com a exclusão social de seu povo negro, e entusiasmada pelo poder de herança de ancestralidade, pelo conhecimento de raiz da cultura matrilinear angolana, pelo profundo conhecimento histórico de resistência da rainha Nzinga Mbandi e pela tradição de quilombolas e guerreiras, viveu e lutou pelo sonho de liberdade. Hoje, a chama desse poder é mantida acesa na caminhada de celebração do 20 de novembro pela comunidade de Pirajá e arredores, enquanto referencial de resistência negra na luta contra as exclusões sociais vigentes.(AU)

Sedimentary record of the western Amundsen Sea Embayment after the last glacial maximum

Reliable dating of glaciomarine sediments deposited on the Antarctic shelf since the Last Glacial Maximum (LGM) is very challenging because of the general absence of calcareous (micro-) fossils and the recycling of fossil organic matter. As a consequence, radiocarbon (14C) ages of the acid-insoluble organic fraction (AIO) of the sediments bear uncertainties that are very difficult to quantify. In this paper we present the results of three different chronostratigraphic methods to date a sedimentary unit consisting of diatomaceous ooze and diatomaceous mud that was deposited following the last deglaciation at five core sites on the inner shelf in the western Amundsen Sea (West Antarctica). In three cores conventional 14C dating of the AIO in bulk sediment samples yielded age reversals down-core, but at all sites the AIO 14C ages obtained from diatomaceous ooze within the diatom-rich unit yielded similar uncorrected 14C ages ranging from 13,517±56 to 11,543±47 years before present (yr BP). Correction of these ages by subtracting the core-top ages, which are assumed to reflect present-day deposition (as indicated by 21044 Pb dating of the sediment surface at one core site), yielded ages between ca. 10,500 and 8,400 calibrated years before present (cal yr BP). Correction of the AIO ages of the diatomaceous ooze by only subtracting the marine reservoir effect (MRE) of 1,300 years indicated deposition of the diatom-rich sediments between 14,100 and 11,900 cal yr BP. Most of these ages are consistent with age constraints between 13.0 and 8.0 ka BP for the diatom-rich unit, which we obtained by correlating the relative palaeomagnetic intensity (RPI) records of three of the sediment cores with global and regional reference curves for palaeomagnetic intensity. As a third dating technique we applied conventional 53 radiocarbon dating of the AIO included in acid-cleaned diatom hard parts that were extracted from the diatomaceous ooze. This method yielded uncorrected 14C ages of only 5,111±38 and 5,106±38 yr BP, respectively. We reject these young ages, because they are likely to be overprinted by the adsorption of modern atmospheric carbon dioxide onto the surfaces of the extracted diatom hard parts prior to sample graphitisation and combustion for 14C dating. The deposition of the diatom-rich unit in the western Amundsen Sea suggests deglaciation of the inner shelf before ca. 13 ka BP. The deposition of diatomaceous oozes on other parts of the Antarctic shelf around the same time, however, seems to be coincidental rather than directly related.

Zinc regeneration in rechargeable zinc-air fuel cells:a review

Zinc-air fuel cells (ZAFCs) present a promising energy source with a competing potential with the lithium-ion battery and even with proton-exchange membrane fuel cells (PEMFCs) for applications in next generation electrified transport and energy storage. The regeneration of zinc is essential for developing the next-generation, i.e., electrochemically rechargeable ZAFCs. This review aims to provide a comprehensive view on both theoretical and industrial platforms already built hitherto, with focus on electrode materials, electrode and electrolyte additives, solution chemistry, zinc deposition reaction mechanisms and kinetics, and electrochemical zinc regeneration systems. The related technological challenges and their possible solutions are described and discussed. A summary of important R&D patents published within the recent 10 years is also presented.

Variability of marine climate on the North Icelandic Shelf in a 1357-year proxy archive based on growth increments in the bivalve Arctica islandica

A multicentennial and absolutely-dated shell-based chronology for the marine environment of the North Icelandic Shelf has been constructed using annual growth increments in the shell of the long-lived bivalve clam Arctica islandica. The region from which the shells were collected is close to the North Atlantic Polar Front and is highly sensitive to the varying influences of Atlantic and Arctic water masses. A strong common environmental signal is apparent in the increment widths, and although the correlations between the growth increment indices and regional sea surface temperatures are significant at the 95% confidence level, they are low (r ~ 0.2), indicating that a more complex combination of environmental forcings is driving growth. Remarkable longevities of individual animals are apparent in the increment-width series used in the chronology, with several animals having lifetimes in excess of 300 years and one, at 507 years, being the longest-lived non-colonial animal so far reported whose age at death can be accurately determined. The sample depth is at least three shells after AD 1175, and the time series has been extended back to AD 649 with a sample depth of one or two by the addition of two further series, thus providing a 1357-year archive of dated shell material. The statistical and spectral characteristics of the chronology are investigated by using two different methods of removing the age-related trend in shell growth. Comparison with other proxy archives from the same region reveals several similarities in variability on multidecadal timescales, particularly during the period surrounding the transition from the Medieval Climate Anomaly to the Little Ice Age.

Coral and mollusc resistance to ocean acidification adversely affected by warming, 2011

Increasing atmospheric carbon dioxide (CO2) concentrations are expectedto decrease surface ocean pH by 0.3-0.5 units by 2100, lowering the carbonate ion concentration of surfacewaters. This rapid acidification is predicted to dramatically decrease calcification in many marine organisms. Reduced skeletal growth under increased CO2 levels has already been shown for corals, molluscs and many other marine organisms. The impact of acidification on the ability of individual species to calcify has remained elusive, however, as measuring net calcification fails to disentangle the relative contributions of gross calcification and dissolution rates on growth. Here, we show that corals and molluscs transplanted along gradients of carbonate saturation state at Mediterranean CO2 vents are able to calcify and grow at even faster than normal rates when exposed to the high CO2 levels projected for the next 300 years. Calcifiers remain at risk, however, owing to the dissolution of exposed shells and skeletons that occurs as pH levels fall. Our results show that tissues and external organic layers play a major role in protecting shells and skeletons from corrosive sea water, limiting dissolution and allowing organisms to calcify. Our combined field and laboratory results demonstrate that the adverse effects of global warming are exacerbated when high temperatures coincide with acidification.

Carbonate sedimentation beneath the Carlifornia Current system

A north-south transect of 17 cores was constructed along the eastern boundary of the California Current system from 33° to 42°N to investigate the changes in biogenic sedimentation over the past 30 kyr. Percentages and mass accumulation rates of CaCO3, Corg, and biogenic opal were assembled at 500 to 1000 years/sample to provide relatively high resolution. Time-space maps reveal a complex pattern of changes that do not follow a simple glacial-interglacial two-mode model. Biogenic sedimentation shows responses that are sometimes time-transgressive and sometimes coeval, and most of the responses show more consistency within a limited geographic area than any temporal consistency. Reconstructed conditions during late oxygen isotope stage 3 were more like early Holocene conditions than any other time during the last 30 kyr. Coastal upwelling and productivity during oxygen isotope stage 3 were relatively strong along the central California margin but were weak along the northern California margin. Precipitation increased during the last glacial interval in the central California region, and the waters of the southern California margin had relatively low productivity. Productivity on the southern Oregon margin was relatively low at the beginning of the last glacial interval, but by about 20 ka, productivity in this area significantly increased. This change suggests that the center of the divergence of the West Wind Drift shifted south at this time. The end of the last glacial interval was characterized by increased productivity in the southern California margin and increased upwelling along the central California margin but upwelling remained weak along the northern California margin. A sudden (<300 years) decrease in CaCO3, Corg, and biogenic opal occurred at 13 ka. The changes suggest a major reorientation of the atmospheric circulation in the North Pacific and western North America and the establishment of a strong seasonality in the central California region. A carbonate preservation event occurred at 10 ka that appears to reflect the uptake of CO2 by the terrestrial biosphere as the northern latitudes were reforested following retreat of the glaciers. The Holocene has been a period of relatively high productivity in the southern California margin, relatively strong coastal upwelling along the central California margin, relatively weak upwelling along the northern California margin, and the northward migration of the divergence zone of the West Wind Drift.

Ecosystem structure of Gomishan Wetland

Gomishan Wetland is situated in the extreme southern part of the eastern coast of Caspian Sea. It is connected to the Caspian Sea, so its hydrological features are directly generated from the sea. The whole wetland area (which also consists of the northern part of the wetland that is situated in Turkmenistan republic) is calculated with the aid of the Satellite Images for the years of 1977, 1987 and 1998 respectively 5070, 16320 and 29520 hectares. To have better ideas about food chains in the aquatic ecosystem, five permanent stations was appointed in different parts of the wetland. During one year field study, at the beginning of each month, physical, chemical and biological characteristics of the water and the sediment was surveyed and different specimens were gathered, fixed and took to the laboratories for the relevant analyses. The factors measured in water samples were mainly consist of turbidity, pH, EC, DO, BOD, PO4, NO3, alkalinity, Cl and hardness . The factors measured from sediment samples were the percentage of Sand, Very Fine Sand, Silt, Clay, K, P, N, and Organic Carbon. Biological examinations of the water has been consist of planktonic sample collections, determination, counting and analysis of both phyto and zoo planktons of the wetland. For example the zooplanktons of the Gomishan Wetland are determined in 15 groups, belonging to 5 phyla. The seasonal changes are recognized considerable. The least density of the zooplanktons is occurred in February. The density of most of the groups is seen from the beginning of the summer until the mid autumn. The annual mean density for any 15-zooplankton groups and also the minimum and maximum density with %95 confidences, for each of them, is calculated for the environment of all of the stations and also for the whole wetland. The spatial distribution of the individuals within the population of each of the groups is introduced, according to regular or contagious or random distribution. Diversity indices are calculated for the zooplanktons living in the environment of the stations. Comparison of the wetland, with the southeastern Caspian Sea, from the point of view of zooplankton density and diversity is also obtained. Benthos invertebrates in each station from sediment samples were also extracted. The specimens were colored by Rose Bengal solvent and then were determinate and counted, in separate groups of macro and meio benthos. Among the macro benthos, the highest density was seen in the species of Fyrgula caspia. After that, more density was seen respectively in Apra ovata, Cerastoderma sp., Balanus sp., Nerds divesicolarr, lifytilaster lineatus and Dreissena sp. Among the meio benthos, the most density was seen in Foraminifera and then respectively in Ostracoda, Nernatoda and Bivalve larvae. The indices of diversity and distribution are also calculated. As the birds in this lagoon are of prime importance, all mid winter waterfowl censuses available from recent 13 years are gathered and analysis. Also a whole year (12 times, each at the beginning of one month) waterfowl census was undertaken, throughout the wetland. According to this study, the Eastern Ecosystem of the wetland, is supporting the most population (%75) of the waterfowls, the Middle Open Water Ecosystem and the Western Reed bed Ecosystem, are supporting respectively %14 and %11 of the population. Four of the species are found in the global threatened red list, and the wintering population of the 20 species of the site, in some years, are observed more than %I of the global populations. The Waterfowl Species Diversity and Similarity Indices are given also.

Vida y obra de Don Juan Suárez de Peralta : cronista y protoalbéytar de América : el hombre de las dos España (1541-1613)

Don Juan Suárez de Peralta nació en la ciudad de México-Tenochtitlán en 1541, habiendo sido sus padres Don Juan Suárez Marcayda y Doña Magdalena de Peralta; el padre también conocido como Juan Suárez de Ávila, o como Juan Suárez “El Viejo”, hizo la campaña militar de la conquista del Imperio Azteca como compañero de armas de Don Hernán Cortés. Suárez de Peralta escribió tres grandes obras: “Tractado de Alveiteria” hacia 1575, “Tractado de Cavallería de la Gineta y Brida” en 1580 y “Tractado del Descubrimiento de las Indias y su Conquista” en 1589. Estos tres tratados hacen de Suárez de Peralta, una inevitable y riquísima fuente de información para todo historiador investigando las vetas de la Historia Virreinal Novohispana y de la Historia de España del siglo XVI. Su obra sobre medicina equina y zootecnia de los caballos, es un magnífico y estupendo trabajo que se levanta como el primer libro de su tipo escrito en América. Suárez de Peralta asociado con su hermano mayor, Don Luis, establece un criadero de caballos de raza fina en Tacubaya, en el poniente de la antigua ciudad de México, y es ahí en donde aprende el arte científico de la médica equina, de la reproducción y de la zootecnia caballar y sus habilidades como jinete y gran caballista. En 1579, Don Juan debido a una serie de circunstancias decide exiliarse a España arribando al puerto de Sanlúcar de Barrameda, como huésped en el Palacio de su pariente el VII Conde-Duque de Medina Sidonia, para después habitar en Trujillo y en Sevilla en donde escribe y publica sus otras dos grandes obras. Se muda a Madrid en donde contrae nupcias con una aristócrata dama de la alta nobleza castellana, Doña Isabel Hurtado de Mendoza, perteneciente a la poderosa Casa del Infantado. Con ella procrea un hijo, llamado Don Lorenzo Suárez de Peralta, quien viaja a la Nueva España para tomar posesión de los bienes de su padre, su abuelo y de su tío Luís. Don Juan, nuestro albéitar, quien “alladese enfermo de calenturas”, fallece el 8 de enero de 1613 y es enterrado en la Iglesia del Spiritu Sanctus de los Clérigos Menores en el Madrid de los Austrias. Su manuscrito “Libro de Alveitería”, permaneció olvidado y sin publicar durante más de tres cientos años en la Biblioteca Nacional de Madrid, hasta que finalmente ve la luz en la ciudad de México, en ocasión del Centenario de la fundación de la Escuela Nacional de Medicina Veterinaria y Zootecnia y del IV Centenario de la Real y Pontificia Universidad de México, ahora, Universidad Nacional Autónoma de México (UNAM) en 195

R2P ten years after the World Summit: Explaining ongoing contestation over Pillar III

This article examines how and why contrasting interpretations of the international community’s role in preventing and responding to mass atrocity crimes continue to exist a decade after the Responsibility to Protect (R2P) was unanimously endorsed at the 2005 World Summit. Building on recent critical constructivist insights into the fluid, dynamic nature of norms, it advances two main arguments. The first is that continuing contestation over R2P’s third pillar is a product of a combination of internal and external sources of norm dynamism. R2P’s inherently complex normative structure, coupled with several external factors, including the broader normative environment, norm implementation experiences and a shift in global power towards the BRICS, have contributed to a period of renewed contestation and triggered attempts to re-formulate R2P thorough Brazil’s ‘Responsibility while Protecting’ (RwP) proposal and China’s semi-official ‘Responsible Protection’ concept. The second central argument is that such contestation is affecting R2P’s distinct normative prescriptions in different ways. While resistance to the implementation of coercive pillar III measures is currently impeding the normative progress of that component of the norm, this contestation has not prevented consensual pillar II assistance from becoming more deeply embedded in international practice and discourse.

More than thirty years of ultimatum bargaining experiments: Motives, variations, and a survey of the recent literature

Take-it or leave-it offers are probably as old as mankind. Our objective here is, first, to provide a, probably subjectively colored, recollection of the initial ultimatum game experiment, its motivation and the immediate responses. Second, we discuss extensions of the standard ultimatum bargaining game in a unified framework, and, third, we offer a survey of the experimental ultimatum bargaining literature containing papers published since the turn of the century. The paper argues that the ultimatum game is a versatile tool for research in bargaining and on social preferences. Finally, we provide examples for open research questions and directions for future studies.