997 resultados para Moors and heaths.
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Mode of access: Internet.
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Mode of access: Internet.
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Owing to proximity of the North Atlantic Stream and the shelf, the And circle divide ya biota are assumed to have responded rapidly to climatic changes taking place after the Weichselian glaciation. Palynological, macrofossil, loss-on-ignition, tephra and C-14 data from three sites at the northern part of the island of And circle divide ya were studied. The period 12 300-11 950 cal. yr BP was characterized by polar desert vegetation, and 11 950-11 050 cal. yr BP by a moisture-demanding predominantly low-arctic Oxyria vegetation. During the period 11 050-10 650 cal. yr BP, there was a climatic amelioration towards a sub-arctic climate and heaths dominated by Empetrum. After 10 650 cal. yr BP the Oxyria vegetation disappeared. As early as about 10 800 cal. yr BP the bryozoan Cristatella mucedo indicated a climate sufficient for Betula woodland. However, tree birch did not establish until 10 420-10 250 cal. yr BP, indicating a time-lag for the formation of Betula ecotypes adapted to the oceanic climate of And circle divide ya. From about 10 150 to 9400 cal. yr BP the summers were dry and warm. There was a change towards moister, though comparatively warm, climatic conditions about 9400 cal. yr BP. The present data are compared with evidence from marine sediments and the deglaciation history in the region. It is suggested that during most of the period 11 500-10 250 cal. yr BP a similar situation as in present southern Greenland existed, with birch woodland in the inner fjords near the ice sheet and low-arctic heath vegetation along the outer coast.
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En el presente trabajo nos proponemos abordar algunos aspectos relacionados con las restricciones, los privilegios y la violencia, que se implementaron sobre los mudéjares de Castilla, Aragón y Valencia. En relación con los primeros, daremos cuenta del endurecimiento legal –real y eclesiástico– que se desplegó hacia los moros hispánicos y que regló casi todos los aspectos del vivir cotidiano y de sus prácticas religiosas. Sin embargo, los mudéjares y sus aljamas en algún área en particular, fueron sujetos de privilegios reales. Es por esto que analizaremos restricciones y privilegios como dos caras de un mismo proceso que se desplegó durante el tránsito de la baja edad media. Finalmente, indagaremos sobre los episodios de violencia hacia los mudéjares contrastando particularidades regionales, para conectar estos sucesos con la segregación y la restricción.
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Resumen: El hispanista francés Georges Cirot fue el primero en emplear el término “maurofilia literaria” (maurophilie littéraire) en 1938 para referirse a la representación del valor y la nobleza de los moros en la literatura española del siglo XVI. Pero como señaló Ramón Menéndez Pidal (1957, 202), ya en los siglos XIV y XV los castellanos se habían sentido atraídos por los musulmanes de Granada, por su exótica civilización, su lujo en el vestir, la espléndida ornamentación de sus edificios y su modo de cabalgar, armarse y combatir. Francisco Márquez Villanueva (1984, 117-118) indicó que aunque la literatura maurófila del siglo XVI fue elaborada bajo el signo avanzado del humanismo cristiano, cuyas características fueron “el inconformismo y la sensibilidad para toda suerte de realidades en divergencia del mundo oficial”, las raíces de la maurofilia literaria se encuentran en el viejo romancero fronterizo y morisco elaborado en el siglo XV. En su opinión, el Romancero fue la patria de la “maurofilia pura” y es donde encontramos un cuadro de referencias temáticas “hecho de toponimia y onomástica, armas, indumentaria, policromía y cabalgadas” tendiente a caracterizar al moro como un ser refinado y superior. Para María Rosa Lida (1960, 355), en cambio, la imagen caballeresca del moro se remonta a don Juan Manuel, pues en sus obras aparecen las cortes musulmanas como “centros de molicie refinada y suntuosa”. En efecto, en el Libro de los estados se afirma el valor del moro como guerrero y en el Conde Lucanor aparecen una serie de reyes moros magnánimos y discretos. Sin embargo, el árabe como personaje sabio o “ejemplar” figura ya en una de las fuentes del Conde Lucanor, la Disciplina clericalis, obra compuesta a principios del siglo XII por el judío converso Pedro Alfonso. Por otra parte, el análisis de la representación de los moros en textos épicos, Avengalvón en el Poema de mio Cid y Almanzor en la Los siete infantes de Lara, nos permite descubrir un importante e insoslayable antecedente de la maurofilia de los últimos siglos de la Edad Media
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Esta dissertação tem por objetivo mostrar como o mito de São Tiago Maior e a peregrinação religiosa na Idade Média são retratados na dramaturgia portuguesa e galega. Para isso, reporta-se a duas obras: Auto de Santiago de Afonso Álvares (Portugal - séc. XVI) e O Peregrino errante que cansou ó demo de Xavier Lama (Galícia séc. XX). Objetiva verificar como os discursos das personagens, associados aos demais elementos que estruturam as obras, têm por finalidade acentuar a importância, no contexto da religiosidade ibérica, do culto à Virgem de Guadalupe e de São Tiago em sua tríplice representação: São Tiago Apóstolo, Peregrino ou Mata-mouros. E, sobretudo, demonstrar o caráter doutrinador e moralizante das peças, principalmente na recomendação das virtudes a serem seguidas e dos pecados a serem evitados pelo cristão em sua peregrinação existencial, objetivando a ascenção espiritual
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Brazilian folklore is rich in legends that inhabit in the imaginary of people and are believed to have originated among Brazilian indigenous peoples and the Africans who were enslaved by Portuguese settlers. However, when those stories are compared with the legends of the Iberian Peninsula , one can notice that a lot of elements in the Brazilian legends clearly reflect, for example, aspects of the popular narratives from Galicia and Portugal, such as “The moors” and “Yara’s legend”; “O trasno” and “Saci pererê”. The objective of this paper is to analyze those cultural traces by means of Comparative Literary and Intertextuality analysis, by observing how the context , the ruling ideology, and both social and cultural aspects retake the stories that are known to a certain culture and readapt them according to the traditions of another, thus producing new discourse-texts with local characteristics.
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"Comprising details of the numerous conflicts for its possession between the Moors and the Christians, until its final surrender in 1462; and of subsequent events: with an appendix containing interesting documents."
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Spanish: [v.10] The tall woman, by P.A. de Alarcón. -- The white butterfly, by J. Selgas. -- The organist, by G.A. Becquer. -- Moors and Christians, by P.A. de Alarcón. -- Bread cast upon the waters, by Fernan Caballero.
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Results of a fossil Coleoptera (beetle) fauna from a fen edge sequence from Hatfield Moors, Humberhead Levels, are presented. Mire ontogeny inferred from this location and others are discussed, particularly in the light of previous palynological and plant macrofossil investigations. Peat initiation across most of the site centres around 3000 cal BC, characterised by a Calluna-Eriophorum heath with areas of Pinus-Betula woodland. The onset of peat accumulation on the southern margins of the site was delayed until 1520-1390 cal BC and appears to overlap closely with a recurrence surface at a pollen site (HAT 2) studied by Brian Smith (1985, 2002) dated to 1610-1440 cal BC, suggesting that increased surface wetness may have caused mire expansion at this time. The faunas illustrate the transition from eutrophic and mesotrophic fen to ombrotrophic raised mire, although the significance of both Pinus- and Calluna-indicating species through the sequence suggests that heath habitats may have continued to be important. Elsewhere, this earlier phase of rich fen is lacking and mesotrophic mire developed immediately above nutrient poor sands, with ombrotrophic conditions indicated soon after. Correspondence analysis of the faunas provides valuable insights into the importance of sandy heath habitats on Hatfield Moors. The continuing influence of the underlying coversands suggests these may have been instrumental in mire ontogeny. The research highlights the usefulness of using Coleoptera to assess mire ontogeny, fluctuations in site hydrology and vegetation cover, particularly when used in conjunction with other peatland proxies. The significance of a suite of extinct beetle species is discussed with reference to forest history and climate change.
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Despite the extensive geographical range of palaeolimnological studies designed to assess the extent of surface water acidification in the United Kingdom during the 1980s, little attention was paid to the status of surface waters in the North York Moors (NYM). In this paper, we present sediment core data from a moorland pool in the NYM that provide a record of air pollution contamination and surface water acidification. The 41-cm-long core was divided into three lithostratigraphic units. The lower two comprise peaty soils and peats, respectively, that date to between approximately 8080 and 6740 cal. BP. The uppermost unit comprises peaty lake muds dating from between approximately ad 1790 and the present day (ad 2006). The lower two units contain pollen dominated by forest taxa, whereas the uppermost unit contains pollen indicative of open landscape conditions similar to those of the present. Heavy metal, spheroidal carbonaceous particle, mineral magnetics and stable isotope analysis of the upper sediments show clear evidence of contamination by air pollutants derived from fossil-fuel combustion over the last c. 150years, and diatom analysis indicates that the naturally acidic pool became more acidic during the 20th century. We conclude that the exceptionally acidic surface waters of the pool at present (pH=c. 4.1) are the result of a long history of air pollution and not because of naturally acidic local conditions. We argue that the highly acidic surface waters elsewhere in the NYM are similarly acidified and that the lack of evidence of significant recovery from acidification, despite major reductions in the emissions of acidic gases that have taken place over the last c. 30years, indicates the continuing influence of pollutant sulphur stored in catchment peats, a legacy of over 150years of acid deposition.
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Mode of access: Internet.