953 resultados para Terra-cotta sculpture, Ancient.
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Ancient stone monuments (ASMs), such as standing stones and rock art panels, are powerful and iconic expressions of Britain’s rich prehistoric past that have major economic and tourism value. However, ASMs are under pressure due to increasing anthropogenic exposure and changing climatic conditions, which accelerate their rates of disrepair. Although scientific data exists on the integrity of stone monuments, most applies to “built” systems; therefore, additional work specific to ASMs in the countryside is needed to develop better-informed safeguarding strategies. Here, we use Neolithic and Bronze Age rock art panels across Northern England as a case study for delineating ASM management actions required to enhance monument preservation. The state of the rock art is described first, including factors that led to current conditions. Rock art management approaches then are described within the context of future environments, which models suggest to be more dynamic and locally variable. Finally, a Condition Assessment and Risk Evaluation (CARE) scheme is proposed to help prioritise interventions; an example of which is provided based on stone deterioration at Petra in Jordon. We conclude that more focused scientific and behavioural data, specific to deterioration mechanisms, are required for an ASM CARE scheme to be successful.
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Human settlement of Oceania marked the culmination of a global colonization process that began when humans first left Africa at least 90,000 years ago. The precise origins and dispersal routes of the Austronesian peoples and the associated Lapita culture remain contentious, and numerous disparate models of dispersal (based primarily on linguistic, genetic, and archeological data) have been proposed. Here, through the use of mtDNA from 781 modern and ancient Sus specimens, we provide evidence for an early human-mediated translocation of the Sulawesi warty pig (Sus celebensis) to Flores and Timor and two later separate human-mediated dispersals of domestic pig (Sus scrofa) through Island Southeast Asia into Oceania. Of the later dispersal routes, one is unequivocally associated with the Neolithic (Lapita) and later Polynesian migrations and links modern and archeological Javan, Sumatran, Wallacean, and Oceanic pigs with mainland Southeast Asian S. scrofa. Archeological and genetic evidence shows these pigs were certainly introduced to islands east of the Wallace Line, including New Guinea, and that so-called "wild" pigs within this region are most likely feral descendants of domestic pigs introduced by early agriculturalists. The other later pig dispersal links mainland East Asian pigs to western Micronesia, Taiwan, and the Philippines. These results provide important data with which to test current models for human dispersal in the region. © 2007 by The National Academy of Sciences of the USA.
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BACKGROUND: Evolution equipped Bdellovibrio bacteriovorus predatory bacteria to invade other bacteria, digesting and replicating, sealed within them thus preventing nutrient-sharing with organisms in the surrounding environment. Bdellovibrio were previously described as "obligate predators" because only by mutations, often in gene bd0108, are 1 in ~1x10(7) of predatory lab strains of Bdellovibrio converted to prey-independent growth. A previous genomic analysis of B. bacteriovorus strain HD100 suggested that predatory consumption of prey DNA by lytic enzymes made Bdellovibrio less likely than other bacteria to acquire DNA by lateral gene transfer (LGT). However the Doolittle and Pan groups predicted, in silico, both ancient and recent lateral gene transfer into the B. bacteriovorus HD100 genome.
RESULTS: To test these predictions, we isolated a predatory bacterium from the River Tiber- a good potential source of LGT as it is rich in diverse bacteria and organic pollutants- by enrichment culturing with E. coli prey cells. The isolate was identified as B. bacteriovorus and named as strain Tiberius. Unusually, this Tiberius strain showed simultaneous prey-independent growth on organic nutrients and predatory growth on live prey. Despite the prey-independent growth, the homolog of bd0108 did not have typical prey-independent-type mutations. The dual growth mode may reflect the high carbon content of the river, and gives B. bacteriovorus Tiberius extended non-predatory contact with the other bacteria present. The HD100 and Tiberius genomes were extensively syntenic despite their different cultured-terrestrial/freshly-isolated aquatic histories; but there were significant differences in gene content indicative of genomic flux and LGT. Gene content comparisons support previously published in silico predictions for LGT in strain HD100 with substantial conservation of genes predicted to have ancient LGT origins but little conservation of AT-rich genes predicted to be recently acquired.
CONCLUSIONS: The natural niche and dual predatory, and prey-independent growth of the B. bacteriovorus Tiberius strain afforded it extensive non-predatory contact with other marine and freshwater bacteria from which LGT is evident in its genome. Thus despite their arsenal of DNA-lytic enzymes; Bdellovibrio are not always predatory in natural niches and their genomes are shaped by acquiring whole genes from other bacteria.
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Organophosphonates are ancient molecules that contain the chemically stable C–P bond, which is considered a relic of the reducing atmosphere on primitive earth. Synthetic phosphonates now have a wide range of applications in the agricultural, chemical and pharmaceutical industries. However, the existence of C–P compounds as contemporary biogenic molecules was not discovered until 1959, with the identification of 2-aminoethylphosphonic acid in rumen protozoa. Here, we review advances in our understanding of the biochemistry and genetics of microbial phosphonate metabolism, and discuss the role of these compounds and of the organisms engaged in their turnover within the P cycle.
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Recensão do livro "Itineraria Sacra. Bracara Augusta Fidelis et Ancient
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The island of São Jorge (38º 45’ 24’’ N - 28º 20’ 44’’W and 38º 33’ 00’’ N - 27º 44’ 32’’ W) is one of the nine islands of the Azores Archipelago that is rooted in the Azores Plateau, a wide and complex region which encompasses the triple junction between the American, Eurasia and Nubia plates. São Jorge Island has grown by fissural volcanic activity along fractures with the regional WNW-ESE trend, unveiling the importance of the regional tectonics during volcanic activity. The combination of the volcanostratigraphy (Forjaz & Fernandes, 1975; and Madeira, 1998) with geochronological data evidences that the island developed during two main volcanic phases. The first subaerial phase that occurred between 1.32 and 1.21 Ma ago (Hildenbrand et al. 2008) is recorded on the lava sequence forming the cliff at Fajã de São João, while the second phase started at 757 ka ago, is still active, and edified the rest of the island. This second phase edified the east side of the island that corresponds to Topo Volcanic Complex, in the period between 757 and 543 ka ago, while the west side named Rosais Volcanic Complex, started at 368 ka ago (Hildenbrand et al. 2008) and was still active at 117 ka ago. After the onset of Rosais, volcanic activity migrates to the center of São Jorge edifying Manadas Volcanic Complex. The volcanism on São Jorge is dominantly alkaline, with a narrow lithological composition ranging between the basanites/tefrites through the basaltic trachyandesites, in spite of this the two volcanic phases show distinct mineralogical, petrographic and geochemical characteristics that should be related with different petrogenetic conditions and growth rates of the island. Abstract viii During the first volcanic phase, growth rates are faster (≈3.4 m/ka), the lavas are slightly less alkaline and plagioclase-richer, pointing to the existence of a relative shallow and dynamic magma chamber where fractional crystallization associated with gravitational segregation and accumulation processes, produced the lavas of Fajã de São João sequence. The average growth rates during the second volcanic phase are lower (≈1.9 m/ka) and the lavas are mainly alkaline sodic, with a mineralogy composed by olivine, pyroxene, plagioclase and oxide phenocrysts, in a crystalline groundmass. The lavas are characterized by enrichment in incompatible trace element and light REE, but show differences for close-spaced lavas that unveil, in some cases, slight different degrees of fertilization of the mantle source along the island. These differences might also result from higher degrees of partial melting, as observed in the early stages of Topo and Rosais volcanic complexes, of a mantle source with residual garnet and amphibole, and/or from changing melting conditions of the mantle source as pressure. The subtle geochemical differences of the lavas contrast with the isotopic signatures, obtained from Sr-Nd-Pb-Hf isotopes, that São Jorge Island volcanism exhibit along its volcanic complexes. The lavas from Topo Volcanic Complex and from the submarine flank, i.e. the lavas located east of Ribeira Seca Fault, sample a mantle source with similar isotopic signature that, in terms of lead, overlaps Terceira Island. The lavas from Rosais and Manadas volcanic complexes, the western lavas, sample a mantle source that becomes progressively more distinct towards the west end of the island and that, in terms of lead isotopes, trends towards the isotopic composition of Faial Island. The two isotopic signatures of São Jorge, observed from the combination of lead isotopes with the other three systems, seem to result from the mixing of three distinct end-members. These end-members are (1) the common component related with the Azores Plateau and the MAR, (2) the eastern component with a FOZO signature and possibly related with the Azores plume located beneath Terceira, and (3) the western component, similar to Faial, where the lithosphere could have been entrained by an ancient magmatic liquid, isolated for a period longer than 2Ga. The two trends observed in the island reinforce the idea of small-scale mantle heterogeneities beneath the Azores region, as it has been proposed to explain the isotopic diversity observed in the Archipelago.
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«Realismo e Lirismo em Terra Sonâmbula e Chuva Braba» é um trabalho de leitura que reflecte a nossa percepção em relação a dois mundos particulares que se constroem a partir das obras dos dois escritores africanos. Com efeito, optamos por uma estrutura pragmática do estudo, centrando a nossa atenção na leitura e interpretação dos romances, sem incluirmos um capítulo específico de referências teóricas. Tal estratégia permitiu cruzar o quadro conceptual com as informações textuais resultantes do processo de análise e interpretação do «corpus» do trabalho. As duas obras estabelecem pontos de intersecção no domínio linguístico e cultural como consequência de partilha de um passado histórico, político e social. A localização geográfica de Cabo Verde, a fome prolongada, por um lado, e a guerra catastrófica que abalou Moçambique entre 1976 e 1992, por outro, permitiram extrapolar recorrências temáticas inspiradas em impressões e experiências dos autores, relacionadas com práticas e vivências que, no trato literário, ganharam uma dimensão lírico-realista de grande valor hermenêutico. A insularidade e a continentalidade que opõem Cabo Verde e Moçambique, assim como a fome e a guerra que os caracterizam respectivamente, a procura de um espaço literário a partir das marcas de crioulidade e moçambicanidade compõem um conjunto de valores estéticos que configuram o imaginário cultural dos dois países africanos de língua portuguesa. Esta tese pesquisa as imagens e os aspectos fundamentais ínsitos nos dois romances, procurando mostrar até que ponto, a partir de temáticas de fome e guerra se pode construir narrativas lírico-realistas. O estudo permitiu observar que as imagens de sofrimento, desolação e desassossego constituem, geralmente, o paradigma estético da escrita lírica e realista de Mia Couto e Manuel Lopes.
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O sector da construção é responsável por muitos efeitos que são devastadores para o nosso mundo. A terra, como material de construção, proporciona edifícios com impactes incomensuravelmente menores no ambiente, do que os decorrentes da prática construtiva, hoje hegemónica. Trata-se, efectivamente, de uma matéria-prima ecológica, abundante e não tóxica. No entanto, todo o seu potencial de material para a construção de edifícios ambientalmente mais saudáveis é subaproveitado, quando não é complementado com todo um conjunto de procedimentos que intensifiquem a interacção sustentável entre o edifício e o ambiente. Há que saber aproveitar as disposições construtivas da arquitectura vernacular, complementando esse saber empírico, com os conhecimentos científicos e tecnológicos actualmente disponíveis. Desde logo na própria implantação, perfilhando uma perspectiva bioclimática que privilegie a adequação estreita do edifício às características climáticas da zona, em termos de sol, vento e água, e que vise a minimização quer do consumo de energia, quer da necessidade de existência de dispositivos mecânicos, ao mesmo tempo que assegura exigências de conforto. Terão que adoptar-se procedimentos abrangentes, que se incluem em quatro grandes grupos, designadamente: gestão energética, gestão da água, gestão de materiais, gestão de resíduos de construção e demolição. Esta pratica de construção ancestral utiliza uma matéria-prima ecológica, abundante e reutilizável, que possibilita ademais, um excelente comportamento térmico, designadamente através da inércia térmica que proporciona. Para além da beleza estética proporcionada, não contribuindo para a poluição visual que vai proliferando por aí, a construção em terra crua contribui também para a sensibilização dos utentes dos edifícios relativamente à implementação de preocupações ambientais na sua conduta, incentivando práticas diárias mais sustentáveis.
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Dissertação mest., Literatura, Universidade do Algarve, 2007
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O presente trabalho teve como objetivo avaliar a produção de peixes em dois diferentes sistemas de cultivo, policultivo e aquacultura multi-trófica integrada, tomando como referência o crescimento das espécies, o estudo patológico das brânquias e análise de conteúdo estomacal das espécies envolvidas no ensaio (Sparus aurata, Diplodus cervinus, D. puntazzo, D. sargus e D. vulgaris), e por fim foi feita uma abordagem teórica para identificar os custos envolvidos no sistema. Para realização do ensaio foram usados seis tanques, sendo dois tratamentos, em regime triplicado. Os resultados indicam uma boa adaptação dos peixes em ambos os sistemas. A biomassa inicial foi de 0,12 Kg.mˉ3, sendo formada por: 12% Sparus aurata (119,5g), 33% Diplodus puntazzo (134,7g), 45% D. sargus (90,3g), 3% D. cervinus (37,6g) e 7% D. vulgaris (93,1g) e em três tanques também com 42 Kg de Holoturia tubulosa, pepinos do mar, e 75 Kg de Crassostrea angulata, ostras. D. cervinus, D. vulgaris e D. sargus apresentaram baixa taxa de crescimento, ≤ 0,7g/dia, ambas as espécies, e Diplodus cervinus apresentou baixa taxa de sobrevivência em ambos os sistemas (57,8% poli cultivo e 73,3% IMTA). Diplodus puntazzo foi a espécie que melhor se adaptou ao sistema de policultivo simples. Sparus aurata foi a espécie que apresentou melhor taxa de crescimento e melhor taxa de sobrevivência nos dois sistemas. Os conteúdos alimentares apresentaram semelhança entre Diplodus cervinus, D. vulgaris e Sparus aurata, semelhantes também foram os itens alimentares identificados em D. sargus e D. puntazzo, entretanto a preferência alimentar das últimas espécies citadas são opostas as das três primeiras. S. aurata e D. puntazzo que apresentaram maior peso médio foram preferencialmente infestadas por Lamellodiscus spp.. Nas espécies com pesos médios inferiores, como D. cervinus, D. sargus e D. vulgaris foram maiores as infestações por Microcotyle spp.
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Dissertação de mestrado, Ecohidrologia, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2015
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Dissertação de Mestrado, Aquacultura e Pescas, Especialização em Aquacultura, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2015