247 resultados para Cervus elaphus


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Seleccionado en la convocatoria: Ayudas a la innovación e investigación educativa en centros docentes de niveles no universitarios, Gobierno de Aragón 2010-11

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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A subordem Heteroptera, é o maior táxon dentre os hemimetábolos, composta por sete infraordens, 23 superfamílias e 80 famílias. Dentre estas, Pentatomidae é a quarta família mais numerosa e diversa entre os heterópteros, possuindo 4.100 espécies distribuídas em 760 gêneros e em sete subfamílias. Edessinae possui atualmente cerca de 290 espécies distribuídas em seis gêneros: Edessa, Brachystethus, Peromatus, Olbia, Pantochlora e Doesburgedessa. De todos estes gêneros, Edessa é o que possui o maior número de espécies e o que concentra quase a totalidade dos problemas taxonômicos e nomenclaturas da subfamília. Devido ao seu tamanho, a revisão está sendo feita em partes, a partir do estudo de grupos de espécies unidos por possíveis sinapomorfias. Assim o objetivo geral do trabalho é propor e descrever um novo grupo de espécies com base em uma análise cladística. Para o estudo foram examinados 114 exemplares pertencentes a instituições nacionais e internacionais e a coleções particulares. As descrições seguem um modelo tradicional também usado para Edessinae. São apresentadas medidas e fotografias das espécies, desenhos do processo metasternal e genitália de ambos os sexos, chave dicotômica e mapa de distribuição. Para a analise cladística, foram levantados 22 caracteres morfológicos polarizados através do método do grupo externo, composto pelas espécies: Tibilis sp., Neotibilis fulvicornis, Brachystethus cribrus, Pantochlora vivida, Olbia elegans, Peromatus sp., Doesburgedessa elongatispina, Edessa cervus e Edessa affinis. Através do programa NONA foi obtida uma única árvore mais parcimoniosa, com 30 passos, índice de Consistência de 0,93 e índice de Retenção de 0,97. Com base nessa análise, o monofiletismo do grupo de espécie é confirmado. Assim, o grupo stolida aqui proposto é formado por quatro espécies já descritas Edessa stolida (Linnaeus, 1758), Edessa heymonsi Breddin, 1904, Edessa verhoeffi Breddin, 1904 e Edessa paravinula Barber, 1935 e por cinco espécies novas. O grupo stolida de Edessa é reconhecido pela presença de uma expansão que se projeta da margem lateral da face posterior do segmento X; região mediana do parâmero com uma projeção de formato triangular; ausência de uma faixa ou de tufo de pelos na face posterior do segmento X e gonapófise 8 esclerotizada. As espécies do grupo stolida são muito parecidas externamente e sua identificação só pode ser feita através da análise da genitália externa de ambos os sexos. A análise cladística apóia a idéia tradicional e o grupo stolida deve ser considerado parte do subgênero Hypoxys de Edessa. A topologia do cladograma resultante é (Tibilis sp. + Neotibilis fulvicornis (Brachystethus cribus (Pantochlora vivida ((Doesbuergedessa elongatispina + Edessa cervus (Peromatus sp. + Olbia elegans)) (Edessa affinis ((Edessa sp. nov 3 + Edessa sp. nov 3a) ((Edessa sp. nov 2 (Edessa verhoeffi + Edessa heymonsi)) (Edessa stolida (Edessa sp. nov 4 (Edessa paravinula + Edessa sp. nov 5))))))))). A fêmea de Edessa stolida e o macho de Edessa verhoeffi são descritos pela primeira vez neste trabalho. Os registros de distribuição das espécies são ampliados.

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In the present work Quaternary radiolarian assemblages from the Southwest Pacific were investigated due to their importance for correlation and identification of climatic changes. The studied Ocean Drilling Program (ODP) Site 1123 (Leg 181) is situated on the northern flanks of the Chatham Rise, 1100 kilometres offshore eastern New Zealand and in a water depth o f 3290 metres. It is situated just north of the Subtropical Convergence (STC) in temperate climatic conditions, influenced by the cold deep Deep Western Boundary Current (DWBC) and by the subtropical East Cape Current (ECC) in shallow water depths. A continuous record of 79 sediment samples from this site with a temporal resolution of ~15,000 years provided a medium-resolution record of radiolarian assemblages through the Quaternary. This allowed investigations on how radiolarian assemblages are influenced by climatic variations at obliquity and eccentricity bandwidth, with periodic variations of 40,000, 100,000 and 400,000 years, respectively. Emphasis was given to changes in radiolarian assemblages through the Mid-Pleistocene climate transition (MPT) that marks a fundamental reorganisation in Earth's climate system by change from 40,000 to 100,000 year cycles. Glacial and interglacial variations in oceanography were investigated. Especially the influence of the DWBC was examined due to its input of deep and cold waters to the Pacific Ocean, which plays an important role in Earth's climate system. 167 radiolarian counting groups were examined concerning variations in radiolarian abundance, preservation, diversity, the relative abundance of orders, families, and selected species in order to detect influences of past climatic variations in the Southwest Pacific. No significant changes in radiolarian assemblages were found in coincidence with the onset of the MPT. Investigations led to the recognition of four characteristic phases within the last 1.2 million years. Within one of these phases (Phase Ill), about 160,000 years after the onset of the MPT, fundamental changes in radiolarian assemblages occurred. Investigations yielded highest diversity and highest numbers of nassellarians in abundant samples, whereas sparse samples were mostly poorly preserved and were dominated by spumellarians. Abundance of certain radiolarian families in interglacials or glacials indicated their usefulness as indicators for climatic conditions at Site 1123. Trends o f selected taxa within these families supported the significance of warm- or cool-water preference of these families. Use of 67 radiolarian species as climate indicators showed abundance of warm-water assemblages within interglacials, whereas abundance of cool-water species was increased within glacials. Depth distributional patterns of 52 radiolarian species indicated a strong influence of shallow waters, possibly the EEC, within interglacials and increased influence of deep and intermediate waters, possibly of southern-sourced character and the DWBC in glacial stages.

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The study of radiolarian assemblages from Core MD 962086 provides new information on the variability in the upwelling intensity and origin of upwelled water masses over the past 350 ky in one of the major filamentous regions of the Benguela Upwelling System (BUS), located off Lüderitz, Namibia. The use of key radiolarian species to trace the source of upwelled waters, and the use of a radiolarian-based upwelling index (URI) to reconstruct the upwelling intensity represent the first use of radiolarians for paleoceanographic reconstructions in the BUS. These radiolarian-based proxies indicate strongest upwelling during Marine Isotope Stages (MIS) 3, 5, and 8, which compares well with other studies. While during MIS 3 and 8, the radiolarian-based proxies indicate the influx of waters of Southern Ocean origin, they also point to the increased influence of tropical waters during the lower portion of MIS 5. During MIS 2, 4 and 6 the radiolarian assemblages indicate generally lower upwelling intensities, although this signal is complicated by the increased occurrence of organic carbon in the sediments during these intervals. During MIS 2 there appears to be less of an input of Southern Ocean waters to the BUS, although during the also glacial MIS 4 and 6, there is evidence for an increased influence of cold Antarctic waters. The comparison of the results from Core MD 962086 with other studies in the BUS area indicates a non-uniform pattern of upwelling intensity and advection of cold, southern waters into this system during MIS 2. Weaker upwelling signaled by the radiolarian-based proxy in MIS 4 is in contrast to other studies that indicate higher productivity during this time period. In general, the data show that there is a strong spatiotemporal complexity in upwelling intensity in the BUS and that the advection of water into it is not strongly tied to glacial-interglacial variations in climate.